Sample records for zones annual events

  1. 75 FR 19304 - Safety Zones; Annual Fireworks Events in the Captain of the Port Detroit Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-04-14

    ... zones for annual events in the Captain of the Port Detroit zone. This proposed rule adds events not... proposed rule will add additional events not previously published in the regulations found in 33 CFR 165...-AA00 Safety Zones; Annual Fireworks Events in the Captain of the Port Detroit Zone AGENCY: Coast Guard...

  2. 77 FR 30245 - Safety Zones; Annual Fireworks Events in the Captain of the Port Detroit Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-05-22

    ...-AA00 Safety Zones; Annual Fireworks Events in the Captain of the Port Detroit Zone AGENCY: Coast Guard... by adding three permanent safety zones within the Captain of the Port Detroit Zone. This action is necessary to provide for the safety of life and property on navigable waters during each event. This action...

  3. 78 FR 45059 - Safety Zones; Annual Fireworks Events in the Captain of the Port Buffalo Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-07-26

    ... DEPARTMENT OF HOMELAND SECURITY Coast Guard 33 CFR Part 165 [Docket No. USCG-2012-1084] Safety Zones; Annual Fireworks Events in the Captain of the Port Buffalo Zone AGENCY: Coast Guard, DHS. ACTION: Notice of enforcement of regulation. SUMMARY: At various times throughout the month of July, the Coast...

  4. 78 FR 41846 - Safety Zones; Annual Fireworks Events in the Captain of the Port Buffalo Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-07-12

    ... DEPARTMENT OF HOMELAND SECURITY Coast Guard 33 CFR Part 165 [Docket No. USCG-2012-1084] Safety Zones; Annual Fireworks Events in the Captain of the Port Buffalo Zone AGENCY: Coast Guard, DHS. ACTION: Notice of enforcement of regulation. SUMMARY: At various times throughout the month of July, the Coast...

  5. 76 FR 37649 - Safety Zone; Northern California Annual Fireworks Events, July 4th Fireworks Display

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-06-28

    ... Zone; Northern California Annual Fireworks Events, July 4th Fireworks Display AGENCY: Coast Guard, DHS... annual July 4th Fireworks Display (Tahoe City 4th of July Fireworks Display). This action is necessary to... INFORMATION: The Coast Guard will enforce the safety zone for the annual Tahoe City 4th of July Fireworks in...

  6. 76 FR 37646 - Safety Zone; Northern California Annual Fireworks Events, Fourth of July Fireworks, City of...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-06-28

    ... Zone; Northern California Annual Fireworks Events, Fourth of July Fireworks, City of Sausalito... Guard will enforce the Fourth of July Fireworks, City of Sausalito annual safety zone. This action is... through, or anchoring in the safety zone, unless authorized by the Patrol Commander (PATCOM). DATES: The...

  7. 76 FR 37646 - Safety Zone; Northern California Annual Fireworks Events, Fourth of July Fireworks, Lake Tahoe, CA

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-06-28

    ... Zone; Northern California Annual Fireworks Events, Fourth of July Fireworks, Lake Tahoe, CA AGENCY... annual safety zone for the Fourth of July Fireworks, Lake Tahoe, California, located off Incline Village...,000 foot safety zone for the annual Fourth of July Fireworks Display in 33 CFR 165.1191 on July 4...

  8. 75 FR 35649 - Safety Zone; Northern California Annual Fireworks Events, July 4th Fireworks Display

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-06-23

    ... Zone; Northern California Annual Fireworks Events, July 4th Fireworks Display AGENCY: Coast Guard, DHS. ACTION: Notice of enforcement of regulation. SUMMARY: The Coast Guard will enforce the Tahoe City 4th of... safety zone for the annual Tahoe City 4th of July Fireworks in 33 CFR 165.1191 on July 4, 2010, from 9 a...

  9. 76 FR 37650 - Safety Zone; Northern California Annual Fireworks Events, Fourth of July Fireworks, South Lake...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-06-28

    ... Zone; Northern California Annual Fireworks Events, Fourth of July Fireworks, South Lake Tahoe Gaming... will enforce the safety zone for the annual Fourth of July Fireworks, South Lake Tahoe Gaming Alliance (Lights on the Lake Fireworks Display). This action is necessary to control vessel traffic and to ensure...

  10. 75 FR 35652 - Safety Zone; Northern California Annual Fireworks Events, Fourth of July Fireworks, South Lake...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-06-23

    ... Zone; Northern California Annual Fireworks Events, Fourth of July Fireworks, South Lake Tahoe Gaming... will enforce Lights on the Lake Fireworks Display safety zone for South Lake Tahoe, from 8:30 a.m. on... the Lake Fireworks in 33 CFR 165.1191 on July 4, 2010, from 8:30 a.m. on July 1, 2010 through 10 p.m...

  11. 33 CFR 100.1101 - Southern California annual marine events for the San Diego Captain of the Port Zone.

    Code of Federal Regulations, 2013 CFR

    2013-07-01

    ... events for the San Diego Captain of the Port Zone. 100.1101 Section 100.1101 Navigation and Navigable... NAVIGABLE WATERS § 100.1101 Southern California annual marine events for the San Diego Captain of the Port... 83] 1. San Diego Fall Classic Sponsor San Diego Rowing Club. Event Description Competitive rowing...

  12. 33 CFR 100.1101 - Southern California annual marine events for the San Diego Captain of the Port Zone.

    Code of Federal Regulations, 2012 CFR

    2012-07-01

    ... events for the San Diego Captain of the Port Zone. 100.1101 Section 100.1101 Navigation and Navigable... NAVIGABLE WATERS § 100.1101 Southern California annual marine events for the San Diego Captain of the Port... 83] 1. San Diego Fall Classic Sponsor San Diego Rowing Club. Event Description Competitive rowing...

  13. 33 CFR 100.1104 - Southern California Annual Marine Events for the Los Angeles Long Beach Captain of the Port Zone.

    Code of Federal Regulations, 2014 CFR

    2014-07-01

    ... Events for the Los Angeles Long Beach Captain of the Port Zone. 100.1104 Section 100.1104 Navigation and... NAVIGABLE WATERS § 100.1104 Southern California Annual Marine Events for the Los Angeles Long Beach Captain... Description Competitive long distance sailboat race from Los Angeles to Honolulu. Date Bi-annually in early...

  14. 78 FR 69007 - Special Local Regulations; Eleventh Coast Guard District Annual Marine Events

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-11-18

    ... marine events that occur annually within the Eleventh Coast Guard District. These updates include adding..., Southern California annual marine events for the San Diego Captain of the Port zone, by adding 12 new... Diego Captain of the Port zone, by adding 9 new events and updating 1 event with [[Page 69009

  15. 78 FR 35790 - Safety Zones; Recurring Events in Captain of the Port Boston Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-06-14

    ...: Notice of proposed rulemaking. SUMMARY: The Coast Guard proposes to add three new permanent safety zones... during annual recurring events. These three permanent safety zones would expedite public notification of..., Coast Guard Sector Boston Waterways Management Division, telephone 617-223-4000, email Mark.E.Cutter...

  16. 76 FR 37649 - Safety Zone; Northern California Annual Fireworks Events, Independence Day Fireworks

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-06-28

    ... Independence Day Fireworks (Kings Beach 4th of July Fireworks) safety zone. This action is necessary to control... . SUPPLEMENTARY INFORMATION: The Coast Guard will enforce the safety zone for the annual Kings Beach 4th of July...

  17. 78 FR 40961 - Safety Zones; Annual Events in the Captain of the Port Detroit Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-07-09

    ... events: (1) Bay-Rama Fishfly Festival Fireworks, New Baltimore, MI. The safety zone listed in 33 CFR 165... Festival Fireworks, Lexington, MI. The safety zone listed in 33 CFR 165.941(a)(42) will be enforced from 10.... until 11:00 p.m. on July 20, 2013. (14) Detroit International Jazz Festival Fireworks, Detroit, MI. The...

  18. 76 FR 50669 - Safety Zones; Eleventh Coast Guard District Annual Fireworks Events

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-08-16

    ... occurring, add new unlisted annual fireworks events to the regulations, and standardize the format for all... to be added. In addition, information for those events that continue to occur has changed in some... sections will be updated or added as follows: update with current information existing events, add...

  19. 75 FR 35650 - Safety Zone; Northern California Annual Fireworks Events, Independence Day Fireworks

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-06-23

    .... ACTION: Notice of enforcement of regulation. SUMMARY: The Coast Guard will enforce Kings Beach 4th of... will enforce the safety zone for the annual Kings Beach 4th of July Fireworks in 33 CFR 165.1191 on...

  20. PEER Annual Meeting | Events

    Science.gov Websites

    window. 2018 PEER Annual Meeting, Jan 18-19, 2018 in Berkeley, CA 2016 PEER Annual Meeting, Jan 28-29 home about peer news events research products laboratories publications nisee b.i.p. members education FAQs links Events Calendar of PEER and Other Events PEER Events Archive PEER Annual Meeting 2009

  1. 33 CFR 165.941 - Safety Zones; Annual Fireworks Events in the Captain of the Port Detroit Zone.

    Code of Federal Regulations, 2011 CFR

    2011-07-01

    ... will be determined annually. (4) The Old Club Fireworks, Harsens Island, MI: (i) Location: All waters...′ N, 082°40.1′ W (NAD 83). This area is located near the southern end of Harsen's Island, MI. (ii... dates and times for this event will be determined annually. (11) Nautical Mile Venetian Festival...

  2. 33 CFR 165.941 - Safety Zones; Annual Fireworks Events in the Captain of the Port Detroit Zone.

    Code of Federal Regulations, 2010 CFR

    2010-07-01

    ... times for this event will be determined annually. (5) Alpena Fireworks, Alpena, MI: (i) Location: All... Alpena, MI. (ii) Expected date: One evening during the last week in of June or the first week of July...

  3. 78 FR 20277 - Safety Zones & Special Local Regulations; Recurring Marine Events in Captain of the Port Long...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-04-04

    ...The Coast Guard proposes to add, delete, and modify safety zones and special local regulations and add language to clarify time frames and notification requirements for annual marine events in the Sector Long Island Sound Captain of the Port (COTP) Zone. When these regulated areas are activated and subject to enforcement, this rule would restrict vessels from portions of water areas during these recurring events. The safety zones and special local regulations will facilitate public notification of events and provide protective measures for the maritime public and event participants from the hazards associated with these recurring events.

  4. 75 FR 32666 - Safety Zones; Annual Fireworks Events in the Captain of the Port Detroit Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-06-09

    ... Events in the Captain of the port Detroit Zone in the Federal Register (75 FR 19304). We received zero.... Discussion of Comments and Changes We received zero comments regarding the proposed rule. There are no...-3520). We received zero comments regarding the proposed rule. Federalism A rule has implications for...

  5. 33 CFR 165.1123 - Southern California Annual Firework Events for the San Diego Captain of the Port Zone.

    Code of Federal Regulations, 2012 CFR

    2012-07-01

    ... Firework Events for the San Diego Captain of the Port Zone. 165.1123 Section 165.1123 Navigation and... Diego Captain of the Port Zone. (a) General. Safety zones are established for the events listed in Table..., or local agencies. Table 1 to § 165.1123 [All coordinates referenced use datum NAD 83.] 1. San Diego...

  6. 33 CFR 165.1123 - Southern California Annual Firework Events for the San Diego Captain of the Port Zone.

    Code of Federal Regulations, 2013 CFR

    2013-07-01

    ... Firework Events for the San Diego Captain of the Port Zone. 165.1123 Section 165.1123 Navigation and... Diego Captain of the Port Zone. (a) General. Safety zones are established for the events listed in Table..., or local agencies. Table 1 to § 165.1123 [All coordinates referenced use datum NAD 83.] 1. San Diego...

  7. 33 CFR 165.173 - Safety Zones for annually recurring marine events held in Coast Guard Southeastern New England...

    Code of Federal Regulations, 2014 CFR

    2014-07-01

    ... recurring marine events held in Coast Guard Southeastern New England Captain of the Port Zone. 165.173... recurring marine events held in Coast Guard Southeastern New England Captain of the Port Zone. (a... to the fireworks displays and swim events listed in the Table to § 165.173. These regulations may be...

  8. 76 FR 26931 - Safety Zone; Second Annual Space Coast Super Boat Grand Prix, Atlantic Ocean, Cocoa Beach, FL

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-05-10

    ...-AA00 Safety Zone; Second Annual Space Coast Super Boat Grand Prix, Atlantic Ocean, Cocoa Beach, FL... Annual Space Coast Super Boat Grand Prix. The Second Annual Space Coast Super Boat Grand Prix will consist of a series of high- speed boat races. The event is scheduled to take place on Saturday, May 21...

  9. 78 FR 41299 - Regattas and Marine Parades; Great Lakes Annual Marine Events

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-07-10

    ... and Marine Parades; Great Lakes Annual Marine Events AGENCY: Coast Guard, DHS. ACTION: Notice of... regattas and marine parades in the Captain of the Port Detroit zone from 9:00 a.m. on June 21, 2013 through... navigable waters immediately prior to, during, and immediately after regattas or marine parades. Enforcement...

  10. 77 FR 37318 - Eighth Coast Guard District Annual Safety Zones; Sound of Independence; Santa Rosa Sound; Fort...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-06-21

    ...-AA00 Eighth Coast Guard District Annual Safety Zones; Sound of Independence; Santa Rosa Sound; Fort... Coast Guard will enforce a Safety Zone for the Sound of Independence event in the Santa Rosa Sound, Fort... during the Sound of Independence. During the enforcement period, entry into, transiting or anchoring in...

  11. 75 FR 47215 - Special Local Regulation; Marine Events Within the Captain of the Port Sector Boston Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-08-05

    ... special local regulations within the Captain of the Port Sector Boston Zone for several swim events and... vessels during annual swim and high speed races that may pose a hazard to the public in the Captain of the..., and after the events. The Captain of the Port will inform the public about the details of each swim...

  12. 78 FR 13811 - Special Local Regulation; Annual Marine Events on the Colorado River, Between Davis Dam (Bullhead...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-03-01

    ... DEPARTMENT OF HOMELAND SECURITY Coast Guard 33 CFR Part 100 [Docket No. USCG-2012-1094] Special Local Regulation; Annual Marine Events on the Colorado River, Between Davis Dam (Bullhead City, AZ) and Headgate Dam (Parker, AZ) Within the San Diego Captain of the Port Zone AGENCY: Coast Guard, DHS. ACTION...

  13. 77 FR 67563 - Special Local Regulation; Annual Marine Events on the Colorado River, Between Davis Dam (Bullhead...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-11-13

    ... DEPARTMENT OF HOMELAND SECURITY Coast Guard 33 CFR Part 100 [Docket No. USCG-2012-0925] Special Local Regulation; Annual Marine Events on the Colorado River, Between Davis Dam (Bullhead City, AZ) and Headgate Dam (Parker, AZ) Within the San Diego Captain of the Port Zone AGENCY: Coast Guard, DHS. ACTION...

  14. 33 CFR 165.173 - Safety Zones for annually recurring marine events held in Coast Guard Southeastern New England...

    Code of Federal Regulations, 2013 CFR

    2013-07-01

    ....0JUNE 6.1Oak Bluffs Summer Solstice • Event Type: Fireworks Display. • Date: One night on the 3rd or 4th... Zone Dimension: Approximately 1000 yards long by 1000 yards wide. 7.0JULY 7.1Marion 4th of July... barge. 7.2Oyster Harbors July 4th Festival • Event Type: Fireworks Display. • Date: One night between...

  15. 33 CFR 165.173 - Safety Zones for annually recurring marine events held in Coast Guard Southeastern New England...

    Code of Federal Regulations, 2012 CFR

    2012-07-01

    ....0JUNE 6.1Oak Bluffs Summer Solstice • Event Type: Fireworks Display. • Date: One night on the 3rd or 4th... Zone Dimension: Approximately 1000 yards long by 1000 yards wide. 7.0JULY 7.1Marion 4th of July... barge. 7.2Oyster Harbors July 4th Festival • Event Type: Fireworks Display. • Date: One night between...

  16. 75 FR 52465 - Safety Zones; Swim Events Within the Sector New York Captain of the Port Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-08-26

    ...-AA00 Safety Zones; Swim Events Within the Sector New York Captain of the Port Zone AGENCY: Coast Guard... zones for swim events occurring on waters of the Hudson River, East River and Long Island Sound. These... with the swim events. Persons and vessels are prohibited from entering into, transiting through, or...

  17. 78 FR 26293 - Safety Zones; Annual Events in the Captain of the Port Detroit Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-05-06

    ... be determined annually. (2) BGSU Football Gridiron Classic Golf and Dinner Fireworks, Catawba Island.... The exact dates and times will be determined annually. (61) BGSU Football Gridiron Classic Golf and...

  18. 77 FR 42176 - Safety Zones; Annual Fireworks Events in the Captain of the Port Detroit Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-07-18

    ... fireworks launch site located at position 41-34'-18.10'' N, 082-51'-18.70'' W (NAD 83). This zone will be... fireworks launch site located at position 41-39'- 19'' N, 082-48'-57'' W (NAD 83). This zone will be...'' W (NAD 83). This zone will be enforced one evening during the first week in July. The safety zone...

  19. 76 FR 55566 - Safety Zones; Fireworks Displays and Surfing Events in Captain of the Port Long Island Sound Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-09-08

    ...-AA00 Safety Zones; Fireworks Displays and Surfing Events in Captain of the Port Long Island Sound Zone... zones for marine events within the Captain of the Port (COTP) Long Island Sound Zone for a surfing event... unless authorized by the COTP Sector Long Island Sound. DATES: This rule is effective in the CFR on...

  20. 78 FR 74048 - Eleventh Coast Guard District Annual Fireworks Events

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-12-10

    .... The first proposed safety zone is for the ``Big Bay Boom Fourth of July Fireworks'' event occurring one evening during the first week of July in San Diego Bay. This event requires four 1,000 foot radius... events. The first proposed safety zone is for the ``Colorado Belle & Edgewater Hotel/Casino Thanksgiving...

  1. 75 FR 35651 - Safety Zone, Long Island Sound Annual Fireworks Displays

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-06-23

    ... Zone, Long Island Sound Annual Fireworks Displays AGENCY: Coast Guard, DHS. ACTION: Notice of... thirteen fireworks displays taking place throughout the Sector Long Island Sound Captain of the Port Zone... Sector Long Island Sound (203) 468 4454 [email protected] . SUPPLEMENTARY INFORMATION: The Coast...

  2. 33 CFR 165.151 - Safety Zones; Long Island Sound annual fireworks displays.

    Code of Federal Regulations, 2011 CFR

    2011-07-01

    ....5″ W; and barge two, 41°20′51.75″ N, 72°05′18.90″ W. (11) Harbor Day Fireworks Safety Zone. All... 33 Navigation and Navigable Waters 2 2011-07-01 2011-07-01 false Safety Zones; Long Island Sound... § 165.151 Safety Zones; Long Island Sound annual fireworks displays. (a) Safety Zones. The following...

  3. 33 CFR 165.151 - Safety Zones; Long Island Sound annual fireworks displays.

    Code of Federal Regulations, 2010 CFR

    2010-07-01

    ....5″ W; and barge two, 41°20′51.75″ N, 72°05′18.90″ W. (11) Harbor Day Fireworks Safety Zone. All... 33 Navigation and Navigable Waters 2 2010-07-01 2010-07-01 false Safety Zones; Long Island Sound... § 165.151 Safety Zones; Long Island Sound annual fireworks displays. (a) Safety Zones. The following...

  4. 78 FR 41694 - Safety Zone; Fireworks Events in Captain of the Port New York Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-07-11

    ... Zone; Fireworks Events in Captain of the Port New York Zone AGENCY: Coast Guard, DHS. ACTION: Notice of enforcement of regulation. SUMMARY: The Coast Guard will enforce safety zones in the Captain of the Port New York Zone on the specified dates and times. This action is necessary to ensure the safety of vessels...

  5. A viscoplastic shear-zone model for episodic slow slip events in oceanic subduction zones

    NASA Astrophysics Data System (ADS)

    Yin, A.; Meng, L.

    2016-12-01

    Episodic slow slip events occur widely along oceanic subduction zones at the brittle-ductile transition depths ( 20-50 km). Although efforts have been devoted to unravel their mechanical origins, it remains unclear about the physical controls on the wide range of their recurrence intervals and slip durations. In this study we present a simple mechanical model that attempts to account for the observed temporal evolution of slow slip events. In our model we assume that slow slip events occur in a viscoplastic shear zone (i.e., Bingham material), which has an upper static and a lower dynamic plastic yield strength. We further assume that the hanging wall deformation is approximated as an elastic spring. We envision the shear zone to be initially locked during forward/landward motion but is subsequently unlocked when the elastic and gravity-induced stress exceeds the static yield strength of the shear zone. This leads to backward/trenchward motion damped by viscous shear-zone deformation. As the elastic spring progressively loosens, the hanging wall velocity evolves with time and the viscous shear stress eventually reaches the dynamic yield strength. This is followed by the termination of the trenchward motion when the elastic stress is balanced by the dynamic yield strength of the shear zone and the gravity. In order to account for the zig-saw slip-history pattern of typical repeated slow slip events, we assume that the shear zone progressively strengthens after each slow slip cycle, possibly caused by dilatancy as commonly assumed or by progressive fault healing through solution-transport mechanisms. We quantify our conceptual model by obtaining simple analytical solutions. Our model results suggest that the duration of the landward motion increases with the down-dip length and the static yield strength of the shear zone, but decreases with the ambient loading velocity and the elastic modulus of the hanging wall. The duration of the backward/trenchward motion depends

  6. 78 FR 57482 - Safety Zone; Fireworks Event in Captain of the Port New York Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-09-19

    ... York Zone on the specified date and time. This action is necessary to ensure the safety of vessels and... regulation for the safety zone described in 33 CFR 165.160 will be enforced on the date and time listed in... Zone; Fireworks Event in Captain of the Port New York Zone AGENCY: Coast Guard, DHS. ACTION: Notice of...

  7. 77 FR 59551 - Safety Zone; Fireworks Event in Captain of the Port New York Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-09-28

    ... Zone; Fireworks Event in Captain of the Port New York Zone AGENCY: Coast Guard, DHS. ACTION: Notice of enforcement of regulation. SUMMARY: The Coast Guard will enforce a safety zone in the Captain of the Port New York Zone on the specified date and time. This action is necessary to ensure the safety of vessels and...

  8. 33 CFR 165.941 - Safety Zones; Annual Events in the Captain of the Port Detroit Zone.

    Code of Federal Regulations, 2014 CFR

    2014-07-01

    ... will be determined annually. (4) The Old Club Fireworks, Harsens Island, MI: (i) Location: All waters...′ N, 082°40.1′ W (NAD 83). This area is located near the southern end of Harsens Island, MI. (ii... determined annually. (10) Nautical Mile Venetian Festival Fireworks, St. Clair Shores, MI: (i) Location: All...

  9. 33 CFR 165.941 - Safety Zones; Annual Events in the Captain of the Port Detroit Zone.

    Code of Federal Regulations, 2013 CFR

    2013-07-01

    ... will be determined annually. (4) The Old Club Fireworks, Harsens Island, MI: (i) Location: All waters...′ N, 082°40.1′ W (NAD 83). This area is located near the southern end of Harsens Island, MI. (ii... determined annually. (10) Nautical Mile Venetian Festival Fireworks, St. Clair Shores, MI: (i) Location: All...

  10. 33 CFR 165.941 - Safety Zones; Annual Events in the Captain of the Port Detroit Zone.

    Code of Federal Regulations, 2012 CFR

    2012-07-01

    ... will be determined annually. (4) The Old Club Fireworks, Harsens Island, MI: (i) Location: All waters...′ N, 082°40.1′ W (NAD 83). This area is located near the southern end of Harsens Island, MI. (ii... determined annually. (10) Nautical Mile Venetian Festival Fireworks, St. Clair Shores, MI: (i) Location: All...

  11. 77 FR 75559 - Safety Zone; Fireworks Event in Captain of the Port New York Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-12-21

    ... DEPARTMENT OF HOMELAND SECURITY Coast Guard 33 CFR Part 165 [Docket No. USCG-2012-1064] Safety Zone; Fireworks Event in Captain of the Port New York Zone AGENCY: Coast Guard, DHS. ACTION: Notice of enforcement of regulation. SUMMARY: The Coast Guard will enforce a safety zone in the Captain of the Port New...

  12. 76 FR 34867 - Safety Zones; Annual Fireworks Events in the Captain of the Port Detroit Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-06-15

    ....941(a)(30) Bay-Rama Fishfly Festival Fireworks, New Baltimore, MI This safety zone will be enforced...) Bay City Fireworks Festival, Bay City, MI This safety zone will be enforced daily from 9:30 p.m. to 11...:45 p.m. to 10:45 p.m. on July 3, 2011. Section 165.941(a)(43) Lexington Independence Festival...

  13. 76 FR 44531 - Safety Zone; Fourth Annual Chillounge Night St. Petersburg Fireworks Display, Tampa Bay, St...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-07-26

    ...-AA00 Safety Zone; Fourth Annual Chillounge Night St. Petersburg Fireworks Display, Tampa Bay, St... proposes to establish a temporary safety zone on the waters of Tampa Bay in St. Petersburg, Florida during the Fourth Annual Chillounge Night St. Petersburg Fireworks Display on Saturday, November 19, 2011...

  14. 76 FR 68098 - Safety Zone; Fourth Annual Chillounge Night St. Petersburg Fireworks Display, Tampa Bay, St...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-11-03

    ...-AA00 Safety Zone; Fourth Annual Chillounge Night St. Petersburg Fireworks Display, Tampa Bay, St... Guard is establishing a temporary safety zone on the waters of Tampa Bay in St. Petersburg, Florida during the Fourth Annual Chillounge Night St. Petersburg Fireworks Display on Saturday, November 19, 2011...

  15. Isotropic events observed with a borehole array in the Chelungpu fault zone, Taiwan.

    PubMed

    Ma, Kuo-Fong; Lin, Yen-Yu; Lee, Shiann-Jong; Mori, Jim; Brodsky, Emily E

    2012-07-27

    Shear failure is the dominant mode of earthquake-causing rock failure along faults. High fluid pressure can also potentially induce rock failure by opening cavities and cracks, but an active example of this process has not been directly observed in a fault zone. Using borehole array data collected along the low-stress Chelungpu fault zone, Taiwan, we observed several small seismic events (I-type events) in a fluid-rich permeable zone directly below the impermeable slip zone of the 1999 moment magnitude 7.6 Chi-Chi earthquake. Modeling of the events suggests an isotropic, nonshear source mechanism likely associated with natural hydraulic fractures. These seismic events may be associated with the formation of veins and other fluid features often observed in rocks surrounding fault zones and may be similar to artificially induced hydraulic fracturing.

  16. 75 FR 41762 - Safety Zone; Annual Kennewick, WA, Columbia Unlimited Hydroplane Races, Kennewick, WA

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-07-19

    ...-AA00 Safety Zone; Annual Kennewick, WA, Columbia Unlimited Hydroplane Races, Kennewick, WA AGENCY..., Columbia Unlimited Hydroplane Races'' also known as the Tri-City Water Follies Hydroplane Races. The safety... Association hosts annual hydroplane races on the Columbia River in Kennewick, Washington. The Association is...

  17. 76 FR 70882 - Safety Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-11-16

    ... Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of Responsibility... published in the Federal Register on October 4, 2011, for the Safety Zones; Annual Firework Displays Within...-6323, email [email protected] . If you have questions on viewing the docket, call Renee V...

  18. 77 FR 38179 - Safety Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-06-27

    ... Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of Responsibility... enforce the safety zones for annual firework displays in the Captain of the Port, Puget Sound area of... prohibited unless authorized by the Captain of the Port, Puget Sound or his Designated Representative. DATES...

  19. Relationships between Tropical Rainfall Events and Regional Annual Rainfall Anomalies

    NASA Astrophysics Data System (ADS)

    Painter, C.; Varble, A.; Zipser, E. J.

    2016-12-01

    Regional annual precipitation anomalies strongly impact the health of regional ecosystems, water resources, agriculture, and the probability of flood and drought conditions. Individual event characteristics, including rain rate, areal coverage, and stratiform fraction are also crucial in considering large-scale impacts on these resources. Therefore, forecasting individual event characteristics is important and could potentially be improved through correlation with longer and better predicted timescale environmental variables such as annual rainfall. This study examines twelve years of retrieved rainfall characteristics from the Tropical Rainfall Measuring Mission (TRMM) satellite at a 5° x 5° resolution between 35°N and 35°S, as a function of annual rainfall anomaly derived from Global Precipitation Climatology Project data. Rainfall event characteristics are derived at a system scale from the University of Utah TRMM Precipitation Features database and at a 5-km pixel scale from TRMM 2A25 products. For each 5° x 5° grid box and year, relationships between these characteristics and annual rainfall anomaly are derived. Additionally, years are separated into wet and dry groups for each grid box and are compared versus one another. Convective and stratiform rain rates, along with system area and volumetric rainfall, generally increase during wetter years, and this increase is most prominent over oceans. This is in agreement with recent studies suggesting that convective systems become larger and rainier when regional annual rainfall increases or when the climate warms. Over some land regions, on the other hand, system rain rate, volumetric rainfall, and area actually decrease as annual rainfall increases. Therefore, land and ocean regions generally exhibit different relationships. In agreement with recent studies of extreme rainfall in a changing climate, the largest and rainiest systems increase in relative size and intensity compared to average systems, and do

  20. Slow slip events and seismic tremor at circum-Pacific subduction zones

    NASA Astrophysics Data System (ADS)

    Schwartz, Susan Y.; Rokosky, Juliana M.

    2007-09-01

    It has been known for a long time that slip accompanying earthquakes accounts for only a fraction of plate tectonic displacements. However, only recently has a fuller spectrum of strain release processes, including normal, slow, and silent earthquakes (or slow slip events) and continuous and episodic slip, been observed and generated by numerical simulations of the earthquake cycle. Despite a profusion of observations and modeling studies the physical mechanism of slow slip events remains elusive. The concurrence of seismic tremor with slow slip episodes in Cascadia and southwestern Japan provides insight into the process of slow slip. A perceived similarity between subduction zone and volcanic tremor has led to suggestions that slow slip involves fluid migration on or near the plate interface. Alternatively, evidence is accumulating to support the notion that tremor results from shear failure during slow slip. Global observations of the location, spatial extent, magnitude, duration, slip rate, and periodicity of these aseismic slip transients indicate significant variation that may be exploited to better understand their generation. Most slow slip events occur just downdip of the seismogenic zone, consistent with rate- and state-dependent frictional modeling that requires unstable to stable transitional properties for slow slip generation. At a few convergent margins the occurrence of slow slip events within the seismogenic zone makes it highly likely that transitions in frictional properties exist there and are the loci of slow slip nucleation. Slow slip events perturb the surrounding stress field and may either increase or relieve stress on a fault, bringing it closer to or farther from earthquake failure, respectively. This paper presents a review of slow slip events and related seismic tremor observed at plate boundaries worldwide, with a focus on circum-Pacific subduction zones. Trends in global observations of slow slip events suggest that (1) slow slip is a

  1. 78 FR 20454 - Safety Zones; Annual Events Requiring Safety Zones in the Captain of the Port Lake Michigan Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-04-05

    ... written--Celebrate Americafest/Fire over the Fox. This event has historically involved both a fireworks... day of the event. To ensure the safety of the Celebrate Americafest/Fire over the Fox event in its... 7 p.m. (2) Michigan Aerospace Challenge Sport Rocket Launch; Muskegon, MI--(i) Location. All waters...

  2. 78 FR 40000 - Eighth Coast Guard District Annual Safety Zones; Riverfront Independence Festival Fireworks; Ohio...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-07-03

    ...-AA00 Eighth Coast Guard District Annual Safety Zones; Riverfront Independence Festival Fireworks; Ohio.... SUMMARY: The Coast Guard will enforce a Safety Zone for the Riverfront Independence Festival Fireworks on... navigable waters during the Riverfront Independence Festival Fireworks. During the enforcement period, in...

  3. 33 CFR 165.T01-1057 - Safety Zones; Marine Events in Northern New England.

    Code of Federal Regulations, 2013 CFR

    2013-07-01

    ... 33 Navigation and Navigable Waters 2 2013-07-01 2013-07-01 false Safety Zones; Marine Events in... § 165.T01-1057 Safety Zones; Marine Events in Northern New England. (a) Regulations. The general regulations contained in 33 CFR 165.23 as well as the following regulations apply to the events listed in the...

  4. 78 FR 13811 - Safety Zone; Underwater Escape Event, Seaport, East River, NY

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-03-01

    ... York Zone on the specified date and time. This action is necessary to ensure the safety of participants... Coast Guard will enforce the safety zone listed in 33 CFR 165.160 on the specified date and time as... Zone; Underwater Escape Event, Seaport, East River, NY AGENCY: Coast Guard, DHS. ACTION: Notice of...

  5. 76 FR 31846 - Safety Zone; 28th Annual Humboldt Bay Festival, Fireworks Display, Eureka, CA

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-06-02

    ...-AA00 Safety Zone; 28th Annual Humboldt Bay Festival, Fireworks Display, Eureka, CA AGENCY: Coast Guard... support of the 28th Annual Humboldt Bay Festival Fireworks Display on the specified waters off the South... Humboldt Bay Festival Fireworks Display. The fireworks display is for entertainment purposes. This safety...

  6. 78 FR 23850 - Safety Zones; Annual Fireworks Events in the Captain of the Port Buffalo Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-04-23

    ... Football Half time Fireworks and the Lorain Port Fest Fireworks are formatted differently than the other... zones. Likewise, this rule will amend the Browns Football Half time and the Lorain Port Fest safety.... (24) Browns Football Halftime Fireworks, Cleveland, OH. (i) Location. All U.S. waters of Cleveland...

  7. 76 FR 24813 - Safety Zone; Fourth Annual Offshore Challenge, Sunny Isles Beach, FL

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-05-03

    ... Annual Offshore Challenge will consist of a series of high-speed boat races. The boat races are scheduled... Events, LLC is hosting the Fourth Annual Offshore Challenge, a series of high-speed boat races. The Fourth Annual Offshore Challenge will commence on June 17, 2011 and conclude on June 19, 2011. The boat...

  8. 76 FR 1065 - Security Zone; 23rd Annual North American International Auto Show, Detroit River, Detroit, MI

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-01-07

    ...-AA87 Security Zone; 23rd Annual North American International Auto Show, Detroit River, Detroit, MI... officials at the 23rd Annual North American International Auto Show (NAIAS) being held at Cobo Hall in... 23rd Annual North American International Auto Show (NAIAS) being held at Cobo Hall in downtown Detroit...

  9. Characterizing Mega-Earthquake Related Tsunami on Subduction Zones without Large Historical Events

    NASA Astrophysics Data System (ADS)

    Williams, C. R.; Lee, R.; Astill, S.; Farahani, R.; Wilson, P. S.; Mohammed, F.

    2014-12-01

    Due to recent large tsunami events (e.g., Chile 2010 and Japan 2011), the insurance industry is very aware of the importance of managing its exposure to tsunami risk. There are currently few tools available to help establish policies for managing and pricing tsunami risk globally. As a starting point and to help address this issue, Risk Management Solutions Inc. (RMS) is developing a global suite of tsunami inundation footprints. This dataset will include both representations of historical events as well as a series of M9 scenarios on subductions zones that have not historical generated mega earthquakes. The latter set is included to address concerns about the completeness of the historical record for mega earthquakes. This concern stems from the fact that the Tohoku Japan earthquake was considerably larger than had been observed in the historical record. Characterizing the source and rupture pattern for the subduction zones without historical events is a poorly constrained process. In many case, the subduction zones can be segmented based on changes in the characteristics of the subducting slab or major ridge systems. For this project, the unit sources from the NOAA propagation database are utilized to leverage the basin wide modeling included in this dataset. The length of the rupture is characterized based on subduction zone segmentation and the slip per unit source can be determined based on the event magnitude (i.e., M9) and moment balancing. As these events have not occurred historically, there is little to constrain the slip distribution. Sensitivity tests on the potential rupture pattern have been undertaken comparing uniform slip to higher shallow slip and tapered slip models. Subduction zones examined include the Makran Trench, the Lesser Antilles and the Hikurangi Trench. The ultimate goal is to create a series of tsunami footprints to help insurers understand their exposures at risk to tsunami inundation around the world.

  10. 77 FR 64411 - Safety Zone; Cooper T. Smith Fireworks Event; Mobile River; Mobile, AL

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-10-22

    ... 1625-AA00 Safety Zone; Cooper T. Smith Fireworks Event; Mobile River; Mobile, AL AGENCY: Coast Guard.... Smith Fireworks Event. Entry into, transiting or anchoring in this zone is prohibited to all vessels... safety hazards associated with a fireworks display. B. Basis and Purpose Cooper T. Smith Corp. has hired...

  11. 76 FR 7131 - Safety Zones; Eleventh Coast Guard District Annual Fireworks Events

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-02-09

    ... engaged in event activities, sightseeing and commercial fishing have ample space outside of the area...[deg]01'05'' N, 114[deg]38'20'' W. 2. Rockets over the River Sponsor Laughlin Tourism Committee. Event...

  12. 76 FR 21677 - Safety Zones; Annual Events Requiring Safety Zones in the Captain of the Port Sault Sainte Marie...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-04-18

    ..., 087[deg]23'07.60'' W [DATUM: NAD 83]. (ii) Enforcement Period This safety zone will be enforced each...]24'50.08'' N, 086[deg]39'08.52'' W [DATUM: NAD 83]. (ii) Enforcement Period This safety zone will be...[deg]57'46.14'' W, and 46[deg]40'19.68'' N, 085[deg]57'43.08'' W [DATUM: NAD 83], with the West Bay...

  13. 78 FR 42451 - Special Local Regulations; Marine Events; Annual Bayview Mackinac Race

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-07-16

    ...-AA08 Special Local Regulations; Marine Events; Annual Bayview Mackinac Race AGENCY: Coast Guard, DHS... regulation for the annual Bayview Mackinac Race, from 9 a.m. to 5 p.m. on July 20, 2013. This special local regulated is necessary to [[Page 42452

  14. 77 FR 41048 - Safety Zone; Hudson Valley Triathlon, Ulster Landing, Hudson River, NY

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-07-12

    ... Hudson Valley Triathlon swim event. This temporary safety zone is necessary to protect swimmers.... Regulatory History and Information The Hudson Valley Triathlon swim is an annual recurring event that has a... Valley Triathlon swim event will occur on July 15, 2012. On May 22, 2012, the sponsor of the event...

  15. 33 CFR 165.T11-0551 - Safety Zone; America's Cup Sailing Events.

    Code of Federal Regulations, 2013 CFR

    2013-07-01

    ... Sailing Events. 165.T11-0551 Section 165.T11-0551 Navigation and Navigable Waters COAST GUARD, DEPARTMENT... § 165.T11-0551 Safety Zone; America's Cup Sailing Events. (a) Definitions—(1) America's Cup Racing... 34th America's Cup sailing events. (2) Patrol Commander. As used in this section, “Patrol Commander” or...

  16. 77 FR 37807 - Regattas and Marine Parades; Great Lakes Annual Marine Events

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-06-25

    ... DEPARTMENT OF HOMELAND SECURITY Coast Guard 33 CFR Part 100 [Docket No. USCG-2012-0572] Regattas and Marine Parades; Great Lakes Annual Marine Events AGENCY: Coast Guard, DHS. ACTION: Notice of enforcement of regulation. SUMMARY: The Coast Guard will enforce various special local regulations for annual...

  17. 75 FR 26091 - Regattas and Marine Parades; Great Lakes Annual Marine Events

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-05-11

    ... DEPARTMENT OF HOMELAND SECURITY Coast Guard 33 CFR Part 100 [Docket No. USCG-2010-0312] Regattas and Marine Parades; Great Lakes Annual Marine Events AGENCY: Coast Guard, DHS. ACTION: Notice of enforcement of regulation. SUMMARY: The Coast Guard will enforce the local regulations for annual regattas and...

  18. 78 FR 53675 - Eighth Coast Guard District Annual Safety Zones; Boomsday Festival; Tennessee River 646.0-649.0...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-08-30

    ...-AA00 Eighth Coast Guard District Annual Safety Zones; Boomsday Festival; Tennessee River 646.0-649.0... Guard will enforce a Safety Zone for the Boomsday Festival Fireworks on the Tennessee River 646.0-649.0... Festival Fireworks. During the enforcement period, entry into, transiting or anchoring in the Safety Zone...

  19. Simple Physical Model for the Probability of a Subduction- Zone Earthquake Following Slow Slip Events and Earthquakes: Application to the Hikurangi Megathrust, New Zealand

    NASA Astrophysics Data System (ADS)

    Kaneko, Yoshihiro; Wallace, Laura M.; Hamling, Ian J.; Gerstenberger, Matthew C.

    2018-05-01

    Slow slip events (SSEs) have been documented in subduction zones worldwide, yet their implications for future earthquake occurrence are not well understood. Here we develop a relatively simple, simulation-based method for estimating the probability of megathrust earthquakes following tectonic events that induce any transient stress perturbations. This method has been applied to the locked Hikurangi megathrust (New Zealand) surrounded on all sides by the 2016 Kaikoura earthquake and SSEs. Our models indicate the annual probability of a M≥7.8 earthquake over 1 year after the Kaikoura earthquake increases by 1.3-18 times relative to the pre-Kaikoura probability, and the absolute probability is in the range of 0.6-7%. We find that probabilities of a large earthquake are mainly controlled by the ratio of the total stressing rate induced by all nearby tectonic sources to the mean stress drop of earthquakes. Our method can be applied to evaluate the potential for triggering a megathrust earthquake following SSEs in other subduction zones.

  20. 33 CFR 165.1191 - Safety zones: Northern California annual fireworks events.

    Code of Federal Regulations, 2011 CFR

    2011-07-01

    ... established for the events listed in Table 1 of this section. Further information on exact dates, times, and...,000 feet off Incline Village, Nevada in Crystal Bay. Regulated Area That area of navigable waters...

  1. 33 CFR 165.1191 - Safety zones: Northern California annual fireworks events.

    Code of Federal Regulations, 2010 CFR

    2010-07-01

    ... established for the events listed in Table 1 of this section. Further information on exact dates, times, and...,000 feet off Incline Village, Nevada in Crystal Bay. Regulated Area That area of navigable waters...

  2. 78 FR 67028 - Safety Zones; Recurring Events in Captain of the Port Boston Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-11-08

    ...]48.4' W (NAD 83). 7.18 Charles River 1-Mile Swim......... Event Type: Swim. Sponsor: Charles River...; 50 U.S.C. 191, 195; Pub. L. 107-295, 116 Stat. 2064; and Department of Homeland Security Delegation... fireworks barge, which will be located at position 42[deg]16.6[min] N, 070[deg]51.7[min] W. This safety zone...

  3. 76 FR 43124 - Safety Zones; July Fireworks Displays and Swim Events in the Captain of the Port New York Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-07-20

    ... York Zone AGENCY: Coast Guard, DHS. ACTION: Temporary final rule. SUMMARY: The Coast Guard is... safety of life on navigable waters during the events. Entry into, transit through, mooring or anchoring within these zones is prohibited unless authorized by the COTP New York. DATES: This rule is effective...

  4. 33 CFR 165.160 - Safety Zones; fireworks displays and swim events in Coast Guard Captain of the Port New York Zone.

    Code of Federal Regulations, 2012 CFR

    2012-07-01

    ..., Hempstead Harbor Safety Zone • Launch site: A barge located in approximate position 40°51′58″ N 073°39′34″ W... 33 Navigation and Navigable Waters 2 2012-07-01 2012-07-01 false Safety Zones; fireworks displays and swim events in Coast Guard Captain of the Port New York Zone. 165.160 Section 165.160 Navigation...

  5. 33 CFR 165.160 - Safety Zones; fireworks displays and swim events in Coast Guard Captain of the Port New York Zone.

    Code of Federal Regulations, 2013 CFR

    2013-07-01

    ..., Hempstead Harbor Safety Zone • Launch site: A barge located in approximate position 40°51′58″ N 073°39′34″ W... 33 Navigation and Navigable Waters 2 2013-07-01 2013-07-01 false Safety Zones; fireworks displays and swim events in Coast Guard Captain of the Port New York Zone. 165.160 Section 165.160 Navigation...

  6. 33 CFR 165.160 - Safety Zones; fireworks displays and swim events in Coast Guard Captain of the Port New York Zone.

    Code of Federal Regulations, 2014 CFR

    2014-07-01

    ..., Hempstead Harbor Safety Zone • Launch site: A barge located in approximate position 40°51′58″ N 073°39′34″ W... 33 Navigation and Navigable Waters 2 2014-07-01 2014-07-01 false Safety Zones; fireworks displays and swim events in Coast Guard Captain of the Port New York Zone. 165.160 Section 165.160 Navigation...

  7. 78 FR 77359 - Eighth Coast Guard District Annual Safety Zones; New Year's Eve Celebration/City of Mobile...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-12-23

    ... in past years but the fireworks display will move to a new location in the Mobile Channel beginning...-AA00 Eighth Coast Guard District Annual Safety Zones; New Year's Eve Celebration/City of Mobile; Mobile... enforce the City of Mobile New Year's Eve Celebration safety zone in the Mobile Channel, Mobile, AL from...

  8. Extreme climatic events change the dynamics and invasibility of semi-arid annual plant communities.

    PubMed

    Jiménez, Milagros A; Jaksic, Fabian M; Armesto, Juan J; Gaxiola, Aurora; Meserve, Peter L; Kelt, Douglas A; Gutiérrez, Julio R

    2011-12-01

    Extreme climatic events represent disturbances that change the availability of resources. We studied their effects on annual plant assemblages in a semi-arid ecosystem in north-central Chile. We analysed 130 years of precipitation data using generalised extreme-value distribution to determine extreme events, and multivariate techniques to analyse 20 years of plant cover data of 34 native and 11 exotic species. Extreme drought resets the dynamics of the system and renders it susceptible to invasion. On the other hand, by favouring native annuals, moderately wet events change species composition and allow the community to be resilient to extreme drought. The probability of extreme drought has doubled over the last 50 years. Therefore, investigations on the interaction of climate change and biological invasions are relevant to determine the potential for future effects on the dynamics of semi-arid annual plant communities. 2011 Blackwell Publishing Ltd/CNRS.

  9. Department of Defense Suicide Event Report Calendar Year 2013 Annual Report

    DTIC Science & Technology

    2014-07-24

    suicide attempt DoDSERs, the most common method was drug/alcohol overdose . Prescription and over-the- MARINE CORPS DoDSER RESULTS The DoDSER system...24 JUL 2014 2. REPORT TYPE 3. DATES COVERED 00-00-2014 to 00-00-2014 4. TITLE AND SUBTITLE Department of Defense Suicide Event Report Calendar...LEFT BLANK 1CALENDAR YEAR 2013 ANNUAL REPORT Chapter 1: Suicide Rates Chapter 1 SUICIDE RATES 3CALENDAR YEAR 2013 ANNUAL REPORT Chapter 2: DoDSER

  10. 33 CFR 165.161 - Safety zones: Coast Guard Captain of the Port New York annual fireworks displays.

    Code of Federal Regulations, 2010 CFR

    2010-07-01

    ... of the Port New York annual fireworks displays. 165.161 Section 165.161 Navigation and Navigable... Coast Guard District § 165.161 Safety zones: Coast Guard Captain of the Port New York annual fireworks... from 6 p.m. (e.s.t.) to 1 a.m. (e.s.t.) on the first Monday in October. (6) Seaport New Year's Eve...

  11. 33 CFR 165.1124 - Annual Firework Events on the Colorado River, between Davis Dam (Bullhead City, Arizona) and...

    Code of Federal Regulations, 2012 CFR

    2012-07-01

    ... Laughlin Tourism Committee. Event Description Fireworks Display Date First week in July. Location Laughlin... 33 Navigation and Navigable Waters 2 2012-07-01 2012-07-01 false Annual Firework Events on the... § 165.1124 Annual Firework Events on the Colorado River, between Davis Dam (Bullhead City, Arizona) and...

  12. 33 CFR 165.1124 - Annual Firework Events on the Colorado River, between Davis Dam (Bullhead City, Arizona) and...

    Code of Federal Regulations, 2013 CFR

    2013-07-01

    ... Laughlin Tourism Committee. Event Description Fireworks Display Date First week in July. Location Laughlin... 33 Navigation and Navigable Waters 2 2013-07-01 2013-07-01 false Annual Firework Events on the... § 165.1124 Annual Firework Events on the Colorado River, between Davis Dam (Bullhead City, Arizona) and...

  13. 76 FR 63841 - Safety Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-10-14

    ... Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of Responsibility..., Puget Sound area of responsibility during the dates and times noted below. This action is necessary to... anchoring within this zone is prohibited unless authorized by the Captain of the Port, Puget Sound or...

  14. 75 FR 43821 - Safety Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-07-27

    ... Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of Responsibility... Port, Puget Sound or Designated Representative. DATES: This safety zone will be enforced from 5 p.m. on... of the Port, Puget Sound Area of Responsibility. A previous notice of enforcement, published on July...

  15. 76 FR 31843 - Safety Zone; Temporary Change to Enforcement Location of Recurring Fireworks Display Event...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-06-02

    ...-AA00 Safety Zone; Temporary Change to Enforcement Location of Recurring Fireworks Display Event... Guard is temporarily changing the enforcement location of a safety zone for one specific recurring... originated from a barge but will this year originate from a location on land. The safety zone is necessary to...

  16. 77 FR 39422 - Eighth Coast Guard District Annual Safety Zones; Niceville July 4th Fireworks Show; Boggy Bayou...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-07-03

    ...-AA00 Eighth Coast Guard District Annual Safety Zones; Niceville July 4th Fireworks Show; Boggy Bayou... Guard will enforce a Safety Zone for the Niceville July 4th Fireworks Show in Boggy Bayou, Niceville... July 4th Fireworks Show. During the enforcement period, entry into, transiting or anchoring in the...

  17. 75 FR 33698 - Safety Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-06-15

    ...-AA00 Safety Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of... of the Port (COTP), Puget Sound Area of Responsibility (AOR). When these safety zones are activated... Captain of the Port, Puget Sound or Designated Representative. DATES: This rule is effective June 15, 2010...

  18. 78 FR 36656 - Safety Zone; Coronado Fourth of July Fireworks, Glorietta Bay; Coronado, CA

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-06-19

    ... 1625-AA00 Safety Zone; Coronado Fourth of July Fireworks, Glorietta Bay; Coronado, CA AGENCY: Coast... zone upon the navigable waters of Glorietta Bay for the Coronado Fourth of July Fireworks on July 4... this annual event on the navigable waters of Glorietta Bay in support of a fireworks show sponsored by...

  19. 75 FR 49847 - Safety Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-08-16

    ... Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of Responsibility... enforce the fireworks safety zone in Possession Sound from 5 p.m. on September 11, 2010 through 1 a.m. on... Captain of the Port, Puget Sound or Designated Representative. DATES: The regulations in 33 CFR 165.1332...

  20. 75 FR 39197 - Safety Zone; Fireworks Display, Portland, OR

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-07-08

    ...-AA00 Safety Zone; Fireworks Display, Portland, OR AGENCY: Coast Guard, DHS. ACTION: Notice of proposed..., and the shoreline to the east and west in support of the Oregon Symphony Celebration Fireworks Display... Register. Basis and Purpose The Oregon Symphony Celebration Fireworks display is an annual event. The...

  1. Trust Territory of the Pacific Islands. 1978 Annual Report.

    ERIC Educational Resources Information Center

    Department of the Interior, Washington, DC.

    Social, political, and economic advances in Micronesia during fiscal year 1978 are highlighted in this annual report to the United States Secretary of the Interior. Introductory chapters summarize the year's achievements and present major events in chronological order. Items include creation of a 200-mile fishery zone for Micronesia and provision…

  2. 77 FR 38484 - Safety Zones; Annual Fireworks Events in the Captain of the Port Detroit Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-06-28

    ..., at the following dates and times for the following events: (1) Bay-Rama Fishfly Festival Fireworks... will be enforced from 9:45 p.m. to 10:45 p.m. on July 4, 2012. (9) Lexington Independence Festival...:00 p.m. on July 21, 2012. (18) Marine City Maritime Festival Fireworks, Marine City, MI. The safety...

  3. Annual modulation of non-volcanic tremor in northern Cascadia

    USGS Publications Warehouse

    Pollitz, Fred; Wech, Aaron G.; Kao, Honn; Burgmann, Roland

    2013-01-01

    Two catalogs of episodic tremor events in northern Cascadia, one from 2006 to 2012 and the other from 1997 to 2011, reveal two systematic patterns of tremor occurrence in southern Vancouver Island: (1) most individual events tend to occur in the third quarter of the year; (2) the number of events in prolonged episodes (i.e., episodic tremor and slip events), which generally propagate to Vancouver Island from elsewhere along the Cascadia subduction zone, is inversely correlated with the amount of precipitation that occurred in the preceding 2 months. We rationalize these patterns as the product of hydrologic loading of the crust of southern Vancouver Island and the surrounding continental region, superimposed with annual variations from oceanic tidal loading. Loading of the Vancouver Island crust in the winter (when the land surface receives ample precipitation) and unloading in the summer tends to inhibit and enhance downdip shear stress, respectively. Quantitatively, for an annually variable surface load, the predicted stress perturbation depends on mantle viscoelastic rheology. A mechanical model of downdip shear stress on the transition zone beneath Vancouver Island—driven predominantly by the annual hydrologic cycle—is consistent with the 1997–2012 tremor observations, with peak-to-peak downdip shear stress of about 0.4 kPa. This seasonal dependence of tremor occurrence appears to be restricted to southern Vancouver Island because of its unique situation as an elongated narrow-width land mass surrounded by ocean, which permits seasonal perturbations in shear stress at depth.

  4. 77 FR 22218 - Safety Zone; Temporary Change for Air and Water Shows Within the Captain of the Port Lake...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-04-13

    ...), (ttt), and (uuu) to read as follows: Sec. 165.929 Safety Zones; Annual events requiring safety zones in... date and time. August 15, 2012 from 12 p.m. to 3 p.m.; August 17-19, 2012, from 9 a.m. to 4 p.m. (uuu...

  5. The Annual Glaciohydrology Cycle in the Ablation Zone of the Greenland Ice Sheet: Part 1. Hydrology Model

    NASA Technical Reports Server (NTRS)

    Colgan, William; Rajaram, Harihar; Anderson, Robert; Steffen. Konrad; Phillips, Thomas; Zwally, H. Jay; Abdalati, Waleed

    2012-01-01

    We apply a novel one-dimensional glacier hydrology model that calculates hydraulic head to the tidewater-terminating Sermeq Avannarleq flowline of the Greenland ice sheet. Within a plausible parameter space, the model achieves a quasi-steady-state annual cycle in which hydraulic head oscillates close to flotation throughout the ablation zone. Flotation is briefly achieved during the summer melt season along a approx.17 km stretch of the approx.50 km of flowline within the ablation zone. Beneath the majority of the flowline, subglacial conduit storage closes (i.e. obtains minimum radius) during the winter and opens (i.e. obtains maximum radius) during the summer. Along certain stretches of the flowline, the model predicts that subglacial conduit storage remains open throughout the year. A calculated mean glacier water residence time of approx.2.2 years implies that significant amounts of water are stored in the glacier throughout the year. We interpret this residence time as being indicative of the timescale over which the glacier hydrologic system is capable of adjusting to external surface meltwater forcings. Based on in situ ice velocity observations, we suggest that the summer speed-up event generally corresponds to conditions of increasing hydraulic head during inefficient subglacial drainage. Conversely, the slowdown during fall generally corresponds to conditions of decreasing hydraulic head during efficient subglacial drainage.

  6. Short-term Slow Slip Events at the Southcentral Alaska Subduction Zone

    NASA Astrophysics Data System (ADS)

    McGuire, J. L.; Fu, Y.; Freymueller, J. T.

    2017-12-01

    The Pacific Plate is subducting beneath the North American Plate along the Aleutian Trench. The Alaska subduction zone is among the most tectonically active areas on Earth and is home to some of the largest earthquakes on record, including the second largest earthquake ever recorded, the M9.2 Prince William Sound earthquake of 1964. With the increasing availability of continuous GPS observations, studying time-dependent crustal movements in this area has become possible. Previous studies have analyzed the presence of long-term slow slip events (SSEs) in the region. Two long-term SSEs occurred from 1998-2001 and from 2010-2014 with durations of 3-4 years. These two long-term events occurred down-dip of the main asperity of the 1964 Prince William Sound earthquake. In addition to these long-term SSEs, there are also short-term SSEs evident in the GPS time series, which have durations of approximately two months. We have adequate data to study three short-term slow slip events, in 2005, 2006 and 2007. We fit the GPS time series data with the combination of a linear trend, a hyperbolic tangent function, and seasonal variations to derive the crustal displacements of all three short-term SSEs at each station in the north, east, and vertical directions. Then, an inversion model using the Green's functions for slip on the plate interface was employed to estimate the location and amplitude of slip and to calculate the magnitude of these slow slip events. Our results show Mw 6.09 for the 2005 event, Mw 6.40 for the 2006 event, and Mw 6.30 for the 2007 event. Our results indicate that both long-term SSEs and short-term SSEs occurred in the same location, down-dip of the rupture asperity of 1964 M9.2 earthquake. We use this information to relate the short-term slow slip events to the long-term events that have occurred in the region and to look for the implications on the slip budget of both short-term and long-term SSEs during the earthquake cycle at Southcentral Alaska

  7. 77 FR 30188 - Safety Zones; Annually Recurring Marine Events in Coast Guard Southeastern New England Captain of...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-05-22

    ...'83'' W (NAD 83). Safety Zone Dimension: Approximately 300 yard radius circle around the fireworks... Providence River, Providence, RI. Position: Within 500 yards of 41[deg]48'50'' N, 071[deg]23'43'' W (NAD 83... 500 yards of 41[deg]42'37'' N, 071[deg]09'53'' W (NAD 83). Safety Zone Dimension: Approximately 200...

  8. 77 FR 5463 - Safety Zones; Annually Recurring Marine Events in Coast Guard Southeastern New England Captain of...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-02-03

    ...]10'83'' W (NAD 83). Safety Zone Dimension: Approximately 300 yard radius circle around the fireworks... Providence River, Providence, RI. Position: Within 500 yards of 41[deg]48'50'' N, 071[deg]23'43'' W (NAD 83... yards of 41[deg]42'37'' N, 071[deg]09'53'' W (NAD 83). Safety Zone Dimension: Approximately 200 yard...

  9. 78 FR 13576 - Special Local Regulations and Safety Zones; Recurring Marine Events and Fireworks Displays Within...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-02-28

    ... area April--2nd Saturday St. Mary's College Seahawk Specified waters of St. Mary's Sprint River... regulations by adding 15 new annual recurring marine events, fireworks displays and revising event date(s) and... provide for the safety of life on navigable waters during these events, reduce the Coast Guard's...

  10. 77 FR 39413 - Safety Zone: Crescent City Fourth of July Fireworks Event, Crescent City, CA

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-07-03

    ...-AA00 Safety Zone: Crescent City Fourth of July Fireworks Event, Crescent City, CA AGENCY: Coast Guard... the navigable waters near Crescent City Harbor in Crescent City, CA in support of the Crescent City... establish safety zones (33 U.S.C sections 1221 et seq.). Crescent City-Del Norte County Chamber of Commerce...

  11. 76 FR 36438 - Special Local Regulations; Safety and Security Zones; Recurring Events in Captain of the Port...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-06-22

    ... Events in Captain of the Port Long Island Sound Zone AGENCY: Coast Guard, DHS. ACTION: Notice of proposed... security zone in the Coast Guard Sector Long Island Sound Captain of the Port (COTP) Zone. When these..., call or e-mail Petty Officer Joseph Graun, Waterways Management Division at Coast Guard Sector Long...

  12. 77 FR 22706 - Special Local Regulation and Safety Zone; America's Cup Sailing Events, San Francisco, CA

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-04-17

    ...] Special Local Regulation and Safety Zone; America's Cup Sailing Events, San Francisco, CA AGENCY: Coast... regulation and temporary safety zone proposed for those portions of the ``America's Cup World Series,'' the ``Louis Vuitton Cup'' challenger selection series, and the ``America's Cup Finals Match'' sailing regattas...

  13. 33 CFR 165.943 - Annual events requiring safety zones in the Captain of the Port Duluth zone.

    Code of Federal Regulations, 2014 CFR

    2014-07-01

    .... (ii) Enforcement date and time. This event historically occurs during the 4th of July week. The... historically occurs the week before, after or during 4th of July week. The Captain of the Port Duluth, will... 4th of July week. The Captain of the Port Duluth, will establish enforcement dates that will be...

  14. 77 FR 40518 - Swim Events in the Captain of the Port New York Zone; Hudson River, East River, Upper New York...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-07-10

    ... 1625-AA00 Swim Events in the Captain of the Port New York Zone; Hudson River, East River, Upper New York Bay, Lower New York Bay; New York, NY ACTION: Final rule. SUMMARY: The Coast Guard is establishing seven temporary safety zones for swim events within the Captain of the Port (COTP) New York Zone. These...

  15. 76 FR 69613 - Special Local Regulations and Safety Zones; Recurring Events in Captain of the Port New York Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-11-09

    ... regulatory text: Safety zones listed in Table 1 to Sec. 165.160 have been reordered and renumbered to more accurately reflect their geographical locations. In the published NPRM regulatory text, the Rumson, NJ... included in this recurring events regulation. In the regulatory text under Sec. 165.160(a), the existing...

  16. 76 FR 55561 - Special Local Regulations for Marine Events; Temporary Change of Dates for Recurring Marine...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-09-08

    ... Wrightsville Channel during the swimming portion of this event. DATES: This rule is effective on September 17... bike-riding portion, and a swimming portion. The swimming portion of the Triathlon takes place in the... safety zone for the swimming portion of the Triathlon. The listing of annual recurring marine events...

  17. 33 CFR 165.118 - Safety Zones; recurring annual events held in Coast Guard Sector Boston Captain of the Port Zone.

    Code of Federal Regulations, 2012 CFR

    2012-07-01

    ... 4th of July Celebration Fireworks • Event Type: Firework Display.• Sponsor: City of Lynn. • Date: July...°27.62′ N, 070°55.58′ W (NAD 83). 7.2Gloucester July 4th Celebration Fireworks • Event Type: Fireworks...: Manchester Parks and Recreation Department. • Date: July 4th, as specified in the USCG District 1 Local...

  18. 33 CFR 165.118 - Safety Zones; recurring annual events held in Coast Guard Sector Boston Captain of the Port Zone.

    Code of Federal Regulations, 2013 CFR

    2013-07-01

    ... 4th of July Celebration Fireworks • Event Type: Firework Display.• Sponsor: City of Lynn. • Date: July...°27.62′ N, 070°55.58′ W (NAD 83). 7.2Gloucester July 4th Celebration Fireworks • Event Type: Fireworks...: Manchester Parks and Recreation Department. • Date: July 4th, as specified in the USCG District 1 Local...

  19. 33 CFR 165.918 - Safety Zones; Annual events requiring safety zones in the Captain of the Port Sault Sainte Marie...

    Code of Federal Regulations, 2014 CFR

    2014-07-01

    ... due to inclement weather, then this section will be enforced July 5 from 9 p.m. until 11 p.m. (2... zone will be enforced each year on July 4 from 9 p.m. until 12:30 a.m. on July 5. If the July 4 fireworks are cancelled due to inclement weather, then this section will be enforced on July 5 from 9 p.m...

  20. 33 CFR 165.918 - Safety Zones; Annual events requiring safety zones in the Captain of the Port Sault Sainte Marie...

    Code of Federal Regulations, 2011 CFR

    2011-07-01

    ... due to inclement weather, then this section will be enforced July 5 from 9 p.m. until 11 p.m. (2... zone will be enforced each year on July 4 from 9 p.m. until 12:30 a.m. on July 5. If the July 4 fireworks are cancelled due to inclement weather, then this section will be enforced on July 5 from 9 p.m...

  1. 33 CFR 165.918 - Safety Zones; Annual events requiring safety zones in the Captain of the Port Sault Sainte Marie...

    Code of Federal Regulations, 2012 CFR

    2012-07-01

    ... due to inclement weather, then this section will be enforced July 5 from 9 p.m. until 11 p.m. (2... zone will be enforced each year on July 4 from 9 p.m. until 12:30 a.m. on July 5. If the July 4 fireworks are cancelled due to inclement weather, then this section will be enforced on July 5 from 9 p.m...

  2. 77 FR 73311 - Special Local Regulation and Safety Zone; America's Cup Sailing Events, San Francisco, CA...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-12-10

    ...-AA00; 1625-AA08 Special Local Regulation and Safety Zone; America's Cup Sailing Events, San Francisco... the 2013 America's Cup events. This document corrects those erroneous coordinates. DATES: Effective on... published a temporary final rule regulating the on-water activities associated with the ``Louis Vuitton Cup...

  3. 33 CFR 165.118 - Safety Zones; recurring annual events held in Coast Guard Sector Boston Captain of the Port Zone.

    Code of Federal Regulations, 2014 CFR

    2014-07-01

    ...°51.7′ W (NAD 83). 7.0 July 7.1City of Lynn 4th of July Celebration Fireworks • Event Type: Firework... the fireworks barge located at position 42°27.62 ′ N, 070°55.58′ W (NAD 83). 7.2Gloucester July 4th... • Event Type: Fireworks Display. • Sponsor: Manchester Parks and Recreation Department. • Date: July 4th...

  4. 77 FR 46285 - Special Local Regulation and Safety Zone; America's Cup Sailing Events, San Francisco, CA

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-08-03

    ...] Special Local Regulation and Safety Zone; America's Cup Sailing Events, San Francisco, CA AGENCY: Coast... 2012 program calendar for the on-water activities associated with the ``2012 America's Cup World Series... waters of San Francisco Bay associated with the 34th America's Cup sailing events taking place adjacent...

  5. 33 CFR 165.151 - Safety Zones; Fireworks Displays, Air Shows and Swim Events in the Captain of the Port Long...

    Code of Federal Regulations, 2012 CFR

    2012-07-01

    ....22″ W (NAD 83). 7.33Clam Shell Foundation Fireworks • Location: Waters of Three Mile Harbor, East..., Air Shows and Swim Events in the Captain of the Port Long Island Sound Zone. 165.151 Section 165.151... Swim Events in the Captain of the Port Long Island Sound Zone. (a) Regulations. (1) The general...

  6. 77 FR 6954 - Special Local Regulations; Safety and Security Zones; Recurring Events in Captain of the Port...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-02-10

    ... Events in Captain of the Port Long Island Sound Zone AGENCY: Coast Guard, DHS. ACTION: Final rule... Sector Long Island Sound Captain of the Port (COTP) Zone. These limited access areas include special... Sector Long Island Sound, telephone 203-468- 4544, email [email protected] . If you have questions...

  7. 78 FR 32990 - Special Local Regulation and Safety Zone; America's Cup Sailing Events, San Francisco, CA

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-06-03

    ...] Special Local Regulation and Safety Zone; America's Cup Sailing Events, San Francisco, CA AGENCY: Coast... ``Louis Vuitton Cup, Red Bull Youth America's Cup and the 34th America's Cup'' regatta scheduled from July... associated with the 34th America's Cup sailing events taking place adjacent to the City of San Francisco...

  8. 77 FR 55143 - Safety Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-09-07

    ... Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of Responsibility... Sound or his Designated Representative. DATES: The regulations in 33 CFR 165.1332 will be enforced from...: If you have questions on this notice, call or email ENS Nathaniel P. Clinger, Sector Puget Sound...

  9. 75 FR 8566 - Safety Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2010-02-25

    ...-AA00 Safety Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of... at various locations the Captain of the Port, Puget Sound Area of Responsibility (AOR). When these... prohibited unless authorized by the Captain of the Port, Puget Sound or Designated Representative. DATES...

  10. The Annual Glaciohydrology Cycle in the Ablation Zone of the Greenland Ice Sheet: Part 2. Observed and Modeled Ice Flow

    NASA Technical Reports Server (NTRS)

    Colgan, William Terence; Rajaram, Harihar; Anderson, Robert S.; Steffen, Konrad; Zwally, H. Jay; Phillips, Thomas; Abdalati, Waleed

    2012-01-01

    Ice velocities observed in 2005/06 at three GPS stations along the Sermeq Avannarleq flowline, West Greenland, are used to characterize an observed annual velocity cycle. We attempt to reproduce this annual ice velocity cycle using a 1-D ice-flow model with longitudinal stresses coupled to a 1-D hydrology model that governs an empirical basal sliding rule. Seasonal basal sliding velocity is parameterized as a perturbation of prescribed winter sliding velocity that is proportional to the rate of change of glacier water storage. The coupled model reproduces the broad features of the annual basal sliding cycle observed along this flowline, namely a summer speed-up event followed by a fall slowdown event. We also evaluate the hypothesis that the observed annual velocity cycle is due to the annual calving cycle at the terminus. We demonstrate that the ice acceleration due to a catastrophic calving event takes an order of magnitude longer to reach CU/ETH ('Swiss') Camp (46km upstream of the terminus) than is observed. The seasonal acceleration observed at Swiss Camp is therefore unlikely to be the result of velocity perturbations propagated upstream via longitudinal coupling. Instead we interpret this velocity cycle to reflect the local history of glacier water balance.

  11. 76 FR 61263 - Safety Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-10-04

    ... coordinates for four of the fireworks displays. This rule changes the coordinates listed for four displays to...-AA00 Safety Zones; Annual Firework Displays Within the Captain of the Port, Puget Sound Area of Responsibility AGENCY: Coast Guard, DHS. ACTION: Final rule. SUMMARY: The Coast Guard is amending our regulations...

  12. The role of suspension events in cross-shore and longshore suspended sediment transport in the surf zone

    USGS Publications Warehouse

    Jaffe, Bruce E.

    2015-01-01

    Suspension of sand in the surf zone is intermittent. Especially striking in a time series of concentration are periods of intense suspension, suspension events, when the water column suspended sediment concentration is an order of magnitude greater than the mean concentration. The prevalence, timing, and contribution of suspension events to cross-shore and longshore suspended sediment transport are explored using field data collected in the inner half of the surf zone during a large storm at Duck, NC. Suspension events are defined as periods when the concentration is above a threshold. Events tended to occur during onshore flow under the wave crest, resulting in an onshore contribution to the suspended sediment transport. Even though large events occurred less than 10 percent of the total time, at some locations onshore transport associated with suspension events was greater than mean-current driven offshore-directed transport during non-event periods, causing the net suspended sediment transport to be onshore. Events and fluctuations in longshore velocity were not correlated. However, events did increase the longshore suspended sediment transport by approximately the amount they increase the mean concentration, which can be up to 35%. Because of the lack of correlation, the longshore suspended sediment transport can be modeled without considering the details of the intensity and time of events as the vertical integration of the product of the time-averaged longshore velocity and an event-augmented time-averaged concentration. However, to accurately model cross-shore suspended sediment transport, the timing and intensity of suspension events must be reproduced.

  13. 78 FR 16211 - Safety Zone, Corp. Event Finale UHC, St. Thomas Harbor; St. Thomas, U.S. Virgin Islands

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-03-14

    ... 1625-AA00 Safety Zone, Corp. Event Finale UHC, St. Thomas Harbor; St. Thomas, U.S. Virgin Islands... establish a temporary safety zone on the waters of St. Thomas Harbor in St. Thomas, U.S. Virgin Islands... near the St. Thomas Harbor channel from which fireworks will be lit. DATES: Comments and related...

  14. Using high-frequency sensors to identify hydroclimatological controls on storm-event variability in catchment nutrient fluxes and source zone activation

    NASA Astrophysics Data System (ADS)

    Blaen, Phillip; Khamis, Kieran; Lloyd, Charlotte; Krause, Stefan

    2017-04-01

    At the river catchment scale, storm events can drive highly variable behaviour in nutrient and water fluxes, yet short-term dynamics are frequently missed by low resolution sampling regimes. In addition, nutrient source contributions can vary significantly within and between storm events. Our inability to identify and characterise time dynamic source zone contributions severely hampers the adequate design of land use management practices in order to control nutrient exports from agricultural landscapes. Here, we utilise an 8-month high-frequency (hourly) time series of streamflow, nitrate concentration (NO3) and fluorescent dissolved organic matter concentration (FDOM) derived from optical in-situ sensors located in a headwater agricultural catchment. We characterised variability in flow and nutrient dynamics across 29 storm events. Storm events represented 31% of the time series and contributed disproportionately to nutrient loads (43% of NO3 and 36% of CDOM) relative to their duration. Principal components analysis of potential hydroclimatological controls on nutrient fluxes demonstrated that a small number of components, representing >90% of variance in the dataset, were highly significant model predictors of inter-event variability in catchment nutrient export. Hysteresis analysis of nutrient concentration-discharge relationships suggested spatially discrete source zones existed for NO3 and FDOM, and that activation of these zones varied on an event-specific basis. Our results highlight the benefits of high-frequency in-situ monitoring for characterising complex short-term nutrient dynamics and unravelling connections between hydroclimatological variability and river nutrient export and source zone activation under extreme flow conditions. These new process-based insights are fundamental to underpinning the development of targeted management measures to reduce nutrient loading of surface waters.

  15. 77 FR 70121 - Special Local Regulation; Annual Marine Events on the Colorado River Between Davis Dam (Bullhead...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-11-23

    ... Local Regulation; Annual Marine Events on the Colorado River Between Davis Dam (Bullhead City, AZ) and... during the Lake Havasu City Boat Parade of Lights on December 01, 2012 from 5 p.m. to 9 p.m. This event... Lake Havasu City Boat Parade of Lights (Item 10 on Table 1 of 33 CFR 100.1102). The Coast Guard will...

  16. 77 FR 31493 - Eighth Coast Guard District Annual Marine Events and Safety Zones; Billy Bowlegs Pirate Festival...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-05-29

    ... Bowlegs Pirate Festival; Santa Rosa Sound; Ft. Walton Beach, FL AGENCY: Coast Guard, DHS. ACTION: Notice... Safety Zone for the Billy Bowlegs Pirate Festival in the Santa Rosa Sound, Ft. Walton Beach, FL on June 1... crews, vessels, and persons on navigable waters during the Billy Bowlegs Pirate Festival. During the...

  17. How senior entomologists can be involved in the annual meeting: organization and the coming together of a large event

    USDA-ARS?s Scientific Manuscript database

    The Annual Meeting for the Entomological Society of America is a large event where planning is started at the end of the previous years’ meeting. The President of the Society named the Program Committee Co-Chairs for Entomology 2017 at the 2015 Annual Meeting, so that they could handle the duties o...

  18. 78 FR 33700 - Special Local Regulations for Marine Events, Pleasantville Aquatics 15th Annual 5K Open Water...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-06-05

    ...-AA08 Special Local Regulations for Marine Events, Pleasantville Aquatics 15th Annual 5K Open Water Swim... from operating while a swim event is taking place. This special local regulation is necessary to... Docket Management Facility in Room W12-140 on the ground floor of the Department of Transportation West...

  19. Seismic constraints on a large dyking event and initiation of a transform fault zone in Western Gulf of Aden

    NASA Astrophysics Data System (ADS)

    Ahmed, AbdulHakim; Doubre, Cecile; Leroy, Sylvie; Perrot, Julie; Audin, Laurence; Rolandone, Frederique; Keir, Derek; Al-Ganad, Ismael; Sholan, Jamal; Khanbari, Khaled; Mohamed, Kassim; Vergne, Jerome; Jacques, Eric; Nercessian, Alex

    2013-04-01

    In November 2010, a large number of events were recorded by the world seismic networks showing important activity occurring along the western part of the Aden Ridge. West of the Shulka El Sheik fracture zone, events in this large seismic swarm (magnitudes above 5) occurred in a complex area, where the change of both the ridge direction and the bathymetry suggest the propagation of the ridge into a continental lithosphere and the influence of the Afar plume. We combine several sets of data from permanent networks and temporary 3C broad stations installed after the beginning of the event along the southern and eastern coasts of Yemen and Djibouti respectively, we located more than 600 earthquakes with magnitudes ranging from 2.5 to 5.6 that occurred during the first months following the first event. The spatial distribution of the main seismicity reveals a very clear N115° -trending alignment, parallel to the mean direction of the en-echelon spreading segments that form the ridge at this longitude. Half of the events, which represent half of the total seismic energy released during the first months, are located in the central third section of the segment. Here several volcanic cones and recent lava flows observed from bathymetric and acoustic reflectivity data during the Tadjouraden cruise (Audin, 1999, Dauteuil et al., 2001) constitute the sea floor. In addition to this main activity, two small groups of events suggest the activiation of landslides into a large fan and the activity in a volcanic area 50 km due east from the main active zone. The time evolution of the seismicity shows several bursts of activity. Some of them are clearly related to sudden activities within the volcanic areas, when others exhibit horizontal migration of the events, with velocity around ˜ 1 km/h. The time-space evolution of the seismicity clearly reveals the intrusion of dykes associated with magma propagation from the crustal magmatic centres into the rift zone. Taking into account

  20. 78 FR 22778 - Safety Zone; Corp. Event Finale UHC, St. Thomas Harbor; St. Thomas, U.S.V.I.

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-04-17

    ...-AA00 Safety Zone; Corp. Event Finale UHC, St. Thomas Harbor; St. Thomas, U.S.V.I. AGENCY: Coast Guard... waters of St. Thomas Harbor in St. Thomas, U.S. Virgin Islands during the Corp. Event Finale UHC, a... barge being positioned near the St. Thomas Harbor channel from which fireworks will be lit. The safety...

  1. 78 FR 59230 - Special Local Regulations; Annual Marine Events on the Colorado River, Between Davis Dam...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-09-26

    ... DEPARTMENT OF HOMELAND SECURITY Coast Guard 33 CFR Part 100 [Docket No. USCG-2013-0644] Special Local Regulations; Annual Marine Events on the Colorado River, Between Davis Dam (Bullhead City, Arizona... INFORMATION: The Coast Guard will enforce the special local regulations on the Colorado River for the...

  2. 78 FR 55214 - Annual Marine Events in the Eighth Coast Guard District, Sabine River; Orange, TX

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-09-10

    ... DEPARTMENT OF HOMELAND SECURITY Coast Guard 33 CFR Part 100 [Docket No. USCG-2013-0723] Annual Marine Events in the Eighth Coast Guard District, Sabine River; Orange, TX AGENCY: Coast Guard, DHS. ACTION: Notice of enforcement of regulation. SUMMARY: The Coast Guard will enforce Special Local...

  3. Secondary melting events in Semarkona chondrules revealed by compositional zoning in low-Ca pyroxene

    NASA Astrophysics Data System (ADS)

    Baecker, Bastian; Rubin, Alan E.; Wasson, John T.

    2017-08-01

    It is well established that many chondrules contain relict grains formed in previous generations of chondrules. We here describe evidence that chondrules experienced multiple mesostasis melting events while remaining closed systems. Spheroidal chondrule shapes resulted from surface-tension effects following a primary heating event that caused substantial melting (≳40%) of the precursor assemblages. In some high-FeO chondrules in LL3.00 Semarkona, low-Ca pyroxene phenocrysts show multiple overgrowth layers produced by secondary melting events. We characterized these layers with the electron microprobe in terms of Fe, Ca and Cr in two Semarkona chondrules. The first low-Ca pyroxene overgrowth that forms after a minor heating/melting event has low Ca and Fe; concentrations of these incompatibles gradually increase over the next 8 ± 4 μm until falling temperatures and slowing diffusion caused growth to stop. The next melting event remelts and mixes the local mesostasis; cooling causes growth of a normal igneously zoned layer. In the simplest cases, the Ca concentrations at the minima gradually increase towards the edge of the phenocryst. Heat deposition during heating events varied over a wide range; the weakest events produced recognizable changes in slopes (that we call "inflections" rather than minima). Large fractions of the individual phenocrysts were formed by the process that produced the overgrowth layers. It appears that overgrowth formation stopped when the Ca content of the mesostasis became high enough to make high-Ca pyroxene a liquidus phase. Both Semarkona chondrules include olivine phenocrysts similar in size and modal abundance to the low-Ca pyroxene phenocrysts. Olivine compositional profiles show symmetrical, apparently normal zoning except for asymmetries attributable to the presence of relict grains. Surface compositions of different olivine phenocrysts in the same chondrule are very similar to one another, consistent with growth from

  4. 77 FR 4501 - Special Local Regulation and Safety Zone; America's Cup Sailing Events, San Francisco, CA

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-01-30

    ...] RIN 1625-AA00; 1625-AA08 Special Local Regulation and Safety Zone; America's Cup Sailing Events, San... those portions of the ``America's Cup World Series,'' the ``Louis Vuitton Cup'' challenger selection series, and the ``America's Cup Finals Match'' sailing regattas that may be conducted in the waters of...

  5. 78 FR 36424 - Special Local Regulations for Summer Events; Captain of the Port Lake Michigan Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-06-18

    ... Guard, DHS. ACTION: Temporary final rule. SUMMARY: The Coast Guard is establishing temporary special local regulations for three summer events within the Captain of the Port Lake Michigan Zone. This rule is intended to provide for the safety of life and property on navigable waters immediately prior to...

  6. Assessing emergency planning zone for new nuclear power plant considering risk of extreme external events

    NASA Astrophysics Data System (ADS)

    Alzbutas, Robertas

    2015-04-01

    In general, the Emergency Planning Zones (EPZ) are defined as well as plant site and arrangement structures are designed to minimize the potential for natural and manmade hazards external to the plant from affecting the plant safety related functions, which can affect nearby population and environment. This may include consideration of extreme winds, fires, flooding, aircraft crash, seismic activity, etc. Thus the design basis for plant and site is deeply related to the effects of any postulated external events and the limitation of the plant capability to cope with accidents i.e. perform safety functions. It has been observed that the Probabilistic Safety Assessment (PSA) methodologies to deal with EPZ and extreme external events have not reached the same level of maturity as for severe internal events. The design basis for any plant and site is deeply related to the effects of any postulated external events and the limitation of the plant capability to cope with accidents i.e. perform safety functions. As a prime example of an advanced reactor and new Nuclear Power Plant (NPP) with enhanced safety, the International Reactor Innovative and Secure (IRIS) and Site selection for New NPP in Lithuania had been considered in this work. In the used Safety-by-Design™ approach, the PSA played obviously a key role; therefore a Preliminary IRIS PSA had been developed along with the design. For the design and pre-licensing process of IRIS the external events analysis included both qualitative evaluation and quantitative assessment. As a result of preliminary qualitative analyses, the external events that were chosen for more detailed quantitative scoping evaluation were high winds and tornadoes, aircraft crash, and seismic events. For the site selection in Lithuania a detail site evaluation process was performed and related to the EPZ and risk zoning considerations. In general, applying the quantitative assessment, bounding site characteristics could be used in order to

  7. Possible correlation between annual gravity change and shallow background seismicity rate at subduction zone by surface load

    NASA Astrophysics Data System (ADS)

    Mitsui, Yuta; Yamada, Kyohei

    2017-12-01

    The Gravity Recovery and Climate Experiment (GRACE) has monitored global gravity changes since 2002. Gravity changes are considered to represent hydrological water mass movements around the surface of the globe, although fault slip of a large earthquake also causes perturbation of gravity. Since surface water movements are expected to affect earthquake occurrences via elastic surface load or pore-fluid pressure increase, correlation between gravity changes and occurrences of small (not large) earthquakes may reflect the effects of surface water movements. In the present study, we focus on earthquakes smaller than magnitude 7.5 and examine the relation between annual gravity changes and earthquake occurrences at worldwide subduction zones. First, we extract amplitudes of annual gravity changes from GRACE data for land. Next, we estimate background seismicity rates in the epidemic-type aftershock sequence model from shallow seismicity data having magnitudes of over 4.5. Then, we perform correlation analysis of the amplitudes of the annual gravity changes and the shallow background seismicity rates, excluding source areas of large earthquakes, and find moderate positive correlation. It implies that annual water movements can activate shallow earthquakes, although the surface load elastostatic stress changes are on the order of or below 1 kPa, as small as a regional case in a previous study. We speculate that periodic stress perturbation is amplified through nonlinear responses of frictional faults.[Figure not available: see fulltext.

  8. Modelling of extreme rainfall events in Peninsular Malaysia based on annual maximum and partial duration series

    NASA Astrophysics Data System (ADS)

    Zin, Wan Zawiah Wan; Shinyie, Wendy Ling; Jemain, Abdul Aziz

    2015-02-01

    In this study, two series of data for extreme rainfall events are generated based on Annual Maximum and Partial Duration Methods, derived from 102 rain-gauge stations in Peninsular from 1982-2012. To determine the optimal threshold for each station, several requirements must be satisfied and Adapted Hill estimator is employed for this purpose. A semi-parametric bootstrap is then used to estimate the mean square error (MSE) of the estimator at each threshold and the optimal threshold is selected based on the smallest MSE. The mean annual frequency is also checked to ensure that it lies in the range of one to five and the resulting data is also de-clustered to ensure independence. The two data series are then fitted to Generalized Extreme Value and Generalized Pareto distributions for annual maximum and partial duration series, respectively. The parameter estimation methods used are the Maximum Likelihood and the L-moment methods. Two goodness of fit tests are then used to evaluate the best-fitted distribution. The results showed that the Partial Duration series with Generalized Pareto distribution and Maximum Likelihood parameter estimation provides the best representation for extreme rainfall events in Peninsular Malaysia for majority of the stations studied. Based on these findings, several return values are also derived and spatial mapping are constructed to identify the distribution characteristic of extreme rainfall in Peninsular Malaysia.

  9. Transition-zone observations of rapid flare events as observed by OSO-8

    NASA Technical Reports Server (NTRS)

    Lites, B. W.

    1981-01-01

    The rapid dissipation of flare energy has been observed in the transition-zone line of C IV at 1548.2 A using the University of Colorado spectrometer aboard OSO-8. Impulsive brightenings have been resolved with characteristic rise times as low as 3.5s. One event is analyzed in detail, and it is inferred that the electron density is greater than 2 x 10 to the 11th/cu cm at a temperature of 60,000 K, and that the flare energy is deposited at a rate of 2 ergs/cu cm per sec or greater. The temporal behavior of the intensity at the center of the C IV line is consistent with a nonequilibrium ionization of C III through C V. If this event is a result of the multiple tearing mode instability as the primary energy release mechanism, then the observations indicate a preflare magnetic field of about 175 G.

  10. 77 FR 47519 - Annual Marine Events in the Eighth Coast Guard District, Sabine River; Orange, TX

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-08-09

    ... DEPARTMENT OF HOMELAND SECURITY Coast Guard 33 CFR Part 100 [Docket No. USCG-2012-0656] Annual Marine Events in the Eighth Coast Guard District, Sabine River; Orange, TX AGENCY: Coast Guard, DHS... Regulations for the S.P.O.R.T. Power Boat Neches River in Orange, TX from 3 p.m. on September 21, 2012...

  11. 33 CFR 100.35T09-0327 - Special Regulated Areas for summer events; Captain of the Port Lake Michigan Zone.

    Code of Federal Regulations, 2013 CFR

    2013-07-01

    ... 33 Navigation and Navigable Waters 1 2013-07-01 2013-07-01 false Special Regulated Areas for summer events; Captain of the Port Lake Michigan Zone. 100.35T09-0327 Section 100.35T09-0327 Navigation... OF LIFE ON NAVIGABLE WATERS § 100.35T09-0327 Special Regulated Areas for summer events; Captain of...

  12. Coccolithophore populations and their contribution to carbonate export during an annual cycle in the Australian sector of the Antarctic zone

    NASA Astrophysics Data System (ADS)

    Rigual Hernández, Andrés S.; Flores, José A.; Sierro, Francisco J.; Fuertes, Miguel A.; Cros, Lluïsa; Trull, Thomas W.

    2018-03-01

    The Southern Ocean is experiencing rapid and relentless change in its physical and biogeochemical properties. The rate of warming of the Antarctic Circumpolar Current exceeds that of the global ocean, and the enhanced uptake of carbon dioxide is causing basin-wide ocean acidification. Observational data suggest that these changes are influencing the distribution and composition of pelagic plankton communities. Long-term and annual field observations on key environmental variables and organisms are a critical basis for predicting changes in Southern Ocean ecosystems. These observations are particularly needed, since high-latitude systems have been projected to experience the most severe impacts of ocean acidification and invasions of allochthonous species. Coccolithophores are the most prolific calcium-carbonate-producing phytoplankton group playing an important role in Southern Ocean biogeochemical cycles. Satellite imagery has revealed elevated particulate inorganic carbon concentrations near the major circumpolar fronts of the Southern Ocean that can be attributed to the coccolithophore Emiliania huxleyi. Recent studies have suggested changes during the last decades in the distribution and abundance of Southern Ocean coccolithophores. However, due to limited field observations, the distribution, diversity and state of coccolithophore populations in the Southern Ocean remain poorly characterised. We report here on seasonal variations in the abundance and composition of coccolithophore assemblages collected by two moored sediment traps deployed at the Antarctic zone south of Australia (2000 and 3700 m of depth) for 1 year in 2001-2002. Additionally, seasonal changes in coccolith weights of E. huxleyi populations were estimated using circularly polarised micrographs analysed with C-Calcita software. Our findings indicate that (1) coccolithophore sinking assemblages were nearly monospecific for E. huxleyi morphotype B/C in the Antarctic zone waters in 2001-2002; (2

  13. Fluctuations of cambial activity in relation to precipitation result in annual rings and intra-annual growth zones of xylem and phloem in teak (Tectona grandis) in Ivory Coast

    PubMed Central

    Dié, Agathe; Kitin, Peter; Kouamé, François N'Guessan; Van den Bulcke, Jan; Van Acker, Joris; Beeckman, Hans

    2012-01-01

    Background and Aims Teak forms xylem rings that potentially carry records of carbon sequestration and climate in the tropics. These records are only useful when the structural variations of tree rings and their periodicity of formation are known. Methods The seasonality of ring formation in mature teak trees was examined via correlative analysis of cambial activity, xylem and phloem formation, and climate throughout 1·5 years. Xylem and phloem differentiation were visualized by light microscopy and scanning electron microscopy. Key Results A 3 month dry season resulted in semi-deciduousness, cambial dormancy and formation of annual xylem growth rings (AXGRs). Intra-annual xylem and phloem growth was characterized by variable intensity. Morphometric features of cambium such as cambium thickness and differentiating xylem layers were positively correlated. Cambium thickness was strongly correlated with monthly rainfall (R2 = 0·7535). In all sampled trees, xylem growth zones (XGZs) were formed within the AXGRs during the seasonal development of new foliage. When trees achieved full leaf, the xylem in the new XGZs appeared completely differentiated and functional for water transport. Two phloem growth rings were formed in one growing season. Conclusions The seasonal formation pattern and microstructure of teak xylem suggest that AXGRs and XGZs can be used as proxies for analyses of the tree history and climate at annual and intra-annual resolution. PMID:22805529

  14. Linking major and trace element headwater stream concentrations to DOC release and hydrologic conditions in a bog and peaty riparian zone

    NASA Astrophysics Data System (ADS)

    Broder, Tanja; Biester, Harald

    2017-04-01

    Peatlands and organic-rich riparian zones are known to export large amounts of dissolved organic carbon (DOC) to surface water. In organic-rich, acidic headwater streams main carriers for element export are dissolved organic matter (DOM) and organic-iron complexes. In this environment DOM might also act as major carrier for metals, which otherwise may have a low solubility. This study examines annual and short term event-based variations of major and trace elements in a headwater catchment. Patterns are used to trace hydrological pathways and element sources under different hydrologic preconditions. Furthermore, it elucidates the importance of DOC as carrier of different elements in a bog and a peaty riparian catchment. The study was conducted in a small headwater stream draining an ombrotrophic peatland with an adjacent forested area with peaty riparian soils in the Harz Mountains (Germany). Discharge sampling was conducted weekly at two sites from snowmelt to begin of snowfall and in high resolution during selected discharge events in 2013 and 2014. Element concentrations were measured by means of ICP-MS and ICP-OES. A PCA was performed for each site and for annual and event datasets. Results show that a large number of element concentrations strongly correlate with DOC concentrations at the bog site. Even elements like Ca and Mg, which are known to have a low affinity to DOC. Congruently, the first principal component integrates the DOC pattern (element loadings > 0.8: Ca, Fe, Mg, Mn, Zn, As, Sr, Cd, DOC) and explained about 35 % of total variance and even 50 % during rain events (loadings > 0.8: Al, Ca, Fe, Mg, Mn, Zn, Li, Co, As, Sr, Cd, Pb, DOC). The study cannot verify that all correlating elements bind to DOC. It is likely that also a common mobilization pattern in the upper peat layer by plant decomposition causes the same response to changes in hydrologic pathways. Additionally, a low mineral content and an enrichment of elements like Fe and Mn in the

  15. 76 FR 61112 - Notice of Proposed Information Collection: Comment Request; Annual Progress Reports for...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-10-03

    ... Information Collection: Comment Request; Annual Progress Reports for Empowerment Zones AGENCY: Office of... lists the following information: Title of proposal: Annual Progress Reports for Empowerment Zones. OMB... information collection for reporting requirements of 30 Urban Empowerment Zones (EZs). HUD will regularly...

  16. 76 FR 38297 - Safety Zone; Marine Events Requiring Safety Zones in the Captain of the Port Sault Sainte Marie Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2011-06-30

    ...'' W [DATUM: NAD 83]. (ii) Enforcement Period. This safety zone will be enforced on July 4, 2011 from 9...'' N, 086[deg]39'08.52'' W [DATUM: NAD 83]. (ii) Enforcement Period. This safety zone will be enforced...: NAD 83], with the West Bay shoreline forming the South and West boundaries of the zone. (ii...

  17. 78 FR 56833 - Safety Zone; Fireworks Events in Captain of the Port New York Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-09-16

    ...[deg]41'45'' N, 074[deg]02'09'' W (NAD 1983), about 365 yards east of Ellis Island. This Safety Zone is... Zone, 33 located in approximate position CFR 165.160(5.4). 40[deg]46'11.8'' N, 074[deg]00'14.8'' W (NAD... River Safety Zone, 33 40[deg]44'24'' N, 073[deg]58'00'' W CFR 165.160(4.2). (NAD 1983), approximately...

  18. 78 FR 68995 - Special Local Regulation; Southern California Annual Marine Events for the San Diego Captain of...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-11-18

    ... enforce the special local regulations in 33 CFR 100.1101 during the San Diego Parade of Lights, held on... regulations in 33 CFR 100.1101 in support of the annual marine event, the San Diego Parade of Lights (Item 5 on Table 1 of 33 CFR 100.1101), held over two Sunday nights in December. The Coast Guard will enforce...

  19. 19 CFR 146.25 - Annual reconciliation.

    Code of Federal Regulations, 2010 CFR

    2010-04-01

    ... 19 Customs Duties 2 2010-04-01 2010-04-01 false Annual reconciliation. 146.25 Section 146.25 Customs Duties U.S. CUSTOMS AND BORDER PROTECTION, DEPARTMENT OF HOMELAND SECURITY; DEPARTMENT OF THE TREASURY (CONTINUED) FOREIGN TRADE ZONES Inventory Control and Recordkeeping System § 146.25 Annual...

  20. The annual cycles of phytoplankton biomass

    USGS Publications Warehouse

    Winder, M.; Cloern, J.E.

    2010-01-01

    Terrestrial plants are powerful climate sentinels because their annual cycles of growth, reproduction and senescence are finely tuned to the annual climate cycle having a period of one year. Consistency in the seasonal phasing of terrestrial plant activity provides a relatively low-noise background from which phenological shifts can be detected and attributed to climate change. Here, we ask whether phytoplankton biomass also fluctuates over a consistent annual cycle in lake, estuarine-coastal and ocean ecosystems and whether there is a characteristic phenology of phytoplankton as a consistent phase and amplitude of variability. We compiled 125 time series of phytoplankton biomass (chloro-phyll a concentration) from temperate and subtropical zones and used wavelet analysis to extract their dominant periods of variability and the recurrence strength at those periods. Fewer than half (48%) of the series had a dominant 12-month period of variability, commonly expressed as the canonical spring-bloom pattern. About 20 per cent had a dominant six-month period of variability, commonly expressed as the spring and autumn or winter and summer blooms of temperate lakes and oceans. These annual patterns varied in recurrence strength across sites, and did not persist over the full series duration at some sites. About a third of the series had no component of variability at either the six-or 12-month period, reflecting a series of irregular pulses of biomass. These findings show that there is high variability of annual phytoplankton cycles across ecosystems, and that climate-driven annual cycles can be obscured by other drivers of population variability, including human disturbance, aperiodic weather events and strong trophic coupling between phytoplankton and their consumers. Regulation of phytoplankton biomass by multiple processes operating at multiple time scales adds complexity to the challenge of detecting climate-driven trends in aquatic ecosystems where the noise to

  1. Seasonal and annual variability of coastal sulphur plumes in the northern Benguela upwelling system.

    PubMed

    Ohde, Thomas; Dadou, Isabelle

    2018-01-01

    We investigated the seasonal and annual variability of surface sulphur plumes in the northern Benguela upwelling system off Namibia because of their significant impacts on the marine ecosystem, fishing industry, aquaculture farming and tourism due to their toxic properties. We identified the sulphur plumes in ocean colour satellite data of the medium resolution imaging spectrometer (MERIS) for the 2002-2012 time period using the differences in the spectral properties of Namibian Benguela optical water types. The sulphur events have a strong seasonal cycle with pronounced main and off-seasons forced by local and remote-driven processes. The main peak season is in late austral summer and early austral autumn at the beginning of the annual upwelling cycle caused by increasing equatorwards alongshore winds. The sulphur plume activity is high between February and April during the seasonal oxygen minimum associated with the seasonal reduction of cross-shore ventilation of the bottom waters, the seasonal southernmost position of the Angola Benguela Frontal Zone, the seasonal maximum of water mass fractions of South Atlantic and Angola Gyre Central Waters as well as the seasonal arrival of the downwelling coastal trapped waves. The off-season is in austral spring and early austral summer during increased upwelling intensity and enhanced oxygen supply. The annual variability of sulphur events is characterized by very high activities in years 2004, 2005 and 2010 interrupted by periods of lower activity in years 2002 to 2003, 2006 to 2009 and 2011 to 2012. This result can be explained by the relative contributions or adding effects of local and remote-driven forces (from the equatorial area). The probability for the occurrence of sulphur plumes is enhanced in years with a lower annual mean of upwelling intensity, decreased oxygen supply associated with decreased lateral ventilation of bottom waters, more southern position of the Angola Benguela Frontal Zone, increased mass

  2. Seasonal and annual variability of coastal sulphur plumes in the northern Benguela upwelling system

    PubMed Central

    Dadou, Isabelle

    2018-01-01

    We investigated the seasonal and annual variability of surface sulphur plumes in the northern Benguela upwelling system off Namibia because of their significant impacts on the marine ecosystem, fishing industry, aquaculture farming and tourism due to their toxic properties. We identified the sulphur plumes in ocean colour satellite data of the medium resolution imaging spectrometer (MERIS) for the 2002–2012 time period using the differences in the spectral properties of Namibian Benguela optical water types. The sulphur events have a strong seasonal cycle with pronounced main and off-seasons forced by local and remote-driven processes. The main peak season is in late austral summer and early austral autumn at the beginning of the annual upwelling cycle caused by increasing equatorwards alongshore winds. The sulphur plume activity is high between February and April during the seasonal oxygen minimum associated with the seasonal reduction of cross-shore ventilation of the bottom waters, the seasonal southernmost position of the Angola Benguela Frontal Zone, the seasonal maximum of water mass fractions of South Atlantic and Angola Gyre Central Waters as well as the seasonal arrival of the downwelling coastal trapped waves. The off-season is in austral spring and early austral summer during increased upwelling intensity and enhanced oxygen supply. The annual variability of sulphur events is characterized by very high activities in years 2004, 2005 and 2010 interrupted by periods of lower activity in years 2002 to 2003, 2006 to 2009 and 2011 to 2012. This result can be explained by the relative contributions or adding effects of local and remote-driven forces (from the equatorial area). The probability for the occurrence of sulphur plumes is enhanced in years with a lower annual mean of upwelling intensity, decreased oxygen supply associated with decreased lateral ventilation of bottom waters, more southern position of the Angola Benguela Frontal Zone, increased mass

  3. Decreasing annual nest counts in a globally important loggerhead sea turtle population.

    PubMed

    Witherington, Blair; Kubilis, Paul; Brost, Beth; Meylan, Anne

    2009-01-01

    The loggerhead sea turtle (Caretta caretta) nests on sand beaches, has both oceanic and neritic life stages, and migrates internationally. We analyzed an 18-year time series of Index Nesting Beach Survey (Index) nest-count data to describe spatial and temporal trends in loggerhead nesting on Florida (USA) beaches. The Index data were highly resolved: 368 fixed zones (mean length 0.88 km) were surveyed daily during annual 109-day survey seasons. Spatial and seasonal coverage averaged 69% of estimated total nesting by loggerheads in the state. We carried out trend analyses on both annual survey-region nest-count totals (N = 18) and annual zone-level nest densities (N = 18 x 368 = 6624). In both analyses, negative binomial regression models were used to fit restricted cubic spline curves to aggregated nest counts. Between 1989 and 2006, loggerhead nest counts on Florida Index beaches increased and then declined, with a net decrease over the 18-year period. This pattern was evident in both a trend model of annual survey-region nest-count totals and a mixed-effect, "single-region" trend model of annual zone-level nest densities that took into account both spatial and temporal correlation between counts. We also saw this pattern in a zone-level model that allowed trend line shapes to vary between six coastal subregions. Annual mean zone-level nest density declined significantly (-28%; 95% CI: -34% to -21%) between 1989 and 2006 and declined steeply (-43%; 95% CI: -48% to -39%) during 1998-2006. Rates of change in annual mean nest density varied more between coastal subregions during the "mostly increasing" period prior to 1998 than during the "steeply declining" period after 1998. The excellent fits (observed vs. expected count R2 > 0.91) of the mixed-effect zone-level models confirmed the presence of strong, positive, within-zone autocorrelation (R > 0.93) between annual counts, indicating a remarkable year-to-year consistency in the longshore spatial distribution of

  4. 77 FR 51951 - Special Local Regulation for Marine Events; Temporary Change of Dates for Recurring Marine Events...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-08-28

    ... Events in the Fifth Coast Guard District, Poquoson Seafood Festival Workboat Races, Back River; Poquoson... recurring marine event in the Fifth Coast Guard District. This event is the Poquoson Seafood Festival... city's annual seafood festival. A special local regulation is effective annually to create a safety...

  5. The Tunguska event in 1908: evidence from tree-ring anatomy.

    PubMed

    Vaganov, Evgenii A; Hughes, Malcolm K; Silkin, Pavel P; Nesvetailo, Valery D

    2004-01-01

    We analyzed tree rings in wood samples collected from some of the few surviving trees found close to the epicenter (within 4-5 km) of the Tunguska event that occurred on the last day of June 1908. Tree-ring growth shows a depression starting in the year after the event and continuing during a 4-5-year period. The most remarkable traces of the event were found in the rings' anatomical structure: (1) formation of "light" rings and a reduction of maximum density in 1908; (2) non-thickened tracheids (the cells that make up most of the wood volume) in the transition and latewood zones (the middle and last-formed parts of the ring, respectively); and (3) deformed tracheids, which are located on the 1908 annual ring outer boundary. In the majority of samples, normal earlywood and latewood tracheids were formed in all annual rings after 1908. The observed anomalies in wood anatomy suggest two main impacts of the Tunguska event on surviving trees--(1) defoliation and (2) direct mechanical stress on active xylem tissue. The mechanical stress needed to fell trees is less than the stress needed to cause the deformation of differentiating tracheids observed in trees close to the epicenter. In order to resolve this apparent contradiction, work is suggested on possible topographic modification of the overpressure experienced by these trees, as is an experimental test of the effects of such stresses on precisely analogous growing trees.

  6. 77 FR 14959 - Special Local Regulation for Marine Event; Temporary Change of Dates for Recurring Marine Events...

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-03-14

    ... to do so. The third event is the annual ``Thunder on the Narrows,'' sponsored by the Kent Narrows... effective annually for the Thunder on the Narrows marine event. The event consists of two days of power boat... establishes the enforcement date for the Thunder on the Narrows. This regulation proposes to temporarily...

  7. The Influences of Drought and Land-Cover Conversion on Inter-Annual Variation of NPP in the Three-North Shelterbelt Program Zone of China Based on MODIS Data

    PubMed Central

    Wu, Chaoyang; Zhang, Bing; Huete, Alfredo; Zhang, Xiaoyang; Sun, Rui; Lei, Liping; Huang, Wenjing; Liu, Liangyun; Liu, Xinjie; Li, Jun; Luo, Shezhou; Fang, Bin

    2016-01-01

    Terrestrial ecosystems greatly contribute to carbon (C) emission reduction targets through photosynthetic C uptake.Net primary production (NPP) represents the amount of atmospheric C fixed by plants and accumulated as biomass. The Three-North Shelterbelt Program (TNSP) zone accounts for more than 40% of China’s landmass. This zone has been the scene of several large-scale ecological restoration efforts since the late 1990s, and has witnessed significant changes in climate and human activities.Assessing the relative roles of different causal factors on NPP variability in TNSP zone is very important for establishing reasonable local policies to realize the emission reduction targets for central government. In this study, we examined the relative roles of drought and land cover conversion(LCC) on inter-annual changes of TNSP zone for 2001–2010. We applied integrated correlation and decomposition analyses to a Standardized Evapotranspiration Index (SPEI) and MODIS land cover dataset. Our results show that the 10-year average NPP within this region was about 420 Tg C. We found that about 60% of total annual NPP over the study area was significantly correlated with SPEI (p<0.05). The LCC-NPP relationship, which is especially evident for forests in the south-central area, indicates that ecological programs have a positive impact on C sequestration in the TNSP zone. Decomposition analysis generally indicated that the contributions of LCC, drought, and other Natural or Anthropogenic activities (ONA) to changes in NPP generally had a consistent distribution pattern for consecutive years. Drought and ONA contributed about 74% and 23% to the total changes in NPP, respectively, and the remaining 3% was attributed to LCC. Our results highlight the importance of rainfall supply on NPP variability in the TNSP zone. PMID:27348303

  8. The Effect of Earthquakes on Episodic Tremor and Slip Events on the Southern Cascadia Subduction Zone

    NASA Astrophysics Data System (ADS)

    Sainvil, A. K.; Schmidt, D. A.; Nuyen, C.

    2017-12-01

    The goal of this study is to explore how slow slip events on the southern Cascadia Subduction Zone respond to nearby, offshore earthquakes by examining GPS and tremor data. At intermediate depths on the plate interface ( 40 km), transient fault slip is observed in the form of Episodic Tremor and Slip (ETS) events. These ETS events occur regularly (every 10 months), and have a longer duration than normal earthquakes. Researchers have been documenting slow slip events through data obtained by continuously running GPS stations in the Pacific Northwest. Some studies have proposed that pore fluid may play a role in these ETS events by lowering the effective stress on the fault. The interaction of earthquakes and ETS can provide constraints on the strength of the fault and the level of stress needed to alter ETS behavior. Earthquakes can trigger ETS events, but the connection between these events and earthquake activity is less understood. We originally hypothesized that ETS events would be affected by earthquakes in southern Cascadia, and could result in a shift in the recurrence interval of ETS events. ETS events were cataloged using GPS time series provided by PANGA, in conjunction with tremor positions, in Southern Cascadia for stations YBHB and DDSN from 1997 to 2017. We looked for evidence of change from three offshore earthquakes that occurred near the Mendocino Triple Junction with moment magnitudes of 7.2 in 2005, 6.5 in 2010, and 6.8 in 2014. Our results showed that the recurrence interval of ETS for stations YBHB and DDSN was not altered by the three earthquake events. Future is needed to explore whether this lack of interaction is explained by the non-optimal orientation of the receiver fault for the earthquake focal mechanisms.

  9. 33 CFR 165.1123 - Southern California Annual Firework Events for the San Diego Captain of the Port Zone.

    Code of Federal Regulations, 2014 CFR

    2014-07-01

    ..., or local agencies. Table 1 to § 165.1123 [All coordinates referenced use datum NAD 83] 1. San Diego.... Big Bay Boom Fourth of July Fireworks Sponsor Port of San Diego. Event Description Fireworks Display...

  10. 78 FR 59313 - Safety Zones; Captain of the Port Boston Fireworks Display Zones, Boston Harbor, Boston, MA

    Federal Register 2010, 2011, 2012, 2013, 2014

    2013-09-26

    ...-AA00 Safety Zones; Captain of the Port Boston Fireworks Display Zones, Boston Harbor, Boston, MA AGENCY... establish six permanent safety zones throughout Boston Inner Harbor to be enforced during fireworks displays. These six permanent safety zones would expedite public notification of a fireworks event and ensure the...

  11. 77 FR 23395 - Safety Zones; Recurring Events in Captain of the Port New York Zone

    Federal Register 2010, 2011, 2012, 2013, 2014

    2012-04-19

    ... Safety Zone....... position 40[deg]46'11.8'' N, 33 CFR 165.160(5.4) 074[deg]00'14.8'' W (NAD 1983...'' W (NAD 1983), approximately 380 yards west of Pier 54, Manhattan, NY. Date: June 24, 2012. Time: 10... Zone located in approximate 33 CFR 165.160(2.5) position 40[deg]30'04'' N 074[deg]15'35'' W (NAD 1983...

  12. Characterizing an "uncharacteristic" ETS event in northern Cascadia

    USGS Publications Warehouse

    Wang, Kelin; Dragert, Herb; Kao, Honn; Roeloffs, Evelyn

    2008-01-01

    GPS and borehole strainmeter data allowed the detection and model characterization of a slow slip event in northern Cascadia in November 2006 accompanying a brief episode of seismic tremor. The event is much smaller in area and duration than other well-known ETS events in northern Cascadia but is strikingly similar to typical ETS events at the Nankai subduction zone. The 30-45 km depth range and the 2-3 cm slip magnitude as interpreted for this event appear to be common to most ETS events in these two subduction zones, regardless of their sizes. We infer that the Nankai-type small ETS events must be abundant at Cascadia and that ETS events at the two subduction zones are governed by a similar physical process.

  13. Unexpected extreme events drive the inter-annual variabilty in carbon exchange at the Pine forest in Netherlands.

    NASA Astrophysics Data System (ADS)

    Sethi, Sanjna; Moors, Eddy; Jamir, Chubamenla

    2017-04-01

    The carbon exchange between vegetation and the atmosphere tends to vary on an annual basis. This change is a continuous process its trend emerging over a period of years can be analysed. In any such trend over a prolonged period, some years stand out more than the others on account of extreme events. Explaining deviations from the expected average emissions may help to understand the drivers behind these interannual deviations. Such noticeable deviations in trend maybe on account of extreme events and need to be analysed in overall context of the ecosystem. This research's focus is to identify the main drivers responsible for the deviations, and how extreme events impact the variability over a prolonged period of time. The hypothesis being that extreme events are driving these deviations. Carbon flux data done for multiple years (1997-2015) for a site at the Loobos Pine Forest is used and compared with an ecosystem model, LPJ-GUESS (Lund-Potsdam-Jena General Ecosystem Simulator) to understand if the deviation of measured data from the simulated data is on account of extreme events on a monthly and daily basis. A Principal Component Analysis is performed on the identified deviations between measured and simulated carbon exchange to pin point the main cause behind their occurrence.​

  14. Characterizing an "uncharacteristics" ETS event in northern Cascadia

    USGS Publications Warehouse

    Wang, K.; Dragert, H.; Kao, H.; Roeloffs, E.

    2008-01-01

    GPS and borehole strainmeter data allowed the detection and model characterization of a slow slip event in northern Cascadia in November 2006 accompanying a brief episode of seismic tremor. The event is much smaller in area and duration than other well-known ETS events in northern Cascadia but is strikingly similar to typical ETS events at the Nankai subduction zone. The 30-45 km depth range and the 2-3 cm slip magnitude as interpreted for this event appear to be common to most ETS events in these two subduction zones, regardless of their sizes. We infer that the Nankai-type small ETS events must be abundant at Cascadia and that ETS event at the two subduction zones are governed by a similar physical process. Copyright 2008 by the American Geophysical Union.

  15. International Observe the Moon Night: A Worldwide Public Observing Event that Annually Engages Scientists, Educators, and Citizen Enthusiasts in NASA Science

    NASA Astrophysics Data System (ADS)

    Buxner, S.; Jones, A. P.; Bleacher, L.; Wasser, M. L.; Day, B. H.; Shaner, A. J.; Bakerman, M. N.; Joseph, E.

    2017-12-01

    International Observe the Moon Night (InOMN) is an annual worldwide event, held in the fall, that celebrates lunar and planetary science and exploration. InOMN is sponsored by NASA's Lunar Reconnaissance Orbiter (LRO) in collaboration with NASA's Solar System Exploration Research Virtual Institute (SSERVI), the NASA's Heliophysics Education Consortium, CosmoQuest, Night Sky Network, and Science Festival Alliance. Other key partners include the NASA Museum Alliance, Night Sky Network, and NASA Solar System Ambassadors. In 2017, InOMN will bring together thousands of people across the globe to observe and learn about the Moon and its connection to planetary science. We are partnering with the NASA Science Mission Directorate total solar eclipse team to highlight InOMN as an opportunity to harness and sustain the interest and momentum in space science and observation following the August 21st eclipse. This is part of a new partnership with the Sun-Earth Day team, through the Heliophysics Education Consortium, to better connect the two largest NASA-sponsored public engagement events, increase participation in both events, and share best practices in implementation and evaluation between the teams. Over 3,800 InOMN events have been registered between 2010 and 2016, engaging over 550,000 visitors worldwide. Most InOMN events are held in the United States, with strong representation from many other countries. InOMN events are evaluated to determine the value of the events and to allow us to improve the experience for event hosts and visitors. Our results show that InOMN events are hosted by scientists, educators, and citizen enthusiasts around the world who leverage InOMN to bring communities together, get visitors excited and learn about the Moon - and beyond, and share resources to extend engagement in lunar and planetary science and observation. Through InOMN, we annually provide resources such as event-specific Moon maps, presentations, advertising materials, and

  16. Turbidite event history--Methods and implications for Holocene paleoseismicity of the Cascadia subduction zone

    USGS Publications Warehouse

    Goldfinger, Chris; Nelson, C. Hans; Morey, Ann E.; Johnson, Joel E.; Patton, Jason R.; Karabanov, Eugene B.; Gutierrez-Pastor, Julia; Eriksson, Andrew T.; Gracia, Eulalia; Dunhill, Gita; Enkin, Randolph J.; Dallimore, Audrey; Vallier, Tracy; Kayen, Robert; Kayen, Robert

    2012-01-01

    Turbidite systems along the continental margin of Cascadia Basin from Vancouver Island, Canada, to Cape Mendocino, California, United States, have been investigated with swath bathymetry; newly collected and archive piston, gravity, kasten, and box cores; and accelerator mass spectrometry radiocarbon dates. The purpose of this study is to test the applicability of the Holocene turbidite record as a paleoseismic record for the Cascadia subduction zone. The Cascadia Basin is an ideal place to develop a turbidite paleoseismologic method and to record paleoearthquakes because (1) a single subduction-zone fault underlies the Cascadia submarine-canyon systems; (2) multiple tributary canyons and a variety of turbidite systems and sedimentary sources exist to use in tests of synchronous turbidite triggering; (3) the Cascadia trench is completely sediment filled, allowing channel systems to trend seaward across the abyssal plain, rather than merging in the trench; (4) the continental shelf is wide, favoring disconnection of Holocene river systems from their largely Pleistocene canyons; and (5) excellent stratigraphic datums, including the Mazama ash and distinguishable sedimentological and faunal changes near the Pleistocene-Holocene boundary, are present for correlating events and anchoring the temporal framework. Multiple tributaries to Cascadia Channel with 50- to 150-km spacing, and a wide variety of other turbidite systems with different sedimentary sources contain 13 post-Mazama-ash and 19 Holocene turbidites. Likely correlative sequences are found in Cascadia Channel, Juan de Fuca Channel off Washington, and Hydrate Ridge slope basin and Astoria Fan off northern and central Oregon. A probable correlative sequence of turbidites is also found in cores on Rogue Apron off southern Oregon. The Hydrate Ridge and Rogue Apron cores also include 12-22 interspersed thinner turbidite beds respectively. We use 14C dates, relative-dating tests at channel confluences, and

  17. Energy-dependent dynamics of keV to MeV electrons in the inner zone, outer zone, and slot regions.

    PubMed

    Reeves, Geoffrey D; Friedel, Reiner H W; Larsen, Brian A; Skoug, Ruth M; Funsten, Herbert O; Claudepierre, Seth G; Fennell, Joseph F; Turner, Drew L; Denton, Mick H; Spence, Harlan E; Blake, J Bernard; Baker, Daniel N

    2016-01-01

    We present observations of the radiation belts from the Helium Oxygen Proton Electron and Magnetic Electron Ion Spectrometer particle detectors on the Van Allen Probes satellites that illustrate the energy dependence and L shell dependence of radiation belt enhancements and decays. We survey events in 2013 and analyze an event on 1 March in more detail. The observations show the following: (a) at all L shells, lower energy electrons are enhanced more often than higher energies; (b) events that fill the slot region are more common at lower energies; (c) enhancements of electrons in the inner zone are more common at lower energies; and (d) even when events do not fully fill the slot region, enhancements at lower energies tend to extend to lower L shells than higher energies. During enhancement events the outer zone extends to lower L shells at lower energies while being confined to higher L shells at higher energies. The inner zone shows the opposite with an outer boundary at higher L shells for lower energies. Both boundaries are nearly straight in log(energy) versus L shell space. At energies below a few 100 keV, radiation belt electron penetration through the slot region into the inner zone is commonplace, but the number and frequency of "slot filling" events decreases with increasing energy. The inner zone is enhanced only at energies that penetrate through the slot. Energy- and L shell-dependent losses (that are consistent with whistler hiss interactions) return the belts to more quiescent conditions.

  18. Energy-dependent dynamics of keV to MeV electrons in the inner zone, outer zone, and slot regions

    DOE PAGES

    Reeves, Geoffrey D.; Friedel, Reiner H. W.; Larsen, Brian A.; ...

    2016-01-28

    Here, we present observations of the radiation belts from the Helium Oxygen Proton Electron and Magnetic Electron Ion Spectrometer particle detectors on the Van Allen Probes satellites that illustrate the energy dependence and L shell dependence of radiation belt enhancements and decays. We survey events in 2013 and analyze an event on 1 March in more detail. The observations show the following: (a) at all L shells, lower energy electrons are enhanced more often than higher energies; (b) events that fill the slot region are more common at lower energies; (c) enhancements of electrons in the inner zone are moremore » common at lower energies; and (d) even when events do not fully fill the slot region, enhancements at lower energies tend to extend to lower L shells than higher energies. During enhancement events the outer zone extends to lower L shells at lower energies while being confined to higher L shells at higher energies. The inner zone shows the opposite with an outer boundary at higher L shells for lower energies. Both boundaries are nearly straight in log(energy) versus L shell space. At energies below a few 100 keV, radiation belt electron penetration through the slot region into the inner zone is commonplace, but the number and frequency of “slot filling” events decreases with increasing energy. The inner zone is enhanced only at energies that penetrate through the slot. Energy- and L shell-dependent losses (that are consistent with whistler hiss interactions) return the belts to more quiescent conditions.« less

  19. Energy‐dependent dynamics of keV to MeV electrons in the inner zone, outer zone, and slot regions

    PubMed Central

    Friedel, Reiner H. W.; Larsen, Brian A.; Skoug, Ruth M.; Funsten, Herbert O.; Claudepierre, Seth G.; Fennell, Joseph F.; Turner, Drew L.; Denton, Mick H.; Spence, Harlan E.; Blake, J. Bernard; Baker, Daniel N.

    2016-01-01

    Abstract We present observations of the radiation belts from the Helium Oxygen Proton Electron and Magnetic Electron Ion Spectrometer particle detectors on the Van Allen Probes satellites that illustrate the energy dependence and L shell dependence of radiation belt enhancements and decays. We survey events in 2013 and analyze an event on 1 March in more detail. The observations show the following: (a) at all L shells, lower energy electrons are enhanced more often than higher energies; (b) events that fill the slot region are more common at lower energies; (c) enhancements of electrons in the inner zone are more common at lower energies; and (d) even when events do not fully fill the slot region, enhancements at lower energies tend to extend to lower L shells than higher energies. During enhancement events the outer zone extends to lower L shells at lower energies while being confined to higher L shells at higher energies. The inner zone shows the opposite with an outer boundary at higher L shells for lower energies. Both boundaries are nearly straight in log(energy) versus L shell space. At energies below a few 100 keV, radiation belt electron penetration through the slot region into the inner zone is commonplace, but the number and frequency of “slot filling” events decreases with increasing energy. The inner zone is enhanced only at energies that penetrate through the slot. Energy‐ and L shell‐dependent losses (that are consistent with whistler hiss interactions) return the belts to more quiescent conditions. PMID:27818855

  20. New constraints on the Pan-African tectonics and the role of the Mwembeshi Zone in Central Zambia: Deformation style and timing of two orthogonal shortening events

    NASA Astrophysics Data System (ADS)

    Naydenov, Kalin; Lehmann, Jeremie; Saalmann, Kerstin; Milani, Lorenzo; Kinnaird, Judith; Charlesworth, Guy; Rankin, William; Frei, Dirk

    2014-05-01

    In Central Zambia the Mwembeshi Zone (MwZ) separates two branches of the Late Neoproterozoic - Cambrian Pan-African Orogen: the NE-convex Lufilian Arc and the E-W trending Zambezi Belt whose distinct features emphasize the role of the zone as a regional structural and metamorphic boundary. North of the MwZ, the Hook Batholith was emplaced within the low metamorphic grade Neoproterozoic metasedimentary rocks, and represents the largest Pan-African intrusion in Southern Africa. The granitoids and their host-rocks were affected by two deformation events. During the D1 deformation of E-W shortening, two high-strained zones developed in the batholith. To the NE, the Nalusanga Zone (NZ) is a ~3 km wide NW-striking subvertical sinistral strike-slip shear zone. To the SW, a ~2.5 km wide N-S trending subvertical pure-shear Itezhi-Tezhi Zone (ITZ) formed. In both structures, the granitoids show a smooth transition from weakly deformed rocks to porphyroclastic mylonites. Microstructural analysis defined them as medium metamorphic grade zones, deforming the granitoids at temperatures between 500 and 550°C. The lower greenschist facies metamorphism in the country rocks indicates that the deformation occurred during the cooling of the granitoids. D1 in the metasedimentary rocks east of the Hook batholith formed tight, upright folds with subvertical axial-planar cleavage and NNW-SSE trending axis consistent with the E-W shortening. U-Pb zircon geochronology and cross-cutting relationships between granites bracket D1 deformation between 549 ± 2 Ma and 541 ± 3 Ma in the NZ and in the SE part of the batholith. In the ITZ, the 533 ± 3 Ma age on a deformed granite indicates prolonged E-W shortening during granite emplacement and cooling history. D2 represents a stage of N-S shortening. Airborne geophysical data revealed bending of the N-S trending ITZ and rotation to the east. The D1 structures in the granitoids are cut by D2 north-vergent thrusts and subvertical NW trending

  1. Zone model predictive control: a strategy to minimize hyper- and hypoglycemic events.

    PubMed

    Grosman, Benyamin; Dassau, Eyal; Zisser, Howard C; Jovanovic, Lois; Doyle, Francis J

    2010-07-01

    Development of an artificial pancreas based on an automatic closed-loop algorithm that uses a subcutaneous insulin pump and continuous glucose sensor is a goal for biomedical engineering research. However, closing the loop for the artificial pancreas still presents many challenges, including model identification and design of a control algorithm that will keep the type 1 diabetes mellitus subject in normoglycemia for the longest duration and under maximal safety considerations. An artificial pancreatic beta-cell based on zone model predictive control (zone-MPC) that is tuned automatically has been evaluated on the University of Virginia/University of Padova Food and Drug Administration-accepted metabolic simulator. Zone-MPC is applied when a fixed set point is not defined and the control variable objective can be expressed as a zone. Because euglycemia is usually defined as a range, zone-MPC is a natural control strategy for the artificial pancreatic beta-cell. Clinical data usually include discrete information about insulin delivery and meals, which can be used to generate personalized models. It is argued that mapping clinical insulin administration and meal history through two different second-order transfer functions improves the identification accuracy of these models. Moreover, using mapped insulin as an additional state in zone-MPC enriches information about past control moves, thereby reducing the probability of overdosing. In this study, zone-MPC is tested in three different modes using unannounced and announced meals at their nominal value and with 40% uncertainty. Ten adult in silico subjects were evaluated following a scenario of mixed meals with 75, 75, and 50 grams of carbohydrates (CHOs) consumed at 7 am, 1 pm, and 8 pm, respectively. Zone-MPC results are compared to those of the "optimal" open-loop preadjusted treatment. Zone-MPC succeeds in maintaining glycemic responses closer to euglycemia compared to the "optimal" open-loop treatment in te three

  2. Genetic parameters of eventing horse competition in France

    PubMed Central

    Ricard, Anne; Chanu, Isabelle

    2001-01-01

    Genetic parameters of eventing horse competitions were estimated. About 13 000 horses, 30 000 annual results during 17 years and 110 000 starts in eventing competitions during 8 years were recorded. The measures of performance were logarithmic transformations of annual earnings, annual earnings per start, and annual earnings per place, and underlying variables responsible for ranks in each competition. Heritabilities were low (0.11/0.17 for annual results, 0.07 for ranks). Genetic correlations between criteria were high (greater than 0.90) except between ranks and earnings per place (0.58) or per start (0.67). Genetic correlations between ages (from 5 to 10 years old) were also high (more than 0.85) and allow selection on early performances. The genetic correlation between the results in different levels of competition (high/international and low/amateur) was near 1. Genetic correlations of eventing with other disciplines, which included partial aptitude needed for eventing, were very low for steeplechase races (0.18) and moderate with sport: jumping (0.45), dressage (0.58). The results suggest that selection on jumping performance will lead to some positive correlated response for eventing performance, but much more response could be obtained if a specific breeding objective and selection criteria were developed for eventing. PMID:11333833

  3. The investigation of form and processes in the coastal zone under extreme storm events - the case study of Rethymno, Greece

    NASA Astrophysics Data System (ADS)

    Afentoulis, Vasileios; Mohammadi, Bijan; Tsoukala, Vasiliki

    2017-04-01

    Coastal zone is a significant geographical and particular region, since it gathers a wide range of social-human's activities and appears to be a complex as well as fragile system of natural variables. Coastal communities are increasingly at risk from serious coastal hazards, such as shoreline erosion and flooding related to extreme hydro-meteorological events: storm surges, heavy precipitation, tsunamis and tides. In order to investigate the impact of these extreme events on the coastal zone, it is necessary to describe the driving mechanisms which contribute to its destabilization and more precisely the interaction between the wave forces and the transport of sediment. The aim of the present study is to examine the capability of coastal zone processes simulation under extreme wave events, using numerical models, in the coastal area of Rethymno, Greece. Rethymno city is one of the eleven case study areas of PEARL (Preparing for Extreme And Rare events in coastal regions) project, an EU funded research project, which aims at developing adaptive risk management strategies for coastal communities focusing on extreme hydro-meteorological events, with a multidisciplinary approach integrating social, environmental and technical research and innovation so as to increase the resilience of coastal regions all over the world. Within this framework, three different numerical models have been used: the MIKE 21 - DHI, the XBeach model and a numerical formulation for sea bed evolution, developed by Afaf Bouharguane and Bijan Mohammadi (2013). For the determination of the wave and hydrodynamic conditions, as well as the assessment of the sediment transport components, the MIKE 21 SW and the MIKE 21 FM modules have been applied and the bathymetry of Rethymno is arranged into a 2D unstructured mesh. This method of digitalization was selected because of its ability to easily represent the complex geometry of the coastal zone. It allows smaller scale wave characteristics to be

  4. Fracture process zone in granite

    USGS Publications Warehouse

    Zang, A.; Wagner, F.C.; Stanchits, S.; Janssen, C.; Dresen, G.

    2000-01-01

    In uniaxial compression tests performed on Aue granite cores (diameter 50 mm, length 100 mm), a steel loading plate was used to induce the formation of a discrete shear fracture. A zone of distributed microcracks surrounds the tip of the propagating fracture. This process zone is imaged by locating acoustic emission events using 12 piezoceramic sensors attached to the samples. Propagation velocity of the process zone is varied by using the rate of acoustic emissions to control the applied axial force. The resulting velocities range from 2 mm/s in displacement-controlled tests to 2 ??m/s in tests controlled by acoustic emission rate. Wave velocities and amplitudes are monitored during fault formation. P waves transmitted through the approaching process zone show a drop in amplitude of 26 dB, and ultrasonic velocities are reduced by 10%. The width of the process zone is ???9 times the grain diameter inferred from acoustic data but is only 2 times the grain size from optical crack inspection. The process zone of fast propagating fractures is wider than for slow ones. The density of microcracks and acoustic emissions increases approaching the main fracture. Shear displacement scales linearly with fracture length. Fault plane solutions from acoustic events show similar orientation of nodal planes on both sides of the shear fracture. The ratio of the process zone width to the fault length in Aue granite ranges from 0.01 to 0.1 inferred from crack data and acoustic emissions, respectively. The fracture surface energy is estimated from microstructure analysis to be ???2 J. A lower bound estimate for the energy dissipated by acoustic events is 0.1 J. Copyright 2000 by the American Geophysical Union.

  5. 33 CFR 165.163 - Safety Zones; Port of New York/New Jersey Fleet Week.

    Code of Federal Regulations, 2011 CFR

    2011-07-01

    ... as safety zones: (1) Safety Zone A—(i) Location. A moving safety zone for the Parade of Ships... Wednesday before Memorial Day. (2) Safety Zone B—(i) Location. A safety zone including all waters of the.... (ii) Enforcement period. Paragraph (a)(2)(i) of this section is enforced annually from 8 a.m. until 5...

  6. Signs of lateral transport of CO2 and CH4 in freshwater systems in boreal zone

    NASA Astrophysics Data System (ADS)

    Ojala, A.; Pumpanen, J. S.

    2013-12-01

    The numerous waterbodies and their riparian zones in the boreal zone are important to lateral carbon transport of terrestrial origin. These freshwater systems are also significant for carbon cycling on the landscape level. However, the lateral signals of carbon gases can be difficult to detect and thus, we used here different approaches to verify the phenomenon. We installed continuous measurement systems with CO2 probes in the riparian zone soil matrix around a small pristine headwater lake, in the lake, and in the outflowing stream and followed up the seasonal variation in CO2 concentration and in rain event-driven changes. We also used the probes in a second-order stream discharging a catchment of managed forest. The conventional weekly sampling protocol on water column CO2 and CH4 concentrations as well as gas fluxes was applied in three lakes surrounded by managed forests and some crop land but having different size and water quality. In two of the lakes most drastic changes in gas fluxes occurred not in spring but during or just after the summer rains when the clear water lake changed from a small carbon sink to carbon source and in the humic lake almost half of the CO2 and CH4 fluxes occurred during or just after the rainy period. Gas concentrations in the water columns revealed that the high surface water concentrations resulting in peak fluxes were not due to transport from hypolimnia rich in gases, but were due to soil processes and export from the flooded catchments. In the third lake, seasonal peak fluxes took place just after ice out, but again this was not a result of carbon gases accumulated under the ice, but gases originated from the surrounding catchment. In this lake, ca. 30 % of the annual CO2 flux occurred in May and 13 % of CH4 was emitted during one single week in May. In general, CH4 appeared as a good tracer for lateral transport. In the soil-lake-stream continuum, seasonal variation in CO2 was greatest and concentrations highest deep in

  7. Annual nitrate drawdown observed by SOCCOM profiling floats and the relationship to annual net community production

    NASA Astrophysics Data System (ADS)

    Johnson, Kenneth S.; Plant, Joshua N.; Dunne, John P.; Talley, Lynne D.; Sarmiento, Jorge L.

    2017-08-01

    Annual nitrate cycles have been measured throughout the pelagic waters of the Southern Ocean, including regions with seasonal ice cover and southern hemisphere subtropical zones. Vertically resolved nitrate measurements were made using in situ ultraviolet spectrophotometer (ISUS) and submersible ultraviolet nitrate analyzer (SUNA) optical nitrate sensors deployed on profiling floats. Thirty-one floats returned 40 complete annual cycles. The mean nitrate profile from the month with the highest winter nitrate minus the mean profile from the month with the lowest nitrate yields the annual nitrate drawdown. This quantity was integrated to 200 m depth and converted to carbon using the Redfield ratio to estimate annual net community production (ANCP) throughout the Southern Ocean south of 30°S. A well-defined, zonal mean distribution is found with highest values (3-4 mol C m-2 yr-1) from 40 to 50°S. Lowest values are found in the subtropics and in the seasonal ice zone. The area weighted mean was 2.9 mol C m-2 yr-1 for all regions south of 40°S. Cumulative ANCP south of 50°S is 1.3 Pg C yr-1. This represents about 13% of global ANCP in about 14% of the global ocean area.Plain Language SummaryThis manuscript reports on 40 <span class="hlt">annual</span> cycles of nitrate observed by chemical sensors on SOCCOM profiling floats. The <span class="hlt">annual</span> drawdown in nitrate concentration by phytoplankton is used to assess the spatial variability of <span class="hlt">annual</span> net community production in the Southern Ocean. This ANCP is a key component of the global carbon cycle and it exerts an important control on atmospheric carbon dioxide. We show that the results are consistent with our prior understanding of Southern Ocean ANCP, which has required decades of observations to accumulate. The profiling floats now enable <span class="hlt">annual</span> resolution of this key process. The results also highlight spatial variability in ANCP in the Southern Ocean.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018E%26PSL.491...81Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018E%26PSL.491...81Y"><span>A viscoplastic shear-<span class="hlt">zone</span> model for deep (15-50 km) slow-slip <span class="hlt">events</span> at plate convergent margins</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yin, An; Xie, Zhoumin; Meng, Lingsen</p> <p>2018-06-01</p> <p>A key issue in understanding the physics of deep (15-50 km) slow-slip <span class="hlt">events</span> (D-SSE) at plate convergent margins is how their initially unstable motion becomes stabilized. Here we address this issue by quantifying a rate-strengthening mechanism using a viscoplastic shear-<span class="hlt">zone</span> model inspired by recent advances in field observations and laboratory experiments. The well-established segmentation of slip modes in the downdip direction of a subduction shear <span class="hlt">zone</span> allows discretization of an interseismic forearc system into the (1) frontal segment bounded by an interseismically locked megathrust, (2) middle segment bounded by episodically locked and unlocked viscoplastic shear <span class="hlt">zone</span>, and (3) interior segment that slips freely. The three segments are assumed to be linked laterally by two springs that tighten with time, and the increasing elastic stress due to spring tightening eventually leads to plastic failure and initial viscous shear. This simplification leads to seven key model parameters that dictate a wide range of mechanical behaviors of an idealized convergent margin. Specifically, the viscoplastic rheology requires the initially unstable sliding to be terminated nearly instantaneously at a characteristic velocity, which is followed by stable sliding (i.e., slow-slip). The characteristic velocity, which is on the order of <10-7 m/s for the convergent margins examined in this study, depends on the (1) effective coefficient of friction, (2) thickness, (3) depth, and (4) viscosity of the viscoplastic shear <span class="hlt">zone</span>. As viscosity decreases exponentially with temperature, our model predicts faster slow-slip rates, shorter slow-slip durations, more frequent slow-slip occurrences, and larger slow-slip magnitudes at warmer convergent margins.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1810383L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1810383L"><span><span class="hlt">Annual</span> glacier dammed lake drainage in Zackenberg, Northeast Greenland</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lane, Timothy; Adamson, Kathryn; Matthews, Tom</p> <p>2016-04-01</p> <p>A.P. Olsen is a 295 km2 ice cap in the Zackenberg region of Northeast Greenland (74.6° N, 21.5° W), 35 km from the ZERO Zackenberg Research Station. The ice cap lies on a gneissic plateau, covering an elevation of 200 to 1450 m a.s.l. A.P. Olsen mass balance has been monitored since 2008 and reconstructed for the period 1995-2007. Meltwater from this ice cap drains into the Zackenberg River, and into Young Sund via the Zackenberg Delta. One outlet dams a c. 0.8 km2 lake fed by the northern part of the ice cap. Observational data suggests this lake drains <span class="hlt">annually</span>, flooding subglacially into the Zackenberg River. But the impacts of these flood <span class="hlt">events</span> on the hydrology, sediment transfer, and geomorphology of the proglacial <span class="hlt">zone</span> downstream have not been examined in detail. Understanding the impacts of glacial lake outburst flood <span class="hlt">events</span> is important in the sensitive Arctic environment, where glacial change is rapid. We use Landsat scenes to reconstruct lake extent from 1999-2015. This is compared to Zackenberg River discharge measurements, available from the ZERO Zackenberg monitoring programme. These datasets are used to examine the nature and timing of flood <span class="hlt">events</span>, and assess the impacts on the Zackenberg river downstream.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018Geote..52..266M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018Geote..52..266M"><span>Structure of Masuleh Shear <span class="hlt">Zone</span>: Evidence for Early–Middle Jurassic Dextral Shear Along Paleo-Tethys Suture <span class="hlt">Zone</span> in the Western Alborz, NW Iran</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Moosavi, E.; Rasouli-Jamadi, F.</p> <p>2018-03-01</p> <p>The Paleo-Tethys suture <span class="hlt">zone</span> in northern Iran was formed when the Paleo-Tethys Ocean, (between Gonwana-derived Alborz Microcontinent and the Turan Plate), closed during the Eocimmerian orogeny and after they collided together in the Mid-Late Triassic. The NW-striking Boghrov-Dagh basement Fault <span class="hlt">Zone</span> that lies in the vicinity of Masuleh village and the southern boundary of Gasht Metamorphic Complex is a part of the Eocimmerian suture <span class="hlt">zone</span> in the Western Alborz. Along this part of the suture <span class="hlt">zone</span>, tourmaline leucogranites intruded in metamorphic rocks. We recognize three distinct deformation stages (D1 to D3) in the study area especially in the Masuleh Shear <span class="hlt">Zone</span>. D1 which was synchronous with formation of the main metamorphic minerals, such as sillimanite and staurolite under medium- to high-grade metamorphic conditions probably during the Hercynian <span class="hlt">event</span> and a NE-directed shortening. The slaty cleavage in metamorphosed Upper Paleozoic rocks and crenulation cleavage and folds in the older rocks were produced due to D2 deformation during the Eocimmerian <span class="hlt">event</span> under greenschist facies conditions. The Masuleh Shear <span class="hlt">Zone</span> formed as a result of a ductile strike-slip shear during the Early-Middle Jurassic Mid-Cimmerian D3 <span class="hlt">event</span> with a pure dextral to transtension shear sense at low to locally medium-grade conditions. All of the D3 structural features agree with a NNW-directed compression and an ENE-directed extension caused by overall dextral shear parallel to the Masuleh shear <span class="hlt">zone</span> and the Boghrov-Dagh Fault <span class="hlt">Zone</span>. Based on the available evidence, especially cross-cutting relationships between structural fabrics and rock units, emplacement of the Gasht-Masuleh leucogranites occurred after the D2 collisional <span class="hlt">event</span> coeval to the possible slab break-off and before the D3 <span class="hlt">event</span>, between Eocimmerian and Mid-Cimmerian movements.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.H41I1558D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.H41I1558D"><span>Estimating the proportion of groundwater recharge from flood <span class="hlt">events</span> in relation to total <span class="hlt">annual</span> recharge in a karst aquifer</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dvory, N. Z.; Ronen, A.; Livshitz, Y.; Adar, E.; Kuznetsov, M.; Yakirevich, A.</p> <p>2017-12-01</p> <p>Sustainable groundwater production from karstic aquifers is primarily dictated by its recharge rate. Therefore, in order to limit over-exploitation, it is essential to accurately quantify groundwater recharge. Infiltration during erratic floods in karstic basins may contribute substantial amount to aquifer recharge. However, the complicated nature of karst systems, which are characterized in part by multiple springs, sinkholes, and losing/gaining streams, present a large obstacle to accurately assess the actual contribution of flood water to groundwater recharge. In this study, we aim to quantify the proportion of groundwater recharge during flood <span class="hlt">events</span> in relation to the <span class="hlt">annual</span> recharge for karst aquifers. The role of karst conduits on flash flood infiltration was examined during four flood and artificial runoff <span class="hlt">events</span> in the Sorek creek near Jerusalem, Israel. The <span class="hlt">events</span> were monitored in short time steps (four minutes). This high resolution analysis is essential to accurately estimating surface flow volumes, which are of particular importance in arid and semi-arid climate where ephemeral flows may provide a substantial contribution to the groundwater reservoirs. For the present investigation, we distinguished between direct infiltration, percolation through karst conduits and diffused infiltration, which is most affected by evapotranspiration. A water balance was then calculated for the 2014/15 hydrologic year using the Hydrologic Engineering Center - Hydrologic Modelling System (HEC-HMS). Simulations show that an additional 8% to 24% of the <span class="hlt">annual</span> recharge volume is added from runoff losses along the creek that infiltrate through the karst system into the aquifer. The results improve the understanding of recharge processes and support the use of the proposed methodology for quantifying groundwater recharge.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ncifrederick.cancer.gov/about/theposter/content/summer-events-scientific-library','NCI'); return false;" href="https://ncifrederick.cancer.gov/about/theposter/content/summer-events-scientific-library"><span>Summer <span class="hlt">Events</span> at the Scientific Library | Poster</span></a></p> <p><a target="_blank" href="http://www.cancer.gov">Cancer.gov</a></p> <p></p> <p></p> <p>Two exciting <span class="hlt">events</span> are coming this summer from the Scientific Library—the <span class="hlt">annual</span> Student Science Jeopardy Tournament and the Summer Video Series. This year, the 10th <span class="hlt">Annual</span> Student Science Jeopardy Tournament will be held on Wednesday, July 20, beginning at 10 a.m. in the auditorium of Building 549. The <span class="hlt">event</span> will also be streamed live to the Advanced Technology Research</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-05-28/pdf/2010-12846.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-05-28/pdf/2010-12846.pdf"><span>75 FR 29886 - Special Local Regulation for Marine <span class="hlt">Events</span>; Temporary Change of Dates for Recurring Marine <span class="hlt">Events</span>...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-05-28</p> <p>... typically comprise marine <span class="hlt">events</span> include sailing regattas, power boat races, swim races and holiday boat... marine <span class="hlt">event</span> that conducts various river boat races and a parade. Special local regulations are necessary... <span class="hlt">annually</span> for this marine <span class="hlt">event</span>. The <span class="hlt">event</span> will consist of several boat races and parades on the Southern...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://peer.berkeley.edu/events','SCIGOVWS'); return false;" href="http://peer.berkeley.edu/events"><span><span class="hlt">Events</span> | Pacific Earthquake Engineering Research Center</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>home about <em>peer</em> news <span class="hlt">events</span> research products laboratories publications nisee b.i.p. members education FAQs links <span class="hlt">Events</span> Calendar of <em>PEER</em> and Other <span class="hlt">Events</span> <em>PEER</em> <span class="hlt">Events</span> Archive <em>PEER</em> <span class="hlt">Annual</span> Meeting 2009 Experimental Structural Engineering <em>PEER</em> Summative Meeting Site Map Search Calendar of <em>PEER</em> and Other <span class="hlt">Events</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70033566','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70033566"><span>Water movement within the unsaturated <span class="hlt">zone</span> in four agricultural areas of the United States</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Fisher, L.H.; Healy, R.W.</p> <p>2008-01-01</p> <p>Millions of tons of agricultural fertilizer and pesticides are applied <span class="hlt">annually</span> in the USA. Due to the potential for these chemicals to migrate to groundwater, a study was conducted in 2004 using field data to calculate water budgets, rates of groundwater recharge and times of water travel through the unsaturated <span class="hlt">zone</span> and to identify factors that influence these phenomena. Precipitation was the only water input at sites in Indiana and Maryland; irrigation accounted for about 80% of total water input at sites in California and Washington. Recharge at the Indiana site (47.5 cm) and at the Maryland site (31.5 cm) were equivalent to 51 and 32%, respectively, of <span class="hlt">annual</span> precipitation and occurred between growing seasons. Recharge at the California site (42.3 cm) and Washington site (11.9 cm) occurred in response to irrigation <span class="hlt">events</span> and was about 29 and 13% of total water input, respectively. Average residence time of water in the unsaturated <span class="hlt">zone</span>, calculated using a piston-flow approach, ranged from less than 1 yr at the Indiana site to more than 8 yr at the Washington site. Results of bromide tracer tests indicate that at three of the four sites, a fraction of the water applied at land surface may have traveled to the water table in less than 1 yr. The timing and intensity of precipitation and irrigation were the dominant factors controlling recharge, suggesting that the time of the year at which chemicals are applied may be important for chemical transport through the unsaturated <span class="hlt">zone</span>. Copyright ?? 2008 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ncifrederick.cancer.gov/about/theposter/node/1383','NCI'); return false;" href="https://ncifrederick.cancer.gov/about/theposter/node/1383"><span>Summer <span class="hlt">Events</span> at the Scientific Library | Poster</span></a></p> <p><a target="_blank" href="http://www.cancer.gov">Cancer.gov</a></p> <p></p> <p></p> <p>Two exciting <span class="hlt">events</span> are coming this summer from the Scientific Library—the <span class="hlt">annual</span> Student Science Jeopardy Tournament and the Summer Video Series. This year, the 10th <span class="hlt">Annual</span> Student Science Jeopardy Tournament will be held on Wednesday, July 20, beginning at 10 a.m. in the auditorium of Building 549. The <span class="hlt">event</span> will also be streamed live to the Advanced Technology Research Facility (ATRF), room E1203.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-05-09/pdf/2012-11140.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-05-09/pdf/2012-11140.pdf"><span>77 FR 27159 - Safety <span class="hlt">Zone</span>, Temporary Change for Recurring Fifth Coast Guard District Fireworks Displays...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-05-09</p> <p>... fireworks. On July 3, 2012, the Tred Avon Yacht Club will sponsor their <span class="hlt">annual</span> fireworks <span class="hlt">event</span>. This <span class="hlt">event</span>... and regulated area for the Tred Avon Yacht Club fireworks <span class="hlt">event</span> held in Oxford, MD. This regulation... <span class="hlt">event</span>. The Tred Avon Yacht Club, which is the sponsor for this <span class="hlt">event</span>, holds this <span class="hlt">event</span> <span class="hlt">annually</span>. Except...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/32465','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/32465"><span>In-vehicle work <span class="hlt">zone</span> messages : final report.</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2017-06-01</p> <p>Work <span class="hlt">zones</span> present an increased risk to drivers and the work crew. To mitigate these risks, this study investigated the : potential effects of in-vehicle messages to communicate work <span class="hlt">zone</span> <span class="hlt">events</span> to the driver. The researchers conducted : literature r...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.T51E0531T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.T51E0531T"><span>Hunting for shallow slow-slip <span class="hlt">events</span> at Cascadia</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Tan, Y. J.; Bletery, Q.; Fan, W.; Janiszewski, H. A.; Lynch, E.; McCormack, K. A.; Phillips, N. J.; Rousset, B.; Seyler, C.; French, M. E.; Gaherty, J. B.; Regalla, C.</p> <p>2017-12-01</p> <p>The discovery of slow earthquakes at subduction <span class="hlt">zones</span> is one of the major breakthroughs of Earth science in the last two decades. Slow earthquakes involve a wide spectrum of fault slip behaviors and seismic radiation patterns, such as tremor, low-frequency earthquakes, and slow-slip <span class="hlt">events</span>. The last of these are particularly interesting due to their large moment releases accompanied by minimal ground shaking. Slow-slip <span class="hlt">events</span> have been reported at various subduction <span class="hlt">zones</span> ; most of these slow-slip <span class="hlt">events</span> are located down-dip of the megathrust seismogenic <span class="hlt">zone</span>, while a few up-dip cases have recently been observed at Nankai and New Zealand. Up-dip slow-slip <span class="hlt">events</span> illuminate the structure of faulting environments and rupture mechanisms of tsunami earthquakes. Their possible presence and location at a particular subduction <span class="hlt">zone</span> can help assess earthquake and tsunami hazard for that region. However, their typical location distant from the coast requires the development of techniques using offshore instrumentation. Here, we investigate the absolute pressure gauges (APG) of the Cascadia Initiative, a four year amphibious seismic experiment, to search for possible shallow up-dip slow-slip <span class="hlt">events</span> in the Cascadia subduction <span class="hlt">zone</span>. These instruments are collocated with ocean bottom seismometers (OBS) and located close to buoys and onshore GPS stations, offering the opportunity to investigate the utility of multiple datasets. Ultimately, we aim to develop a protocol to analyze APG data for offshore shallow slow-slip <span class="hlt">event</span> detections and quantify uncertainties, with direct applications to understanding the up-dip subduction interface system in Cascadia.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.S41C0812T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.S41C0812T"><span>Systematic detection of long-term slow slip <span class="hlt">events</span> along Hyuga-nada to central Shikoku, Nankai subduction <span class="hlt">zone</span>, using GNSS data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Takagi, R.; Obara, K.; Uchida, N.</p> <p>2017-12-01</p> <p>Understanding slow earthquake activity improves our knowledge of slip behavior in brittle-ductile transition <span class="hlt">zone</span> and subduction process including megathrust earthquakes. In order to understand overall picture of slow slip activity, it is important to make a comprehensive catalog of slow slip <span class="hlt">events</span> (SSEs). Although short-term SSEs have been detected by GNSS and tilt meter records systematically, analysis of long-term slow slip <span class="hlt">events</span> relies on individual slip inversions. We develop an algorism to systematically detect long-term SSEs and estimate source parameters of the SSEs using GNSS data. The algorism is similar to GRiD-MT (Tsuruoka et al., 2009), which is grid-based automatic determination of moment tensor solution. Instead of moment tensor fitting to long period seismic records, we estimate parameters of a single rectangle fault to fit GNSS displacement time series. First, we make a two dimensional grid covering possible location of SSE. Second, we estimate best-fit parameters (length, width, slip, and rake) of the rectangle fault at each grid point by an iterative damped least square method. Depth, strike, and dip are fixed on the plate boundary. Ramp function with duration of 300 days is used for expressing time evolution of the fault slip. Third, a grid maximizing variance reduction is selected as a candidate of long-term SSE. We also search onset of ramp function based on the grid search. We applied the method to GNSS data in southwest Japan to detect long-term SSEs in Nankai subduction <span class="hlt">zone</span>. With current selection criteria, we found 13 <span class="hlt">events</span> with Mw6.2-6.9 in Hyuga-nada, Bungo channel, and central Shikoku from 1998 to 2015, which include unreported <span class="hlt">events</span>. Key finding is along strike migrations of long-term SSEs from Hyuga-nada to Bungo channel and from Bungo channel to central Shikoku. In particular, three successive <span class="hlt">events</span> migrating northward in Hyuga-nada preceded the 2003 Bungo channel SSE, and one <span class="hlt">event</span> in central Shikoku followed the 2003 SSE in</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_8");'>8</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li class="active"><span>10</span></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_10 --> <div id="page_11" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li class="active"><span>11</span></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="201"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol1/pdf/CFR-2012-title33-vol1-sec100-1104.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol1/pdf/CFR-2012-title33-vol1-sec100-1104.pdf"><span>33 CFR 100.1104 - Southern California <span class="hlt">annual</span> marine <span class="hlt">events</span> for the Los Angeles Long Beach Captain of the Port <span class="hlt">Zone</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... to Ensenada Yacht Race Sponsor Newport Ocean Sailing Association. <span class="hlt">Event</span> Description Sailing vessel race; open ocean. Date Fourth Friday in April. Location Newport Beach, CA. Regulated Area Starting area only. All waters of the Pacific Ocean near Newport Beach, CA bounded by a line starting 33°35′18″ N...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.S42B..08P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.S42B..08P"><span>Potential Seismic Signatures of Megathrust Preparatory <span class="hlt">Zones</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Parameswaran, R. M.; Maheswari, K.; Rajendran, K.</p> <p>2017-12-01</p> <p>The Mw 9.2, 2004 Sumatra earthquake awakened the otherwise inactive Andaman-Sumatra subduction <span class="hlt">zone</span> (ASSZ), pushing it into an era of amplified seismicity. The subduction <span class="hlt">zone</span> has since witnessed an array of inter- and intra-plate <span class="hlt">events</span> along and around its trench. Several intra-plate <span class="hlt">events</span> like the 2012 Wharton Basin earthquakes (Mw 8.6 and 8.2), are believed to be the triggered response of the plateward transmission of stresses due to the 2004 earthquake (Ishii et al., 2013). On the other hand, the Mw 7.5, 2009 33-km-deep intra-plate normal-faulting <span class="hlt">event</span> in the northern Andaman segment is an example of outer-rise seismicity resulting from the post-seismic relaxation of the subducting slab (Andrade and Rajendran, 2011). These are aftermaths of a drastic change in the stress regime from compressional to extensional, following the 2004 megathrust <span class="hlt">event</span>. But, pre-megathrust, aside from the inter-plate thrust mechanisms that are widely observed along the trench, how does the plate-motion-driven compression manifest in the regional seismicity? What happens to the stresses accumulating within the bending subducting slab; does it source deeper compressional <span class="hlt">events</span> prior to a megathrust? The 2009 normal outer-rise earthquake was preceded by the 13 September 2002, Mw 6.5 Diglipur outer-rise thrust earthquake (22 km depth), both occurring at the northern terminus of the 2004-rupture, in the compressing forearc that experienced surface uplift pre-megathrust (Rajendran et al., 2003; Rajendran et al., 2007). This work, therefore, examines the slip models of such pre-<span class="hlt">event</span> outer-rise thrust earthquakes along the stretch of the 2004 rupture <span class="hlt">zone</span> in the ASSZ. The work is also being extended to understand the preparatory <span class="hlt">zones</span> of other global megathrust earthquakes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/23024783','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/23024783"><span>Population, behavioural and physiological responses of an urban population of black swans to an intense <span class="hlt">annual</span> noise <span class="hlt">event</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Payne, Catherine J; Jessop, Tim S; Guay, Patrick-Jean; Johnstone, Michele; Feore, Megan; Mulder, Raoul A</p> <p>2012-01-01</p> <p>Wild animals in urban environments are exposed to a broad range of human activities that have the potential to disturb their life history and behaviour. Wildlife responses to disturbance can range from emigration to modified behaviour, or elevated stress, but these responses are rarely evaluated in concert. We simultaneously examined population, behavioural and hormonal responses of an urban population of black swans Cygnus atratus before, during and after an <span class="hlt">annual</span> disturbance <span class="hlt">event</span> involving large crowds and intense noise, the Australian Formula One Grand Prix. Black swan population numbers were lowest one week before the <span class="hlt">event</span> and rose gradually over the course of the study, peaking after the <span class="hlt">event</span>, suggesting that the disturbance does not trigger mass emigration. We also found no difference in the proportion of time spent on key behaviours such as locomotion, foraging, resting or self-maintenance over the course of the study. However, basal and capture stress-induced corticosterone levels showed significant variation, consistent with a modest physiological response. Basal plasma corticosterone levels were highest before the <span class="hlt">event</span> and decreased over the course of the study. Capture-induced stress levels peaked during the Grand Prix and then also declined over the remainder of the study. Our results suggest that even intensely noisy and apparently disruptive <span class="hlt">events</span> may have relatively low measurable short-term impact on population numbers, behaviour or physiology in urban populations with apparently high tolerance to anthropogenic disturbance. Nevertheless, the potential long-term impact of such disturbance on reproductive success, individual fitness and population health will need to be carefully evaluated.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3443219','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3443219"><span>Population, Behavioural and Physiological Responses of an Urban Population of Black Swans to an Intense <span class="hlt">Annual</span> Noise <span class="hlt">Event</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Payne, Catherine J.; Jessop, Tim S.; Guay, Patrick-Jean; Johnstone, Michele; Feore, Megan; Mulder, Raoul A.</p> <p>2012-01-01</p> <p>Wild animals in urban environments are exposed to a broad range of human activities that have the potential to disturb their life history and behaviour. Wildlife responses to disturbance can range from emigration to modified behaviour, or elevated stress, but these responses are rarely evaluated in concert. We simultaneously examined population, behavioural and hormonal responses of an urban population of black swans Cygnus atratus before, during and after an <span class="hlt">annual</span> disturbance <span class="hlt">event</span> involving large crowds and intense noise, the Australian Formula One Grand Prix. Black swan population numbers were lowest one week before the <span class="hlt">event</span> and rose gradually over the course of the study, peaking after the <span class="hlt">event</span>, suggesting that the disturbance does not trigger mass emigration. We also found no difference in the proportion of time spent on key behaviours such as locomotion, foraging, resting or self-maintenance over the course of the study. However, basal and capture stress-induced corticosterone levels showed significant variation, consistent with a modest physiological response. Basal plasma corticosterone levels were highest before the <span class="hlt">event</span> and decreased over the course of the study. Capture-induced stress levels peaked during the Grand Prix and then also declined over the remainder of the study. Our results suggest that even intensely noisy and apparently disruptive <span class="hlt">events</span> may have relatively low measurable short-term impact on population numbers, behaviour or physiology in urban populations with apparently high tolerance to anthropogenic disturbance. Nevertheless, the potential long-term impact of such disturbance on reproductive success, individual fitness and population health will need to be carefully evaluated. PMID:23024783</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.nrel.gov/workingwithus/entrepreneurship-events.html','SCIGOVWS'); return false;" href="https://www.nrel.gov/workingwithus/entrepreneurship-events.html"><span>Innovation and Entrepreneurship <span class="hlt">Events</span> | NREL</span></a></p> <p><a target="_blank" href="http://www.science.gov/aboutsearch.html">Science.gov Websites</a></p> <p></p> <p></p> <p>Innovation and Entrepreneurship <span class="hlt">Events</span> Innovation and Entrepreneurship <span class="hlt">Events</span> Industry <em>Growth</em> Forum NREL's <span class="hlt">annual</span> Industry <em>Growth</em> Forum (IGF) provides clean energy innovators an opportunity to maximize communities. Learn more and register for the 2018 Industry <em>Growth</em> Forum. Text Version</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol1/pdf/CFR-2012-title33-vol1-sec100-801.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol1/pdf/CFR-2012-title33-vol1-sec100-801.pdf"><span>33 CFR 100.801 - <span class="hlt">Annual</span> Marine <span class="hlt">Events</span> in the Eighth Coast Guard District.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... so directed by that officer and will be operated at a no wake speed in a manner which will not... Drag Boat Association/Pisgah Bay Boat Races Grand Rivers KY No wake <span class="hlt">zone</span> in Pisgah Bay, mile marker 30... No wake <span class="hlt">zone</span> in Pisgah Bay, mile marker 30 Tennessee River. <span class="hlt">Zone</span> is in a bay roughly 1/2 mile from...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol1/pdf/CFR-2013-title33-vol1-sec100-801.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol1/pdf/CFR-2013-title33-vol1-sec100-801.pdf"><span>33 CFR 100.801 - <span class="hlt">Annual</span> Marine <span class="hlt">Events</span> in the Eighth Coast Guard District.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-07-01</p> <p>... so directed by that officer and will be operated at a no wake speed in a manner which will not... Drag Boat Association/Pisgah Bay Boat Races Grand Rivers KY No wake <span class="hlt">zone</span> in Pisgah Bay, mile marker 30... No wake <span class="hlt">zone</span> in Pisgah Bay, mile marker 30 Tennessee River. <span class="hlt">Zone</span> is in a bay roughly 1/2 mile from...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ThApC.131.1397W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ThApC.131.1397W"><span>A first approach to calculate BIOCLIM variables and climate <span class="hlt">zones</span> for Antarctica</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wagner, Monika; Trutschnig, Wolfgang; Bathke, Arne C.; Ruprecht, Ulrike</p> <p>2018-02-01</p> <p>For testing the hypothesis that macroclimatological factors determine the occurrence, biodiversity, and species specificity of both symbiotic partners of Antarctic lecideoid lichens, we present a first approach for the computation of the full set of 19 BIOCLIM variables, as available at http://www.worldclim.org/ for all regions of the world with exception of Antarctica. <span class="hlt">Annual</span> mean temperature (Bio 1) and <span class="hlt">annual</span> precipitation (Bio 12) were chosen to define climate <span class="hlt">zones</span> of the Antarctic continent and adjacent islands as required for ecological niche modeling (ENM). The <span class="hlt">zones</span> are based on data for the years 2009-2015 which was obtained from the Antarctic Mesoscale Prediction System (AMPS) database of the Ohio State University. For both temperature and precipitation, two separate <span class="hlt">zonings</span> were specified; temperature values were divided into 12 <span class="hlt">zones</span> (named 1 to 12) and precipitation values into five (named A to E). By combining these two partitions, we defined climate <span class="hlt">zonings</span> where each geographical point can be uniquely assigned to exactly one <span class="hlt">zone</span>, which allows an immediate explicit interpretation. The soundness of the newly calculated climate <span class="hlt">zones</span> was tested by comparison with already published data, which used only three <span class="hlt">zones</span> defined on climate information from the literature. The newly defined climate <span class="hlt">zones</span> result in a more precise assignment of species distribution to the single habitats. This study provides the basis for a more detailed continental-wide ENM using a comprehensive dataset of lichen specimens which are located within 21 different climate regions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title14-vol4/pdf/CFR-2011-title14-vol4-sec417-411.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title14-vol4/pdf/CFR-2011-title14-vol4-sec417-411.pdf"><span>14 CFR 417.411 - Safety clear <span class="hlt">zones</span> for hazardous operations.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-01-01</p> <p>... <span class="hlt">zone</span> on the following criteria: (i) For a possible explosive <span class="hlt">event</span>, base a safety clear <span class="hlt">zone</span> on the... 14 Aeronautics and Space 4 2011-01-01 2011-01-01 false Safety clear <span class="hlt">zones</span> for hazardous operations... ADMINISTRATION, DEPARTMENT OF TRANSPORTATION LICENSING LAUNCH SAFETY Ground Safety § 417.411 Safety clear <span class="hlt">zones</span>...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-05-21/pdf/2013-12032.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-05-21/pdf/2013-12032.pdf"><span>78 FR 29651 - Safety <span class="hlt">Zone</span>; Fireworks <span class="hlt">Events</span> in Captain of the Port New York <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-05-21</p> <p>... <span class="hlt">Zone</span>, 33 located in approximate CFR 165.160(4.2). position 40[deg]42'57.5'' N, 074[deg]01'34'' W (NAD....160(3.8). position 40[deg]46'11.8'' N, 074[deg]00'14.8'' W (NAD 1983), approximately 375 yards west of...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.S43B2849A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.S43B2849A"><span>Constraints on Fault Damage <span class="hlt">Zone</span> Properties and Normal Modes from a Dense Linear Array Deployment along the San Jacinto Fault <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Allam, A. A.; Lin, F. C.; Share, P. E.; Ben-Zion, Y.; Vernon, F.; Schuster, G. T.; Karplus, M. S.</p> <p>2016-12-01</p> <p>We present earthquake data and statistical analyses from a month-long deployment of a linear array of 134 Fairfield three-component 5 Hz seismometers along the Clark strand of the San Jacinto fault <span class="hlt">zone</span> in Southern California. With a total aperture of 2.4km and mean station spacing of 20m, the array locally spans the entire fault <span class="hlt">zone</span> from the most intensely fractured core to relatively undamaged host rock on the outer edges. We recorded 36 days of continuous seismic data at 1000Hz sampling rate, capturing waveforms from 751 local <span class="hlt">events</span> with Mw>0.5 and 43 teleseismic <span class="hlt">events</span> with M>5.5, including two 600km deep M7.5 <span class="hlt">events</span> along the Andean subduction <span class="hlt">zone</span>. For any single local <span class="hlt">event</span> on the San Jacinto fault, the central stations of the array recorded both higher amplitude and longer duration waveforms, which we interpret as the result of damage-related low-velocity structure acting as a broad waveguide. Using 271 San Jacinto <span class="hlt">events</span>, we compute the distributions of three quantities for each station: maximum amplitude, mean amplitude, and total energy (the integral of the envelope). All three values become statistically lower with increasing distance from the fault, but in addition show a nonrandom zigzag pattern which we interpret as normal mode oscillations. This interpretation is supported by polarization analysis which demonstrates that the high-amplitude late-arriving energy is strongly vertically polarized in the central part of the array, consistent with Love-type trapped waves. These results, comprising nearly 30,000 separate coseismic waveforms, support the consistent interpretation of a 450m wide asymmetric damage <span class="hlt">zone</span>, with the lowest velocities offset to the northeast of the mapped surface trace by 100m. This asymmetric damage <span class="hlt">zone</span> has important implications for the earthquake dynamics of the San Jacinto and especially its ability to generate damaging multi-segment ruptures.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.S33A2813K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.S33A2813K"><span>Tidal modulation of slow slip <span class="hlt">events</span> in the Nankai trough subduction <span class="hlt">zone</span> detected by borehole strainmeters</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kikuchi, J.; Ide, S.; Matsumoto, N.</p> <p>2016-12-01</p> <p>Slow slip <span class="hlt">events</span> (SSEs) often occur in the Nankai subduction <span class="hlt">zone</span>, Japan, within a band-like <span class="hlt">zone</span> extended from the center of Honshu to western Shikoku. SSEs are believed as shear slip on the plate interface, where the frictional property changes from velocity weakening to strengthening in the dip direction. Therefore the dynamics of SSEs may give some hints on the depth dependent friction and plate subduction. The tidal modulation of SSEs has been identified by statistical analysis using strain data of Plate Boundary Observatory, in the Cascadia subduction <span class="hlt">zone</span> [Hawthorne & Rubin, 2010]. Here, we perform similar statistical analyses using strain data recorded at borehole stations maintained by National Institute of Advanced Industrial Science and Technology, in western Japan. The correlation between the oscillation in SSEs and tidal stress was confirmed statistically. In Nankai subduction <span class="hlt">zone</span>, it is known that SSEs are accompanied with high activity of deep tectonic tremors [Hirose & Obara, 2006]. These tremors have been known to be sensitive to tidal stress [Nakata et al., 2008]. Therefore, the tidal modulation of SSEs is another representation of tidal modulation of tremors. To clarify the relation between SSEs and tremors, we investigate whether strain changes corresponding to SSEs can be explained only by tremors activity. For an SSE occurred in Aug. 2010 in Bungo channel, we assume that the seismic moment of the SSE is 1.6 × 1018 Nm (Mw 6.1) based on the inversion of GNSS data [Nishimura et al., 2013], and that this moment is released by 715 tremors that occur during this SSE [Idehara et al., 2014]. In this case, each tremor is assigned with seismic moment of 2.2 × 1015 Nm (Mw 4.2). Then the strain change at the observation station by these tremors is calculated using the Okada [1992] method, assuming a half space and focal mechanism consistent with the regional plate motion. The calculated strain is qualitatively similar with the observed strain</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26096382','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26096382"><span>Temporal Hyporheic <span class="hlt">Zone</span> Response to Water Table Fluctuations.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Malzone, Jonathan M; Anseeuw, Sierra K; Lowry, Christopher S; Allen-King, Richelle</p> <p>2016-03-01</p> <p>Expansion and contraction of the hyporheic <span class="hlt">zone</span> due to temporal hydrologic changes between stream and riparian aquifer influence the biogeochemical cycling capacity of streams. Theoretical studies have quantified the control of groundwater discharge on the depth of the hyporheic <span class="hlt">zone</span>; however, observations of temporal groundwater controls are limited. In this study, we develop the concept of groundwater-dominated differential hyporheic <span class="hlt">zone</span> expansion to explain the temporal control of groundwater discharge on the hyporheic <span class="hlt">zone</span> in a third-order stream reach flowing through glacially derived terrain typical of the Great Lakes region. We define groundwater-dominated differential expansion of the hyporheic <span class="hlt">zone</span> as: differing rates and magnitudes of hyporheic <span class="hlt">zone</span> expansion in response to seasonal vs. storm-related water table fluctuation. Specific conductance and vertical hydraulic gradient measurements were used to map changes in the hyporheic <span class="hlt">zone</span> during seasonal water table decline and storm <span class="hlt">events</span>. Planar and riffle beds were monitored in order to distinguish the cause of increasing hyporheic <span class="hlt">zone</span> depth. Planar bed seasonal expansion of the hyporheic <span class="hlt">zone</span> was of a greater magnitude and longer in duration (weeks to months) than storm <span class="hlt">event</span> expansion (hours to days). In contrast, the hyporheic <span class="hlt">zone</span> beneath the riffle bed exhibited minimal expansion in response to seasonal groundwater decline compared to storm related expansion. Results indicated that fluctuation in the riparian water table controlled seasonal expansion of the hyporheic <span class="hlt">zone</span> along the planar bed. This groundwater induced hyporheic <span class="hlt">zone</span> expansion could increase the potential for biogeochemical cycling and natural attenuation. © 2015, National Ground Water Association.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70026792','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70026792"><span>Importance of storm <span class="hlt">events</span> in controlling ecosystem structure and function in a Florida Gulf Coast estuary</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Davis, S. E.; Cable, J.E.; Childers, D.L.; Coronado-Molina, C.; Day, J.W.; Hittle, C.D.; Madden, C.J.; Reyes, E.; Rudnick, D.; Sklar, F.</p> <p>2004-01-01</p> <p>From 8/95 to 2/01, we investigated the ecological effects of intra- and inter-<span class="hlt">annual</span> variability in freshwater flow through Taylor Creek in southeastern Everglades National Park. Continuous monitoring and intensive sampling studies overlapped with an array of pulsed weather <span class="hlt">events</span> that impacted physical, chemical, and biological attributes of this region. We quantified the effects of three <span class="hlt">events</span> representing a range of characteristics (duration, amount of precipitation, storm intensity, wind direction) on the hydraulic connectivity, nutrient and sediment dynamics, and vegetation structure of the SE Everglades estuarine ecotone. These <span class="hlt">events</span> included a strong winter storm in November 1996, Tropical Storm Harvey in September 1999, and Hurricane Irene in October 1999. Continuous hydrologic and daily water sample data were used to examine the effects of these <span class="hlt">events</span> on the physical forcing and quality of water in Taylor Creek. A high resolution, flow-through sampling and mapping approach was used to characterize water quality in the adjacent bay. To understand the effects of these <span class="hlt">events</span> on vegetation communities, we measured mangrove litter production and estimated seagrass cover in the bay at monthly intervals. We also quantified sediment deposition associated with Hurricane Irene's flood surge along the Buttonwood Ridge. These three <span class="hlt">events</span> resulted in dramatic changes in surface water movement and chemistry in Taylor Creek and adjacent regions of Florida Bay as well as increased mangrove litterfall and flood surge scouring of seagrass beds. Up to 5 cm of bay-derived mud was deposited along the ridge adjacent to the creek in this single pulsed <span class="hlt">event</span>. These short-term <span class="hlt">events</span> can account for a substantial proportion of the <span class="hlt">annual</span> flux of freshwater and materials between the mangrove <span class="hlt">zone</span> and Florida Bay. Our findings shed light on the capacity of these storm <span class="hlt">events</span>, especially when in succession, to have far reaching and long lasting effects on coastal ecosystems such</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2008JAfES..50..111M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2008JAfES..50..111M"><span>CL-imaging and ion microprobe dating of single zircons from a high-grade rock from the Central <span class="hlt">Zone</span>, Limpopo Belt, South Africa: Evidence for a single metamorphic <span class="hlt">event</span> at ˜2.0 Ga</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mouri, H.; Brandl, G.; Whitehouse, M.; de Waal, S.; Guiraud, M.</p> <p>2008-02-01</p> <p>The combination of ion microprobe dating and cathodoluminescence (CL) imaging of zircons from a high-grade rock from the Central <span class="hlt">Zone</span> of the Limpopo Belt were used to constrain the age of metamorphic <span class="hlt">events</span> in the area. Zircon grains extracted from an orthopyroxene-gedrite-bearing granulite were prepared for single crystal CL-imaging and ion microprobe dating. The grains display complex <span class="hlt">zoning</span> when using SEM-based CL-imaging. A common feature in most grains is the presence of a distinct core with a broken oscillatory <span class="hlt">zoned</span> structure, which clearly appears to be the remnant of an original grain of igneous origin. This core is overgrown by an unzoned thin rim measuring about 10-30 μm in diameter, which is considered as new zircon growth during a single metamorphic <span class="hlt">event</span>. Selected domains of the zircon grains were analysed for U, Pb and Th isotopic composition using a CAMECA IMS 1270 ion microprobe (Nordsim facility). Most of the grains define a near-concordant cluster with some evidence of Pb loss. The most concordant ages of the cores yielded a weighted mean 207Pb/ 206Pb age of 2689 ± 15 (2 σ) Ma, interpreted as the age of the protolith of an igneous origin. The unzoned overgrowths of the zircon grains yielded a considerably younger weighted mean 207Pb/ 206Pb age of ˜2006.5 ± 8.0 Ma (2 σ), and these data are interpreted to reflect closely the age of the ubiquitous high-grade metamorphic <span class="hlt">event</span> in the Central <span class="hlt">Zone</span>. This study shows clearly, based on both the internal structure of the zircons and the data obtained by ion microprobe dating, that only a single metamorphic <span class="hlt">event</span> is recorded by the studied 2.69 Ga old rocks, and we found no evidence of an earlier metamorphic <span class="hlt">event</span> at ˜2.5 Ga as postulated earlier by some workers.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017ACP....17.4627P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017ACP....17.4627P"><span><span class="hlt">Annual</span> variation in <span class="hlt">event</span>-scale precipitation δ2H at Barrow, AK, reflects vapor source region</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Putman, Annie L.; Feng, Xiahong; Sonder, Leslie J.; Posmentier, Eric S.</p> <p>2017-04-01</p> <p>In this study, precipitation isotopic variations at Barrow, AK, USA, are linked to conditions at the moisture source region, along the transport path, and at the precipitation site. Seventy precipitation <span class="hlt">events</span> between January 2009 and March 2013 were analyzed for δ2H and deuterium excess. For each precipitation <span class="hlt">event</span>, vapor source regions were identified with the hybrid single-particle Lagrangian integrated trajectory (HYSPLIT) air parcel tracking program in back-cast mode. The results show that the vapor source region migrated <span class="hlt">annually</span>, with the most distal (proximal) and southerly (northerly) vapor source regions occurring during the winter (summer). This may be related to equatorial expansion and poleward contraction of the polar circulation cell and the extent of Arctic sea ice cover. <span class="hlt">Annual</span> cycles of vapor source region latitude and δ2H in precipitation were in phase; depleted (enriched) δ2H values were associated with winter (summer) and distal (proximal) vapor source regions. Precipitation δ2H responded to variation in vapor source region as reflected by significant correlations between δ2H with the following three parameters: (1) total cooling between lifted condensation level (LCL) and precipitating cloud at Barrow, Δ<span style="text-decoration: overline;">Tcool, (2) meteorological conditions at the evaporation site quantified by 2 m dew point, <span style="text-decoration: overline;">Td, and (3) whether the vapor transport path crossed the Brooks and/or Alaskan ranges, expressed as a Boolean variable, mtn. These three variables explained 54 % of the variance (p<0. 001) in precipitation δ2H with a sensitivity of -3.51 ± 0.55 ‰ °C-1 (p<0. 001) to Δ<span style="text-decoration: overline;">Tcool, 3.23 ± 0.83 ‰ °C-1 (p<0. 001) to Td, and -32.11 ± 11.04 ‰ (p = 0. 0049) depletion when mtn is true. The magnitude of each effect on isotopic composition also varied with vapor source region proximity. For storms with proximal vapor source regions</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-03-11/pdf/2013-05546.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-03-11/pdf/2013-05546.pdf"><span>78 FR 15293 - Safety <span class="hlt">Zone</span>; St. Patrick's Day Fireworks; Manitowoc River, Manitowoc, WI</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-03-11</p> <p>...-AA00 Safety <span class="hlt">Zone</span>; St. Patrick's Day Fireworks; Manitowoc River, Manitowoc, WI AGENCY: Coast Guard, DHS... will hold its <span class="hlt">annual</span> St. Patrick's Day fireworks display. This fireworks display will be launched from... as follows: Sec. 165.T09-0116 Safety <span class="hlt">Zone</span>; St. Patrick's Day Fireworks; Manitowoc River, Manitowoc...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.S42A..04H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.S42A..04H"><span>Very low frequency earthquakes (VLFEs) detected during episodic tremor and slip (ETS) <span class="hlt">events</span> in Cascadia using a match filter method indicate repeating <span class="hlt">events</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hutchison, A. A.; Ghosh, A.</p> <p>2016-12-01</p> <p>Very low frequency earthquakes (VLFEs) occur in transitional <span class="hlt">zones</span> of faults, releasing seismic energy in the 0.02-0.05 Hz frequency band over a 90 s duration and typically have magntitudes within the range of Mw 3.0-4.0. VLFEs can occur down-dip of the seismogenic <span class="hlt">zone</span>, where they can transfer stress up-dip potentially bringing the locked <span class="hlt">zone</span> closer to a critical failure stress. VLFEs also occur up-dip of the seismogenic <span class="hlt">zone</span> in a region along the plate interface that can rupture coseismically during large megathrust <span class="hlt">events</span>, such as the 2011 Tohoku-Oki earthquake [Ide et al., 2011]. VLFEs were first detected in Cascadia during the 2011 episodic tremor and slip (ETS) <span class="hlt">event</span>, occurring coincidentally with tremor [Ghosh et al., 2015]. However, during the 2014 ETS <span class="hlt">event</span>, VLFEs were spatially and temporally asynchronous with tremor activity [Hutchison and Ghosh, 2016]. Such contrasting behaviors remind us that the mechanics behind such <span class="hlt">events</span> remain elusive, yet they are responsible for the largest portion of the moment release during an ETS <span class="hlt">event</span>. Here, we apply a match filter method using known VLFEs as template <span class="hlt">events</span> to detect additional VLFEs. Using a grid-search centroid moment tensor inversion method, we invert stacks of the resulting match filter detections to ensure moment tensor solutions are similar to that of the respective template <span class="hlt">events</span>. Our ability to successfully employ a match filter method to VLFE detection in Cascadia intrinsically indicates that these <span class="hlt">events</span> can be repeating, implying that the same asperities are likely responsible for generating multiple VLFEs.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.C53B1037M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.C53B1037M"><span>Continuous Estimates of Surface Density and <span class="hlt">Annual</span> Snow Accumulation with Multi-Channel Snow/Firn Penetrating Radar in the Percolation <span class="hlt">Zone</span>, Western Greenland Ice Sheet</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Meehan, T.; Marshall, H. P.; Bradford, J.; Hawley, R. L.; Osterberg, E. C.; McCarthy, F.; Lewis, G.; Graeter, K.</p> <p>2017-12-01</p> <p>A priority of ice sheet surface mass balance (SMB) prediction is ascertaining the surface density and <span class="hlt">annual</span> snow accumulation. These forcing data can be supplied into firn compaction models and used to tune Regional Climate Models (RCM). RCMs do not accurately capture subtle changes in the snow accumulation gradient. Additionally, leading RCMs disagree among each other and with accumulation studies in regions of the Greenland Ice Sheet (GrIS) over large distances and temporal scales. RCMs tend to yield inconsistencies over GrIS because of sparse and outdated validation data in the reanalysis pool. Greenland Traverse for Accumulation and Climate Studies (GreenTrACS) implemented multi-channel 500 MHz Radar in multi-offset configuration throughout two traverse campaigns totaling greater than 3500 km along the western percolation <span class="hlt">zone</span> of GrIS. The multi-channel radar has the capability of continuously estimating snow depth, average density, and <span class="hlt">annual</span> snow accumulation, expressed at 95% confidence (+-) 0.15 m, (+-) 17 kgm-3, (+-) 0.04 m w.e. respectively, by examination of the primary reflection return from the previous year's summer surface.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/50938','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/50938"><span>Watershed and longitudinal monitoring <span class="hlt">events</span></span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Harold Harbert; Steven Blackburn</p> <p>2016-01-01</p> <p>Georgia Adopt-A-Stream partners <span class="hlt">annually</span> with many organizations, universities and watershed groups to conduct sampling <span class="hlt">events</span> with volunteers at a watershed level. These monitoring <span class="hlt">events</span> range from one-day snapshots to week-long paddle trips. One-day sampling <span class="hlt">events</span>, also called “Blitzs,” River Adventures and River Rendezvous, generally target 20-50 sites within a...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_9");'>9</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li class="active"><span>11</span></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_11 --> <div id="page_12" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li class="active"><span>12</span></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="221"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015rasc.conf..443M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015rasc.conf..443M"><span>Armenian Astronomical Society <span class="hlt">Annual</span> Activities in 2014</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mickaelian, A. M.</p> <p>2015-07-01</p> <p>A report is given on the achievements of the Armenian astronomy during the last year and on the present activities of the Armenian Astronomical Society (ArAS). ArAS membership, ArAS electronic newsletters (ArASNews), ArAS webpage, <span class="hlt">annual</span> meetings, <span class="hlt">Annual</span> Prize for Young Astronomers (Yervant Terzian Prize) and other awards, international relations, presence in international organizations, summer schools, astronomical Olympiads and other <span class="hlt">events</span>, matters related to astronomical education, astronomical heritage, astronomy outreach and ArAS further projects are discussed. The present meeting, BAO Science Camp, ArAS School lectures are among 2014 <span class="hlt">events</span> as well.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-05-07/pdf/2013-10774.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-05-07/pdf/2013-10774.pdf"><span>78 FR 26508 - Safety <span class="hlt">Zone</span>; Fireworks <span class="hlt">Event</span> in Captain of the Port New York <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-05-07</p> <p>...(4.2). position 40[deg]44'24'' N, 073[deg]58'00'' W (NAD 1983), approximately 785 yards south of...'' W (NAD 1983), approximately 500 yards northeast of Glen Cove Breakwater Light 5 (LLNR 27065). This... approximate <span class="hlt">Zone</span>, 33 CFR 165.160(3.8). position 41[deg]30'01.2'' N, 073[deg]59'42.5'' W (NAD 1983...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/782768','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/782768"><span>Oak Ridge Reservation Public Warning Siren System <span class="hlt">Annual</span> Test Report</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>R. F. Gee</p> <p>2000-10-01</p> <p>The full operational test of the Oak Ridge Reservation (ORR) Public Warning Siren System (PWSS) was successfully conducted on September 27, 2000. The <span class="hlt">annual</span> test is a full-scale sounding of the individual siren systems around each of the three Department of Energy (DOE) sites in Oak Ridge, Tennessee. The purpose of the <span class="hlt">annual</span> test is to demonstrate and validate the siren systems' ability to alert personnel outdoors in the Immediate Notification <span class="hlt">Zones</span> (INZ) (approximately two miles) around each site. The success of this test is based on two critical functions of the siren system. The first function is system operability.more » The system is considered operable if 90% of the sirens are operational. System diagnostics and direct field observations were used to validate the operability of the siren systems. Based on the diagnostic results and field observations, greater than 90% of the sirens were considered operational. The second function is system audibility. The system is considered audible if the siren could be heard in the immediate notification <span class="hlt">zones</span> around each of the three sites. Direct field observations, along with sound level measurements, were used to validate the audibility of the siren system. Based on the direct field observations and sound level measurements, the siren system was considered audible. The combination of field observations, system diagnostic status reports, and sound level measurements provided a high level of confidence that the system met and would meet operational requirements upon demand. As part of the overall system test, the Tennessee Emergency Management Agency (TEMA) activated the Emergency Alerting System (EAS), which utilized area radio stations to make announcements regarding the test and to remind residents of what to do in the <span class="hlt">event</span> of an actual emergency.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-07-15/pdf/2011-17798.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-07-15/pdf/2011-17798.pdf"><span>76 FR 41693 - Safety <span class="hlt">Zone</span>; <span class="hlt">Annual</span> <span class="hlt">Events</span> Requiring Safety <span class="hlt">Zones</span> in Milwaukee Harbor, Milwaukee, WI</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-07-15</p> <p>..., 2010 from 10 p.m. through 10:45 p.m. (2) German Festival fireworks display on July 29, 2011 from 9:45 p.m. through 10:30 p.m.; on July 30, 2011 from 10:15 p.m. through 11 p.m. (3) Irish Festival fireworks...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-06-12/pdf/2012-14217.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-06-12/pdf/2012-14217.pdf"><span>77 FR 34797 - Safety <span class="hlt">Zones</span>; Recurring <span class="hlt">Events</span> in Captain of the Port New York <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-06-12</p> <p>... Safety <span class="hlt">Zone</span>, 33 CFR 165.160(5.9). position 40[deg]45'56.9'' N, 074[deg]00'25.4'' W (NAD 1983..., 074[deg]04'29.6'' W (NAD 1983), approximately 800 yards southeast of the Midland Beach. Date: June 16...]30'52.1'' N, 074[deg]10'58.8'' W (NAD 1983), approximately 540 yards east of Wolfe's Pond Park...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-07-02/pdf/2013-15638.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-07-02/pdf/2013-15638.pdf"><span>78 FR 39594 - Safety <span class="hlt">Zone</span>; Seafair Blue Angels Air Show Performance, Seattle, WA</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-07-02</p> <p>... <span class="hlt">Zone</span>; Seafair Blue Angels Air Show Performance, Seattle, WA AGENCY: Coast Guard, DHS. ACTION: Notice of enforcement of regulation. SUMMARY: The Coast Guard will enforce the <span class="hlt">annual</span> Seafair Blue Angels Air Show.... This safety <span class="hlt">zone</span> is being enforced for the Patriots Jet Team, which will be flying in place of the Blue...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-06-14/pdf/2013-14116.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-06-14/pdf/2013-14116.pdf"><span>78 FR 35783 - Regattas and Marine Parades in the COTP Lake Michigan <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-06-14</p> <p>..., Harborfest Dragon Boat Race; South Haven, MI. The Harborfest Dragon Boat Race is an <span class="hlt">annual</span> <span class="hlt">event</span> involving an... 100.909; Chinatown Chamber of Commerce Dragon Boat Race; Chicago, IL. The Chinatown Chamber of Commerce Dragon Boat Race is an <span class="hlt">annual</span> <span class="hlt">event</span> involving an estimated 1000 participants maneuvering self...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=women+AND+working+AND+performance&pg=7&id=EJ470444','ERIC'); return false;" href="https://eric.ed.gov/?q=women+AND+working+AND+performance&pg=7&id=EJ470444"><span>Crossing Comfort <span class="hlt">Zones</span>.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Madison, D. Soyini</p> <p>1993-01-01</p> <p>Offers a narrative based on a real <span class="hlt">event</span>, in the form of a "docustory," describing that moment when teaching worked--when, in an instructional setting, communication was "perfect" or "excellent." Describes how three very different students, in a course on the cultures of women of color, moved beyond comfort <span class="hlt">zones</span> while working together on a class…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-07-14/pdf/2010-17168.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-07-14/pdf/2010-17168.pdf"><span>75 FR 40726 - Safety <span class="hlt">Zones</span>: <span class="hlt">Annual</span> <span class="hlt">Events</span> Requiring Safety <span class="hlt">Zones</span> in the Captain of the Port Buffalo <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-07-14</p> <p>... July 5, 2010 from 10 p.m. to 10:30 p.m. 12. Mentor Harbor Yacht Club Fireworks Celebration on Lake Erie, Mentor Harbor, OH in 33 CFR 165.939(a)(19) on July 3, 2010 from 10 p.m. to 10:30 p.m. 13. City of...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/54223','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/54223"><span><span class="hlt">Annual</span> rings in a native Hawaiian tree, Sophora chrysophylla, on Maunakea, Hawai‘i</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Kainana S. Francisco; Patrick J. Hart; Jinbao Li; Edward R. Cook; Patrick J. Baker</p> <p>2015-01-01</p> <p><span class="hlt">Annual</span> rings are not commonly produced in tropical trees because they grow in a relatively aseasonal environment. However, in the subalpine <span class="hlt">zones</span> of Hawai‘i's highest volcanoes, there is often strong seasonal variability in temperature and rainfall. Using classical dendrochronological methods, <span class="hlt">annual</span> growth rings were shown to occur in Sophora...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMEP53C1760J','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMEP53C1760J"><span>InSAR coherence study of unusual rain <span class="hlt">events</span> in the Atacama Desert</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Jordan, T. E.; Scott, C. P.; Lohman, R.</p> <p>2017-12-01</p> <p>The Atacama Desert (AD) occupies much of Chile at latitudes 18-27°S. The surficial materials vary, dependent on proximity to the ocean, slope, position within a surface water drainage system, mean <span class="hlt">annual</span> rainfall, human land disturbance, and the local history of climate changes. Three major divisions of soil composition include: near coastal <span class="hlt">zone</span> of silicate mineral soils, mostly devoid of plants; central hyperarid <span class="hlt">zone</span> dominated by gypsum, devoid of plants; eastern <span class="hlt">zone</span> of silicate-based soils, very sparse plants. The AD in March 2015 experienced the largest rain <span class="hlt">event</span> of modern history, and again in June 2017 almost as much rain fell within the study area (24.2-25.7°S, coast to Andes Mountains). Those natural experiments set the stage for InSAR remote sensing of surface changes in a 24,000 square kilometer area. We used interferometric coherence of radar to measure the similarity in the reflective ground properties at the time of two SAR acquisitions, and a time series of European Space Agency's Sentinel-1A data sets acquired between January 2015 and August 2017. Date pairs lacking an intervening rain <span class="hlt">event</span> reveal extensive regions of high coherence, and in those areas we focus on the temporal evolution of coherence across dates of, and following dates of, the major rains. Permanent change of the surface is most extensive in the eastern and western sectors, yet the degree of permanent change was small except in valley bottoms. In the sector with gypsum soil small degrees of permanent change occurred over 30% of the surface including in narrow (1-3 km) elongate (10-60 km) stripes that cross-cut topography, likely revealing rain bands. The spatial pattern of transient change in coherence differs. Over half the gypsum-dominated <span class="hlt">zone</span> displays a transient change signal, whose spatial pattern corresponds to geomorphological forms; older landforms display greater transient coherence changes. In the silicate-dominated eastern region the transient signals are smaller</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.A43G0386O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.A43G0386O"><span>Climatic <span class="hlt">Zones</span>, Soil Moisture Seasonality and Biomass Burning and Their Influence On Ozone Precursor Concentrations Over West Africa as Retrieved from Satellites</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Onojeghuo, A. R.; Balzter, H.; Monks, P. S.</p> <p>2015-12-01</p> <p>West Africa is a region with six different climatic <span class="hlt">zones</span> including a rich savannah affected by biomass burning <span class="hlt">annually</span>, the Niger delta oil producing region with major gas flaring sites and a long coastline. Research on atmospheric pollution using remotely sensed data over West Africa has mostly been conducted at regional scale or for individual countries, with little emphasis on the dynamics of climatic <span class="hlt">zones</span> and the diversity of land cover types. This study analyses <span class="hlt">annual</span> seasonal dynamics of emissions of two ozone precursors stratified by climatic <span class="hlt">zone</span>: nitrogen dioxide (NO2) from OMI and carbon monoxide (CO) from TES. The different sources of these pollutants and their seasonality are explicitly considered. Results indicate that the highest <span class="hlt">annual</span> wet season NO2 column concentrations were in the semi-arid <span class="hlt">zone</span> (1.33 x 1015 molecules cm-2) after prolonged periods of low soil moisture while the highest dry season were observed in the wet sub-humid <span class="hlt">zone</span> (2.62 x 1015 molecules cm-2) where the savannah fires occur <span class="hlt">annually</span>. The highest <span class="hlt">annual</span> CO concentrations (> 3.1 x 1018 molecules cm-2) were from the Niger Delta, located in the humid <span class="hlt">zone</span>. There were indications of atmospheric transport of CO from the southern hemisphere in the west season. Climate change induced soil moisture variability was most prominent in the dry sub-humid and semi-arid climatic <span class="hlt">zones</span> (±0.015m3m-3) . The causal effects of soil moisture variability on NO2 emissions and their seasonal cycles were tested using the Granger causality test. Causal effects of inter-zonal exchanges/transport of NO2 and CO emissions respectively were inferred using Directed Acyclic Graphs. The results indicate that NO2, CO and their seasonal ratios are strongly affected by changes in soil moisture.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec165-1191.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec165-1191.pdf"><span>33 CFR 165.1191 - Northern California and Lake Tahoe Area <span class="hlt">Annual</span> Fireworks <span class="hlt">Events</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... exact dates, times, and other details concerning the exact geographical description of the areas are... <span class="hlt">zone</span> during all applicable effective dates and times unless cleared to do so by or through an official... a safety <span class="hlt">zone</span> during all applicable effective dates and times shall come to an immediate stop. (3...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec165-1191.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec165-1191.pdf"><span>33 CFR 165.1191 - Northern California and Lake Tahoe Area <span class="hlt">Annual</span> Fireworks <span class="hlt">Events</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-07-01</p> <p>... exact dates, times, and other details concerning the exact geographical description of the areas are... <span class="hlt">zone</span> during all applicable effective dates and times unless cleared to do so by or through an official... a safety <span class="hlt">zone</span> during all applicable effective dates and times shall come to an immediate stop. (3...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol2/pdf/CFR-2013-title33-vol2-sec165-1191.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol2/pdf/CFR-2013-title33-vol2-sec165-1191.pdf"><span>33 CFR 165.1191 - Northern California and Lake Tahoe Area <span class="hlt">Annual</span> Fireworks <span class="hlt">Events</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-07-01</p> <p>... exact dates, times, and other details concerning the exact geographical description of the areas are... <span class="hlt">zone</span> during all applicable effective dates and times unless cleared to do so by or through an official... a safety <span class="hlt">zone</span> during all applicable effective dates and times shall come to an immediate stop. (3...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED128645.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED128645.pdf"><span><span class="hlt">Annual</span> Rural Manpower Report, 1975. State of Maine.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Maine State Dept. of Manpower Affairs, Augusta.</p> <p></p> <p>The <span class="hlt">Annual</span> Rural Manpower Report is a summary of <span class="hlt">events</span> and programs affecting rural communities during 1975. Intended as a general overview of activities in rural Maine, it is not an indepth study of all manpower programs serving the state. Part I provides the <span class="hlt">annual</span> summary and discusses planning, economic development, employment and…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=166939','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=166939"><span>Seasonal and Perennial Changes in the Distribution of Water in the Sapwood of Conifers in a Sub-Frigid <span class="hlt">Zone</span>1</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Utsumi, Yasuhiro; Sano, Yuzou; Funada, Ryo; Ohtani, Jun; Fujikawa, Seizo</p> <p>2003-01-01</p> <p>An analysis was made of progressive changes in patterns of cavitation in the sapwood of three species of conifer (Larix kaempferi, Abies sachalinensis, and Picea jezoensis) that were growing in a sub-frigid <span class="hlt">zone</span>. In all three conifers, all tracheids of the newly forming outermost <span class="hlt">annual</span> ring were filled with water or cytoplasm during the period from May to August. However, many tracheids in the transition <span class="hlt">zone</span> from earlywood to latewood lost water in September, presumably through drought-induced cavitation. Cavitated tracheids tended to be continuously distributed in a tangential direction. Subsequently, some earlywood tracheids of the outermost <span class="hlt">annual</span> ring lost water during the period from January to March. This was associated with freeze-thaw cycles. In the second and third <span class="hlt">annual</span> rings from the cambium of all three conifers, the lumina of most tracheids in the transition <span class="hlt">zone</span> from earlywood to latewood contained no water. In contrast, some latewood tracheids near the <span class="hlt">annual</span> ring boundary and many earlywood tracheids retained water in their lumina. The third <span class="hlt">annual</span> ring had more cavitated tracheids than the second <span class="hlt">annual</span> ring. Our observations indicated that cavitation progressed gradually in the tracheids of the conifers and that they were never refilled once cavitation had occurred. The region involved in water transport in conifers did not include the entire sapwood and differed among <span class="hlt">annual</span> rings. PMID:12692342</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eos.org/opinions/planning-for-a-subduction-zone-observatory','USGSPUBS'); return false;" href="https://eos.org/opinions/planning-for-a-subduction-zone-observatory"><span>Building a Subduction <span class="hlt">Zone</span> Observatory</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Gomberg, Joan S.; Bodin, Paul; Bourgeois, Jody; Cashman, Susan; Cowan, Darrel; Creager, Kenneth C.; Crowell, Brendan; Duvall, Alison; Frankel, Arthur; González, Frank I.; Houston, Heidi; Johnson, Paul; Kelsey, Harvey; Miller, Una; Roland, Emily C.; Schmidt, David; Staisch, Lydia; Vidale, John; Wilcock, William; Wirth, Erin</p> <p>2016-01-01</p> <p>Subduction <span class="hlt">zones</span> contain many of Earth’s most remarkable geologic structures, from the deepest oceanic trenches to glacier-covered mountains and steaming volcanoes. These environments formed through spectacular <span class="hlt">events</span>: Nature’s largest earthquakes, tsunamis, and volcanic eruptions are born here.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1994PApGe.142..101R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1994PApGe.142..101R"><span>Rupture process of large earthquakes in the northern Mexico subduction <span class="hlt">zone</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ruff, Larry J.; Miller, Angus D.</p> <p>1994-03-01</p> <p>The Cocos plate subducts beneath North America at the Mexico trench. The northernmost segment of this trench, between the Orozco and Rivera fracture <span class="hlt">zones</span>, has ruptured in a sequence of five large earthquakes from 1973 to 1985; the Jan. 30, 1973 Colima <span class="hlt">event</span> ( M s 7.5) at the northern end of the segment near Rivera fracture <span class="hlt">zone</span>; the Mar. 14, 1979 Petatlan <span class="hlt">event</span> ( M s 7.6) at the southern end of the segment on the Orozco fracture <span class="hlt">zone</span>; the Oct. 25, 1981 Playa Azul <span class="hlt">event</span> ( M s 7.3) in the middle of the Michoacan “gap”; the Sept. 19, 1985 Michoacan mainshock ( M s 8.1); and the Sept. 21, 1985 Michoacan aftershock ( M s 7.6) that reruptured part of the Petatlan <span class="hlt">zone</span>. Body wave inversion for the rupture process of these earthquakes finds the best: earthquake depth; focal mechanism; overall source time function; and seismic moment, for each earthquake. In addition, we have determined spatial concentrations of seismic moment release for the Colima earthquake, and the Michoacan mainshock and aftershock. These spatial concentrations of slip are interpreted as asperities; and the resultant asperity distribution for Mexico is compared to other subduction <span class="hlt">zones</span>. The body wave inversion technique also determines the Moment Tensor Rate Functions; but there is no evidence for statistically significant changes in the moment tensor during rupture for any of the five earthquakes. An appendix describes the Moment Tensor Rate Functions methodology in detail. The systematic bias between global and regional determinations of epicentral locations in Mexico must be resolved to enable plotting of asperities with aftershocks and geographic features. We have spatially “shifted” all of our results to regional determinations of epicenters. The best point source depths for the five earthquakes are all above 30 km, consistent with the idea that the down-dip edge of the seismogenic plate interface in Mexico is shallow compared to other subduction <span class="hlt">zones</span>. Consideration of uncertainties in</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70018510','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70018510"><span>Effects of thermal vapor diffusion on seasonal dynamics of water in the unsaturated <span class="hlt">zone</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Milly, Paul C.D.</p> <p>1996-01-01</p> <p>The response of water in the unsaturated <span class="hlt">zone</span> to seasonal changes of temperature (T) is determined analytically using the theory of nonisothermal water transport in porous media, and the solutions are tested against field observations of moisture potential and bomb fallout isotopic (36Cl and 3H) concentrations. Seasonally varying land surface temperatures and the resulting subsurface temperature gradients induce thermal vapor diffusion. The <span class="hlt">annual</span> mean vertical temperature gradient is close to zero; however, the <span class="hlt">annual</span> mean thermal vapor flux is downward, because the temperature‐dependent vapor diffusion coefficient is larger, on average, during downward diffusion (occurring at high T) than during upward diffusion (low T). The <span class="hlt">annual</span> mean thermal vapor flux is shown to decay exponentially with depth; the depth (about 1 m) at which it decays to e−1of its surface value is one half of the corresponding decay depth for the amplitude of seasonal temperature changes. This depth‐dependent <span class="hlt">annual</span> mean flux is effectively a source of water, which must be balanced by a flux divergence associated with other transport processes. In a relatively humid environment the liquid fluxes greatly exceed the thermal vapor fluxes, so such a balance is readily achieved without measurable effect on the dynamics of water in the unsaturated <span class="hlt">zone</span>. However, if the mean vertical water flux through the unsaturated <span class="hlt">zone</span> is very small (<1 mm y−1), as it may be at many locations in a desert landscape, the thermal vapor flux must be balanced mostly by a matric‐potential‐induced upward flux of water. This return flux may include both vapor and liquid components. Below any near‐surface <span class="hlt">zone</span> of weather‐related fluctuations of matric potential, maintenance of this upward flux requires an increase with depth in the <span class="hlt">annual</span> mean matric potential; this theoretical prediction is supported by long‐term field measurements in the Chihuahuan Desert. The analysis also makes predictions</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_10");'>10</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li class="active"><span>12</span></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_12 --> <div id="page_13" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li class="active"><span>13</span></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="241"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMMR33B0473A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMMR33B0473A"><span>Dynamic permeability in fault damage <span class="hlt">zones</span> induced by repeated coseismic fracturing <span class="hlt">events</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Aben, F. M.; Doan, M. L.; Mitchell, T. M.</p> <p>2017-12-01</p> <p>Off-fault fracture damage in upper crustal fault <span class="hlt">zones</span> change the fault <span class="hlt">zone</span> properties and affect various co- and interseismic processes. One of these properties is the permeability of the fault damage <span class="hlt">zone</span> rocks, which is generally higher than the surrounding host rock. This allows large-scale fluid flow through the fault <span class="hlt">zone</span> that affects fault healing and promotes mineral transformation processes. Moreover, it might play an important role in thermal fluid pressurization during an earthquake rupture. The damage <span class="hlt">zone</span> permeability is dynamic due to coseismic damaging. It is crucial for earthquake mechanics and for longer-term processes to understand how the dynamic permeability structure of a fault looks like and how it evolves with repeated earthquakes. To better detail coseismically induced permeability, we have performed uniaxial split Hopkinson pressure bar experiments on quartz-monzonite rock samples. Two sample sets were created and analyzed: single-loaded samples subjected to varying loading intensities - with damage varying from apparently intact to pulverized - and samples loaded at a constant intensity but with a varying number of repeated loadings. The first set resembles a dynamic permeability structure created by a single large earthquake. The second set resembles a permeability structure created by several earthquakes. After, the permeability and acoustic velocities were measured as a function of confining pressure. The permeability in both datasets shows a large and non-linear increase over several orders of magnitude (from 10-20 up to 10-14 m2) with an increasing amount of fracture damage. This, combined with microstructural analyses of the varying degrees of damage, suggests a percolation threshold. The percolation threshold does not coincide with the pulverization threshold. With increasing confining pressure, the permeability might drop up to two orders of magnitude, which supports the possibility of large coseismic fluid pulses over relatively</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.T52B..03A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.T52B..03A"><span>Paleoseismological surveys on the Hinagu fault <span class="hlt">zone</span> in Kumamoto, central Kyushu, Japan</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Azuma, T.</p> <p>2017-12-01</p> <p>The Hinagu fault <span class="hlt">zone</span> is located on the south of the Futagawa fault <span class="hlt">zone</span>, which was a main part of the source fault of the 2016 Kumamoto earthquake of Mj 7.3. Northernmost part of the Hinagu fault <span class="hlt">zone</span> was also acted in 2016 <span class="hlt">event</span> and surface faults with right-lateral displacement upto ca. 50 cm were appeared. Seismicity along the central part of the Hinagu fault was increased just after the 2016 Kumamoto Earthquake. It seems that the Hinagu fault <span class="hlt">zone</span> would produce the next large earthquake in the near future, although it has not occurred yet. The Headquarters of the Earthquake Research Promotions (HERP) conducted active fault surveys on the Hinagu fault <span class="hlt">zone</span> to recognize the probability of the occurrence of the next faulting <span class="hlt">event</span>. The Hinagu fault <span class="hlt">zone</span> is composed with 3 fault segments, Takano-Shirahata, Hinagu, and Yatsushiro Bay. Yatsushiro Bay segment is offshore fault. In FY2016, we conducted paleoseismological trenching surveys at 2 sites (Yamaide, Minamibeta) and offshore drilling. Those result showed evidences that the recurrence intervals of the Hinagu fault <span class="hlt">zone</span> was rather short and the last faulting <span class="hlt">event</span> occurred around 1500-2000 yrsBP. In FY2017, we are planning another trenching survey on the southern part of the central segment, where Yatsushiro city located close to the fault.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-05-04/pdf/2010-10312.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-05-04/pdf/2010-10312.pdf"><span>75 FR 23589 - Safety <span class="hlt">Zone</span> Regulations, Seafair Blue Angels Air Show Performance, Seattle, WA</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-05-04</p> <p>... <span class="hlt">Zone</span> Regulations, Seafair Blue Angels Air Show Performance, Seattle, WA AGENCY: Coast Guard, DHS... Washington, WA for the <span class="hlt">annual</span> Seafair Blue Angels Air Show from 10 a.m. on August 5, 2010 to 6 p.m. on August... Washington for the <span class="hlt">annual</span> Seafair Blue Angels Air Show Performance. The Coast Guard will enforce the safety...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-05-06/pdf/2010-10613.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-05-06/pdf/2010-10613.pdf"><span>75 FR 24799 - Safety <span class="hlt">Zone</span>; Tri-City Water Follies Hydroplane Races Practice Sessions, Columbia River, Kennewick...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-05-06</p> <p>...-AA00 Safety <span class="hlt">Zone</span>; Tri-City Water Follies Hydroplane Races Practice Sessions, Columbia River, Kennewick...-City Water Follies Association hosts <span class="hlt">annual</span> hydroplane races on the Columbia River in Kennewick... Safety <span class="hlt">Zone</span>; Tri-City Water Follies Hydroplane Races Practice Sessions, Columbia River, Kennewick, WA (a...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70024637','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70024637"><span>Quantitative analysis of seismic fault <span class="hlt">zone</span> waves in the rupture <span class="hlt">zone</span> of the 1992 Landers, California, earthquake: Evidence for a shallow trapping structure</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Peng, Z.; Ben-Zion, Y.; Michael, A.J.; Zhu, L.</p> <p>2003-01-01</p> <p>We analyse quantitatively a waveform data set of 238 earthquakes recorded by a dense seismic array across and along the rupture <span class="hlt">zone</span> of the 1992 Landers earthquake. A grid-search method with station delay corrections is used to locate <span class="hlt">events</span> that do not have catalogue locations. The quality of fault <span class="hlt">zone</span> trapped waves generated by each <span class="hlt">event</span> is determined from the ratios of seismic energy in time windows corresponding to trapped waves and direct S waves at stations close to and off the fault <span class="hlt">zone</span>. Approximately 70 per cent of the <span class="hlt">events</span> with S-P times of less than 2 s, including many clearly off the fault, produce considerable trapped wave energy. This distribution is in marked contrast with previous claims that trapped waves are generated only by sources close to or inside the Landers rupture <span class="hlt">zone</span>. The time difference between the S arrival and trapped waves group does not grow systematically with increasing hypocentral distance and depth. The dispersion measured from the trapped waves is weak. These results imply that the seismic trapping structure at the Landers rupture <span class="hlt">zone</span> is shallow and does not extend continuously along-strike by more than a few kilometres. Synthetic waveform modelling indicates that the fault <span class="hlt">zone</span> waveguide has depth of approximately 2-4 km, a width of approximately 200 m, an S-wave velocity reduction relative to the host rock of approximately 30-40 per cent and an S-wave attenuation coefficient of approximately 20-30. The fault <span class="hlt">zone</span> waveguide north of the array appears to be shallower and weaker than that south of the array. The waveform modelling also indicates that the seismic trapping structure below the array is centred approximately 100 m east of the surface break.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29398634','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29398634"><span>Existing and potential infection risk <span class="hlt">zones</span> of yellow fever worldwide: a modelling analysis.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Shearer, Freya M; Longbottom, Joshua; Browne, Annie J; Pigott, David M; Brady, Oliver J; Kraemer, Moritz U G; Marinho, Fatima; Yactayo, Sergio; de Araújo, Valdelaine E M; da Nóbrega, Aglaêr A; Fullman, Nancy; Ray, Sarah E; Mosser, Jonathan F; Stanaway, Jeffrey D; Lim, Stephen S; Reiner, Robert C; Moyes, Catherine L; Hay, Simon I; Golding, Nick</p> <p>2018-03-01</p> <p> was estimated to be substantially less than the recommended threshold to prevent outbreaks. Overall, we estimated that vaccination coverage levels achieved by 2016 avert between 94 336 and 118 500 cases of yellow fever <span class="hlt">annually</span> within risk <span class="hlt">zones</span>, on the basis of conservative and optimistic vaccination scenarios. The areas outside at-risk regions with predicted high receptivity to yellow fever transmission (eg, parts of Malaysia, Indonesia, and Thailand) were less extensive than the distribution of the main urban vector, A aegypti, with low receptivity to yellow fever transmission in southern China, where A aegypti is known to occur. Our results provide the evidence base for targeting vaccination campaigns within risk <span class="hlt">zones</span>, as well as emphasising their high effectiveness. Our study highlights areas where public health authorities should be most vigilant for potential spread or importation <span class="hlt">events</span>. Bill & Melinda Gates Foundation. Copyright © 2018 The Author(s). Published by Elsevier Ltd. This is an Open Access article under the CC BY 4.0 license. Published by Elsevier Ltd.. All rights reserved.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://images.nasa.gov/#/details-KSC-03pd2181.html','SCIGOVIMAGE-NASA'); return false;" href="https://images.nasa.gov/#/details-KSC-03pd2181.html"><span>KENNEDY SPACE CENTER, FLA. - Children enjoy displays of security equipment during Take Our Children to Work Day. Employees were invited to share their work experience with their children on this <span class="hlt">annual</span> <span class="hlt">event</span>.</span></a></p> <p><a target="_blank" href="https://images.nasa.gov/">NASA Image and Video Library</a></p> <p></p> <p>2003-07-24</p> <p>KENNEDY SPACE CENTER, FLA. - Children enjoy displays of security equipment during Take Our Children to Work Day. Employees were invited to share their work experience with their children on this <span class="hlt">annual</span> <span class="hlt">event</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://images.nasa.gov/#/details-KSC-03pd2182.html','SCIGOVIMAGE-NASA'); return false;" href="https://images.nasa.gov/#/details-KSC-03pd2182.html"><span>KENNEDY SPACE CENTER, FLA. - Children enjoy displays of fire equipment during Take Our Children to Work Day. Employees were invited to share their work experience with their children on this <span class="hlt">annual</span> <span class="hlt">event</span>.</span></a></p> <p><a target="_blank" href="https://images.nasa.gov/">NASA Image and Video Library</a></p> <p></p> <p>2003-07-24</p> <p>KENNEDY SPACE CENTER, FLA. - Children enjoy displays of fire equipment during Take Our Children to Work Day. Employees were invited to share their work experience with their children on this <span class="hlt">annual</span> <span class="hlt">event</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMGC23G1194S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMGC23G1194S"><span>Classification and Space-Time Analysis of Precipitation <span class="hlt">Events</span> in Manizales, Caldas, Colombia.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Suarez Hincapie, J. N.; Vélez, J.; Romo Melo, L.; Chang, P.</p> <p>2015-12-01</p> <p>Manizales is a mid-mountain Andean city located near the Nevado del Ruiz volcano in west-central Colombia, this location exposes it to earthquakes, floods, landslides and volcanic eruptions. It is located in the intertropical convergence <span class="hlt">zone</span> (ITCZ) and presents a climate with a bimodal rainfall regime (Cortés, 2010). Its mean <span class="hlt">annual</span> rainfall is 2000 mm, one may observe precipitation 70% of the days over a year. This rain which favors the formation of large masses of clouds and the presence of macroclimatic phenomenon as "El Niño South Oscillation", has historically caused great impacts in the region (Vélez et al, 2012). For example the geographical location coupled with rain <span class="hlt">events</span> results in a high risk of landslides in the city. Manizales has a hydrometeorological network of 40 stations that measure and transmit data of up to eight climate variables. Some of these stations keep 10 years of historical data. However, until now this information has not been used for space-time classification of precipitation <span class="hlt">events</span>, nor has the meteorological variables that influence them been thoroughly researched. The purpose of this study was to classify historical <span class="hlt">events</span> of rain in an urban area of Manizales and investigate patterns of atmospheric behavior that influence or trigger such <span class="hlt">events</span>. Classification of <span class="hlt">events</span> was performed by calculating the "n" index of the heavy rainfall, describing the behavior of precipitation as a function of time throughout the <span class="hlt">event</span> (Monjo, 2009). The analysis of meteorological variables was performed using statistical quantification over variable time periods before each <span class="hlt">event</span>. The proposed classification allowed for an analysis of the evolution of rainfall <span class="hlt">events</span>. Specially, it helped to look for the influence of different meteorological variables triggering rainfall <span class="hlt">events</span> in hazardous areas as the city of Manizales.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017CSR...151...40T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017CSR...151...40T"><span>Nearshore circulation on a sea breeze dominated beach during intense wind <span class="hlt">events</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Torres-Freyermuth, Alec; Puleo, Jack A.; DiCosmo, Nick; Allende-Arandía, Ma. Eugenia; Chardón-Maldonado, Patricia; López, José; Figueroa-Espinoza, Bernardo; de Alegria-Arzaburu, Amaia Ruiz; Figlus, Jens; Roberts Briggs, Tiffany M.; de la Roza, Jacobo; Candela, Julio</p> <p>2017-12-01</p> <p>A field experiment was conducted on the northern Yucatan coast from April 1 to April 12, 2014 to investigate the role of intense wind <span class="hlt">events</span> on coastal circulation from the inner shelf to the swash <span class="hlt">zone</span>. The study area is characterized by a micro-tidal environment, low-energy wave conditions, and a wide and shallow continental shelf. Furthermore, easterly trade winds, local breezes, and synoptic-scale <span class="hlt">events</span>, associated with the passage of cold-fronts known as Nortes, are ubiquitous in this region. Currents were measured concurrently at different cross-shore locations during both local and synoptic-scale intense wind <span class="hlt">events</span> to investigate the influence of different forcing mechanisms (i.e., large-scale currents, winds, tides, and waves) on the nearshore circulation. Field observations revealed that nearshore circulation across the shelf is predominantly alongshore-directed (westward) during intense winds. However, the mechanisms responsible for driving instantaneous spatial and temporal current variability depend on the weather conditions and the across-shelf location. During local strong sea breeze <span class="hlt">events</span> (W > 10 m s-1 from the NE) occurring during spring tide, westward circulation is controlled by the tides, wind, and waves at the inner-shelf, shallow waters, and inside the surf/swash <span class="hlt">zone</span>, respectively. The nearshore circulation is relaxed during intense land breeze <span class="hlt">events</span> (W ≈ 9 m s-1 from the SE) associated with the low atmospheric pressure system that preceded a Norte <span class="hlt">event</span>. During the Norte <span class="hlt">event</span> (Wmax≈ 15 m s-1 from the NNW), westward circulation dominated outside the surf <span class="hlt">zone</span> and was correlated to the Yucatan Current, whereas wave breaking forces eastward currents inside the surf/swash <span class="hlt">zone</span>. The latter finding implies the existence of large alongshore velocity shear at the offshore edge of the surf <span class="hlt">zone</span> during the Norte <span class="hlt">event</span>, which enhances mixing between the surf <span class="hlt">zone</span> and the inner shelf. These findings suggest that both sea breezes and Nortes play</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3943949','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3943949"><span>An Abrupt Centennial-Scale Drought <span class="hlt">Event</span> and Mid-Holocene Climate Change Patterns in Monsoon Marginal <span class="hlt">Zones</span> of East Asia</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Li, Yu; Wang, Nai'ang; Zhang, Chengqi</p> <p>2014-01-01</p> <p>The mid-latitudes of East Asia are characterized by the interaction between the Asian summer monsoon and the westerly winds. Understanding long-term climate change in the marginal regions of the Asian monsoon is critical for understanding the millennial-scale interactions between the Asian monsoon and the westerly winds. Abrupt climate <span class="hlt">events</span> are always associated with changes in large-scale circulation patterns; therefore, investigations into abrupt climate changes provide clues for responses of circulation patterns to extreme climate <span class="hlt">events</span>. In this paper, we examined the time scale and mid-Holocene climatic background of an abrupt dry mid-Holocene <span class="hlt">event</span> in the Shiyang River drainage basin in the northwest margin of the Asian monsoon. Mid-Holocene lacustrine records were collected from the middle reaches and the terminal lake of the basin. Using radiocarbon and OSL ages, a centennial-scale drought <span class="hlt">event</span>, which is characterized by a sand layer in lacustrine sediments both from the middle and lower reaches of the basin, was absolutely dated between 8.0–7.0 cal kyr BP. Grain size data suggest an abrupt decline in lake level and a dry environment in the middle reaches of the basin during the dry interval. Previous studies have shown mid-Holocene drought <span class="hlt">events</span> in other places of monsoon marginal <span class="hlt">zones</span>; however, their chronologies are not strong enough to study the mechanism. According to the absolutely dated records, we proposed a new hypothesis that the mid-Holocene dry interval can be related to the weakening Asian summer monsoon and the relatively arid environment in arid Central Asia. Furthermore, abrupt dry climatic <span class="hlt">events</span> are directly linked to the basin-wide effective moisture change in semi-arid and arid regions. Effective moisture is affected by basin-wide precipitation, evapotranspiration, lake surface evaporation and other geographical settings. As a result, the time scales of the dry interval could vary according to locations due to different</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24599259','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24599259"><span>An abrupt centennial-scale drought <span class="hlt">event</span> and mid-holocene climate change patterns in monsoon marginal <span class="hlt">zones</span> of East Asia.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Li, Yu; Wang, Nai'ang; Zhang, Chengqi</p> <p>2014-01-01</p> <p>The mid-latitudes of East Asia are characterized by the interaction between the Asian summer monsoon and the westerly winds. Understanding long-term climate change in the marginal regions of the Asian monsoon is critical for understanding the millennial-scale interactions between the Asian monsoon and the westerly winds. Abrupt climate <span class="hlt">events</span> are always associated with changes in large-scale circulation patterns; therefore, investigations into abrupt climate changes provide clues for responses of circulation patterns to extreme climate <span class="hlt">events</span>. In this paper, we examined the time scale and mid-Holocene climatic background of an abrupt dry mid-Holocene <span class="hlt">event</span> in the Shiyang River drainage basin in the northwest margin of the Asian monsoon. Mid-Holocene lacustrine records were collected from the middle reaches and the terminal lake of the basin. Using radiocarbon and OSL ages, a centennial-scale drought <span class="hlt">event</span>, which is characterized by a sand layer in lacustrine sediments both from the middle and lower reaches of the basin, was absolutely dated between 8.0-7.0 cal kyr BP. Grain size data suggest an abrupt decline in lake level and a dry environment in the middle reaches of the basin during the dry interval. Previous studies have shown mid-Holocene drought <span class="hlt">events</span> in other places of monsoon marginal <span class="hlt">zones</span>; however, their chronologies are not strong enough to study the mechanism. According to the absolutely dated records, we proposed a new hypothesis that the mid-Holocene dry interval can be related to the weakening Asian summer monsoon and the relatively arid environment in arid Central Asia. Furthermore, abrupt dry climatic <span class="hlt">events</span> are directly linked to the basin-wide effective moisture change in semi-arid and arid regions. Effective moisture is affected by basin-wide precipitation, evapotranspiration, lake surface evaporation and other geographical settings. As a result, the time scales of the dry interval could vary according to locations due to different geographical</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-08-12/pdf/2013-19417.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-08-12/pdf/2013-19417.pdf"><span>78 FR 48802 - Safety <span class="hlt">Zones</span>; Recurring <span class="hlt">Events</span> in Captain of the Port Duluth <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-08-12</p> <p>... fireworks, and other historically recurring marine <span class="hlt">events</span>, including the Lake Superior Dragon Boat Festival... with a Notice of Enforcement and marine information broadcast. (2) Lake Superior Dragon Boat Festival...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29284546','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29284546"><span>Medical Emergencies Related to Ethanol and Illicit Drugs at an <span class="hlt">Annual</span>, Nocturnal, Indoor, Electronic Dance Music <span class="hlt">Event</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Calle, Paul; Sundahl, Nora; Maudens, Kristof; Wille, Sarah Mr; Van Sassenbroeck, Diederik; De Graeve, Koen; Gogaert, Stefan; De Paepe, Peter; Devriese, Dieter; Arno, Geert; Blanckaert, Peter</p> <p>2018-02-01</p> <p> clinical presentations were rather mild. It should be stressed that these observations only apply to this particular <span class="hlt">event</span> and cannot be generalized to other EDM <span class="hlt">events</span>. Calle P , Sundahl N , Maudens K , Wille SMR , Van Sassenbroeck D , De Graeve K , Gogaert S , De Paepe P , Devriese D , Arno G , Blanckaert P . Medical emergencies related to ethanol and illicit drugs at an <span class="hlt">annual</span>, nocturnal, indoor, electronic dance music <span class="hlt">event</span>. Prehosp Disaster Med. 2018;33(1):71-76.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/6819396-implications-localized-zone-seismic-activity-near-inner-piedmont-blue-ridge-boundary','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/6819396-implications-localized-zone-seismic-activity-near-inner-piedmont-blue-ridge-boundary"><span>Implications of a localized <span class="hlt">zone</span> of seismic activity near the Inner Piedmont-Blue Ridge boundary</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Douglas, S.; Powell, C.</p> <p>1994-03-01</p> <p>A small but distinct cluster of earthquake activity is located in Henderson County, NC, near the boundary of the Inner Piedmont and Blue Ridge physiographic provinces. Over twenty <span class="hlt">events</span> have occurred within the cluster since 1776 and four had body-wave magnitudes exceeding 3.0. Average focal depth for instrumentally recorded <span class="hlt">events</span> is 7.7 km. Epicenters plot within the Inner Piedmont, roughly 13 km from the surface expression of the Brevard fault <span class="hlt">zone</span>. The reason for sustained earthquake activity in Henderson County is not known but the close spatial association of the <span class="hlt">events</span> with the Brevard fault suggests a causal relationship. Themore » Brevard <span class="hlt">zone</span> dips steeply to the SE and the <span class="hlt">events</span> could be associated with the fault at depth. An even more intriguing possibility is that the <span class="hlt">events</span> are associated with the intersection of the Brevard <span class="hlt">zone</span> and the decollemont; this possibility is compatible with available information concerning the depth to the decollemont and the dip on the Brevard <span class="hlt">zone</span>. An association of seismic activity with the Brevard <span class="hlt">zone</span> at depth is supported by the presence of another small cluster of activity located in Rutherford County, NC. This cluster is located in the Inner Piedmont, roughly 30 km NE of the Henderson cluster and 16 km from the Brevard fault <span class="hlt">zone</span>. Association of seismic activity with known faults is very rare in the eastern US and has implications for tectonic models and hazard evaluation. Additional research must be conducted to determine the feasibility that activity is associated with the Brevard <span class="hlt">zone</span>.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-09-04/pdf/2012-21717.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-09-04/pdf/2012-21717.pdf"><span>77 FR 53769 - Safety <span class="hlt">Zone</span>; Liberty to Freedom Swims, Liberty Island, Upper Bay and Hudson River, NY</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-09-04</p> <p>... 1625-AA00 Safety <span class="hlt">Zone</span>; Liberty to Freedom Swims, Liberty Island, Upper Bay and Hudson River, NY AGENCY... September 5, 2012 and September 15, 2012 Liberty to Freedom swim <span class="hlt">events</span>. This temporary safety <span class="hlt">zone</span> is necessary to protect the maritime public and <span class="hlt">event</span> participants from the hazards associated with swim <span class="hlt">events</span>...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/872459','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/872459"><span>Mobile machine hazardous working <span class="hlt">zone</span> warning system</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Schiffbauer, William H.; Ganoe, Carl W.</p> <p>1999-01-01</p> <p>A warning system is provided for a mobile working machine to alert an individual of a potentially dangerous condition in the <span class="hlt">event</span> the individual strays into a hazardous working <span class="hlt">zone</span> of the machine. The warning system includes a transmitter mounted on the machine and operable to generate a uniform magnetic field projecting beyond an outer periphery of the machine in defining a hazardous working <span class="hlt">zone</span> around the machine during operation thereof. A receiver, carried by the individual and activated by the magnetic field, provides an alarm signal to alert the individual when he enters the hazardous working <span class="hlt">zone</span> of the machine.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/678578','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/biblio/678578"><span>Mobile machine hazardous working <span class="hlt">zone</span> warning system</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Schiffbauer, W.H.; Ganoe, C.W.</p> <p>1999-08-17</p> <p>A warning system is provided for a mobile working machine to alert an individual of a potentially dangerous condition in the <span class="hlt">event</span> the individual strays into a hazardous working <span class="hlt">zone</span> of the machine. The warning system includes a transmitter mounted on the machine and operable to generate a uniform magnetic field projecting beyond an outer periphery of the machine in defining a hazardous working <span class="hlt">zone</span> around the machine during operation. A receiver, carried by the individual and activated by the magnetic field, provides an alarm signal to alert the individual when he enters the hazardous working <span class="hlt">zone</span> of the machine. 3 figs.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010EGUGA..1212942H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010EGUGA..1212942H"><span>Revisiting the physical characterisitics of the subduction interplate seismogenic <span class="hlt">zones</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Heuret, Arnauld; Lallemand, Serge; Funiciello, Francesca; Piromallo, Claudia</p> <p>2010-05-01</p> <p>Based on the Centennial earthquake catalog, the revised 1964-2007 EHB hypocenters catalog and the 1976-2007 CMT Harvard catalog, we have extracted the hypocenters, nodal planes and seismic moments of worldwide subduction earthquakes for the 1900-2007 period. For the 1976-2007 period, we combine the focal solutions provided by Harvard and the revised hypocenters from Engdahl et al. (1998). Older <span class="hlt">events</span> are extracted from the Centennial catalogue (Engdahl and Villasenor, 2002) and they are used to estimate the cumulated seismic moment only. The selection criteria for the subduction earthquakes are similar to those used by Mc Caffrey (1994), i.e., we test if the focal mechanisms are consistent with 1/ shallow thrust <span class="hlt">events</span> (depth > 70 km, positive slips, and at least one nodal plane gets dip < 45°), and, 2/ the plate interface local geometry and orientation (one nodal plane is oriented toward the volcanic arc, the azimuth of this nodal plane ranges between ± 45° with respect to the trench one, its dip ranges between ± 20° with respect to the slab one and the epicentre is located seaward of the volcanic arc). Our study concerns segments of subduction <span class="hlt">zones</span> that fit with estimated paleoruptures associated with major <span class="hlt">events</span> (M > 8). We assume that the seismogenic <span class="hlt">zone</span> coincides with the distribution of 5.5 < M < 7 subduction earthquakes. We provide a map of the interplate seismogenic <span class="hlt">zones</span> for 80% of the trench systems including dip, length, downdip and updip limits, we revisit the statistical study done by Pacheco et al. (1993) and test some empirical laws obtained for example by Ruff and Kanamori (1980) in light of a more complete, detailed, accurate and uniform description of the subduction interplate seismogenic <span class="hlt">zone</span>. Since subduction earthquakes result from stress accumulation along the interplate and stress depends on plates kinematics, subduction <span class="hlt">zone</span> geometry, thermal state and seismic coupling, we aim to isolate some correlations between parameters. The</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70186690','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70186690"><span>Fault-<span class="hlt">zone</span> waves observed at the southern Joshua Tree earthquake rupture <span class="hlt">zone</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Hough, S.E.; Ben-Zion, Y.; Leary, P.</p> <p>1994-01-01</p> <p>Waveform and spectral characteristics of several aftershocks of the M 6.1 22 April 1992 Joshua Tree earthquake recorded at stations just north of the Indio Hills in the Coachella Valley can be interpreted in terms of waves propagating within narrow, low-velocity, high-attenuation, vertical <span class="hlt">zones</span>. Evidence for our interpretation consists of: (1) emergent P arrivals prior to and opposite in polarity to the impulsive direct phase; these arrivals can be modeled as headwaves indicative of a transfault velocity contrast; (2) spectral peaks in the S wave train that can be interpreted as internally reflected, low-velocity fault-<span class="hlt">zone</span> wave energy; and (3) spatial selectivity of <span class="hlt">event</span>-station pairs at which these data are observed, suggesting a long, narrow geologic structure. The observed waveforms are modeled using the analytical solution of Ben-Zion and Aki (1990) for a plane-parallel layered fault-<span class="hlt">zone</span> structure. Synthetic waveform fits to the observed data indicate the presence of NS-trending vertical fault-<span class="hlt">zone</span> layers characterized by a thickness of 50 to 100 m, a velocity decrease of 10 to 15% relative to the surrounding rock, and a P-wave quality factor in the range 25 to 50.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_11");'>11</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li class="active"><span>13</span></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_13 --> <div id="page_14" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li class="active"><span>14</span></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="261"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29569319','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29569319"><span>Modeling the Impact of Stream Discharge <span class="hlt">Events</span> on Riparian Solute Dynamics.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Mahmood, Muhammad Nasir; Schmidt, Christian; Fleckenstein, Jan H; Trauth, Nico</p> <p>2018-03-22</p> <p>The biogeochemical composition of stream water and the surrounding riparian water is mainly defined by the exchange of water and solutes between the stream and the riparian <span class="hlt">zone</span>. Short-term fluctuations in near stream hydraulic head gradients (e.g., during stream flow <span class="hlt">events</span>) can significantly influence the extent and rate of exchange processes. In this study, we simulate exchanges between streams and their riparian <span class="hlt">zone</span> driven by stream stage fluctuations during single stream discharge <span class="hlt">events</span> of varying peak height and duration. Simulated results show that strong stream flow <span class="hlt">events</span> can trigger solute mobilization in riparian soils and subsequent export to the stream. The timing and amount of solute export is linked to the shape of the discharge <span class="hlt">event</span>. Higher peaks and increased durations significantly enhance solute export, however, peak height is found to be the dominant control for overall mass export. Mobilized solutes are transported to the stream in two stages (1) by return flow of stream water that was stored in the riparian <span class="hlt">zone</span> during the <span class="hlt">event</span> and (2) by vertical movement to the groundwater under gravity drainage from the unsaturated parts of the riparian <span class="hlt">zone</span>, which lasts for significantly longer time (> 400 days) resulting in long tailing of bank outflows and solute mass outfluxes. We conclude that strong stream discharge <span class="hlt">events</span> can mobilize and transport solutes from near stream riparian soils into the stream. The impact of short-term stream discharge variations on solute exchange may last for long times after the flow <span class="hlt">event</span>. © 2018, National Ground Water Association.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-02-20/pdf/2013-03826.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-02-20/pdf/2013-03826.pdf"><span>78 FR 11798 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> Fireworks <span class="hlt">Events</span> in the Captain of the Port Buffalo <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-02-20</p> <p>... include your name and a mailing address, an email address, or a telephone number in the body of your... feet. With the above findings in mind, the Coast Guard proposes to amend 33 CFR 165.939 to disestablish...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-06-23/pdf/2010-15145.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-06-23/pdf/2010-15145.pdf"><span>75 FR 35648 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> Fireworks <span class="hlt">Events</span> in the Captain of the Port Detroit <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-06-23</p> <p>... regulation will also be enforced from 9:30 p.m. to 11 p.m. on July 4, 2010. Sec. 165.941(a)(37) Caseville... weather on July 3, 2010, this regulation will also be enforced from 9:30 p.m. to 11 p.m. on July 4, 2010... regulation will also be enforced from 9:30 p.m. to 11 p.m. on July 4, 2010. Sec. 165.941(a)(36) Grosse Point...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=ASE+AND+1&pg=2&id=EJ911832','ERIC'); return false;" href="https://eric.ed.gov/?q=ASE+AND+1&pg=2&id=EJ911832"><span>ASE <span class="hlt">Annual</span> Conference 2010</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>McCune, Roger</p> <p>2010-01-01</p> <p>In this article, the author describes the ASE <span class="hlt">Annual</span> Conference 2010 which was held at Nottingham after a gap of 22 years. As always, the main conference was preceded by International Day, an important <span class="hlt">event</span> for science educators from across the world. There were two strands to the programme: (1) "What works for me?"--sharing new ideas…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/5939921-bermuda-earthquake-march-significant-oceanic-intraplate-event','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/5939921-bermuda-earthquake-march-significant-oceanic-intraplate-event"><span>Bermuda earthquake of March 24, 1978: A significant oceanic intraplate <span class="hlt">event</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Stewart, G.S.; Helmberger, D.V.</p> <p>1981-08-10</p> <p>The Bremuda earthquake (Mapprox.6) occured near the westerly extension of the Kane Fracture <span class="hlt">Zone</span> roughly 370 km southwest of the island of Bermuda. It is one of the largest oceanic intraplate earthquakes to occur off the eastern coast of North America. Because of its size and location, it has provided an excellent set of WWSSN body waves. They can be used to infer its depth and faulting parameters by waveform modeling techniques. The results indicate a north-northwest striking thrust mechanism (strike = N20 /sup 0/W, dip = 42 /sup 0/NE, rake = 90/sup 0/) with the hypocenter located at amore » depth of 11 km, which for an oceanic crust places it predominantly in the mantle. The <span class="hlt">event</span> had a seismic moment of 3.4 x 10/sup 25/ dyne cm, and its time history was modeled with a symmetric trapezoidal time function 3 s in duration. The north-northwest strike of the <span class="hlt">event</span> is in good agreement with the bathymetry of the area, the epicenter being close to the southwestern edge of the Bermuda Rise. The strike of the <span class="hlt">event</span> is also close to that of the inferred extensions of the present ridge fracture <span class="hlt">zones</span> in the region. The strike of the <span class="hlt">event</span> is also close to that of the inferred extensions of the present ridge fracture <span class="hlt">zones</span> in the region. The presence of fracture <span class="hlt">zones</span> is indicative of local weak <span class="hlt">zones</span> in the lithosphere. The Bermuda earthquake most likely is associated with one of these <span class="hlt">zones</span> of weakness and is the result of the application of present day stress imposed on the region by the North American plate in the direction of its absolute motion. This is an important <span class="hlt">event</span> in terms of understanding and estimating seismic hazard on the eastern seaboard of North America.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-02-27/pdf/2012-4390.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-02-27/pdf/2012-4390.pdf"><span>77 FR 11426 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> <span class="hlt">Events</span> Requiring Safety <span class="hlt">Zones</span> in the Captain of the Port Lake Michigan <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-02-27</p> <p>... Aerospace Challenge Sport Rocket Launch; Muskegon, MI. (i) Location. All waters of Muskegon Lake, near the... 5 p.m. (5) Celebrate De Pere; De Pere, WI. (i) Location. All waters of the Fox River, near Voyageur... waters of the Fox River, near the Western Lime Company 1.13 miles above the head of the Fox River, within...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-02-11/pdf/2013-02955.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-02-11/pdf/2013-02955.pdf"><span>78 FR 9640 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> <span class="hlt">Events</span> Requiring Safety <span class="hlt">Zones</span> in the Captain of the Port Lake Michigan <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-02-11</p> <p>.... to 7 p.m. (2) Michigan Aerospace Challenge Sport Rocket Launch; Muskegon, MI. (i) Location. All.... All waters of the Fox River, near Voyageur Park, within the arc of a circle with a 500 foot radius... waters of the Fox River, near the Western Lime Company 1.13 miles above the head of the Fox River, within...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-05-24/pdf/2011-12374.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-05-24/pdf/2011-12374.pdf"><span>76 FR 30072 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> <span class="hlt">Events</span> Requiring Safety <span class="hlt">Zones</span> in the Captain of the Port Lake Michigan <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-05-24</p> <p>... March; 5:30 p.m. to 7 p.m. (2) [Reserved] (b) Michigan Aerospace Challenge Sport Rocket Launch; Muskegon...) Location. All waters of the Fox River, near Voyageur Park, within the arc of a circle with a 500 foot... the Fox River, near the Western Lime Company 1.13 miles above the head of the Fox River, within the...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-07-13/pdf/2011-17635.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-07-13/pdf/2011-17635.pdf"><span>76 FR 41065 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> <span class="hlt">Events</span> Requiring Safety <span class="hlt">Zones</span> in the Captain of the Port Lake Michigan <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-07-13</p> <p>... Sport Rocket Launch; Muskegon, MI. (1) Location. All waters of Muskegon Lake, near the West Michigan... De Pere; De Pere, WI. (1) Location. All waters of the Fox River, near Voyageur Park, within the arc... waters of the Fox River, near the Western Lime Company 1.13 miles above the head of the Fox River, within...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-04-10/pdf/2012-8542.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-04-10/pdf/2012-8542.pdf"><span>77 FR 21439 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> <span class="hlt">Events</span> Requiring Safety <span class="hlt">Zones</span> in the Captain of the Port Lake Michigan <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-04-10</p> <p>... 7 p.m. (2) Michigan Aerospace Challenge Sport Rocket Launch; Muskegon, MI. (i) Location. All waters... Saturday of May; 8 a.m. to 5 p.m. (5) Celebrate De Pere; De Pere, WI. (i) Location. All waters of the Fox...; Green Bay, WI. (i) Location. All waters of the Fox River, near the Western Lime Company 1.13 miles above...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-05-12/pdf/2010-11265.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-05-12/pdf/2010-11265.pdf"><span>75 FR 26650 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> <span class="hlt">Events</span> Requiring Safety <span class="hlt">Zones</span> in the Captain of the Port Lake Michigan <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-05-12</p> <p>... at two locations: The Docket Management Facility (M-30), U.S. Department of Transportation, West... section 6(a)(3) of that Order. The Office of Management and Budget has not reviewed this rule under that... entities. The term ``small entities'' comprises small businesses, not-for-profit organizations that are...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-03-23/pdf/2010-6294.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-03-23/pdf/2010-6294.pdf"><span>75 FR 13707 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> <span class="hlt">Events</span> Requiring Safety <span class="hlt">Zones</span> in the Captain of the Port Lake Michigan <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-03-23</p> <p>...: Docket Management Facility (M-30), U.S. Department of Transportation, West Building Ground Floor, Room... the ``Keyword'' box. Click ``Search'' then click on the balloon shape in the ``Actions'' column. If... also visit the Docket Management Facility in Room W12-140 on the ground floor of the Department of...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005EP%26S...57..925S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005EP%26S...57..925S"><span>Izu detachment hypothesis: A proposal of a unified cause for the Miyake-Kozu <span class="hlt">event</span> and the Tokai slow <span class="hlt">event</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Seno, Tetsuzo</p> <p>2005-10-01</p> <p>Based on the fact that interseismic deformation of collision <span class="hlt">zones</span> is generally described by slip along a detachment at depth, I attempt to interpret the deformation of the Izu collision <span class="hlt">zone</span> in terms of a detachment model. The systematic deviation of the GPS velocities of the Izu Peninsula (Nov. 1998-June 2000) from the Philippine Sea-Eurasian relative plate motions is fitted by the slip on the detachment at a depth of 15-20 km with a rate of 3 cm/yr. On June 26, 2000, seismo-magmatic activity that started near Miyakejima expanded NW by 20 km close to Kozushima in association with dike intrusion over a few months. The horizontal movements associated with this <span class="hlt">event</span>, however, spread over wide areas in central Honshu. Simple dike intrusion models cannot explain these movements. To explain these, I hypothesize that a 20 cm of rapid slip occurred on the detachment at the time of this <span class="hlt">event</span>. The abnormal crustal movements in the Tokai-central Honshu-Kanto region then started after the <span class="hlt">event</span>. I propose that they represent delayed diffusive transfer of the slip on the detachment over surrounding low viscosity layers, such as nearby rupture <span class="hlt">zones</span> of great earthquakes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title49-vol1/pdf/CFR-2012-title49-vol1-sec71-2.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title49-vol1/pdf/CFR-2012-title49-vol1-sec71-2.pdf"><span>49 CFR 71.2 - <span class="hlt">Annual</span> advancement of standard time.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-10-01</p> <p>..., requires that the standard time of each State observing Daylight Saving Time shall be advanced 1 hour... 49 Transportation 1 2012-10-01 2012-10-01 false <span class="hlt">Annual</span> advancement of standard time. 71.2 Section 71.2 Transportation Office of the Secretary of Transportation STANDARD TIME <span class="hlt">ZONE</span> BOUNDARIES § 71.2...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title49-vol1/pdf/CFR-2014-title49-vol1-sec71-2.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title49-vol1/pdf/CFR-2014-title49-vol1-sec71-2.pdf"><span>49 CFR 71.2 - <span class="hlt">Annual</span> advancement of standard time.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-10-01</p> <p>..., requires that the standard time of each State observing Daylight Saving Time shall be advanced 1 hour... 49 Transportation 1 2014-10-01 2014-10-01 false <span class="hlt">Annual</span> advancement of standard time. 71.2 Section 71.2 Transportation Office of the Secretary of Transportation STANDARD TIME <span class="hlt">ZONE</span> BOUNDARIES § 71.2...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title49-vol1/pdf/CFR-2013-title49-vol1-sec71-2.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title49-vol1/pdf/CFR-2013-title49-vol1-sec71-2.pdf"><span>49 CFR 71.2 - <span class="hlt">Annual</span> advancement of standard time.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-10-01</p> <p>..., requires that the standard time of each State observing Daylight Saving Time shall be advanced 1 hour... 49 Transportation 1 2013-10-01 2013-10-01 false <span class="hlt">Annual</span> advancement of standard time. 71.2 Section 71.2 Transportation Office of the Secretary of Transportation STANDARD TIME <span class="hlt">ZONE</span> BOUNDARIES § 71.2...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title49-vol1/pdf/CFR-2011-title49-vol1-sec71-2.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title49-vol1/pdf/CFR-2011-title49-vol1-sec71-2.pdf"><span>49 CFR 71.2 - <span class="hlt">Annual</span> advancement of standard time.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-10-01</p> <p>..., requires that the standard time of each State observing Daylight Saving Time shall be advanced 1 hour... 49 Transportation 1 2011-10-01 2011-10-01 false <span class="hlt">Annual</span> advancement of standard time. 71.2 Section 71.2 Transportation Office of the Secretary of Transportation STANDARD TIME <span class="hlt">ZONE</span> BOUNDARIES § 71.2...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70193556','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70193556"><span>Ecological impacts of winter water level drawdowns on lake littoral <span class="hlt">zones</span>: A review</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Roy, Allison</p> <p>2017-01-01</p> <p>Freshwater littoral <span class="hlt">zones</span> harbor diverse ecological communities and serve numerous ecosystem functions that are controlled, in part, by natural water level fluctuations. However, human alteration of lake hydrologic regimes beyond natural fluctuations threaten littoral <span class="hlt">zone</span> ecological integrity. One type of hydrologic alteration in lakes is winter water level drawdowns, which are frequently employed for hydropower, flood control, and macrophyte control, among other purposes. Here, we synthesize the abiotic and biotic responses to <span class="hlt">annual</span> and novel winter water level drawdowns in littoral <span class="hlt">zones</span> of lakes and reservoirs. The dewatering, freezing, and increased erosion of exposed lakebeds drive changes in the littoral <span class="hlt">zone</span>. Shoreline-specific physicochemical conditions such as littoral slope and shoreline exposure further induce modifications. Loss of fine sediment decreases nutrient availability over time, but desiccation may promote a temporary nutrient pulse upon re-inundation. <span class="hlt">Annual</span> winter drawdowns can decrease taxonomic richness of macrophytes and benthic invertebrates and shift assemblage composition to favor taxa with r-selected life history strategies and with functional traits resistant to direct and indirect drawdown effects. Fish assemblages, though less directly affected by winter drawdowns (except where there is critically low dissolved oxygen), experience negative effects via indirect pathways like decreased food resources and spawning habitat. We identify eight general research gaps to guide future research that could improve our understanding about the complex effects of winter drawdowns on littoral <span class="hlt">zone</span> ecology.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/20945758','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/20945758"><span>Least-cost control of agricultural nutrient contributions to the Gulf of Mexico hypoxic <span class="hlt">zone</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Rabotyagov, Sergey; Campbell, Todd; Jha, Manoj; Gassman, Philip W; Arnold, Jeffrey; Kurkalova, Lyubov; Secchi, Silvia; Feng, Hongli; Kling, Catherine L</p> <p>2010-09-01</p> <p>In 2008, the hypoxic <span class="hlt">zone</span> in the Gulf of Mexico, measuring 20 720 km2, was one of the two largest reported since measurement of the <span class="hlt">zone</span> began in 1985. The extent of the hypoxic <span class="hlt">zone</span> is related to nitrogen and phosphorous loadings originating on agricultural fields in the upper Midwest. This study combines the tools of evolutionary computation with a water quality model and cost data to develop a trade-off frontier for the Upper Mississippi River Basin specifying the least cost of achieving nutrient reductions and the location of the agricultural conservation practices needed. The frontier allows policymakers and stakeholders to explicitly see the trade-offs between cost and nutrient reductions. For example, the cost of reducing <span class="hlt">annual</span> nitrate-N loadings by 30% is estimated to be US$1.4 billion/year, with a concomitant 36% reduction in P and the cost of reducing <span class="hlt">annual</span> P loadings by 30% is estimated to be US$370 million/year, with a concomitant 9% reduction in nitrate-N.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19930001003','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19930001003"><span>A late Devonian impact <span class="hlt">event</span> and its association with a possible extinction <span class="hlt">event</span> on Eastern Gondwana</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Wang, K.; Geldsetzer, H. H. J.</p> <p>1992-01-01</p> <p>Evidence from South China and Western Australia for a 365-Ma impact <span class="hlt">event</span> in the Lower crepida conodont <span class="hlt">zone</span> of the Famennian stage of the Late Devonian (about 1.5 Ma after the Frasnian/Famennian extinction <span class="hlt">event</span>) includes microtektitelike glassy microspherules, geochemical anomalies (including a weak Ir), a probable impact crater (greater than 70 k) at Taihu in South China, and an Ir anomaly in Western Australia. A brachiopod faunal turnover in South China, and the 'strangelove ocean'-like c-delta 13 excursions in both Chinese and Australian sections indicate that at least a regional-scale extinction might have occurred at the time of the impact. A paleoreconstruction shows that South China was very close to and facing Western Australia in the Late Devonian. The carbon isotopic excursions, which occur at the same stratigraphic level in both South China and Western Australia cannot be explained as being coincidental. The c-delta 13 excursions and the brachiopod faunal turnover in South China indicate that there might have been at least a regional (possibly global) extinction in the Lower crepida <span class="hlt">zone</span>. The impact-derived microspherules and geochemical anomalies (especially the Ir) indicate a Lower crepida <span class="hlt">zone</span> impact <span class="hlt">event</span> on eastern Gondwana. The location, type of target rocks, and possibly age of the Taihu Lake crater qualify as the probable site of this Late Devonian impact.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_12");'>12</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li class="active"><span>14</span></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_14 --> <div id="page_15" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li class="active"><span>15</span></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="281"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016ERL....11c5003W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016ERL....11c5003W"><span>Measurement of inter- and intra-<span class="hlt">annual</span> variability of landscape fire activity at a continental scale: the Australian case</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Williamson, Grant J.; Prior, Lynda D.; Jolly, W. Matt; Cochrane, Mark A.; Murphy, Brett P.; Bowman, David M. J. S.</p> <p>2016-03-01</p> <p>Climate dynamics at diurnal, seasonal and inter-<span class="hlt">annual</span> scales shape global fire activity, although difficulties of assembling reliable fire and meteorological data with sufficient spatio-temporal resolution have frustrated quantification of this variability. Using Australia as a case study, we combine data from 4760 meteorological stations with 12 years of satellite-derived active fire detections to determine day and night time fire activity, fire season start and end dates, and inter-<span class="hlt">annual</span> variability, across 61 objectively defined climate regions in three climate <span class="hlt">zones</span> (monsoon tropics, arid and temperate). We show that geographic patterns of landscape burning (onset and duration) are related to fire weather, resulting in a latitudinal gradient from the monsoon tropics in winter, through the arid <span class="hlt">zone</span> in all seasons except winter, and then to the temperate <span class="hlt">zone</span> in summer and autumn. Peak fire activity precedes maximum lightning activity by several months in all regions, signalling the importance of human ignitions in shaping fire seasons. We determined median daily McArthur forest fire danger index (FFDI50) for days and nights when fires were detected: FFDI50 varied substantially between climate <span class="hlt">zones</span>, reflecting effects of fire management in the temperate <span class="hlt">zone</span>, fuel limitation in the arid <span class="hlt">zone</span> and abundance of flammable grasses in the monsoon tropical <span class="hlt">zone</span>. We found correlations between the proportion of days when FFDI exceeds FFDI50 and the Southern Oscillation index across the arid <span class="hlt">zone</span> during spring and summer, and Indian Ocean dipole mode index across south-eastern Australia during summer. Our study demonstrates that Australia has a long fire weather season with high inter-<span class="hlt">annual</span> variability relative to all other continents, making it difficult to detect long term trends. It also provides a way of establishing robust baselines to track changes to fire seasons, and supports a previous conceptual model highlighting multi-temporal scale effects of climate in</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title19-vol2/pdf/CFR-2010-title19-vol2-sec146-23.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title19-vol2/pdf/CFR-2010-title19-vol2-sec146-23.pdf"><span>19 CFR 146.23 - Accountability for merchandise in a <span class="hlt">zone</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-04-01</p> <p>... or value and the records are made available for Customs review; (4) Beginning balance, cumulative... merchandise; and (6) Scrap, waste, and by-products. (c) Physical inventory. The operator shall take at least an <span class="hlt">annual</span> physical inventory of all merchandise in the <span class="hlt">zone</span> (unless continuous cycle counts are taken...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28320966','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28320966"><span>Tropical dead <span class="hlt">zones</span> and mass mortalities on coral reefs.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Altieri, Andrew H; Harrison, Seamus B; Seemann, Janina; Collin, Rachel; Diaz, Robert J; Knowlton, Nancy</p> <p>2017-04-04</p> <p>Degradation of coastal water quality in the form of low dissolved oxygen levels (hypoxia) can harm biodiversity, ecosystem function, and human wellbeing. Extreme hypoxic conditions along the coast, leading to what are often referred to as "dead <span class="hlt">zones</span>," are known primarily from temperate regions. However, little is known about the potential threat of hypoxia in the tropics, even though the known risk factors, including eutrophication and elevated temperatures, are common. Here we document an unprecedented hypoxic <span class="hlt">event</span> on the Caribbean coast of Panama and assess the risk of dead <span class="hlt">zones</span> to coral reefs worldwide. The <span class="hlt">event</span> caused coral bleaching and massive mortality of corals and other reef-associated organisms, but observed shifts in community structure combined with laboratory experiments revealed that not all coral species are equally sensitive to hypoxia. Analyses of global databases showed that coral reefs are associated with more than half of the known tropical dead <span class="hlt">zones</span> worldwide, with >10% of all coral reefs at elevated risk for hypoxia based on local and global risk factors. Hypoxic <span class="hlt">events</span> in the tropics and associated mortality <span class="hlt">events</span> have likely been underreported, perhaps by an order of magnitude, because of the lack of local scientific capacity for their detection. Monitoring and management plans for coral reef resilience should incorporate the growing threat of coastal hypoxia and include support for increased detection and research capacity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5389270','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5389270"><span>Tropical dead <span class="hlt">zones</span> and mass mortalities on coral reefs</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Altieri, Andrew H.; Harrison, Seamus B.; Seemann, Janina; Collin, Rachel; Diaz, Robert J.; Knowlton, Nancy</p> <p>2017-01-01</p> <p>Degradation of coastal water quality in the form of low dissolved oxygen levels (hypoxia) can harm biodiversity, ecosystem function, and human wellbeing. Extreme hypoxic conditions along the coast, leading to what are often referred to as “dead <span class="hlt">zones</span>,” are known primarily from temperate regions. However, little is known about the potential threat of hypoxia in the tropics, even though the known risk factors, including eutrophication and elevated temperatures, are common. Here we document an unprecedented hypoxic <span class="hlt">event</span> on the Caribbean coast of Panama and assess the risk of dead <span class="hlt">zones</span> to coral reefs worldwide. The <span class="hlt">event</span> caused coral bleaching and massive mortality of corals and other reef-associated organisms, but observed shifts in community structure combined with laboratory experiments revealed that not all coral species are equally sensitive to hypoxia. Analyses of global databases showed that coral reefs are associated with more than half of the known tropical dead <span class="hlt">zones</span> worldwide, with >10% of all coral reefs at elevated risk for hypoxia based on local and global risk factors. Hypoxic <span class="hlt">events</span> in the tropics and associated mortality <span class="hlt">events</span> have likely been underreported, perhaps by an order of magnitude, because of the lack of local scientific capacity for their detection. Monitoring and management plans for coral reef resilience should incorporate the growing threat of coastal hypoxia and include support for increased detection and research capacity. PMID:28320966</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.S23B0800S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.S23B0800S"><span>Dynamic Triggering of Seismic <span class="hlt">Events</span> and Their Relation to Slow Slip in Interior Alaska</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Sims, N. E.; Holtkamp, S. G.</p> <p>2017-12-01</p> <p>We conduct a search for dynamically triggered <span class="hlt">events</span> in the Minto Flats Fault <span class="hlt">Zone</span> (MFFZ), a left-lateral strike-slip <span class="hlt">zone</span> expressed as multiple, partially overlapping faults, in central Alaska. We focus on the MFFZ because we have observed slow slip processes (earthquake swarms and Very Low Frequency Earthquakes) and interaction between earthquake swarms and larger main-shock (MS) <span class="hlt">events</span> in this area before. We utilize the Alaska Earthquake Center catalog to identify potential earthquake swarms and dynamically triggered foreshock and mainshock <span class="hlt">events</span> along the fault <span class="hlt">zone</span>. We find 30 swarms occurring in the last two decades, five of which we classify as foreshock (FS) swarms due to their close proximity in both time and space to MS <span class="hlt">events</span>. Many of the earthquake swarms cluster around 15-20 km depth, which is near the seismic-aseismic transition along this fault <span class="hlt">zone</span>. Additionally, we observe instances of large teleseismic <span class="hlt">events</span> such as the M8.6 2012 Sumatra earthquake and M7.4 2012 Guatemala earthquake triggering seismic <span class="hlt">events</span> within the MFFZ, with the Sumatra earthquake triggering a mainshock <span class="hlt">event</span> that was preceded by an ongoing earthquake swarm and the Guatemala <span class="hlt">event</span> triggering earthquake swarms that subsequently transition into a larger mainshock <span class="hlt">event</span>. In both cases an earthquake swarm transitioned into a mainshock-aftershock <span class="hlt">event</span> and activity continued for several days after the teleseismic waves had passed, lending some evidence to delayed dynamic triggering of seismic <span class="hlt">events</span>. We hypothesize that large dynamic transient strain associated with the passage of teleseismic surface waves is triggering slow slip processes near the base of the seismogenic <span class="hlt">zone</span>. These triggered aseismic transient <span class="hlt">events</span> result in earthquake swarms, which sometimes lead to the nucleation of larger earthquakes. We utilize network matched filtering to build more robust catalogs of swarm earthquake families in this region to search for additional swarm-like or triggered activity in</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.T51J..07P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.T51J..07P"><span>Characterizing the structural maturity of fault <span class="hlt">zones</span> using high-resolution earthquake locations.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Perrin, C.; Waldhauser, F.; Scholz, C. H.</p> <p>2017-12-01</p> <p>We use high-resolution earthquake locations to characterize the three-dimensional structure of active faults in California and how it evolves with fault structural maturity. We investigate the distribution of aftershocks of several recent large earthquakes that occurred on immature faults (i.e., slow moving and small cumulative displacement), such as the 1992 (Mw7.3) Landers and 1999 (Mw7.1) Hector Mine <span class="hlt">events</span>, and earthquakes that occurred on mature faults, such as the 1984 (Mw6.2) Morgan Hill and 2004 (Mw6.0) Parkfield <span class="hlt">events</span>. Unlike previous studies which typically estimated the width of fault <span class="hlt">zones</span> from the distribution of earthquakes perpendicular to the surface fault trace, we resolve fault <span class="hlt">zone</span> widths with respect to the 3D fault surface estimated from principal component analysis of local seismicity. We find that the <span class="hlt">zone</span> of brittle deformation around the fault core is narrower along mature faults compared to immature faults. We observe a rapid fall off of the number of <span class="hlt">events</span> at a distance range of 70 - 100 m from the main fault surface of mature faults (140-200 m fault <span class="hlt">zone</span> width), and 200-300 m from the fault surface of immature faults (400-600 m fault <span class="hlt">zone</span> width). These observations are in good agreement with fault <span class="hlt">zone</span> widths estimated from guided waves trapped in low velocity damage <span class="hlt">zones</span>. The total width of the active <span class="hlt">zone</span> of deformation surrounding the main fault plane reach 1.2 km and 2-4 km for mature and immature faults, respectively. The wider <span class="hlt">zone</span> of deformation presumably reflects the increased heterogeneity in the stress field along complex and discontinuous faults strands that make up immature faults. In contrast, narrower deformation <span class="hlt">zones</span> tend to align with well-defined fault planes of mature faults where most of the deformation is concentrated. Our results are in line with previous studies suggesting that surface fault traces become smoother, and thus fault <span class="hlt">zones</span> simpler, as cumulative fault slip increases.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70017743','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70017743"><span>Detection of and response to a probable volcanogenic T-wave <span class="hlt">event</span> swarm on the western Blanco Transform Fault <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Dziak, R.P.; Fox, C.G.; Embley, R.W.; Lupton, J.E.; Johnson, G.C.; Chadwick, W.W.; Koski, R.A.</p> <p>1996-01-01</p> <p>The East Blanco Depression (EBD), a pull-apart basin within the western Blanco Transform Fault <span class="hlt">Zone</span> (BTFZ), was the site of an intense earthquake T-wave swarm that began at 1317Z on January 9, 1994. Although tectonically generated earthquakes occur frequently along the BTFZ, this swarm was unusual in that it was preceded and accompanied by periodic, low-frequency, long-duration acoustic signals, that originated from near the swarm epicenters. These tremor-like signals were very similar in character to acoustic energy produced by a shallow-submarine eruption near Socorro Island, a seamount several hundred km west of Baja, California. The ???69 earthquakes and ???400 tremor-like <span class="hlt">events</span> at the EBD occurred sporadically, with two periods of peak activity occurring between January 5-16 and 27-31. The swarm-like character of the earthquakes and the similarity of the tremor activity to the Socorro eruption indicated that the EBD was undergoing an intrusion or eruption episode. On January 27, six CTD/rosette casts were conducted at the site. Water samples from two of the stations yielded anomalous 3He concentrations, with maxima at ???2800 m depth over the main basin. In June 1994 two camera tows within the basin yielded evidence of pillow-lava volcanism and hydrothermal deposits, but no conclusive evidence of a recent seafloor eruption. In September 1994, deployments of the U.S. Navy's Advanced Tethered Vehicle resulted in the discovery of an active hydrothermal mound on the flanks of a pillow-lava volcano. The hydrothermal mound consists of Fe-rich hydrothermal precipitate and bacterial mats. Temperatures to 60??C were measured 30 cm below the surface. This is the first discovery of active hydrothermal vents along an oceanic fracture <span class="hlt">zone</span>. Although no conclusive evidence of volcanic activity associated with the T-wave <span class="hlt">event</span> swarm was found during these response efforts, the EBD has been the site of recent seafloor eruptions. Copyright 1996 by the American Geophysical</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4685810','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4685810"><span><span class="hlt">Annual</span> coral bleaching and the long-term recovery capacity of coral</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Schoepf, Verena; Grottoli, Andréa G.; Levas, Stephen J.; Aschaffenburg, Matthew D.; Baumann, Justin H.; Matsui, Yohei; Warner, Mark E.</p> <p>2015-01-01</p> <p>Mass bleaching <span class="hlt">events</span> are predicted to occur <span class="hlt">annually</span> later this century. Nevertheless, it remains unknown whether corals will be able to recover between <span class="hlt">annual</span> bleaching <span class="hlt">events</span>. Using a combined tank and field experiment, we simulated <span class="hlt">annual</span> bleaching by exposing three Caribbean coral species (Porites divaricata, Porites astreoides and Orbicella faveolata) to elevated temperatures for 2.5 weeks in 2 consecutive years. The impact of <span class="hlt">annual</span> bleaching stress on chlorophyll a, energy reserves, calcification, and tissue C and N isotopes was assessed immediately after the second bleaching and after both short- and long-term recovery on the reef (1.5 and 11 months, respectively). While P. divaricata and O. faveolata were able to recover from repeat bleaching within 1 year, P. astreoides experienced cumulative damage that prevented full recovery within this time frame, suggesting that repeat bleaching had diminished its recovery capacity. Specifically, P. astreoides was not able to recover protein and carbohydrate concentrations. As energy reserves promote bleaching resistance, failure to recover from <span class="hlt">annual</span> bleaching within 1 year will likely result in the future demise of heat-sensitive coral species. PMID:26582020</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005AGUFM.T14A..05C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005AGUFM.T14A..05C"><span>Periodic Viscous Shear Heating Instability in Fine-Grained Shear <span class="hlt">Zones</span>: Mechanism for Intermediate Depth Earthquakes</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Coon, E.; Kelemen, P.; Hirth, G.; Spiegelman, M.</p> <p>2005-12-01</p> <p> initial T of 600 to 850 C, this produced periodic viscous shear heating <span class="hlt">events</span> with periods of 100's to 1000's of years. Strain rates during these <span class="hlt">events</span> approach 1 per second as temperatures reach 1400. Cooling between <span class="hlt">events</span> returns the shear <span class="hlt">zone</span> almost to its initial temperature, though ultimately shear <span class="hlt">zone</span> temperature between <span class="hlt">events</span> exceeds 850 C resulting in stable viscous creep. Analysis shows that our system of equations jumps from one steady state to another, depending on a non-dimensional number relating the rate of shear heating to the rate of diffusive cooling. This year, Kelemen and Hirth show that the rate of stress drop during shear heating <span class="hlt">events</span> is greater than the rate of elastic stress relaxation, so that shear heating <span class="hlt">events</span> are a runaway instability. Rather than capping the temperature at 1400 C, we parameterize melt fraction as a function of T, and shear viscosity as a function of melt fraction. A problem with our 1D model is that predicted displacements are too large (1 to 20 m) during shear heating <span class="hlt">events</span>, essentially because there is no resistance at shear <span class="hlt">zone</span> ends. To address this, Coon and Spiegelman have embarked on a 3D model, incorporating a pre-existing fine-grained, tabular shear <span class="hlt">zone</span> of finite extent, with a visco-elastic rheology for both shear <span class="hlt">zone</span> and wall rocks. Preliminary 1D models using this approach show that the more complicated rheology yields the same result as the simpler model. We will present preliminary results, and determine the Maxwell time for this problem, since low strain rates could produce viscous relaxation in both shear <span class="hlt">zone</span> and wall rocks with negligible shear heating.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFMGC13E0820W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFMGC13E0820W"><span>Future Extreme <span class="hlt">Event</span> Vulnerability in the Rural Northeastern United States</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Winter, J.; Bowen, F. L.; Partridge, T.; Chipman, J. W.</p> <p>2017-12-01</p> <p>Future climate change impacts on humans will be determined by the convergence of evolving physical climate and socioeconomic systems. Of particular concern is the intersection of extreme <span class="hlt">events</span> and vulnerable populations. Rural areas of the Northeastern United States have experienced increased temperature and precipitation extremes, especially over the past three decades, and face unique challenges due to their physical isolation, natural resources dependent economies, and high poverty rates. To explore the impacts of future extreme <span class="hlt">events</span> on vulnerable, rural populations in the Northeast, we project extreme <span class="hlt">events</span> and vulnerability indicators to identify where changes in extreme <span class="hlt">events</span> and vulnerable populations coincide. Specifically, we analyze future (2046-2075) maximum <span class="hlt">annual</span> daily temperature, minimum <span class="hlt">annual</span> daily temperature, maximum <span class="hlt">annual</span> daily precipitation, and maximum consecutive dry day length for Representative Concentration Pathways (RCP) 4.5 and 8.5 using four global climate models (GCM) and a gridded observational dataset. We then overlay those projections with estimates of county-level population and relative income for 2060 to calculate changes in person-<span class="hlt">events</span> from historical (1976-2005), with a focus on Northeast counties that have less than 250,000 people and are in the bottom income quartile. We find that across the rural Northeast for RCP4.5, heat person-<span class="hlt">events</span> per year increase tenfold, far exceeding decreases in cold person-<span class="hlt">events</span> and relatively small changes in precipitation and drought person-<span class="hlt">events</span>. Counties in the bottom income quartile have historically (1976-2005) experienced a disproportionate number of heat <span class="hlt">events</span>, and counties in the bottom two income quartiles are projected to experience a greater heat <span class="hlt">event</span> increase by 2046-2075 than counties in the top two income quartiles. We further explore the relative contributions of <span class="hlt">event</span> frequency, population, and income changes to the total and geographic distribution of climate change</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..14...11Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..14...11Y"><span>Archaean and Palaeoproterozoic metamorphic <span class="hlt">events</span> in the Orekhov-Pavlograd compressional <span class="hlt">zone</span>, Ukrainian Shield</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yurchenko, A. V.</p> <p>2012-04-01</p> <p>The Orekhov-Pavlograd <span class="hlt">zone</span> (OPZ) is located between the Mesoarchaean-Neoarchaean Middle Dnieper Province and the Mesoarchaean-Palaeoproterozoic Azov Province in the eastern Ukrainian Shield. The OPZ consists of Archaean and Palaeoproterozoic high-grade metamorphic rocks. According U-Pb isotope analyses Archaean methaigneous rocks have age of 3.5-3.3 Ga, and latest AR <span class="hlt">events</span> dated form both individual grains and metamorphic rims in the tonalite and the granitic vein occurred at about 2.88 Ga ego. Paleoproterozoic zircons from a hornblende granulite have a concordia age of 2.08 Ga [1]. P-T conditions of the 3.5-3.3 Ga processes calculated from the Ti content in zircon are of 730-760°C. Metamorphic <span class="hlt">event</span> dated as 2.88 Ga is more preserved and detected in some amphibolites after mafic dykes. According to different methods of hornblende-plagioclase geothermometry along with Al- and Ti-geobarometry of hornblende, the amphibolites have formed at temperature of 735-749 °C and pressure of 5.2 to 7.8 kbar. P-T conditions of Paleoproterozoic metamorphic processes have been calculated for a Paleoproterozoic high-Al paragneiss and mafic rocks. On the base of the computer software THERIAK-DOMINO [2], near-isothermal decompression from ca. 8.5 to 6.0 kbar at 650 °C and then to 5.8 kbar at 740 °C has been determined for small irregular garnet grains (grs 4-7% and XMg 0.36-0.37) associated with the same biotite and plagioclase. P-T conditions obtained by means of the P-T pseudosection calculation are identical within errors to those defined by the Grt + Bt + Pl + Ozt geothermometer by [3] and the geobarometer by [4], T = 675 °C and P = 5.6 kbar. Temperature and pressure calculated for assemblage Grt-Pl-Opx-Amph-Ilm-Ru (mafic rock) by using the TWEEQU method shows: 1) high values of pressure and temperature (ca. 7 kbar and 800 °C) are linked with the first metamorphic <span class="hlt">event</span> with Opx-Cpx assemblage, 2) moderate values (ca. 5 kbar and ca. 600 °C) are referred to the second</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.S31A2712C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.S31A2712C"><span>Investigation of complex slow slip behavior along the Hikurangi subduction <span class="hlt">zone</span> with earthquake simulator RSQSim</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Colella, H.; Ellis, S. M.; Williams, C. A.</p> <p>2015-12-01</p> <p>The Hikurangi subduction <span class="hlt">zone</span> (New Zealand) is one of many subudction <span class="hlt">zones</span> that exhibit slow slip behavior. Geodetic observations along the Hikurangi subduction <span class="hlt">zone</span> are unusual in that not only does the subduction <span class="hlt">zone</span> exhibit periodic slow slip <span class="hlt">events</span> at "typical" subduction-<span class="hlt">zone</span> depths of 25-50 km along the southern part of the margin, but also much shallower depths of 8-15 km along the northern part of the margin. Furthermore, there is evidence for interplay between slow slip <span class="hlt">events</span> at these different depth ranges (between the deep and shallow <span class="hlt">events</span>) along the central part of the margin, and some of the slow slip behavior is observed along regions of the interface that were previously considered locked, which raises questions about the slip behavior of this region. This study employs the earthquake simulator, RSQSim, to explore variations in the effective normal stress (i.e., stress after the addition of pore fluid pressures) and the frictional instability necessary to generate the complex slow slip <span class="hlt">events</span> observed along the Hikurangi margin. Preliminary results suggest that to generate slow slip <span class="hlt">events</span> with similar recurrence intervals to those observed the effective normal stress (MPa) is 3x higher in the south than the north, 6-9MPa versus 2-3MPa, respectively. Results also suggest that, at a minimum, that some overlap along the central margin must exist between the slow slip sections in the north and south to reproduce the types of slip <span class="hlt">events</span> observed along the Hikurangi subduction <span class="hlt">zone</span>. To further validate the results from the simulations, Okada solutions for surface displacements will be compared to geodetic solution to more accurately constrain the areas in which slip behavior varies and the cause(s) for the variation(s).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-08-22/pdf/2012-20698.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-08-22/pdf/2012-20698.pdf"><span>77 FR 50593 - Safety <span class="hlt">Zone</span>; Seafood Festival Fireworks Display, Marquette, MI</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-08-22</p> <p>...-AA00 Safety <span class="hlt">Zone</span>; Seafood Festival Fireworks Display, Marquette, MI AGENCY: Coast Guard, DHS. ACTION... the <span class="hlt">Annual</span> Marquette Seafood Festival. The Captain of the Port, Sector Sault Sainte Marie, has determined that the Marquette Seafood Festival Fireworks Display will pose significant risks to the public...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/17378','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/17378"><span>Rail-trails and special <span class="hlt">events</span>: community and economic benefits</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Charles Nelson; Christine Vogt; Joel Lynch; Daniel Stynes</p> <p>2002-01-01</p> <p>This paper discusses community and economic benefits associated with two recreational bicycle special <span class="hlt">events</span> held on the Pere Marquette Rail-Trail (PMRT) in Midland County Michigan during the summer of 1999. One <span class="hlt">event</span> was an <span class="hlt">annual</span> ride to fundraise for the Rails to Trails Conservancy of Michigan. Approximately 1,800 participants rode in the <span class="hlt">event</span> which included two...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3929565','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3929565"><span>Surviving Coral Bleaching <span class="hlt">Events</span>: Porites Growth Anomalies on the Great Barrier Reef</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Cantin, Neal E.; Lough, Janice M.</p> <p>2014-01-01</p> <p>Mass coral bleaching affected large parts of the Great Barrier Reef (GBR) in 1998 and 2002. In this study, we assessed if signatures of these major thermal stress <span class="hlt">events</span> were recorded in the growth characteristics of massive Porites colonies. In 2005 a suite of short (<50 cm) cores were collected from apparently healthy, surviving Porites colonies, from reefs in the central GBR (18–19°S) that have documented observations of widespread bleaching. Sites included inshore (Nelly Bay, Pandora Reef), <span class="hlt">annually</span> affected by freshwater flood <span class="hlt">events</span>, midshelf (Rib Reef), only occasionally affected by freshwater floods and offshore (Myrmidon Reef) locations primarily exposed to open ocean conditions. <span class="hlt">Annual</span> growth characteristics (extension, density and calcification) were measured in 144 cores from 79 coral colonies and analysed over the common 24-year period, 1980–2003. Visual examination of the <span class="hlt">annual</span> density bands revealed growth hiatuses associated with the bleaching years in the form of abrupt decreases in <span class="hlt">annual</span> linear extension rates, high density stress bands and partial mortality. The 1998 mass-bleaching <span class="hlt">event</span> reduced Porites calcification by 13 and 18% on the two inshore locations for 4 years, followed by recovery to baseline calcification rates in 2002. Evidence of partial mortality was apparent in 10% of the offshore colonies in 2002; however no significant effects of the bleaching <span class="hlt">events</span> were evident in the calcification rates at the mid shelf and offshore sites. These results highlight the spatial variation of mass bleaching <span class="hlt">events</span> and that all reef locations within the GBR were not equally stressed by the 1998 and 2002 mass bleaching <span class="hlt">events</span>, as some models tend to suggest, which enabled recovery of calcification on the GBR within 4 years. The dynamics in <span class="hlt">annual</span> calcification rates and recovery displayed here should be used to improve model outputs that project how coral calcification will respond to ongoing warming of the tropical oceans. PMID:24586377</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24586377','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24586377"><span>Surviving coral bleaching <span class="hlt">events</span>: porites growth anomalies on the Great Barrier Reef.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Cantin, Neal E; Lough, Janice M</p> <p>2014-01-01</p> <p>Mass coral bleaching affected large parts of the Great Barrier Reef (GBR) in 1998 and 2002. In this study, we assessed if signatures of these major thermal stress <span class="hlt">events</span> were recorded in the growth characteristics of massive Porites colonies. In 2005 a suite of short (<50 cm) cores were collected from apparently healthy, surviving Porites colonies, from reefs in the central GBR (18-19°S) that have documented observations of widespread bleaching. Sites included inshore (Nelly Bay, Pandora Reef), <span class="hlt">annually</span> affected by freshwater flood <span class="hlt">events</span>, midshelf (Rib Reef), only occasionally affected by freshwater floods and offshore (Myrmidon Reef) locations primarily exposed to open ocean conditions. <span class="hlt">Annual</span> growth characteristics (extension, density and calcification) were measured in 144 cores from 79 coral colonies and analysed over the common 24-year period, 1980-2003. Visual examination of the <span class="hlt">annual</span> density bands revealed growth hiatuses associated with the bleaching years in the form of abrupt decreases in <span class="hlt">annual</span> linear extension rates, high density stress bands and partial mortality. The 1998 mass-bleaching <span class="hlt">event</span> reduced Porites calcification by 13 and 18% on the two inshore locations for 4 years, followed by recovery to baseline calcification rates in 2002. Evidence of partial mortality was apparent in 10% of the offshore colonies in 2002; however no significant effects of the bleaching <span class="hlt">events</span> were evident in the calcification rates at the mid shelf and offshore sites. These results highlight the spatial variation of mass bleaching <span class="hlt">events</span> and that all reef locations within the GBR were not equally stressed by the 1998 and 2002 mass bleaching <span class="hlt">events</span>, as some models tend to suggest, which enabled recovery of calcification on the GBR within 4 years. The dynamics in <span class="hlt">annual</span> calcification rates and recovery displayed here should be used to improve model outputs that project how coral calcification will respond to ongoing warming of the tropical oceans.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-05-26/pdf/2011-13036.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-05-26/pdf/2011-13036.pdf"><span>76 FR 30584 - Safety <span class="hlt">Zones</span>; Eleventh Coast Guard District <span class="hlt">Annual</span> Fireworks <span class="hlt">Events</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-05-26</p> <p>.... 2. LA County Dept of Beach and Harbors 4th of July Fireworks Sponsor Los Angeles, CA County Dept of... waters of the Sea Cliff State Beach Pier. 27. Rio Vista Bass Derby Fireworks Sponsor Rio Vista Chamber of... Vista, CA waterfront. Regulated Area 100-foot radius around the fireworks launch barge during the...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-07-24/pdf/2013-17677.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-07-24/pdf/2013-17677.pdf"><span>78 FR 44433 - Safety <span class="hlt">Zone</span>; Metedeconk River; Brick Township, NJ</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-07-24</p> <p>...-AA00 Safety <span class="hlt">Zone</span>; Metedeconk River; Brick Township, NJ AGENCY: Coast Guard, DHS. ACTION: Temporary... recurring fireworks <span class="hlt">event</span> held in the Metedeconk River in Brick Township, NJ. The fireworks display is... for the Metedeconk River, Brick Township, NJ Safety <span class="hlt">Zone</span> will be added from 6:30 p.m. until 10 p.m. on...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-07-03/pdf/2013-16064.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-07-03/pdf/2013-16064.pdf"><span>78 FR 39992 - Safety <span class="hlt">Zone</span>; Feast of Lanterns Fireworks Display, Pacific Grove, CA</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-07-03</p> <p>...-AA00 Safety <span class="hlt">Zone</span>; Feast of Lanterns Fireworks Display, Pacific Grove, CA AGENCY: Coast Guard, DHS... <span class="hlt">zone</span> in the navigable waters near Lover's Point Park in the Pacific Grove, CA in support of The Feast of Lanterns Fireworks <span class="hlt">Event</span> on July 27, 2013. This safety <span class="hlt">zone</span> is established to ensure the safety of...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009EGUGA..1113394V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009EGUGA..1113394V"><span>Monitoring of thermal regime of permafrost in the coastal <span class="hlt">zone</span> of Western Yamal</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Vasiliev, A.</p> <p>2009-04-01</p> <p>Data on thermal regime of permafrost are required for estimation of the climate change influence on permafrost dynamics. Monitoring of thermal regime of permafrost was arranged in the area of weather station "Marre-Sale", western Yamal. In terms of geomorphology, the area of our observations belongs to the second and third marine terraces; the surface of these terraces has been partly modified by recent cryogenic processes. The elevation varies from 10 to 30 m a.s.l. Marine clays lie at the base of the geological section of the coastal deposits. Their upper part was eroded and uneven surface of marine sediments is overlain by continental sandy sediments. Marine clays are saline. In the southern part of study area, low accumulative islands are forming. Their heights above sea level do not exceed 0.5 meters, and during high tides their surface is covered by sea water. The sediments accumulating at these islands are saline silty clays. Western Yamal region is located within continuous permafrost <span class="hlt">zone</span> with thickness of 150 to 200 meters. Study of thermal regime in the on-shore <span class="hlt">zone</span> has been performed since 1979 using the 10-12-m-deep boreholes. In 2007, five boreholes were included in the work program of the Thermal State of Permafrost (TSP) project developed as a part of IPY scientific activities. According to TSP program, temperature sensors were installed at depths 2, 3, 5, and 10 meters; measurements have been performed every six hours. In this presentation, results of our observations related to climate change are discussed. For different terrain units, increase of mean <span class="hlt">annual</span> permafrost temperature during the last 30 years has reached 0.6 to 1.5 deg. C. In the transit <span class="hlt">zone</span>, monitoring of thermal regime have been performed since 2006. Sensors were installed at depths 0, 0.25, 0.6, 0.75, 1.25, 1.75, and 2.25 meters. The active layer depth here reaches 1.9 meters, thus the 2.25-m-sensor is located within permafrost. Monitoring data show the sharp increase in mean</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_13");'>13</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li class="active"><span>15</span></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_15 --> <div id="page_16" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li class="active"><span>16</span></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="301"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..1616675H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..1616675H"><span>The 1945 Balochistan earthquake and probabilistic tsunami hazard assessment for the Makran subduction <span class="hlt">zone</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Höchner, Andreas; Babeyko, Andrey; Zamora, Natalia</p> <p>2014-05-01</p> <p>Iran and Pakistan are countries quite frequently affected by destructive earthquakes. For instance, the magnitude 6.6 Bam earthquake in 2003 in Iran with about 30'000 casualties, or the magnitude 7.6 Kashmir earthquake 2005 in Pakistan with about 80'000 casualties. Both <span class="hlt">events</span> took place inland, but in terms of magnitude, even significantly larger <span class="hlt">events</span> can be expected to happen offshore, at the Makran subduction <span class="hlt">zone</span>. This small subduction <span class="hlt">zone</span> is seismically rather quiescent, but a tsunami caused by a thrust <span class="hlt">event</span> in 1945 (Balochistan earthquake) led to about 4000 casualties. Nowadays, the coastal regions are more densely populated and vulnerable to similar <span class="hlt">events</span>. Additionally, some recent publications raise the question of the possiblity of rare but huge magnitude 9 <span class="hlt">events</span> at the Makran subduction <span class="hlt">zone</span>. We first model the historic Balochistan <span class="hlt">event</span> and its effect in terms of coastal wave heights, and then generate various synthetic earthquake and tsunami catalogs including the possibility of large <span class="hlt">events</span> in order to asses the tsunami hazard at the affected coastal regions. Finally, we show how an effective tsunami early warning could be achieved by the use of an array of high-precision real-time GNSS (Global Navigation Satellite System) receivers along the coast.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-08-30/pdf/2013-21171.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-08-30/pdf/2013-21171.pdf"><span>78 FR 53671 - Regulated Navigation Areas, Security <span class="hlt">Zones</span>: Dignitary Arrival/Departure and United Nations...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-08-30</p> <p>... security <span class="hlt">zones</span>. We are reorganizing Sec. 165.164 and adding descriptive designations to name each of the... evaluates these actions <span class="hlt">annually</span> and rates each agency's responsiveness to small business. If you wish to...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1913875B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1913875B"><span>An <span class="hlt">annually</span> resolved marine proxy record for the 8.2K cold <span class="hlt">event</span> from the northern North Sea based on bivalve shells</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Butler, Paul; Estrella-Martínez, Juan; Scourse, James</p> <p>2017-04-01</p> <p>The so-called 8.2K cold <span class="hlt">event</span> is a rapid cooling of about 6° +/- 2° recorded in the Greenland ice core record and thought to be a consequence of a freshwater pulse from the Laurentide ice sheet which reduced deepwater formation in the North Atlantic. In the Greenland ice cores the <span class="hlt">event</span> is characterized by a maximum extent of 159 years and a central <span class="hlt">event</span> lasting for 70 years. As discussed by Thomas et al (QSR, 2007), the low resolution and dating uncertainty of much palaeoclimate data makes it difficult to determine the rates of change and causal sequence that characterise the <span class="hlt">event</span> at different locations. We present here a bivalve shell chronology based on four shells of Arctica islandica from the northern North Sea which (within radiocarbon uncertainty) is coeval with the 8.2K <span class="hlt">event</span> recorded in the Greenland ice cores. The years of death of each shell based on radiocarbon analysis and crossmatching are 8094, 8134, 8147, and 8208 yrs BP (where "present" = AD 1950), with an associated radiocarbon uncertainty of +/-80 yrs, and their longevities are 106, 122, 112 and 79 years respectively. The total length of the chronology is 192 years (8286 - 8094 BP +/- 80 yrs). The most noticeable feature of the chronology is an 60-year period of increasing growth which may correspond to a similar period of decreasing ice accumulation in the GRIP (central Greenland) ice core record. We tentatively suggest that this reflects increasing food supply to the benthos as summer stratification is weakened by colder seawater temperatures. Stable isotope analyses (results expected to be available when this abstract is presented), will show changes at <span class="hlt">annual</span> and seasonal resolution, potentially giving a very detailed insight into the causal factors associated with the 8.2K <span class="hlt">event</span> and its impact in the northern North Sea.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=APA&pg=3&id=EJ769787','ERIC'); return false;" href="https://eric.ed.gov/?q=APA&pg=3&id=EJ769787"><span>2006 <span class="hlt">Annual</span> Report of the American Psychological Association</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Anderson, Norman B.</p> <p>2007-01-01</p> <p>This report is designed to keep you up-to-date on APA's priorities, ongoing activities, and <span class="hlt">annual</span> special <span class="hlt">events</span>. This issue contains APA Directorate reports, the President's report, and the Treasurer's report.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=230835','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=230835"><span>Standardized Analytical Methods for Environmental Restoration Following Homeland Security <span class="hlt">Events</span></span></a></p> <p><a target="_blank" href="https://www.ars.usda.gov/research/publications/find-a-publication/">USDA-ARS?s Scientific Manuscript database</a></p> <p></p> <p></p> <p>Methodology was formulated for use in the <span class="hlt">event</span> of a terrorist attack using a variety of chemical, radioactive, biological, and toxic agents. Standardized analysis procedures were determined for use should these <span class="hlt">events</span> occur. This publication is <span class="hlt">annually</span> updated....</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFM.T13F2680H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFM.T13F2680H"><span>Areas of slip of recent earthquakes in the Mexican subduction <span class="hlt">zone</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Hjorleifsdottir, V.; Sánchez-Reyes, H. S.; Singh, S.; Ji, C.; Iglesias, A.; Perez-Campos, X.</p> <p>2012-12-01</p> <p>The Mexican subduction <span class="hlt">zone</span> is unusual: the width of the seismogenic <span class="hlt">zone</span> is relatively narrow and a large portion of the co-seismic slip generally occurs below the coast, ~ 45 to 80 km from the trench. The earthquake recurrence interval is relatively short and almost the entire length of the <span class="hlt">zone</span> has experienced a large (Mw≥7.4) earthquake in the last 100 years (Singh et al., 1981). In this study we present detailed analysis of the areas of significant slip during several recent (last 20 years) large earthquakes in the Mexican subduction <span class="hlt">zone</span>. The most recent earthquake of 20 March 2012 (Mw7.4) occurred near the Guerrero/Oaxaca border. The slip was concentrated on the plate interface below land and the epicentral PGAs ranged between 0.2 and 0.7g. The updip portion of the plate interface had previously broken during the 25 Feb 1996 earthquake (Mw7.1), which was a slow earthquake and produced anomalously low PGAs (Iglesias et al., 2003). This indicates that in this region the area close to the trench is at least partially locked, with some earthquakes breaking the down-dip portion of the interface and others rupturing the up-dip portion. The Jalisco/Colima segment of the subduction <span class="hlt">zone</span> seems to behave in a similar fashion. The 9 October 1995 (Mw 8.0) earthquake generated small accelerations relative to its size. The energy to moment ratio, E0/M0, is 4.2e-6 (Pérez-Campos, Singh and Beroza, 2003), a value similar to the Feb, 1996 earthquake. This value is low compared to other thrust <span class="hlt">events</span> in the region. The earthquake also had the largest (Ms-Mw) disparity along the Mexican subduction <span class="hlt">zone</span>, 7.4 vs 8.0. The <span class="hlt">event</span> produced relatively large tsunami. On the contrary, the 3 June 1932 earthquake (Ms8.2, Mw8.0), that is believed to have broken the same segment of the subduction <span class="hlt">zone</span>, appears to be "normal." Based on the available evidence, it may be concluded that the 1932 <span class="hlt">event</span> broke a deeper patch of the plate interface relative to the 1995 <span class="hlt">event</span>. The mode of rupture</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016PhDT........77F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016PhDT........77F"><span>Effects of a significant New Madrid Seismic <span class="hlt">Zone</span> <span class="hlt">event</span> on oil and natural gas pipelines and their cascading effects to critical infrastructures</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fields, Damon E.</p> <p></p> <p>Critical Infrastructure Protection (CIP) is a construct that relates preparedness and responsiveness to natural or man-made disasters that involve vulnerable assets deemed essential for the functioning of our economy and society. Infrastructure systems (power grids, bridges, airports, etc.) are vulnerable to disastrous types of <span class="hlt">events</span>--natural or man-made. Failures of these systems can have devastating effects on communities and entire regions. CIP relates our willingness, ability, and capability to defend, mitigate, and re-constitute those assets that succumb to disasters affecting one or more infrastructure sectors. This qualitative research utilized ethnography and employed interviews with subject matter experts (SMEs) from various fields of study regarding CIP with respect to oil and natural gas pipelines in the New Madrid Seismic <span class="hlt">Zone</span>. The study focused on the research question: What can be done to mitigate vulnerabilities in the oil and natural gas infrastructures, along with the potential cascading effects to interdependent systems, associated with a New Madrid fault <span class="hlt">event</span>? The researcher also analyzed National Level Exercises (NLE) and real world <span class="hlt">events</span>, and associated After Action Reports (AAR) and Lessons Learned (LL) in order to place a holistic lens across all infrastructures and their dependencies and interdependencies. Three main themes related to the research question emerged: (a) preparedness, (b) mitigation, and (c) impacts. These themes comprised several dimensions: (a) redundancy, (b) node hardening, (c) education, (d) infrastructure damage, (e) cascading effects, (f) interdependencies, (g) exercises, and (h) earthquake readiness. As themes and dimensions are analyzed, they are considered against findings in AARs and LL from previous real world <span class="hlt">events</span> and large scale exercise <span class="hlt">events</span> for validation or rejection.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26582020','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26582020"><span><span class="hlt">Annual</span> coral bleaching and the long-term recovery capacity of coral.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Schoepf, Verena; Grottoli, Andréa G; Levas, Stephen J; Aschaffenburg, Matthew D; Baumann, Justin H; Matsui, Yohei; Warner, Mark E</p> <p>2015-11-22</p> <p>Mass bleaching <span class="hlt">events</span> are predicted to occur <span class="hlt">annually</span> later this century. Nevertheless, it remains unknown whether corals will be able to recover between <span class="hlt">annual</span> bleaching <span class="hlt">events</span>. Using a combined tank and field experiment, we simulated <span class="hlt">annual</span> bleaching by exposing three Caribbean coral species (Porites divaricata, Porites astreoides and Orbicella faveolata) to elevated temperatures for 2.5 weeks in 2 consecutive years. The impact of <span class="hlt">annual</span> bleaching stress on chlorophyll a, energy reserves, calcification, and tissue C and N isotopes was assessed immediately after the second bleaching and after both short- and long-term recovery on the reef (1.5 and 11 months, respectively). While P. divaricata and O. faveolata were able to recover from repeat bleaching within 1 year, P. astreoides experienced cumulative damage that prevented full recovery within this time frame, suggesting that repeat bleaching had diminished its recovery capacity. Specifically, P. astreoides was not able to recover protein and carbohydrate concentrations. As energy reserves promote bleaching resistance, failure to recover from <span class="hlt">annual</span> bleaching within 1 year will likely result in the future demise of heat-sensitive coral species. © 2015 The Author(s).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://images.nasa.gov/#/details-KSC-03pd2178.html','SCIGOVIMAGE-NASA'); return false;" href="https://images.nasa.gov/#/details-KSC-03pd2178.html"><span>KENNEDY SPACE CENTER, FLA. - Children enjoy a hands-on display of security equipment during Take Our Children to Work Day. Employees were invited to share their work experience with their children on this <span class="hlt">annual</span> <span class="hlt">event</span>.</span></a></p> <p><a target="_blank" href="https://images.nasa.gov/">NASA Image and Video Library</a></p> <p></p> <p>2003-07-24</p> <p>KENNEDY SPACE CENTER, FLA. - Children enjoy a hands-on display of security equipment during Take Our Children to Work Day. Employees were invited to share their work experience with their children on this <span class="hlt">annual</span> <span class="hlt">event</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol2/pdf/CFR-2013-title33-vol2-sec165-929.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol2/pdf/CFR-2013-title33-vol2-sec165-929.pdf"><span>33 CFR 165.929 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> <span class="hlt">events</span> requiring safety <span class="hlt">zones</span> in the Captain of the Port Lake Michigan <span class="hlt">zone</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-07-01</p> <p>... Aerospace Challenge Sport Rocket Launch; Muskegon, MI—(i) Location. All waters of Muskegon Lake, near the...) Celebrate De Pere; De Pere, WI—(i) Location. All waters of the Fox River, near Voyageur Park, within the arc...) International Bayfest; Green Bay, WI—(i) Location. All waters of the Fox River, near the Western Lime Company 1...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec165-929.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec165-929.pdf"><span>33 CFR 165.929 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> <span class="hlt">events</span> requiring safety <span class="hlt">zones</span> in the Captain of the Port Lake Michigan <span class="hlt">zone</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... Aerospace Challenge Sport Rocket Launch; Muskegon, MI. (i) Location. All waters of Muskegon Lake, near the... Pere, WI. (i) Location. All waters of the Fox River, near Voyageur Park, within the arc of a circle... Bayfest; Green Bay, WI. (i) Location. All waters of the Fox River, near the Western Lime Company 1.13...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec165-929.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec165-929.pdf"><span>33 CFR 165.929 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> <span class="hlt">events</span> requiring safety <span class="hlt">zones</span> in the Captain of the Port Lake Michigan <span class="hlt">zone</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-07-01</p> <p>... Challenge Sport Rocket Launch Muskegon, MI. All waters of Muskegon Lake, near the West Michigan Dock and... 5 p.m. (4) Celebrate De Pere De Pere, WI. All waters of the Fox River, near Voyageur Park, within...) International Bayfest Green Bay, WI. All waters of the Fox River, near the Western Lime Company 1.13 miles above...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec165-929.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec165-929.pdf"><span>33 CFR 165.929 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> <span class="hlt">events</span> requiring safety <span class="hlt">zones</span> in the Captain of the Port Lake Michigan <span class="hlt">zone</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... Aerospace Challenge Sport Rocket Launch; Muskegon, MI—(i) Location. All waters of Muskegon Lake, near the... Pere, WI—(i) Location. All waters of the Fox River, near Voyageur Park, within the arc of a circle with...) Location. All waters of the Fox River, near the Western Lime Company 1.13 miles above the head of the Fox...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol2/pdf/CFR-2010-title33-vol2-sec165-929.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol2/pdf/CFR-2010-title33-vol2-sec165-929.pdf"><span>33 CFR 165.929 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> <span class="hlt">events</span> requiring safety <span class="hlt">zones</span> in the Captain of the Port Lake Michigan <span class="hlt">zone</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... and time. The last Saturday of April; 8 a.m. to 4 p.m. (3) Tulip Time Festival Fireworks; Holland, MI....m. to 11 p.m. (9) Harborfest Music and Family Festival; Racine, WI—(i) Location. All waters of Lake... 11 p.m. each day. (10) Jordan Valley Freedom Festival Fireworks; East Jordan, MI—(i) Location. All...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70182184','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70182184"><span>Critical <span class="hlt">zone</span> properties control the fate of nitrogen during experimental rainfall in montane forests of the Colorado Front Range</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Hinckley, Eve-Lyn S.; Ebel, Brian A.; Barnes, Rebecca T.; Murphy, Sheila F.; Anderson, Suzanne P.</p> <p>2017-01-01</p> <p>Several decades of research in alpine ecosystems have demonstrated links among the critical <span class="hlt">zone</span>, hydrologic response, and the fate of elevated atmospheric nitrogen (N) deposition. Less research has occurred in mid-elevation forests, which may be important for retaining atmospheric N deposition. To explore the fate of N in the montane <span class="hlt">zone</span>, we conducted plot-scale experimental rainfall <span class="hlt">events</span> across a north–south transect within a catchment of the Boulder Creek Critical <span class="hlt">Zone</span> Observatory. Rainfall <span class="hlt">events</span> mimicked relatively common storms (20–50% <span class="hlt">annual</span> exceedance probability) and were labeled with 15N-nitrate (NO3−">NO−3NO3−) and lithium bromide tracers. For 4 weeks, we measured soil–water and leachate concentrations of Br−, 15NO3−,">15NO−3,15NO3−, and NO3−">NO−3NO3− daily, followed by recoveries of 15N species in bulk soils and microbial biomass. Tracers moved immediately into the subsurface of north-facing slope plots, exhibiting breakthrough at 10 and 30 cm over 22 days. Conversely, little transport of Br− or 15NO3−">15NO−315NO3− occurred in south-facing slope plots; tracers remained in soil or were lost via pathways not measured. Hillslope position was a significant determinant of soil 15N-NO3−">NO−3NO3− recoveries, while soil depth and time were significant determinants of 15N recovery in microbial biomass. Overall, 15N recovery in microbial biomass and leachate was greater in upper north-facing slope plots than lower north-facing (toeslope) and both south-facing slope plots in August; by October, 15N recovery in microbial N biomass within south-facing slope plots had increased substantially. Our results point to the importance of soil properties in controlling the fate of N in mid-elevation forests during the summer season.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19920007754','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19920007754"><span>Marshall Space Flight Center 1990 <span class="hlt">annual</span> chronology of <span class="hlt">events</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Wright, Michael</p> <p>1991-01-01</p> <p>A chronological listing is provided of the major <span class="hlt">events</span> for the Marshall Space Flight Center for the calendar year 1990. The MSFC Historian, Management Operations Office, compiled the chronology from various sources and from supplemental information provided by the major MSFC organizations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://hdl.handle.net/2060/19940015013','NASA-TRS'); return false;" href="http://hdl.handle.net/2060/19940015013"><span>Marshall Space Flight Center 1989 <span class="hlt">annual</span> chronology of <span class="hlt">events</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Wright, Michael</p> <p>1990-01-01</p> <p>A chronological listing of the major <span class="hlt">events</span> for the Marshall Space Flight Center for the calendar year 1989 is provided. The MSFC Historian, Management Operations Office, compiled the chronology from various sources and from supplemental information provided by the major MSFC organizations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA279847','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA279847"><span>The Novaya Zemlya <span class="hlt">Event</span> of 31 December 1992 and Seismic Identification Issues: <span class="hlt">Annual</span> Seismic Research Symposium (15th) Held in Vail, Colorado on 8-10 September 1993</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>1993-09-10</p> <p>1993). A bootstrap generalizedlikelihood ratio test in discriminant analysis, Proc. 15th <span class="hlt">Annual</span> Seismic Research Symposium, in press. I Hedlin, M., J... ratio indicate that the <span class="hlt">event</span> does not belong to the first class. The bootstrap technique is used here as well to set the critical value of the test ...Methodist University. Baek, J., H. L. Gray, W. A. Woodward and M.D. Fisk (1993). A Bootstrap Generalized Likelihood Ratio Test in Discriminant</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-02-25/pdf/2010-3834.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-02-25/pdf/2010-3834.pdf"><span>75 FR 8563 - Safety <span class="hlt">Zone</span>; Fleet Week Maritime Festival, Pier 66, Elliott Bay, Seattle, WA</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-02-25</p> <p>...-AA00 Safety <span class="hlt">Zone</span>; Fleet Week Maritime Festival, Pier 66, Elliott Bay, Seattle, WA AGENCY: Coast Guard... Fleet Week Maritime Festival. Entry into, transit through, mooring, or anchoring within these <span class="hlt">zones</span> is... Fleet Week Maritime Festival. This safety <span class="hlt">zone</span> is necessary as these <span class="hlt">events</span> have historically resulted...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016PrOce.149..174A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016PrOce.149..174A"><span>Micro-phytoplankton community structure in the coastal upwelling <span class="hlt">zone</span> off Concepción (central Chile): <span class="hlt">Annual</span> and inter-<span class="hlt">annual</span> fluctuations in a highly dynamic environment</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Anabalón, V.; Morales, C. E.; González, H. E.; Menschel, E.; Schneider, W.; Hormazabal, S.; Valencia, L.; Escribano, R.</p> <p>2016-12-01</p> <p>An intensification of upwelling-favorable winds in recent decades has been detected in some of the main eastern boundary current systems, especially at higher latitudes, but the response of coastal phytoplankton communities in the Humboldt Current System (HCS) remains unknown. At higher latitudes in the HCS (35-40°S), strong seasonality in wind-driven upwelling during spring-summer coincides with an <span class="hlt">annual</span> increase in coastal chlorophyll-a and primary production, and a dominance of micro-phytoplankton. In order to understand the effects of potential upwelling intensification on the micro-phytoplankton community in this region, <span class="hlt">annual</span> and inter-<span class="hlt">annual</span> variability in its structure (total and taxa-specific abundance and biomass) and its association with oceanographic fluctuations were analyzed using in situ time series data (2002-2009) from a shelf station off Concepcion (36.5°S). At the <span class="hlt">annual</span> scale, total mean abundance and biomass, attributed to a few dominant diatom taxa, were at least one order of magnitude greater during spring-summer than autumn-winter, in association with changes in upwelling and surface salinity and temperature, whereas macro-nutrient concentrations remained relatively high all the year. At the inter-<span class="hlt">annual</span> scale, total abundance and biomass decreased during the upwelling season of the 2006-2009 period compared with the 2002-2006 period, notably due to lower abundances of Skeletonema and Leptocylindrus, but the relative dominance of a few taxa was maintained. The 2006-2009 period was characterized by higher upwelling intensity, colder and higher salinity waters, and changes in nutrient concentrations and ratios compared with the first period. The inter-<span class="hlt">annual</span> changes in the micro-phytoplankton community were mostly associated with changes in surface salinity and temperature (changes in upwelling intensity) but also with changes in Si/N and N/P, which relate to other land-derived processes.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_14");'>14</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li class="active"><span>16</span></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_16 --> <div id="page_17" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li class="active"><span>17</span></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="321"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009AGUFM.T53C1600A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009AGUFM.T53C1600A"><span>K-Ar constraints on fluid-rock interaction and dissolution-precipitation <span class="hlt">events</span> within the actively creeping shear <span class="hlt">zones</span> from SAFOD cores</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ali, S.; Hemming, S. R.; Torgersen, T.; Fleisher, M. Q.; Cox, S. E.; Stute, M.</p> <p>2009-12-01</p> <p>The San Andreas Fault Observatory at Depth (SAFOD) was drilled to study the physical and chemical processes responsible for faulting and earthquake generation along an active, plate-bounding fault at depth. SAFOD drill cores show multiple <span class="hlt">zones</span> of alteration and deformation due to fluid-rock interaction in the fault rocks(Schleicher et al. 2008). In context of fluid studies in the SAFZ, noble gas and potassium measurements were performed on solid samples of sedimentary rocks obtained from drill cores across the fault (3050-4000m-MD). We used a combination of 40Ar/39Ar and K-Ar methods on crushed samples of mudrock with variable amounts of visible slickensides to constrain the degree of resetting of the K-Ar system across the San Andreas Fault <span class="hlt">zone</span>. 40Ar/39Ar was analyzed from small fragments (sand sized grains) while K-Ar was measured in crushed bulk rock samples (100-250 mg for Ar, and 5-10 mg for K analyses). The apparent 40Ar/39Ar ages based on single step laser fusion of small fragments corresponding to the detrital component in the coarse fraction, show varying ages ranging from the provenance age to <13Ma. Although more data are needed to make detailed comparisons, the apparent K-Ar ages of bulk samples in the fault <span class="hlt">zone</span> are biased toward authigenic materials contained in the fine fraction, similar to the 40Ar/39Ar ages reported for mineralogical separates from very fine size fractions of samples obtained from 3065.98m-MD and 3294.89m-MD (Schleicher et al., submitted to Geology). The small samples measured for 40Ar/39Ar show scatter in the apparent ages, generally bracketing the bulk ages. However they are picked from sieved portions of the samples, and it is likely that there may be a loss of the younger (finer) material. Detrital provenance ages appear to be 50-60Ma in the Pacific Plate, and 100Ma in the North American Plate. 40Ar/39Ar ages within the SAFZ, as defined by geophysical logs (3200-3400m MD), are dominated by apparent detrital ages of ˜100Ma</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.T51D2906B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.T51D2906B"><span>An International Coastline Collaboratory to Broaden Scientific Impacts of a Subduction <span class="hlt">Zone</span> Observatory</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bodin, P.</p> <p>2015-12-01</p> <p>A global Subduction <span class="hlt">Zone</span> Observatory (SZO) presents an exciting opportunity to broaden involvement in scientific research and to ensure multidisciplinary impact. Most subduction <span class="hlt">zones</span> feature dynamic interactions of the seafloor, the coastline, and the onshore environments also being perturbed by global climate change. Tectonic deformation, physical environment changes (temperature and chemistry), and resulting ecological shifts (intertidal population redistribution, etc.) are all basic observables for important scientific investigation. Yet even simple baseline studies like repeated transects of intertidal biological communities are rare. A coordinated program of such studies would document the local variability across time and spatial scales, permit comparisons with other subducting coastlines, and extend the reach and importance of other SZO studies. One goal is to document the patterns, and separate the component causes of, coastal uplift and subsidence and ecological response to a subduction <span class="hlt">zone</span> earthquake using a database of pre-<span class="hlt">event</span> biological and surveying observations. Observations would be directed by local scientists using students and trained volunteers as observers, under the auspices of local educational entities and using standardized sampling and reporting methods. The observations would be added to the global, Internet-accessible, database for use by the entire scientific community. Data acquisition and analysis supports the educational missions of local schools and universities, forming the basis for educational programs. All local programs would be coordinated by an international panel convened by the SZO. The facility would include a web-hosted lecture series and an <span class="hlt">annual</span> web conference to aid organization and collaboration. Small grants could support more needy areas. This SZO collaboratory advances not only scientific literacy, but also multinational collaboration and scholarship, and (most importantly) produces important scientific results.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..17.9599K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..17.9599K"><span><span class="hlt">Annually</span> laminated lake sediments as recorders of flood <span class="hlt">events</span>: evidence from combining monitoring and calibration</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kämpf, Lucas; Brauer, Achim; Mueller, Philip; Güntner, Andreas; Merz, Bruno</p> <p>2015-04-01</p> <p>The relation of changing climate and the occurrence of strong flood <span class="hlt">events</span> has been controversially debated over the last years. One major limitation in this respect is the temporal extension of instrumental flood time series, rarely exceeding 50-100 years, which is too short to reflect the full range of natural climate variability in a region. Therefore, geoarchives are increasingly explored as natural flood recorders far beyond the range of instrumental flood time series. <span class="hlt">Annually</span> laminated (varved) lake sediments provide particularly valuable archives since (i) lakes form ideal traps in the landscape continuously recording sediment flux from the catchment and (ii) individual flood <span class="hlt">events</span> are recorded as detrital layers and can be dated with seasonal precision by varve counting. Despite the great potential of varved lake sediments for reconstructing long flood time series, there are still some confinements with respect to their interpretation due to a lack in understanding processes controlling the formation of detrital layers. For this purpose, we investigated the formation of detrital flood layers in Lake Mondsee (Upper Austria) in great detail by monitoring flood-related sediment flux and comparing detrital layers in sub-recent sediments with river runoff data. Sediment flux at the lake bottom was trapped over a three-year period (2011-2013) at two locations in Lake Mondsee, one located 0.9 km off the main inflow (proximal) and one in a more distal position at a distance of 2.8 km. The monitoring data include 26 floods of different amplitude (max. hourly discharge=10-110 cbm/s) which triggered variable fluxes of catchment sediment to the lake floor (4-760 g/(sqm*d)). The comparison of runoff and sediment data revealed empiric runoff thresholds for triggering significant detrital sediment influx to the proximal (20 cbm/s) and distal lake basin (30 cbm/s) and an exponential relation between runoff amplitude and the amount of deposited sediment. A succession of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec165-939.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec165-939.pdf"><span>33 CFR 165.939 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> Fireworks <span class="hlt">Events</span> in the Captain of the Port Buffalo <span class="hlt">Zone</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... effective from 9 p.m. to 10 p.m. on July 1 of each year. (3) French Festival Fireworks, Cape Vincent, NY—(i... 10:30 p.m. on the first weekend of July each year. (5) Celebrate Baldwinsville Fireworks.... to 10 p.m. on the third weekend of September each year. (6) Island Festival Fireworks Display...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol2/pdf/CFR-2010-title33-vol2-sec165-939.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title33-vol2/pdf/CFR-2010-title33-vol2-sec165-939.pdf"><span>33 CFR 165.939 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> Fireworks <span class="hlt">Events</span> in the Captain of the Port Buffalo <span class="hlt">Zone</span>.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-07-01</p> <p>... effective from 9 p.m. to 10 p.m. on July 1 of each year. (3) French Festival Fireworks, Cape Vincent, NY—(i.... to 10 p.m. on the third weekend of September each year. (6) Island Festival Fireworks Display... Festival, Rochester, NY—(i) Location. All waters of Lake Ontario within a 500-foot radius of land position...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70028052','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70028052"><span>Earthquakes triggered by silent slip <span class="hlt">events</span> on Kīlauea volcano, Hawaii</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Segall, Paul; Desmarais, Emily K.; Shelly, David; Miklius, Asta; Cervelli, Peter F.</p> <p>2006-01-01</p> <p>Slow-slip <span class="hlt">events</span>, or ‘silent earthquakes’, have recently been discovered in a number of subduction <span class="hlt">zones</span> including the Nankai trough1, 2, 3 in Japan, Cascadia4, 5, and Guerrero6 in Mexico, but the depths of these <span class="hlt">events</span> have been difficult to determine from surface deformation measurements. Although it is assumed that these silent earthquakes are located along the plate megathrust, this has not been proved. Slow slip in some subduction <span class="hlt">zones</span> is associated with non-volcanic tremor7, 8, but tremor is difficult to locate and may be distributed over a broad depth range9. Except for some <span class="hlt">events</span> on the San Andreas fault10, slow-slip <span class="hlt">events</span> have not yet been associated with high-frequency earthquakes, which are easily located. Here we report on swarms of high-frequency earthquakes that accompany otherwise silent slips on Kīlauea volcano, Hawaii. For the most energetic <span class="hlt">event</span>, in January 2005, the slow slip began before the increase in seismicity. The temporal evolution of earthquakes is well explained by increased stressing caused by slow slip, implying that the earthquakes are triggered. The earthquakes, located at depths of 7–8 km, constrain the slow slip to be at comparable depths, because they must fall in <span class="hlt">zones</span> of positive Coulomb stress change. Triggered earthquakes accompanying slow-slip <span class="hlt">events</span> elsewhere might go undetected if background seismicity rates are low. Detection of such <span class="hlt">events</span> would help constrain the depth of slow slip, and could lead to a method for quantifying the increased hazard during slow-slip <span class="hlt">events</span>, because triggered <span class="hlt">events</span> have the potential to grow into destructive earthquakes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007PhDT........59L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007PhDT........59L"><span>An investigation of deformation and fluid flow at subduction <span class="hlt">zones</span> using newly developed instrumentation and finite element modeling</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Labonte, Alison Louise</p> <p></p> <p>Detecting seafloor deformation <span class="hlt">events</span> in the offshore convergent margin environment is of particular importance considering the significant seismic hazard at subduction <span class="hlt">zones</span>. Efforts to gain insight into the earthquake cycle have been made at the Cascadia and Costa Rica subduction margins through recent expansions of onshore GPS and seismic networks. While these studies have given scientists the ability to quantify and locate slip <span class="hlt">events</span> in the seismogenic <span class="hlt">zone</span>, there is little technology available for adequately measuring offshore aseismic slip. This dissertation introduces an improved flow meter for detecting seismic and aseismic deformation in submarine environments. The value of such hydrologic measurements for quantifying the geodetics at offshore margins is verified through a finite element modeling (FEM) study in which the character of deformation in the shallow subduction <span class="hlt">zone</span> is determined from previously recorded hydrologic <span class="hlt">events</span> at the Costa Rica Pacific margin. Accurately sensing aseismic <span class="hlt">events</span> is one key to determining the stress state in subduction <span class="hlt">zones</span> as these slow-slip <span class="hlt">events</span> act to load or unload the seismogenic <span class="hlt">zone</span> during the interseismic period. One method for detecting seismic and aseismic strain <span class="hlt">events</span> is to monitor the hydrogeologic response to strain <span class="hlt">events</span> using fluid flow meters. Previous instrumentation, the Chemical Aqueous Transport (CAT) meter which measures flow rates through the sediment-water interface, can detect transient <span class="hlt">events</span> at very low flowrates, down to 0.0001 m/yr. The CAT meter performs well in low flow rate environments and can capture gradual changes in flow rate, as might be expected during ultra slow slip <span class="hlt">events</span>. However, it cannot accurately quantify high flow rates through fractures and conduits, nor does it have the temporal resolution and accuracy required for detecting transient flow <span class="hlt">events</span> associated with rapid deformation. The Optical Tracer Injection System (OTIS) developed for this purpose is an</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=marketing+AND+strategy&pg=6&id=EJ1163533','ERIC'); return false;" href="https://eric.ed.gov/?q=marketing+AND+strategy&pg=6&id=EJ1163533"><span>Evaluation of an <span class="hlt">Annual</span> Community-Focused Agricultural Literacy <span class="hlt">Event</span></span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Sandlin, M'Randa R.; Perez, Kauahi</p> <p>2017-01-01</p> <p>Agricultural literacy programs are effective pathways to informally teach the public about agriculture through stakeholder (attendee and exhibitor) interaction. Such programs are generally evaluated using attendee feedback but fail to include exhibitors' experience. The purpose of this study was to evaluate a local community agricultural <span class="hlt">event</span> by…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-03-16/pdf/2012-6379.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-03-16/pdf/2012-6379.pdf"><span>77 FR 15604 - <span class="hlt">Annual</span> Marine <span class="hlt">Events</span> in the Eighth Coast Guard District</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-03-16</p> <p>... Festival boat races in Port Neches, TX from 3 p.m. on May 4, 2012 through 6 p.m. on May 6, 2012. This... the <span class="hlt">annual</span> Neches River Festival in 33 CFR 100.801 (Table 1, paragraph 118) on May 4, 2012, from 3 p.m...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012ECSS..102..116M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012ECSS..102..116M"><span>Do mud deposition <span class="hlt">events</span> on sandy beaches affect surf <span class="hlt">zone</span> ichthyofauna? A southern Brazilian case study</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mont'Alverne, Renata; Moraes, Leonardo E.; Rodrigues, Fábio L.; Vieira, João P.</p> <p>2012-05-01</p> <p>Using fluid mud deposition <span class="hlt">events</span> which occur regularly at Cassino Beach in south Brazil, we evaluated the influence of such <span class="hlt">events</span> on the structure of the ichthyofauna inhabiting its shallow surf <span class="hlt">zone</span>. Wave action was the dominant factor in differentiating between sampling sites, being lower or even absent at the mud-influenced sectors compared to beach area without mud. Samples were collected using a beach seine net at two control locations (A1 and A2), and at three locations influenced by mud deposition (B1, B2, and B3). During the study period (21 April-04 August 2009), 15,245 fishes were captured and separated into 26 taxonomic groups, from species to family. Individuals of a total length (TL) up to 50 mm accounted for 65% of the catch, while individuals of TL < 30 mm were the most numerous and more responsible for the total abundance spatial pattern. The area with higher wave action (A2) had the lowest relative species abundance and greatest diversity, whereas the areas with mud-forced lowest wave action (B2 and B3) had the highest species abundance values. Three hypotheses were proposed to explain the higher concentration and capture of juvenile fishes at mud locations. First, longshore currents may be responsible for the displacement of juvenile aggregations toward areas of lower energy. Second, individuals may select habitats with turbid waters, which may provide greater protection from predators and increased food availability. Third, areas under the influence of fluid mud deposition show higher values of viscosity, which may reduce swimming activity and hinder the escape of juvenile fishes from nets, resulting in an increased capture of individuals compared to areas without mud.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016JSeis..20.1207F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016JSeis..20.1207F"><span>Cohesive <span class="hlt">zone</span> length of metagabbro at supershear rupture velocity</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fukuyama, Eiichi; Xu, Shiqing; Yamashita, Futoshi; Mizoguchi, Kazuo</p> <p>2016-10-01</p> <p>We investigated the shear strain field ahead of a supershear rupture. The strain array data along the sliding fault surfaces were obtained during the large-scale biaxial friction experiments at the National Research Institute for Earth Science and Disaster Resilience. These friction experiments were done using a pair of meter-scale metagabbro rock specimens whose simulated fault area was 1.5 m × 0.1 m. A 2.6-MPa normal stress was applied with loading velocity of 0.1 mm/s. Near-fault strain was measured by 32 two-component semiconductor strain gauges installed at an interval of 50 mm and 10 mm off the fault and recorded at an interval of 1 MHz. Many stick-slip <span class="hlt">events</span> were observed in the experiments. We chose ten unilateral rupture <span class="hlt">events</span> that propagated with supershear rupture velocity without preceding foreshocks. Focusing on the rupture front, stress concentration was observed and sharp stress drop occurred immediately inside the ruptured area. The temporal variation of strain array data is converted to the spatial variation of strain assuming a constant rupture velocity. We picked up the peak strain and zero-crossing strain locations to measure the cohesive <span class="hlt">zone</span> length. By compiling the stick-slip <span class="hlt">event</span> data, the cohesive <span class="hlt">zone</span> length is about 50 mm although it scattered among the <span class="hlt">events</span>. We could not see any systematic variation at the location but some dependence on the rupture velocity. The cohesive <span class="hlt">zone</span> length decreases as the rupture velocity increases, especially larger than √{2} times the shear wave velocity. This feature is consistent with the theoretical prediction.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..1913987C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..1913987C"><span>Radiocarbon dating with <span class="hlt">annual</span>-resolution of subfossil trees from the Younger Dryas <span class="hlt">event</span> in the southern French Alps</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Capano, Manuela; Miramont, Cécile; Guibal, Frédéric; Kromer, Bernd; Tuna, Thibaut; Fagault, Yoann; Bard, Edouard</p> <p>2017-04-01</p> <p>Tree rings are an important archive for the calibration of radiocarbon data. The younger part of the IntCal curve is based essentially on tree-ring chronologies, absolutely dated by dendrochronological analysis. For the Northern Hemisphere (NH), a gap still exists between the absolutely dated sequences and a floating chronology. Based on the Southern Hemisphere (SH) tree-ring chronologies a link has been previously proposed (Reimer et al. 2013, Radiocarbon; see also update in Hogg et al. 2016, Radiocarbon). By measuring radiocarbon at <span class="hlt">annual</span> resolution in French subfossil pines (Pinus sylvestris L.) we propose to improve the connection between the absolute chronology and the floating chronology. Several subfossil pines have been found in the Southern French Alps; they were buried by flood deposits, allowing their preservation. Some trees discovered in the Barbier riverbed were dated to the Younger Dryas periods by previous decadal radiocarbon measurements, performed in Heidelberg and Mannheim. The trees selected for our new study are Barb12 and Barb17 (analyzed sequences of 163 and 152 rings, respectively). These sequences were sampled at <span class="hlt">annual</span> resolution when permitted by the ring width. As a first step, every third ring was pretreated for radiocarbon analysis. These samples were sliced in small pieces and pretreated by using the ABA-B method before being combusted, graphitized with the AGE system and measured with AixMICADAS (Bard et al. 2015, Nucl. Instr. Meth. B). From the comparison with the kauri sequence, the Barb12-17 sequence can be dated from about 12835 to 12606 cal. BP. It can also be used to calculate the interhemispheric gradient (IHG) over the overlapping period. In order to reduce the inter-<span class="hlt">annual</span> variability, the Barb12-17 record was smoothed, grouped and averaged over the same decades as in the Kauri record. On the basis of twenty values, a mean IHG value of ca. 60 years was calculated. Quantification of the IHG around 50 yr is particularly</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-08-08/pdf/2013-19214.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-08-08/pdf/2013-19214.pdf"><span>78 FR 48311 - Special Local Regulations; Regattas and Marine Parades in the Captain of the Port Lake Michigan <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-08-08</p> <p>... <span class="hlt">Zone</span> AGENCY: Coast Guard, DHS. ACTION: Final rule. SUMMARY: The Coast Guard is amending special local regulations for <span class="hlt">annual</span> regattas and marine parades in the Captain of the Port Lake Michigan <span class="hlt">Zone</span>. This rule is intended to provide for the safety of life and property on navigable waters immediately prior to, during...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29028690','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29028690"><span>Adverse <span class="hlt">Event</span> Reporting: Harnessing Residents to Improve Patient Safety.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Tevis, Sarah E; Schmocker, Ryan K; Wetterneck, Tosha B</p> <p>2017-10-13</p> <p>Reporting of adverse and near miss <span class="hlt">events</span> are essential to identify system level targets to improve patient safety. Resident physicians historically report few <span class="hlt">events</span> despite their role as front-line patient care providers. We sought to evaluate barriers to adverse <span class="hlt">event</span> reporting in an effort to improve reporting. Our main outcomes were as follows: resident attitudes about <span class="hlt">event</span> reporting and the frequency of <span class="hlt">event</span> reporting before and after interventions to address reporting barriers. We surveyed first year residents regarding barriers to adverse <span class="hlt">event</span> reporting and used this input to construct a fishbone diagram listing barriers to reporting. Barriers were addressed, and resident <span class="hlt">event</span> reporting was compared before and after efforts were made to reduce obstacles to reporting. First year residents (97%) recognized the importance of submitting <span class="hlt">event</span> reports; however, the majority (85%) had not submitted an <span class="hlt">event</span> report in the first 6 months of residency. Only 7% of residents specified that they had not witnessed an adverse <span class="hlt">event</span> in 6 months, whereas one third had witnessed 10 or more <span class="hlt">events</span>. The main barriers were as follows: lack of knowledge about how to submit <span class="hlt">events</span> (38%) and lack of time to submit reports (35%). After improving resident education around <span class="hlt">event</span> reporting and simplifying the reporting process, resident <span class="hlt">event</span> reporting increased 230% (68 to 154 <span class="hlt">annual</span> reports, P = 0.025). We were able to significantly increase resident <span class="hlt">event</span> reporting by educating residents about adverse <span class="hlt">events</span> and near misses and addressing the primary barriers to <span class="hlt">event</span> reporting. Moving forward, we will continue <span class="hlt">annual</span> resident education about patient safety, focus on improving feedback to residents who submit reports, and empower senior residents to act as role models to junior residents in patient safety initiatives.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title49-vol4/pdf/CFR-2011-title49-vol4-part222-appC.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title49-vol4/pdf/CFR-2011-title49-vol4-part222-appC.pdf"><span>49 CFR Appendix C to Part 222 - Guide to Establishing Quiet <span class="hlt">Zones</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-10-01</p> <p>... Horns will not be subject to <span class="hlt">annual</span> reviews. (5) The use of FRA's web-based Quiet <span class="hlt">Zone</span> Calculator is... appendix A (e.g., shorter than required traffic channelization devices), non-engineering ASMs (e.g., programmed law enforcement), and engineering ASMs (i.e., engineering improvements other than modified SSMs...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1998JMS....17..375V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1998JMS....17..375V"><span>Comparative abundance and distribution of major filter-feeders in the Antarctic pelagic <span class="hlt">zone</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Voronina, N. M.</p> <p>1998-11-01</p> <p>The filter-feeding plankton, herbivorous copepods, salps and euphausiids, form the basic level of metazoans in the Antarctic pelagic trophic web. This paper sets out to determine the comparative share of these taxonomic groups in the total biomass and <span class="hlt">annual</span> production. Their most abundant representatives, four copepod species ( Calanus propinquus, Calanoides acutus, Rhincalanus gigas and Metridia gerlachei), all salps and krill Euphausia superba were studied. For the first two groups net samples from six Russian expeditions in different sectors of the Antarctic were used. In total 752 samples from 118 stations were considered. The mean fresh biomass of filter-feeding copepods in the 0-1500 m layer was 18.0 g m -2 and in the entire Antarctic 576 10 6 t. The biomass of salps in comparatively restricted rich regions exceeded 500 g m -2 and in the remaining area was 1.2±0.8 g m -2, giving a total quantity of 882 10 6 t. The krill abundance estimation was based on published data, using a map of its quantitative distribution compiled from commercial trawling made by Soviet fishing and scientific ships during 17 seasons [Parfenovich, S.S., 1980. O zakonomernostyakh razmeshcheniya i regionalnoi differentsiatsii mestoskoplenii krilya v Yuzhnom Okeane. VNIRO, Moskva, in Russian.]. Three main <span class="hlt">zones</span> based on commercial characteristics were determined by this author: (1) <span class="hlt">zone</span> of regular occurrence of dense concentrations; (2) <span class="hlt">zone</span> of rare occurrence of concentrations; (3) <span class="hlt">zone</span> of low-abundance dispersed krill. All available data on E. superba biomass in the Antarctic were grouped together according to these <span class="hlt">zones</span> and their means were calculated. The biomass of krill was found to be 60.1±11.2, 3.3±1.3 and 0.8±0.4 g m -2 fresh mass in <span class="hlt">zones</span> 1, 2 and 3, respectively, with a total of 272 10 6 t. All estimates are compared with the literature data and their validity is discussed. For the <span class="hlt">annual</span> production determinations the obtained biomass characteristics were multiplied by</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012EGUGA..1411835V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012EGUGA..1411835V"><span>A non extensive statistical physics analysis of the Hellenic subduction <span class="hlt">zone</span> seismicity</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Vallianatos, F.; Papadakis, G.; Michas, G.; Sammonds, P.</p> <p>2012-04-01</p> <p>The Hellenic subduction <span class="hlt">zone</span> is the most seismically active region in Europe [Becker & Meier, 2010]. The spatial and temporal distribution of seismicity as well as the analysis of the magnitude distribution of earthquakes concerning the Hellenic subduction <span class="hlt">zone</span>, has been studied using the concept of Non-Extensive Statistical Physics (NESP) [Tsallis, 1988 ; Tsallis, 2009]. Non-Extensive Statistical Physics, which is a generalization of Boltzmann-Gibbs statistical physics, seems a suitable framework for studying complex systems (Vallianatos, 2011). Using this concept, Abe & Suzuki (2003;2005) investigated the spatial and temporal properties of the seismicity in California and Japan and recently Darooneh & Dadashinia (2008) in Iran. Furthermore, Telesca (2011) calculated the thermodynamic parameter q of the magnitude distribution of earthquakes of the southern California earthquake catalogue. Using the external seismic <span class="hlt">zones</span> of 36 seismic sources of shallow earthquakes in the Aegean and the surrounding area [Papazachos, 1990], we formed a dataset concerning the seismicity of shallow earthquakes (focal depth ≤ 60km) of the subduction <span class="hlt">zone</span>, which is based on the instrumental data of the Geodynamic Institute of the National Observatory of Athens (http://www.gein.noa.gr/, period 1990-2011). The catalogue consists of 12800 seismic <span class="hlt">events</span> which correspond to 15 polygons of the aforementioned external seismic <span class="hlt">zones</span>. These polygons define the subduction <span class="hlt">zone</span>, as they are associated with the compressional stress field which characterizes a subducting regime. For each <span class="hlt">event</span>, moment magnitude was calculated from ML according to the suggestions of Papazachos et al. (1997). The cumulative distribution functions of the inter-<span class="hlt">event</span> times and the inter-<span class="hlt">event</span> distances as well as the magnitude distribution for each seismic <span class="hlt">zone</span> have been estimated, presenting a variation in the q-triplet along the Hellenic subduction <span class="hlt">zone</span>. The models used, fit rather well to the observed</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2004DSRI...51..307P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2004DSRI...51..307P"><span>Geochemical particle fluxes in the Southern Indian Ocean seasonal ice <span class="hlt">zone</span>: Prydz Bay region, East Antarctica</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pilskaln, C. H.; Manganini, S. J.; Trull, T. W.; Armand, L.; Howard, W.; Asper, V. L.; Massom, R.</p> <p>2004-02-01</p> <p>Time-series sediment traps were deployed between December 1998 and January 2000 and from March 2000 to February 2001 at two offshore Prydz Bay sites within the seasonal ice <span class="hlt">zone</span> (SIZ) of the Southern Indian Ocean located between 62-63°S and 73-76°E to quantify seasonal biogeochemical particle fluxes. Samples were obtained from traps placed at 1400, 2400, and 3400 m during the first deployment year (PZB-1) and from 3300 m in the second deployment year (PZB-2). All geochemical export fluxes were highly seasonal with primary peaks occurring during the austral summer and relatively low fluxes prevailing through the winter months. Secondary flux peaks in mid-winter and in early spring were suggestive of small-scale, sea-ice break-up <span class="hlt">events</span> and the spring retreat of seasonal ice, respectively. Biogenic silica represented over 70% (by weight) of the collected trap material and provided an <span class="hlt">annual</span> opal export of 18 g m -2 to 1 km and 3-10 g m -2 to 3 km. POC fluxes supplied an <span class="hlt">annual</span> export of approximately 1 g m -2, equal to the estimated ocean-wide average. Elevated particulate C org/C inorg and Si bio/C inorg molar ratios indicate a productive, diatom-dominated system, although consistently small fluxes of planktonic foraminifera and pteropod shells document a heterotrophic source of carbonate to deeper waters in the SIZ. The observation of high Si bio/C org ratios and the δ15N time-series data suggest enhanced rates of diatom-POC remineralization in the upper 1000 m relative to bioSiO 2. The occurrence in this region of a pronounced temperature minimum, associated with a strong pycnocline and subsurface particle maximum at 50-100 m, may represent a <span class="hlt">zone</span> where sinking, diatom-rich particulates temporarily accumulate and POC is remineralized.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-08-01/pdf/2011-19321.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-08-01/pdf/2011-19321.pdf"><span>76 FR 45693 - Safety <span class="hlt">Zone</span>; San Diego POPS Fireworks, San Diego, CA</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-08-01</p> <p>...-AA00 Safety <span class="hlt">Zone</span>; San Diego POPS Fireworks, San Diego, CA AGENCY: Coast Guard, DHS. ACTION: Temporary... San Diego Bay in support of the San Diego POPS Fireworks. This safety <span class="hlt">zone</span> is necessary to provide for... of the waterway during scheduled fireworks <span class="hlt">events</span>. Persons and vessels will be prohibited from...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-06-30/pdf/2011-16115.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-06-30/pdf/2011-16115.pdf"><span>76 FR 38305 - Safety <span class="hlt">Zone</span>; San Francisco Chronicle Fireworks Display, San Francisco, CA</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-06-30</p> <p>... DEPARTMENT OF HOMELAND SECURITY Coast Guard 33 CFR Part 165 [Docket No. USCG 2011-0402] Safety <span class="hlt">Zone</span>; San Francisco Chronicle Fireworks Display, San Francisco, CA AGENCY: Coast Guard, DHS. ACTION... <span class="hlt">annual</span> San Francisco Chronicle Fireworks Display (Independence Day Celebration for the City of San...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_15");'>15</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li class="active"><span>17</span></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_17 --> <div id="page_18" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li class="active"><span>18</span></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="341"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70022832','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70022832"><span>Paleoearthquake recurrence on the East Paradise fault <span class="hlt">zone</span>, metropolitan Albuquerque, New Mexico</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Personius, Stephen F.; Mahan, Shannon</p> <p>2000-01-01</p> <p>A fortuitous exposure of the East Paradise fault <span class="hlt">zone</span> near Arroyo de las Calabacillas has helped us determine a post-middle Pleistocene history for a long-forgotten Quaternary fault in the City of Albuquerque, New Mexico. Mapping of two exposures of the fault <span class="hlt">zone</span> allowed us to measure a total vertical offset of 2.75 m across middle Pleistocene fluvial and eolian deposits and to estimate individual surface-faulting <span class="hlt">events</span> of about 1, 0.5, and 1.25 m. These measurements and several thermoluminescence ages allow us to calculate a long-term average slip rate of 0.01 ± 0.001 mm/yr and date two surface-faulting <span class="hlt">events</span> to 208 ± 25 ka and 75 ± 7 ka. The youngest <span class="hlt">event</span> probably occurred in the late Pleistocene, sometime after 75 ± 7 ka. These data yield a single recurrence interval of 133 ± 26 ka and an average recurrence interval of 90 ± 10 ka. However, recurrence intervals are highly variable because the two youngest <span class="hlt">events</span> occurred in less than 75 ka. Offsets of 0.5-1.25 m and a fault length of 13-20 km indicate that surface-rupturing paleoearthquakes on the East Paradise fault <span class="hlt">zone</span> had probable Ms or Mw magnitudes of 6.8-7.0. Although recurrence intervals are long on the East Paradise fault <span class="hlt">zone</span>, these data are significant because they represent some of the first published slip rate, paleoearthquake magnitude, and recurrence information for any of the numerous Quaternary faults in the rapidly growing Albuquerque-Rio Rancho metropolitan area.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-02-07/pdf/2012-2753.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-02-07/pdf/2012-2753.pdf"><span>77 FR 6019 - Western Pacific Fisheries; 2012 <span class="hlt">Annual</span> Catch Limits and Accountability Measures</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-02-07</p> <p>... <span class="hlt">annual</span> catch limits for western Pacific bottomfish, crustacean, precious coral, and coral reef ecosystem... coral reef ecosystem fishery management unit species (MUS) in the U.S. Exclusive Economic <span class="hlt">Zone</span> (EEZ...,205 lb (1,000 kg). the American Samoa Exploratory Area. Coral Reef Ecosystem........ Acanthuridae...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFMNH13C1944G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFMNH13C1944G"><span>Modelling Inland Flood <span class="hlt">Events</span> for Hazard Maps in Taiwan</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ghosh, S.; Nzerem, K.; Sassi, M.; Hilberts, A.; Assteerawatt, A.; Tillmanns, S.; Mathur, P.; Mitas, C.; Rafique, F.</p> <p>2015-12-01</p> <p>Taiwan experiences significant inland flooding, driven by torrential rainfall from plum rain storms and typhoons during summer and fall. From last 13 to 16 years data, 3,000 buildings were damaged by such floods <span class="hlt">annually</span> with a loss US$0.41 billion (Water Resources Agency). This long, narrow island nation with mostly hilly/mountainous topography is located at tropical-subtropical <span class="hlt">zone</span> with <span class="hlt">annual</span> average typhoon-hit-frequency of 3-4 (Central Weather Bureau) and <span class="hlt">annual</span> average precipitation of 2502mm (WRA) - 2.5 times of the world's average. Spatial and temporal distributions of countrywide precipitation are uneven, with very high local extreme rainfall intensities. <span class="hlt">Annual</span> average precipitation is 3000-5000mm in the mountainous regions, 78% of it falls in May-October, and the 1-hour to 3-day maximum rainfall are about 85 to 93% of the world records (WRA). Rivers in Taiwan are short with small upstream areas and high runoff coefficients of watersheds. These rivers have the steepest slopes, the shortest response time with rapid flows, and the largest peak flows as well as specific flood peak discharge (WRA) in the world. RMS has recently developed a countrywide inland flood model for Taiwan, producing hazard return period maps at 1arcsec grid resolution. These can be the basis for evaluating and managing flood risk, its economic impacts, and insured flood losses. The model is initiated with sub-daily historical meteorological forcings and calibrated to daily discharge observations at about 50 river gauges over the period 2003-2013. Simulations of hydrologic processes, via rainfall-runoff and routing models, are subsequently performed based on a 10000 year set of stochastic forcing. The rainfall-runoff model is physically based continuous, semi-distributed model for catchment hydrology. The 1-D wave propagation hydraulic model considers catchment runoff in routing and describes large-scale transport processes along the river. It also accounts for reservoir storage</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2006JHyd..327..304B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2006JHyd..327..304B"><span>Extreme rainfall <span class="hlt">events</span>: Learning from raingauge time series</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Boni, G.; Parodi, A.; Rudari, R.</p> <p>2006-08-01</p> <p>SummaryThis study analyzes the historical records of <span class="hlt">annual</span> rainfall maxima recorded in Northern Italy, cumulated over time windows (durations) of 1 and 24 h and considered paradigmatic descriptions of storms of both short and long duration. Three large areas are studied: Liguria, Piedmont and Triveneto (Triveneto includes the Regions of Veneto, Trentino Alto Adige and Friuli Venezia Giulia). A regional frequency analysis of <span class="hlt">annual</span> rainfall maxima is carried out through the Two Components Extreme Value (TCEV) distribution. A hierarchical approach is used to define statistically homogeneous areas so that the definition of a regional distribution becomes possible. Thanks to the peculiar nature of the TCEV distribution, a frequency-based threshold criterion is proposed. Such criterion allows to distinguish the observed ordinary values from the observed extra-ordinary values of <span class="hlt">annual</span> rainfall maxima. A second step of this study focuses on the analysis of the probability of occurrence of extra-ordinary <span class="hlt">events</span> over a period of one year. Results show the existence of a four month dominant season that maximizes the number of occurrences of <span class="hlt">annual</span> rainfall maxima. Such results also show how the seasonality of extra-ordinary <span class="hlt">events</span> changes whenever a different duration of <span class="hlt">events</span> is considered. The joint probability of occurrence of extreme storms of short and long duration is also analyzed. Such analysis demonstrates how the joint probability of occurrence significantly changes when all rainfall maxima or only extra-ordinary maxima are used. All results undergo a critical discussion. Such discussion seems to lead to the point that the identified statistical characteristics might represent the landmark of those mechanisms causing heavy precipitation in the analyzed regions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014ACP....1413411D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014ACP....1413411D"><span>Long-term variability of dust <span class="hlt">events</span> in Iceland (1949-2011)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dagsson-Waldhauserova, P.; Arnalds, O.; Olafsson, H.</p> <p>2014-12-01</p> <p>The long-term frequency of atmospheric dust observations was investigated for the southern part of Iceland and interpreted together with earlier results obtained from northeastern (NE) Iceland (Dagsson-Waldhauserova et al., 2013). In total, over 34 dust days per year on average occurred in Iceland based on conventionally used synoptic codes for dust observations. However, frequent volcanic eruptions, with the re-suspension of volcanic materials and dust haze, increased the number of dust <span class="hlt">events</span> fourfold (135 dust days <span class="hlt">annually</span>). The position of the Icelandic Low determined whether dust <span class="hlt">events</span> occurred in the NE (16.4 dust days <span class="hlt">annually</span>) or in the southern (S) part of Iceland (about 18 dust days <span class="hlt">annually</span>). The decade with the most frequent dust days in S Iceland was the 1960s, but the 2000s in NE Iceland. A total of 32 severe dust storms (visibility < 500 m) were observed in Iceland with the highest frequency of <span class="hlt">events</span> during the 2000s in S Iceland. The Arctic dust <span class="hlt">events</span> (NE Iceland) were typically warm, occurring during summer/autumn (May-September) and during mild southwesterly winds, while the subarctic dust <span class="hlt">events</span> (S Iceland) were mainly cold, occurring during winter/spring (March-May) and during strong northeasterly winds. About half of the dust <span class="hlt">events</span> in S Iceland occurred in winter or at sub-zero temperatures. A good correlation was found between particulate matter (PM10) concentrations and visibility during dust observations at the stations Vík and Stórhöfði. This study shows that Iceland is among the dustiest areas of the world and that dust is emitted year-round.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.dtic.mil/docs/citations/ADA534224','DTIC-ST'); return false;" href="http://www.dtic.mil/docs/citations/ADA534224"><span>DCERP <span class="hlt">Annual</span> Technical Report III: March 2009-February 2010. Executive Summary</span></a></p> <p><a target="_blank" href="http://www.dtic.mil/">DTIC Science & Technology</a></p> <p></p> <p>2010-04-01</p> <p>groundwater passing though marshes to the estuary. Loading estimates may vary considerably depending on inter-<span class="hlt">annual</span> hydrologic (storm versus drought ...climatic <span class="hlt">events</span> (i.e., hurricanes and droughts ); and integrate results with the other DCERP modules. The benefits of the Aquatic/Estuarine Module...inter-<span class="hlt">annual</span> hydrologic (storm versus drought years) variability. ▪ Several large phytoplankton blooms in mid-estuary to upper estuary locations</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29022167','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29022167"><span>Stochastic evaluation of <span class="hlt">annual</span> micropollutant loads and their uncertainties in separate storm sewers.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Hannouche, Ali; Chebbo, Ghassan; Joannis, Claude; Gasperi, Johnny; Gromaire, Marie-Christine; Moilleron, Régis; Barraud, Sylvie; Ruban, Véronique</p> <p>2017-12-01</p> <p>This article describes a stochastic method to calculate the <span class="hlt">annual</span> pollutant loads and its application over several years at the outlet of three catchments drained by separate storm sewers. A stochastic methodology using Monte Carlo simulations is proposed for assessing <span class="hlt">annual</span> pollutant load, as well as the associated uncertainties, from a few <span class="hlt">event</span> sampling campaigns and/or continuous turbidity measurements (representative of the total suspended solids concentration (TSS)). Indeed, in the latter case, the proposed method takes into account the correlation between pollutants and TSS. The developed method was applied to data acquired within the French research project "INOGEV" (innovations for a sustainable management of urban water) at the outlet of three urban catchments drained by separate storm sewers. Ten or so <span class="hlt">event</span> sampling campaigns for a large range of pollutants (46 pollutants and 2 conventional water quality parameters: TSS and total organic carbon (TOC)) are combined with hundreds of rainfall <span class="hlt">events</span> for which, at least one among three continuously monitored parameters (rainfall intensity, flow rate, and turbidity) is available. Results obtained for the three catchments show that the <span class="hlt">annual</span> pollutant loads can be estimated with uncertainties ranging from 10 to 60%, and the added value of turbidity monitoring for lowering the uncertainty is demonstrated. A low inter-<span class="hlt">annual</span> and inter-site variability of pollutant loads, for many of studied pollutants, is observed with respect to the estimated uncertainties, and can be explained mainly by <span class="hlt">annual</span> precipitation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2002PEPI..132..157L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2002PEPI..132..157L"><span>Slab-pull and slab-push earthquakes in the Mexican, Chilean and Peruvian subduction <span class="hlt">zones</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lemoine, A.; Madariaga, R.; Campos, J.</p> <p>2002-09-01</p> <p>We studied intermediate depth earthquakes in the Chile, Peru and Mexican subduction <span class="hlt">zones</span>, paying special attention to slab-push (down-dip compression) and slab-pull (down-dip extension) mechanisms. Although, slab-push <span class="hlt">events</span> are relatively rare in comparison with slab-pull earthquakes, quite a few have occurred recently. In Peru, a couple slab-push <span class="hlt">events</span> occurred in 1991 and one slab-pull together with several slab-push <span class="hlt">events</span> occurred in 1970 near Chimbote. In Mexico, several slab-push and slab-pull <span class="hlt">events</span> occurred near Zihuatanejo below the fault <span class="hlt">zone</span> of the 1985 Michoacan <span class="hlt">event</span>. In central Chile, a large M=7.1 slab-push <span class="hlt">event</span> occurred in October 1997 that followed a series of four shallow Mw>6 thrust earthquakes on the plate interface. We used teleseismic body waveform inversion of a number of Mw>5.9 slab-push and slab-pull earthquakes in order to obtain accurate mechanisms, depths and source time functions. We used a master <span class="hlt">event</span> method in order to get relative locations. We discussed the occurrence of the relatively rare slab-push <span class="hlt">events</span> in the three subduction <span class="hlt">zones</span>. Were they due to the geometry of the subduction that produces flexure inside the downgoing slab, or were they produced by stress transfer during the earthquake cycle? Stress transfer can not explain the occurence of several compressional and extensional intraplate intermediate depth earthquakes in central Chile, central Mexico and central Peru. It seemed that the heterogeneity of the stress field produced by complex slab geometry has an important influence on intraplate intermediate depth earthquakes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://rosap.ntl.bts.gov/view/dot/36185','DOTNTL'); return false;" href="https://rosap.ntl.bts.gov/view/dot/36185"><span>Blowout Prevention System <span class="hlt">Events</span> and Equipment Component Failures : 2016 SafeOCS <span class="hlt">Annual</span> Report</span></a></p> <p><a target="_blank" href="http://ntlsearch.bts.gov/tris/index.do">DOT National Transportation Integrated Search</a></p> <p></p> <p>2017-09-22</p> <p>The SafeOCS 2016 <span class="hlt">Annual</span> Report, produced by the Bureau of Transportation Statistics (BTS), summarizes blowout prevention (BOP) equipment failures on marine drilling rigs in the Outer Continental Shelf. It includes an analysis of equipment component f...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-09-05/pdf/2013-21511.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-09-05/pdf/2013-21511.pdf"><span>78 FR 54576 - Safety <span class="hlt">Zone</span>; LK <span class="hlt">Events</span> Fireworks; Lake Michigan, Chicago, IL</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-09-05</p> <p>... of any grant or loan recipients, and will not raise any novel legal or policy issues. The safety <span class="hlt">zone</span>... Port. 2. Impact on Small Entities Under the Regulatory Flexibility Act (5 U.S.C. 601-612), we have considered the impact of this temporary rule on small entities. The Coast Guard certifies under 5 U.S.C. 605...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2005Tectp.408..237G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2005Tectp.408..237G"><span>Late Pleistocene and Holocene paleoseismology of an intraplate seismic <span class="hlt">zone</span> in a large alluvial valley, the New Madrid seismic <span class="hlt">zone</span>, Central USA</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Guccione, Margaret J.</p> <p>2005-10-01</p> <p>The New Madrid seismic <span class="hlt">zone</span> (NMSZ) is an intraplate right-lateral strike-slip and thrust fault system contained mostly within the Mississippi Alluvial Valley. The most recent earthquake sequence in the <span class="hlt">zone</span> occurred in 1811 1812 and had estimated moment magnitudes of 7 8 (e.g., [Johnston, A.C., 1996. Seismic moment assessment of stable continental earthquakes, Part 3: 1811 1812 New Madrid, 1886 Charleston, and 1755 Lisbon. Geophysical Journal International 126, 314 344; Johnston, A.C., Schweig III, E.S, 1996. The enigma of the New Madrid earthquakes of 1811 1812. <span class="hlt">Annual</span> Reviews of Earth and Planetary Sciences 24, 339 384; Hough, S.E., Armbruster, J.G., Seeber, L., Hough, J.F., 2000. On the modified Mercalli intensities and magnitudes of the New Madrid earthquakes. Journal of Geophysical Research 105 (B10), 23,839 23,864; Tuttle, M.P., 2001. The use of liquefaction features in paleoseismology: Lessons learned in the New Madrid seismic <span class="hlt">zone</span>, central United States. Journal of Seismology 5, 361 380]). Four earlier prehistoric earthquakes or earthquake sequences have been dated A.D. 1450 ± 150, 900 ± 100, 300 ± 200, and 2350 B.C. ± 200 years using paleoliquefaction features, particularly those associated with native American artifacts, and in some cases surface deformation ([Craven, J. A. 1995. Paleoseismology study in the New Madrid seismic <span class="hlt">zone</span> using geological and archeological features to constrain ages of liquefaction deposits. M.S thesis, University of Memphis, Memphis, TN, U.S.A.; Tuttle, M.P., Lafferty III, R.H., Guccione, M.J., Schweig III, E.S., Lopinot, N., Cande, R., Dyer-Williams, K., Haynes, M., 1996. Use of archaeology to date liquefaction features and seismic <span class="hlt">events</span> in the New Madrid seismic <span class="hlt">zone</span>, central United States. Geoarchaeology 11, 451 480; Guccione, M.J., Mueller, K., Champion, J., Shepherd, S., Odhiambo, B., 2002b. Stream response to repeated co-seismic folding, Tiptonville dome, western Tennessee. Geomorphology 43(2002), 313 349; Tuttle, M</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.T21C2818A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.T21C2818A"><span>Sequence of slow slip <span class="hlt">events</span> and low frequency earthquakes in the shallow part of the Nankai Trough seismogenic <span class="hlt">zone</span> observed by seafloor observation network.</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Araki, E.; Saffer, D. M.; Kopf, A.; To, A.; Ide, S.; Nakano, M.; Kimura, T.; Machida, Y.</p> <p>2016-12-01</p> <p>Seismic behavior of the thrust <span class="hlt">zone</span> in trench side of the seismically coupled plate interface in the Nankai Trough is poorly understood because shore based seismic and geodetic observation does not have enough sensitivity to detect slow activity in the area. In these years, we constructed dense seafloor observation network in combination with pore-fluid pressure, strain, and seismic sensing in IODP deep boreholes (C0002G and C0010A) and 20+ seafloor broadband seismometers cabled to the observation network called DONET for long-term continuous observation in the To-Nankai area of the Nankai Trough, south of Japan. Analysis of the seismic records from DONET seafloor seismometer and pore-fluid pressure records from the boreholes in the period from Jan. 2011 to Apr. 2016 revealed the activities of the slow slip <span class="hlt">events</span> (SSE), low frequency tremor (LFT), and very low frequency earthquakes (VLFE) in the observation network, detecting seven sequence of pore-fluid pressure transients in these boreholes representing SSEs and many LFT and VLFEs from seismic records. Some of the SSE sequence accompanies active LFT swarms in the regions offshore of the locked seismogenic <span class="hlt">zone</span>. Some of the pressure transient initiate precedent to the LFT swarms, as well as some does not accompany obvious LFT activity, as if the SSE occurs "silently", suggesting LFT does not express SSE but LFT seems activated by the SSE. This is also supported by change of SSE pressure transient rate in accordance with LFT activity, observed in sequences in Mar. 2011, Oct. 2015, and April 2016. In the Oct. 2015 sequence, observed pressure transient in two boreholes indicates the slip propagates updip in the shallow subduction <span class="hlt">zone</span>. In many sequences including this sequence, we ientify that the LFT swarm tends to migrate updip direction. The pressure transient in Apr. 2016 also followed this tendency, initiating from co-seismic compression by Apr. 1 earthquake occurred downdip side of the boreholes, followed by</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18.5687T','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18.5687T"><span>Human-water interactions in Myanmar's Dry <span class="hlt">Zone</span> under climate change</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Taft, Linda; Evers, Mariele</p> <p>2016-04-01</p> <p>Understanding human-water interactions is particularly essential in countries where the economy and the people's well-being and income strongly depend on the availability and quality of sufficient water resources. Such a strong dependency on water is existent in Myanmar's Dry <span class="hlt">Zone</span> located in the central Ayeyarwady River basin. In this area, rainfall is associated with high heterogeneity across space and time. Precipitation amounts in the Dry <span class="hlt">Zone</span> (500-1000 mm <span class="hlt">annually</span>) are generally less compared to other regions in Myanmar (up to 4000-6000 mm). Following the Global Climate Risk Index, Myanmar is one of the countries which were most affected by extreme weather <span class="hlt">events</span> between 1994 and 2013. Severe drought periods e.g in the years 1997-1998, 2010 and 2014 led to crop failures and water shortage in the Dry <span class="hlt">Zone</span>, where more than 14 mio people predominantly practice agriculture. Due to the high variability of rainfalls, farming is only possible with irrigation, mainly conducted by canal systems from the rivers and groundwater withdrawal. Myanmar is recently facing big challenges which result from comprehensive political and economic reforms since 2011. These may also include increasing water use by new industrial <span class="hlt">zones</span> and urbanization. However, not only policy and economy modify the need for water. Variability of river runoff and changes in seasonality are expected as a result of climate change. The overarching goal of the study is to understand and increase the knowledge on human-water-climate interactions and to elaborate possible future scenarios for Myanmar's Dry <span class="hlt">Zone</span>. It is not well studied yet how current and future climate change and increasing human impact will influence the country's abundant water resources including groundwater. Therefore, the first step of this study is to identify the major drivers within the central Ayeyarwady River basin. We are in the process of collecting and analyzing data sets and information including hydrologic and eco</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19750055654&hterms=Crystal+wave+frequency&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DCrystal%2Bwave%2Bfrequency','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19750055654&hterms=Crystal+wave+frequency&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D20%26Ntt%3DCrystal%2Bwave%2Bfrequency"><span>High-frequency lunar teleseismic <span class="hlt">events</span></span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Nakamura, Y.; Dorman, J.; Duennebier, F.; Ewing, M.; Lammlein, D.; Latham, G.</p> <p>1974-01-01</p> <p>A small number of seismic signals, including some of the strongest observed to date, have been identified as representing a fourth principal category of natural lunar seismic <span class="hlt">events</span> with characteristics distinct from those produced by normal meteoroid impacts, deep moonquakes, and thermal moonquakes. These signals are much richer in high frequencies than other <span class="hlt">events</span> observed at comparable distances, and display relatively impulsive P- and S-wave beginnings, indicating negligible seismic-wave scattering near the source. Source depths of these <span class="hlt">events</span> may range between 0 and perhaps 300 km. These and other characteristics could represent either (1) meteoroids impacting upon outcrops of competent lunar crystal rock, (2) rare impacting objects that penetrate to competent rock below a scattering <span class="hlt">zone</span>, or (3) shallow tectonic moonquakes.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70017613','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70017613"><span>Large mid-Holocene and late Pleistocene earthquakes on the Oquirrh fault <span class="hlt">zone</span>, Utah</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Olig, S.S.; Lund, W.R.; Black, B.D.</p> <p>1994-01-01</p> <p>The Oquirrh fault <span class="hlt">zone</span> is a range-front normal fault that bounds the east side of Tooele Valley and it has long been recognized as a potential source for large earthquakes that pose a significant hazard to population centers along the Wasatch Front in central Utah. Scarps of the Oquirrh fault <span class="hlt">zone</span> offset the Provo shoreline of Lake Bonneville and previous studies of scarp morphology suggested that the most recent surface-faulting earthquake occurred between 9000 and 13,500 years ago. Based on a potential rupture length of 12 to 21 km from previous mapping, moment magnitude (Mw) estimates for this <span class="hlt">event</span> range from 6.3 to 6.6 In contrast, our results from detailed mapping and trench excavations at two sites indicate that the most-recent <span class="hlt">event</span> actually occurred between 4300 and 6900 yr B.P. (4800 and 7900 cal B.P.) and net vertical displacements were 2.2 to 2.7 m, much larger than expected considering estimated rupture lengths for this <span class="hlt">event</span>. Empirical relations between magnitude and displacement yield Mw 7.0 to 7.2. A few, short discontinuous fault scarps as far south as Stockton, Utah have been identified in a recent mapping investigation and our results suggest that they may be part of the Oquirrh fault <span class="hlt">zone</span>, increasing the total fault length to 32 km. These results emphasize the importance of integrating stratigraphic and geomorphic information in fault investigations for earthquake hazard evaluations. At both the Big Canyon and Pole Canyon sites, trenches exposed faulted Lake Bonneville sediments and thick wedges of fault-scarp derived colluvium associated with the most-recent <span class="hlt">event</span>. Bulk sediment samples from a faulted debris-flow deposit at the Big Canyon site yield radiocarbon ages of 7650 ?? 90 yr B.P. and 6840 ?? 100 yr B.P. (all lab errors are ??1??). A bulk sediment sample from unfaulted fluvial deposits that bury the fault scarp yield a radiocarbon age estimate of 4340 ?? 60 yr B.P. Stratigraphic evidence for a pre-Bonneville lake cycle penultimate</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018AdSpR..61.1444D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018AdSpR..61.1444D"><span>Role of Equatorial Anomaly in Earthquake time precursive features: A few strong <span class="hlt">events</span> over West Pacific <span class="hlt">zone</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Devi, Minakshi; Patgiri, S.; Barbara, A. K.; Oyama, Koh-Ichiro; Ryu, K.; Depuev, V.; Depueva, A.</p> <p>2018-03-01</p> <p>The earthquake (EQ) time coupling processes between equator-low-mid latitude ionosphere are complex due to inherent dynamical status of each latitudinal <span class="hlt">zone</span> and qualified geomagnetic roles working in the system. In an attempt to identify such process, the paper presents temporal and latitudinal variations of ionization density (foF2) covering 45°N to 35°S, during a number of earthquake <span class="hlt">events</span> (M > 5.5). The approaches adopted for extraction of features by the earthquake induced preparatory processes are discussed in the paper through identification of parameters like the 'EQ time modification in density gradient' defined by δ = (foF2 max - foF2 min)/τmm, where τmm - time span (in days) between EQ modified density maximum and minimum, and the Earthquake time Equatorial Anomaly, i.e. EEA, one of the most significant phenomenon which develops even during night time irrespective of epicenter position. Based on the observations, the paper presents the seismic time coupling dynamics through anomaly like manifestations between equator, low and mid latitude ionosphere bringing in the global Total Electron Content (TEC) features as supporting indices.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016Tectp.681..135A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016Tectp.681..135A"><span>The Galicia-Ossa-Morena <span class="hlt">Zone</span>: Proposal for a new <span class="hlt">zone</span> of the Iberian Massif. Variscan implications</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Arenas, Ricardo; Díez Fernández, Rubén; Rubio Pascual, Francisco J.; Sánchez Martínez, Sonia; Martín Parra, Luis Miguel; Matas, Jerónimo; González del Tánago, José; Jiménez-Díaz, Alberto; Fuenlabrada, Jose M.; Andonaegui, Pilar; Garcia-Casco, Antonio</p> <p>2016-06-01</p> <p>Correlation of a group of allochthonous terranes (referred to as basal, ophiolitic and upper units) exposed in the NW and SW of the Iberian Massif, is used to propose a new geotectonic <span class="hlt">zone</span> in the southern branch of the Variscan Orogen: the Galicia-Ossa-Morena <span class="hlt">Zone</span>. Recent advances in SW Iberia identify most of the former Ossa-Morena <span class="hlt">Zone</span> as another allochthonous complex of the Iberian Massif, the Ossa-Morena Complex, equivalent to the Cabo Ortegal, Órdenes, Malpica-Tui, Bragança and Morais complexes described in NW Iberia. The new geotectonic <span class="hlt">zone</span> and its counterparts along the rest of the Variscan Orogen constitute an Internal Variscan <span class="hlt">Zone</span> with ophiolites and units affected by high-P metamorphism. The Galicia-Ossa-Morena <span class="hlt">Zone</span> includes a Variscan suture and pieces of continental crust bearing the imprint of Ediacaran-Cambrian <span class="hlt">events</span> related to the activity of peri-Gondwanan magmatic arcs (Cadomian orogenesis). In the Iberian Massif, the general structure of this geotectonic <span class="hlt">zone</span> represents a duplication of the Gondwanan platform, the outboard sections being juxtaposed on top of domains located closer to the mainland before amalgamation. This interpretation offers an explanation that overcomes some issues regarding the differences between the stratigraphic and paleontological record of the central and southern sections of the Iberian Massif. Also, equivalent structural relationships between other major geotectonic domains of the rest of the Variscan Orogen are consistent with our interpretation and allow suspecting similar configurations along strike of the orogen. A number of issues may be put forward in this respect that potentially open new lines of thinking about the architecture of the Variscan Orogen.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/28379077','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/28379077"><span>Perils of using speed <span class="hlt">zone</span> data to assess real-world compliance to speed limits.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Chevalier, Anna; Clarke, Elizabeth; Chevalier, Aran John; Brown, Julie; Coxon, Kristy; Ivers, Rebecca; Keay, Lisa</p> <p>2017-11-17</p> <p>Real-world driving studies, including those involving speeding alert devices and autonomous vehicles, can gauge an individual vehicle's speeding behavior by comparing measured speed with mapped speed <span class="hlt">zone</span> data. However, there are complexities with developing and maintaining a database of mapped speed <span class="hlt">zones</span> over a large geographic area that may lead to inaccuracies within the data set. When this approach is applied to large-scale real-world driving data or speeding alert device data to determine speeding behavior, these inaccuracies may result in invalid identification of speeding. We investigated speeding <span class="hlt">events</span> based on service provider speed <span class="hlt">zone</span> data. We compared service provider speed <span class="hlt">zone</span> data (Speed Alert by Smart Car Technologies Pty Ltd., Ultimo, NSW, Australia) against a second set of speed <span class="hlt">zone</span> data (Google Maps Application Programming Interface [API] mapped speed <span class="hlt">zones</span>). We found a systematic error in the <span class="hlt">zones</span> where speed limits of 50-60 km/h, typical of local roads, were allocated to high-speed motorways, which produced false speed limits in the speed <span class="hlt">zone</span> database. The result was detection of false-positive high-range speeding. Through comparison of the service provider speed <span class="hlt">zone</span> data against a second set of speed <span class="hlt">zone</span> data, we were able to identify and eliminate data most affected by this systematic error, thereby establishing a data set of speeding <span class="hlt">events</span> with a high level of sensitivity (a true positive rate of 92% or 6,412/6,960). Mapped speed <span class="hlt">zones</span> can be a source of error in real-world driving when examining vehicle speed. We explored the types of inaccuracies found within speed <span class="hlt">zone</span> data and recommend that a second set of speed <span class="hlt">zone</span> data be utilized when investigating speeding behavior or developing mapped speed <span class="hlt">zone</span> data to minimize inaccuracy in estimates of speeding.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25044878','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25044878"><span>The cumulative impact of <span class="hlt">annual</span> coral bleaching can turn some coral species winners into losers.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Grottoli, Andréa G; Warner, Mark E; Levas, Stephen J; Aschaffenburg, Matthew D; Schoepf, Verena; McGinley, Michael; Baumann, Justin; Matsui, Yohei</p> <p>2014-12-01</p> <p>Mass coral bleaching <span class="hlt">events</span> caused by elevated seawater temperatures result in extensive coral loss throughout the tropics, and are projected to increase in frequency and severity. If bleaching becomes an <span class="hlt">annual</span> <span class="hlt">event</span> later in this century, more than 90% of coral reefs worldwide may be at risk of long-term degradation. While corals can recover from single isolated bleaching and can acclimate to recurring bleaching <span class="hlt">events</span> that are separated by multiple years, it is currently unknown if and how they will survive and possibly acclimatize to <span class="hlt">annual</span> coral bleaching. Here, we demonstrate for the first time that <span class="hlt">annual</span> coral bleaching can dramatically alter thermal tolerance in Caribbean corals. We found that high coral energy reserves and changes in the dominant algal endosymbiont type (Symbiodinium spp.) facilitated rapid acclimation in Porites divaricata, whereas low energy reserves and a lack of algal phenotypic plasticity significantly increased susceptibility in Porites astreoides to bleaching the following year. Phenotypic plasticity in the dominant endosymbiont type of Orbicella faveolata did not prevent repeat bleaching, but may have facilitated rapid recovery. Thus, coral holobiont response to an isolated single bleaching <span class="hlt">event</span> is not an accurate predictor of its response to bleaching the following year. Rather, the cumulative impact of <span class="hlt">annual</span> coral bleaching can turn some coral species 'winners' into 'losers', and can also facilitate acclimation and turn some coral species 'losers' into 'winners'. Overall, these findings indicate that cumulative impact of <span class="hlt">annual</span> coral bleaching could result in some species becoming increasingly susceptible to bleaching and face a long-term decline, while phenotypically plastic coral species will acclimatize and persist. Thus, <span class="hlt">annual</span> coral bleaching and recovery could contribute to the selective loss of coral diversity as well as the overall decline of coral reefs in the Caribbean. © 2014 John Wiley & Sons Ltd.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-01-18/pdf/2012-787.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-01-18/pdf/2012-787.pdf"><span>77 FR 2453 - Security <span class="hlt">Zone</span>; 24th <span class="hlt">Annual</span> North American International Auto Show, Detroit River, Detroit, MI</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-01-18</p> <p>... Docket Management Facility (M-30), U.S. Department of Transportation, West Building Ground Floor, Room.... The security <span class="hlt">zone</span> will encompass an area of the Detroit River beginning at a point of origin on land... shoreline to connect back to the point of origin. Vessels in close proximity to the security <span class="hlt">zone</span> will be...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_16");'>16</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li class="active"><span>18</span></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_18 --> <div id="page_19" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li class="active"><span>19</span></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="361"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://images.nasa.gov/#/details-ARC-20160309-AAV2833-CAAerospaceDay-RptrPkg-NASAWeb.html','SCIGOVIMAGE-NASA'); return false;" href="https://images.nasa.gov/#/details-ARC-20160309-AAV2833-CAAerospaceDay-RptrPkg-NASAWeb.html"><span>NASA Participates in 5th <span class="hlt">Annual</span> California Aerospace Week</span></a></p> <p><a target="_blank" href="https://images.nasa.gov/">NASA Image and Video Library</a></p> <p></p> <p>2016-03-03</p> <p>The fifth <span class="hlt">annual</span> California Aerospace Days <span class="hlt">event</span> was recently held at the Capitol in Sacramento. It was an opportunity for NASA's Ames Research Center to showcase some of its key achievements and innovations in the Golden State.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.T51E0532K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.T51E0532K"><span>Detection of Repeating Earthquakes within the Cascadia Subduction <span class="hlt">Zone</span> Using 2013-2014 Cascadia Initiative Amphibious Network Data</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kenefic, L.; Morton, E.; Bilek, S.</p> <p>2017-12-01</p> <p>It is well known that subduction <span class="hlt">zones</span> create the largest earthquakes in the world, like the magnitude 9.5 Chile earthquake in 1960, or the more recent 9.1 magnitude Japan earthquake in 2011, both of which are in the top five largest earthquakes ever recorded. However, off the coast of the Pacific Northwest region of the U.S., the Cascadia subduction <span class="hlt">zone</span> (CSZ) remains relatively quiet and modern seismic instruments have not recorded earthquakes of this size in the CSZ. The last great earthquake, a magnitude 8.7-9.2, occurred in 1700 and is constrained by written reports of the resultant tsunami in Japan and dating a drowned forest in the U.S. Previous studies have suggested the margin is most likely segmented along-strike. However, variations in frictional conditions in the CSZ fault <span class="hlt">zone</span> are not well known. Geodetic modeling indicates that the locked seismogenic <span class="hlt">zone</span> is likely completely offshore, which may be too far from land seismometers to adequately detect related seismicity. Ocean bottom seismometers, as part of the Cascadia Initiative Amphibious Network, were installed directly above the inferred seismogenic <span class="hlt">zone</span>, which we use to better detect small interplate seismicity. Using the subspace detection method, this study looks to find new seismogenic <span class="hlt">zone</span> earthquakes. This subspace detection method uses multiple previously known <span class="hlt">event</span> templates concurrently to scan through continuous seismic data. Template <span class="hlt">events</span> that make up the subspace are chosen from <span class="hlt">events</span> in existing catalogs that likely occurred along the plate interface. Corresponding waveforms are windowed on the nearby Cascadia Initiative ocean bottom seismometers and coastal land seismometers for scanning. Detections that are found by the scan are similar to the template waveforms based upon a predefined threshold. Detections are then visually examined to determine if an <span class="hlt">event</span> is present. The presence of repeating <span class="hlt">event</span> clusters can indicate persistent seismic patches, likely corresponding to</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.C51B0976R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.C51B0976R"><span>Velocity Field of the McMurdo Shear <span class="hlt">Zone</span> from <span class="hlt">Annual</span> Three-Dimensional Ground Penetrating Radar Imaging and Crevasse Matching</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ray, L.; Jordan, M.; Arcone, S. A.; Kaluzienski, L. M.; Koons, P. O.; Lever, J.; Walker, B.; Hamilton, G. S.</p> <p>2017-12-01</p> <p>The McMurdo Shear <span class="hlt">Zone</span> (MSZ) is a narrow, intensely crevassed strip tens of km long separating the Ross and McMurdo ice shelves (RIS and MIS) and an important pinning feature for the RIS. We derive local velocity fields within the MSZ from two consecutive <span class="hlt">annual</span> ground penetrating radar (GPR) datasets that reveal complex firn and marine ice crevassing; no englacial features are evident. The datasets were acquired in 2014 and 2015 using robot-towed 400 MHz and 200 MHz GPR over a 5 km x 5.7 km grid. 100 west-to-east transects at 50 m spacing provide three-dimensional maps that reveal the length of many firn crevasses, and their year-to-year structural evolution. Hand labeling of crevasse cross sections near the MSZ western and eastern boundaries reveal matching firn and marine ice crevasses, and more complex and chaotic features between these boundaries. By matching crevasse features from year to year both on the eastern and western boundaries and within the chaotic region, marine ice crevasses along the western and eastern boundaries are shown to align directly with firn crevasses, and the local velocity field is estimated and compared with data from strain rate surveys and remote sensing. While remote sensing provides global velocity fields, crevasse matching indicates greater local complexity attributed to faulting, folding, and rotation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29247158','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29247158"><span>Hydrologically-driven crustal stresses and seismicity in the New Madrid Seismic <span class="hlt">Zone</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Craig, Timothy J; Chanard, Kristel; Calais, Eric</p> <p>2017-12-15</p> <p>The degree to which short-term non-tectonic processes, either natural and anthropogenic, influence the occurrence of earthquakes in active tectonic settings or 'stable' plate interiors, remains a subject of debate. Recent work in plate-boundary regions demonstrates the capacity for long-wavelength changes in continental water storage to produce observable surface deformation, induce crustal stresses and modulate seismicity rates. Here we show that a significant variation in the rate of microearthquakes in the intraplate New Madrid Seismic <span class="hlt">Zone</span> at <span class="hlt">annual</span> and multi-<span class="hlt">annual</span> timescales coincides with hydrological loading in the upper Mississippi embayment. We demonstrate that this loading, which results in geodetically observed surface deformation, induces stresses within the lithosphere that, although of small amplitude, modulate the ongoing seismicity of the New Madrid region. Correspondence between surface deformation, hydrological loading and seismicity rates at both <span class="hlt">annual</span> and multi-<span class="hlt">annual</span> timescales indicates that seismicity variations are the direct result of elastic stresses induced by the water load.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70029713','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70029713"><span>GSA committees: Progress through service the <span class="hlt">Annual</span> Program Committee</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Costa, J.E.</p> <p>2007-01-01</p> <p>The GSA's <span class="hlt">Annual</span> Program Committee (APC) is directly responsible for the GSA's meeting and other responsibilities especially before the main <span class="hlt">event</span>. It decides on the locations, the number and content of the technical sessions, <span class="hlt">annual</span> membership surveys, hospitality for the guests, field trips and more. In addition, it pays significant attention to creative thinking about geoscience discoveries and directions as well as identify new and emerging areas of earth science. APC is also looking for new ideas, approaches and directions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-05-16/pdf/2012-11809.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-05-16/pdf/2012-11809.pdf"><span>77 FR 28766 - Eighth Coast Guard District <span class="hlt">Annual</span> Marine <span class="hlt">Events</span> and Safety <span class="hlt">Zones</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-05-16</p> <p>... adverse comment or notice of intent to submit an adverse comment was received. The rule will go into... docket, go to http://www.regulations.gov , type the docket number (USCG-2011-0286) in the ``SEARCH'' box...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-03-01/pdf/2012-4930.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-03-01/pdf/2012-4930.pdf"><span>77 FR 12456 - Eighth Coast Guard District <span class="hlt">Annual</span> Marine <span class="hlt">Events</span> and Safety <span class="hlt">Zones</span></span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-03-01</p> <p>... restricting and governing vessel movements are also short in duration. Additionally, the public is given.... Protection of Children We have analyzed this rule under Executive Order 13045, Protection of Children from... create an environmental risk to health or risk to safety that may disproportionately affect children...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.C53B1034S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.C53B1034S"><span>Spatiotemporal Variability of Great Lakes Basin Snow Cover Ablation <span class="hlt">Events</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Suriano, Z. J.; Leathers, D. J.</p> <p>2017-12-01</p> <p>In the Great Lakes basin of North America, <span class="hlt">annual</span> runoff is dominated by snowmelt. This snowmelt-induced runoff plays an important role within the hydrologic cycle of the basin, influencing soil moisture availability and driving the seasonal cycle of spring and summer Lake levels. Despite this, relatively little is understood about the patterns and trends of snow ablation <span class="hlt">event</span> frequency and magnitude within the Great Lakes basin. This study uses a gridded dataset of Canadian and United States surface snow depth observations to develop a regional climatology of snow ablation <span class="hlt">events</span> from 1960-2009. An ablation <span class="hlt">event</span> is defined as an inter-diurnal snow depth decrease within an individual grid cell. A clear seasonal cycle in ablation <span class="hlt">event</span> frequency exists within the basin and peak ablation <span class="hlt">event</span> frequency is latitudinally dependent. Most of the basin experiences peak ablation frequency in March, while the northern and southern regions of the basin experience respective peaks in April and February. An investigation into the inter-<span class="hlt">annual</span> frequency of ablation <span class="hlt">events</span> reveals ablation <span class="hlt">events</span> significantly decrease within the northeastern and northwestern Lake Superior drainage basins and significantly increase within the eastern Lake Huron and Georgian Bay drainage basins. In the eastern Lake Huron and Georgian Bay drainage basins, larger ablation <span class="hlt">events</span> are occurring more frequently, and a larger impact to the hydrology can be expected. Trends in ablation <span class="hlt">events</span> are attributed primarily to changes in snowfall and snow depth across the region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/22391502-prediction-subsurface-fracture-mining-zone-papua-using-passive-seismic-tomography-based-fresnel-zone','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/22391502-prediction-subsurface-fracture-mining-zone-papua-using-passive-seismic-tomography-based-fresnel-zone"><span>Prediction of subsurface fracture in mining <span class="hlt">zone</span> of Papua using passive seismic tomography based on Fresnel <span class="hlt">zone</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Setiadi, Herlan; Nurhandoko, Bagus Endar B.; Wely, Woen</p> <p></p> <p>Fracture prediction in a block cave of underground mine is very important to monitor the structure of the fracture that can be harmful to the mining activities. Many methods can be used to obtain such information, such as TDR (Time Domain Relectometry) and open hole. Both of them have limitations in range measurement. Passive seismic tomography is one of the subsurface imaging method. It has advantage in terms of measurements, cost, and rich of rock physical information. This passive seismic tomography studies using Fresnel <span class="hlt">zone</span> to model the wavepath by using frequency parameter. Fresnel <span class="hlt">zone</span> was developed by Nurhandoko inmore » 2000. The result of this study is tomography of P and S wave velocity which can predict position of fracture. The study also attempted to use sum of the wavefronts to obtain position and time of seismic <span class="hlt">event</span> occurence. Fresnel <span class="hlt">zone</span> tomography and the summation wavefront can predict location of geological structure of mine area as well.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?direntryid=335670&keyword=air&subject=air%20research&showcriteria=2&fed_org_id=111&datebeginpublishedpresented=11/18/2011&dateendpublishedpresented=11/18/2016&sortby=pubdateyear','PESTICIDES'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?direntryid=335670&keyword=air&subject=air%20research&showcriteria=2&fed_org_id=111&datebeginpublishedpresented=11/18/2011&dateendpublishedpresented=11/18/2016&sortby=pubdateyear"><span>Air Quality Side <span class="hlt">Event</span> Proposal November 2016 GEO XIII ...</span></a></p> <p><a target="_blank" href="http://www.epa.gov/pesticides/search.htm">EPA Pesticide Factsheets</a></p> <p></p> <p></p> <p>The Group on Earth Observations (GEO), which EPA has participated in since 2003, has put out a call for Side <span class="hlt">Events</span> for its thirteenth <span class="hlt">annual</span> international Plenary Meeting which is in St. Petersburg, Russia this year during November, 2016. EPA has put on Side <span class="hlt">Events</span> on Air Quality and Health observational systems at eight of the previous Plenaries. This document is a Side <span class="hlt">Event</span> proposal regarding air quality, health and next generation monitoring and observations techniques. It is submitted to the GEO Secretariat for consideration. If accepted, there will likely be presentations by EPA and NASA, other GEO Member Countries and UNEP and other GEO Participating Organizations at the Side <span class="hlt">Event</span>. It is an opportunity to share scientific and technological advances in this area and build partnerships and collaboration. The Group on Earth Observations (GEO), which EPA has participated in since 2003, has put out a call for Side <span class="hlt">Events</span> for its thirteenth <span class="hlt">annual</span> international Plenary Meeting which is in St. Petersburg, Russia this year during November, 2016. EPA has put on Side <span class="hlt">Events</span> on Air Quality and Health observational systems at eight of the previous Plenaries. This document is a Side <span class="hlt">Event</span> proposal regarding air quality, health and next generation monitoring and observations techniques.  It is submitted to the GEO Secretariat for consideration. If accepted, there will likely be presentations by EPA and NASA, other GEO Member Countries and UNEP and other GEO P</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/1401','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/1401"><span>The Dynamics of Two Hybrid <span class="hlt">Zones</span> in Appalachian Salamanders of the Genus Plethodon</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Nelson G. Hairston; R. Haven Wiley; Charles K. Smith; Kenneth A. Kneidel</p> <p>1992-01-01</p> <p>Two <span class="hlt">zones</span> of intergradation between populations of Plethodon have been studied for 18 and 20 years, respectively. The data consist of systematic scores of colors, made at least twice <span class="hlt">annually</span>. Near Heintooga Overlook in the Balsam Mountains (Great Smoky Mountains National Park), the salamanders' cheeks are gray. Proceeding north toward the...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/973168','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/973168"><span><span class="hlt">Annual</span> Report for Gravity Collection Lysimeter Monitoring Plan- ERDF Cells 5 and 6, CY 2008</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>R. L. Weiss; D. W. Woolery</p> <p>2009-08-25</p> <p>The purpose of this <span class="hlt">annual</span> report is to evaluate the conditions and identify trends to develop Hanford site-specific data on the performance of the lysimeter systems related to the vadose <span class="hlt">zone</span> monitoring and potential future use of lysimeter systems.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-10-04/pdf/2011-25547.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-10-04/pdf/2011-25547.pdf"><span>76 FR 61261 - Safety <span class="hlt">Zone</span>; IJSBA World Finals; Lower Colorado River, Lake Havasu, AZ</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-10-04</p> <p>...-AA00 Safety <span class="hlt">Zone</span>; IJSBA World Finals; Lower Colorado River, Lake Havasu, AZ AGENCY: Coast Guard, DHS... Boating Association (IJSBA) World Finals. This temporary safety <span class="hlt">zone</span> is necessary to provide for the... The International Jet Sports Boating Association is sponsoring the IJSBA World Finals. The <span class="hlt">event</span> will...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-11-27/pdf/2013-28360.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-11-27/pdf/2013-28360.pdf"><span>78 FR 70901 - Safety <span class="hlt">Zone</span>; Bone Island Triathlon, Atlantic Ocean; Key West, FL</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-11-27</p> <p>... 1625-AA00 Safety <span class="hlt">Zone</span>; Bone Island Triathlon, Atlantic Ocean; Key West, FL AGENCY: Coast Guard, DHS... <span class="hlt">zone</span> on the waters of the Atlantic Ocean in Key West, Florida, during the Bone Island Triathlon on... <span class="hlt">event</span>. C. Discussion of Proposed Rule On January 25, 2014, Questor Multisport, LLC. is hosting the Bone...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-11-05/pdf/2013-26394.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-11-05/pdf/2013-26394.pdf"><span>78 FR 66269 - Safety <span class="hlt">Zone</span>, Sea World Fireworks; Mission Bay, San Diego, CA</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-11-05</p> <p>...-AA00 Safety <span class="hlt">Zone</span>, Sea World Fireworks; Mission Bay, San Diego, CA AGENCY: Coast Guard, DHS. ACTION... waters of Mission Bay in San Diego, California for Sea World Fireworks on the evenings of November 15 and... firework <span class="hlt">event</span> that is part of Sea World Christmas festivities. This safety <span class="hlt">zone</span> is necessary to provide...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFMNH13A3719R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFMNH13A3719R"><span>Unrevealing the History of Earthquakes and Tsunamis of the Mexican Subduction <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ramirez-Herrera, M. T.; Castillo-Aja, M. D. R.; Cruz, S.; Corona, N.; Rangel Velarde, V.; Lagos, M.</p> <p>2014-12-01</p> <p>The great earthquakes and tsunamis of the last decades in Sumatra, Chile, and Japan remind us of the need for expanding the record of history of such catastrophic <span class="hlt">events</span>. It can't be argued that even countries with extensive historical documents and tsunami sand deposits still have unsolved questions on the frequency of them, and the variables that control them along subduction <span class="hlt">zones</span>. We present here preliminary results of a combined approach using historical archives and multiple proxies of the sedimentary record to unrevealing the history of possible great earthquakes and their tsunamis on the Mexican Subduction <span class="hlt">zone</span>. The Mexican subduction <span class="hlt">zone</span> extends over 1000 km long and little is known if the entire subduction <span class="hlt">zone</span> along the Middle American Trench behaves as one enormous unit rather than in segments that rupture at different frequencies and with different strengths (as the short instrumental record shows). We searched on historical archives and earthquake databases to distinguish tsunamigenic <span class="hlt">events</span> registered from the 16th century to now along the Jalisco-Colima and Guerrero-Oaxaca coastal stretches. The historical data referred are mostly from the 19th century on since the population on the coast was scarce before. We found 21 earthquakes with tsunamigenic potential, and of those 16 with doubtful to definitive accompanying tsunami on the Jalisco-Colima coast, and 31 tsunamigenic earthquakes on the Oaxaca-Guerrero coast. Evidence of great earthquakes and their tsunamis from the sedimentary record are scarce, perhaps due poor preservation of tsunami deposits in this tropical environment. Nevertheless, we have found evidence for a number of tsunamigenic <span class="hlt">events</span>, both historical and prehistorical, 1932 and 1400 AD on Jalisco, and 3400 BP, 1789 AD, 1979 ad, and 1985 AD on Guerrero-Oaxaca. We continue working and a number of <span class="hlt">events</span> are still to be dated. This work would aid in elucidating the history of earthquakes and tsunamis on the Mexican subduction <span class="hlt">zone</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFM.A13E0319S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFM.A13E0319S"><span>Inter-<span class="hlt">annual</span> Variability of Temperature and Extreme Heat <span class="hlt">Events</span> during the Nairobi Warm Season</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Scott, A.; Misiani, H. O.; Zaitchik, B. F.; Ouma, G. O.; Anyah, R. O.; Jordan, A.</p> <p>2016-12-01</p> <p>Extreme heat <span class="hlt">events</span> significantly stress all organisms in the ecosystem, and are likely to be amplified in peri-urban and urban areas. Understanding the variability and drivers behind these <span class="hlt">events</span> is key to generating early warnings, yet in Equatorial East Africa, this information is currently unavailable. This study uses daily maximum and minimum temperature records from weather stations within Nairobi and its surroundings to characterize variability in daily minimum temperatures and the number of extreme heat <span class="hlt">events</span>. ERA-Interim reanalysis is applied to assess the drivers of these <span class="hlt">events</span> at <span class="hlt">event</span> and seasonal time scales. At seasonal time scales, high temperatures in Nairobi are a function of large scale climate variability associated with the Atlantic Multi-decadal Oscillation (AMO) and Global Mean Sea Surface Temperature (GMSST). Extreme heat <span class="hlt">events</span>, however, are more strongly associated with the El Nino Southern Oscillation (ENSO). For instance, the persistence of AMO and ENSO, in particular, provide a basis for seasonal prediction of extreme heat <span class="hlt">events</span>/days in Nairobi. It is also apparent that the temporal signal from extreme heat <span class="hlt">events</span> in tropics differs from classic heat wave definitions developed in the mid-latitudes, which suggests that a new approach for defining these <span class="hlt">events</span> is necessary for tropical regions.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014ACPD...1417331D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014ACPD...1417331D"><span>Long-term variability of dust <span class="hlt">events</span> in Iceland (1949-2011)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dagsson-Waldhauserova, P.; Arnalds, O.; Olafsson, H.</p> <p>2014-06-01</p> <p>Long-term frequency of atmospheric dust observations was investigated for the southern part of Iceland and merged with results obtained from the Northeast Iceland (Dagsson-Waldhauserova et al., 2013). In total, over 34 dust days per year on average occurred in Iceland based on conventionally used synoptic codes for dust. Including codes 04-06 into the criteria for dust observations, the frequency was 135 dust days <span class="hlt">annually</span>. The Sea Level Pressure (SLP) oscillation controlled whether dust <span class="hlt">events</span> occurred in NE (16.4 dust days <span class="hlt">annually</span>) or in southern part of Iceland (about 18 dust days <span class="hlt">annually</span>). The most dust-frequent decade in S Iceland was the 1960s while the most frequent decade in NE Iceland was the 2000s. A total of 32 severe dust storms (visibility < 500 m) was observed in Iceland with the highest frequency during the 2000s in S Iceland. The Arctic dust <span class="hlt">events</span> (NE Iceland) were typically warm and during summer/autumn (May-September) while the Sub-Arctic dust <span class="hlt">events</span> (S Iceland) were mainly cold and during winter/spring (March-May). About half of dust <span class="hlt">events</span> in S Iceland occurred in winter or at sub-zero temperatures. A good correlation was found between PM10 concentrations and visibility during dust observations at the stations Vik and Storhofdi. This study shows that Iceland is among the dustiest areas of the world and dust is emitted the year-round.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007AGUFM.T51D0764L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007AGUFM.T51D0764L"><span>Possible Non-volcanic Tremor Discovered in the Reelfoot Fault <span class="hlt">Zone</span>, Northern Tennessee</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Langston, C. A.; Williams, R. A.; Magnani, M.; Rieger, D. M.</p> <p>2007-12-01</p> <p>A swarm of ~80 microearthquakes was fortuitously detected in 20, 14 second-duration long-offset vibroseis shotgathers collected for a seismic reflection experiment near Mooring, TN, directly over the Reelfoot fault <span class="hlt">zone</span> on the afternoon of 16 November 2006. These natural <span class="hlt">events</span> show up in the shotgathers as near-vertically incident P waves with a dominant frequency of 10-15 Hz. The reflection line was 715m in length consisting of 144 channels with a sensor spacing of 5m, 8Hz vertical geophones, and recording using a Geometrics 24bit Geode seismograph. Small variations in <span class="hlt">event</span> moveout across the linear array indicate that the seismicity was not confined to the same hypocenter and probably occurred at depths of approximately 10 km. The largest <span class="hlt">events</span> in the series are estimated to have local magnitudes of ~-1 if at 10 km distance from the array. This is about 2.5 magnitude units lower than the threshold for local <span class="hlt">events</span> detected and located by the CERI cooperative network in the area. The seismicity rate was ~1000 <span class="hlt">events</span> per hour based on the total time duration of the shotgathers. The expected number of earthquakes of ML greater than or equal to -1 for the entire central United States is only 1 per hour. This detection of microseismic swarms in the Reelfoot fault <span class="hlt">zone</span> indicates active physical processes that may be similar to non-volcanic tremor seen in the Cascadia and San Andreas fault <span class="hlt">zones</span> and merits long-term monitoring to understand its source.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFM.S24A..03M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFM.S24A..03M"><span>Limits on great earthquake size at subduction <span class="hlt">zones</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>McCaffrey, R.</p> <p>2012-12-01</p> <p>Subduction <span class="hlt">zones</span> are where the world's greatest earthquakes occur due to the large fault area available to slip. Yet some subduction <span class="hlt">zones</span> are thought to be immune from these massive <span class="hlt">events</span>, where quake size is limited by some physical processes or properties. Accordingly, the size of the 2011 Tohoku-oki Mw 9.0 earthquake caught some in the earthquake research community by surprise. The expectations of these massive quakes have been driven in the past by reliance on our short, incomplete history of earthquakes and causal relationships derived from it. The logic applied is that if a great earthquake has not happened in the past, that we know of, one cannot happen in the future. Using the ~100-year global earthquake seismological history, and in some cases extended with geologic observations, relationships between maximum earthquake sizes and other properties of subduction <span class="hlt">zones</span> are suggested, leading to the notion that some subduction <span class="hlt">zones</span>, like the Japan Trench, would never produce a magnitude ~9 <span class="hlt">event</span>. Empirical correlations of earthquake behavior with other subduction parameters can give false positive results when the data are incomplete or incorrect, of small numbers and numerous attributes are examined. Given multi-century return times of the greatest earthquakes, ignorance of those return times and our relatively limited temporal observation span (in most places), I suggest that we cannot yet rule out great earthquakes at any subduction <span class="hlt">zones</span>. Alternatively, using the length of a subduction <span class="hlt">zone</span> that is available for slip as the predominant factor in determining maximum earthquake size, we cannot rule out that any subduction <span class="hlt">zone</span> of a few hundred kilometers or more in length may be capable of producing a magnitude 9 or larger earthquake. Based on this method, the expected maximum size for the Japan Trench was 9.0 (McCaffrey, Geology, p. 263, 2008). The same approach indicates that a M > 9 off Java, with twice the population density as Honshu and much lower</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_17");'>17</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li class="active"><span>19</span></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_19 --> <div id="page_20" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li class="active"><span>20</span></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="381"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-02-10/pdf/2012-3085.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-02-10/pdf/2012-3085.pdf"><span>77 FR 7025 - Safety <span class="hlt">Zones</span>; America's Cup World Series, East Passage, Narragansett Bay, RI</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-02-10</p> <p>...-AA00 Safety <span class="hlt">Zones</span>; America's Cup World Series, East Passage, Narragansett Bay, RI AGENCY: Coast Guard... the America's Cup World Series sailing vessel racing <span class="hlt">event</span>. This safety <span class="hlt">zone</span> is intended to safeguard... participants and spectators involved with the America's Cup World Series in the vicinity of Newport, RI...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-07-13/pdf/2012-17085.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-07-13/pdf/2012-17085.pdf"><span>77 FR 41271 - Safety <span class="hlt">Zone</span>; Newburgh to Beacon Swim, Newburgh, Hudson River, NY</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-07-13</p> <p>... 1625-AA00 Safety <span class="hlt">Zone</span>; Newburgh to Beacon Swim, Newburgh, Hudson River, NY AGENCY: Coast Guard, DHS... navigable waters of the Hudson River, NY in the vicinity of Newburgh, NY for the <span class="hlt">annual</span> Newburgh Beacon Swim... hazards associated with swimmers competing in a swim across the Hudson River. Persons and vessels are...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017Geomo.295..480C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017Geomo.295..480C"><span>A proposed cell model for multiple-occurrence regional landslide <span class="hlt">events</span>: Implications for landslide susceptibility mapping</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Crozier, M. J.</p> <p>2017-10-01</p> <p>Multiple-occurrence regional landslide <span class="hlt">events</span> (MORLEs) consist of hundreds to thousands of shallow landslides occurring more or less simultaneously within defined areas, ranging from tens to thousands of square kilometres. While MORLEs can be triggered by rainstorms and earthquakes, this paper is confined to those landslide <span class="hlt">events</span> triggered by rainstorms. Globally, MORLEs occur in a range of geological settings in areas of moderate to steep slopes subject to intense rainstorms. Individual landslides in rainstorm-triggered <span class="hlt">events</span> are dominantly small, shallow debris and earth flows, and debris and earth slides involving regolith or weathered bedrock. The model used to characterise these <span class="hlt">events</span> assumes that energy distribution within the <span class="hlt">event</span> area is represented on the land surface by a cell structure; with maximum energy expenditure within an identifiable core and rapid dissipation concentrically away from the centre. The version of the model presented here has been developed for rainfall-triggered landslide <span class="hlt">events</span>. It proposes that rainfall intensity can be used to determine different critical landslide response <span class="hlt">zones</span> within the cell (referred to as core, middle, and periphery <span class="hlt">zones</span>). These <span class="hlt">zones</span> are most readily distinguished by two conditions: the proportion of the slope that fails and the particular type of the slope stability factor that assumes dominance in determining specific sites of landslide occurrence. The latter condition means that the power of any slope stability factor to distinguish between stable and unstable sites varies throughout the affected area in accordance with the landslide response <span class="hlt">zones</span> within the cell; certain factors critical for determining the location of landslide sites in one part of the <span class="hlt">event</span> area have little influence in other parts of the <span class="hlt">event</span> area. The implication is that landslide susceptibility maps (and subsequently derived mitigation measures) based on conventional slope stability factors may have only limited validity</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70026109','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70026109"><span>Paleoearthquakes and Eolian-dominated fault sedimentation along the Hubbell Spring fault <span class="hlt">zone</span> near Albuquerque, New Mexico</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Personius, S.F.; Mahan, S.A.</p> <p>2003-01-01</p> <p>The Hubbell Spring fault <span class="hlt">zone</span> forms the modern eastern margin of the Rio Grande rift in the Albuquerque basin of north-central New Mexico. Knowledge of its seismic potential is important because the fault <span class="hlt">zone</span> transects Kirtland Air Force Base/Sandia National Laboratories and underlies the southern Albuquerque metropolitan area. No earthquakes larger than ML 5.5 have been reported in the last 150 years in this region, so we excavated the first trench across this fault <span class="hlt">zone</span> to determine its late Quaternary paleoseismic history. Our trench excavations revealed a complex, 16-m-wide fault <span class="hlt">zone</span> overlain by four tapered blankets of mixed eolian sand and minor colluvium that we infer were deposited after four large-magnitude, surface-rupturing earthquakes. Although the first (oldest) rupture <span class="hlt">event</span> is undated, we used luminescence (thermoluminescence and infrared-stimulated luminescence) ages to determine that the subsequent three rupture <span class="hlt">events</span> occurred about 56 ?? 6, 29 ?? 3, and 12 ?? 1 ka. These ages yield recurrence intervals of 27 and 17 k.y. between <span class="hlt">events</span> and an elapsed time of 12 k.y. since the latest surface-rupturing paleoearthquake. Slip rates are not well constrained, but our preferred average slip rate since rupture <span class="hlt">event</span> 2 (post-56 ka) is 0.05 mm/yr, and interval slip rates between the last three <span class="hlt">events</span> are 0.06 and 0.09 mm/yr, respectively. Vertical displacements of 1-2 m per <span class="hlt">event</span> and probable rupture lengths of 34-43 km indicate probable paleoearthquake magnitudes (Ms or Mw) of 6.8-7.1. Future earthquakes of this size likely would cause strong ground motions in the Albuquerque metropolitan area.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://images.nasa.gov/#/details-KSC-20161115-PH_KLS02_0143.html','SCIGOVIMAGE-NASA'); return false;" href="https://images.nasa.gov/#/details-KSC-20161115-PH_KLS02_0143.html"><span>34th <span class="hlt">Annual</span> SWAT Round-Up</span></a></p> <p><a target="_blank" href="https://images.nasa.gov/">NASA Image and Video Library</a></p> <p></p> <p>2016-11-15</p> <p>The entrance to the Lawson Lamar Firearms and Tactical Training Center in Orlando, Florida. NASA Kennedy Space Center's Emergency Response Team members will compete in the 34th <span class="hlt">Annual</span> SWAT Round-up International from Nov. 15 to 18. The <span class="hlt">event</span> features five different competition categories. Kennedy's ERT members exchanged best practices and competed with 60 teams from the U.S. and around the world.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016SPIE.9842E..1MF','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016SPIE.9842E..1MF"><span>Information fusion for the Gray <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fenstermacher, Laurie</p> <p>2016-05-01</p> <p>United States Special Operations Command (SOCOM) recently published a white paper describing the "Gray <span class="hlt">Zone</span>", security challenges characterized by "ambiguity about the nature of the conflict, opacity of the parties involved…competitive interactions among and within state and non-state actors that fall between the traditional war and peace duality."1 Ambiguity and related uncertainty about actors, situations, relationships, and intent require new approaches to information collection, processing and fusion. General Votel, the current SOCOM commander, during a recent speech on "Operating in the Gray <span class="hlt">Zone</span>" emphasized that it would be important to get left of the next crises and stated emphatically, "to do that we must understand the Human Domain."2 This understanding of the human domain must come from making meaning based on different perspectives, including the "emic" or first person/participant and "etic" or third person/observer perspectives. Much of the information currently collected and processed is etic. Incorporation and fusion with the emic perspective enables forecasting of behaviors/<span class="hlt">events</span> and provides context for etic information (e.g., video).3 Gray <span class="hlt">zone</span> challenges are perspective-dependent; for example, the conflict in Ukraine is interpreted quite differently by Russia, the US and Ukraine. Russia views it as war, necessitating aggressive action, the US views it as a security issue best dealt with by economic sanctions and diplomacy and the Ukraine views it as a threat to its sovereignty.4 General Otto in the Air Force ISR 2023 vision document stated that Air Force ISR is needed to anticipate strategic surprise.5 Anticipatory analysis enabling getting left of a crisis inherently requires a greater focus on information sources that elucidate the human environment as well as new methods that elucidate not only the "who's" and "what's", but the "how's and "why's," extracting features and/or patterns and subtle cues useful for forecasting behaviors and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFM.S53A2488S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFM.S53A2488S"><span>Comparisons of Source Characteristics between Recent Inland Crustal Earthquake Sequences inside and outside of Niigata-Kobe Tectonic <span class="hlt">Zone</span>, Japan</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Somei, K.; Asano, K.; Iwata, T.; Miyakoshi, K.</p> <p>2012-12-01</p> <p>After the 1995 Kobe earthquake, many M7-class inland earthquakes occurred in Japan. Some of those <span class="hlt">events</span> (e.g., the 2004 Chuetsu earthquake) occurred in a tectonic <span class="hlt">zone</span> which is characterized as a high strain rate <span class="hlt">zone</span> by the GPS observation (Sagiya et al., 2000) or dense distribution of active faults. That belt-like <span class="hlt">zone</span> along the coast in Japan Sea side of Tohoku and Chubu districts, and north of Kinki district, is called as the Niigata-Kobe tectonic <span class="hlt">zone</span> (NKTZ, Sagiya et al, 2000). We investigate seismic scaling relationship for recent inland crustal earthquake sequences in Japan and compare source characteristics between <span class="hlt">events</span> occurring inside and outside of NKTZ. We used S-wave coda part for estimating source spectra. Source spectral ratio is obtained by S-wave coda spectral ratio between the records of large and small <span class="hlt">events</span> occurring close to each other from nation-wide strong motion network (K-NET and KiK-net) and broad-band seismic network (F-net) to remove propagation-path and site effects. We carefully examined the commonality of the decay of coda envelopes between <span class="hlt">event</span>-pair records and modeled the observed spectral ratio by the source spectral ratio function with assuming omega-square source model for large and small <span class="hlt">events</span>. We estimated the corner frequencies and seismic moment (ratio) from those modeled spectral ratio function. We determined Brune's stress drops of 356 <span class="hlt">events</span> (Mw: 3.1-6.9) in ten earthquake sequences occurring in NKTZ and six sequences occurring outside of NKTZ. Most of source spectra obey omega-square source spectra. There is no obvious systematic difference between stress drops of <span class="hlt">events</span> in NKTZ <span class="hlt">zone</span> and others. We may conclude that the systematic tendency of seismic source scaling of the <span class="hlt">events</span> occurred inside and outside of NKTZ does not exist and the average source scaling relationship can be effective for inland crustal earthquakes. Acknowledgements: Waveform data were provided from K-NET, KiK-net and F-net operated by</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2004cosp...35..413P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2004cosp...35..413P"><span>Semi-<span class="hlt">annual</span> Sq-variation in solar activity cycle</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pogrebnoy, V.; Malosiev, T.</p> <p></p> <p>The peculiarities of semi-<span class="hlt">annual</span> variation in solar activity cycle have been studied. The data from observatories having long observational series and located in different latitude <span class="hlt">zones</span> were used. The following observatories were selected: Huancayo (magnetic equator), from 1922 to 1959; Apia (low latitudes), from 1912 to 1961; Moscow (middle latitudes), from 1947 to 1965. Based on the hourly values of H-components, the average monthly diurnal amplitudes (a difference between midday and midnight values), according to five international quiet days, were computed. Obtained results were compared with R (relative sunspot numbers) in the ranges of 0-30R, 40-100R, and 140-190R. It was shown, that the amplitude of semi-<span class="hlt">annual</span> variation increases with R, from minimum to maximum values, on average by 45%. At equatorial Huancayo observatory, the semi-<span class="hlt">annual</span> Sq(H)-variation appears especially clearly: its maximums take place at periods of equinoxes (March-April, September-October), and minimums -- at periods of solstices (June-July, December-January). At low (Apia observatory) and middle (Moscow observatory) latitudes, the character of semi-<span class="hlt">annual</span> variation is somewhat different: it appears during the periods of equinoxes, but considerably less than at equator. Besides, with the growth of R, semi-<span class="hlt">annual</span> variation appears against a background of <span class="hlt">annual</span> variation, in the form of second peaks (maximum in June). At observatories located in low and middle latitudes, second peaks become more appreciable with an increase of R (March-April and September-October). During the periods of low solar activity, they are insignificant. This work has been carried out with the support from International Scientific and Technology Center (Project #KR-214).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://ntrs.nasa.gov/search.jsp?R=19770059464&hterms=neither+deep+shallow&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Dneither%2Bdeep%2Bshallow','NASA-TRS'); return false;" href="https://ntrs.nasa.gov/search.jsp?R=19770059464&hterms=neither+deep+shallow&qs=Ntx%3Dmode%2Bmatchall%26Ntk%3DAll%26N%3D0%26No%3D30%26Ntt%3Dneither%2Bdeep%2Bshallow"><span>HFT <span class="hlt">events</span> - Shallow moonquakes. [High-Frequency Teleseismic</span></a></p> <p><a target="_blank" href="http://ntrs.nasa.gov/search.jsp">NASA Technical Reports Server (NTRS)</a></p> <p>Nakamura, Y.</p> <p>1977-01-01</p> <p>A few large distant seismic <span class="hlt">events</span> of distinctly high signal frequency, designated HFT (high-frequency teleseismic) <span class="hlt">events</span>, are observed yearly by the Apollo lunar seismic network. Their sources are located on or near the surface of the moon, leaving a large gap in seismic activity between the <span class="hlt">zones</span> of HFT sources and deep moonquakes. No strong regularities are found in either their spatial or temporal distributions. Several working hypotheses for the identity of these sources have advanced, but many characteristics of the <span class="hlt">events</span> seem to favor a hypothesis that they are shallow moonquakes. Simultaneous observations of other lunar phenomena may eventually enable the determination of their true identity.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.T41C0648L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.T41C0648L"><span>Fault <span class="hlt">zone</span> property near Xinfengjiang Reservoir using dense, across-fault seismic array</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lee, M. H. B.; Yang, H.; Sun, X.</p> <p>2017-12-01</p> <p>Properties of fault <span class="hlt">zones</span> are important to the understanding of earthquake process. Around the fault <span class="hlt">zone</span> is a damaged <span class="hlt">zone</span> which is characterised by a lower seismic velocity. This is detectable as a low velocity <span class="hlt">zone</span> and measure some physical property of the fault <span class="hlt">zone</span>, which is otherwise difficult sample directly. A dense, across-fault array of short period seismometer is deployed on an inactive fault near Xinfengjiang Reservoir. Local <span class="hlt">events</span> were manually picked. By computing the synthetic arrival time, we were able to constrain the parameters of the fault <span class="hlt">zone</span> Preliminary result shows that the fault <span class="hlt">zone</span> is around 350 m wide with a P and S velocity increase of around 10%. The fault is geologically inferred, and this result suggested that it may be a geological layer. The other possibility is that the higher velocity is caused by a combination of fault <span class="hlt">zone</span> healing and fluid intrusion. Whilst the result was not able to tell us the nature of the fault, it demonstrated that this method is able to derive properties from a fault <span class="hlt">zone</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24174659','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24174659"><span>Spontaneous and evoked release are independently regulated at individual active <span class="hlt">zones</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Melom, Jan E; Akbergenova, Yulia; Gavornik, Jeffrey P; Littleton, J Troy</p> <p>2013-10-30</p> <p>Neurotransmitter release from synaptic vesicle fusion is the fundamental mechanism for neuronal communication at synapses. Evoked release following an action potential has been well characterized for its function in activating the postsynaptic cell, but the significance of spontaneous release is less clear. Using transgenic tools to image single synaptic vesicle fusion <span class="hlt">events</span> at individual release sites (active <span class="hlt">zones</span>) in Drosophila, we characterized the spatial and temporal dynamics of exocytotic <span class="hlt">events</span> that occur spontaneously or in response to an action potential. We also analyzed the relationship between these two modes of fusion at single release sites. A majority of active <span class="hlt">zones</span> participate in both modes of fusion, although release probability is not correlated between the two modes of release and is highly variable across the population. A subset of active <span class="hlt">zones</span> is specifically dedicated to spontaneous release, indicating a population of postsynaptic receptors is uniquely activated by this mode of vesicle fusion. Imaging synaptic transmission at individual release sites also revealed general rules for spontaneous and evoked release, and indicate that active <span class="hlt">zones</span> with similar release probability can cluster spatially within individual synaptic boutons. These findings suggest neuronal connections contain two information channels that can be spatially segregated and independently regulated to transmit evoked or spontaneous fusion signals.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2002AGUFMOS21B0197M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2002AGUFMOS21B0197M"><span>Biologically-Oriented Processes in the Coastal Sea Ice <span class="hlt">Zone</span> of the White Sea</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Melnikov, I. A.</p> <p>2002-12-01</p> <p>The <span class="hlt">annual</span> advance and retreat of sea ice is a major physical determinant of spatial and temporal changes in the structure and function of marine coastal biological communities. Sea ice biological data obtained in the tidal <span class="hlt">zone</span> of Kandalaksha Gulf (White Sea) during 1996-2001 period will be presented. Previous observations in this area were mainly conducted during the ice-free summer season. However, there is little information on the ice-covered winter season (6-7 months duration), and, especially, on the sea-ice biology in the coastal <span class="hlt">zone</span> within tidal regimes. During the January-May period time-series observations were conducted on transects along shorelines with coastal and fast ice. Trends in the <span class="hlt">annual</span> extent of sea ice showed significant impacts on ice-associated biological communities. Three types of sea ice impact on kelps, balanoides, littorinas and amphipods are distinguished: (i) positive, when sea ice protects these populations from grinding (ii) negative, when ice grinds both fauna and flora, and (iii) a combined effect, when fast ice protects, but anchored ice grinds plant and animals. To understand the full spectrum of ecological problems caused by pollution on the coastal <span class="hlt">zone</span>, as well as the problems of sea ice melting caused by global warming, an integrated, long-term study of the physical, chemical, and biological processes is needed.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70024397','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70024397"><span>The earthquake potential of the New Madrid seismic <span class="hlt">zone</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Tuttle, Martitia P.; Schweig, Eugene S.; Sims, John D.; Lafferty, Robert H.; Wolf, Lorraine W.; Haynes, Marion L.</p> <p>2002-01-01</p> <p>The fault system responsible for New Madrid seismicity has generated temporally clustered very large earthquakes in A.D. 900 ± 100 years and A.D. 1450 ± 150 years as well as in 1811–1812. Given the uncertainties in dating liquefaction features, the time between the past three New Madrid <span class="hlt">events</span> may be as short as 200 years and as long as 800 years, with an average of 500 years. This advance in understanding the Late Holocene history of the New Madrid seismic <span class="hlt">zone</span> and thus, the contemporary tectonic behavior of the associated fault system was made through studies of hundreds of earthquake-induced liquefaction features at more than 250 sites across the New Madrid region. We have found evidence that prehistoric sand blows, like those that formed during the 1811–1812 earthquakes, are probably compound structures resulting from multiple earthquakes closely clustered in time or earthquake sequences. From the spatial distribution and size of sand blows and their sedimentary units, we infer the source <span class="hlt">zones</span> and estimate the magnitudes of earthquakes within each sequence and thereby characterize the detailed behavior of the fault system. It appears that fault rupture was complex and that the central branch of the seismic <span class="hlt">zone</span> produced very large earthquakes during the A.D. 900 and A.D. 1450 <span class="hlt">events</span> as well as in 1811–1812. On the basis of a minimum recurrence rate of 200 years, we are now entering the period during which the next 1811–1812-type <span class="hlt">event</span> could occur.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015JGRG..120.2306H','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015JGRG..120.2306H"><span>Remote sensing-based estimation of <span class="hlt">annual</span> soil respiration at two contrasting forest sites</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Huang, Ni; Gu, Lianhong; Black, T. Andrew; Wang, Li; Niu, Zheng</p> <p>2015-11-01</p> <p>Soil respiration (Rs), an important component of the global carbon cycle, can be estimated using remotely sensed data, but the accuracy of this technique has not been thoroughly investigated. In this study, we proposed a methodology for the remote estimation of <span class="hlt">annual</span> Rs at two contrasting FLUXNET forest sites (a deciduous broadleaf forest and an evergreen needleleaf forest). A version of the Akaike's information criterion was used to select the best model from a range of models for <span class="hlt">annual</span> Rs estimation based on the remotely sensed data products from the Moderate Resolution Imaging Spectroradiometer and root-<span class="hlt">zone</span> soil moisture product derived from assimilation of the NASA Advanced Microwave Scanning Radiometer soil moisture products and a two-layer Palmer water balance model. We found that the Arrhenius-type function based on nighttime land surface temperature (LST-night) was the best model by comprehensively considering the model explanatory power and model complexity at the Missouri Ozark and BC-Campbell River 1949 Douglas-fir sites. In addition, a multicollinearity problem among LST-night, root-<span class="hlt">zone</span> soil moisture, and plant photosynthesis factor was effectively avoided by selecting the LST-night-driven model. Cross validation showed that temporal variation in Rs was captured by the LST-night-driven model with a mean absolute error below 1 µmol CO2 m-2 s-1 at both forest sites. An obvious overestimation that occurred in 2005 and 2007 at the Missouri Ozark site reduced the evaluation accuracy of cross validation because of summer drought. However, no significant difference was found between the Arrhenius-type function driven by LST-night and the function considering LST-night and root-<span class="hlt">zone</span> soil moisture. This finding indicated that the contribution of soil moisture to Rs was relatively small at our multiyear data set. To predict intersite Rs, maximum leaf area index (LAImax) was used as an upscaling factor to calibrate the site-specific reference respiration</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=%22career+and+technical+education%22&id=EJ981989','ERIC'); return false;" href="https://eric.ed.gov/?q=%22career+and+technical+education%22&id=EJ981989"><span><span class="hlt">Annual</span> Convention in St. Louis: A Dynamic Convergence</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Emeagwali, N. Susan</p> <p>2012-01-01</p> <p>Nearly 3,000 career and technical educators from across the country converged upon St. Louis, Missouri, for the premier professional development <span class="hlt">event</span> in career and technical education (CTE). The Association for Career and Technical Education (ACTE) held its <span class="hlt">Annual</span> Convention and Career Tech Expo November 17-19, bringing together teachers,…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015IJEaS.104..587S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015IJEaS.104..587S"><span>Structural evidence for slip partitioning and inclined dextral transpression along the SE Sanandaj-Sirjan <span class="hlt">zone</span>, Iran</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Shafiei Bafti, Shahram; Mohajjel, Mohammad</p> <p>2015-04-01</p> <p>The structural evolution of the Sanandaj-Sirjan <span class="hlt">zone</span> is the result of the convergence of the Iranian microcontinent and the Afro-Arabian continent. The study area at Khabr in the SE Sanandaj-Sirjan <span class="hlt">zone</span>, in the hinterland of the Zagros orogen, consists of Paleozoic, Mesozoic and Cenozoic rocks. In this area, deformation phases were distinguished in different rock units based on structural and stratigraphical evidence, and the deformational <span class="hlt">events</span> are divided into two stages: (1) a Late Triassic <span class="hlt">event</span> and (2) a Late Cretaceous to Miocene <span class="hlt">event</span>. The Late Triassic deformation <span class="hlt">event</span> caused regional metamorphism in the Paleozoic units. These units are overlain by unmetamorphosed Jurassic clastic sequences. Fabrics and structural evidence confirm that the F1 folding recumbent and refolded folds were synchronous with the metamorphism of the Paleozoic units and terminated in the Early Jurassic. The time table of the orogenic phases shows that this deformation <span class="hlt">event</span> is related to the Cimmerian orogenic phase. From a geodynamic point of view, the early Cimmerian deformation in the southeastern Iranian margin suggests that the SE Sanandaj-Sirjan <span class="hlt">zone</span> was an active margin at that time. The early Cimmerian discordance recorded the onset of a contractional component related to the oblique subduction of Neo-Tethys beneath the central Iranian microcontinent. Structures related to the Late Cretaceous to Miocene deformation phase are observed in Jurassic to Oligocene units, which contain moderately inclined and plunging folds. Comparing these folds with domains of deformation generated in models of transpression shows that the folding was caused by a combination of contractional and dip-slip components of movement, eventually resulting in the formation of a thrust system. The Khabr thrust systems consist of five sheets of oblique thrusts, duplex structures and shear <span class="hlt">zones</span>. The shear <span class="hlt">zones</span> generally strike E-W and dip moderately N (30°-40°). The occurrence of asymmetric folds with</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.fs.usda.gov/treesearch/pubs/36943','TREESEARCH'); return false;" href="https://www.fs.usda.gov/treesearch/pubs/36943"><span>Analysis of conifer mortality in Colorado using Forest Inventory and Analysis's <span class="hlt">annual</span> forest inventory</span></a></p> <p><a target="_blank" href="http://www.fs.usda.gov/treesearch/">Treesearch</a></p> <p>Michael T. Thompson</p> <p>2009-01-01</p> <p>Aerial detection surveys indicate that widespread conifer mortality has been steadily increasing in Colorado, particularly since 2002. The Forest Inventory and Analysis (FIA) <span class="hlt">annual</span> inventory system began in Colorado in 2002, which coincided with the onset of elevated conifer mortality rates. The current mortality <span class="hlt">event</span> coupled with collection of 6 years of <span class="hlt">annual</span>...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/12738870','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/12738870"><span>Episodic tremor and slip on the Cascadia subduction <span class="hlt">zone</span>: the chatter of silent slip.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Rogers, Garry; Dragert, Herb</p> <p>2003-06-20</p> <p>We found that repeated slow slip <span class="hlt">events</span> observed on the deeper interface of the northern Cascadia subduction <span class="hlt">zone</span>, which were at first thought to be silent, have unique nonearthquake seismic signatures. Tremorlike seismic signals were found to correlate temporally and spatially with slip <span class="hlt">events</span> identified from crustal motion data spanning the past 6 years. During the period between slips, tremor activity is minor or nonexistent. We call this associated tremor and slip phenomenon episodic tremor and slip (ETS) and propose that ETS activity can be used as a real-time indicator of stress loading of the Cascadia megathrust earthquake <span class="hlt">zone</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5359104','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=5359104"><span>Failure of fertility therapy and subsequent adverse cardiovascular <span class="hlt">events</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Udell, Jacob A.; Lu, Hong; Redelmeier, Donald A.</p> <p>2017-01-01</p> <p>BACKGROUND: Infertility may indicate an underlying predisposition toward premature cardiovascular disease, yet little is known about potential long-term cardiovascular <span class="hlt">events</span> following fertility therapy. We investigated whether failure of fertility therapy is associated with subsequent adverse cardiovascular <span class="hlt">events</span>. METHODS: We performed a population-based cohort analysis of women who received gonadotropin-based fertility therapy between Apr. 1, 1993, and Mar. 31, 2011, distinguishing those who subsequently gave birth and those who did not. Using multivariable Poisson regression models, we estimated the relative rate ratio of adverse cardiovascular <span class="hlt">events</span> associated with fertility therapy failure, accounting for age, year, baseline risk factors, health care history and number of fertility cycles. The primary outcome was subsequent treatment for nonfatal coronary ischemia, stroke, transient ischemic attack, heart failure or thromboembolism. RESULTS: Of 28 442 women who received fertility therapy, 9349 (32.9%) subsequently gave birth and 19 093 (67.1%) did not. The median number of fertility treatments was 3 (interquartile range 1–5). We identified 2686 cardiovascular <span class="hlt">events</span> over a median 8.4 years of follow-up. The <span class="hlt">annual</span> rate of cardiovascular <span class="hlt">events</span> was 19% higher among women who did not give birth after fertility therapy than among those who did (1.08 v. 0.91 per 100 patient-years, p < 0.001), equivalent to a 21% relative increase in the <span class="hlt">annual</span> rate (95% confidence interval 13%–30%). We observed no association between <span class="hlt">event</span> rates and number of treatment cycles. INTERPRETATION: Fertility therapy failure was associated with an increased risk of long-term adverse cardiovascular <span class="hlt">events</span>. These women merit surveillance for subsequent cardiovascular <span class="hlt">events</span>. PMID:28385819</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-06-26/pdf/2013-15310.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-06-26/pdf/2013-15310.pdf"><span>78 FR 38200 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> Independence Day Fireworks Displays, Skagway, Haines, and Wrangell, AK</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-06-26</p> <p>..., darkness punctuated by bright flashes of light, and burning debris has the potential to result in serious... enforcement of these safety <span class="hlt">zones</span> will be of short duration, approximately three hours. Furthermore, vessels...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_18");'>18</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li class="active"><span>20</span></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_20 --> <div id="page_21" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li class="active"><span>21</span></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="401"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-06-02/pdf/2010-13118.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-06-02/pdf/2010-13118.pdf"><span>75 FR 30708 - Safety <span class="hlt">Zone</span>; Red Bull Air Race, Detroit River, Detroit, MI</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-06-02</p> <p>... each day of its effective period. Additionally, prior to the <span class="hlt">event</span>, local sailing and yacht clubs will... local sailing and yacht clubs. In the <span class="hlt">event</span> this temporary safety <span class="hlt">zone</span> affects shipping, commercial... and yacht clubs will be provided with information by Coast Guard Station Belle Isle on what to expect...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2009EGUGA..11.9142D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2009EGUGA..11.9142D"><span>Continuous monitoring of water flow and solute transport using vadose <span class="hlt">zone</span> monitoring technology</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dahan, O.</p> <p>2009-04-01</p> <p>Groundwater contamination is usually attributed to pollution <span class="hlt">events</span> that initiate on land surface. These may be related to various sources such as industrial, urban or agricultural, and may appear as point or non point sources, through a single accidental <span class="hlt">event</span> or a continuous pollution process. In all cases, groundwater pollution is a consequence of pollutant transport processes that take place in the vadose <span class="hlt">zone</span> above the water table. Attempts to control pollution <span class="hlt">events</span> and prevent groundwater contamination usually involve groundwater monitoring programs. This, however, can not provide any protection against contamination since pollution identification in groundwater is clear evidence that the groundwater is already polluted and contaminants have already traversed the entire vadose <span class="hlt">zone</span>. Accordingly, an efficient monitoring program that aims at providing information that may prevent groundwater pollution has to include vadose-<span class="hlt">zone</span> monitoring systems. Such system should provide real-time information on the hydrological and chemical properties of the percolating water and serve as an early warning system capable of detecting pollution <span class="hlt">events</span> in their early stages before arrival of contaminants to groundwater. Recently, a vadose-<span class="hlt">zone</span> monitoring system (VMS) was developed to allow continuous monitoring of the hydrological and chemical properties of percolating water in the deep vadose <span class="hlt">zone</span>. The VMS includes flexible time-domain reflectometry (FTDR) probes for continuous tracking of water content profiles, and vadose-<span class="hlt">zone</span> sampling ports (VSPs) for frequent sampling of the deep vadose pore water at multiple depths. The monitoring probes and sampling ports are installed through uncased slanted boreholes using a flexible sleeve that allows attachment of the monitoring devices to the borehole walls while achieving good contact between the sensors and the undisturbed sediment column. The system has been successfully implemented in several studies on water flow and</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=renewable+AND+energy+AND+project&pg=7&id=ED155037','ERIC'); return false;" href="https://eric.ed.gov/?q=renewable+AND+energy+AND+project&pg=7&id=ED155037"><span>Environmental Quality - 1977: The Eighth <span class="hlt">Annual</span> Report of the Council on Environmental Quality.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Council on Environmental Quality, Washington, DC.</p> <p></p> <p>This eighth <span class="hlt">annual</span> report considers the state of the environment and new or continuing efforts to improve it. The publication is divided into two chapters. The first chapter summarizes important environmental <span class="hlt">events</span> of the past year. <span class="hlt">Events</span> include new legislation, court rulings, major accidents, policy changes, and similar material. The second…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/6281282-intra-annual-variability-radiocarbon-content-corals-from-galapagos-islands','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/6281282-intra-annual-variability-radiocarbon-content-corals-from-galapagos-islands"><span>Intra-<span class="hlt">annual</span> variability of the radiocarbon content of corals from the Galapagos Islands</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Brown, T.A.; Farwell, G.W.; Schmidt, F.H.</p> <p>1993-01-01</p> <p>The authors report AMS [sup 14]C measurements on sub <span class="hlt">annual</span> samples of coral from the Galapagos Islands that span the period, 1970-1973. Both the major 1972 El Nino/Southern Oscillation <span class="hlt">event</span> and intra-<span class="hlt">annual</span> changes in regional upwelling of [sup 14]C-depleted waters associated with alternation of surface-ocean current patterns are evident in the record. These data show that the corals preserve a detailed record of past intra-<span class="hlt">annual</span> variations of the [sup 14]C content of surface ocean water.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015AGUFM.S23B2709L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015AGUFM.S23B2709L"><span>Imaging Fracking <span class="hlt">Zones</span> by Microseismic Reverse Time Migration for Downhole Microseismic Monitoring</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lin, Y.; Zhang, H.</p> <p>2015-12-01</p> <p>Hydraulic fracturing is an engineering tool to create fractures in order to better recover oil and gas from low permeability reservoirs. Because microseismic <span class="hlt">events</span> are generally associated with fracturing development, microseismic monitoring has been used to evaluate the fracking process. Microseismic monitoring generally relies on locating microseismic <span class="hlt">events</span> to understand the spatial distribution of fractures. For the multi-stage fracturing treatment, fractures created in former stages are strong scatterers in the medium and can induce strong scattering waves on the waveforms for microseismic <span class="hlt">events</span> induced during later stages. In this study, we propose to take advantage of microseismic scattering waves to image fracking <span class="hlt">zones</span> by using seismic reverse time migration method. For downhole microseismic monitoring that involves installing a string of seismic sensors in a borehole near the injection well, the observation geometry is actually similar to the VSP (vertical seismic profile) system. For this reason, we adapt the VSP migration method for the common shot gather to the common <span class="hlt">event</span> gather. Microseismic reverse-time migration method involves solving wave equation both forward and backward in time for each microseismic <span class="hlt">event</span>. At current stage, the microseismic RTM is based on 2D acoustic wave equation (Zhang and Sun, 2008), solved by the finite-difference method with PML absorbing boundary condition applied to suppress the reflections of artificial boundaries. Additionally, we use local wavefield decomposition instead of cross-correlation imaging condition to suppress the imaging noise. For testing the method, we create a synthetic dataset for a downhole microseismic monitoring system with multiple fracking stages. It shows that microseismic migration using individual <span class="hlt">event</span> is able to clearly reveal the fracture <span class="hlt">zone</span>. The shorter distance between fractures and the microseismic <span class="hlt">event</span> the clearer the migration image is. By summing migration images for many</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017EGUGA..19.6593D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017EGUGA..19.6593D"><span>Focal mechanism and stress analyses for main tectonic <span class="hlt">zones</span> in Albania</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dushi, Edmond; Koçi, Rexhep; Begu, Enkela; Bozo, Rrezart</p> <p>2017-04-01</p> <p>In this study, a number of 33 moderate earthquakes for the period 2013-2015, ranging in magnitude within 2.2 ≤ MW ≤ 4.9 and located within the Albanian territory, have been analyzed. As an earthquake prone country, situated at the frontal collision boundary between Adria microplate and Eurasian tectonic plate, Albania is characterized frequently by micro earthquakes, many moderate and seldom by strong ones. It is evidenced that the whole territory is divided in two different tectonic domains, correspondingly the outer and the inner domain, showing different stress regime as clearly evidenced based on earthquake focal mechanism and geodetic studies. Although strong earthquakes are clearly related to faults in tectonically active areas, moderate <span class="hlt">events</span> are more frequent revealing valuable information on this purpose. All the studied <span class="hlt">events</span> are selected to be well-recorded by a maximum possible number of the local broadband (BB) seismological stations of Albanian Seismological Network (ASN), although regional stations have been used as well to constrain the solution. Earthquakes are grouped according to their location, within three well-defined tectonic <span class="hlt">zones</span>, namely: Adriatic-Ionian (AI), Lushnja-Elbasani-Dibra (LED) and Ohrid-Korça (OK). For each <span class="hlt">event</span>, the seismic moment M0is determined, through spectral analyses. Moment values vary ranging 1012 - 1015 Nm, for the Adriatic-Ionian (AI) outer <span class="hlt">zone</span>; 1013 - 1016 Nm, for the Lushnja-Elbasani-Dibra (LED) transversal <span class="hlt">zone</span>, which cuts through both the outer and the inner domains and 1012 - 1014 Nm, for the Ohrid-Korça (OK), north-south trending inner <span class="hlt">zone</span>. Focal mechanism solutions (FMS) have been determined for each earthquake, based on the robust first motion polarities method, as applied in the FOCMEC (Seisan 10.1) routine. Using the Michael's linear bootstrap invertion on FMS, a stress analysis is applied. Results show the minimum compressional stress directions variation: σ1 370/270, σ23030/80 and σ31980</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-08-20/pdf/2012-20355.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-08-20/pdf/2012-20355.pdf"><span>77 FR 50065 - Safety <span class="hlt">Zone</span>; Jacksonville Sea and Sky Spectacular, Atlantic Ocean; Jacksonville Beach, FL</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-08-20</p> <p>... 1625-AA00 Safety <span class="hlt">Zone</span>; Jacksonville Sea and Sky Spectacular, Atlantic Ocean; Jacksonville Beach, FL... during the Jacksonville Sea and Sky Spectacular air show. The <span class="hlt">event</span> is scheduled to take place from....T07-0660 Safety <span class="hlt">Zone</span>; Jacksonville Sea and Sky Spectacular, Atlantic Ocean, Jacksonville Beach, FL. (a...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-05-24/pdf/2010-12343.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-05-24/pdf/2010-12343.pdf"><span>75 FR 28769 - Safety <span class="hlt">Zone</span>; Osage River, Mile 016.8 to 017.2</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-05-24</p> <p>...-AA00 Safety <span class="hlt">Zone</span>; Osage River, Mile 016.8 to 017.2 AGENCY: Coast Guard, DHS. ACTION: Notice of proposed... Osage River, Mile 016.8 to 017.2, extending the entire width of the river. This safety <span class="hlt">zone</span> is needed to... between mile 016.8 and 017.2 on the Osage River. This <span class="hlt">event</span> presents safety hazards to the navigation of...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015EGUGA..17.6498Y','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015EGUGA..17.6498Y"><span>Complex fragmentation and silicification structures in fault <span class="hlt">zones</span>: quartz crystallization and repeated fragmentation in the Rusey fault <span class="hlt">zone</span> (Cornwall/UK)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Yilmaz, Tim I.; Blenkinsop, Tom; Duschl, Florian; Kruhl, Jörn H.</p> <p>2015-04-01</p> <p>Silicified fault rocks typically show structures resulting from various stages of fragmentation and quartz crystallization. Both processes interact episodically and result in complex structures on various scales, which require a wide spectrum of analysis tools. Based on field and microstructural data, the spatial-temporal connection between deformation, quartz crystallization and fluid and material flow along the Rusey fault <span class="hlt">zone</span> was investigated. The fault can be examined in detail in three dimensions on the north Cornwall coast, UK. It occurs within Carboniferous sandstones, siltstones, mudstones and slates of the Culm basin, and is likely to have had a long history. The fault rocks described here formed during the younger <span class="hlt">events</span>, possibly due to Tertiary strike-slip reactivation. Frequent fragmentation, flow and crystallization <span class="hlt">events</span> and their interaction led to various generations of complex-structured quartz units, among them quartz-mantled and partly silicified wall-rock fragments, microcrystalline quartz masses of different compositions and structures, and quartz vein patterns of various ages. Lobate boundaries of quartz masses indicate viscous flow. Fragments are separated by quartz infill, which contains cm-sized open pores, in which quartz crystals have pyramidal terminations. Based on frequent occurrence of feathery textures and the infill geometry, quartz crystallization from chalcedony appears likely, and an origin from silica gel is discussed. Fragmentation structures are generally fractal. This allows differentiation between various processes, such as corrosive wear, wear abrasion and hydraulic brecciation. Material transport along the brittle shear <span class="hlt">zone</span>, and displacement of the wall-rocks, were at least partly governed by flow of mobile fluid-quartz-particle suspensions. The complex meso- to microstructures were generated by repeated processes of fragmentation, quartz precipitation and grain growth. In general, the brittle Rusey fault <span class="hlt">zone</span></p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/circ/1997/1142/report.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/circ/1997/1142/report.pdf"><span>1996 <span class="hlt">annual</span> report on Alaska's mineral resources</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Schneider, Jill L.</p> <p>1997-01-01</p> <p>This is the fifteenth <span class="hlt">annual</span> report that has been prepared in response to the Alaska National Interest Lands Conservation Act. Current Alaskan mineral projects and <span class="hlt">events</span> that occurred during 1995 are summarized. For the purpose of this document, the term 'minerals' encompasses both energy resources (oil and gas, coal and peat, uranium, and geothermal) and nonfuel-mineral resources (metallic and industrial minerals).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015JAfES.101..322M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015JAfES.101..322M"><span>Late Devonian conodonts and <span class="hlt">event</span> stratigraphy in northwestern Algerian Sahara</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Mahboubi, Abdessamed; Gatovsky, Yury</p> <p>2015-01-01</p> <p>Conodonts recovered from the Late Devonian South Marhouma section comprise 5 genera with 31 species (3 undetermined). The fauna establishes the presence of MN <span class="hlt">Zones</span> 5, undifferentiated 6/7, 8/10 for the Middle Frasnian, the MN <span class="hlt">Zones</span> 11, 12, 13 for the Upper Frasnian as well as the Early through Late triangularis <span class="hlt">Zones</span> in the basal Famennian. The outcropping lithological succession is one of mostly nodular calcilutites alternating with numerous marly and shaly deposits, which, in the lower and upper part, comprise several dysoxic dark shale intervals. Among these the Upper Kellwasser horizon can be precisely dated and as such the presence of the terminal Frasnian Kellwasser <span class="hlt">Event</span> is recognized for the first time in Algeria. Both the Middlesex and Rhinestreet <span class="hlt">Events</span> cannot yet be precisely located, but supposedly occur among the dark shale horizons in the lower part of the section. However, their assignment to a precise level has so far not been established. Though poor in conodont abundance the South Marhouma section provides first evidence of the presence of several Montagne Noire conodont <span class="hlt">zones</span> within the so far widely unstudied Frasnian of the Ougarta Chain. As such it is considered representative for the northwestern Algerian Saoura region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=138286&keyword=bribe+OR+gift&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50','EPA-EIMS'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=138286&keyword=bribe+OR+gift&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50"><span>EPA SCIENTISTS PARTICIPATE IN THE SRA 2005 <span class="hlt">ANNUAL</span> MEETING</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>Several NCEA Scientists presented at this years Society For Risk Analysis (SRA) <span class="hlt">Annual</span> Meeting (see <a href='#OSO'>other sources for the SRA meeting agenda</a>). The meeting was held December 4-7, 2005 in Orlando, Fl. The table below contains the <span class="hlt">event</span> names (with external links...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=63975&keyword=accounting+AND+system&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50','EPA-EIMS'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=63975&keyword=accounting+AND+system&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50"><span>AN EXACT SOLUTION FOR THE ASSESSMENT OF NONEQUILIBRIUM SORPTION OF RADIONUCLIDES IN THE VADOSE <span class="hlt">ZONE</span></span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>In a report on model evaluation, the authors ran the HYDRUS Code, among other transport codes, to evaluate the impacts of nonequilibrium sorption sites on the time-evolution of 99Tc and 90Sr through the vadose <span class="hlt">zone</span>. Since our evaluation was based on a rather low, <span class="hlt">annual</span> recharge...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3501619','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3501619"><span>Extreme climatic <span class="hlt">events</span> drive mammal irruptions: regression analysis of 100-year trends in desert rainfall and temperature</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Greenville, Aaron C; Wardle, Glenda M; Dickman, Chris R</p> <p>2012-01-01</p> <p>Extreme climatic <span class="hlt">events</span>, such as flooding rains, extended decadal droughts and heat waves have been identified increasingly as important regulators of natural populations. Climate models predict that global warming will drive changes in rainfall and increase the frequency and severity of extreme <span class="hlt">events</span>. Consequently, to anticipate how organisms will respond we need to document how changes in extremes of temperature and rainfall compare to trends in the mean values of these variables and over what spatial scales the patterns are consistent. Using the longest historical weather records available for central Australia – 100 years – and quantile regression methods, we investigate if extreme climate <span class="hlt">events</span> have changed at similar rates to median <span class="hlt">events</span>, if <span class="hlt">annual</span> rainfall has increased in variability, and if the frequency of large rainfall <span class="hlt">events</span> has increased over this period. Specifically, we compared local (individual weather stations) and regional (Simpson Desert) spatial scales, and quantified trends in median (50th quantile) and extreme weather values (5th, 10th, 90th, and 95th quantiles). We found that median and extreme <span class="hlt">annual</span> minimum and maximum temperatures have increased at both spatial scales over the past century. Rainfall changes have been inconsistent across the Simpson Desert; individual weather stations showed increases in <span class="hlt">annual</span> rainfall, increased frequency of large rainfall <span class="hlt">events</span> or more prolonged droughts, depending on the location. In contrast to our prediction, we found no evidence that intra-<span class="hlt">annual</span> rainfall had become more variable over time. Using long-term live-trapping records (22 years) of desert small mammals as a case study, we demonstrate that irruptive <span class="hlt">events</span> are driven by extreme rainfalls (>95th quantile) and that increases in the magnitude and frequency of extreme rainfall <span class="hlt">events</span> are likely to drive changes in the populations of these species through direct and indirect changes in predation pressure and wildfires. PMID:23170202</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=event+AND+management+AND+articles&id=EJ886365','ERIC'); return false;" href="https://eric.ed.gov/?q=event+AND+management+AND+articles&id=EJ886365"><span>Conducting a Successful National Girls and Women in Sports Day <span class="hlt">Event</span></span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Appleby, Karen M.; Pemberton, Cynthia Lee A.</p> <p>2010-01-01</p> <p>National Girls and Women in Sports Day (NGWSD) is a nationally celebrated <span class="hlt">event</span> that promotes sport and physical activity opportunities for girls and women. Over 1,500 <span class="hlt">events</span> and activities are held <span class="hlt">annually</span> in all 50 states to celebrate and promote female participation in sport. This article introduces the sport/activity-clinic model of the NGWSD…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/pages/biblio/1378974-attributing-historical-changes-probabilities-record-breaking-daily-temperature-precipitation-extreme-events','SCIGOV-DOEP'); return false;" href="https://www.osti.gov/pages/biblio/1378974-attributing-historical-changes-probabilities-record-breaking-daily-temperature-precipitation-extreme-events"><span>Attributing Historical Changes in Probabilities of Record-Breaking Daily Temperature and Precipitation Extreme <span class="hlt">Events</span></span></a></p> <p><a target="_blank" href="http://www.osti.gov/pages">DOE PAGES</a></p> <p>Shiogama, Hideo; Imada, Yukiko; Mori, Masato; ...</p> <p>2016-08-07</p> <p>Here, we describe two unprecedented large (100-member), longterm (61-year) ensembles based on MRI-AGCM3.2, which were driven by historical and non-warming climate forcing. These ensembles comprise the "Database for Policy Decision making for Future climate change (d4PDF)". We compare these ensembles to large ensembles based on another climate model, as well as to observed data, to investigate the influence of anthropogenic activities on historical changes in the numbers of record-breaking <span class="hlt">events</span>, including: the <span class="hlt">annual</span> coldest daily minimum temperature (TNn), the <span class="hlt">annual</span> warmest daily maximum temperature (TXx) and the <span class="hlt">annual</span> most intense daily precipitation <span class="hlt">event</span> (Rx1day). These two climate model ensembles indicatemore » that human activity has already had statistically significant impacts on the number of record-breaking extreme <span class="hlt">events</span> worldwide mainly in the Northern Hemisphere land. Specifically, human activities have altered the likelihood that a wider area globally would suffer record-breaking TNn, TXx and Rx1day <span class="hlt">events</span> than that observed over the 2001- 2010 period by a factor of at least 0.6, 5.4 and 1.3, respectively. However, we also find that the estimated spatial patterns and amplitudes of anthropogenic impacts on the probabilities of record-breaking <span class="hlt">events</span> are sensitive to the climate model and/or natural-world boundary conditions used in the attribution studies.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2003EAEJA....12159P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2003EAEJA....12159P"><span>A cathodoluminescence study on zircons with a complex thermal history traces back Permian crustal <span class="hlt">events</span> in the Ivrea <span class="hlt">Zone</span> (South Alpine, Northern Italy)</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Peressini, G.; Poller, U.</p> <p>2003-04-01</p> <p>In the context of a U-Pb SHRIMP data-set, a cathodoluminescence (CL) study has been performed on zircons from the Ivrea-Verbano <span class="hlt">Zone</span>; this is a tectonically bounded section of intermediate to deep crust, tilted and obducted in Alpine time, in which a large deep-crustal intrusion of mantle origin, the Mafic Complex (MC), was emplaced in the Early Permian. Zircons from 16 samples from the different units of the MC have been studied using CL. Three samples collected from the Paragneiss Bearing Belt (PBB) yield some partially reset spot-ages, reflecting the field observation that country rock slabs are frequent in that area. On the other side, unlike in zircons from granites, the cores are invisible under CL-imaging, and this makes the U-Pb spot-age results unpredictable, with a continuous range of ages in the same sample, spanning for an interval of over 35 Ma, followed by some much older peaks, up to 600 Ma. A fourth sample, collected 2 km far, but still within the PBB, defines instead a unique, well-defined age at 287±3 Ma, with no older peaks, its zircons showing a CL pattern typical for metamorphic grains. A different case is displayed by a sample collected from the deeper Amphibole Gabbro unit: each single grain records a complex story of magmatic growth with variable diffusivity conditions. All of them show a second major overprint, that lead to both (re)crystallization and resorption, always corresponding to much lower U and Th contents, with no sensible modification of the Th-U ratio. The age of the second <span class="hlt">event</span>, though, is not distinguishable from that of first crystallization of the grains, and has not been at such a temperature as to obliterate the fine <span class="hlt">zoning</span> pattern of the primary grain. The CL patterns of each single grain, composed of different domains, allow considerations on the environmental conditions of growth and (re)crystallization. CL is a very powerful tool itself, revealing crystal-chemical processes. The integration of the CL-study with the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec165-166.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec165-166.pdf"><span>33 CFR 165.166 - Safety <span class="hlt">Zone</span>: Macy's July 4th Fireworks, East River, NY.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2011-07-01 2011-07-01 false Safety <span class="hlt">Zone</span>: Macy's July 4th... § 165.166 Safety <span class="hlt">Zone</span>: Macy's July 4th Fireworks, East River, NY. (a) Regulated area. The following area.... on July 4th. If the <span class="hlt">event</span> is cancelled due to inclement weather then this section is in effect from 6...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol2/pdf/CFR-2013-title33-vol2-sec165-166.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol2/pdf/CFR-2013-title33-vol2-sec165-166.pdf"><span>33 CFR 165.166 - Safety <span class="hlt">Zone</span>: Macy's July 4th Fireworks, East River, NY.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2013-07-01 2013-07-01 false Safety <span class="hlt">Zone</span>: Macy's July 4th... § 165.166 Safety <span class="hlt">Zone</span>: Macy's July 4th Fireworks, East River, NY. (a) Regulated area. The following area.... on July 4th. If the <span class="hlt">event</span> is cancelled due to inclement weather then this section is in effect from 6...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec165-166.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec165-166.pdf"><span>33 CFR 165.166 - Safety <span class="hlt">Zone</span>: Macy's July 4th Fireworks, East River, NY.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2012-07-01 2012-07-01 false Safety <span class="hlt">Zone</span>: Macy's July 4th... § 165.166 Safety <span class="hlt">Zone</span>: Macy's July 4th Fireworks, East River, NY. (a) Regulated area. The following area.... on July 4th. If the <span class="hlt">event</span> is cancelled due to inclement weather then this section is in effect from 6...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_19");'>19</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li class="active"><span>21</span></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_21 --> <div id="page_22" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li class="active"><span>22</span></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="421"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec165-166.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec165-166.pdf"><span>33 CFR 165.166 - Safety <span class="hlt">Zone</span>: Macy's July 4th Fireworks, East River, NY.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-07-01</p> <p>... 33 Navigation and Navigable Waters 2 2014-07-01 2014-07-01 false Safety <span class="hlt">Zone</span>: Macy's July 4th... § 165.166 Safety <span class="hlt">Zone</span>: Macy's July 4th Fireworks, East River, NY. (a) Regulated area. The following area.... on July 4th. If the <span class="hlt">event</span> is cancelled due to inclement weather then this section is in effect from 6...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017PApGe.174.3451C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017PApGe.174.3451C"><span>Within-<span class="hlt">Event</span> and Between-<span class="hlt">Events</span> Ground Motion Variability from Earthquake Rupture Scenarios</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Crempien, Jorge G. F.; Archuleta, Ralph J.</p> <p>2017-09-01</p> <p>Measurement of ground motion variability is essential to estimate seismic hazard. Over-estimation of variability can lead to extremely high <span class="hlt">annual</span> hazard estimates of ground motion exceedance. We explore different parameters that affect the variability of ground motion such as the spatial correlations of kinematic rupture parameters on a finite fault and the corner frequency of the moment-rate spectra. To quantify the variability of ground motion, we simulate kinematic rupture scenarios on several vertical strike-slip faults and compute ground motion using the representation theorem. In particular, for the entire suite of rupture scenarios, we quantify the within-<span class="hlt">event</span> and the between-<span class="hlt">events</span> ground motion variability of peak ground acceleration (PGA) and response spectra at several periods, at 40 stations—all approximately at an equal distance of 20 and 50 km from the fault. Both within-<span class="hlt">event</span> and between-<span class="hlt">events</span> ground motion variability increase when the slip correlation length on the fault increases. The probability density functions of ground motion tend to truncate at a finite value when the correlation length of slip decreases on the fault, therefore, we do not observe any long-tail distribution of peak ground acceleration when performing several rupture simulations for small correlation lengths. Finally, for a correlation length of 6 km, the within-<span class="hlt">event</span> and between-<span class="hlt">events</span> PGA log-normal standard deviations are 0.58 and 0.19, respectively, values slightly smaller than those reported by Boore et al. (Earthq Spectra, 30(3):1057-1085, 2014). The between-<span class="hlt">events</span> standard deviation is consistently smaller than the within-<span class="hlt">event</span> for all correlations lengths, a feature that agrees with recent ground motion prediction equations.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-02-10/pdf/2012-3144.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-02-10/pdf/2012-3144.pdf"><span>77 FR 7134 - Proposed Information Collection; Comment Request; <span class="hlt">Annual</span> Economic Survey of Federal Gulf and...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-02-10</p> <p>... Collection; Comment Request; <span class="hlt">Annual</span> Economic Survey of Federal Gulf and South Atlantic Shrimp Permit Holders... from commercial fishermen in the Gulf of Mexico and South Atlantic shrimp fisheries who hold one or more permits for shrimp fishing in federal waters (United States (U.S.) Exclusive Economic <span class="hlt">Zone</span> (EEZ...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18.6542R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18.6542R"><span>Seasonal and inter-<span class="hlt">annual</span> variation in ecosystem scale methane emission from a boreal fen</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Rinne, Janne; Li, Xuefei; Raivonen, Maarit; Peltola, Olli; Sallantaus, Tapani; Haapanala, Sami; Smolander, Sampo; Alekseychik, Pavel; Aurela, Mika; Korrensalo, Aino; Mammarella, Ivan; Tuittila, Eeva-Stiina; Vesala, Timo</p> <p>2016-04-01</p> <p>Northern wetlands are one of the major sources of atmospheric methane. We have measured ecosystem scale methane emissions from a boreal fen continuously since 2005. The site is an oligotrophic fen in boreal vegetation <span class="hlt">zone</span> situated in Siikaneva wetland complex in Southern Finland. The mean <span class="hlt">annual</span> temperature in the area is 3.3°C and total <span class="hlt">annual</span> precipitation 710 mm. We have conducted the methane emission measurements by the eddy covariance method. Additionally we have measured fluxes of carbon dioxide, water vapor, and sensible heat together with a suite of other environmental parameters. We have analyzed this data alongside with a model run with University of Helsinki methane model. The measured fluxes show generally highest methane emission in late summers coinciding with the highest temperatures in saturated peat <span class="hlt">zone</span>. During winters the fluxes show small but detectable emission despite the snow and ice cover on the fen. More than 90% of the <span class="hlt">annual</span> methane emission occurs in snow-free period. The methane emission and peat temperature are connected in exponential manner in seasonal scales, but methane emission does not show the expected behavior with water table. The lack of water table position dependence also contrasts with the spatial variation across microtopography. There is no systematic variation in sub-diurnal time scale. The general seasonal cycle in methane emission is captured well with the methane model. We will show how well the model reproduces the temperature and water table position dependencies observed. The <span class="hlt">annual</span> methane emission is typically around 10 gC m-2. This is a significant part of the total carbon exchange between the fen and the atmosphere and about twice the estimated carbon loss by leaching from the fen area. The inter-<span class="hlt">annual</span> variability in the methane emission is modest. The June-September methane emissions from different years, comprising most of the <span class="hlt">annual</span> emission, correlates positively with peat temperature, but not with</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-06-06/pdf/2013-13422.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-06-06/pdf/2013-13422.pdf"><span>78 FR 33972 - Safety <span class="hlt">Zone</span>; RXR Sea Faire Celebration Fireworks, Glen Cove, NY</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-06-06</p> <p>...-AA00 Safety <span class="hlt">Zone</span>; RXR Sea Faire Celebration Fireworks, Glen Cove, NY AGENCY: Coast Guard, DHS. ACTION... proposed rulemaking. The <span class="hlt">event</span> sponsor advised that the <span class="hlt">event</span> is in correlation with a local Sea faire... fireworks are taking place as part of the RXR Sea Faire Celebration Fireworks in Glen Cove, NY. Based on the...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007AGUSM.S52A..02P','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007AGUSM.S52A..02P"><span>Seismic sequences in the Sombrero Seismic <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Pulliam, J.; Huerfano, V. A.; ten Brink, U.; von Hillebrandt, C.</p> <p>2007-05-01</p> <p>The northeastern Caribbean, in the vicinity of Puerto Rico and the Virgin Islands, has a long and well-documented history of devastating earthquakes and tsunamis, including major <span class="hlt">events</span> in 1670, 1787, 1867, 1916, 1918, and 1943. Recently, seismicity has been concentrated to the north and west of the British Virgin Islands, in the region referred to as the Sombrero Seismic <span class="hlt">Zone</span> by the Puerto Rico Seismic Network (PRSN). In the combined seismicity catalog maintained by the PRSN, several hundred small to moderate magnitude <span class="hlt">events</span> can be found in this region prior to 2006. However, beginning in 2006 and continuing to the present, the rate of seismicity in the Sombrero suddenly increased, and a new locus of activity developed to the east of the previous location. Accurate estimates of seismic hazard, and the tsunamigenic potential of seismic <span class="hlt">events</span>, depend on an accurate and comprehensive understanding of how strain is being accommodated in this corner region. Are faults locked and accumulating strain for release in a major <span class="hlt">event</span>? Or is strain being released via slip over a diffuse system of faults? A careful analysis of seismicity patterns in the Sombrero region has the potential to both identify faults and modes of failure, provided the aggregation scheme is tuned to properly identify related <span class="hlt">events</span>. To this end, we experimented with a scheme to identify seismic sequences based on physical and temporal proximity, under the assumptions that (a) <span class="hlt">events</span> occur on related fault systems as stress is refocused by immediately previous <span class="hlt">events</span> and (b) such 'stress waves' die out with time, so that two <span class="hlt">events</span> that occur on the same system within a relatively short time window can be said to have a similar 'trigger' in ways that two nearby <span class="hlt">events</span> that occurred years apart cannot. Patterns that emerge from the identification, temporal sequence, and refined locations of such sequences of <span class="hlt">events</span> carry information about stress accommodation that is obscured by large clouds of</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..18.5068B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..18.5068B"><span>The Himalayan Seismogenic <span class="hlt">Zone</span>: A New Frontier for Earthquake Research</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Brown, Larry; Hubbard, Judith; Karplus, Marianne; Klemperer, Simon; Sato, Hiroshi</p> <p>2016-04-01</p> <p>The Mw 7.8 Gorkha, Nepal, earthquake that occurred on April 25 of this year was a dramatic reminder that great earthquakes are not restricted to the large seismogenic <span class="hlt">zones</span> associated with subduction of oceanic lithosphere. Not only does Himalayan seismogenesis represents important scientific and societal issues in its own right, it constitutes a reference for evaluating general models of the earthquake cycle derived from the studies of the oceanic subduction systems. This presentation reports results of a Mini-Workshop sponsored by the GeoPrisms project that was held in conjunction with the American Geophysical Union on December 15, 2015, designed to organize a new initiative to study the great Himalaya earthquake machine. The Himalayan seismogenic <span class="hlt">zone</span> shares with its oceanic counterparts a number of fundamental questions, including: a) What controls the updip and downdip limits of rupture? b) What controls the lateral segmentation of rupture <span class="hlt">zones</span> (and hence magnitude)? c) What is the role of fluids in facilitating slip and or rupture? d) What nucleates rupture (e..g. asperities?)? e) What physical properties can be monitored as precursors to future <span class="hlt">events</span>? f) How effectively can the radiation pattern of future <span class="hlt">events</span> be modeled? g) How can a better understanding of Himalayan rupture be translated into more cost effective preparations for the next major <span class="hlt">event</span> in this region? However the underthrusting of continental, as opposed to oceanic, lithosphere in the Himalayas frames these questions in a very different context: h) How does the greater thickness and weaker rheology of continental crust/lithosphere affect locking of the seismogenic <span class="hlt">zone</span>? i) How does the different thermal structure of continental vs oceanic crust affect earthquake geodynamics? j) Are fluids a significant factor in intercontinental thrusting? k) How does the basement morphology of underthrust continental crust affect locking/creep, and how does it differ from the oceanic case? l) What is the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018BGeo...15.1293V','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018BGeo...15.1293V"><span>Impacts of droughts and extreme-temperature <span class="hlt">events</span> on gross primary production and ecosystem respiration: a systematic assessment across ecosystems and climate <span class="hlt">zones</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>von Buttlar, Jannis; Zscheischler, Jakob; Rammig, Anja; Sippel, Sebastian; Reichstein, Markus; Knohl, Alexander; Jung, Martin; Menzer, Olaf; Altaf Arain, M.; Buchmann, Nina; Cescatti, Alessandro; Gianelle, Damiano; Kiely, Gerard; Law, Beverly E.; Magliulo, Vincenzo; Margolis, Hank; McCaughey, Harry; Merbold, Lutz; Migliavacca, Mirco; Montagnani, Leonardo; Oechel, Walter; Pavelka, Marian; Peichl, Matthias; Rambal, Serge; Raschi, Antonio; Scott, Russell L.; Vaccari, Francesco P.; van Gorsel, Eva; Varlagin, Andrej; Wohlfahrt, Georg; Mahecha, Miguel D.</p> <p>2018-03-01</p> <p>Extreme climatic <span class="hlt">events</span>, such as droughts and heat stress, induce anomalies in ecosystem-atmosphere CO2 fluxes, such as gross primary production (GPP) and ecosystem respiration (Reco), and, hence, can change the net ecosystem carbon balance. However, despite our increasing understanding of the underlying mechanisms, the magnitudes of the impacts of different types of extremes on GPP and Reco within and between ecosystems remain poorly predicted. Here we aim to identify the major factors controlling the amplitude of extreme-<span class="hlt">event</span> impacts on GPP, Reco, and the resulting net ecosystem production (NEP). We focus on the impacts of heat and drought and their combination. We identified hydrometeorological extreme <span class="hlt">events</span> in consistently downscaled water availability and temperature measurements over a 30-year time period. We then used FLUXNET eddy covariance flux measurements to estimate the CO2 flux anomalies during these extreme <span class="hlt">events</span> across dominant vegetation types and climate <span class="hlt">zones</span>. Overall, our results indicate that short-term heat extremes increased respiration more strongly than they downregulated GPP, resulting in a moderate reduction in the ecosystem's carbon sink potential. In the absence of heat stress, droughts tended to have smaller and similarly dampening effects on both GPP and Reco and, hence, often resulted in neutral NEP responses. The combination of drought and heat typically led to a strong decrease in GPP, whereas heat and drought impacts on respiration partially offset each other. Taken together, compound heat and drought <span class="hlt">events</span> led to the strongest C sink reduction compared to any single-factor extreme. A key insight of this paper, however, is that duration matters most: for heat stress during droughts, the magnitude of impacts systematically increased with duration, whereas under heat stress without drought, the response of Reco over time turned from an initial increase to a downregulation after about 2 weeks. This confirms earlier theories that</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/26263717','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/26263717"><span><span class="hlt">Annual</span> State of Connecticut Obstetrics and Gynecology Resident Research Day.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Seagle, Brandon-Luke L; Ballard, Jennifer; Kakar, Freshta; Panarelli, Erin; Samuelson, Robert; Shahabi, Shohreh</p> <p>2015-01-01</p> <p>To increase opportunities for Obstetrics and Gynecology(Ob/Gyn) residents to present their research, an <span class="hlt">Annual</span> State of Connecticut Ob/Gyn Resident Research Day (RRD) was created. At the first <span class="hlt">annual</span> RRD, 33 residents, representing five of six Connecticut Ob/Gyn residency programs, presented 39 poster and eight oral presentations. RRD evaluators rated the overall symposium and the quality of resident oral and poster presentations as either "excellent" or "above average." Residency program directors reported that the symposium was "very helpful" for evidencing resident scholarship as required by the Accreditation Council for Graduate Medical Education (ACGME). Surveyed residents reported that the symposium promoted their research and was a valuable investment of their time. An <span class="hlt">annual</span> specialty-specific, statewide RRD was created, experienced good participation, and was well evaluated. The <span class="hlt">annual</span>, statewide Ob/Gyn RRD may serve as a model for development of other specialty-specific, statewide RRD <span class="hlt">events</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUFMGC23A1223L','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUFMGC23A1223L"><span>Temporal Variation of NDVI and the Drivers of Climate Variables in the Arctic Tundra Transition <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Lee, J.; Ryu, Y.; Lee, Y. K.</p> <p>2016-12-01</p> <p>The Arctic is a sensitive region to temperature, which is drastically increasing with climate change. Vegetation in transition <span class="hlt">zones</span> of the sub-arctic tundra biome are most sensitive to the warming climate, as temperature in the Arctic ecosystem is one of important limiting factors of vegetation growth and decomposition. Previous research in the transition <span class="hlt">zone</span> show that there is a difference of sensible heat flux (21 Wm-2), Leaf Area Index increase from 0.58 - 2.76 and canopy height from 0.1 - 6.1m across dwarf and tall shrubs to forest, however, we lack understanding of NDVI trend of this <span class="hlt">zone</span>. To better understand the vegetation in transition <span class="hlt">zones</span> of the arctic ecosystem, we analyze the long-term trend of NDVI (AVHRR 3g GIMMs data), temperature and precipitation (Climate Research Unit data) trend from 1982 - 2010 in Council, Alaska that is a region where arctic tundra is transitioning to boreal forest. We also analyze how the climatic factors, temperature or precipitation, affect NDVI. <span class="hlt">Annual</span> precipitation had the highest interannual variability compared to temperature and NDVI. There was an overall decreasing trend of <span class="hlt">annual</span> maximum NDVI (y = -0.0019x+4.7). During 1982 to 2003, NDVI and temperature had a similar pattern, but when temperature suddenly jumped to 13.2°C in 2004, NDVI and precipitation declined. This study highlights that temperature increase does not always lead to greening, but after a certain threshold they may cause damage to sub-arctic tundra vegetation.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.usgs.gov/sir/2015/5110/sir20155110.pdf','USGSPUBS'); return false;" href="https://pubs.usgs.gov/sir/2015/5110/sir20155110.pdf"><span>2013 volcanic activity in Alaska: summary of <span class="hlt">events</span> and response of the Alaska Volcano Observatory</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Dixon, James P.; Cameron, Cheryl; McGimsey, Robert G.; Neal, Christina A.; Waythomas, Chris</p> <p>2015-08-14</p> <p>The Alaska Volcano Observatory (AVO) responded to eruptions, volcanic unrest or suspected unrest, and seismic <span class="hlt">events</span> at 18 volcanic centers in Alaska during 2013. Beginning with the 2013 AVO Summary of <span class="hlt">Events</span>, the <span class="hlt">annual</span> description of the AVO seismograph network and activity, once a stand-alone publication, is now part of this report. Because of this change, the <span class="hlt">annual</span> summary now contains an expanded description of seismic activity at Alaskan volcanoes. Eruptions occurred at three volcanic centers in 2013: Pavlof Volcano in May and June, Mount Veniaminof Volcano in June through December, and Cleveland Volcano throughout the year. None of these three eruptive <span class="hlt">events</span> resulted in 24-hour staffing at AVO facilities in Anchorage or Fairbanks.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018ClDy...50..249A','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018ClDy...50..249A"><span>Extreme weather <span class="hlt">events</span> in Iran under a changing climate</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Alizadeh-Choobari, Omid; Najafi, M. S.</p> <p>2018-01-01</p> <p>Observations unequivocally show that Iran has been rapidly warming over recent decades, which in sequence has triggered a wide range of climatic impacts. Meteorological records of several ground stations across Iran with daily temporal resolution for the period 1951-2013 were analyzed to investigate the climate change and its impact on some weather extremes. Iran has warmed by nearly 1.3 °C during the period 1951-2013 (+0.2 °C per decade), with an increase of the minimum temperature at a rate two times that of the maximum. Consequently, an increase in the frequency of heat extremes and a decrease in the frequency of cold extremes have been observed. The <span class="hlt">annual</span> precipitation has decreased by 8 mm per decade, causing an expansion of Iran's dry <span class="hlt">zones</span>. Previous studies have pointed out that warming is generally associated with more frequent heavy precipitation because a warmer air can hold more moisture. Nevertheless, warming in Iran has been associated with more frequent light precipitation, but less frequent moderate, heavy and extremely heavy precipitation. This is because in the subtropical dry <span class="hlt">zones</span>, a longer time is required to recharge the atmosphere with water vapour in a warmer climate, causing more water vapour to be transported from the subtropics to high latitudes before precipitations forms. In addition, the altitude of the condensation level increases in a warmer climate in subtropical regions, causing an overall decrease of precipitation. We argue that changing in the frequency of heavy precipitation in response to warming varies depending on the geographical location. Warming over the dry subtropical regions is associated with a decrease in the frequency of heavy precipitation, while an increase is expected over both subpolar and tropical regions. The warmer climate has also led to the increase in the frequency of both thunderstorms (driven by convective heating) and dust <span class="hlt">events</span> over Iran.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014AGUFM.T51B4620C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014AGUFM.T51B4620C"><span>Slab anisotropy from subduction <span class="hlt">zone</span> guided waves in Taiwan</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chen, K. H.; Tseng, Y. L.; Hu, J. C.</p> <p>2014-12-01</p> <p>Frozen-in anisotropic structure in the oceanic lithosphere and faulting/hydration in the upper layer of the slab are expected to play an important role in anisotropic signature of the subducted slab. Over the past several decades, despite the advances in characterizing anisotropy using shear wave splitting method and its developments, the character of slab anisotropy remains poorly understood. In this study we investigate the slab anisotropy using subduction <span class="hlt">zone</span> guided waves characterized by long path length in the slab. In the southernmost Ryukyu subduction <span class="hlt">zone</span>, seismic waves from <span class="hlt">events</span> deeper than 100 km offshore northern Taiwan reveal wave guide behavior: (1) a low-frequency (< 1 Hz) first arrival recognized on vertical and radial components but not transverse component (2) large, sustained high-frequency (3-10 Hz) signal in P and S wave trains. The depth dependent high-frequency content (3-10Hz) confirms the association with a waveguide effect in the subducting slab rather than localized site amplification effects. Using the selected subduction <span class="hlt">zone</span> guided wave <span class="hlt">events</span>, we further analyzed the shear wave splitting for intermediate-depth earthquakes in different frequency bands, to provide the statistically meaningful shear wave splitting parameters. We determine shear wave splitting parameters from the 34 PSP guided <span class="hlt">events</span> that are deeper than 100 km with ray path traveling along the subducted slab. From shear wave splitting analysis, the slab and crust effects reveal consistent polarization pattern of fast directions of EN-WS and delay time of 0.13 - 0.27 sec. This implies that slab anisotropy is stronger than the crust effect (<0.1 s) but weaker than the mantle wedge and sub-slab mantle effect (0.3-1.3 s) in Taiwan.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2003AGUFM.T52A0239M','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2003AGUFM.T52A0239M"><span>Spatio-temporal Evolution of On-going Tokai Slow Thrust Slip <span class="hlt">Event</span>, Central Japan</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Miyazaki, S.; Segall, P.; Kato, T.; McGuire, J.; Hatanaka, Y.</p> <p>2003-12-01</p> <p>We investigate an on-going slow thrust slip <span class="hlt">event</span> that occurred at a subduction <span class="hlt">zone</span> along the Nankai Trough off central Japan. The area we investimate, referred as the Tokai seismic gap, is located to the east of the 1944 Tonankai earthquake, which did not slip in the 1944 <span class="hlt">event</span>. Continuous GPS data from April 1996 to the end of 1999 shows that the stations in this region have secular velocities of ˜ 2 cm/yr to the northwest relative to the landward plate. The GPS time series show an abrupt increase in rate in late June, 2000. The accelerated rate is currently on-going. We model this non-secular deformation, which we refer to the 2000 Tokai slow slip <span class="hlt">event</span>, by transient slip at the plate interface and estimate their distribution with Kalman Filter based inversion methods. This <span class="hlt">event</span> initiated around (137.3oE, 34.9oN) almost at the same time of the onset of volcanic activity on Miyake-jima in late June, 2000. This suggests that the 2000 Tokai slow slip <span class="hlt">event</span> is triggered by the volcanic activity on Miyake-jima. Then the locus of the slip propagated to (137.5oE, 34.75oN) in second half of 2000, and kept slipping at the maximum rate of ˜ 15cm/yr through 2001. The peak slip-rate propagated to around (137.75oE, 34.9oN) in early 2002. The depth of slip <span class="hlt">zone</span> is ˜ 25km, which may correspond to the lower edge of the seismogenic <span class="hlt">zone</span> for the anticipated Tokai earthquake defined from seismicity. The cumulative moment magnitude of the slow slip <span class="hlt">event</span> to date is MW ˜ 6.8. The duration of this <span class="hlt">event</span> is longer than previously studied slow slip <span class="hlt">events</span> using GPS data, including the 1996 Bungo slow slip <span class="hlt">event</span> (about 1 year) and the 1996 and the 2000 Boso slow <span class="hlt">events</span> (a few weeks).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-08-20/pdf/2012-20348.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-08-20/pdf/2012-20348.pdf"><span>77 FR 50062 - Safety <span class="hlt">Zone</span>; Embry-Riddle Wings and Waves, Atlantic Ocean; Daytona Beach, FL</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-08-20</p> <p>... 1625-AA00 Safety <span class="hlt">Zone</span>; Embry-Riddle Wings and Waves, Atlantic Ocean; Daytona Beach, FL AGENCY: Coast...-Riddle Wings and Waves air show. The <span class="hlt">event</span> is scheduled to take place from Thursday, October 11, 2012...: Sec. 165.T07-0653 Safety <span class="hlt">Zone</span>; Embry Riddle Wings and Waves, Atlantic Ocean, Daytona Beach, FL. (a...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2010-title25-vol1/pdf/CFR-2010-title25-vol1-sec213-19.pdf','CFR'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2010-title25-vol1/pdf/CFR-2010-title25-vol1-sec213-19.pdf"><span>25 CFR 213.19 - Crediting advance <span class="hlt">annual</span> payments.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2010&page.go=Go">Code of Federal Regulations, 2010 CFR</a></p> <p></p> <p>2010-04-01</p> <p>... been made. No refund of such advance payments made under any lease will be allowed in the <span class="hlt">event</span> the royalty on production is not sufficient to equal such advance payment; nor will any part of the moneys so... 25 Indians 1 2010-04-01 2010-04-01 false Crediting advance <span class="hlt">annual</span> payments. 213.19 Section 213.19...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/24485908','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/24485908"><span>Effects of storm runoff on the thermal regime and water quality of a deep, stratified reservoir in a temperate monsoon <span class="hlt">zone</span>, in Northwest China.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Huang, Tinglin; Li, Xuan; Rijnaarts, Huub; Grotenhuis, Tim; Ma, Weixing; Sun, Xin; Xu, Jinlan</p> <p>2014-07-01</p> <p>Jinpen Reservoir is a deep, stratified reservoir in Shaanxi province, located in a warm temperate <span class="hlt">zone</span> of Northwest China. Influenced by a temperate monsoon climate, more than 60% of the <span class="hlt">annual</span> precipitation is concentrated from late summer to autumn (July-September). In recent years, extreme rainfall <span class="hlt">events</span> occurred more frequently and strongly affected the thermal structure, mixing layer depth and evolution of stratification of Jinpen Reservoir. The reservoir's inflow volume increased sharply after heavy rainfall during the flooding season. Large volumes of inflow induced mixing of stratified water <span class="hlt">zones</span> in early autumn and disturbed the stratification significantly. A temporary positive effect of such disturbance was the oxygenation of the water close to the bottom of the reservoir, leading to inhibition of the release of nutrients from sediments, especially phosphate. However, the massive inflow induced by storm runoff with increased oxygen-consuming substances led to an increase of the oxygen consumption rate. After the bottom water became anaerobic again, the bottom water quality would deteriorate due to the release of pollutants from sediments. Heavy rainfall <span class="hlt">events</span> could lead to very high nutrient input into the reservoir due to massive erosion from the surrounding uninhabited steep mountains, and the particulate matter contributed to most nutrient inputs. Reasonably releasing density flow is an effective way to reduce the amounts of particulate associated pollutants entering the reservoir. Significant turbid density flow always followed high rainfall <span class="hlt">events</span> in Jinpen Reservoir, which not only affected the reservoir water quality but also increased costs of the drinking water treatment plant. Understanding the effects of the storm runoff on the vertical distributions of water quality indicators could help water managers to select the proper position of the intake for the water plant in order to avoid high turbidity outflow. Copyright © 2014 Elsevier B</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018Geomo.307....3C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018Geomo.307....3C"><span>Reprint of "A proposed cell model for multiple-occurrence regional landslide <span class="hlt">events</span>: Implications for landslide susceptibility mapping"</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Crozier, M. J.</p> <p>2018-04-01</p> <p>Multiple-occurrence regional landslide <span class="hlt">events</span> (MORLEs) consist of hundreds to thousands of shallow landslides occurring more or less simultaneously within defined areas, ranging from tens to thousands of square kilometres. While MORLEs can be triggered by rainstorms and earthquakes, this paper is confined to those landslide <span class="hlt">events</span> triggered by rainstorms. Globally, MORLEs occur in a range of geological settings in areas of moderate to steep slopes subject to intense rainstorms. Individual landslides in rainstorm-triggered <span class="hlt">events</span> are dominantly small, shallow debris and earth flows, and debris and earth slides involving regolith or weathered bedrock. The model used to characterise these <span class="hlt">events</span> assumes that energy distribution within the <span class="hlt">event</span> area is represented on the land surface by a cell structure; with maximum energy expenditure within an identifiable core and rapid dissipation concentrically away from the centre. The version of the model presented here has been developed for rainfall-triggered landslide <span class="hlt">events</span>. It proposes that rainfall intensity can be used to determine different critical landslide response <span class="hlt">zones</span> within the cell (referred to as core, middle, and periphery <span class="hlt">zones</span>). These <span class="hlt">zones</span> are most readily distinguished by two conditions: the proportion of the slope that fails and the particular type of the slope stability factor that assumes dominance in determining specific sites of landslide occurrence. The latter condition means that the power of any slope stability factor to distinguish between stable and unstable sites varies throughout the affected area in accordance with the landslide response <span class="hlt">zones</span> within the cell; certain factors critical for determining the location of landslide sites in one part of the <span class="hlt">event</span> area have little influence in other parts of the <span class="hlt">event</span> area. The implication is that landslide susceptibility maps (and subsequently derived mitigation measures) based on conventional slope stability factors may have only limited validity</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012Litho.136....1Z','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012Litho.136....1Z"><span>Processes in continental collision <span class="hlt">zones</span>: Preface</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Zheng, Yong-Fei; Zhang, Lifei; McClelland, William C.; Cuthbert, Simon</p> <p>2012-04-01</p> <p>Formation and exhumation of high-pressure (HP) to ultrahigh-pressure (UHP) metamorphic rocks in continental subduction <span class="hlt">zones</span> are the two fundamental geodynamic aspects of collisional orogensis. This volume is based on the Session 08c titled "Geochemical processes in continental collision <span class="hlt">zones</span>" at Goldschmidt 2010 in Knoxville, USA. It focuses on micro- to macro-scale processes that are temporally and spatially linked to different depths of crustal subduction/exhumation and associated mineralogical changes. They are a key to understanding a wide spectrum of phenomena, involving HP/UHP metamorphism and syn-/post-collisional magmatism. Papers in this volume report progresses in petrological, geochronological and geochemical studies of UHP metamorphic rocks and their derivatives in China, with tectonic settings varying from arc-continent collision to continent-continent collision. Microbeam in-situ analyses of metamorphic and magmatic minerals are successfully utilized to solve various problems in the study of continental deep subduction and UHP metamorphism. In addition to their geochronological applications to dating of HP to UHP metamorphic <span class="hlt">events</span> during continental collision, microbeam techniques have also served as an efficient means to recognize different generations of mineral growth during continental subduction-<span class="hlt">zone</span> metamorphism. Furthermore, metamorphic dehydration and partial melting of UHP metamorphic rocks during subduction and exhumation are highlighted with respect to their effects on fluid action and element mobilization. These have provided new insights into chemical geodynamics in continental subduction <span class="hlt">zones</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-05-11/pdf/2010-11087.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-05-11/pdf/2010-11087.pdf"><span>75 FR 26157 - Safety <span class="hlt">Zone</span>; Reedville July 4th Celebration, Cockrell's Creek, Reedville, VA</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-05-11</p> <p>...-AA00 Safety <span class="hlt">Zone</span>; Reedville July 4th Celebration, Cockrell's Creek, Reedville, VA AGENCY: Coast Guard... Reedville July 4th Celebration <span class="hlt">event</span>. This action is intended to restrict vessel traffic movement on... established in the interest of public safety during the Reedville July 4th Celebration <span class="hlt">event</span> and will be...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_20");'>20</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li class="active"><span>22</span></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_22 --> <div id="page_23" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li class="active"><span>23</span></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="441"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=event&pg=5&id=EJ1025235','ERIC'); return false;" href="https://eric.ed.gov/?q=event&pg=5&id=EJ1025235"><span>Genetic and Environmental Influences on Negative Life <span class="hlt">Events</span> from Late Childhood to Adolescence</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Johnson, Daniel P.; Rhee, Soo Hyun; Whisman, Mark A.; Corley, Robin P.; Hewitt, John K.</p> <p>2013-01-01</p> <p>This multiwave longitudinal study tested two quantitative genetic developmental models to examine genetic and environmental influences on exposure to negative dependent and independent life <span class="hlt">events</span>. Participants (N = 457 twin pairs) completed measures of life <span class="hlt">events</span> <span class="hlt">annually</span> from ages 9 to 16. The same genetic factors influenced exposure to…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=rehydration&pg=2&id=ED346518','ERIC'); return false;" href="https://eric.ed.gov/?q=rehydration&pg=2&id=ED346518"><span>10 Cents To Save a Life: Ending Hunger as a Special <span class="hlt">Event</span>.</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Ames, Ina Ruth</p> <p></p> <p>The <span class="hlt">annual</span> "10 Cents to Save a Life" program is a special <span class="hlt">event</span> that has been held at Mount Ida College in Newton Centre, Massachusetts for two years. The purposes of the <span class="hlt">event</span> include: (1) teaching the public relations class and communication majors applied public relations theory through both a fundraising campaign and an education…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-07-05/pdf/2013-16049.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-07-05/pdf/2013-16049.pdf"><span>78 FR 40399 - Safety <span class="hlt">Zone</span>; Fifth Coast Guard District Fireworks Displays, Delaware River; Philadelphia, PA.</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-07-05</p> <p>... Philadelphia, Pennsylvania. The fireworks display is normally held on July 4th, but this year it will be held... America sponsors an <span class="hlt">annual</span> fireworks display held on July 4th over the waters of Delaware River... <span class="hlt">annually</span> on July 4th. However, this year, the fireworks <span class="hlt">event</span> will be held on July 6, 2013. A fleet of...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016AGUOSEC14C1001C','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016AGUOSEC14C1001C"><span>Field Observations of Swash-<span class="hlt">Zone</span> Dynamics on a Sea-Breeze Dominated Beach at the Yucatán Peninsula, México</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Chardon-Maldonado, P.; Puleo, J. A.; Torres-Freyermuth, A.</p> <p>2016-02-01</p> <p>Sea breezes can modify the nearshore processes and alter beach morphology depending on the geographical location. Prior studies have shown that surf <span class="hlt">zone</span> wave energy intensifies during strong sea-breeze conditions (wind speeds > 10 ms-1) and the impact on the coast can be similar to a small storm. However, few research efforts have investigated the coastal dynamics on sea-breeze dominated beaches (e.g., Masselink and Pattiaratchi, 1998, Mar. Geol.; Pattiaratchi et al., 1997, Cont. Shelf Res.) and, to the authors' knowledge, only one study has focused on swash-<span class="hlt">zone</span> processes (Sonu et al., 1973, EOS). A field study was performed on a microtidal, low wave energy, sea-breeze dominated sandy beach in order to investigate the effects of local (sea breeze) and synoptic (storm) scale meteorological <span class="hlt">events</span> on swash-<span class="hlt">zone</span> dynamics. In-situ measurements of swash-<span class="hlt">zone</span> hydrodynamics and sediment transport processes were collected from March 31st to April 12th, 2014 in Sisal, Yucatán located on the northern coast of the Yucatán Peninsula. Flow velocities and suspended sediment concentrations were measured concurrently, at multiple cross-shore and alongshore locations, using Vectrino-II profiling velocimeters and optical backscatter sensors, respectively. The high resolution data allowed the quantification of bed shear stress, turbulent dissipation rate, sediment loads and sediment flux during a mesoscale frontal system (cold-front passage referred to as an El Norte) and local sea-breeze cycles. Field observations showed that strong swash-<span class="hlt">zone</span> bed shear stresses, turbulence intensity and sediment suspension occur during energetic conditions (i.e., El Norte <span class="hlt">event</span>). On the other hand, despite milder energy conditions during the sea-breeze <span class="hlt">events</span>, the alongshore component of bed-shear stresses and velocities can be significant owing to the high incidence wave angle associated with the sea-breeze system in the study area. The increased forcing in the swash <span class="hlt">zone</span> induced sediment</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25512489','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25512489"><span>Cost-effective targeting of conservation investments to reduce the northern Gulf of Mexico hypoxic <span class="hlt">zone</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Rabotyagov, Sergey S; Campbell, Todd D; White, Michael; Arnold, Jeffrey G; Atwood, Jay; Norfleet, M Lee; Kling, Catherine L; Gassman, Philip W; Valcu, Adriana; Richardson, Jeffrey; Turner, R Eugene; Rabalais, Nancy N</p> <p>2014-12-30</p> <p>A seasonally occurring summer hypoxic (low oxygen) <span class="hlt">zone</span> in the northern Gulf of Mexico is the second largest in the world. Reductions in nutrients from agricultural cropland in its watershed are needed to reduce the hypoxic <span class="hlt">zone</span> size to the national policy goal of 5,000 km(2) (as a 5-y running average) set by the national Gulf of Mexico Task Force's Action Plan. We develop an integrated assessment model linking the water quality effects of cropland conservation investment decisions on the more than 550 agricultural subwatersheds that deliver nutrients into the Gulf with a hypoxic <span class="hlt">zone</span> model. We use this integrated assessment model to identify the most cost-effective subwatersheds to target for cropland conservation investments. We consider targeting of the location (which subwatersheds to treat) and the extent of conservation investment to undertake (how much cropland within a subwatershed to treat). We use process models to simulate the dynamics of the effects of cropland conservation investments on nutrient delivery to the Gulf and use an evolutionary algorithm to solve the optimization problem. Model results suggest that by targeting cropland conservation investments to the most cost-effective location and extent of coverage, the Action Plan goal of 5,000 km(2) can be achieved at a cost of $2.7 billion <span class="hlt">annually</span>. A large set of cost-hypoxia tradeoffs is developed, ranging from the baseline to the nontargeted adoption of the most aggressive cropland conservation investments in all subwatersheds (estimated to reduce the hypoxic <span class="hlt">zone</span> to less than 3,000 km(2) at a cost of $5.6 billion <span class="hlt">annually</span>).</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-06-17/pdf/2013-14332.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-06-17/pdf/2013-14332.pdf"><span>78 FR 36122 - Fisheries of the Exclusive Economic <span class="hlt">Zone</span> Off Alaska; Bering Sea and Aleutian Islands Crab...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-06-17</p> <p>... the harvesting and processing sectors'' and to monitor the ``economic stability for harvesters.... 120806311-3530-02] RIN 0648-BC25 Fisheries of the Exclusive Economic <span class="hlt">Zone</span> Off Alaska; Bering Sea and... Tanner Crabs (FMP). These regulations revise the <span class="hlt">annual</span> economic data reports (EDRs) currently required...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=conference+AND+experiment&id=EJ1035026','ERIC'); return false;" href="https://eric.ed.gov/?q=conference+AND+experiment&id=EJ1035026"><span>The Virtual Extension <span class="hlt">Annual</span> Conference: Addressing Contemporary Professional Development Needs</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Franz, Nancy K.; Brekke, Robin; Coates, Deb; Kress, Cathann; Hlas, Julie</p> <p>2014-01-01</p> <p>Extension systems are experimenting with new models for conducting professional development to enhance staff competence and other returns on professional development investments. The ISUEO virtual <span class="hlt">annual</span> conference provides a successful flipped classroom model of asynchronous and synchronous learning <span class="hlt">events</span> for conducting an Extension annual…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-06-19/pdf/2013-14548.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-06-19/pdf/2013-14548.pdf"><span>78 FR 36664 - Safety <span class="hlt">Zone</span>; Fifth Coast Guard District Fireworks Display, Currituck Sound; Corolla, NC</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-06-19</p> <p>... 1625-AA00 Safety <span class="hlt">Zone</span>; Fifth Coast Guard District Fireworks Display, Currituck Sound; Corolla, NC.... This regulation applies to only one recurring fireworks <span class="hlt">event</span>, held adjacent to the Currituck Sound... portion of the Currituck Sound, Corolla, NC, during the <span class="hlt">event</span>. DATES: This rule will be effective from...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70036368','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70036368"><span>Quantifying potential tsunami hazard in the Puysegur subduction <span class="hlt">zone</span>, south of New Zealand</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Hayes, G.P.; Furlong, K.P.</p> <p>2010-01-01</p> <p>Studies of subduction <span class="hlt">zone</span> seismogenesis and tsunami potential, particularly of large subduction <span class="hlt">zones</span>, have recently seen a resurgence after the great 2004 earthquake and tsunami offshore of Sumatra, yet these global studies have generally neglected the tsunami potential of small subduction <span class="hlt">zones</span> such as the Puysegur subduction <span class="hlt">zone</span>, south of New Zealand. Here, we study one such relatively small subduction <span class="hlt">zone</span> by analysing the historical seismicity over the entire plate boundary region south of New Zealand, using these data to determine the seismic moment deficit of the subduction <span class="hlt">zone</span> over the past ~100 yr. Our calculations indicate unreleased moment equivalent to a magnitude Mw 8.3 earthquake, suggesting this subduction <span class="hlt">zone</span> has the potential to host a great, tsunamigenic <span class="hlt">event</span>. We model this tsunami hazard and find that a tsunami caused by a great earthquake on the Puysegur subduction <span class="hlt">zone</span> would pose threats to the coasts of southern and western South Island, New Zealand, Tasmania and southeastern Australia, nearly 2000 km distant. No claim to original US government works Geophysical Journal International ?? 2010 RAS.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2015CoMP..170...11S','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2015CoMP..170...11S"><span>Genesis of the central <span class="hlt">zone</span> of the Nolans Bore rare earth element deposit, Northern Territory, Australia</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Schoneveld, Louise; Spandler, Carl; Hussey, Kelvin</p> <p>2015-08-01</p> <p> the surrounding host rocks. Where allanite and fluorapatite are texturally related, the fluorapatite is relatively depleted in the light rare earth elements (LREEs), whereas allanite is relatively LREE enriched, suggesting co-crystallisation. We tentatively date the BX1 ore stage to 1440 ± 80 Ma based on U-Pb dating of thorianite. Sm-Nd isotope isochrons derived from in situ isotope analysis of cognate apatite and allanite date the BX2 and BX3 <span class="hlt">events</span> to ca. 400 Ma, while U-Pb dating of late-stage monazite from the BX4 ore stage returned an age of ca. 350 Ma. Therefore, formation of the central <span class="hlt">zone</span> at Nolans Bore involved multiple alteration/brecciation <span class="hlt">events</span> that collectively span over 1 billion years in duration. We suggest that the BX1-type veins and breccias were formed from REE-rich, saline (F- and Cl-bearing) fluids that infiltrated the granulite-grade host rocks in association with either shear activation <span class="hlt">events</span> of the Redbank Shear <span class="hlt">Zone</span> (1500-1400 Ma) or intrusion of late-stage pegmatites of the Mt Boothby area. BX2, BX3, and BX4 <span class="hlt">events</span> record deformation and hydrothermal alteration associated with the Alice Springs Orogeny (400-350 Ma). These hydrothermal <span class="hlt">events</span> occurred at temperatures of 450 to ~600 °C, due to inflow of highly acidic hydrous fluids derived from a magmatic source, or from mixing of meteoric and metamorphic fluids. Our data testify to the long and complex geological history of not only the Nolans Bore REE deposit, but also of the rocks of the eastern Reynolds Range, and demonstrate the great utility of using hydrothermally derived REE minerals to trace the timing of crustal deformation <span class="hlt">events</span> and source of associated hydrothermal fluids.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://eric.ed.gov/?q=%22marketing+performance%22&pg=2&id=ED180338','ERIC'); return false;" href="https://eric.ed.gov/?q=%22marketing+performance%22&pg=2&id=ED180338"><span>Issues for the Eighties. Association for Institutional Research <span class="hlt">Annual</span> Forum Proceedings No. 2. Nineteenth <span class="hlt">Annual</span> Forum. (San Diego, California, May 13-17, 1979).</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>Staskey, Paul J., Ed.</p> <p></p> <p>Proceedings of the nineteenth <span class="hlt">annual</span> AIR (Association for Institutional Research) forum on issues for the 1980's are provided. The proceedings contain 71 abstracts or descriptions of the contributed papers, seminars, panels, special interest groups, and workshops presented during the four-day <span class="hlt">event</span>. The following four major addresses are included…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-04-20/pdf/2012-9519.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-04-20/pdf/2012-9519.pdf"><span>77 FR 23601 - Special Local Regulations and Safety <span class="hlt">Zones</span>; Recurring <span class="hlt">Events</span> in Northern New England</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-04-20</p> <p>... Multiple Sclerosis Regatta......... <span class="hlt">Event</span> Type: Regatta and Sailboat Race. Sponsor: Maine Chapter, Multiple...'' W. 8.7 Multiple Sclerosis Harborfest <span class="hlt">Event</span> Type: Power Boat Tugboat Race. Race. Sponsor: Maine Chapter, National Multiple Sclerosis Society. Date: A one day <span class="hlt">event</span> on Sunday during the third week of...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-06-12/pdf/2012-14220.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-06-12/pdf/2012-14220.pdf"><span>77 FR 34894 - Safety <span class="hlt">Zone</span>; Bostock 50th Anniversary Fireworks, Long Island Sound; Manursing Island, NY</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-06-12</p> <p>... 1625-AA00 Safety <span class="hlt">Zone</span>; Bostock 50th Anniversary Fireworks, Long Island Sound; Manursing Island, NY... establish a temporary safety <span class="hlt">zone</span> on the navigable waters of Long Island Sound in the vicinity of Manursing... from a portion of Long Island Sound before, during, and immediately after the fireworks <span class="hlt">event</span>. DATES...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-08-24/pdf/2012-20831.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-08-24/pdf/2012-20831.pdf"><span>77 FR 51473 - Safety <span class="hlt">Zone</span>; Bostock 50th Anniversary Fireworks, Long Island Sound; Manursing Island, NY</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-08-24</p> <p>... 1625-AA00 Safety <span class="hlt">Zone</span>; Bostock 50th Anniversary Fireworks, Long Island Sound; Manursing Island, NY... <span class="hlt">zone</span> on the navigable waters of Long Island Sound in the vicinity of Manursing Island, NY for a... of Long Island Sound before, during, and immediately after the fireworks <span class="hlt">event</span>. DATES: This rule is...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec165-1332.pdf','CFR2014'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2014-title33-vol2/pdf/CFR-2014-title33-vol2-sec165-1332.pdf"><span>33 CFR 165.1332 - Safety <span class="hlt">Zones</span>; <span class="hlt">annual</span> firework displays within the Captain of the Port, Puget Sound Area of...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2014&page.go=Go">Code of Federal Regulations, 2014 CFR</a></p> <p></p> <p>2014-07-01</p> <p>... displays within the Captain of the Port, Puget Sound Area of Responsibility. 165.1332 Section 165.1332... within the Captain of the Port, Puget Sound Area of Responsibility. (a) Safety <span class="hlt">Zones</span>. The following areas are designated safety <span class="hlt">zones</span>: (1) All waters of Puget Sound, Washington, extending to a 450 yard radius...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec165-1332.pdf','CFR2011'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2011-title33-vol2/pdf/CFR-2011-title33-vol2-sec165-1332.pdf"><span>33 CFR 165.1332 - Safety <span class="hlt">Zones</span>; <span class="hlt">annual</span> firework displays within the Captain of the Port, Puget Sound Area of...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2011&page.go=Go">Code of Federal Regulations, 2011 CFR</a></p> <p></p> <p>2011-07-01</p> <p>... displays within the Captain of the Port, Puget Sound Area of Responsibility. 165.1332 Section 165.1332... within the Captain of the Port, Puget Sound Area of Responsibility. (a) Safety <span class="hlt">Zones</span>. The following areas are designated safety <span class="hlt">zones</span>: (1) All waters of Puget Sound, Washington, extending to a 450 yard radius...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec165-1332.pdf','CFR2012'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2012-title33-vol2/pdf/CFR-2012-title33-vol2-sec165-1332.pdf"><span>33 CFR 165.1332 - Safety <span class="hlt">Zones</span>; <span class="hlt">annual</span> firework displays within the Captain of the Port, Puget Sound Area of...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2012&page.go=Go">Code of Federal Regulations, 2012 CFR</a></p> <p></p> <p>2012-07-01</p> <p>... displays within the Captain of the Port, Puget Sound Area of Responsibility. 165.1332 Section 165.1332... within the Captain of the Port, Puget Sound Area of Responsibility. (a) Safety <span class="hlt">Zones</span>. The following areas are designated safety <span class="hlt">zones</span>: (1) All waters of Puget Sound, Washington, extending to a 450 yard radius...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol2/pdf/CFR-2013-title33-vol2-sec165-1332.pdf','CFR2013'); return false;" href="https://www.gpo.gov/fdsys/pkg/CFR-2013-title33-vol2/pdf/CFR-2013-title33-vol2-sec165-1332.pdf"><span>33 CFR 165.1332 - Safety <span class="hlt">Zones</span>; <span class="hlt">annual</span> firework displays within the Captain of the Port, Puget Sound Area of...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collectionCfr.action?selectedYearFrom=2013&page.go=Go">Code of Federal Regulations, 2013 CFR</a></p> <p></p> <p>2013-07-01</p> <p>... displays within the Captain of the Port, Puget Sound Area of Responsibility. 165.1332 Section 165.1332... within the Captain of the Port, Puget Sound Area of Responsibility. (a) Safety <span class="hlt">Zones</span>. The following areas are designated safety <span class="hlt">zones</span>: (1) All waters of Puget Sound, Washington, extending to a 450 yard radius...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/biblio/6215692-geophysical-geological-studies-possible-extensions-new-madrid-fault-zone-annual-report-vol','SCIGOV-STC'); return false;" href="https://www.osti.gov/biblio/6215692-geophysical-geological-studies-possible-extensions-new-madrid-fault-zone-annual-report-vol"><span>Geophysical-geological studies of possible extensions of the New Madrid Fault <span class="hlt">Zone</span>. <span class="hlt">Annual</span> report, 1982. Vol. 1</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Hinze, W.J.; Braile, L.W.; Keller, G.R.</p> <p>1983-05-01</p> <p>An integrated geophysical/geologic program is being conducted to evaluate the rift complex hypothesis as an explanation for the earthquake activity in the New Madrid Seismic <span class="hlt">Zone</span> and its extensions, to refine our knowledge of the rift complex, and to investigate the possible northern extensions of the New Madrid Fault <span class="hlt">Zone</span>, especially its possible connection to the Anna, Ohio seismogenic region. Drillhole basement lithologies are being investigated to aid in tectonic analysis and geophysical interpretation, particularly in the Anna, Ohio area. Gravity and magnetic modeling combined with limited seismic reflection studies in southwest Indiana are interpreted as confirming speculation that anmore » arm of the New Madrid Rift Complex extends northeasterly into Indiana. The geologic and geophysical evidence confirm that the basement lithology in the Anna, Ohio area is highly variable reflecting a complex geologic history. The data indicate that as many as three major Late Precambrian tectonic features intersect within the basement of the Anna area suggesting that the seismicity may be related to basement <span class="hlt">zones</span> of weakness.« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-06-02/pdf/2011-13438.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-06-02/pdf/2011-13438.pdf"><span>76 FR 31839 - Safety <span class="hlt">Zones</span>; <span class="hlt">Annual</span> <span class="hlt">Events</span> Requiring Safety <span class="hlt">Zones</span> in the Captain of the Port Sault Sainte Marie...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-06-02</p> <p>... first Saturday of August from 9 p.m. until 11 p.m. (20) Alpena Fourth of July Celebration Fireworks, Alpena, MI: (i) Location. All U.S. navigable waters of Lake Huron within an 800-foot radius of the...</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li class="active"><span>23</span></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_23 --> <div id="page_24" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li class="active"><span>24</span></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="461"> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-09-20/pdf/2011-24142.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-09-20/pdf/2011-24142.pdf"><span>76 FR 58108 - Safety <span class="hlt">Zone</span>; Ryder Cup Captain's Duel Golf Shot, Chicago River, Chicago, IL</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-09-20</p> <p>...-AA00 Safety <span class="hlt">Zone</span>; Ryder Cup Captain's Duel Golf Shot, Chicago River, Chicago, IL AGENCY: Coast Guard... Ryder Cup Captain's Duel Golf Shot <span class="hlt">event</span> takes place on the Chicago River near Chicago, Illinois from 4... reasons: the safety <span class="hlt">zone</span> will only be in effect for one hour on a single day and vessels will be allowed...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-04-13/pdf/2010-8374.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-04-13/pdf/2010-8374.pdf"><span>75 FR 18778 - Safety <span class="hlt">Zone</span>; Ocean City Air Show 2010, Atlantic Ocean, Ocean City, MD</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-04-13</p> <p>...-AA00 Safety <span class="hlt">Zone</span>; Ocean City Air Show 2010, Atlantic Ocean, Ocean City, MD AGENCY: Coast Guard, DHS... <span class="hlt">zone</span> on the Atlantic Ocean in the vicinity of Ocean City, Maryland to support the Ocean City Air Show..., 5, and 6, 2010 Ocean City, Maryland will host an air show <span class="hlt">event</span> on the Atlantic Ocean between Talbot...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/25061132','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/25061132"><span>Intense foreshocks and a slow slip <span class="hlt">event</span> preceded the 2014 Iquique Mw 8.1 earthquake.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Ruiz, S; Metois, M; Fuenzalida, A; Ruiz, J; Leyton, F; Grandin, R; Vigny, C; Madariaga, R; Campos, J</p> <p>2014-09-05</p> <p>The subduction <span class="hlt">zone</span> in northern Chile is a well-identified seismic gap that last ruptured in 1877. The moment magnitude (Mw) 8.1 Iquique earthquake of 1 April 2014 broke a highly coupled portion of this gap. To understand the seismicity preceding this <span class="hlt">event</span>, we studied the location and mechanisms of the foreshocks and computed Global Positioning System (GPS) time series at stations located on shore. Seismicity off the coast of Iquique started to increase in January 2014. After 16 March, several Mw > 6 <span class="hlt">events</span> occurred near the low-coupled <span class="hlt">zone</span>. These <span class="hlt">events</span> migrated northward for ~50 kilometers until the 1 April earthquake occurred. On 16 March, on-shore continuous GPS stations detected a westward motion that we model as a slow slip <span class="hlt">event</span> situated in the same area where the mainshock occurred. Copyright © 2014, American Association for the Advancement of Science.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17330457','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17330457"><span>[Variability of vegetation growth season in different latitudinal <span class="hlt">zones</span> of North China: a monitoring by NOAA NDVI and MSAVI].</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Wang, Hong; Li, Xiaobing; Han, Ruibo; Ge, Yongqin</p> <p>2006-12-01</p> <p>In this study, North China was latitudinally divided into five <span class="hlt">zones</span>, i.e., 32 degrees - 36 degrees N (<span class="hlt">Zone</span> I), 36 degrees - 40 degrees N (<span class="hlt">Zone</span> II), 40 degrees - 44 degrees N (<span class="hlt">Zone</span> III), 44 degrees - 48 degrees N (<span class="hlt">Zone</span> IV) and 48 degrees - 52 degrees N (<span class="hlt">Zone</span> V), and the NOAA/ AVHRR NDVI and MSAVI time-series images from 1982 to 1999 were smoothed with Savitzky-Golay filter algorithm. Based on the EOF analysis, the principal components of NDVI and MSAVI for the vegetations in different latitudinal <span class="hlt">zones</span> of North China were extracted, the <span class="hlt">annual</span> beginning and ending dates and the length of growth season in 1982 - 1999 were estimated, and the related parameters were linearly fitted, aimed to analyze the variability of vegetation growth season. The results showed that the beginning date of the growth season in different <span class="hlt">zones</span> tended to be advanced, while the ending date tended to be postponed with increasing latitude. The length of the growth season was also prolonged, with the prolonging time exceeded 10 days.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/17545134','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/17545134"><span>Intra-<span class="hlt">annual</span> height increment of Pinus sylvestris at high latitudes in Finland.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Salminen, Hannu; Jalkanen, Risto</p> <p>2007-09-01</p> <p>Intra-<span class="hlt">annual</span> height growth of Scots pine (Pinus sylvestris L.) in four stands was followed for up to four growing seasons (2000-2003) in the northern boreal <span class="hlt">zone</span> in Lapland. Elongation of the leader shoot correlated with temperature sum expressed as degree-days. Total length of the leader shoot correlated with growth rate but not with duration of the height-growth period. The longer the <span class="hlt">annual</span> shoot at the end of the season, the greater the height increment per degree- and growing day. Height-growth cessation was defined as the date when 95% of the total shoot length was achieved. In all stands and all years, height growth ceased when, on average, 41% of the relative temperature sum of the site was achieved (range of variation 38-43%). The relative temperature sum was calculated by dividing the actual temperature sum by the long-term mean for the site. Our results suggest that <span class="hlt">annual</span> height growth is finished when a location-specific temperature sum threshold is attained.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014JSG....66...75R','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014JSG....66...75R"><span>Coseismic microstructures of experimental fault <span class="hlt">zones</span> in Carrara marble</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ree, Jin-Han; Ando, Jun-ichi; Han, Raehee; Shimamoto, Toshihiko</p> <p>2014-09-01</p> <p>Experimental fault <span class="hlt">zones</span> developed in Carrara marble that were deformed at seismic slip rates (1.18-1.30 m s-1) using a high-velocity-rotary-shear apparatus exhibit very low friction (friction coefficient as low as 0.06) at steady state due to nanoparticle lubrication of the decomposition product (lime). The fault <span class="hlt">zones</span> show a layered structure; a central slip-localization layer (5-60 μm thick) of lime nanograins mantled by gouge layers (5-150 μm thick) and a plastically deformed layer (45-500 μm thick) between the wall rock and gouge layer in the marginal portion of cylindrical specimens. Calcite grains of the wall rock adjacent to the slip <span class="hlt">zone</span> deform by dislocation glide when subjected to frictional heating and a lower strain rate than that of the principal slip <span class="hlt">zone</span>. The very fine (2-5 μm) calcite grains in the gouge layer show a foam structure with relatively straight grain boundaries and 120° triple junctions. This foam structure is presumed to develop by welding at high temperature and low strain once slip is localized along the central layer. We suggest that a seismic <span class="hlt">event</span> can be inferred from deformed marbles, given: (i) the presence of welded gouge with foam structure in a fault <span class="hlt">zone</span> where wall rocks show no evidence of thermal metamorphism and (ii) a thin plastically deformed layer immediately adjacent to the principal slip <span class="hlt">zone</span> of a cataclastic fault <span class="hlt">zone</span>.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70186619','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70186619"><span>Latest Paleocene lithologic and biotic <span class="hlt">events</span> in neritic deposits of southwestern New Jersey</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Gibson, Thomas G.; Bybell, Laurel M.; Owens, James P.</p> <p>1993-01-01</p> <p>In the southwestern New Jersey Coastal Plain, four drill holes contain continuous neritic sedimentation across the Paleocene/Eocene boundary (calcareous nannofossil <span class="hlt">Zone</span> NP 9/NP 10 boundary). Significant lithologic and biotic changes occur in these strata near the top of the Paleocene. Global warming, increased precipitation, and other oceanographic and climatic <span class="hlt">events</span> that have been recognized in high-latitude, deep-oceanic deposits of the latest Paleocene also influenced mid-latitude, shallow-marine, and terrestrial environments of the western North Atlantic. The diverse, well-preserved calcareous nannofossil flora that is present throughout the entire New Jersey boundary section accurately places these <span class="hlt">events</span> within the uppermost part of the upper Paleocene <span class="hlt">Zone</span> NP 9. Several rapid but gradational changes occur within a 1.1-m interval near the top of <span class="hlt">Zone</span> NP 9. The changes include (1) a change in lithology from glauconitic quartz sand to clay, (2) a change in clay mineral suites from illite/smectite-dominated to kaolinite-dominated, (3) a change in benthic foraminiferal assemblages to a lower diversity fauna suggestive of low-oxygen environments, (4) a significant increase in planktonic foraminiferal abundance, and (5) an increased species turnover rate in marine calcareous nannofossils. Pollen was sparse in the New Jersey drill holes, but terrestrial sporomorph species in Virginia exhibit increased turnover rates at a correlative level. Foraminiferal assemblages and lithology indicate that relative sea level rose in New Jersey at the same time as these late Paleocene <span class="hlt">events</span> occurred in late Biochron NP 9. The higher sea levels influenced sediment type and absolute abundance of planktonic foraminifers in the deposits. Above the initial increase of kaolinite in the upper part of <span class="hlt">Zone</span> NP 9, the kaolinite percentage continues to increase, and the maximum kaolinite value occurs in the uppermost part of <span class="hlt">Zone</span> NP 9. There are few changes in either the sediments or the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://www.ars.usda.gov/research/publications/publication/?seqNo115=336035','TEKTRAN'); return false;" href="http://www.ars.usda.gov/research/publications/publication/?seqNo115=336035"><span>Atmospheric dust <span class="hlt">events</span> in Central Asia: Relationship to wind, soil type, and land use</span></a></p> <p><a target="_blank" href="https://www.ars.usda.gov/research/publications/find-a-publication/">USDA-ARS?s Scientific Manuscript database</a></p> <p></p> <p></p> <p>Xinjiang Province is one of the most important source regions of atmospheric dust in China. Spatial-temporal characteristics of dust <span class="hlt">events</span> in the region were investigated by time series analysis of <span class="hlt">annual</span> dust <span class="hlt">event</span> frequency and meteorological data collected at 101 stations in Xinjiang Province fr...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-03-30/pdf/2011-6783.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-03-30/pdf/2011-6783.pdf"><span>76 FR 17530 - Special Local Regulations and Safety <span class="hlt">Zones</span>; Recurring <span class="hlt">Events</span> in Northern New England</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-03-30</p> <p>...'' N 069[deg] 31'56'' W. 8.6 Multiple Sclerosis Regatta.... <span class="hlt">Event</span> Type: Regatta and Sailboat Race. Sponsor: Maine Chapter, Multiple Sclerosis Society. Date: A one day <span class="hlt">event</span> on Saturday during the third... 070[deg] 13'51'' W. 8.7 Multiple Sclerosis Harborfest <span class="hlt">Event</span> Type: Power Boat Tugboat Race. Race...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2014EGUGA..16.4242F','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2014EGUGA..16.4242F"><span>Vadose <span class="hlt">zone</span> studies at an industrial contaminated site: the vadose <span class="hlt">zone</span> monitoring system and cross-hole geophysics</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Fernandez de Vera, Natalia; Beaujean, Jean; Jamin, Pierre; Nguyen, Frédéric; Dahan, Ofer; Vanclooster, Marnik; Brouyère, Serge</p> <p>2014-05-01</p> <p> installed in two slanted boreholes on site, together with four vertical boreholes containing electrodes for geophysical measurements. Currently the site is being monitored under natural recharge conditions. Initial results show the reaction of the vadose <span class="hlt">zone</span> to rainfall <span class="hlt">events</span>, as well as chemical evolution of soil water with depth.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-03-05/pdf/2013-05076.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-03-05/pdf/2013-05076.pdf"><span>78 FR 14188 - Safety <span class="hlt">Zone</span>, Change to Enforcement Period, Patapsco River, Northwest and Inner Harbors; Baltimore...</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-03-05</p> <p>... enforcement period of a safety <span class="hlt">zone</span> regulation for the <span class="hlt">annual</span> movement of the historic sloop-of-war USS... sloop-of-war USS CONSTELLATION in Baltimore, Maryland on the Thursday before Memorial Day (observed... McHenry National Monument and Historic Site. Beginning at 3 p.m., the historic Sloop-of-War USS...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/1999Tectp.314..161W','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/1999Tectp.314..161W"><span>Regional and teleseismic <span class="hlt">events</span> recorded across the TESZ during POLONAISE'97</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Wilde-Piórko, M.; Grad, M.; Polonaise Working Group</p> <p>1999-12-01</p> <p>20 Polish short-period three-component stations were continuously operating for three weeks during POLONAISE'97 in the contact <span class="hlt">zone</span> between Palaeozoic and Precambrian platforms in Poland. The distances between seismometers were about 20 km and the digitization interval was 0.02 s. Besides the shots, a few regional <span class="hlt">events</span> from the Lubin area and teleseismic <span class="hlt">events</span> mainly from the SE backazimuth were also recorded. Interpretation of traveltimes for P and S waves for regional <span class="hlt">events</span> using a simplified LT-7 model of crustal structure for theoretical calculation allowed correction of their origin time. The same model can also explain the traveltime residuals of P waves for teleseismic <span class="hlt">events</span>. The main features of the division of Poland into two platforms by the Teisseyre-Tornquist tectonic <span class="hlt">zone</span> (TTZ) is seen both in the shape of residuals of teleseismic phases and in the receiver function. A passive seismic experiment made during POLONAISE'97 as a reconnaissance for future teleseismic tomography experiment TOR-2 gave quite promising results; however, to make a traveltime tomography and receiver function analysis, the duration of data acquisition should be about half a year.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70012388','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70012388"><span>Littoral transport in the surf <span class="hlt">zone</span> elucidated by an Eulerian sediment tracer.</span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Duane, D.B.; James, W.R.</p> <p>1980-01-01</p> <p>An Eulerian, or time integration, sand tracer experiment was designed and carried out in the surf <span class="hlt">zone</span> near Pt. Mugu, California on April 19, 1972. Data indicate that conditions of stationarity and finite boundaries required for proper application of Eulerian tracer theory exist for short time periods in the surf <span class="hlt">zone</span>. Grain counts suggest time required for tracer sand to attain equilibrium concentration is on the order of 30-60 minutes. Grain counts also indicate transport (discharge) was strongly dependent upon grain size, with the maximum rate occurring in the size 2.5-2.75 phi, decreasing to both finer and coarser sizes. The measured instantaneous transport was at the <span class="hlt">annual</span> rate of 2.4 x 106 m3/yr.- Authors</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-06-15/pdf/2012-14727.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-06-15/pdf/2012-14727.pdf"><span>77 FR 35848 - Safety <span class="hlt">Zone</span>, Fourth of July Fireworks <span class="hlt">Event</span>, Pagan River, Smithfield, VA</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-06-15</p> <p>.... ACTION: Temporary Final rule. SUMMARY: The Coast Guard is establishing a 420-foot radius safety <span class="hlt">zone</span> on..., and falling hot embers or other debris, vessel traffic will be temporarily restricted within 420 feet... navigable waters of the Pagan River within the area bounded by a 420-foot radius circle centered on position...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2012AGUFM.T21F..01I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2012AGUFM.T21F..01I"><span>Episodic slow slip <span class="hlt">events</span> in the Japan subduction <span class="hlt">zone</span> before the 2011 Tohoku-Oki earthquake</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ito, Y.; Hino, R.; Kido, M.; Fujimoto, H.; Osada, Y.; Inazu, D.; Ohta, Y.; Iinuma, T.; Ohzono, M.; Mishina, M.; Miura, S.; Suzuki, K.; Tsuji, T.; Ashi, J.</p> <p>2012-12-01</p> <p>We describe two transient slow slip <span class="hlt">events</span> that occurred before the 2011 Tohoku-Oki earthquake. The first transient crustal deformation, which occurred over a period of a week in November 2008, was recorded simultaneously using ocean-bottom pressure gauges and an on-shore volumetric strainmeter; this deformation has been interpreted as being an M6.8 episodic slow slip <span class="hlt">event</span>. The second had a duration exceeding 1 month and was observed in February 2011, just before the 2011 Tohoku-Oki earthquake; the moment magnitude of this <span class="hlt">event</span> reached 7.0. The two <span class="hlt">events</span> preceded interplate earthquakes of magnitudes M6.1 (December 2008) and M7.3 (March 9, 2011), respectively; the latter is the largest foreshock of the 2011 Tohoku-Oki earthquake. Our findings indicate that these slow slip <span class="hlt">events</span> induced increases in shear stress, which in turn triggered the interplate earthquakes. The slow slip <span class="hlt">event</span> source area on the fault is also located within the downdip portion of the huge-coseismic-slip area of the 2011 earthquake. This demonstrates episodic slow slip and seismic behavior occurring on the same portions of the megathrust fault, suggesting that the faults undergo slip in slow slip <span class="hlt">events</span> can also rupture seismically.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2013Tectp.600...14I','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2013Tectp.600...14I"><span>Episodic slow slip <span class="hlt">events</span> in the Japan subduction <span class="hlt">zone</span> before the 2011 Tohoku-Oki earthquake</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Ito, Yoshihiro; Hino, Ryota; Kido, Motoyuki; Fujimoto, Hiromi; Osada, Yukihito; Inazu, Daisuke; Ohta, Yusaku; Iinuma, Takeshi; Ohzono, Mako; Miura, Satoshi; Mishina, Masaaki; Suzuki, Kensuke; Tsuji, Takeshi; Ashi, Juichiro</p> <p>2013-07-01</p> <p>We describe two transient slow slip <span class="hlt">events</span> that occurred before the 2011 Tohoku-Oki earthquake. The first transient crustal deformation, which occurred over a period of a week in November 2008, was recorded simultaneously using ocean-bottom pressure gauges and an on-shore volumetric strainmeter; this deformation has been interpreted as being an M6.8 episodic slow slip <span class="hlt">event</span>. The second had a duration exceeding 1 month and was observed in February 2011, just before the 2011 Tohoku-Oki earthquake; the moment magnitude of this <span class="hlt">event</span> reached 7.0. The two <span class="hlt">events</span> preceded interplate earthquakes of magnitudes M6.1 (December 2008) and M7.3 (March 9, 2011), respectively; the latter is the largest foreshock of the 2011 Tohoku-Oki earthquake. Our findings indicate that these slow slip <span class="hlt">events</span> induced increases in shear stress, which in turn triggered the interplate earthquakes. The slow slip <span class="hlt">event</span> source area on the fault is also located within the downdip portion of the huge-coseismic-slip area of the 2011 earthquake. This demonstrates episodic slow slip and seismic behavior occurring on the same portions of the megathrust fault, suggesting that the faults undergo slip in slow slip <span class="hlt">events</span> can also rupture seismically.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2013-12-23/pdf/2013-30387.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2013-12-23/pdf/2013-30387.pdf"><span>78 FR 77385 - Special Local Regulations and Safety <span class="hlt">Zones</span>; Recurring <span class="hlt">Events</span> in Northern New England</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2013-12-23</p> <p>...[deg]12'19'' W. 6.2 Charlie Begin Memorial Lobster Boat <span class="hlt">Event</span> Type: Power Boat Races. Race. Sponsor: Boothbay Harbor Lobster Boat Race Committee. Date: A one day <span class="hlt">event</span> in June.* Time (Approximate): 10:00 am...'' W. 6.3 Rockland Harbor Lobster Boat Races. <span class="hlt">Event</span> Type: Power Boat Race. Sponsor: Rockland Harbor...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70017110','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70017110"><span>Reconciling short recurrence intervals with minor deformation in the New Madrid seismic <span class="hlt">zone</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Schweig, E.S.; Ellis, M.A.</p> <p>1994-01-01</p> <p>At least three great earthquakes occurred in the New Madrid seismic <span class="hlt">zone</span> in 1811 and 1812. Estimates of present-day strain rates suggest that such <span class="hlt">events</span> may have a repeat time of 1000 years or less. Paleoseismological data also indicate that earthquakes large enough to cause soil liquefaction have occurred several times in the past 5000 years. However, pervasive crustal deformation expected from such a high frequency of large earthquakes is not observed. This suggests that the seismic <span class="hlt">zone</span> is a young feature, possibly as young as several tens of thousands of years old and no more than a few million years old.At least three great earthquakes occurred in the New Madrid seismic <span class="hlt">zone</span> in 1811 and 1812. Estimates of present-day strain rates suggest that such <span class="hlt">events</span> may have a repeat time of 1000 years or less. Paleoseismological data also indicate that earthquakes large enough to cause soil liquefaction have occurred several times in the past 5000 years. However, pervasive crustal deformation expected from such a high frequency of large earthquakes is not observed. This suggests that the seismic <span class="hlt">zone</span> is a young feature, possibly as young as several tens of thousands of years old and no more than a few million years old.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2007GPC....55..155K','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2007GPC....55..155K"><span>Biostratigraphy and <span class="hlt">event</span> stratigraphy in Iran around the Permian Triassic Boundary (PTB): Implications for the causes of the PTB biotic crisis</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Kozur, H. W.</p> <p>2007-01-01</p> <p>The conodont succession and stratigraphic <span class="hlt">events</span> around the Permian-Triassic boundary (PTB) have been investigated in detail in the open sea deposits of Iran (Abadeh and Shahreza in central Iran, and Jolfa and Zal in northwestern Iran). This investigation produced a very detailed conodont zonation from the Clarkina nodosa <span class="hlt">Zone</span> up to the Isarcicella isarcica <span class="hlt">Zone</span>. All significant <span class="hlt">events</span> have been accurately located and dated within this zonation, and the duration of most of these conodont <span class="hlt">zones</span> has been calculated by cross-correlation with continental lake deposits that display obvious Milankovitch cyclicity. The unusually short duration of all conodont <span class="hlt">zones</span> in the interval from the C. nodosa up to the Hindeodus parvus <span class="hlt">Zone</span> indicates that there was persistent high ecological stress during this time interval. Most of the conodont <span class="hlt">zones</span> can be accurately correlated with South China. In the interval from the C. hauschkei <span class="hlt">Zone</span> to the H. parvus <span class="hlt">Zone</span>, even correlation with the Arctic is possible. Within three thin stratigraphic intervals, the Changhsingian (Dorashamian) warm water conodont fauna of the C. subcarinata lineage is replaced by a cool water fauna with small H. typicalis, rare Merrillina sp., and cool water Clarkina that have very widely spaced denticles. The uppermost cool water fauna horizon comprises the lower C. zhangi <span class="hlt">Zone</span> and can be accurately correlated with continental beds by recognition of a short reversed magnetozone below the long uppermost Permian-lowermost Triassic normal magnetozone. In Iran and Transcaucasia, this short reversed <span class="hlt">zone</span> comprises the upper C. changxingensis- C. deflecta <span class="hlt">Zone</span> and most of the C. zhangi <span class="hlt">Zone</span>. Its top lies 50 cm below the top of the Paratirolites Limestone (s.s.) in the Dorasham 2 section, which is at the beginning of the upper quarter of the C. zhangi <span class="hlt">Zone</span>. In the Germanic Basin, this short palaeomagnetic interval comprises the lower and the basal part of the upper Fulda Formation. On the Russian Platform, the</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2001AGUFM.T52E..04D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2001AGUFM.T52E..04D"><span>Characteristics of the Central Costa Rican Seismogenic <span class="hlt">Zone</span> Determined from Microseismicity</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>DeShon, H. R.; Schwartz, S. Y.; Bilek, S. L.; Dorman, L. M.; Protti, M.; Gonzalez, V.</p> <p>2001-12-01</p> <p>Large or great subduction <span class="hlt">zone</span> thrust earthquakes commonly nucleate within the seismogenic <span class="hlt">zone</span>, a region of unstable slip on or near the converging plate interface. A better understanding of the mechanical, thermal and hydrothermal processes controlling seismic behavior in these regions requires accurate earthquake locations. Using arrival time data from an onland and offshore local seismic array and advanced 3D absolute and relative earthquake location techniques, we locate interplate seismic activity northwest of the Osa Peninsula, Costa Rica. We present high resolution locations of ~600 aftershocks of the 8/20/1999 Mw=6.9 underthrusting earthquake recorded by our local network between September and December 1999. We have developed a 3D velocity model based on published refraction lines and located <span class="hlt">events</span> within a subducting slab geometry using QUAKE3D, a finite-differences based grid-searching algorithm (Nelson & Vidale, 1990). These absolute locations are input into HYPODD, a location program that uses P and S wave arrival time differences from nearby <span class="hlt">events</span> and solves for the best relative locations (Waldhauser & Ellsworth, 2000). The pattern of relative earthquake locations is tied to an absolute reference using the absolute positions of the best-located earthquakes in the entire population. By using these programs in parallel, we minimize location errors, retain the aftershock pattern and provide the best absolute locations within a complex subduction geometry. We use the resulting seismicity pattern to determine characteristics of the seismogenic <span class="hlt">zone</span> including geometry and up- and down-dip limits. These are compared with thermal models of the Middle America subduction <span class="hlt">zone</span>, structures of the upper and lower plates, and characteristics of the Nankai seismogenic <span class="hlt">zone</span>.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li class="active"><span>24</span></li> <li><a href="#" onclick='return showDiv("page_25");'>25</a></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_24 --> <div id="page_25" class="hiddenDiv"> <div class="row"> <div class="col-sm-12"> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li class="active"><span>25</span></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div> </div> <div class="row"> <div class="col-sm-12"> <ol class="result-class" start="481"> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2016EGUGA..1810577G','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2016EGUGA..1810577G"><span>Effect of climate, intra and inter-<span class="hlt">annual</span> variability, on nutrients emission (C,N, P) in stream water: lessons from an agricultural long term observatory of the temperate <span class="hlt">zone</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Gascuel-Odoux, Chantal; Remi, Dupas; Patrick, Durand; Ophélie, Fovet; Gerard, Gruau; Anne, Jaffrezic; Guillaume, Humbert; Philippe, Merot; Gu, Sen</p> <p>2016-04-01</p> <p>Agriculture greatly contributes to modify C, N and P cycles, particularly in animal breeding regions due to high inputs. Climatic conditions, intra and inter-<span class="hlt">annual</span> variabilities, modify nutrient stream water emissions, acting in time on transfer and transformation, accumulation and mobilization processes, connecting and disconnecting in time different compartments (soil, riparian areas, groundwater). In agricultural catchments, nutrient perturbations are dominated by agricultural land use, and decoupling human activities and climate effects is far from easy. Climate change generally appears as a secondary driver compared to land use. If studied, generally only one nutrient is considered. Only long term, high frequency and multiple element data series can decouple these two drivers. The Kervidy-Naizin watershed belongs to the AgrHyS environmental research observatory (http://www6.inra.fr/ore_agrhys_eng), itself included in RBV (French catchment network of the CZO). On this catchment, 6 years of daily data on DOC, NO3, SRP, TP concentrations allow us to analyze the effect of seasonal and inter-<span class="hlt">annual</span> climatic variabilities on water quality (C, N, P). Different papers have been published on the effect of climate on nitrate (Molenat et al, 2008), SRP and TP (Dupas et al, 2015) and DOC (Humbert et al, 2015). We will present first results comparing the effect of climate on these three major solute forms of C, N and P. While C and P dynamics are very close and controlled by fluctuation of water table downslope, i.e. in riparian areas, mobilizing C and P in time, nitrate dynamics is controlled by GW dynamics upslope acting as the major N reservoir. As example, the dryness conditions in summer appears a key factor of the C and P emissions in autumn. All the three solute forms interact when anoxic conditions are observed in riparian <span class="hlt">zones</span>. These basic processes explain how climatic variability can influence and explain interactions between C, N and P emissions in stream</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4331181','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=4331181"><span>Association of stressful life <span class="hlt">events</span> with accelerated bone loss in older men: the Osteoporotic Fractures in Men (MrOS) Study</span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Fink, Howard A.; Kuskowski, Michael A.; Cauley, Jane A.; Taylor, Brent C.; Schousboe, John T.; Cawthon, Peggy M.; Ensrud, Kristine E.</p> <p>2015-01-01</p> <p>Purpose/Introduction Prior studies suggest that stressful life <span class="hlt">events</span> may increase adverse health outcomes, including falls and possibly fractures. The current study builds on these findings and examines whether stressful life <span class="hlt">events</span> are associated with increased bone loss. Methods 4388 men aged ≥65 years in the Osteoporotic Fractures in Men study completed total hip bone mineral density (BMD) measures at baseline and visit 2, approximately 4.6 years later, and self-reported stressful life <span class="hlt">events</span> data mid-way between baseline and visit 2, and at visit 2. We used linear regression to model the association of stressful life <span class="hlt">events</span> with concurrent <span class="hlt">annualized</span> total hip BMD loss, and log binomial regression or Poisson regression to model risk of concurrent accelerated BMD loss (>1 SD more than mean <span class="hlt">annualized</span> change). Results 75.3% of men reported ≥1 type of stressful life <span class="hlt">event</span>, including 43.3% with ≥2 types of stressful life <span class="hlt">events</span>. Mean <span class="hlt">annualized</span> BMD loss was −0.36% (SD 0.88) and 13.9% of men were categorized with accelerated BMD loss (about 5.7% or more total loss). Rate of <span class="hlt">annualized</span> BMD loss increased with the number of types of stressful life <span class="hlt">events</span> after adjustment for age (p<0.001), but not after multivariable adjustment (p=0.07). Multivariable-adjusted risk of accelerated BMD loss increased with the number of types of stressful life <span class="hlt">events</span> (RR, 1.10 [95% CI, 1.04–1.16]) per increase of 1 type of stressful life <span class="hlt">event</span>). Fracture risk was not significantly different between stressful life <span class="hlt">event</span>-accelerated bone loss subgroups (p=0.08). Conclusions In these older men, stressful life <span class="hlt">events</span> were associated with a small, dose-related increase in risk of concurrent accelerated hip bone loss. Low frequency of fractures limited assessment of whether rapid bone loss mediates any association of stressful life <span class="hlt">events</span> with incident fractures. Future studies are needed to confirm these findings and to investigate the mechanism that may underlie this association</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-12-27/pdf/2011-33032.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-12-27/pdf/2011-33032.pdf"><span>76 FR 80850 - Special Local Regulations and Safety <span class="hlt">Zones</span>; Recurring <span class="hlt">Events</span> in Northern New England</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-12-27</p> <p>...[deg]31'29'' W. 43[deg]52'09'' N, 069[deg]31'56'' W. 8.6 Multiple Sclerosis Regatta......... <span class="hlt">Event</span> Type: Regatta and Sailboat Race. Sponsor: Maine Chapter, Multiple Sclerosis Society. Date: A one day <span class="hlt">event</span> on..., 070[deg]13'51'' W. 8.7 Multiple Sclerosis Harborfest <span class="hlt">Event</span> Type: Power Boat Tugboat Race. Race...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/16915286','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/16915286"><span>Resonant slow fault slip in subduction <span class="hlt">zones</span> forced by climatic load stress.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lowry, Anthony R</p> <p>2006-08-17</p> <p>Global Positioning System (GPS) measurements at subduction plate boundaries often record fault movements similar to earthquakes but much slower, occurring over timescales of approximately 1 week to approximately 1 year. These 'slow slip <span class="hlt">events</span>' have been observed in Japan, Cascadia, Mexico, Alaska and New Zealand. The phenomenon is poorly understood, but several observations hint at the processes underlying slow slip. Although slip itself is silent, seismic instruments often record coincident low-amplitude tremor in a narrow (1-5 cycles per second) frequency range. Also, modelling of GPS data and estimates of tremor location indicate that slip focuses near the transition from unstable ('stick-slip') to stable friction at the deep limit of the earthquake-producing seismogenic <span class="hlt">zone</span>. Perhaps most intriguingly, slow slip is periodic at several locations, with recurrence varying from 6 to 18 months depending on which subduction <span class="hlt">zone</span> (or even segment) is examined. Here I show that such periodic slow fault slip may be a resonant response to climate-driven stress perturbations. Fault slip resonance helps to explain why slip <span class="hlt">events</span> are periodic, why periods differ from place to place, and why slip focuses near the base of the seismogenic <span class="hlt">zone</span>. Resonant slip should initiate within the rupture <span class="hlt">zone</span> of future great earthquakes, suggesting that slow slip may illuminate fault properties that control earthquake slip.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3788588','PMC'); return false;" href="https://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=3788588"><span>Root Apex Transition <span class="hlt">Zone</span> As Oscillatory <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pmc">PubMed Central</a></p> <p>Baluška, František; Mancuso, Stefano</p> <p>2013-01-01</p> <p>Root apex of higher plants shows very high sensitivity to environmental stimuli. The root cap acts as the most prominent plant sensory organ; sensing diverse physical parameters such as gravity, light, humidity, oxygen, and critical inorganic nutrients. However, the motoric responses to these stimuli are accomplished in the elongation region. This spatial discrepancy was solved when we have discovered and characterized the transition <span class="hlt">zone</span> which is interpolated between the apical meristem and the subapical elongation <span class="hlt">zone</span>. Cells of this <span class="hlt">zone</span> are very active in the cytoskeletal rearrangements, endocytosis and endocytic vesicle recycling, as well as in electric activities. Here we discuss the oscillatory nature of the transition <span class="hlt">zone</span> which, together with several other features of this <span class="hlt">zone</span>, suggest that it acts as some kind of command center. In accordance with the early proposal of Charles and Francis Darwin, cells of this root <span class="hlt">zone</span> receive sensory information from the root cap and instruct the motoric responses of cells in the elongation <span class="hlt">zone</span>. PMID:24106493</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2004AGUFM.S42B..08N','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2004AGUFM.S42B..08N"><span>Nonvolcanic Deep Tremors in the Transform Plate Bounding San Andreas Fault <span class="hlt">Zone</span></span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Nadeau, R. M.; Dolenc, D.</p> <p>2004-12-01</p> <p>Recently, deep ( ˜ 20 to 40 km) nonvolcanic tremor activity has been observed on convergent plate boundaries in Japan and in the Cascadia region of North America (Obara, 2002; Rodgers and Dragert, 2003; Szeliga et al., 2004). Because of the abundance of available fluids from subduction processes in these convergent <span class="hlt">zones</span>, fluids are believed to play an important role in the generation of the tremor activity. The transient rates of tremor activity in these regions are also observed to correlate either with the occurrence of larger earthquakes (Obara, 2002) or with geodetically determined transient creep <span class="hlt">events</span> that release large amounts of strain energy deep beneath the locked Cascadia megathrust (M.M. Miller et al., 2002; Rodgers and Dragert, 2003; Szeliga et al., 2004). These associations suggest that nonvolcanic tremor activity may participate in a fundamental mode of deep moment release and in the triggering of large subduction <span class="hlt">zone</span> <span class="hlt">events</span> (Rodgers and Dragert, 2003). We report the discovery of deep ( ˜ 20 to 45 km) nonvolcanic tremor activity on the transform plate bounding San Andreas Fault (SAF) in central California where, in contrast to subduction <span class="hlt">zones</span>, long-term deformation directions are horizontal and fluid availability from subduction <span class="hlt">zone</span> processes is absent. The source region of the SAF tremors lies beneath the epicentral region of the great 1857 magnitude (M) ˜ 8, Fort Tejon earthquake whose rupture <span class="hlt">zone</span> is currently locked (Sieh, 1978). Activity rate transients of the tremors occurring since early 2001 also correlate with seismicity rate variations above the tremor source region.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2017AGUFM.A23D2393D','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2017AGUFM.A23D2393D"><span>Do Atmospheric Rivers explain the extreme precipitation <span class="hlt">events</span> over East Asia?</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Dairaku, K.; Nayak, S.</p> <p>2017-12-01</p> <p>Extreme precipitation <span class="hlt">events</span> are now of serious concern due to their damaging societal impacts over last few decades. Thus, climate indices are widely used to identify and quantify variability and changes in particular aspects of the climate system, especially when considering extremes. In our study, we focus on few climate indices of <span class="hlt">annual</span> precipitation extremes for the period 1979-2013 over East Asia to discuss some straightforward information and interpretation of certain aspects of extreme precipitation <span class="hlt">events</span> that occur over the region. To do so, we first discuss different percentiles of precipitation and maximum length of wet spell with different thresholds from a regional climate model (NRAMS) simulation at 20km. Results indicate that the 99 percentile of precipitation <span class="hlt">events</span> correspond to about 80mm/d over few regions of East Asia during 1979-2013 and maximum length of wet spell with minimum 20mm precipitation corresponds to about 10days (Figure 1). We then linked the extreme precipitation <span class="hlt">events</span> with the intense moisture transport <span class="hlt">events</span> associated with atmospheric rivers (ARs). The ARs are identified by computing the vertically integrated horizontal water vapor transport (IVT) between 1000hpa and 300hpa with IVT ≥ 250 kg/m/s and 2000 km minimum long. With this threshold and condition (set by previous research), our results indicate that some extreme propitiation <span class="hlt">events</span> are associated with some ARs over East Asia, while some <span class="hlt">events</span> are not associated with any ARs. Similarly, some ARs are associated with some extreme precipitation <span class="hlt">events</span>, while some ARs are not associated with any <span class="hlt">events</span>. Since the ARs are sensitive to the threshold and condition depending on region, so we will analyze the characteristics of ARs (frequency, duration, and <span class="hlt">annual</span> variability) with different thresholds and discuss their relationship with extreme precipitation <span class="hlt">events</span> over East Asia.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2011-07-01/pdf/2011-16618.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2011-07-01/pdf/2011-16618.pdf"><span>76 FR 38570 - Safety <span class="hlt">Zone</span>; Fourth of July Fireworks <span class="hlt">Event</span>, Pagan River, Smithfield, VA</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2011-07-01</p> <p>.... ACTION: Temporary final rule. SUMMARY: The Coast Guard is establishing a 420-foot radius safety <span class="hlt">zone</span> on..., vessel traffic will be temporarily restricted within 420 feet of the fireworks launch site. Discussion of... the area bounded by a 420-foot radius circle centered on position 36[deg]59'18'' N/076[deg]37'45'' W...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2010-06-17/pdf/2010-14626.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2010-06-17/pdf/2010-14626.pdf"><span>75 FR 34372 - Safety <span class="hlt">Zone</span>; Fourth of July Fireworks <span class="hlt">Event</span>, Pagan River, Smithfield, VA</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2010-06-17</p> <p>.... ACTION: Temporary final rule. SUMMARY: The Coast Guard is establishing a 420-foot radius safety <span class="hlt">zone</span> on... other debris, vessel traffic will be temporarily restricted within 420 feet of the fireworks launch site... within the area bounded by a 420-foot radius circle centered on position 36[deg]59'18'' N/076[deg]37'45...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://files.eric.ed.gov/fulltext/ED438819.pdf','ERIC'); return false;" href="http://files.eric.ed.gov/fulltext/ED438819.pdf"><span>OCLC <span class="hlt">Annual</span> Report 1998/99. A Great Time for Libraries!</span></a></p> <p><a target="_blank" href="http://www.eric.ed.gov/ERICWebPortal/search/extended.jsp?_pageLabel=advanced">ERIC Educational Resources Information Center</a></p> <p>OCLC Online Computer Library Center, Inc., Dublin, OH.</p> <p></p> <p>Beginning this <span class="hlt">annual</span> report is a letter to OCLC members from OCLC President and Chief Executive Jay Jordan. The report contains the following sections: (1) program and financial highlights; (2) the year in review, including membership <span class="hlt">events</span>, online services, strategic alliances, Forest Press, preservation resources, research, and the OCLC…</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=335670&Lab=NRMRL&keyword=NASA&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50','EPA-EIMS'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=335670&Lab=NRMRL&keyword=NASA&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50"><span>Air Quality Side <span class="hlt">Event</span> Proposal November 2016 GEO XIII Plenary in St. Petersburg, Russia</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>The Group on Earth Observations (GEO), which EPA has participated in since 2003, has put out a call for Side <span class="hlt">Events</span> for its thirteenth <span class="hlt">annual</span> international Plenary Meeting which is in St. Petersburg, Russia this year during November, 2016. EPA has put on Side <span class="hlt">Events</span> on Air Quali...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://pubs.er.usgs.gov/publication/70032008','USGSPUBS'); return false;" href="https://pubs.er.usgs.gov/publication/70032008"><span>Artificial recharge through a thick, heterogeneous unsaturated <span class="hlt">zone</span></span></a></p> <p><a target="_blank" href="http://pubs.er.usgs.gov/pubs/index.jsp?view=adv">USGS Publications Warehouse</a></p> <p>Izbicki, J.A.; Flint, A.L.; Stamos, C.L.</p> <p>2008-01-01</p> <p>Thick, heterogeneous unsaturated <span class="hlt">zones</span> away from large streams in desert areas have not previously been considered suitable for artificial recharge from ponds. To test the potential for recharge in these settings, 1.3 ?? 10 6 m3 of water was infiltrated through a 0.36-ha pond along Oro Grande Wash near Victorville, California, between October 2002 and January 2006. The pond overlies a regional pumping depression 117 m below land surface and is located where thickness and permeability of unsaturated deposits allowed infiltration and saturated alluvial deposits were sufficiently permeable to allow recovery of water. Because large changes in water levels caused by nearby pumping would obscure arrival of water at the water table, downward movement of water was measured using sensors in the unsaturated <span class="hlt">zone</span>. The downward rate of water movement was initially as high as 6 m/d and decreased with depth to 0.07 m/d; the initial time to reach the water table was 3 years. After the unsaturated <span class="hlt">zone</span> was wetted, water reached the water table in 1 year. Soluble salts and nitrate moved readily with the infiltrated water, whereas arsenic and chromium were less mobile. Numerical simulations done using the computer program TOUGH2 duplicated the downward rate of water movement, accumulation of water on perched <span class="hlt">zones</span>, and its arrival at the water table. Assuming 10 ?? 10 6 m3 of recharge <span class="hlt">annually</span> for 20 years, a regional ground water flow model predicted water level rises of 30 m beneath the ponds, and rises exceeding 3 m in most wells serving the nearby urban area.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2010EGUGA..1215693O','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2010EGUGA..1215693O"><span>Chile's seismogenic coupling <span class="hlt">zones</span> - geophysical and neotectonic observations from the South American subduction <span class="hlt">zone</span> prior to the Maule 2010 earthquake</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Oncken With Tipteq, Onno; Ipoc Research Groups</p> <p>2010-05-01</p> <p>Accumulation of deformation at convergent plate margins is recently identified to be highly discontinuous and transient in nature: silent slip <span class="hlt">events</span>, non-volcanic tremors, afterslip, fault coupling and complex response patterns of the upper plate during a single <span class="hlt">event</span> as well as across several seismic cycles have all been observed in various settings and combinations. Segments of convergent plate margins with high recurrence rates and at different stages of the rupture cycle like the Chilean margin offer an exceptional opportunity to study these features and their interaction resolving behaviour during the seismic cycle and over repeated cycles. A past (TIPTEQ) and an active international initiative (IPOC; Integrated Plate Boundary Observatory Chile) address these goals with research groups from IPG Paris, Seismological Survey of Chile, Free University Berlin, Potsdam University, Hamburg University, IFM-GEOMAR Kiel, and GFZ Potsdam employing an integrated plate boundary observatory and associated projects. We focus on the south Central Chilean convergent margin and the North Chilean margin as natural laboratories embracing the recent Maule 2010 megathrust <span class="hlt">event</span>. Here, major recent seismic <span class="hlt">events</span> have occurred (south Central Chile: 1960, Mw = 9.5; 2010, Mw = 8.8; North Chile: 1995, Mw = 8; 2001, Mw = 8.7; 2007, Mw: 7.8) or are expected in the very near future (Iquique, last ruptured 1877, Mw = 8.8) allowing observation at critical time windows of the seismic cycle. Seismic imaging and seismological data have allowed us to relocate major rupture hypocentres and to locate the geometry of the locked <span class="hlt">zone</span> and the degree of locking in both areas. The reflection seismic data exhibit well defined changes of reflectivity and Vp/Vs ratio along the plate interface that can be correlated with different parts of the coupling <span class="hlt">zone</span> as well as with changes during the seismic cycle. Observations suggest an important role of the hydraulic system, an inference that is strongly</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/1394465','SCIGOV-STC'); return false;" href="https://www.osti.gov/servlets/purl/1394465"><span><span class="hlt">Annual</span> and Seasonal Global Variation in Total Ozone and Layer-Mean Ozone, 1958-1987 (1991)</span></a></p> <p><a target="_blank" href="http://www.osti.gov/search">DOE Office of Scientific and Technical Information (OSTI.GOV)</a></p> <p>Angell, J. K.; Korshover, J.; Planet, W. G.</p> <p></p> <p>For 1958 through 1987, this data base presents total ozone variations and layer mean ozone variations expressed as percent deviations from the 1958 to 1977 mean. The total ozone variations were derived from mean monthly ozone values published in Ozone Data for the World by the Atmospheric Environment Service in cooperation with the World Meteorological Organization. The layer mean ozone variations are derived from ozonesonde and Umkehr observations. The data records include year, seasonal and <span class="hlt">annual</span> total ozone variations, and seasonal and <span class="hlt">annual</span> layer mean ozone variations. The total ozone data are for four regions (Soviet Union, Europe, North America,more » and Asia); five climatic <span class="hlt">zones</span> (north and south polar, north and south temperate, and tropical); both hemispheres; and the world. Layer mean ozone data are for four climatic <span class="hlt">zones</span> (north and south temperate and north and south polar) and for the stratosphere, troposphere, and tropopause layers. The data are in two files [seasonal and year-average total ozone (13.4 kB) and layer mean ozone variations (24.2 kB)].« less</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/19303128','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/19303128"><span>Assessment of <span class="hlt">annual</span> pollutant loads in combined sewers from continuous turbidity measurements: sensitivity to calibration data.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Lacour, C; Joannis, C; Chebbo, G</p> <p>2009-05-01</p> <p>This article presents a methodology for assessing <span class="hlt">annual</span> wet weather Suspended Solids (SS) and Chemical Oxygen Demand (COD) loads in combined sewers, along with the associated uncertainties from continuous turbidity measurements. The proposed method is applied to data from various urban catchments in the cities of Paris and Nantes. The focus here concerns the impact of the number of rain <span class="hlt">events</span> sampled for calibration (i.e. through establishing linear SS/turbidity or COD/turbidity relationships) on the uncertainty of <span class="hlt">annual</span> pollutant load assessments. Two calculation methods are investigated, both of which rely on Monte Carlo simulations: random assignment of <span class="hlt">event</span>-specific calibration relationships to each individual rain <span class="hlt">event</span>, and the use of an overall relationship built from the entire available data set. Since results indicate a fairly low inter-<span class="hlt">event</span> variability for calibration relationship parameters, an accurate assessment of pollutant loads can be derived, even when fewer than 10 <span class="hlt">events</span> are sampled for calibration purposes. For operational applications, these results suggest that turbidity could provide a more precise evaluation of pollutant loads at lower cost than typical sampling methods.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.gpo.gov/fdsys/pkg/FR-2012-06-11/pdf/2012-14126.pdf','FEDREG'); return false;" href="https://www.gpo.gov/fdsys/pkg/FR-2012-06-11/pdf/2012-14126.pdf"><span>77 FR 34285 - Safety <span class="hlt">Zone</span>; 2012 Ironman U.S. Championship Swim, Hudson River, Fort Lee, NJ</span></a></p> <p><a target="_blank" href="http://www.gpo.gov/fdsys/browse/collection.action?collectionCode=FR">Federal Register 2010, 2011, 2012, 2013, 2014</a></p> <p></p> <p>2012-06-11</p> <p>...-AA00 Safety <span class="hlt">Zone</span>; 2012 Ironman U.S. Championship Swim, Hudson River, Fort Lee, NJ AGENCY: Coast Guard... safety <span class="hlt">zone</span> on the navigable waters of the Hudson River in the vicinity of Englewood Cliffs and Fort Lee... the Hudson River in the vicinity of Englewood Cliffs and Fort Lee, New Jersey. This swim <span class="hlt">event</span> poses...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.osti.gov/servlets/purl/864478','DOE-PATENT-XML'); return false;" href="https://www.osti.gov/servlets/purl/864478"><span><span class="hlt">Zone</span> separator for multiple <span class="hlt">zone</span> vessels</span></a></p> <p><a target="_blank" href="http://www.osti.gov/doepatents">DOEpatents</a></p> <p>Jones, John B.</p> <p>1983-02-01</p> <p>A solids-gas contact vessel, having two vertically disposed distinct reaction <span class="hlt">zones</span>, includes a dynamic seal passing solids from an upper to a lower <span class="hlt">zone</span> and maintaining a gas seal against the transfer of the separate treating gases from one <span class="hlt">zone</span> to the other, and including a stream of sealing fluid at the seal.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=338581&Lab=NHEERL&keyword=biomass&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50','EPA-EIMS'); return false;" href="https://cfpub.epa.gov/si/si_public_record_report.cfm?dirEntryId=338581&Lab=NHEERL&keyword=biomass&actType=&TIMSType=+&TIMSSubTypeID=&DEID=&epaNumber=&ntisID=&archiveStatus=Both&ombCat=Any&dateBeginCreated=&dateEndCreated=&dateBeginPublishedPresented=&dateEndPublishedPresented=&dateBeginUpdated=&dateEndUpdated=&dateBeginCompleted=&dateEndCompleted=&personID=&role=Any&journalID=&publisherID=&sortBy=revisionDate&count=50"><span>Effects of microtopographic variation and macroalgal cover on morphometrics and survival of the <span class="hlt">annual</span> form of eelgrass (Zostera marina)</span></a></p> <p><a target="_blank" href="http://oaspub.epa.gov/eims/query.page">EPA Science Inventory</a></p> <p></p> <p></p> <p>A disjunct population of the <span class="hlt">annual</span> form of the seagrass Zostera marina that occurred in the upper intertidal <span class="hlt">zone</span> of Yaquina Bay, Oregon was sampled to determine whether there were differences in recruitment, growth, survivorship and morphology associated with microtopographic l...</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('https://www.ncbi.nlm.nih.gov/pubmed/29540688','PUBMED'); return false;" href="https://www.ncbi.nlm.nih.gov/pubmed/29540688"><span>Shallow very-low-frequency earthquakes accompany slow slip <span class="hlt">events</span> in the Nankai subduction <span class="hlt">zone</span>.</span></a></p> <p><a target="_blank" href="https://www.ncbi.nlm.nih.gov/entrez/query.fcgi?DB=pubmed">PubMed</a></p> <p>Nakano, Masaru; Hori, Takane; Araki, Eiichiro; Kodaira, Shuichi; Ide, Satoshi</p> <p>2018-03-14</p> <p>Recent studies of slow earthquakes along plate boundaries have shown that tectonic tremor, low-frequency earthquakes, very-low-frequency <span class="hlt">events</span> (VLFEs), and slow-slip <span class="hlt">events</span> (SSEs) often accompany each other and appear to share common source faults. However, the source processes of slow <span class="hlt">events</span> occurring in the shallow part of plate boundaries are not well known because seismic observations have been limited to land-based stations, which offer poor resolution beneath offshore plate boundaries. Here we use data obtained from seafloor observation networks in the Nankai trough, southwest of Japan, to investigate shallow VLFEs in detail. Coincident with the VLFE activity, signals indicative of shallow SSEs were detected by geodetic observations at seafloor borehole observatories in the same region. We find that the shallow VLFEs and SSEs share common source regions and almost identical time histories of moment release. We conclude that these slow <span class="hlt">events</span> arise from the same fault slip and that VLFEs represent relatively high-frequency fluctuations of slip during SSEs.</p> </li> <li> <p><a target="_blank" onclick="trackOutboundLink('http://adsabs.harvard.edu/abs/2018GeoRL..45.2761B','NASAADS'); return false;" href="http://adsabs.harvard.edu/abs/2018GeoRL..45.2761B"><span>Defining Flood <span class="hlt">Zone</span> Transitions in Low-Gradient Coastal Regions</span></a></p> <p><a target="_blank" href="http://adsabs.harvard.edu/abstract_service.html">NASA Astrophysics Data System (ADS)</a></p> <p>Bilskie, M. V.; Hagen, S. C.</p> <p>2018-03-01</p> <p>Worldwide, coastal, and deltaic communities are susceptible to flooding from the individual and combined effects of rainfall excess and astronomic tide and storm surge inundation. Such flood <span class="hlt">events</span> are a present (and future) cause of concern as observed from recent storms such as the 2016 Louisiana flood and Hurricanes Harvey, Irma, and Maria. To assess flood risk across coastal landscapes, it is advantageous to first delineate flood transition <span class="hlt">zones</span>, which we define as areas susceptible to hydrologic and coastal flooding and their collective interaction. We utilize numerical simulations combining rainfall excess and storm surge for the 2016 Louisiana flood to describe a flood transition <span class="hlt">zone</span> for southeastern Louisiana. We show that the interaction of rainfall excess with coastal surge is nonlinear and less than the superposition of their individual components. Our analysis provides a foundation to define flooding <span class="hlt">zones</span> across coastal landscapes throughout the world to support flood risk assessments.</p> </li> </ol> <div class="pull-right"> <ul class="pagination"> <li><a href="#" onclick='return showDiv("page_1");'>«</a></li> <li><a href="#" onclick='return showDiv("page_21");'>21</a></li> <li><a href="#" onclick='return showDiv("page_22");'>22</a></li> <li><a href="#" onclick='return showDiv("page_23");'>23</a></li> <li><a href="#" onclick='return showDiv("page_24");'>24</a></li> <li class="active"><span>25</span></li> <li><a href="#" onclick='return showDiv("page_25");'>»</a></li> </ul> </div> </div><!-- col-sm-12 --> </div><!-- row --> </div><!-- page_25 --> <div class="footer-extlink text-muted" style="margin-bottom:1rem; text-align:center;">Some links on this page may take you to non-federal websites. Their policies may differ from this site.</div> </div><!-- container --> <footer><a id="backToTop" href="#top"> </a><nav><a id="backToTop" href="#top"> </a><ul class="links"><a id="backToTop" href="#top"> </a><li><a id="backToTop" href="#top"></a><a href="/sitemap.html">Site Map</a></li> <li><a href="/members/index.html">Members Only</a></li> <li><a href="/website-policies.html">Website Policies</a></li> <li><a href="https://doe.responsibledisclosure.com/hc/en-us" target="_blank">Vulnerability Disclosure Program</a></li> <li><a href="/contact.html">Contact Us</a></li> </ul> <div class="small">Science.gov is maintained by the U.S. Department of Energy's <a href="https://www.osti.gov/" target="_blank">Office of Scientific and Technical Information</a>, in partnership with <a href="https://www.cendi.gov/" target="_blank">CENDI</a>.</div> </nav> </footer> <script type="text/javascript"><!-- // var lastDiv = ""; function showDiv(divName) { // hide last div if (lastDiv) { document.getElementById(lastDiv).className = "hiddenDiv"; } //if value of the box is not nothing and an object with that name exists, then change the class if (divName && document.getElementById(divName)) { document.getElementById(divName).className = "visibleDiv"; lastDiv = divName; } } //--> </script> <script> /** * Function that tracks a click on an outbound link in Google Analytics. * This function takes a valid URL string as an argument, and uses that URL string * as the event label. */ var trackOutboundLink = function(url,collectionCode) { try { h = window.open(url); setTimeout(function() { ga('send', 'event', 'topic-page-click-through', collectionCode, url); }, 1000); } catch(err){} }; </script> <!-- Google Analytics --> <script> (function(i,s,o,g,r,a,m){i['GoogleAnalyticsObject']=r;i[r]=i[r]||function(){ (i[r].q=i[r].q||[]).push(arguments)},i[r].l=1*new Date();a=s.createElement(o), m=s.getElementsByTagName(o)[0];a.async=1;a.src=g;m.parentNode.insertBefore(a,m) })(window,document,'script','//www.google-analytics.com/analytics.js','ga'); ga('create', 'UA-1122789-34', 'auto'); ga('send', 'pageview'); </script> <!-- End Google Analytics --> <script> showDiv('page_1') </script> </body> </html>