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1

Taxonomy, biogeography and ecology of quaternary Benthic Ostracoda (Crustacea) from circumpolar deep water of the Emerald Basin (Southern Ocean) and the S Tasman Rise (Tasman Sea)  

Microsoft Academic Search

Benthic Ostracoda were recovered from 19 box core samples collected during the cruise SO 136 of the German R\\/VSONNE in the Tasman Sea and Southern Ocean (SW Pacific sector). The detailed taxonomic study of more than 10.000 specimens recovered\\u000a from eleven box-corer samples from circumpolar deep water of the Emerald Basin (Southern Ocean) and the S Tasman Rise (Tasman\\u000a Sea)

Ilaria Mazzini

2005-01-01

2

Deep currents of the northern Tasman Sea Basin  

NASA Astrophysics Data System (ADS)

Off the southeast Australian cost in the Tasman Basin, north of 40°S, the deeper structure obtained from hydrological data is highly correlated with the surface flow, especially in the region east of Sydney where the East Australian Current forms southwards meanders that often break off to form large, warm-core rings. This indicates that the East Australian Current and its warm-core rings have a dominant influence on the baroclinic flow down to abyssal depths. Typical current shears below 2000 m are estimated to be of order 4 cm s-1 km-1. Further north, between 30 and 32.5°S, the correlation between deep and shallow structure is of similar magnitude and there is a definite correlation between parameters of the deep flow and distance offshore. It is concluded that the correlation is due to an east-west tilt of the surface of no motion. Still further north, no significant correlations exist between the deep structure and either distance offshore or shallow structure parameters. No evidence has been found for a swift, narrow, western boundary undercurrent in the Tasman Sea north of 40°S.

Mulhearn, P. J.

1983-11-01

3

Deep upper-mantle melting beneath the Tasman and Coral Seas detected with multiple ScS reverberations  

E-print Network

Elsevier B.V. All rights reserved. Keywords: mantle; transition zone; discontinuities; partial meltingDeep upper-mantle melting beneath the Tasman and Coral Seas detected with multiple Sc Multiple ScS reverberations are used to search for mantle reflectors beneath the Tasman and Coral Seas

Courtier, Anna M.

4

An avenue of eddies: Quantifying the biophysical properties of mesoscale eddies in the Tasman Sea  

E-print Network

western boundary current that breaks down into a complicated field of mesoscale eddies almost immediately Tasman Sea. We find that Eddy Avenue cyclonic and anti- cyclonic eddies have more strongly differentiated from Coral Sea water depressing chl. a concentrations, and for coastal cyclonic eddies due

Oke, Peter

5

Geology and geochemistry of Gannet (Karewa) Island, Tasman Sea: A rift?related nephelinitic tuff ring  

Microsoft Academic Search

Gannet (Karewa) Island is a small (0.06 km) island situated in the Tasman Sea, northwest of Kawhia Harbour, western North Island, New Zealand. It consists of well indurated, palagonitic tuff and lapilli tuff with subordinate scoriaceous basalt bombs and blocks (Karewa Volcanic Formation) which are considered to represent the eroded remnants of a tuff ring. Evidence for this includes such

R. M. Briggs; M. D. Rosenberg; P. J. de Lange; T. Itaya; P. R. King; R. C. Price

1997-01-01

6

South Tasman Sea alkenone palaeothermometry over the last four glacial\\/interglacial cycles  

Microsoft Academic Search

Alkenone palaeothermometry has demonstrated a wide spatial and temporal applicability for the reconstruction of sea-surface temperatures (SST). Some oceanic realms, however, remain poorly studied. We document U37K' index data for two sediment cores retrieved from the South Tasman Sea, one west of New Zealand (SO136-GC3) and the other southeast of Tasmania (FR1\\/94-GC3), extending back 280 kyr BP for the former and

C. Pelejero; E. Calvo; T. T. Barrows; G. A. Logan; P. De Deckker

2006-01-01

7

Geology and petroleum potential of the Fairway Basin in the Tasman Sea  

Microsoft Academic Search

The Fairway Basin is a large, generally north – south-trending, sediment-filled structure in water 1500 – 3000 m deep, on the eastern slope of the Lord Howe Rise in the Tasman Sea, and is partly within Australian jurisdiction. It was poorly known until a few years ago, when seismic profiling and piston coring cruises were carried out. The basin, about 1100 km long and 120 – 200 km wide,

N. F. Exon; Y. Lafoy; P. J. Hill; G. R. Dickens; I. Pecher

2007-01-01

8

A virgin flight across the Tasman Sea? Satellite tracking of post-fledging movement in the Australasian Gannet Morus serrator  

Microsoft Academic Search

New technologies enable tracking of the route, duration, and destination of previously unassessed long-distance movements.\\u000a Fledgling Australasian Gannets Morus serrator from breeding populations in New Zealand had been reported to fly across the Tasman Sea to Australia, with this historic\\u000a knowledge derived from the recovery of banded carcasses and from observations of initial flight direction. We deployed Argos\\u000a satellite devices

Stefanie M. H. Ismar; Colin Hunter; Kevin Lay; Tamsin Ward-Smith; Peter R. Wilson; Mark E. Hauber

2010-01-01

9

The geomorphology of the flanks of the Lord Howe Island volcano, Tasman Sea, Australia  

NASA Astrophysics Data System (ADS)

The flanks of mid-ocean volcanoes are inherently unstable features especially in the constructional phase of development when the volcano is active. Lateral and vertical stresses are placed on the volcanic edifice as it builds, with the flanks continuing to be unstable up to at least 1 Ma after volcanism has ceased. The flanks of the Lord Howe Island volcano record this period of greatest instability and a subsequent period in which marine and subaerial erosion have dominated its geomorphic evolution. Lord Howe Island lies in the Tasman Sea of the Southern Pacific region and is the subaerial remnant of a Miocene mid-ocean volcano. The island has only recently entered reef building seas and therefore has been subject to marine erosive processes over the past 5-6 Ma. The island is unique as it sits on the stable drowned continental crust of the Lord Howe Rise rather than oceanic crust like many other mid-plate basaltic islands. Multibeam sonar bathymetry data were collected to a depth of 3500 m where the island flanks grade into the surrounding planar sea floor. Several slump features are evident, the largest being over 130 km 2 in area. These features are inferred to be old (late Tertiary) based on an extensive cover of marine sediment as indicated by low multibeam backscatter intensity and subdued topography. Most likely the slumps formed during the immediate post-eruptive stage of volcano evolution, before the bulk of the subaerial portion of the volcano was removed by marine erosion. Flank processes are now dominated by the deposition of carbonate sediment composed of mollusc and foraminiferal remains. Based on radiocarbon and stable isotope analyses of a sediment core (760 m depth) collected on a trough in the centre of the volcanic edifice, Quaternary sediment was likely deposited predominantly during glacial periods. The erosional morphology, sediment cover and tectonic stability of the region suggest that the flanks of the volcano are at present relatively stable.

Kennedy, D. M.; Brooke, B. P.; Woodroffe, C. D.; Jones, B. G.; Waikari, C.; Nichol, S.

2011-04-01

10

A synoptic comparison of fishes and crustaceans from a warm-core eddy, the East Australian Current, the Coral Sea and the Tasman Sea  

NASA Astrophysics Data System (ADS)

Mesopelagic fishes and crustaceans inside a newly formed, warm-core eddy off eastern Australia were similar in composition and abundance of species to those from the more northerly Coral Sea and East Australian Current (EAC) source waters of the eddy. The crustaceans inside the eddy were a mixture of warm-water and cold-water species and were dissimilar to the crustacean fauna on either the Tasman Sea or the Coral Sea-EAC sampling sites. In contrast, of the fishes collected (all from the family Myctophidae), only warm-water or widespread species were present in the eddy. A zoogeographic transect along 155° between 16°S and 32°S showed cold-water crustaceans were present between 24°S and 32°S whereas cold-water fishes were absent. The crustacean fauna of a new eddy was distinct from both the fauna of the source region and of the Tasman Sea because sufficient cold-water species were already present in the geographical location where a new eddy forms. The myctophid fauna of a new warm-core eddy was essentially identical to the Coral Sea fauna because cold-water species do not penetrate into the warmer waters of the source of the eddies. A temperature of 15°C at 250 m depth may be a useful oceanographic marker separating subtropical from temperate myctophids in the Coral and Tasman seas.

Griffiths, F. B.; Wadley, V. A.

1986-11-01

11

High resolution satellite observations of mesoscale oceanography in the Tasman Sea, 1978 - 1979  

NASA Technical Reports Server (NTRS)

Of the Nearly 1000 standard infrared photographic images received, 273 images were on computer compatible tape. It proved necessary to digitally enhance the scene contrast to cover only a select few degrees K over the photographic grey scale appropriate to the scene-specific range of sea surface temperature (SST). Some 178 images were so enhanced. Comparison with sea truth show that SST, as seen by satellite, provides a good guide to the ocean currents and eddies off East Australia, both in summer and winter. This is in contrast, particularly in summer, to SST mapped by surface survey, which usually lacks the necessary spatial resolution.

Nilsson, C. S.; Andrews, J. C.; Hornibrook, M.; Latham, A. R.; Speechley, G. C.; Scully-Power, P. (principal investigators)

1982-01-01

12

Design and operation of a deep seismic survey in the Tasman Sea Basin  

NASA Astrophysics Data System (ADS)

Deep crustal reflections, appearing at two-way times of 6-20 s, are characterised by a low signal-to-noise ratio and a low-frequency content (~ 5-30 Hz). Optimising the visibility of these reflections requires that: (1) the source energy be concentrated in this band; (2) the receiver be as long as practically possible; (3) the shot spacing be as snail as possible. An airgun array simulation program was used to investigate the effect of operating a 10-gun array at different depths. It predicted that the source energy could be enhanced at low frequencies by running the gun array at depths of up to 25 m, which would improve the signal-to-noise ratio for deep reflectors by a factor of 2 relative to the same array at 7.5 m depth at the expense of some loss of temporal resolution. The receiver length was limited to 4.4 km by the number of cable sections available and the maximum tension allowable in the cable. It was configured as 88 channels of 50 m length. To reduce the shot spacing, minimise the tow noise and reduce tension in the cable, the ship speed was reduced to 4 knots. A cable depth of 20 m was chosen to reduce sea state noise and keep the receiver ghost notch frequency outside the frequency band of interest. A variety of operational problems was encountered. Fish bites holed 50% of the total cable inventory and cable sections were damaged when they sank below their maximum rated depth after being holed. Shot-generated noise was the limiting factor in deep water. Despite these problems, useful data were obtained over the Lord Howe Rise, Dampier Ridge, Gippsland Basin margin and the deep abyssal plain and the survey demonstrated the use of an airgun array tuned for maximum energy.

Kravis, S. P.; Coffin, M. F.; Whitworth, R.

1990-02-01

13

Parapercis nigrodorsalis (Perciformes: Pinguipedidae), a new species of sandperch from northern New Zealand and the Norfolk Ridge, Tasman Sea and remarks on P. binivirgata (Waite, 1904).  

PubMed

A new species of pinguipedid fish, Parapercis nigrodorsalis, is described from 17 specimens collected off the North Island of New Zealand and Wanganella Bank, Norfolk Ridge, Tasman Sea, in depths of 56-280 m. The species has also been photographed underwater off the Poor Knights Islands Reserve and Burgess Island, Mokohinau Group, in New Zealand. It is most similar to Parapercis binivirgata (Waite, 1904) in morphology, coloration and meristic values, but is unique among the genus in having a combination of dorsal-fin rays V, 23, anal-fin rays I, 19, lateral-line scales 57-63, vomer with 1-2 irregular rows of robust conical teeth, palatines with 1-2 rows of small teeth, angle of subopercle smooth, 10 abdominal and 22 caudal vertebrae, and coloration, including seven broad reddish-brown bands on the upper body between the spinous dorsal-fin and the caudal peduncle, most bands bifurcated into close-set double bars with black smudge-like blotches below, and membrane of the spinous dorsal fin black. Comparison of the mitochondrial cytochrome c oxidase subunit 1 (CO 1) genetic marker utilised in DNA barcoding produced a genetic divergence of 5.38% and 7.63% between the new species and its two closest sampled congeners. The holotype of P. binivirgata is identified from two specimens previously regarded as syntypes, some revisions are made to meristic data in the original description of the latter, and a detailed description of the revised geographic range of P. binivirgata is provided.   PMID:25284671

Johnson, Jeffrey W; Struthers, Carl D; Wilmer, Jessica Worthington

2014-01-01

14

Flows in the Tasman Front south of Norfolk Island  

NASA Astrophysics Data System (ADS)

The Tasman Front is a narrow band of eastward flowing subtropical water crossing the Tasman Sea from Australia to North Cape, New Zealand. It is the link between the two subtropical western boundary currents of the South Pacific, the East Australian Current (EAC) off eastern Australia, and the East Auckland Current (EAUC) off northeastern New Zealand. Here we report the first direct measurements of flow in the Tasman Front from a moored array deployed across gaps in the submarine ridges south of Norfolk Island and hydrographic and ADCP measurements during the deployment and recovery voyages. The mean flow through the array over July 2003 to August 2004 was found to be eastward only in the upper 800 m with a transport of ˜6 Sv. Below 800 m a weak westward mean flow (˜1.5 Sv) was measured, associated with Antarctic Intermediate Water (AAIW). Using sea surface height to account for additional transport south of the moored array results in a total mean eastward transport between Norfolk Island and North Cape, New Zealand of ˜8 Sv, varying between -4 and 18 Sv. The measurements show that the Tasman Front is much shallower than either the EAC or EAUC, both of which extend below 2000 m depth, has less transport than either the EAC or EAUC and has instances of flow reversal. Thus, the Tasman Front is a weaker connection between the EAC and EAUC than the paradigm of a contiguous South Pacific western boundary current system would suggest.

Sutton, Philip J. H.; Bowen, Melissa

2014-05-01

15

Tasman Leakage of intermediate waters as inferred from Argo floats  

NASA Astrophysics Data System (ADS)

use Argo float trajectories to infer ocean current velocity at the sea surface and 1000 dbar near Australia. The East Australian Current flows southward along the east coast of Australia at both surface and intermediate levels, but only the intermediate waters leak round the southern tip of Tasmania and cross the Great Australian Bight. We calculate the transport of Antarctic Intermediate Water (AAIW) between the southern Australian coast and the Antarctic Circumpolar Current (ACC) as the velocity at 1000 dbar times the layer thickness. Between March 2006 and December 2012, the Eulerian AAIW transport through 147°E ranges between 0 and 12.0 sverdrup (Sv). The mean Tasman Leakage of intermediate waters from the Pacific Ocean into the Indian Ocean, obtained using all Argo data until March 2013, is 3.8 ± 1.3 Sv. The mean intermediate water transport into the Indian Ocean through 115°E increases to 5.2 ± 1.8 Sv due to contributions from the westward recirculation of ACC waters.

Rosell-Fieschi, Miquel; Rintoul, Stephen R.; Gourrion, Jeröme; Pelegrí, Josep L.

2013-10-01

16

170 West Tasman Drive San Jose, CA 95134-1706  

E-print Network

170 West Tasman Drive San Jose, CA 95134-1706 USA http://www.cisco.com Cisco Systems, Inc. Corporate Headquarters Tel: 800 553-NETS (6387) 408 526-4000 Fax: 408 526-4100 Guide to Cisco Systems' Vo OR LIMITED WARRANTY, CONTACT YOUR CISCO REPRESENTATIVE FOR A COPY. The Cisco implementation of TCP header

Westall, James M.

17

Pleistocene variability of the Subtropical Convergence at East Tasman Plateau: Evidence from planktonic foraminiferal Mg/Ca (ODP Site 1172A)  

NASA Astrophysics Data System (ADS)

Combined measurements of Mg/Ca and stable oxygen isotopes in tests of the planktonic foraminifer G. bulloides from Ocean Drilling Program (ODP) Site 1172A (East Tasman Plateau) allowed us to reconstruct sea surface temperature (SSTMg/Ca), sea surface salinity (SSS), and hence variations in the Subtropical Convergence (STC) in the southwestern Tasman Sea over the last four major glacial-interglacial changes. During interglacials the commonly enhanced SSTMg/Ca and SSS correspond to a lowered marine productivity and a lowered terrigenous flux, implying that the STC separating cool, high-nutrient Subantarctic Surface Water from warm, saline, oligotrophic Subtropical Surface Water and hence the band of zonal westerlies responsible for the eolian dust flux were located south of East Tasman Plateau. The warm East Australian Current was well established during warm periods and propagated far south. During glacial times, SSTMg/Ca and SSS were lower, while both marine productivity and eolian flux increased. Such conditions prevailed during glacial Marine Isotope Stages MIS 12, MIS 10, and to a lesser degree MIS 6 and implied the extended northward influence of Subantarctic Surface Water and a shift of the STC to <44°S. The overall climatic signal at Site 1172A appears to be largely attenuated when compared to published climate records from comparable latitudes to the west and to the east. SSTMg/Ca amplitudes were more pronounced in the subantarctic Indian Ocean and at Chatham Rise. They exhibit a consistent pattern suggesting that latitudinal shifts of the STC occurred synchronously in the subantarctic Indian Ocean and at Chatham Rise but were largely damped at East Tasman Plateau due to the influence of the East Australian Current.

Nürnberg, Dirk; Groeneveld, Jeroen

2006-04-01

18

Acute health effects of the Tasman Spirit oil spill on residents of Karachi, Pakistan  

PubMed Central

Background On July 27 2003, a ship carrying crude oil run aground near Karachi and after two weeks released 37,000 tons of its cargo into the sea. Oil on the coastal areas and fumes in air raised health concerns among people. We assessed the immediate health impact of oil spill from the tanker Tasman Spirit on residents of the affected coastline in Karachi, Pakistan. Methods We conducted a study consisting of an exposed group including adults living in houses on the affected shoreline and two control groups (A and B) who lived at the distance of 2 km and 20 km away from the sea, respectively. We selected households through systematic sampling and interviewed an adult male and female in each household about symptoms relating to eyes, respiratory tract, skin and nervous system, smoking, allergies, beliefs about the effect on their health and anxiety about the health effects. We used logistic regression procedures to model each symptom as an outcome and the exposure status as an independent variable while adjusting for confounders. We also used linear regression procedure to assess the relationship exposure status with symptoms score; calculated by summation of all symptoms. Results Overall 400 subjects were interviewed (exposed, n = 216; group A, n = 83; and group B, n = 101). The exposed group reported a higher occurrence of one or more symptoms compared to either of the control groups (exposed, 96% vs. group A, 70%, group B 85%; P < 0.001). Mean summary symptom scores were higher among the exposed group (14.5) than control group A (4.5) and control group B (3.8, P < 0.001). Logistic regression models indicated that there were statistically significant, moderate-to-strong associations (Prevalence ORs (POR) ranging from 2.3 to 37.0) between the exposed group and the symptoms. There was a trend of decreasing symptom-specific PORs with increase in distance from the spill site. Multiple linear regression model revealed strong relationship of exposure status with the symptoms score (? = 8.24, 95% CI: 6.37 – 10.12). Conclusion Results suggest that the occurrence of increased symptoms among the exposed group is more likely to be due to exposure to the crude oil spill. PMID:16584541

Janjua, Naveed Zafar; Kasi, Pashtoon Murtaza; Nawaz, Haq; Farooqui, Sadia Zohra; Khuwaja, Urooj Bakht; Najam-ul-Hassan; Jafri, Syed Nadim; Lutfi, Shahid Ali; Kadir, Muhammad Masood; Sathiakumar, Nalini

2006-01-01

19

Wave energy and clast transport in eastern Tasman Bay, New Zealand  

Microsoft Academic Search

Coarse-gravel beaches are common features along the eastern margin of Tasman Bay, at the north end of South Island, New Zealand. Although these features have traditionally been interpreted as spits, contemporary incident wave energy appears too small to transport boulders and cobbles persistently along the beaches and platforms by longshore drift. An alternative explanation suggests that boulder beaches are essentially

Neil D. Hartstein; Warren W. Dickinson

2006-01-01

20

Oligopoly behaviour in the Trans?Tasman air travel market: The case of kiwi international  

Microsoft Academic Search

The duopoly of Air New Zealand and Qantas serving the Trans?Tasman air travel market was disturbed in August 1995 by the entry of a small former charter airline, Kiwi International, based in Hamilton, NZ. Kiwi exited into liquidation in September 1996. The intervening thirteen months saw the entry of a ‘fighting brand’ no?frills airline, Freedom Air, set up by Air

David Haugh; Tim Hazledine

1999-01-01

21

Assessment of hydrocarbons concentration in marine fauna due to Tasman Spirit oil spill along the Clifton beach at Karachi coast.  

PubMed

On 27 July 2003, Tasman Spirit spilled 31,000 tonnes of crude oil into the sea at the Karachi coast. This disaster badly affected the marine life (Flora and Fauna.) Present research has been proposed to ascertain the level of Polycyclic Aromatic hydrocarbons (PAHs) contamination in different fisheries including Fishes, Crustaceans; Crabs and Shrimps, Mollusks and Echinoderms along with passing time. Heavier components of crude oil such as Polycyclic Aromatic Hydrocarbons (PAHs) appear to cause most damages as these are relatively unreactive and persist in water. High concentrations of toxic PAHs were observed in all the fisheries and shellfishes caught form oil-impacted area. In this study fishes were found most contaminated than shellfishes i.e. summation operator 16 PAH = 1821.24 microg/g and summation operator 1164.34 microg/g, respectively. Naphthalene was found in the range of 0.042-602.23 microg/g. Acenaphthylene, acenaphthene, fluorene, phenanthrene and anthracene were detected in the range 0.008-80.03 microg/g, fluoranthene, pyrene, benzo(a)anthracene and chrysene 0.0008-221.32 microg/g, benzo(b) fluoranthene, benzo(k)fluoranthene and benzo(a) pyrene 0.0005-7.71 microg/g, benzo(g,h,i)perylene and indeno(1,2,3-c,d)pyrene 0.02-503.7 microg/g. Dibenzo(a,h)anthracenre was not detected in any specie. PMID:18302003

Siddiqi, Hina A; Ansari, Fayyaz A; Munshi, Alia B

2009-01-01

22

Formation of glaciolacustrine Late Pleistocene end moraines in the Tasman Valley, New Zealand  

Microsoft Academic Search

Detailed examination of the Tekapo Formation in the Tasman Valley, New Zealand has identified 20 facies, and five facies associations. These associations are delta foresets and bottomsets, sediment density flows, ice-contact lake sediments with ice-rafted debris and resedimentation deposits, and outwash gravels. Interpretation of the sediment-landform associations informed by observations at modern glacier termini suggests that the Late Pleistocene Tekapo

Sarah Mager; Sean Fitzsimons

2007-01-01

23

Recent and future higher sea levels in New Zealand: A review  

Microsoft Academic Search

Understanding past sea levels is essential to respond to the challenges of climate change. In the Pacific and Tasman, sea level has been up to 1.5 m higher during the mid-Holocene, similar to the predictions of some global warming models. Within New Zealand the knowledge of sea-level movements, especially during the recent past is poor, with the last major investigation

David M. Kennedy

2008-01-01

24

Earth Interactions 1 The Opening of the Tasman Sea: A Gravity  

E-print Network

of Geosciences, Division of Geology and Geophysics, University of Sydney, Sydney, Australia E-mail: carmen, University of Sydney, Sydney, Australia E-mail: dietmar@es.su.oz.au P. Symonds, Australian Geological Survey of Geology and Geo- physics, David Edgeworth Building, F05, University of Sydney, NSW 2006, Australia. #12

Müller, Dietmar

25

Large scale features and energetics of the hybrid subtropical low `Duck' over the Tasman Sea  

NASA Astrophysics Data System (ADS)

New aspects of the genesis and partial tropical transition of a rare hybrid subtropical cyclone on the eastern Australian coast are presented. The `Duck' (March 2001) attracted more recent attention due to its underlying genesis mechanisms being remarkably similar to the first South Atlantic hurricane (March 2004). Here we put this cyclone in climate perspective, showing that it belongs to a class within the 1 % lowest frequency percentile in the Southern Hemisphere as a function of its thermal evolution. A large scale analysis reveals a combined influence from an existing tropical cyclone and a persistent mid-latitude block. A Lagrangian tracer showed that the upper level air parcels arriving at the cyclone's center had been modified by the blocking. Lorenz energetics is used to identify connections with both tropical and extratropical processes, and reveal how these create the large scale environment conducive to the development of the vortex. The results reveal that the blocking exerted the most important influence, with a strong peak in barotropic generation of kinetic energy over a large area traversed by the air parcels just before genesis. A secondary peak also coincided with the first time the cyclone developed an upper level warm core, but with insufficient amplitude to allow for a full tropical transition. The applications of this technique are numerous and promising, particularly on the use of global climate models to infer changes in environmental parameters associated with severe storms.

Pezza, Alexandre Bernardes; Garde, Luke Andrew; Veiga, José Augusto Paixão; Simmonds, Ian

2014-01-01

26

Downwasting of the Tasman Glacier, South Island, New Zealand: Changes in the terminus region between 1971 and 1993  

Microsoft Academic Search

Downwasting has altered the morphology of the terminus region of the Tasman Glacier between 1971 and 1993. Rapid melting began in the late 1960s in a few isolated melt ponds in the centre and in a small elongated lakelet at the eastern lateral moraine. These ponds and lakes grew rapidly in size during the 1970s and coalesced to form a

Manfred P. Hochstein; David Claridge; Stuart A. Henrys; Alex Pyne; David C. Nobes; Stephen F. Leary

1995-01-01

27

Palynomorph assemblages from marine Eocene sediments on the west Tasmanian continental margin and the South Tasman Rise  

Microsoft Academic Search

Eocene sediments have been sampled at five localities on the continental margin off western Tasmania and on the South Tasman Rise. Palynomorph assemblages recovered from these show that carbonaceous, pollen?rich sediments in the Strahan Sub?basin sampled by gravity coring during the RV Sonne cruise of 1985, which were probably laid down in shallow water, belong to the Proteacidites asperopolus Zone

E. M. Truswell

1997-01-01

28

@Sea  

NSDL National Science Digital Library

This site describes the Harbor Branch Oceanographic Institution's at-sea research expeditions and presents both current and archived expeditions from 1999 to the present. Each expedition is described in a feature story with background, definitions, research technology and sampling equipment, maps, photos, daily logs, some videos and virtual tours, researcher profiles, and related links. HBOI scientists have studied maritime history, pharmaceuticals from the sea, sharks, behavior and physiology of marine life, marine sanctuaries and submersible technology.

29

Southern high-latitude terrestrial climate change during the Palaeocene-Eocene derived from a marine pollen record (ODP Site 1172, East Tasman Plateau)  

NASA Astrophysics Data System (ADS)

Reconstructing the early Palaeogene climate dynamics of terrestrial settings in the high southern latitudes is important to assess the role of high-latitude physical and biogeochemical processes in the global climate system. However, whereas a number of high-quality Palaeogene climate records has become available for the marine realm of the high southern latitudes over the recent past, the long-term evolution of coeval terrestrial climates and ecosystems is yet poorly known. We here explore the climate and vegetation dynamics on Tasmania from the middle Palaeocene to the early Eocene (60.7-54.2 Ma) based on a sporomorph record from Ocean Drilling Program (ODP) Site 1172 on the East Tasman Plateau. Our results show that three distinctly different vegetation types thrived on Tasmania under a high-precipitation regime during the middle Palaeocene to early Eocene, with each type representing different temperature conditions: (i) warm-temperate forests dominated by gymnosperms that were dominant during the middle and late Palaeocene (excluding the middle/late Palaeocene transition); (ii) cool-temperate forests dominated by southern beech (Nothofagus) and araucarians that transiently prevailed across the middle/late Palaeocene transition interval (~ 59.5 to ~ 59.0 Ma); and (iii) paratropical forests rich in ferns that were established during and in the wake of the Palaeocene-Eocene Thermal Maximum (PETM). The transient establishment of cool-temperate forests lacking any frost-sensitive elements (i.e. palms and cycads) across the middle/late Palaeocene transition interval indicates markedly cooler conditions, with the occurrence of frosts in winter, on Tasmania during that time. The integration of our sporomorph data with previously published TEX86-based sea-surface temperatures from ODP Site 1172 documents that the vegetation dynamics on Tasmania were closely linked with the temperature evolution in the Tasman sector of the Southwest Pacific region. Moreover, the comparison of our season-specific climate estimates for the sporomorph assemblages from ODP Site 1172 with the TEX86L- and TEX86H-based temperature data suggests a warm bias of both calibrations for the early Palaeogene of the high southern latitudes.

Contreras, L.; Pross, J.; Bijl, P. K.; O'Hara, R. B.; Raine, J. I.; Sluijs, A.; Brinkhuis, H.

2014-07-01

30

Southern high-latitude terrestrial climate change during the Paleocene-Eocene derived from a marine pollen record (ODP Site 1172, East Tasman Plateau)  

NASA Astrophysics Data System (ADS)

Reconstructing the early Paleogene climate dynamics of terrestrial settings in the high southern latitudes is important to assess the role of high-latitude physical and biogeochemical processes in the global climate system. However, whereas a number of high-quality Paleogene climate records has become available for the marine realm of the high southern latitudes over the recent past, the long-term evolution of coeval terrestrial climates and ecosystems is yet poorly known. We here explore the climate and vegetation dynamics on Tasmania from the middle Paleocene to the early Eocene (60.7-54.2 Ma) based on a sporomorph record from Ocean Drilling Program (ODP) Site 1172 on the East Tasman Plateau. Our results show that three distinctly different vegetation types thrived on Tasmania under a high-precipitation regime during the middle Paleocene to early Eocene, with each type representing different temperature conditions: (i) warm-temperate forests dominated by gymnosperms that were dominant during the middle and late Paleocene; (ii) cool-temperate forests dominated by southern beech (Nothofagus) and araucarians across the middle/late Paleocene transition interval (~59.5 to ~59.0 Ma); and (iii) paratropical forests rich in ferns that were established during and in the wake of the Paleocene-Eocene Thermal Maximum (PETM). The transient establishment of cool-temperate forests lacking any frost-sensitive elements (i.e., palms and cycads) across the middle/late Paleocene transition interval indicates markedly cooler conditions, with the occurrence of frosts in winter, on Tasmania during that time. The integration of our sporomorph data with previously published TEX86-based sea-surface temperatures from ODP Site 1172 documents that the vegetation dynamics on Tasmania were closely linked with the temperature evolution in the Tasman sector of the Southwest Pacific region. Moreover, the comparison of our season-specific climate estimates for the sporomorph assemblages from ODP Site 1172 with the TEX86L- and TEX86H-based temperature data suggests a warm-season bias of both calibrations for the early Paleogene of the high southern latitudes.

Contreras, L.; Pross, J.; Bijl, P. K.; O'Hara, R. B.; Raine, J. I.; Sluijs, A.; Brinkhuis, H.

2014-01-01

31

Tasman Spirit Oil Spill in Pakistan – Research Response and Lessons Learned  

PubMed Central

Background This paper presents lessons learned from an investigation of the acute human health effects of the “Tasman Spirit' oil spill from a perspective of conducting rapid response investigations in developing countries. Methods We reviewed various steps in our investigation, other studies on oil spills in Pakistan and around the world, and reflected upon our discussions and interactions with various stakeholders. Results The paper highlights the importance of applying a public health, legal, and ethical framework for conducting rapid response investigations, developing a pre-established funding mechanism, and addressing study design issues, exposure and outcome measurements, political issues, community engagement, and communication of results. Conclusion There is need to develop ethical and legal framework and funding mechanism for conducting rapid response research in developing countries. A repository of study protocols, validated tools, and laboratory methods for exposure and outcome assessment would be greatly beneficial. PMID:22473418

Janjua, Naveed Zafar; Kadir, Muhammad Masood; Lutfi, Shahid; Tipre, Meghan; Sathiakumar, Nalini

2012-01-01

32

The Tasman Spirit oil spill: implications for regulatory change in Pakistan.  

PubMed

An oil spill in July 2003 from the tanker Tasman Spirit attracted considerable public and media attention in Pakistan. This paper focuses on the experience of a developing country such as Pakistan in dealing with a major oil spill and its impact on bringing about change in the national regulatory framework. A major outcome has been the ratification of the International Convention on Civil Liability for Oil Pollution Damage 1992, which came into force in March 2006 in Pakistan. The convention provides a compensation mechanism for victims incurring oil pollution damages from maritime casualties involving oil laden ships. Several additional changes are still required to improve the country's ability to cope with marine oil spills. These include the development of a comprehensive domestic regulatory framework, implementation of an effective contingency plan, and capacity building of all relevant agencies. PMID:19178550

Mian, Saima; Bennett, Suzan

2009-07-01

33

Working towards a group A streptococcal vaccine: report of a collaborative Trans-Tasman workshop.  

PubMed

Group A Streptococcus (GAS) infections represent a major public health burden in both developing and developed countries. In Australia and New Zealand GAS associated diseases are serious problems in Indigenous populations and a major cause of health inequality. Political recognition of these inequalities is providing impetus for strategies that reduce GAS disease and the development of a GAS vaccine now has governmental support in both Australia and New Zealand. Accordingly, an expert workshop was convened in March 2013 to consider available data on GAS vaccines. M-protein based vaccines constructed from the hyper-variable N-terminal region (30-valent vaccine) or the conserved C-repeat domain (J8 vaccine) were reviewed together with vaccine candidates identified using multi high-throughput approaches. Performing a comprehensive assessment of regional GAS strain epidemiology, defining the immune correlates of protection, and the establishment of clinical trial sites were identified as critical activities for a Trans-Tasman vaccine development programme. PMID:24837510

Moreland, Nicole J; Waddington, Claire S; Williamson, Deborah A; Sriskandan, Shiranee; Smeesters, Pierre R; Proft, Thomas; Steer, Andrew C; Walker, Mark J; Baker, Edward N; Baker, Michael G; Lennon, Diana; Dunbar, Rod; Carapetis, Jonathan; Fraser, John D

2014-06-24

34

Coseismic-initiated calving at a freshwater-terminating glacier: Tasman Glacier, New Zealand  

NASA Astrophysics Data System (ADS)

Glacier retreat resulting from iceberg calving represents one of the major controls on ice loss from water-terminating glaciers (ice sheets, tidewater and freshwater glaciers) globally. However, the impact that calving has on the transfer of mass between the cryosphere and hydrosphere is still heavily debated, and the physical mechanisms behind calving remain poorly understood. Hitherto, the initiation of calving events has largely been attributed to underlying glaciological mechanisms (including fracturing of ice due to high longitudinal stress gradients) and changes in the proglacial water-body characteristics. We present evidence for a large-magnitude calving event following high magnitude (>Mw 6) earthquakes as a potentially important triggering mechanism of calving in tectonically-active areas. We describe the response of Tasman Glacier, New Zealand, a freshwater-terminating glacier undergoing accelerated calving retreat, to the Mw 6.3, 5.7 and 4.5 Christchurch 22 February 2011 earthquakes and the subsequent calving event. Time-series analysis of timed video and photographic records of the glacier terminus immediately pre-, co- and post- the 22 February earthquakes demonstrates that the large calving event on the 22 February 2011 occurred in direct response to a resonance effect caused by shear (S-) waves oscillating the terminus at the ice-water interface. We suggest that, in this instance, the magnitude of calving was amplified because Tasman Glacier had reached a critical threshold for buoyancy-induced calving in relation to perturbations in lake level. Prior to this event, small- to intermediate magnitude calving, leading to terminus retreat, had been dominated by thermo-erosional notching at the waterline, destabilising the subaerial ice cliff. Indeed, recent (post-2006) large calving events have primarily been driven by torque-induced, buoyancy-driven calving. Hence, in tectonically-active areas, coseismic-initiated calving can have an episodic, but strong control on retreat, potentially destabilising a glacier system and leading to accelerated recession, accentuating climate-forced mass balance changes.

Dykes, R. C.; Lube, G.; Brook, M. S.

2012-04-01

35

The Cretaceous/Paleogene Transition on the East Tasman Plateau, Southwestern Pacific  

NASA Technical Reports Server (NTRS)

Ocean Drilling Program Leg 189 recovered a potentially complete shallow marine record of the Cretaceous-Paleogene boundary (KPB) at Site 1172 on the East Tasman Plateau. Here we present high-resolution (cm-scale) data from micropaleontology, geochemistry, sedimentology, and paleomagnetism that provide no evidence for a complete KPB, but instead suggest a boundary-spanning hiatus of at least 0.8 Ma. We interpret this hiatus to represent the sequence boundary between the uppermost Maastrichtian Tal.1 and lowermost Danian Ta1.2/ Da- 1 3rd-order sequence stratigraphic cycles. Microfloral assemblages indicate generally shallow paleodepths, restricted circulation, and eutrophic conditions through the section. Paleodepths progressively shallow through the late Maastrichtian, while more oceanic and warmer conditions dominate the early Danian. The Site 1172 KPB section is broadly comparable to other southern highlatitude sections in Antarctica and New Zealand, but appears to record a shallower and more restricted environment that permitted a eustatically-driven hiatus across the KPB mass extinction event.

Schellenberg, Stephen A.; Brinkhuis, Henk; Stickley, Catherine E.; Fuller, Michael; Kyte, Frank T.; Williams, Graham L.

2004-01-01

36

Survey of ULF wave signatures seen in the Tasman International Geospace Environment Radars data  

NASA Astrophysics Data System (ADS)

Ultralow frequency (ULF) plasma waves propagate through the magnetosphere and ionosphere where they can alter the Doppler velocity of HF radar echoes. Data from the two Tasman International Geospace Environment Radars and the fluxgate and induction coil magnetometers located on Macquarie Island (54.5°S, 158.95°E geographic) over 2006-2009 show that ULF wave signatures are common. Using coincident radar and magnetometer data selection criteria, 194 events representing a total of 233.4 h were identified. The majority of ULF signatures seen in the radar data were detected between 06 and 12 UT (15 and 21 LT). Using the Maximum Entropy Method, the spectral content showed favored frequencies of 1.6, 2.1, 2.9, and 3.3 mHz but no obvious variation of frequency with latitude. Most of the observed frequencies were in the range 1-4 mHz. A class of Doppler velocity signatures that appeared as a zigzag shape in the radar range:time plots were identified and may be related to the expected plasmapause latitudes. Regularly spaced, favored frequencies appeared in the ground magnetometer data during the afternoon, night, and morning sectors for those days where ULF wave events were observed in the radar data.

Norouzi-Sedeh, L.; Waters, C. L.; Menk, F. W.

2015-02-01

37

Genome Sequence of "Thalassospira australica" NP3b2T Isolated from St. Kilda Beach, Tasman Sea.  

PubMed

Here, we present the draft genome of "Thalassospira australica" NP3b2(T), a potential poly(ethylene terephthalate) (PET) plastic biodegrader. This genomic information will enhance information on the genetic basis of metabolic pathways for the degradation of PET plastic. PMID:25395631

López-Pérez, Mario; Rodriguez-Valera, Francisco; Webb, Hayden K; Crawford, Russell J; Ivanova, Elena P

2014-01-01

38

Genome Sequence of “Thalassospira australica” NP3b2T Isolated from St. Kilda Beach, Tasman Sea  

PubMed Central

Here, we present the draft genome of “Thalassospira australica” NP3b2T, a potential poly(ethylene terephthalate) (PET) plastic biodegrader. This genomic information will enhance information on the genetic basis of metabolic pathways for the degradation of PET plastic. PMID:25395631

López-Pérez, Mario; Webb, Hayden K.; Crawford, Russell J.

2014-01-01

39

Mean circulation of the Coral Sea  

NASA Astrophysics Data System (ADS)

The mean absolute geostrophic circulation of the Coral Sea is constructed from climatological hydrographic data referenced to a 1000 m velocity field derived from Argo float drift. Two branches of the South Equatorial Current (SEC) enter the Coral Sea between New Caledonia and the Solomon Islands: the broad, upper thermocline North Vanuatu Jet (NVJ), and the narrow North Caledonian Jet (NCJ) extending to at least 1500 m. Most of this incoming flow leaves to the Solomon Sea. Four distinct pathways through the Coral Sea are traced by their water properties: (1) The NCJ crosses the Sea to the coast of Australia and turns north at densities sigma 25-27.4 as the main source of the Gulf of Papua (GPC) western boundary current, eventually feeding the New Guinea Coastal Undercurrent; (2) part of the shallow NVJ turns into the Solomon Sea in midbasin, carrying high-salinity water above sigma 25.5; (3) another part of the NVJ continues to Australia, then turns north to join the GPC, extending it to the surface; (4) a shallow finger of NVJ water, traced by low oxygen above sigma 25, turns south along the coast, beginning the East Australian Current (EAC) at 15°S. Total transport from the Coral to the Tasman Sea is small and shallow; instead, most of the EAC is fed from south of New Caledonia, consistent with the Island Rule. However, large transport fractions occur in narrow jets close to coastlines and reefs and are not well sampled, precluding a quantitative estimate of meridional redistribution of the incoming SEC.

Kessler, William S.; Cravatte, Sophie

2013-12-01

40

Tracking surface water mass movements in the Southwest Pacific for the last 5,000 years: Perspectives from deep-sea corals  

NASA Astrophysics Data System (ADS)

Current understanding of present-day natural climate variability can be improved by obtaining a good baseline through investigating past variability during the Holocene (11,500 cal yr B.P. to the present). In particular, changes in marine reservoir radiocarbon ages through the Holocene can provide information on regional ocean circulation. In the southwest Pacific, little is known about the variability of reservoir ages during this period. This limits efforts to reconstruct Southern Hemisphere Ocean and atmospheric circulation over this period. Here we present mid- to late-Holocene reservoir ages for the southwest Pacific. Reservoir ages were calculated using coupled uranium series (MC ICPMS) and radiocarbon (AMS) measurements on deep-sea (200 - 1000m) black coral (Anthozoa, Antipatharia) collected live from the Tasman Sea. Black corals have enormous potential as environmental archives to provide valuable long-term, high-resolution records. We confirm that black corals are slow growing (typical radial growth rate is 0.005 mm/yr) and extremely long-lived (maximum age 5,823 × 41 years), making them excellent candidates for proxies to extend environmental records into the Holocene. Our results also indicate comparatively lower reservoir ages for the mid-Holocene than present day for the south Tasman Sea. The lower reservoir ages in the mid-Holocene reflect a greater influx of well-equilibrated warm water of sub-tropical origin into this region, as well as increased stratification. During the late Holocene in the north Tasman, the average reservoir age between 1790 and 1900 was ˜330 years, followed by a steep decrease over time of about 70 years to 1950 AD (our most modern value). This indicates an increase in surface ocean ventilation of water masses in this region. These results are consistent with observational and modeling studies for the last century, which show significant changes in regional circulation and suggest these changes started as early as the 17th century.

Komugabe, A. F.; Fallon, S.; Thresher, R.; Eggins, S. M.

2013-12-01

41

GODAE inter-comparisons in the Tasman and Coral Seas 11Volume 5 No 2 August 2012 Journal of Operational Oceanography  

E-print Network

Oke is a Research Scientist at the Commonwealth Scientific and Industrial Research Organisation (CSIRO. Based on these results and other practical considerations the adoption of multi- model consensus

Oke, Peter

42

Southern Ocean seasonal temperature and Subtropical Front movement on the South Tasman Rise in the late Quaternary  

Microsoft Academic Search

The Subtropical Front (STF) marking the northern boundary of the Southern Ocean has a steep gradient in sea surface temperature (SST) of approximately 4°C over 0.5° of latitude. Presently, in the region south of Tasmania, the STF lies nominally at 47°S in the summer and 45°S in the winter. We present here SST reconstructions in a latitudinal transect of cores

E. L. Sikes; W. R. Howard; C. R. Samson; T. S. Mahan; L. G. Robertson; J. K. Volkman

2009-01-01

43

Introduction of online adaptive radiotherapy for bladder cancer through a multicentre clinical trial (Trans-Tasman Radiation Oncology Group 10.01): Lessons learned  

PubMed Central

Online adaptive radiotherapy for bladder cancer is a novel radiotherapy technique that was found feasible in a pilot study at a single academic institution. In September 2010 this technique was opened as a multicenter study through the Trans-Tasman Radiation Oncology Group (TROG 10.01 bladder online adaptive radiotherapy treatment). Twelve centers across Australia and New-Zealand registered interest into the trial. A multidisciplinary team of radiation oncologists, radiation therapists and medical physicists represented the trial credentialing and technical support team. To provide timely activation and proper implementation of the adaptive technique the following key areas were addressed at each site: Staff education/training; Practical image guided radiotherapy assessment; provision of help desk and feedback. The trial credentialing process involved face-to-face training and technical problem solving via full day site visits. A dedicated “help-desk” team was developed to provide support for the clinical trial. 26% of the workload occurred at the credentialing period while the remaining 74% came post-center activation. The workload was made up of the following key areas; protocol clarification (36%), technical problems (46%) while staff training was less than 10%. Clinical trial credentialing is important to minimizing trial deviations. It should not only focus on site activation quality assurance but also provide ongoing education and technical support. PMID:23776308

Pham, Daniel; Roxby, Paul; Kron, Tomas; Rolfo, Aldo; Foroudi, Farshad

2013-01-01

44

Sea Education Association (SEA)  

NSDL National Science Digital Library

The Sea Education Association (SEA) in Woods Hole, MA provides undergraduates with an opportunity to participate in an academic study-abroad program called the SEA Semester. The program combines intensive research in the areas of oceanography, maritime studies, and nautical science with hands-on experience aboard a traditional sailing ship. Piloting, celestial navigation, and practical seamanship are learned together with oceanographic sampling techniques and marine laboratory procedures. Critical thinking, problem-solving, team-building and leadership skills are emphasized throughout the program. SEA Semester is appropriate for students in marine biology, geology and physical science, environmental studies, American studies, and most other areas within the liberal arts and sciences. Academic credit for SEA Semester is obtained through Boston University.

45

Sea Turtles  

NSDL National Science Digital Library

Sea World informational resource on all eight species of sea turtles. Excellent introduction to sea turtles including information on their classification, habitat, diet, reproduction, and much more. Includes photographs and illustrations throughout. Features two teaching activities for grades K-2.

46

Red Sea  

Atmospheric Science Data Center

article title:  The Red Sea     View Larger Image ... Multi-angle Imaging SpectroRadiometer (MISR) image of the Red Sea was acquired on August 13, 2000. Located between the East African coast ... the Red Sea got its name because the blooms of a type of algae,  Trichodesmium erythraeum , found in the sea turn reddish-brown when ...

2013-04-16

47

SEA TURTLES Sea Turtles  

E-print Network

in the United States are currently listed either as endangered or threatened under the Endangered Species Act, Malaysia Hawksbill Endangered Hawaii 1Status under the Endangered Species Act (ESA). 2Sea turtles in the U the world's oceans. Of the seven species found worldwide, six are found in U.S. waters and include

48

Sea urchin  

NSDL National Science Digital Library

The sea urchin is a type of echinoderm. It is a consumer because it cannot make its own food and must eat other organisms to get energy. Sea urchins are omnivores, meaning they eat both plants and other animals to gain energy. Sea urchins have been known to eat algae, mussels, and sponges.

N/A N/A (NOAA; Channel Islands National Marine Sanctuary)

2004-12-23

49

Sea Stars  

NSDL National Science Digital Library

At first glance, starfish, more properly called sea stars, aren’t doing much of anything. In this video, Jonathan’s investigations reveal a slow-motion predator that hunts and attacks its prey. Traveling the world, Jonathan investigates sea stars from the tropics to the Antarctic and uses time-lapse photography to reveal an amazing complexity to the world of the sea star. Please see the accompanying study guide for educational objectives and discussion points.

2012-07-28

50

Sea Chest  

NSDL National Science Digital Library

By exploring life at sea for sailors and passengers, the Maritime Museum of San Diego offers insight into the history of maritime exploration, emigration, and commerce. Background and classroom activities are applicable to history, geography, social studies, science, art and other subjects. Emphasis on 19th Century sea travel and sailing ships, with topics including navigation techniques and technology, sailor's crafts, health and medicine at sea, shipboard life and social interactions.

51

Sea Turtles  

NSDL National Science Digital Library

In Malaysia there is an island known for more sea turtles than virtually anywhere on Earth. In this video, Jonathan visits this amazing ecosystem to learn about the life cycle of sea turtles. He is surprised to discover an amazingly complex and competitive environment. Please see the accompanying study guide for educational objectives and discussion points.

2012-07-26

52

Sea turtles  

Microsoft Academic Search

odern sea turtles are an important component of a wide range of tropical, temperate, and cold water marine ecosystems . Their inclusion on various lists of endangered specie s reflects past over-exploitation and the current need for better management . Today, seven or eight species of sea turtles are recognised, in two families and six genera. Adults typically migrate between

Catherine M. F. Lohmann; Kenneth J. Lohmann

2006-01-01

53

Sea Level  

NSDL National Science Digital Library

This problem provides an opportunity to increase familiarity with negative and positive numbers on a number line. The vertical number line is presented as black markings every one meter all the way up a lighthouse and on the underwater support going down to the sea bed, with sea level being "0". In answering the nine questions, children begin to calculate with negative numbers in the context of the distances between the sea creatures. The Teachers' Notes page offers suggestions for implementation, discussion questions, ideas for extension and support, and a link to a related resource, Swimming Pool (cataloged separately).

54

Sea Legs  

NASA Astrophysics Data System (ADS)

Forty-foot, storm-swept seas, Spitzbergen polar bears roaming vast expanses of Arctic ice, furtive exchanges of forbidden manuscripts in Cold War Moscow, the New York city fashion scene, diving in mini-subs to the sea floor hot srings, life with the astronauts, romance and heartbreak, and invading the last bastions of male exclusivity: all are present in this fast-moving, non-fiction account of one woman' fascinating adventures in the world of marine geology and oceanography.

Macdonald, Kenneth C.

55

Student Experiments at Sea (SEAS)  

NSDL National Science Digital Library

Interdisciplinary curriculum introduces the scientific process, experimental design and data analysis. Units on plate tectonics, hydrothermal vents, ridge visualization, surveying deep sea organisms. Students become the scientists, developing proposals for at-sea investigations, teacher coordinates submission to researchers studying the East Pacific Rise. Students retrieve, organize, analyze and report data from their experiment. Past experimental journals are posted. Free registration required to access curriculum and submit proposal.

56

Sea level trends in South East Asian Seas (SEAS)  

NASA Astrophysics Data System (ADS)

Southeast Asian Seas (SEAS) span the largest archipelago in the global ocean and provide a complex oceanic pathway connecting the Pacific and Indian Oceans. The SEAS regional sea level trends are some of the highest observed in the modern satellite altimeter record that now spans almost two decades. Initial comparisons of global sea level reconstructions find that 17 year sea level trends over the past 60 years exhibit good agreement in areas and at times of strong signal to noise associated decadal variability forced by low frequency variations in Pacific trade winds. The SEAS region exhibits sea level trends that vary dramatically over the studied time period. This historical variation suggests that the strong regional sea level trends observed during the modern satellite altimeter record will abate as trade winds fluctuate on decadal and longer time scales. Furthermore, after removing the contribution of the Pacific Decadal Oscillation (PDO) to sea level trends in the past twenty years, the rate of sea level rise is greatly reduced in the SEAS region. As a result of the influence of the PDO, the SEAS regional sea level trends during 2010s and 2020s are likely to be less than the global mean sea level (GMSL) trend if the observed oscillations in wind forcing and sea level persist. Nevertheless, long-term sea level trends in the SEAS will continue to be affected by GMSL rise occurring now and in the future.

Strassburg, M. W.; Hamlington, B. D.; Leben, R. R.; Manurung, P.; Lumban Gaol, J.; Nababan, B.; Vignudelli, S.; Kim, K.-Y.

2014-10-01

57

Limited Chemotherapy and Shrinking Field Radiotherapy for Osteolymphoma (Primary Bone Lymphoma): Results From the Trans-Tasman Radiation Oncology Group 99.04 and Australasian Leukaemia and Lymphoma Group LY02 Prospective Trial;Bone; Lymphoma; Radiotherapy; Chemotherapy; Clinical trial  

SciTech Connect

Purpose: To establish benchmark outcomes for combined modality treatment to be used in future prospective studies of osteolymphoma (primary bone lymphoma). Methods and Materials: In 1999, the Trans-Tasman Radiation Oncology Group (TROG) invited the Australasian Leukemia and Lymphoma Group (ALLG) to collaborate on a prospective study of limited chemotherapy and radiotherapy for osteolymphoma. The treatment was designed to maintain efficacy but limit the risk of subsequent pathological fractures. Patient assessment included both functional imaging and isotope bone scanning. Treatment included three cycles of CHOP chemotherapy and radiation to a dose of 45 Gy in 25 fractions using a shrinking field technique. Results: The trial closed because of slow accrual after 33 patients had been entered. Accrual was noted to slow down after Rituximab became readily available in Australia. After a median follow-up of 4.3 years, the five-year overall survival and local control rates are estimated at 90% and 72% respectively. Three patients had fractures at presentation that persisted after treatment, one with recurrent lymphoma. Conclusions: Relatively high rates of survival were achieved but the number of local failures suggests that the dose of radiotherapy should remain higher than it is for other types of lymphoma. Disability after treatment due to pathological fracture was not seen.

Christie, David, E-mail: david.christie@premion.com.au [Premion and Bond University, Gold Coast, Queensland (Australia); Dear, Keith [Department of Epidemiology and Population Studies, Australian National University, Canberra, New South Wales (Australia); Le, Thai [BHB, Premion, Brisbane, Queensland (Australia); Barton, Michael [Collaboration for Cancer Outcomes and Research (CCORE) and University of NSW, Sydney, New South Wales (Australia); Wirth, Andrew [Peter MacCallum Cancer Institute, Melbourne, Victoria (Australia); Porter, David [Auckland Hospital, Auckland (New Zealand); Roos, Daniel [Royal Adelaide Hospital, Adelaide, South Australia (Australia); Pratt, Gary [Royal Brisbane Hospital, Brisbane, Queensland (Australia)

2011-07-15

58

Savage Seas  

NSDL National Science Digital Library

This companion site to the new PBS series offers a collection of informative pieces and activities centered around the world's oceans. The site is divided into four principal sections, each of which features an article, brief sidebars, video clips, and in some cases, animations. The first, The Captain's Bridge, explores shipwrecks, stormy seas, and ocean rescues. The second, The Crow's Nest, dives into the power of waves. The Deep Sea section takes users to the nether regions of the ocean, while The Weather Factory touches on cyclones, ice and icebergs, and El Nino. Additional features at the site include Ask the Expert, Facts from the Sea, an annotated collection of related sites, and information about the series.

59

Sea Ice  

NASA Technical Reports Server (NTRS)

During 2013, Arctic sea ice extent remained well below normal, but the September 2013 minimum extent was substantially higher than the record-breaking minimum in 2012. Nonetheless, the minimum was still much lower than normal and the long-term trend Arctic September extent is -13.7 per decade relative to the 1981-2010 average. The less extreme conditions this year compared to 2012 were due to cooler temperatures and wind patterns that favored retention of ice through the summer. Sea ice thickness and volume remained near record-low levels, though indications are of slightly thicker ice compared to the record low of 2012.

Perovich, D.; Gerland, S.; Hendricks, S.; Meier, Walter N.; Nicolaus, M.; Richter-Menge, J.; Tschudi, M.

2013-01-01

60

Sea Launch  

NSDL National Science Digital Library

Sea Launch is an international satellite launch service company that has a unique way of delivering payloads into space. With the launch platform situated on the equator in the middle of the Pacific Ocean, a specially designed rocket propels satellites into orbit with very good accuracy. The Sea Launch home page has plenty of information about its operation, including an overview of the technology, statistics about its successes and failures, and Webcasts of many of its launches. A 200+ page user's guide goes into detail about all the various stages of a mission; everything from design considerations for the spacecraft to transportation to the launch site is mentioned in the document.

61

Aral Sea  

NASA Technical Reports Server (NTRS)

This series of MODIS images shows the dwindling Aral Sea. Once one of the world's largest freshwater lakes, the Aral Sea has decreased by as much as 60% over the past few decades due to diversion of the water to grow cotton and rice. These diversion have dropped the lake levels, increased salinity, and nearly decimated the fishing industry. The previous extent of the lake is clearly visible as a whitish perimeter in these image from April 16, May 18, and June 3, 2002. s. Credit: Jacques Descloitres, MODIS Land Rapid Response Team, NASA/GSFC

2002-01-01

62

Sea ice in the China Sea  

SciTech Connect

In every winter, sea ice occurring in Bohai Sea and the North Yellow Sea is the first-year ice which is going through generating, developing and thawing processes. Therefore, it is necessary to spatially and temporally describe ice period, freezing range, thickness variations and general motion of sea ice. The purpose of this paper is to provide initial general situation and features of sea ice for forecasting and researching sea ice.

Deng Shuqi [National Research Center for Marine Environmental Forecasts, Beijing (China)

1993-12-31

63

Aral Sea  

Atmospheric Science Data Center

... The retreating shoreline leaves the surface encrusted with salt and with agrochemicals brought in by the rivers. As the Sea's moderating ... Large Aral, and may be associated with windblown snow and/or salt particles carried aloft. The Multi-angle Imaging SpectroRadiometer ...

2013-04-16

64

From Sea to Shining Sea  

ERIC Educational Resources Information Center

Deep down in the depths of the sea, beautiful fish, mysterious ocean life, and unusual plants glimmer and glow in the eerie atmosphere of an ever-changing ocean. This article describes how, with this vision and a purpose in mind, three teachers pulled open classroom walls and joined forces so their second graders could create a mammoth 30 x 75"…

Scott, Beverly

2005-01-01

65

A Paired, Double-Blind, Randomized Comparison of a Moisturizing Durable Barrier Cream to 10% Glycerine Cream in the Prophylactic Management of Postmastectomy Irradiation Skin Care: Trans Tasman Radiation Oncology Group (TROG) 04.01  

SciTech Connect

Purpose: A previous, unblinded study demonstrated that an alcohol-free barrier film containing an acrylate terpolymer (ATP) was effective in reducing skin reactions compared with a 10% glycerine cream (sorbolene). The different appearances of these products precluded a blinded comparison. To test the acrylate terpolymer principle in a double-blinded manner required the use of an alternative cream formulation, a moisturizing durable barrier cream (MDBC); the study was conducted by the Trans Tasman Radiation Oncology Group (TROG) as protocol 04.01. Methods and Materials: A total of 333 patients were randomized; 1 patient was ineligible and 14 patients withdrew or had less than 7 weeks' observations, leaving 318 for analysis. The chest wall was divided into medial and lateral compartments, and patients were randomized to have MDBC applied daily to the medial or lateral compartment and sorbolene to the other compartment. Weekly observations, photographs, and symptom scores (pain and pruritus) were collected to week 12 or resolution of skin reactions if earlier. Skin dose was confirmed by centrally calibrated thermoluminescent dosimeters. Results: Rates of medial and lateral compartment Common Toxicity Criteria (CTC), version 3, greater than or equal to grade 3 skin reactions were 23% and 41%, but rates by skin care product were identical at 32%. There was no significant difference between MDBC and sorbolene in the primary endpoint of peak skin reactions or secondary endpoints of area-under-the-curve skin reaction scores. Conclusions: The MDBC did not reduce the peak skin reaction compared to sorbolene. It is possible that this is related to the difference in the formulation of the cream compared with the film formulation. Skin dosimetry verification and double blinding are essential for radiation skin care comparative studies.

Graham, Peter H., E-mail: peter.graham@sesiahs.health.nsw.gov.au [Cancer Care Centre, St. George Hospital, Kogarah, New South Wales (Australia); Plant, Natalie; Graham, Jennifer L.; Browne, Lois [Cancer Care Centre, St. George Hospital, Kogarah, New South Wales (Australia)] [Cancer Care Centre, St. George Hospital, Kogarah, New South Wales (Australia); Borg, Martin [Department of Radiation Oncology, Royal Adelaide Hospital (Australia)] [Department of Radiation Oncology, Royal Adelaide Hospital (Australia); Capp, Anne [Department of Radiation Oncology, Mater Hospital, Newcastle, New South Wales (Australia)] [Department of Radiation Oncology, Mater Hospital, Newcastle, New South Wales (Australia); Delaney, Geoff P. [Cancer Care Centre, Liverpool Hospital, Liverpool, New South Wales (Australia)] [Cancer Care Centre, Liverpool Hospital, Liverpool, New South Wales (Australia); Harvey, Jennifer [Mater Hospital, South Brisbane, Queensland (Australia)] [Mater Hospital, South Brisbane, Queensland (Australia); Kenny, Lisbeth [Royal Brisbane Hospital, Herston, Queensland (Australia)] [Royal Brisbane Hospital, Herston, Queensland (Australia); Francis, Michael [Andrew Love Cancer Centre, Geelong (Australia)] [Andrew Love Cancer Centre, Geelong (Australia); Zissiadis, Yvonne [Department of Radiation Oncology, Royal Perth Hospital, Perth (Australia)] [Department of Radiation Oncology, Royal Perth Hospital, Perth (Australia)

2013-05-01

66

Sea Ice  

NSDL National Science Digital Library

In this resource, students will discover that there are notable differences between sea ice and fresh-water ice, such as density. In on segment, students learn that the first sign of freezing on the sea is an oily appearance of the water caused by the formation of needle-like crystals. The site explains the relationship between growth and the rate at which heat flows from the water and that the ice pack can alter its shape and dimension due to the movement of winds, currents, thermal expansion, and contraction of the ice. Types of ice described here include new ice, nilas, young ice, first-year ice, and old ice while the forms of ice covered include pancake ice, brash ice, ice cake, floe, and fast ice. The site also explains the meteorological and oceanographic factors that control the amount and movement of ice.

67

Sea World  

NSDL National Science Digital Library

Excellent resource for information and teaching activities on marine life, designed primarily for elementary level. Teachers can sign up for a monthly e-newsletter (or access archived newsletters) filled with classroom activities, current information, and special links. Also features a searchable database of Sea World education materials and information on camps, marine science careers, and Shamu TV, an award-winning series broadcast around the country via satellite and cable.

68

Sea Cucumbers  

NSDL National Science Digital Library

What reef animal comes in a rainbow of crazy colors, can throw out its innards to immobilize predators, then creep away and regrow a brand-new stomach? It’s the sea cucumber, prized as a gastronomic delight by some cultures and beginning to yield some of its secrets to scientists. Follow host Ari Daniel Shapiro from a Chinatown market to the reefs of Fiji to learn more about this amazing creature. Also included is a Learn More section that provides background information on the scientists recorded in the podcast, lessons, images, and cool facts.

2009-01-01

69

Mammals of the Sea.  

ERIC Educational Resources Information Center

Presents information on sea mammals, including definitions and characteristics of cetaceans, pinnipeds, and sirenians. Contains descriptions of the teaching activities "Whale Music,""Draw A Whale to Scale,""Adopt a Sea Mammal," and "Sea Mammal Sleuths." (TW)

Naturescope, 1986

1986-01-01

70

Tracking Sea Otters  

USGS Multimedia Gallery

USGS sea otter researcher Tim Tinker drives the boat on an expedition to track and observe sea otters in Monterey Bay, California. USGS scientists study sea otters in efforts to help the threatened species continue to recover from near extinction....

71

Studying Sea Otters  

USGS Multimedia Gallery

Sea otter researcher Michelle Staedler, of the Monterey Bay Aquarium, records sea otter behavior in her logbook as part of a study with the USGS and the University of California at Santa Cruz on sea otter behavior. ...

72

Sea Ice  

NASA Technical Reports Server (NTRS)

Sea ice covers vast areas of the polar oceans, with ice extent in the Northern Hemisphere ranging from approximately 7 x 10(exp 6) sq km in September to approximately 15 x 10(exp 6) sq km in March and ice extent in the Southern Hemisphere ranging from approximately 3 x 10(exp 6) sq km in February to approximately 18 x 10(exp 6) sq km in September. These ice covers have major impacts on the atmosphere, oceans, and ecosystems of the polar regions, and so as changes occur in them there are potential widespread consequences. Satellite data reveal considerable interannual variability in both polar sea ice covers, and many studies suggest possible connections between the ice and various oscillations within the climate system, such as the Arctic Oscillation, North Atlantic Oscillation, and Antarctic Oscillation, or Southern Annular Mode. Nonetheless, statistically significant long-term trends are also apparent, including overall trends of decreased ice coverage in the Arctic and increased ice coverage in the Antarctic from late 1978 through the end of 2003, with the Antarctic ice increases following marked decreases in the Antarctic ice during the 1970s. For a detailed picture of the seasonally varying ice cover at the start of the 21st century, this chapter includes ice concentration maps for each month of 2001 for both the Arctic and the Antarctic, as well as an overview of what the satellite record has revealed about the two polar ice covers from the 1970s through 2003.

Parkinson, Claire L.; Cavalieri, Donald J.

2005-01-01

73

A Critical Evaluation of High TEX86-derived Sea Surface Temperatures from the Early Eocene  

NASA Astrophysics Data System (ADS)

The application of glycerol dialkyl glycerol tetraether (GDGT) based sea surface temperature proxies (eg TEX-86) has brought about major advances in our understanding of Cenozoic climate. However, TEX-86 approaches yield high temperatures at high latitudes during the EECO, and the resulting low latitudinal temperature gradients challenge our understanding of the physical climate system. We examine existing Paleogene TEX-86 data using three approaches. First, we have compared TEX-86 SST estimates to those derived from oxygen isotopes or Mg/Ca ratios of co-occurring well-preserved planktonic foraminifera. This reveals a strong correlation between foraminiferal SSTs and those obtained from linear TEX-86 calibrations, but the latter are systematically 4-6°C warmer. SSTs derived from non-linear TEX-86 calibrations are similar to inorganic SST estimates at high temperatures, but an offset still persists at lower temperatures. We have also compared TEX-86 SST estimates from marginal settings to associated continental mean air temperatures (MAT) derived from soil bacterial GDGTs (the MBT/CBT index). Again, the two approaches exhibit a strong correlation but with the former yielding 4-6°C warmer temperatures. Second, we have developed SST records from New Zealand, in order to place the EECO SSTs into a longer-term Paleogene context. Our temperature estimates indicate that sea floor and sea surface temperatures increased by ~10°C from late Paleocene to early Eocene times. Late Paleocene TEX-86-derived SSTs for the Canterbury Basin range from 18 to 23°C, consistent with coeval TEX-86 records from the Campbell Plateau and south Tasman Sea. During the EECO, TEX-86 derived SSTs from the Canterbury Basin and south Tasman Sea indicate tropical conditions, with temperatures peaking at 30-32°C at 50 Ma and then declining to 24-26°C into the Middle Eocene. MBT/CBT-derived MATs broadly parallel the SST trends, albeit with slightly lower values. These records suggest that elevated high southern latitude SSTs are reproducible at multiple sites and do document the relative long-term Paleogene climate evolution recorded by benthic foraminifera and inferred from faunal and floral assemblages. Combined, these two lines of evidence indicate that high latitude EECO temperatures were indeed significantly higher than those of today, but they also suggest that the specific estimates could be as much as 4-6°C too warm. There are multiple explanations for this, but one possibility is an oceanographic and/or ecological control on the GDGT assemblages exported to sediments. To explore this, we have directly examined the entirety of the NZ GDGT distributions. This approach indicates that high southern latitude GDGT distributions from the EECO are similar to those from the tropics today, providing further evidence for elevated temperatures. However, Paleocene sediments with markedly different GDGT distributions yield similar TEX-86 SSTs, due to the multi-component nature of the proxy. Thus, interpretations derived from GDGT distributions should be done cautiously and take into account the oceanographic context of the study site.

Pancost, R. D.; Taylor, K. W.; Handley, L.; Huber, M.; Hollis, C. J.

2011-12-01

74

California Sea Grant 1 California Sea Grant  

E-print Network

California Sea Grant 1 California Sea Grant Strategic Plan 2010­2013 #12;2 Strategic Plan 2010­2013 The National Sea Grant College Program, U.S. Department of Commerce, National Oceanic and Atmospheric Administration, supported this publication under NOAA grant number NA08OAR4170669, project number C/P-1 through

Jaffe, Jules

75

Colorful Underwater Sea Creatures  

ERIC Educational Resources Information Center

In this article, the author describes a project wherein students created colorful underwater sea creatures. This project began with a discussion about underwater sea creatures and how they live. The first step was making the multi-colored tissue paper that would become sea creatures and seaweed. Once students had the shapes of their sea creatures…

McCutcheon, Heather

2011-01-01

76

Beaufort Sea: information update  

SciTech Connect

The report is based on a multi-disciplinary meeting held March 6-7, 1985, as part of preparations for the Beaufort Sea Sale 97. The chapters are based on presentations given: The causeway effect: Modification of nearshore thermal regime resulting from causeways; Summertime sea ice intrusions in the Chukchi Sea; The deepwater limit of ice gouging on the Beaufort Sea shelf; Distribution, abundance, migration, harvest, and stock identity of Belukha Whales in the Beaufort Sea; Ringed seals in the Beaufort Sea; Beaufort Sea socioeconomics; The Baffin Island Oil Spill, (BIOS) Project.

Becker, P.R.

1988-04-01

77

Pronounced zonal heterogeneity in Eocene southern high-latitude sea surface temperatures.  

PubMed

Paleoclimate studies suggest that increased global warmth during the Eocene epoch was greatly amplified at high latitudes, a state that climate models cannot fully reproduce. However, proxy estimates of Eocene near-Antarctic sea surface temperatures (SSTs) have produced widely divergent results at similar latitudes, with SSTs above 20 °C in the southwest Pacific contrasting with SSTs between 5 and 15 °C in the South Atlantic. Validation of this zonal temperature difference has been impeded by uncertainties inherent to the individual paleotemperature proxies applied at these sites. Here, we present multiproxy data from Seymour Island, near the Antarctic Peninsula, that provides well-constrained evidence for annual SSTs of 10-17 °C (1? SD) during the middle and late Eocene. Comparison of the same paleotemperature proxy at Seymour Island and at the East Tasman Plateau indicate the presence of a large and consistent middle-to-late Eocene SST gradient of ?7 °C between these two sites located at similar paleolatitudes. Intermediate-complexity climate model simulations suggest that enhanced oceanic heat transport in the South Pacific, driven by deep-water formation in the Ross Sea, was largely responsible for the observed SST gradient. These results indicate that very warm SSTs, in excess of 18 °C, did not extend uniformly across the Eocene southern high latitudes, and suggest that thermohaline circulation may partially control the distribution of high-latitude ocean temperatures in greenhouse climates. The pronounced zonal SST heterogeneity evident in the Eocene cautions against inferring past meridional temperature gradients using spatially limited data within given latitudinal bands. PMID:24753570

Douglas, Peter M J; Affek, Hagit P; Ivany, Linda C; Houben, Alexander J P; Sijp, Willem P; Sluijs, Appy; Schouten, Stefan; Pagani, Mark

2014-05-01

78

Sea Turtle Conservancy  

NSDL National Science Digital Library

The Caribbean Conservation Corporation (CCC) was founded in 1959 by sea turtle champions such as ecologist Dr. Archie Carr, who served as the CCC's Scientific Director for nearly three decades. As the oldest sea turtle organization on the globe, the CCC "works to enact protective laws and establish refuges for the preservation of sea turtle habitats and coastal environments." The CCC created the Sea Turtle Survival League (STSL) in 1993 "as a public education and advocacy program to begin addressing the threats that face U.S. sea turtle populations." The CCC & STSL website contains information about a number of sea turtle programs and projects, tracking sea turtles, different sea turtle species, and ways to become a sea turtle conservationist. CCC also offers a public discussion board, a variety of downloadable publications (including activities for kids), and a collection of related links.

79

Sea Surface Temperatures  

NSDL National Science Digital Library

Users can search for and view sea surface temperature imagery. They may choose from the latest image, or browse archived imagery that dates back approximately two weeks. Links to other sea surface temperature datasets are included.

1999-10-30

80

Sea Turtle Populations  

NSDL National Science Digital Library

In this activity, learners will model how a sea turtle population changes over time, from eggs to adults, using puffed rice. Learners create a chart, calculate population fluctuation for each transitional stage of sea turtles' lives, and graph the population at each stage. Learners investigate different factors including migration and human fishing that affect the size of the sea turtle population. Relates to the linked video, DragonflyTV GPS: Sea Turtles.

Twin Cities Public Television, Inc.

2007-01-01

81

Sea Education Association  

NSDL National Science Digital Library

Headquartered in Woods Hole, Massachusetts, SEA offers a variety of science programs at sea for high school and college students. Site features information on the vessels, the crew, current voyages, admissions information, and a wealth of photographs from past expeditions. Also includes a section where you can track the progress of the SEA boats and hear daily, and archived, audio reports.

82

Tracking Sea Otters  

USGS Multimedia Gallery

Sea otter researchers Michelle Staedler, Monterey Bay Aquarium, and Tim Tinker, USGS, work together to locate sea otters in their study project. USGS scientists and their partners study sea otters in efforts to help the threatened species continue to recover from near extinction....

83

Alaska: Beaufort Sea  

Atmospheric Science Data Center

... Imaging SpectroRadiometer (MISR), illustrate different methods that may be used to assess sea ice type. Sea ice in the Beaufort Sea ... scattering. The MISR map at right was generated using a statistical classification routine (called ISODATA) and analyzed using ice ...

2014-05-15

84

All That Unplowed Sea  

ERIC Educational Resources Information Center

Hunting and gathering at sea may fast be approaching their productive limits. Aquaculture - farming at sea - linked to conservation represents the sea's promise. If the system works, it might prove to be the key to supplying large amounts of food and fresh water at no cost in nonrenewable energy resources. (BT)

MOSAIC, 1975

1975-01-01

85

Deep-Sea Technology  

NSDL National Science Digital Library

In this lesson plan students will learn about special vehicles used in recent Black Sea research and the theory that the Black Sea during the Ice Age was an isolated freshwater lake surrounded by farmland that was eventually flooded. Students will describe the purpose of the research vehicles by writing newspaper articles pretending they have just returned from the Black Sea expedition.

86

Sea Level Rise  

NSDL National Science Digital Library

In this activity, students will learn the difference between sea ice and glaciers in relation to sea level rise. They will create and explore topographic maps as a means of studying sea level rise and how it will affect Alaska's coastline.

Geophysical Institute of University of Fairbanks

87

Plate-tectonic setting of the Tasmanian region  

Microsoft Academic Search

The South Tasman Rise is a large submarine plateau of continental origin, located south of Tasmania. In the light of satellite?derived gravity data and shipboard swath?bathymetry and magnetic data collected in 1994 in the South Tasman Rise region, this paper re?examines the sea?floor spreading history of the surrounding ocean basins (northeastern Australian?Antarctic Basin and southwestern Tasman Sea). This information is

N. Rollet

1997-01-01

88

Dust Storm, Aral Sea  

NASA Technical Reports Server (NTRS)

The Aral Sea has shrunk to less than half its size since 1985. The Aral Sea receives little water (sometimes no water) from the two major rivers that empty into it-the Syr Darya and Amu Darya. Instead, the river water is diverted to support irrigation for the region's extensive cotton fields. Recently, water scarcity has increased due to a prolonged drought in Central Asia. As the Aral Sea recedes, its former sea bed is exposed. The Aral's sea bed is composed of fine sediments-including fertilizers and other agricultural chemicals-that are easily picked up by the region's strong winds, creating thick dust storms. The International Space Station crew observed and recorded a large dust storm blowing eastward from the Aral Sea in late June 2001. This image illustrates the strong coupling between human activities (water diversions and irrigation), and rapidly changing land, sea and atmospheric processes-the winds blow across the

2002-01-01

89

Sea level extremes in the Caribbean Sea  

NASA Astrophysics Data System (ADS)

Sea level extremes in the Caribbean Sea are analyzed on the basis of hourly records from 13 tide gauges. The largest sea level extreme observed is 83 cm at Port Spain. The largest nontidal residual in the records is 76 cm, forced by a category 5 hurricane. Storm surges in the Caribbean are primarily caused by tropical storms and stationary cold fronts intruding the basin. However, the seasonal signal and mesoscale eddies also contribute to the creation of extremes. The five stations that have more than 20 years of data show significant trends in the extremes suggesting that flooding events are expected to become more frequent in the future. The observed trends in extremes are caused by mean sea level rise. There is no evidence of secular changes in the storm activity. Sea level return periods have also been estimated. In the south Colombian Basin, where large hurricane-induced surges are rare, stable estimates can be obtained with 30 years of data or more. For the north of the basin, where large hurricane-induced surges are more frequent, at least 40 years of data are required. This suggests that the present data set is not sufficiently long for robust estimates of return periods. ENSO variability correlates with the nontidal extremes, indicating a reduction of the storm activity during positive ENSO events. The period with the highest extremes is around October, when the various sea level contributors' maxima coincide.

Torres, R. Ricardo; Tsimplis, Michael N.

2014-08-01

90

THE SEALS, SEA-LIONS, AND SEA OTTER OF  

E-print Network

THE SEALS, SEA-LIONS, AND SEA OTTER OF THE PACIFIC COAST Marine Biological Laboratory OODS HOLE, SEA-LIONS, AND SEA OTTER OF THE PACIFIC COAST Descriptions, Life History Notes, Photographs, and sea otter of the Pacific from Mexico to Point Barrow and the Hawaiian Islands. For each of twelve

91

Sea Ice Variability in the Bering Sea  

NASA Astrophysics Data System (ADS)

The Bering Sea consists of a shallow continental shelf in the northeast and a deep basin in the southwest. Sea ice in the Bering Sea concentrating in the shelf region exhibits large seasonal and interannual variations, which significantly impact the local marine ecosystem. Understanding of the physical mechanisms governing this sea-ice variability, however, remains incomplete. To better understand regional sea-ice variability we use a fine resolution (1/10-degree) global ocean and sea-ice model and available observations. The simulation consists of the Los Alamos National Laboratory Parallel Ocean Program (POP) and CICE models, and was run with Coordinated Ocean-ice Reference Experiment (CORE2) interannually varying atmospheric forcing for 1970-1989. Here we analyze 1980-1989; the first 10 years are treated as the spin-up period. We examine the partitioning of the ice volume tendencies into thermodynamic and dynamic components, as well as corresponding surface atmospheric and oceanic variables, in order to understand the relationship between sea ice variability and varying atmospheric and oceanic conditions. Focusing on the seasonal cycle first, we find that sea ice is mainly formed in the northern Bering Sea with the maximum ice growth rate occurring along the coast. Winds cause sea ice to drift southwestward from the north to the western ice edge. Along the ice edge, ice is melted by warm waters carried by the Bering Slope Current, especially in the west in winter; while in fall and spring, basal melting of sea ice spreads into the interior of ice pack. The ice growth rate is larger in winter than in fall and spring. Ice transport from the north to the southwest becomes weaker in fall and spring than in winter. The Bering Sea is ice free in summer. Surface melting is insignificant in all seasons. The interannual variability of sea ice in the Bering Sea can be largely explained by thermodynamics on the large scale. The dynamic ice transport, however, is often important locally, especially around the ice margins with ocean and land. Local dynamic and thermodynamic ice volume changes usually have opposite signs with similar magnitudes, implying a negative feedback between them. Through the surface heat flux budget, we find that sensible heat flux dominates the surface heat exchange with the atmosphere, which controls the ice growth in the north. Ocean-ice heat flux largely determines the basal melting along the ice edge in the south. Through the force balance analysis, we find that the ice motion is in steady state on the monthly timescale. Ice velocity correlates well with the wind stress, which is nearly balanced by the opposite ocean stress. Internal ice stress is not substantial except near the land boundaries in the north.

Li, L.; Miller, A. J.; McClean, J.; Eisenman, I.; Hendershott, M.

2013-12-01

92

East Siberian Sea, Russia  

NASA Technical Reports Server (NTRS)

The winter sea ice in the east Siberian Sea is looking a bit like a cracked windshield in these true-color Moderate Resolution Imaging Spectroradiometer (MODIS) images from June 16 and 23, 2002. North of the thawing tundra, the sea ice takes on its cracked, bright blue appearance as it thins, which allows the reflection of the water to show through. Numerous still-frozen lakes dot the tundra. Credit: Jacques Descloitres, MODIS Land Rapid Response Team, NASA/GSFC

2002-01-01

93

Focus on Sea Otters  

NSDL National Science Digital Library

A Monterey Bay Aquarium website where you can learn about the biology and population recovery of sea otters. Features include the opportunity to "meet" the otters on exhibit at the aquarium and viewing them through the live otter cam. Many sea otter-related games, activities, and resources. Links to other fascinating exhibits at the Aquarium. Several downloadable videos available, each with their own enjoyable sea otter antics.

94

SeaWIFS Project  

NSDL National Science Digital Library

SeaWIFS (Sea-viewing Wide Field-of-view Sensor), a NASA project using satellites to collect ocean color data to quantify phytoplankton abundance. Provides background information on SeaWIFS project, technology and data. Teacher Resource section has: online presentation on how and why scientists study ocean color; Living Ocean Teacher's Guide with brief information on ocean color, carbon cycle and greenhouse gas effect; and, links to other websites with ocean color activities.

95

Sea Turtle Science  

NSDL National Science Digital Library

This packet includes background information, quick facts, links to additional sea turtle resources, and a classroom modeling activity that demonstrates population estimation, life history, and hatching success rates.

96

Marinobacter salarius sp. nov. and Marinobacter similis sp. nov., Isolated from Sea Water  

PubMed Central

Two non-pigmented, motile, Gram-negative marine bacteria designated R9SW1T and A3d10T were isolated from sea water samples collected from Chazhma Bay, Gulf of Peter the Great, Sea of Japan, Pacific Ocean, Russia and St. Kilda Beach, Port Phillip Bay, the Tasman Sea, Pacific Ocean, respectively. Both organisms were found to grow between 4°C and 40°C, between pH 6 to 9, and are moderately halophilic, tolerating up to 20% (w/v) NaCl. Both strains were found to be able to degrade Tween 40 and 80, but only strain R9SW1T was found to be able to degrade starch. The major fatty acids were characteristic for the genus Marinobacter including C16:0, C16:1?7c, C18:1?9c and C18:1?7c. The G+C content of the DNA for strains R9SW1T and A3d10T were determined to be 57.1 mol% and 57.6 mol%, respectively. The two new strains share 97.6% of their 16S rRNA gene sequences, with 82.3% similarity in the average nucleotide identity (ANI), 19.8% similarity in the in silico genome-to-genome distance (GGD), 68.1% similarity in the average amino acid identity (AAI) of all conserved protein-coding genes, and 31 of the Karlin's genomic signature dissimilarity. A phylogenetic analysis showed that R9SW1T clusters with M. algicola DG893T sharing 99.40%, and A3d10T clusters with M. sediminum R65T sharing 99.53% of 16S rRNA gene sequence similarities. The results of the genomic and polyphasic taxonomic study, including genomic, genetic, phenotypic, chemotaxonomic and phylogenetic analyses based on the 16S rRNA, gyrB and rpoD gene sequence similarities, the analysis of the protein profiles generated using MALDI-TOF mass spectrometry, and DNA-DNA relatedness data, indicated that strains R9SW1T and A3d10T represent two novel species of the genus Marinobacter. The names Marinobacter salarius sp. nov., with the type strain R9SW1T (?=? LMG 27497T ?=? JCM 19399T ?=? CIP 110588T ?=? KMM 7502T) and Marinobacter similis sp. nov., with the type strain A3d10T (?=? JCM 19398T ?=? CIP 110589T ?=? KMM 7501T), are proposed. PMID:25198502

Ng, Hooi Jun; López-Pérez, Mario; Webb, Hayden K.; Gomez, Daniela; Sawabe, Tomoo; Ryan, Jason; Vyssotski, Mikhail; Bizet, Chantal; Malherbe, François; Mikhailov, Valery V.; Crawford, Russell J.; Ivanova, Elena P.

2014-01-01

97

Pelagic sea snakes dehydrate at sea.  

PubMed

Secondarily marine vertebrates are thought to live independently of fresh water. Here, we demonstrate a paradigm shift for the widely distributed pelagic sea snake, Hydrophis (Pelamis) platurus, which dehydrates at sea and spends a significant part of its life in a dehydrated state corresponding to seasonal drought. Snakes that are captured following prolonged periods without rainfall have lower body water content, lower body condition and increased tendencies to drink fresh water than do snakes that are captured following seasonal periods of high rainfall. These animals do not drink seawater and must rehydrate by drinking from a freshwater lens that forms on the ocean surface during heavy precipitation. The new data based on field studies indicate unequivocally that this marine vertebrate dehydrates at sea where individuals may live in a dehydrated state for possibly six to seven months at a time. This information provides new insights for understanding water requirements of sea snakes, reasons for recent declines and extinctions of sea snakes and more accurate prediction for how changing patterns of precipitation might affect these and other secondarily marine vertebrates living in tropical oceans. PMID:24648228

Lillywhite, Harvey B; Sheehy, Coleman M; Brischoux, François; Grech, Alana

2014-05-01

98

Hawksbill Sea Turtle (Eretmochelys imbricata)  

USGS Multimedia Gallery

Hawksbill Sea Turtles (Eretmochelys imbricata), such as the one hiding here under a boulder, and Green Sea Turtles (Chelonia mydas) are occasionally seen in Hurricane Hole. Hawksbills feed mostly on sponges while Greens eat mostly sea grasses....

99

Aerial dispersal of biological material from Australia to New Zealand  

Microsoft Academic Search

New Zealand lies 2000 km across the Tasman Sea, southeast of Australia, in the path of prevailing westerly winds and thus is well sited for studies of long distance dispersal. The aerial transfer of biological material across the Tasman Sea from Australia to New Zealand is not well documented and evidence for this is reviewed. Plant Pathogens: Regular surveys have

R. C. Close; N. T. Moar; A. I. Tomlinson; A. D. Lowe

1978-01-01

100

Kara Sea radioactivity assessment  

Microsoft Academic Search

Investigations following five international expeditions to the Kara Sea have shown that no radiologically significant contamination has occurred outside of the dumping sites in Novaya Zemlya bays. Increased levels of radionuclides in sediment have only been observed in Abrosimov and Stepovoy Bays very close to dumped containers. Evaluations of radionuclide inventories in water and sediment of the open Kara Sea

Iolanda Osvath; Pavel P Povinec; Murdoch S Baxter

1999-01-01

101

Bering Sea Expedition  

NSDL National Science Digital Library

In this investigation learners research the effects of melting sea ice in the Bering Sea Ecosystem. They create research proposals to earn a place on the scientific research vessel Healy and present their findings and proposals to a Research Board committee.

Alaska Seas and Rivers Curriculum

102

Tracking Sea Otters  

USGS Multimedia Gallery

USGS wildlife biologist Alisha Kage holds out a VHF receiver, hoping to hear the tell-tale beep that helps her locate sea otters that are part of study to monitor and learn more about the species. USGS scientists study sea otters in efforts to help the threatened species continue to recover from nea...

103

Spotting Sea Otters  

USGS Multimedia Gallery

USGS wildlife biologist Alisha Kage looks through a telescope to help her locate and identify tagged sea otters, then records the otter's location for a study aimed at learning more about the species. USGS scientists study sea otters in efforts to help the threatened species continue to recover from...

104

Sea wave energy conversion  

Microsoft Academic Search

A fixed structure encloses a vertically spaced plurality of superimposed channels that are open at one end of the sea to receive deep sea waves approaching a shoreline. Each of the channels has an entrance ramp that slopes upwardly shorewardly to induce breaking of a wave at and over an apex of the ramp that merges into a shorewardly downwardly

Perkins; C. A. Jr

1978-01-01

105

Getting Your Sea Legs  

PubMed Central

Sea travel mandates changes in the control of the body. The process by which we adapt bodily control to life at sea is known as getting one's sea legs. We conducted the first experimental study of bodily control as maritime novices adapted to motion of a ship at sea. We evaluated postural activity (stance width, stance angle, and the kinematics of body sway) before and during a sea voyage. In addition, we evaluated the role of the visible horizon in the control of body sway. Finally, we related data on postural activity to two subjective experiences that are associated with sea travel; seasickness, and mal de debarquement. Our results revealed rapid changes in postural activity among novices at sea. Before the beginning of the voyage, the temporal dynamics of body sway differed among participants as a function of their (subsequent) severity of seasickness. Body sway measured at sea differed among participants as a function of their (subsequent) experience of mal de debarquement. We discuss implications of these results for general theories of the perception and control of bodily orientation, for the etiology of motion sickness, and for general phenomena of perceptual-motor adaptation and learning. PMID:23840560

Stoffregen, Thomas A.; Chen, Fu-Chen; Varlet, Manuel; Alcantara, Cristina; Bardy, Benoît G.

2013-01-01

106

Red sea drillings  

USGS Publications Warehouse

Recent drilling in the Red Sea has shown that much of the basin is underlain by evaporites of a similar age to that of evaporites found in the Mediterranean Sea. These evaporites and their structural positions indicate that other brine areas are present - and, indeed, several others have been discovered.

Ross, D.A.; Whitmarsh, R.B.; Ali, S.A.; Boudreaux, J.E.; Coleman, R.; Fleisher, R.L.; Girdler, R.; Manheim, F.; Matter, A.; Nigrini, C.; Stoffers, P.; Supko, P.R.

1973-01-01

107

Sea Level Viewer  

NSDL National Science Digital Library

Video and animations of sea level from NASA's Climate website. Since 1992, NASA and CNES have studied sea surface topography as a proxy for ocean temperatures. NASA Missions TOPEX/Poseidon, Jason 1 and Jason 2 have been useful in predicting major climate, weather, and geologic events including El Nino, La Nina, Hurricane Katrina, and the Indian Ocean Tsunami.

Randall Jackson

108

White Sea - Russia  

NASA Technical Reports Server (NTRS)

At bottom center of this true-color Moderate Resolution Imaging Spectroradiometer (MODIS) image from April 13, 2001, the White Sea in western Russia is becoming free of ice in its southern extent. Meanwhile, the blue-green waters along the coast of the peninsula jutting out into the Barents Sea to the northeast could be due to a phytoplankton bloom.

2002-01-01

109

Antarctica: Sea Ice  

NSDL National Science Digital Library

This video segment, adapted from a NOVA broadcast, shows how sea ice forms in the Southern Ocean around Antarctica and how its seasonal fluctuation dramatically changes the continent. The segment, two minutes thirty-five seconds in length, includes rare footage of the destruction of the British ship 'Endurance', trapped and crushed by sea ice in 1914.

110

Tracking Sea Turtles  

NSDL National Science Digital Library

Classroom activity introduces the biology of sea turtles, population status, human impacts. Focuses on Kemp's ridley (Lepidochelys kempii), smallest and more endangered of sea turtle species. This teacher's guide provides NOAA tracking data and instructions for students to follow the migration routes of six turtles in the Gulf of Mexico. Links to related activities using satellite data.

111

Sea Lion Skeleton - Skull  

NSDL National Science Digital Library

The carnivorous sea lion uses its sharp pointed teeth and large mouth to shred and tear its prey. The large nose and large eyes on either side of the skull help the sea lion to detect prey. The skull protects the brain from damage and injury.

Ketan Patel (California State University, Fullerton; Student, Biological Sciences)

2007-07-26

112

Sea Lion Skeleton - Nostrils  

NSDL National Science Digital Library

The carnivorous sea lion uses its sharp pointed teeth and large mouth to shred and tear its prey. The large nose and large eyes on either side of the skull help the sea lion to detect prey. The skull protects the brain from damage and injury.

Ketan Patel (California State University, Fullerton; Student, Biological Sciences)

2007-07-26

113

Black Sea in Bloom  

NASA Technical Reports Server (NTRS)

This true-color image shows bright, turquoise-colored swirls across the surface of the Black Sea, signifying the presence of a large phytoplankton bloom. Scientists have observed similar blooms recurring annually, roughly this same time of year. The Sea of Azov, which is the smaller body of water located just north of the Black Sea in this image, also shows a high level of biological activity currently ongoing. The brownish pixels in the Azov are probably sediments carried in from high waters upstream. This scene was acquired by the Sea-viewing Wide Field-of-view Sensor (SeaWiFS), flying aboard the OrbView-2 satellite, on May 4, 2002. According to the Black Sea Environment Programme's Marine Hydrophysical Institute, the Black Sea is 'one of the marine areas of the world most damaged by human activities.' The coastal zone around these Eastern European inland water bodies is densely populated-supporting a permanent population of roughly 16 million people and another 4 million tourists each year. Six countries border with the Black Sea, including Ukraine to the north, Russia and Georgia to the east, Turkey to the south, and Bulgaria and Romania to the west. Because it is isolated from the world's oceans, and because there is an extensive drainage network of rivers that empty into it, the Black Sea has a unique and delicate water balance which is very important for supporting its marine ecosystem. Of particular concern to scientists is the salinity, water level, and nutrient levels of the Black Sea's waters, all of which are, unfortunately, being impacted by human activities. Within the last three decades the combination of increased nutrient loads from human sources together with pollution and over-harvesting of fisheries has resulted in a sharp decline in water quality. Scientists from each of the Black Sea's bordering nations are currently working together to study the issues and formulate a joint, international strategy for saving this unique marine ecosystem. Working with a spirit of placing more emphasis on joint ownership of the Black Sea's resources, and less emphasis on blame, it is hoped that the cooperating countries can strike an effective balance between both enjoying and preserving the Black Sea. Image courtesy the SeaWiFS Project, NASA GSFC, and ORBIMAGE

2002-01-01

114

Sea Cucumbers (Holothuroidea)  

NSDL National Science Digital Library

This Report's Topic in Depth explores the world of sea cucumbers, or Holothuroidea, a diverse group of intriguing marine animals. The first site (1), from the Tree of Life Web Project, provides nice clear images of sea cucumbers and brief concise sections on Characteristics, The Orders of Holothuroidea, Fossil History, and Discussion of Phylogenetic Relationships. The second site (2), from the Charles Darwin Research Station, displays short answers to commonly asked questions about sea cucumbers like: What is their importance within the marine communities?; How do sea cucumbers reproduce?; and What is the potential environment impact of overexploiting sea cucumber populations? From Enchanted Learning, the third site (3) features a diagrammed print-out of a s ea cucumber along with short descriptions of Holothuroidea anatomy, diet, classification, and predators. Hosted by the Royal BC Museum, the fourth site (4) contains a brief research paper by curator Philip Lambert on taxonomy issues concerning sea cucumbers. The fifth site (5), developed by Richard Fox of Lander University, contains detailed instructions for a laboratory exercise with Sclerodactyla briareus, a species of sea cucumber. From MoonDragon's Health & Wellness website, the sixth site (6) contains a sea cucumber recipe and briefly discusses sea cucumber cuisine and health benefits. Hosted by the Secretariat of the Pacific Community, the seventh site (7) provides information about an international conference titled: Conservation of s ea cucumbers in Malaysia, their Taxonomy, Ecology and Trade. The site contains concluding remarks, abstracts from papers presented at the conference, and a list of email contacts for conference participants. The final (8) site from the Environmental News Network'features a short article about an Ecuadorian court upholding sea cucumber fishing limits in the Galapagos islands.

115

KILLER WHALES PURSUE SEA LIONS IN BERING SEA DRAMA  

E-print Network

KILLER WHALES PURSUE SEA LIONS IN BERING SEA DRAMA Jim Branson NMFS Fisheries Management Agent a pod of 7 killer whales ( rampus vectipinna) pursue a band of 20 to ~' 5 Steller sea lions (Eumetopias E of N from Bogoslof Island, a very large sea lion rookery. At the time, there were 9 SRTMs

116

SEAS Safety Program SEAS SAFETY PROGRAM 2012-2103  

E-print Network

Streeto · Biosafety Manager: Sid Paula · Laser Safety Officer: Xiaowei Yan · Radiation Safety: StephenSEAS Safety Program SEAS SAFETY PROGRAM 2012-2103 Program Structure and Responsibilities Dr. Anas Chalah #12;SEAS Safety Program SEAS Safety Program Structure We have developed a great model

117

Global sea level rise  

SciTech Connect

Published values for the long-term, global mean sea level rise determined from tide gauge records exhibit considerable scatter, from about 1 mm to 3 mm/yr. This disparity is not attributable to instrument error; long-term trends computed at adjacent sites often agree to within a few tenths of a millimeter per year. Instead, the differing estimates of global sea level rise appear to be in large part due to authors' using data from gauges located at convergent tectonic plate boundaries, where changes of land elevation give fictitious sea level trends. In addition, virtually all gauges undergo subsidence or uplift due to postglacial rebound (PGR) from the last deglaciation at a rate comparable to or greater than the secular rise of sea level. Modeling PGR by the ICE-3G model of Tushingham and Peltier (1991) and avoiding tide gauge records in areas of converging tectonic plates produces a highly consistent set of long sea level records. The value for mean sea level rise obtained from a global set of 21 such stations in nine oceanic regions with an average record length of 76 years during the period 1880-1980 is 1.8 mm/yr {plus minus} 0.1. This result provides confidence that carefully selected long tide gauge records measure the same underlying trend of sea level and that many old tide gauge records are of very high quality.

Douglas, B.C. (NOAA, Rockville, MD (USA))

1991-04-15

118

Arctic Sea Ice  

NSDL National Science Digital Library

In this activity, learners explore how the area of Arctic sea ice has changed over recent years. First, learners graph the area of Arctic sea ice over time from 1979 to 2007. Then, learners use this information to extrapolate what the area will be in 2018 and graph their predictions. In part two of the activity, learners make a flip book to simulate the sea changes they just graphed. This resource includes background information related to the Northwest Passage and questions for learners to answer after completing this activity.

Beverly L. Meier

2012-06-26

119

Is The Sea Level?  

NSDL National Science Digital Library

In this activity students will observe that the sea level changes and will hypothesize what causes this change. They will then check their hypothesis with a data set. Many students are surprised to learn that sea level is not the same everywhere on earth and that it changes with the seasons. The main cause of this change is the temperature change in the ocean - warmer waters are higher than colder waters. Students will discover this information as they complete the activity and then see if the temperature effect holds true on another data set showing temperature and sea height changes caused by the El Nino/Southern Oscillation (ENSO).

2007-12-12

120

Sea level variation  

NASA Technical Reports Server (NTRS)

Published values for the long-term, global mean sea level rise determined from tide gauge records range from about one to three mm per year. The scatter of the estimates appears to arise largely from the use of data from gauges located at convergent tectonic plate boundaries where changes of land elevation give fictitious sea level trends, and the effects of large interdecadal and longer sea level variations on short (less than 50+ years) or sappy records. In addition, virtually all gauges undergo subsidence or uplift due to isostatic rebound from the last deglaciation at a rate comparable to or greater than the secular rise of sea level. Modeling rebound by the ICE-3G model of Tushingham and Peltier (1990) and avoiding tide gauge records in areas of converging tectonic plates produces a highly consistent set of long sea level records. A global set of 21 such stations in nine oceanic regions with an average record length of 76 years during the period 1880-1980 yields the global sea level rise value 1.8 mm/year +/- 0.1. Greenhouse warming scenarios commonly forecast an additional acceleration of global sea level in the next 5 or 6+ decades in the range 0.1-0.2 mm/yr2. Because of the large power at low frequencies in the sea level spectrum, very long tide gauge records (75 years minimum) have been examined for past apparent sea level acceleration. For the 80-year period 1905-1985, 23 essentially complete tide gauge records in 10 geographic groups are available for analysis. These yielded the apparent global acceleration -0.011 (+/- 0.012) mm/yr2. A larger, less uniform set of 37 records in the same 10 groups with 92 years average length covering the 141 years from 1850-1991 gave 0.001 (+/- 0.008) mm/yr2. Thus there is no evidence for an apparent acceleration in the past 100+ years that is significant either statistically, or in comparison to values associated with global warming. Unfortunately, the large interdecadal fluctuations of sea level severely affect estimates of global sea level acceleration for time spans of less than about 50 years. This means that tide gauges alone cannot serve as a reliable leading indicator of climate change in less than many decades. This time required can be significantly reduced if the interdecadal fluctuations of sea level can be understood in terms of their forcing mechanisms, and then removed from the tide gauge records.

Douglas, Bruce C.

1992-01-01

121

Sea Level: On The Rise  

NSDL National Science Digital Library

Learners will understand the relationship between climate change and sea-level rise. In the first activity, they will learn that heated water causes sea level to rise through a process called thermal expansion. They will also perform an experiment to learn that melting land-based ice contributes to greater sea-level rise than melting sea ice.

2013-11-26

122

A Sea Experience.  

ERIC Educational Resources Information Center

Described is a teacher education program organized by the Sea Education Association in Woods Hole (Massachusetts). The experience, including activities and examples of studies conducted, is discussed. Contact information for future cruises is included. (CW)

Glickstein, Neil

1989-01-01

123

Dead Sea Scrolls  

NASA Technical Reports Server (NTRS)

A consortium of researchers from Jet Propulsion Laboratory and three other organizations used charged coupled devices (CCDs) and other imaging enhancement technology to decipher previously unreadable portions of the Dead Sea Scrolls. The technique has potentially important implications for archeology.

1994-01-01

124

Sea level change  

SciTech Connect

The IPCC (Intergovernmental Panel on Climate Change) 1995 Scientific Assessment, Chapter 7. Sea Level Change, presents a modest revision of the similar chapter in the 1990 Assessment. Principal conclusions on observed sea-level change and the principal terms in the sea-level equation (ocean thermal expansion, glaciers, ice sheets, and land hydrology), including our knowledge of the present-day (defined as the 20th Century) components of sea-level rise, and projections of these for the future, are presented here. Some of the interesting glaciological problems which are involved in these studies are discussed in more detail. The emphasis here is on trends over decades to a century, not on shorter variations nor on those of the geologic past. Unfortunately, some of the IPCC projections had not been agreed at the time of writing of this paper, and these projections will not be given here. 15 refs., 2 figs.

Meier, M.F. [Univ. of Colorado, Boulder, CO (United States)

1996-12-31

125

Purple sea urchin swarm  

NSDL National Science Digital Library

Sea urchins live in low tide regions and eat seaweed. Urchins have no arms but have five rows of tube feet for movement. They are found in holes and use their spines for protection and to burrow into the rocks.

Katie Hale (California State University, Fullerton; Student, Biological Sciences)

2007-01-04

126

Sea Floor Spreading I  

NSDL National Science Digital Library

In this introductory Excel tutorial (Activity I) students use Excel to explore the geodynamics model equation for ocean depth around a sea-floor spreading center. For students with no prior Excel experience.

Activity and Starting Point page by R.M. MacKay. Clark College, Physics and Meteorology.

127

Record Sea Ice Minimum  

NASA Technical Reports Server (NTRS)

Arctic sea ice reached a record low in September 2007, below the previous record set in 2005 and substantially below the long-term average. This image shows the Arctic as observed by the Advanced Microwave Scanning Radiometer for EOS (AMSR-E) aboard NASA's Aqua satellite on September 16, 2007. In this image, blue indicates open water, white indicates high sea ice concentration, and turquoise indicates loosely packed sea ice. The black circle at the North Pole results from an absence of data as the satellite does not make observations that far north. Three contour lines appear on this image. The red line is the 2007 minimum, as of September 15, about the same time the record low was reached, and it almost exactly fits the sea ice observed by AMSR-E. The green line indicates the 2005 minimum, the previous record low. The yellow line indicates the median minimum from 1979 to 2000.

2007-01-01

128

Sea ice ecosystems.  

PubMed

Polar sea ice is one of the largest ecosystems on Earth. The liquid brine fraction of the ice matrix is home to a diverse array of organisms, ranging from tiny archaea to larger fish and invertebrates. These organisms can tolerate high brine salinity and low temperature but do best when conditions are milder. Thriving ice algal communities, generally dominated by diatoms, live at the ice/water interface and in recently flooded surface and interior layers, especially during spring, when temperatures begin to rise. Although protists dominate the sea ice biomass, heterotrophic bacteria are also abundant. The sea ice ecosystem provides food for a host of animals, with crustaceans being the most conspicuous. Uneaten organic matter from the ice sinks through the water column and feeds benthic ecosystems. As sea ice extent declines, ice algae likely contribute a shrinking fraction of the total amount of organic matter produced in polar waters. PMID:24015900

Arrigo, Kevin R

2014-01-01

129

Sea Ice Ecosystems  

NASA Astrophysics Data System (ADS)

Polar sea ice is one of the largest ecosystems on Earth. The liquid brine fraction of the ice matrix is home to a diverse array of organisms, ranging from tiny archaea to larger fish and invertebrates. These organisms can tolerate high brine salinity and low temperature but do best when conditions are milder. Thriving ice algal communities, generally dominated by diatoms, live at the ice/water interface and in recently flooded surface and interior layers, especially during spring, when temperatures begin to rise. Although protists dominate the sea ice biomass, heterotrophic bacteria are also abundant. The sea ice ecosystem provides food for a host of animals, with crustaceans being the most conspicuous. Uneaten organic matter from the ice sinks through the water column and feeds benthic ecosystems. As sea ice extent declines, ice algae likely contribute a shrinking fraction of the total amount of organic matter produced in polar waters.

Arrigo, Kevin R.

2014-01-01

130

Sensing the sea bed  

NASA Astrophysics Data System (ADS)

William Wilcock and a team of scientists and engineers drilled holes in the sea floor, and inadvertently provided a breeding ground for octopuses, in their attempt to understand deep-ocean hydrothermal venting.

2009-07-01

131

Smart Sea Lions  

NSDL National Science Digital Library

This video segment adapted from NOVA scienceNOW explores whether animals and humans are more similar than we think. Meet Rio, a sea lion who demonstrates to researchers reasoning skills once thought limited to humans.

2009-08-27

132

Science at Sea.  

ERIC Educational Resources Information Center

Describes a three-week inservice teacher education program that involves two sessions of preparatory classes ashore in nautical science and oceanography, and concludes with a nine-day sea voyage. (ASK)

Phillips, Mary Nied

2001-01-01

133

Stellar Sea Lion Research  

NSDL National Science Digital Library

The phenomenon is the decline in population of western Stellar Sea Lions from 1969 to 1986, shown in a series of three images. The accompanying text describes the possible factors that may be contributing to the change in population.

134

South China Sea.  

PubMed

The South China Sea is poorly understood in terms of its marine biota, ecology and the human impacts upon it. What is known is most often contained in reports and workshop and conference documents that are not available to the wider scientific community. The South China Sea has an area of some 3.3 million km2 and depths range from the shallowest coastal fringe to 5377 m in the Manila Trench. It is also studded with numerous islets, atolls and reefs many of which are just awash at low tide. It is largely confined within the Tropic of Cancer and, therefore, experiences a monsoonal climate being influenced by the Southwest Monsoon in summer and the Northeast Monsoon in winter. The South China Sea is a marginal sea and, therefore, largely surrounded by land. Countries that have a major influence on and claims to the sea include China, Malaysia, the Philippines and Vietnam, although Thailand, Indonesia and Taiwan have some too. The coastal fringes of the South China Sea are home to about 270 million people that have had some of the fastest developing and most vibrant economies on the globe. Consequently, anthropogenic impacts, such as over-exploitation of resources and pollution, are anticipated to be huge although, in reality, relatively little is known about them. The Indo-West Pacific biogeographic province, at the centre of which the South China Sea lies, is probably the world's most diverse shallow-water marine area. Of three major nearshore habitat types, i.e., coral reefs, mangroves and seagrasses, 45 mangrove species out of a global total of 51, most of the currently recognised 70 coral genera and 20 of 50 known seagrass species have been recorded from the South China Sea. The island groups of the South China Sea are all disputed and sovereignty is claimed over them by a number of countries. Conflicts have in recent decades arisen over them because of perceived national rights. It is perhaps because of this that so little research has been undertaken on the South China Sea. What data are available, however, and if Hong Kong is used, as it is herein, as an indicator of what the perturbations of other regional cities upon the South China Sea are like, then it is impacted grossly and an ecological disaster has probably already, but unknowingly, happened. PMID:11827109

Morton, B; Blackmore, G

2001-12-01

135

Black Sea Becomes Turquoise  

NASA Technical Reports Server (NTRS)

This true-color image shows bright, turquoise-colored swirls across the surface of the Black Sea, signifying the presence of a large phytoplankton bloom. Scientists have observed similar blooms recurring annually, roughly this same time of year. The Sea of Azov, which is the smaller body of water located just north of the Black Sea in this image, also shows a high level of color variance. The brownish pixels in the Azov are probably due to sediments carried in from high waters and snowmelt from upstream. This scene was acquired by the Moderate Resolution Imaging Spectroradiometer, flying aboard NASA's Terra satellite, on May 14, 2002. According to the Black Sea Environment Programme's Marine Hydrophysical Institute, the Black Sea is ?one of the marine areas of the world most damaged by human activities.? The coastal zone around these Eastern European inland water bodies is densely populated'supporting a permanent population of roughly 16 million people and another 4 million tourists each year. Six countries border with the Black Sea, including Ukraine to the north, Russia and Georgia to the east, Turkey to the south, and Bulgaria and Romania to the west. Because it is isolated from the world's oceans, and because there is an extensive drainage network of rivers that empty into it, the Black Sea has a unique and delicate water balance which is very important for supporting its marine ecosystem. Of particular concern to scientists is the salinity, water level, and nutrient levels of the Black Sea's waters, all of which are, unfortunately, being impacted by human activities. Within the last three decades the combination of increased nutrient loads from human sources together with pollution and over-harvesting of fisheries has resulted in a sharp decline in water quality. Scientists from each of the Black Sea's bordering nations are currently working together to study the issues and formulate a joint, international strategy for saving this unique marine ecosystem. Working with a spirit of placing more emphasis on joint ownership of the Black Sea's resources, and less emphasis on blame, it is hoped that the cooperating countries can strike an effective balance between both enjoying and preserving the Black Sea.

2002-01-01

136

Green Sea Turtles  

NSDL National Science Digital Library

Detailed information on the biology, natural history, factors influencing the population, and protection measures of green sea turtles (Chelonia mydas). Included are three in-class activities and one field activity all designed to raise awareness of the green sea turtle and what humans are doing to affect the population. The site is geared towards the Hawaiian sub-species, however, most of the facts and activities are applicable elsewhere.

137

National Sea Grant Library  

NSDL National Science Digital Library

Only facility housing complete collection of Sea Grant funded work. An archive and lending library for reprints, books, reports, maps, newsletters, handbooks, videos, CD-roms and computer programs regarding: oceanography; marine education; aquaculture; fisheries; limnology; coastal zone management; marine recreation and law. Lends documents worldwide, aiding scientists, teachers, students, fishermen and others in research and study. Bibliographic database is searchable from the website, obtain citations, abstracts and over 20,000 downloadable texts of Sea Grant publications.

138

Sea Urchin Embryology  

NSDL National Science Digital Library

Advanced high school level laboratory activities using sea urchins to observe fertilization and early developmental stages. This is a comprehensive site complete with multiple labs, support lessons, background information, animated graphics illustrating lab techniques, printable overheads (also available in Spanish and French), and a glossary of terms. A one-stop site for sea urchin information, experiments, suppliers, and research. Links to additional resources are available.

139

All About Sea Ice  

NSDL National Science Digital Library

This comprehensive site is an introduction to sea ice: what it is, how it forms, how it is studied, how it affected historical expedition in the polar regions, and what role it plays in the global climate. The site contains a glossary of sea ice terms and references to additional information, which all serve as an excellent introduction. Data are also available from various collection methods for student interpretation.

140

Sea Level rise contributors  

NSDL National Science Digital Library

This web page from the National Snow and Ice Data Center contains two related visualizations. The first visualization gives an estimate of the percent contribution to sea level change since the 1990s from three contributors - small glaciers and ice caps, the Greenland Ice Sheet and the Antarctic Ice Sheet. The second visualization shows the cumulative contribution to sea level from small glaciers and ice caps plotted with the annual global surface air temperature anomaly.

M.F. Meier

141

Contemporary sea level rise.  

PubMed

Measuring sea level change and understanding its causes has considerably improved in the recent years, essentially because new in situ and remote sensing observations have become available. Here we report on most recent results on contemporary sea level rise. We first present sea level observations from tide gauges over the twentieth century and from satellite altimetry since the early 1990s. We next discuss the most recent progress made in quantifying the processes causing sea level change on timescales ranging from years to decades, i.e., thermal expansion of the oceans, land ice mass loss, and land water-storage change. We show that for the 1993-2007 time span, the sum of climate-related contributions (2.85 +/- 0.35 mm year(-1)) is only slightly less than altimetry-based sea level rise (3.3 +/- 0.4 mm year(-1)): approximately 30% of the observed rate of rise is due to ocean thermal expansion and approximately 55% results from land ice melt. Recent acceleration in glacier melting and ice mass loss from the ice sheets increases the latter contribution up to 80% for the past five years. We also review the main causes of regional variability in sea level trends: The dominant contribution results from nonuniform changes in ocean thermal expansion. PMID:21141661

Cazenave, Anny; Llovel, William

2010-01-01

142

The White Sea, Russia  

NASA Technical Reports Server (NTRS)

Editor's Note: The caption below, published on May 10, 2001, is incorrect. According to Masha Vorontsova, director of the International Fund for Animal Welfare in Moscow, the situation with the seal pups in the White Sea is normal. There is no disaster and there never was. For more details, refer to the article entitled 'No Danger' on the New Scientist home page. The Earth Observatory regrets the earlier errant report. Original Caption According to the Russian Polar Research Institute for Fisheries and Oceanography, between 250,000 and 300,000 Greenland seal pups face death by starvation over the next two months due to a cruel trick by mother nature. The seals, most of them less than two months old, are trapped on ice sheets that remain locked in the White Sea, located near Archangel in Northern Russia. Typically, during the spring thaw the ice sheets break up and flow with the currents northward into the Barents Sea, the seals' spring feeding grounds. The seal pups hitch a ride on the ice floes, living on their own individual stores of fat until they arrive in the Barents Sea. Their mothers departed for the Barents Sea weeks ago. In a normal year, the seal pups' trip from the White Sea out to the Barents takes about six weeks and the seals have adapted to rely upon this mechanism of mother nature. During their yearly migration, the mother seals usually stay with their pups and feed them until their pelts turn from white to grey--a sign that the pups are mature enough to swim and feed themselves. Unfortunately, this year unusually strong northerly winds created a bottleneck of ice near the mouth of the white sea, thus blocking the flow of ice and trapping the pups. These true-color images of the White Sea were acquired by the Moderate-resolution Imaging Spectroradiometer (MODIS), flying aboard NASA's Terra spacecraft. This image, taken May 2, 2000 that there is usually much less ice in the White Sea this time of year as most of it is typically en route to the Barents Sea.

2002-01-01

143

The Dead Sea  

NASA Technical Reports Server (NTRS)

The Dead Sea is the lowest point on Earth at 418 meters below sea level, and also one of the saltiest bodies of water on Earth with a salinity of about 300 parts-per-thousand (nine times greater than ocean salinity). It is located on the border between Jordan and Israel, and is fed by the Jordan River. The Dead Sea is located in the Dead Sea Rift, formed as a result of the Arabian tectonic plate moving northward away from the African Plate. The mineral content of the Dead Sea is significantly different from that of ocean water, consisting of approximately 53% magnesium chloride, 37% potassium chloride and 8% sodium chloride. In the early part of the 20th century, the Dead Sea began to attract interest from chemists who deduced that the Sea was a natural deposit of potash and bromine. From the Dead Sea brine, Israel and Jordan produce 3.8 million tons potash, 200,000 tons elemental bromine, 45,000 tons caustic soda, 25, 000 tons magnesium metal, and sodium chloride. Both countries use extensive salt evaporation pans that have essentially diked the entire southern end of the Dead Sea.

With its 14 spectral bands from the visible to the thermal infrared wavelength region, and its high spatial resolution of 15 to 90 meters (about 50 to 300 feet), ASTER images Earth to map and monitor the changing surface of our planet.

ASTER is one of five Earth-observing instruments launched December 18, 1999, on NASA's Terra satellite. The instrument was built by Japan's Ministry of Economy, Trade and Industry. A joint U.S./Japan science team is responsible for validation and calibration of the instrument and the data products.

The broad spectral coverage and high spectral resolution of ASTER provides scientists in numerous disciplines with critical information for surface mapping, and monitoring of dynamic conditions and temporal change. Example applications are: monitoring glacial advances and retreats; monitoring potentially active volcanoes; identifying crop stress; determining cloud morphology and physical properties; wetlands evaluation; thermal pollution monitoring; coral reef degradation; surface temperature mapping of soils and geology; and measuring surface heat balance.

The U.S. science team is located at NASA's Jet Propulsion Laboratory, Pasadena, Calif. The Terra mission is part of NASA's Science Mission Directorate.

Size: 18.5 by 48.1 kilometers (11.5 by 29.8 miles) Location: 31.4 degrees North latitude, 35.4 degrees East longitude Orientation: North at top Image Data: ASTER bands 3, 2, and 1 Original Data Resolution: 15 meters (49.2 feet) Dates Acquired: May 3, 2005

2006-01-01

144

Bioprospecting / Deep Sea Research  

NSDL National Science Digital Library

The first portion of the radio broadcast discusses the relatively new field of bioprospecting, the exploration of the sea floor for novel compounds and processes that may have industrial or medical applications. Bioprospectors are trying to collect samples of deep-sea organisms which may yield new pharmaceutical compounds, as in the case of Conus magnus, a sea snail whose venom has yielded a painkiller 1000 times more potent than morphine. There is also discussion of who owns these resources and what can be done to protect them. This segment is 12 minutes in length. The second segment of the broadcast traces the history of undersea exploration, including methods of measuring ocean depth, the bathysphere used by William Beebe and Otis Barton, the modern Alvin submersible, and remotely operated vehicles. There is also discussion of the motives and inspiration for ocean exploration; the deep sea knowledge of whalers; and comparisons of deep sea research with space exploration. This segment is 34 minutes and 40 seconds in length.

145

Geology of Barents Sea  

SciTech Connect

The Barents Sea is situated on the continental shelf between Norway, the Spitsbergen Islands, and Novaya Zemlya. The main structural framework of the area was formed during the Caledonian and Hercynian orogenies, whereas the western parts were reactivated by the Kimmerian and Alpine orogenies. Because of the complex opening of the Greenland Norwegian Sea, important tertiary reactivation of Mesozoic normal faults occurred along southwest-northeast-trending systems of wrench faults. Owing to substantial erosion in the late Tertiary, the subsidence history and thermal development are more difficult to unravel in this area than in other places along the Norwegian Shelf. The erosion products were deposited in a huge sedimentary wedge extending onto the oceanic crust. The hydrocarbon discoveries in the Troms area in the southern part of the Barents Sea are encouraging for further exploration. However, the petroleum potential for large areas is not well known at this stage.

Riis, F.; Vollset, J.

1984-09-01

146

SeaWeb  

NSDL National Science Digital Library

SeaWeb is a nonprofit organization aimed at raising awareness of the ocean and marine life that play "a critical role in our everyday life and in the future of our planet." SeaWeb employs a team of professionals from biology, exploration, and various communication disciplines. The current campaigns include an effort to protect the declining Caspian Sea Sturgeon ("the source of most of the world's caviar"), an attempt to reduce overfishing of swordfish, and a report about the changes occurring in the world's oceans. This Web site is a robust source of information about many threats that are facing marine ecosystems, and an attempt to reduce the dangers by educating the public about the impacts of their behavior.

147

New York Sea Grant  

NSDL National Science Digital Library

The National Sea Grant program was established in 1966, and a few years later, the state of New York sponsored the program's first outpost. Currently, the New York Sea Grant (NYSG) is a cooperative program of the State University of New York (SUNY) and Cornell University. On the homepage, visitors can look over sections that include "Extension", "Research", "Education", "Publications", and "Theme Areas". The "Theme Areas" is a good place to start, as it features topical material on coastal processes and hazards, fisheries, and aquatic invasive species. Their helpful publication "Currents" is also worth a look, and it contains materials on grant opportunities, research materials, fact sheets, and public awareness programs. Moving on, the "Related Sites" area contains links to "Hot Topics" (topical news items related to the sea and such) and affiliated organizations.

148

Caribbean Sea Level Network  

NASA Astrophysics Data System (ADS)

Over the past 500 years almost 100 tsunamis have been observed in the Caribbean and Western Atlantic, with at least 3510 people having lost their lives to this hazard since 1842. Furthermore, with the dramatic increase in population and infrastructure along the Caribbean coasts, today, millions of coastal residents, workers and visitors are vulnerable to tsunamis. The UNESCO IOC Intergovernmental Coordination Group for Tsunamis and other Coastal Hazards for the Caribbean and Adjacent Regions (CARIBE EWS) was established in 2005 to coordinate and advance the regional tsunami warning system. The CARIBE EWS focuses on four areas/working groups: (1) Monitoring and Warning, (2) Hazard and Risk Assessment, (3) Communication and (4) Education, Preparedness and Readiness. The sea level monitoring component is under Working Group 1. Although in the current system, it's the seismic data and information that generate the initial tsunami bulletins, it is the data from deep ocean buoys (DARTS) and the coastal sea level gauges that are critical for the actual detection and forecasting of tsunamis impact. Despite multiple efforts and investments in the installation of sea level stations in the region, in 2004 there were only a handful of sea level stations operational in the region (Puerto Rico, US Virgin Islands, Bermuda, Bahamas). Over the past 5 years there has been a steady increase in the number of stations operating in the Caribbean region. As of mid 2012 there were 7 DARTS and 37 coastal gauges with additional ones being installed or funded. In order to reach the goal of 100 operational coastal sea level stations in the Caribbean, the CARIBE EWS recognizes also the importance of maintaining the current stations. For this, a trained workforce in the region for the installation, operation and data analysis and quality control is considered to be critical. Since 2008, three training courses have been offered to the sea level station operators and data analysts. Other requirements and factors have been considered for the sustainability of the stations. The sea level stations have to potentially sustain very aggressive conditions of not only tsunamis, but on a more regular basis, hurricanes. Given the requirement that the data be available in near real time, for tsunami and other coastal hazard application, robust communication systems are also essential. For the local operator, the ability to be able to visualize the data is critical and tools like the IOC Sea level Monitoring Facility and the Tide Tool program are very useful. It has also been emphasized the need for these stations to serve multiple purposes. For climate and other research applications the data need to be archived, QC'd and analyzed. Increasing the user base for the sea level data has also been seen as an important goal to gain the local buy in; local weather and meteorological offices are considered as key stakeholders but for whom applications still need to be developed. The CARIBE EWS continues to look forward to working with other IOC partners including the Global Sea Level Observing System (GLOSS) and Sub-Commission for the Caribbean and Adjacent Regions (IOCARIBE)/GOOS, as well as with local, national and global sea level station operators and agencies for the development of a sustainable sea level network.

von Hillebrandt-Andrade, C.; Crespo Jones, H.

2012-12-01

149

Understanding Sea Level Changes  

NASA Technical Reports Server (NTRS)

Today more than 100 million people worldwide live on coastlines within one meter of mean sea level; any short-term or long-term sea level change relative to vertical ground motion is of great societal and economic concern. As palm-environment and historical data have clearly indicated the existence and prevalence of such changes in the past, new scientific information regarding to the nature and causes and a prediction capability are of utmost importance for the future. The 10-20 cm global sea-level rise recorded over the last century has been broadly attributed to two effects: (1) the steric effect (thermal expansion and salinity-density compensation of sea water) following global climate; (2) mass-budget changes due to a number of competing geophysical and hydrological processes in the Earth-atmosphere-hydrosphere-cryosphere system, including water exchange from polar ice sheets and mountain glaciers to the ocean, atmospheric water vapor and land hydrological variations, and anthropogenic effects such as water impoundment in artificial reservoirs and extraction of groundwater, all superimposed on the vertical motions of solid Earth due to tectonics, rebound of the mantle from past and present deglaciation, and other local ground motions. As remote-sensing tools, a number of space geodetic measurements of sea surface topography (e.g., TOPEX/Poseidon, Jason), ice mass (e.g., ICESat), time-variable gravity (e.g. GRACE), and ground motions (SLR, VLBI, GPS, InSAR, Laser altimetry, etc.) become directly relevant. Understanding sea level changes "anywhere, anytime" in a well-defined terrestrial reference frame in terms of climate change and interactions among ice masses, oceans, and the solid Earth, and being able to predict them, emerge as one of the scientific challenges in the Solid Earth Science Working Group (SESWG, 2003) conclusions.

Chao, Benjamin F.

2004-01-01

150

RADIOCARBON RESERVOIR AGES IN THE MEDITERRANEAN SEA AND BLACK SEA  

Microsoft Academic Search

We measured apparent marine radiocarbon ages for the Mediterranean Sea, Black Sea, and Red Sea by accel- erator mass spectrometry radiocarbon analyses of 26 modern, pre-bomb mollusk shells collected living between AD 1837 and 1950. The marine reservoir (R(t)) ages were estimated at some 390 ± 85 yr BP, 415 ± 90 yr BP and 440 ± 40 yr BP,

Nadine Tisnerat; Franck Bassinot

151

Deep Drilling at Sea  

NSDL National Science Digital Library

This Science News for Kids article provides an image-rich overview of a deep-sea drilling project off the coast of British Columbia. The article guides students through the exploration, explaining how deep sediment cores are taken, what researchers find in the cores, and details of what life is like on a research ship. It features links to an online poll, an opportunity for students to submit comments, a deep-sea drilling word find, and links to supplementary reading questions and related sites.

Kate Ramsayer

152

Melting Sea Ice  

NSDL National Science Digital Library

This activity uses a mix of multimedia resources and hands-on activities to support a storyline of investigation into melting sea ice. The lesson begins with a group viewing of a video designed to get students to consider both the local and global effects of climate change. The class then divides into small groups for inquiry activities on related topics followed by a presentation of the findings to the entire class. A final class discussion reveals a more complex understanding of both the local and global impacts of melting sea ice.

WGBH Educational Foundation Teachers' Domain

153

Lighting Up the Sea  

NSDL National Science Digital Library

This National Geographic lesson plan explores bioluminescent organisms in the sea. In this activity, students explore the benefits of bioluminescence by conducting a simulation and viewing pictures of bioluminescent marine animals on the Web. The conclusion of the activity entails students pretending to be deep-sea divers and writing journal entries about their impressions of a bioluminescent animal they have encountered. In addition to a detailed procedure, the lesson plan includes suggestions for assessment, ideas for extending the lesson, and links to related websites.

National Geographic Xpeditions

154

Melting Sea Ice  

NSDL National Science Digital Library

This activity uses a mix of multimedia resources and hands-on activities to support a storyline of investigation into melting sea ice. The lesson begins with a group viewing of a video designed to get students to consider both the local and global effects of climate change. The class then divides into small groups for inquiry activities on related topics followed by a presentation of the findings to the entire class. A final class discussion reveals a more complex understanding of both the local and global impacts of melting sea ice.

2007-01-01

155

National Sea Grant Library  

NSDL National Science Digital Library

This is the website for the only facility housing a complete collection of Sea Grant funded work. An archive and lending library for reprints, books, reports, maps, newsletters, handbooks, videos, CD-roms and computer programs regarding: oceanography; marine education; aquaculture; fisheries; limnology; coastal zone management; marine recreation and law. Lends documents worldwide, aiding scientists, teachers, students, fishermen and others in research and study. Bibliographic database is searchable from the website, where users may obtain citations, abstracts and access to over 20,000 downloadable texts of Sea Grant publications.

156

Spectacled Eiders Wintering in Northern Bering Sea  

USGS Multimedia Gallery

Large flock of Spectacled Eiders aggregated in a sea ice lead and on sea ice in the northern Bering Sea, south of St. Lawrence Island, Alaska.  Aerial photograph from a helicopter deployed from the USCG Cutter Polar Sea....

157

Seafloor Control on Sea Ice  

NASA Technical Reports Server (NTRS)

The seafloor has a profound role in Arctic sea ice formation and seasonal evolution. Ocean bathymetry controls the distribution and mixing of warm and cold waters, which may originate from different sources, thereby dictating the pattern of sea ice on the ocean surface. Sea ice dynamics, forced by surface winds, are also guided by seafloor features in preferential directions. Here, satellite mapping of sea ice together with buoy measurements are used to reveal the bathymetric control on sea ice growth and dynamics. Bathymetric effects on sea ice formation are clearly observed in the conformation between sea ice patterns and bathymetric characteristics in the peripheral seas. Beyond local features, bathymetric control appears over extensive ice-prone regions across the Arctic Ocean. The large-scale conformation between bathymetry and patterns of different synoptic sea ice classes, including seasonal and perennial sea ice, is identified. An implication of the bathymetric influence is that the maximum extent of the total sea ice cover is relatively stable, as observed by scatterometer data in the decade of the 2000s, while the minimum ice extent has decreased drastically. Because of the geologic control, the sea ice cover can expand only as far as it reaches the seashore, the continental shelf break, or other pronounced bathymetric features in the peripheral seas. Since the seafloor does not change significantly for decades or centuries, sea ice patterns can be recurrent around certain bathymetric features, which, once identified, may help improve short-term forecast and seasonal outlook of the sea ice cover. Moreover, the seafloor can indirectly influence cloud cover by its control on sea ice distribution, which differentially modulates the latent heat flux through ice covered and open water areas.

Nghiem, S. V.; Clemente-Colon, P.; Rigor, I. G.; Hall, D. K.; Neumann, G.

2011-01-01

158

National Sea Grant Educators Network  

NSDL National Science Digital Library

Compilation of Sea Grant marine education resources. Site includes the latest news, a pdf file discussing Sea Grant education initiatives, links to all Sea Grant Education websites, several teaching and learning resources, and several interactive classroom activities. An excellent site to begin preparations for a marine science or oceanography course.

159

3, 637669, 2006 Mediterranean Sea  

E-print Network

OSD 3, 637­669, 2006 Central Mediterranean Sea forecast S. Natale et al. Title Page Abstract Mediterranean Sea forecast: effects of high-resolution atmospheric forcings S. Natale1 , R. Sorgente2 , S­669, 2006 Central Mediterranean Sea forecast S. Natale et al. Title Page Abstract Introduction Conclusions

Paris-Sud XI, Université de

160

Tides & Currents: Sea Level Trends  

NSDL National Science Digital Library

The Center for Operational Oceanographic Products and Services has been measuring sea level for over 150 years. This resource illustrates regional trends in sea level, with arrows representing the direction and magnitude of change including national and global stations. Impacts on changing sea levels in relation to atmospheric and oceanic processes as well as other Earth systems are explained and supported with educations resources.

2010-01-01

161

Sea Level : Frequently Asked Questions and Answers  

NSDL National Science Digital Library

Visitors can find answers to frequently asked questions regarding sea level and sea level changes. Topics addressed include how mean sea level is defined, how much sea level would rise if all the worlds ice were to melt, differences in sea level between oceans and at different latitudes, the meaning of altitude above sea level, and others.

2007-12-12

162

Steller Sea Lion  

NSDL National Science Digital Library

A comprehensive site featuring the threatened Steller Sea Lion. Site includes information on its critical habitat, protection measures, distribution information, and much more. Explore the Literature, Presentations, and Images section for an abundance of information from conferences, workshops, and research. Site features a wealth of photographs and video, as well as contact information for the program.

163

Sea Turtles Coloring Book  

NSDL National Science Digital Library

Using excellent line drawings, this coloring book provides great background information about sea turtles in both English and Spanish. Species profiles, biology and life cycle, ecology, distribution, uses and threats, like fishing and habitat destruction, are covered. Measures for protection and conservation are introduced.

164

Farming the Sea  

ERIC Educational Resources Information Center

Florida has initiated a training program in an entirely new dimension--Sea Farming. Presented is a description of the vocational agriculture program designed to teach propagation, cultivation, harvesting, marketing, and conservation practices related to production of oysters, shrimp, scallops, crabs, and fin fishes. (Editor/GB)

Morgan, William

1971-01-01

165

Labour Flexibilization at Sea  

Microsoft Academic Search

Cruise line employment of men and women contract seafarers from all over the world since the late twentieth century has produced what is called multinational or ‘mini UN’ crew on board large modern cruise ships. This phenomenon is encouraged by open ship registries that legally endorse and affirm the flexibilization of labour at sea. Labour flexibilization processes, however, are not

Christine B. N. Chin

2008-01-01

166

Redlands Institute: Salton Sea  

NSDL National Science Digital Library

The Salton Sea Database Program (SSDP) at the University of Redlands, Redlands Institute (RI) was a project administered by the U.S. Environmental Protection Agency (EPA), Center for Special Programs. The purpose behind the SSDP was to bring a wide range of data management and analysis tools and professionals "to support multi-disciplinary and coordinated decision-making across all the professional and scientific teams and stakeholders involved in the restoration of California's largest inland body of water, the Salton Sea." Part of their outreach work includes this fine website, which includes sections titled "Ecological Issues", "Data & Research", and "Exploring the Area". First-time visitors may want to start by clicking on the "Ecological Issues" area. Here they can learn about the science of the area, the contemporary issues facing the survival of the Salton Sea, and some of the proposed solutions to restore the Sea. Journalists and scientists will appreciate the "Data & Research" area, as it features digital maps of the area, GIS data, public policy documents, and an image database. The casual traveler will enjoy the "Exploring the Area" section, and here they will find information about current weather conditions, fishing reports, and California State park materials.

167

Solomon's Sea and [Pi  

ERIC Educational Resources Information Center

This paper is a whimsical survey of the various explanations which might account for the biblical passage in I Kings 7:23 that describes a round object--a bronze basin called Solomon's Sea--as having diameter ten cubits and circumference thirty cubits. Can the biblical pi be any number other than 3? We offer seven different perspectives on this…

Simoson, Andrew J.

2009-01-01

168

Whither Arctic Sea Ice?  

NSDL National Science Digital Library

In this activity students work with real datasets to investigate a real situation regarding disappearing Arctic sea ice. The case study has students working side-by-side with a scientist from the National Snow and Ice Data Center and an Inuit community in Manitoba.

Betsy Youngman

169

SeaDiscovery.com  

NSDL National Science Digital Library

SeaDiscovery.com is an online source for "underwater tech and ocean science news." The site presents not only news, but information about maritime technology employment which includes featured jobs and resumes. It also allows access to the Maritime Technology Reporter magazine and provides links to a number of important directories.

170

Classroom of the Sea  

NSDL National Science Digital Library

Although most students do not have the opportunity to conduct in situ research projects until college, the Classroom of the Sea program at the American School for the Deaf (ASD) provides an unusual opportunity for students to work directly with scientists

Denise Monte

2000-03-01

171

Sea Grant's Education Mission.  

ERIC Educational Resources Information Center

Considers the status of the education agenda of the Sea Grant Program as it turns 30. Projects described include Operation Pathfinder, which aims to educate minority teachers and/or teachers of minority students. Also described are a program in which seafood processors and resellers are trained in safety and health areas, and programs to train…

Sherman, Douglas

1998-01-01

172

Black Sea Battle  

NSDL National Science Digital Library

Story of the invasion of jellyfish into the Black Sea and the resulting affects on the native fish population. An excellent introduction into introduced species and their effects on an ecosystem. Site features an abundance of information on alien species and the delicacy that goes into eradicating them. Also links to additional non-traditional science-related news events.

173

Egyptian Sea Cave  

ERIC Educational Resources Information Center

This brief article describes an archaeological expedition to the Red Sea coast area of Egypt in 2004. Kathryn Bard, an associate professor of archaeology at Boston University, along with her team, discovered the well-preserved cedar timbers of an ancient Egyptian seafaring vessel near the entrance to a large man-made cave. Limestone tablets with…

Journal of College Science Teaching, 2005

2005-01-01

174

Solar Sea Power  

ERIC Educational Resources Information Center

In their preoccupation with highly complex new energy systems, scientists and statesmen may be overlooking the possibilities of Ocean Thermal Energy Conversion (OTEC). That is the view of a Carnegie-Mellon University physicist who is in the forefront of solar sea power investigation. (Author/BT)

Zener, Clarence

1976-01-01

175

Autophagy at sea.  

PubMed

The 3rd EMBO Conference on, "Autophagy: Molecular mechanism, physiology and pathology" organized by Anne Simonsen and Sharon Tooze, was held in May 2013 on a sea cruise along the Norwegian coastline from Bergen to Tromsø. Researchers from all corners of the world presented work covering autophagosome biogenesis, physiological regulation of autophagy, selective autophagy and disease. PMID:23917436

Martens, Sascha; Rusten, Tor Erik; Kraft, Claudine

2013-09-01

176

Under the Sea  

NSDL National Science Digital Library

This activity integrates art and science as students use books and other sources to learn more about the creatures that live in the ocean. Once they have learned about various sea creatures and their habitats, they will construct an undersea environment in their classroom.

177

Sea Surface Temperature Climatology  

NSDL National Science Digital Library

This interactive animation shows global sea surface temperature averages for the same months over a number of years. Click on the map to see values for a particular month. This takes leads to a viewer that allows users to manipulate the figure, zooming in to a particular spot, altering the size, or changing the format.

Earth Education Online

178

Harvesting the Sea.  

ERIC Educational Resources Information Center

Information on commercial fishing is provided, and a board game is described which requires students to watch for ocean signs of good fishing, choose equipment to catch specific types of fish, and consider effects of weather on working at sea. A reproducible copy of the game, with instructions, is included. (IAH)

Markle, Sandra

1989-01-01

179

Rising Sea Levels  

NSDL National Science Digital Library

In the past century, as the climate has warmed, sea level rise has accelerated. Scientists predict it will only increase, and they're studying changes in the ocean and land to better understand how and why the water is rising. "Changing Planet" is produced in partnership with the National Science Foundation.

NBC Learn

2010-10-07

180

Sea Level Viewer  

NSDL National Science Digital Library

This interactive program focuses on the role of sea level in climate change. Sections include an overview and a list of relevant NASA satellite missions and their objectives. A third section, entitled Global View, covers the following 5 topics: Latest View, Large El Niño, Hurricane Katrina, Indian Ocean Tsunami, and La Niña.

181

SeaWeb  

NSDL National Science Digital Library

A multimedia public education project designed to raise awareness of the world ocean and the life within it. Find articles on the latest ocean issues, links to resources and audio clips of the radio show Ocean Report. Also features information on SeaWeb programs, such as aquaculture initiatives for both fish and their eggs (caviar), and publications.

182

The Cosmonaut Sea Wedge  

USGS Publications Warehouse

A set of multi-channel seismic profiles (~15000 km) acquired by Russia, Norway and Australia has been used to investigate the depositional evolution of the Cosmonaut Sea margin of East Antarctica. We recognize a regional sediment wedge below the upper part of the continental rise. The wedge, herein termed the Cosmonaut Sea Wedge, is positioned stratigraphically underneath the inferred glaciomarine section and extends for at least 1200 km along the continental margin and from 80 to about 250 km seaward or to the north. Lateral variations in the growth pattern of the wedge indicate several overlapping depocentres, which at their distal northern end are flanked by elongated mounded drifts and contourite sheets. The internal stratification of the mounded drift deposits suggests that westward flowing bottom currents reworked the marginal deposits. The action of these currents together with sea-level changes is considered to have controlled the growth of the wedge. We interpret the Cosmonaut Sea Wedge as a composite feature comprising several bottom current reworked fan systems.

Solli, K.; Kuvaas, B.; Kristoffersen, Y.; Leitchenkov, G.; Guseva, J.; Gandyukhin, V.

2007-01-01

183

Modern sea power  

SciTech Connect

This book provides discussions of political, technical and military aspects of nuclear power. The contents include naval warfare in the nuclear age; politics, money, law and technology; a technological change; implications of technology; sea control; strategic deterrents; amphibious operations, maritime interdiction; inshore operations, naval diplomacy and conclusion.

Till, G.

1987-01-01

184

Sea Turtle Skeleton - Skull  

NSDL National Science Digital Library

The carnivorous sea turtle's skull has two eye sockets for good vision on each side along with nostrils to detect prey. It does not have teeth, but has sharp edges on its jaw to rip and tear food. The skull protects the brain from damage and injury.

Ketan Patel (California State University, Fullerton; Student, Biological Sciences)

2007-07-26

185

Sea Turtle Skeleton - Nostrils  

NSDL National Science Digital Library

The carnivorous sea turtle's skull has two eye sockets for good vision on each side along with nostrils to detect prey. It does not have teeth, but has sharp edges on its jaw to rip and tear food. The skull protects the brain from damage and injury.

Ketan Patel (California State University, Fullerton; Student, Biological Sciences)

2007-07-26

186

Sea Lion Skeleton - Backbone  

NSDL National Science Digital Library

Sea lions are vertebrates with both backbones and ribs. The backbone is a gliding joint, allowing the animal to be flexible, while the ribs main function is to protect it's inner organs. The short tail helps to balance the animal while walking on land.

Ketan Patel (California State University, Fullerton; Student, Biological Sciences)

2007-07-27

187

Sea Lion Skeleton - Ribcage  

NSDL National Science Digital Library

Sea lions are vertebrates with both backbones and ribs. The backbone is a gliding joint, allowing the animal to be flexible, while the ribs main function is to protect it's inner organs. The short tail helps to balance the animal while walking on land.

Ketan Patel (California State University, Fullerton; Student, Biological Sciences)

2007-07-15

188

The Weddell Sea  

NASA Technical Reports Server (NTRS)

Several large, irregularly shaped icebergs are floating in the Weddell Sea, east of the Antarctic Peninsula, in this true-color MODIS image from February 17, 2002. The location of several of the bergs has changed little over the last three months. Compared to an image acquired on November 13, 2001, the berg at the upper right of the image has spun around, but is still hanging around in the same general location. Similar slow-movers can be seen just to the east of the Larsen Ice Shelf, which hugs the eastern coast of the Peninsula. The northernmost of those two bergs is designated A38b; the southernmost one is A38a. These bergs were once part of an iceberg greater than 2,700 square miles that broke off the Ronne Ice Shelf (to the south) back in 1998. While the waters of the Weddell Sea in the area ought to be deep enough to float those bergs, it is possible that they have run aground on a topographic high, or ridge, in the sea floor. However, little is known about the underwater topography of that region, and it is also possible that the bergs are simply so massive that they resist being moved by surface wind or ocean currents. While four years might seem like a long time for an iceberg to hang around, these are certainly no record holders. A berg that broke off the Ross Ice Shelf (on the other side of Antarctica) drifted north and went aground south of Australia. That berg calved in 1987, and hasn't really moved in ten years. While the big bergs have not moved much in the span of time between these images, there is a big difference in the amount of sea ice present in the two images. In general, the rounder chunks of ice are more likely to be seasonal sea ice that forms from the freezing of sea water, while the larger, jagged-edged pieces of ice are more likely to be bergs that broke off an ice shelf at the margin of the continent. It's the height of summer in Antarctica in the February image, and much of the sea ice has melted or drifted away, leaving a relatively large expanse of clear ocean. Credit:

2002-01-01

189

Sea-Level Projections from the SeaRISE Initiative  

NASA Technical Reports Server (NTRS)

SeaRISE (Sea-level Response to Ice Sheet Evolution) is a community organized modeling effort, whose goal is to inform the fifth IPCC of the potential sea-level contribution from the Greenland and Antarctic ice sheets in the 21st and 22nd century. SeaRISE seeks to determine the most likely ice sheet response to imposed climatic forcing by initializing an ensemble of models with common datasets and applying the same forcing to each model. Sensitivity experiments were designed to quantify the sea-level rise associated with a change in: 1) surface mass balance, 2) basal lubrication, and 3) ocean induced basal melt. The range of responses, resulting from the multi-model approach, is interpreted as a proxy of uncertainty in our sea-level projections. http://websrv.cs .umt.edu/isis/index.php/SeaRISE_Assessment.

Nowicki, Sophie; Bindschadler, Robert

2011-01-01

190

Northern Sand Sea  

NASA Technical Reports Server (NTRS)

[figure removed for brevity, see original site]

Our topic for the weeks of April 4 and April 11 is dunes on Mars. We will look at the north polar sand sea and at isolated dune fields at lower latitudes. Sand seas on Earth are often called 'ergs,' an Arabic name for dune field. A sand sea differs from a dune field in two ways: 1) a sand sea has a large regional extent, and 2) the individual dunes are large in size and complex in form.

This VIS image was taken at 82 degrees North latitude during Northern spring. The image is completely dominated by dunes. In sand seas, it is very common for a single type of dune to occur, and for a single predominate wind to control the alignment of the dunes.

Image information: VIS instrument. Latitude 82.2, Longitude 152.5 East (207.5 West). 19 meter/pixel resolution.

Note: this THEMIS visual image has not been radiometrically nor geometrically calibrated for this preliminary release. An empirical correction has been performed to remove instrumental effects. A linear shift has been applied in the cross-track and down-track direction to approximate spacecraft and planetary motion. Fully calibrated and geometrically projected images will be released through the Planetary Data System in accordance with Project policies at a later time.

NASA's Jet Propulsion Laboratory manages the 2001 Mars Odyssey mission for NASA's Office of Space Science, Washington, D.C. The Thermal Emission Imaging System (THEMIS) was developed by Arizona State University, Tempe, in collaboration with Raytheon Santa Barbara Remote Sensing. The THEMIS investigation is led by Dr. Philip Christensen at Arizona State University. Lockheed Martin Astronautics, Denver, is the prime contractor for the Odyssey project, and developed and built the orbiter. Mission operations are conducted jointly from Lockheed Martin and from JPL, a division of the California Institute of Technology in Pasadena.

2005-01-01

191

Sea ice radiative forcing, sea ice area, and climate sensitivity  

NASA Astrophysics Data System (ADS)

Changes in sea ice cover affect climate sensitivity by modifying albedo and surface heat flux exchange, which in turn affect the absorbed solar radiation at the surface as well as cloud cover, atmospheric water content and poleward atmospheric heat transport. Here, we use a configuration of the Community Earth System Model 1.0.4 with a slab ocean model and a thermodynamic-dynamic sea ice model to investigate the overall net effect of feedbacks associated with the sea ice loss. We analyze the strength of the overall sea ice feedback in terms of two factors: the sensitivity of sea ice area to changes in temperature, and the sensitivity of sea ice radiative forcing to changes in sea ice area. In this model configuration, sea ice area decreases by ~3 × 1012 m2 per K of global warming, while the effective global radiative forcing per square meter of sea ice loss is ~0.1 × 10-12 W m-2. The product of these two terms (~0.3 W m-2 K-1) approximately equals the difference in climate feedback parameter found in simulations with sea ice response (1.05 W m-2 K-1) and simulations without sea ice response (1.31 W m-2 K-1 or 1.35 W m-2 K-1, depending on the method used to disable changes in sea ice cover). Thus, we find that in our model simulations, sea ice response accounts for about 20% to 22% of the climate sensitivity to an imposed change in radiative forcing. In our model, the additional radiative forcing resulting from a loss of all sea ice in the 'pre-industrial' state is comparable to but somewhat less than the radiative forcing from a doubling of atmospheric CO2 content.

Caldeira, Ken; Cvijanovic, Ivana

2014-05-01

192

North Sea Sediment Dynamics  

NASA Astrophysics Data System (ADS)

The North Sea is a semi-enclosed shelf sea attached to the North-east Atlantic and in its south-eastern part receives significant matter from river discharge and atmospheric deposition: Anthropogenic nutrients, dissolved carbon and organic compounds have elevated pristine background concentrations in the coastal strip of the North Sea since about 250 years as a consequence of intensified agriculture and industrialisation since then, In such a marine environment the legacy of old inputs and the influence of processes in the sediment on the biogeochemistry of the overlying water column increases with decreasing water depth. On the other hand the flux of particulate organic matter into the surface sediment (~15 cm depth) also increases with decreasing water depth or distance from the coast. Both effects are also described by results of ECOHAM-M simulations, the coupled pelagic-benthic ecosystem model that includes a prognostic multi-layer sediment module adopted from the global biogeochemical model HAMOCC as part of the MPI-earth-system model (MPI-ESM).The transfer from deep sea to coastal applications required different adaptations, such as changes in porosity values, in dissolution and organic matter remineralisation rates, and stoichiometries. In the model, two pelagic detritus pools, one slowly sinking with semi-labile organic matter, and one fast sinking with labile organic matter are collected in one sediment pool. After a spin-up of several hundred years the 3d-coupled model for the southern and central North Sea attains equilibrium, where the local inputs and outputs of the pelagic and benthic module are balanced. From this equilibrium state we initialised a realistic decadal run (2000-2009). Analysing the seasonal and interannual model results we found that the variability of sediment efflux in the model is low compared to the more dynamic pelagic system components, but simulated (and observed) sediment pore water profiles clearly show concentration gradients from the coast into the central North Sea. Data on organic matter concentration and quality in surface sediments along a comparable transect suggest that not only the loading with POM decreases with distance to land, but also the reactivity of organic matter, indicated by amino acid composition as a measure of the degree of protein degradation. This ageing or degradation effect can also be seen in a near-shore surface sediment core where the C/N ratio increases with depth, while the relative concentration of labile material in sedimentary organic matter decreases. We discuss how the quality of organic particulate matter could be integrated into the sediment model equations.

Paetsch, Johannes; Kuehn, Wilfried; Serna, Alexandra; Lahajnar, Niko; Emeis, Kay

2014-05-01

193

The North Sea - A shelf sea in the Anthropocene  

NASA Astrophysics Data System (ADS)

Global and regional change clearly affects the structure and functioning of ecosystems in shelf seas. However, complex interactions within the shelf seas hinder the identification and unambiguous attribution of observed changes to drivers. These include variability in the climate system, in ocean dynamics, in biogeochemistry, and in shelf sea resource exploitation in the widest sense by societies. Observational time series are commonly too short, and resolution, integration time, and complexity of models are often insufficient to unravel natural variability from anthropogenic perturbation. The North Sea is a shelf sea of the North Atlantic and is impacted by virtually all global and regional developments. Natural variability (from interannual to multidecadal time scales) as response to forcing in the North Atlantic is overlain by global trends (sea level, temperature, acidification) and alternating phases of direct human impacts and attempts to remedy those. Human intervention started some 1000 years ago (diking and associated loss of wetlands), expanded to near-coastal parts in the industrial revolution of the mid-19th century (river management, waste disposal in rivers), and greatly accelerated in the mid-1950s (eutrophication, pollution, fisheries). The North Sea is now a heavily regulated shelf sea, yet societal goals (good environmental status versus increased uses), demands for benefits and policies diverge increasingly. Likely, the southern North Sea will be re-zoned as riparian countries dedicate increasing sea space for offshore wind energy generation - with uncertain consequences for the system's environmental status. We review available observational and model data (predominantly from the southeastern North Sea region) to identify and describe effects of natural variability, of secular changes, and of human impacts on the North Sea ecosystem, and outline developments in the next decades in response to environmental legislation, and in response to increased use of shelf sea space.

Emeis, Kay-Christian; van Beusekom, Justus; Callies, Ulrich; Ebinghaus, Ralf; Kannen, Andreas; Kraus, Gerd; Kröncke, Ingrid; Lenhart, Hermann; Lorkowski, Ina; Matthias, Volker; Möllmann, Christian; Pätsch, Johannes; Scharfe, Mirco; Thomas, Helmuth; Weisse, Ralf; Zorita, Eduardo

2015-01-01

194

Tachyonic Dirac sea  

E-print Network

We consider a system of many fermions with tachyonic energy spectrum \\varepsilon_k=\\sqrt{k^2-m^2} and clarify that tachyons with imaginary energy and low momentum (ktachyon Fermi system and make contribution to the thermodynamical functions. The energy and pressure acquire additional constant terms that, however, is not reflected in the sound speed. Replacement $m=im$ results in the thermodynamical functions and the sound speed of an ordinary Fermi gas. When the Fermi momentum approaches the Dirac sea level k_F=m, the group velocity of most tachyons above the sea is unbound, while the sound speed tends to infinity. This scenario is not encountered in practice because the cold tachyon Fermi gas becomes unstable with respect to hydrodynamical perturbations when k_Ftachyon system is always finite and exceeds the critical value depending on the tachyon mass m.

Ernst Trojan

2012-04-03

195

Sea Ice 1987 - 2012  

NSDL National Science Digital Library

This site features a video that illustrates both seasonal patterns and long-term changes in sea ice distribution across the Arctic Ocean. It draws data from two satellite instruments that measure emitted microwave radiation, which helps distinguish open ocean from ice. It shows that during the winter months, a layer of ice forms across vast expanses of the Arctic Ocean and each summer, more than half of that ice vanishes. Students discover that this natural cycle of freezing and thawing is influenced both by seasonal temperature variations and long-term climate change and that scientists are using satellite images to measure the distribution of Arctic sea ice in order to gain a better understanding of how it is linked to Earth's climate system.

196

The Disappearing Aral Sea  

NSDL National Science Digital Library

In just 30 years, the Aral Sea has lost more than 60 percent of its water. Barring change, it may disappear entirely by 2020. In this visualization, satellite images dating from 1973 to 2000 show how water diverted from this inland lake for agriculture has caused it to shrink considerably over a short period of time. The feature can be run as an animation or as a series of slides. A background essay and discussion questions are included.

197

Salish Sea Expeditions  

NSDL National Science Digital Library

At-sea education program combines classroom study with shipboard science studies in Puget Sound, Washington. Offers spring programs for schools and home schoolers, summer programs for families and youngsters; expeditions of 1 to 5 days involve oceanographic sampling activities, navigation and sailing responsibilities aboard a 61-foot sailing vessel. Teachers can join a preview sail to evaluate; site provides details on water quality, plankton and other studies and equipment used.

198

WINDandSEA  

NSDL National Science Digital Library

Site was built in response to the many reference questions that are posed to the library and is meant to make internet searching more efficient for those concerned with oceanic and atmospheric issues, and the general public. Presently WINDandSEA has over 1,000 links to science and policy sites organized by topic and alphabetically within topic. All sites have been reviewed and annotated by NOAA staff.

199

Kara Sea radioactivity assessment.  

PubMed

Investigations following five international expeditions to the Kara Sea have shown that no radiologically significant contamination has occurred outside of the dumping sites in Novaya Zemlya bays. Increased levels of radionuclides in sediment have only been observed in Abrosimov and Stepovoy Bays very close to dumped containers. Evaluations of radionuclide inventories in water and sediment of the open Kara Sea and Novaya Zemlya bays as well as soil from the shore of Abrosimov bay have shown that radionuclide contamination of the open Kara Sea is mainly due to global fallout, with smaller contributions from the Sellafield reprocessing plant, the Chernobyl accident run-off from the Ob and Yenisey rivers and local fallout. Computer modelling results have shown that maximum annual doses of approximately 1 mSv are expected for a hypothetical critical group subsisting on fish caught in the Novaya Zemlya bays whereas populations living on the mainland can be expected to receive doses at least three orders of magnitude lower. PMID:10568274

Osvath, I; Povinec, P P; Baxter, M S

1999-09-30

200

Bering Sea in Bloom  

NASA Technical Reports Server (NTRS)

The surface waters of the Bering Sea around the Pribilof Islands, off Alaska's west coast, exhibited a dark green color on May 15, 2002, in this SeaWiFS true-color image. The green color of the currents there suggests the presence of a large phytoplankton bloom. Careful inspection reveals some a reddish tinges of light reflected by this bloom, particularly in a long east to west band just south of the Pribilof Islands, and just north of the Aleutian Island chain (disappearing toward the lower righthand corner of this scene beneath the cloud bank). Some scientists speculate this could be another Phaeocystis bloom, similar to the bloom of this species that was observed in these waters roughly this time last year. Such blooms are typically accompanied by a strong, unpleasant odor in the immediate vicinity. The light brown color of the surface waters along the Alaskan shoreline are probably due to suspended sediments washed off from the land. Image courtesy the SeaWiFS Project, NASA GSFC, and ORBIMAGE

2002-01-01

201

Curonian Spit, Baltic Sea  

NASA Technical Reports Server (NTRS)

On July 25, 2006, the Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER), flying on NASA's Terra satellite, captured this image of the Curonian (or Courland)spit, the Curonian Lagoon (also known as the Courland Lagoon) it encloses, and part of the Baltic Sea. Just 3,800 meters (about 12,460 feet) at its widest point, the spit encloses a lagoon of some 1,620 square kilometers (625 square miles). In this image, dark blue indicates deep water, and lighter blue indicates shallow and/or sediment-laden water. Different shades of blue distinguish the deeper Baltic Sea and the shallower Curonian Lagoon. Vegetation appears in varying shades of green, paved surfaces and bare ground appear in shades of beige and gray, and sandy areas appear off-white. Obvious sandy areas appear along the length of the spit. On the Baltic Sea side, a thin off-white band of beach runs the length of the spit; on the Curonian Lagoon side, intermittent beaches carve their way into the narrow strip of land.

2006-01-01

202

Aral Sea Evaporation (WMS)  

NSDL National Science Digital Library

The Aral Sea is actually not a sea at all, but an immense fresh water lake. In the last thirty years, more than sixty percent of the lake has disappeared because much of the river flow feeding the lake was diverted to irrigate cotton fields and rice paddies. Concentrations of salts and minerals began to rise in the shrinking body of water, leading to staggering alterations in the lakes ecology and precipitous drops in the Arals fish population. Powerful winds that blow across this part of Asia routinely pick up and deposit the now exposed lake bed soil. This has contributed to a significant reduction in breathable air quality, and crop yields have been appreciably affected due to heavily salt laden particles falling on arable land. This series of Landsat images taken in 1973, 1987 and 2000 show the profound reduction in overall area at the north end of the Aral, and a commensurate increase in land area as the floor of the sea now lies exposed.

Joycelyn Thomson

2005-02-15

203

Sea & Ships: Explore online  

NSDL National Science Digital Library

The National Maritime Museum (NMM) in England notes that its goal is "working to illustrate for everyone the importance of the sea, ships, time and the stars and their relationship with people." There is so much to explore in the "Sea and Ships" portion of the NMM website, but a great way to see everything it has to offer is by using the "Sea and Ships Directory" at the bottom of the homepage. It divides the material up by "Subjects", "People", "Collections", "Online Galleries", and "Games and Interactives". Visitors interested in lessons about the ocean that come in the form of games, quizzes and stories, should definitely check out the "Your Ocean" link from the "Games and Interactives". The "Your Waste" lesson gives visitors the opportunity to test their skills at "managing an oil spill clean-up operation", in the game "Oil Crisis!" Keeping waste to a minimum is what the quiz "Pollution Solutions" addresses, and is also on the "Your Waste" page. Other lessons include "Your Energy", "Your Stuff" and "Your Climate".

204

50 CFR 697.12 - At-sea sea sampler/observer coverage.  

Code of Federal Regulations, 2012 CFR

...must: (1) Notify the sea sampler/observer of any sea turtles, marine mammals, or other specimens taken by the vessel. (2) Provide the sea sampler/observer with sea turtles, marine mammals, or other specimens taken by the...

2012-10-01

205

50 CFR 697.12 - At-sea sea sampler/observer coverage.  

Code of Federal Regulations, 2014 CFR

...must: (1) Notify the sea sampler/observer of any sea turtles, marine mammals, or other specimens taken by the vessel. (2) Provide the sea sampler/observer with sea turtles, marine mammals, or other specimens taken by the...

2014-10-01

206

50 CFR 697.12 - At-sea sea sampler/observer coverage.  

Code of Federal Regulations, 2013 CFR

...must: (1) Notify the sea sampler/observer of any sea turtles, marine mammals, or other specimens taken by the vessel. (2) Provide the sea sampler/observer with sea turtles, marine mammals, or other specimens taken by the...

2013-10-01

207

50 CFR 697.12 - At-sea sea sampler/observer coverage.  

Code of Federal Regulations, 2011 CFR

...must: (1) Notify the sea sampler/observer of any sea turtles, marine mammals, or other specimens taken by the vessel. (2) Provide the sea sampler/observer with sea turtles, marine mammals, or other specimens taken by the...

2011-10-01

208

Water Mass Properties and Distribution between South China Sea, Sulu Sea and Celebes Sea  

NASA Astrophysics Data System (ADS)

A definition of water mass properties, characteristics and its origin along the coast of northern Borneo are presented based on 55 CTD casts cruises in July 2009 combined with five Argo profiling floats at surrounding seas. The T-S relation in the study area, which includes South China Sea, Sulu Sea and Celebes Sea, show existences of eight water masses. In reference of earlier studies, we define water masses in the surface mixed layer with strong mixed of Open Sea Water (OSW), Continental Shelf Water (CSW) and Tropical Surface Water (TSW). Below the layer of this active mixing is a zone of rapid transition called the Seasonal Thermocline Water (STW). Meanwhile, the Maximum Salinity Water (MSW), Permanent Thermocline Water (PTW), North Pacific Intermediate Water (NPIW) and Deep Water (DW) were found at the depth range from below the seasonal thermocline to about 1000 m. In addition, study of BRAN (BLUElink ReANalysis) global ocean model was conducted to demonstrate how current circulation influence the exchange of water mass between the 3 seas. Sulu Sea sits in the middle and has very limited connection between the other two seas. Connection with Celebes Sea occurs at the inlet of 200m depth. Water exchange happens in two ways; surface inflow and subsurface outflow. While in South China Sea, inlet is limited to 50m depth and surface flow is mostly dominant. The current circulation of the adjacent sea demonstrate some of the water mass were origiated as far as north South China Sea and Pacific Ocean. Water mass differences between the seas were further classified to distinguish dissimilarities and define the origin the difference. Given the unique geographical background and current circulation of the area, the characteristics of the interaction between water mass distribution and current circulation has provide important overview to the area which previously not well understood.

Fadzil Akhir, Mohd; Arsad, Shukri

2013-04-01

209

Aliens among us SEA-MONKEYS  

E-print Network

Aliens among us SEA-MONKEYS® FUN FACTS Did you know? Sea-Monkeys® · breathe through their legs, so adults have three. W hat is the connection between Sea-Monkeys® and aliens? Be- lieve it or not NASA scientists think it is possible that some alien life might resemble Sea-Monkeys®. Sea

Maxwell, Bruce D.

210

Isotope studies in the Caspian Sea  

Microsoft Academic Search

Oceanographic and isotopic investigations in the Caspian Sea and the analyses of the available data on the discharge to the sea and the observed sea level changes suggest that climatically caused changes of river inflow are the major cause of the sea level fluctuations over the last century. Hydrogen-3 and 3H–3He data indicate that the deep basins of the sea

K. Froehlich; K. Rozanski; P. Povinec; B. Oregioni; J. Gastaud

1999-01-01

211

Sea Otter, River Otter. The Wonder Series.  

ERIC Educational Resources Information Center

This curriculum guide is all about otters and provides information on both sea and river otters. Included are activities related to the diet of sea otters, the adaptations sea otters have made to live in the sea, their tool-using abilities, where they live and how to spot them, comparative anatomy of sea and river otters, and otter movement. The…

Robinson, Sandra Chisholm

212

Sea Scallop Shell Lab Handout  

NSDL National Science Digital Library

Used in combination with the Sea Scallop Shell Lab teacher's guide, students will examine sea scallop shells to figure out as much as possible about the scallops living on the sea floor in one three important fishery grounds, Hudson Canyon, off New Bedford, MA, and George's Bank. The activity emphasizes observation, measurements, and basic calculations. The teacher's guide is available from the COSEE-NE OSEI resource site.

213

Aerosols Over Yellow Sea Sediments  

NASA Technical Reports Server (NTRS)

This SeaWiFS image shows complex phytoplankton distribution patterns in the Bohai and Yellow seas. A wide band of brownish water along the coast north and south of the mouth of the Yangtze River indicates a heavy load of suspended sediment. The air over eastern central China and the Yellow Sea is thick with aerosols. Farther north over the Manchurian Plain and Greater Khingan Range, the air is much clearer.

2002-01-01

214

Experiencing the Full Research Process at Sea Education Association (SEA)  

NASA Astrophysics Data System (ADS)

While some undergraduate research experiences include only a small piece of the research process, students attending Sea Education Association's SEA Semester complete all aspects of oceanographic research in an intensive 12 week program that earns a full semester's credit. In the first half of the program, students read and discuss background literature on a subject, ask questions, pose hypotheses, and develop a written research proposal, which they defend orally. The second half of the course takes place at sea on one of SEA's state-of-the-art oceanographic research vessels where students carry out their sampling plans, analyze samples and data, write a final paper and present their results before the vessel reaches port, completing the course. At sea, students participate in sample collection and analysis for all student projects in addition to learning the general oceanography along their cruise track. This structure exposes students to the realities of research from start to finish and allows them to take full ownership of their projects. In addition to honing writing, public speaking, and problem-solving skills, students learn that research requires dedication, flexibility, and creativity, particularly when their results are unexpected or negate their hypothesis. SEA's undergraduate research program has been developing since 1971. Over that time, SEA has collected an extensive historical oceanographic database in the western Atlantic and Caribbean, plus Pacific data since 2001. This database is available to both students and outside research scientists. Collaborations with scientists outside SEA enhance the student experience and help facilitate oceanographic research by providing "ship-of-opportunity" sampling in remote locations. SEA Semester provides an excellent model for undergraduate research experiences with over 5000 alumni, about 30% of whom enter graduate school. About half the students in SEA's undergraduate programs are non-science majors. Although their experience at SEA may be their only hands-on exposure to scientific research, they take away an understanding of the process and an ability to think critically about scientific problems.

Harris, S. E.; Joyce, P.; Jaroslow, G.; Graziano, L.; Lea, C.; Witting, J.; Bower, A.

2003-12-01

215

Salton, A Sea of Controversy  

NSDL National Science Digital Library

The Salton Sea is an “accidental” lake that receives used irrigation water from the Colorado River. Humans have profoundly altered the area’s ecosystems. The Salton Sea is important for wildlife and recreation, but is now saltier than the ocean. How might it be saved? This case examines the Salton Sea’s problems and uncertain future. The case would be suitable for introductory environmental, biology, geography and geology classes, and courses dealing with land use, water resources, agriculture, birds or fish, ecosystems, and government policy.

Kristin B. Vessey

1999-01-01

216

Clues from the Black Sea  

NSDL National Science Digital Library

This activity has students apply scientific theory and hypothesis to studies being conducted in the Black Sea. They will discuss the purpose of and theory behind the Black Sea study and use maps to explain the flood theory. Students will also write hypotheses suggesting what certain pieces of evidence might reveal about the Black Sea and the flood. Next, they will read about the researchers' discoveries and list the items they found. Students will conclude by writing plans, pretending they are going to lead the next Black Sea expedition, and hypothesizing what they might find and what those findings might signify.

217

NOVA: Deep Sea Invasion  

NSDL National Science Digital Library

This is the companion Web site to "Deep Sea Invasion," a PBS NOVA documentary broadcast April 1, 2003. The program follows marine biologist Alexandre Meinesz and his scientific detective work to explain the rampant spread of the tropical alga Caulerpa taxifolia through the Mediterranean and his struggle to instigate control efforts. The features of this Web site include a timeline chronicling the invasion, an article by Meinesz on the impact of invasive species, another article addressing strategies for controlling invasives, and an interactive quiz in which users match up species with their invasive characteristics. With interesting material covering a range of ecological topics, this Web site should be of interest to any reader.

2003-01-01

218

The Sea Around Us  

NASA Astrophysics Data System (ADS)

Published in 1951, The Sea Around Us is one of the most remarkably successful books ever written about the natural world. Rachel Carson's rare ability to combine scientific insight with moving, poetic prose catapulted her book to first place on The New York Times best-seller list, where it enjoyed wide attention for thirty-one consecutive weeks. It remained on the list for more than a year and a half and ultimately sold well over a million copies, has been translated into 28 languages, inspired an Academy Award-winning documentary, and won both the 1952 National Book Award and the John Burroughs Medal. This classic work remains as fresh today as when it first appeared. Carson's writing teems with stunning, memorable images--the newly formed Earth cooling beneath an endlessly overcast sky; the centuries of nonstop rain that created the oceans; giant squids battling sperm whales hundreds of fathoms below the surface; and incredibly powerful tides moving 100 billion tons of water daily in the Bay of Fundy. Quite simply, she captures the mystery and allure of the ocean with a compelling blend of imagination and expertise. Reintroducing a classic work to a whole new generation of readers, this Special Edition features a new chapter written by Jeffrey Levinton, a leading expert in marine ecology, that brings the scientific side of The Sea Around Us completely up to date. Levinton incorporates the most recent thinking on continental drift, coral reefs, the spread of the ocean floor, the deterioration of the oceans, mass extinction of sea life, and many other topics. In addition, acclaimed nature writer Ann Zwinger has contributed a brief foreword. Today, with the oceans endangered by the dumping of medical waste and ecological disasters such as the Exxon oil spill in Alaska, this illuminating volume provides a timely reminder of both the fragility and the importance of the ocean and the life that abounds within it. Anyone who loves the sea, or who is concerned about our natural environment, will want to read this classic work.

Carson, Rachel L.

1991-12-01

219

Sea and Sky  

NSDL National Science Digital Library

This comprehensive site contains information about both astronomy and the oceans. The Sky section contains astronomical resources, news links, an image gallery, games and general links for more information. The Cosmos contains details about stars, planets, moons, pulsars, galaxies, black holes, quasars, star clusters, nebulas, dark matter and constellations. There is also a section about astronomers and a timeline of space exploration. The Sea section contains news links, aquarium resources, an image gallery, games and links for more information about the oceans. The Ocean Realm highlights the many creatures that live in the oceans. There are also details about ocean exploration and an exploration timeline.

J. Knight

220

Science Nation: Sea Turtles  

NSDL National Science Digital Library

Researchers at the University of North Carolina are studying how loggerhead and other sea turtles use the Earth's magnetic field for a journey of thousands of miles around the Atlantic Ocean. The turtles react to the Earth's magnetic field as they navigate a five-to-10-year journey that takes them from the east coast of the United States to the coast of Portugal, south toward the west coast of Africa, then back toward the beach where they were born. A better understanding of this turtle ability could help in research of both animal and human navigation.

221

SeaWeb  

NSDL National Science Digital Library

SeaWeb is a project designed to raise awareness of the world's oceans and the lifeforms within them, and to encourage conservation efforts. Information provided here includes the latest news about ocean-related issues, audio files of the Ocean Report which provides a tour of the world's oceans, email updates, a bookstore, and an on-line book about issues facing our oceans. This includes habitats, fisheries and other issues. This site is searchable and provides links and resources for further information.

222

Two Sea-Level Challenges  

NASA Astrophysics Data System (ADS)

"No place on the sandy ocean shores of the world has been shown to be eroding because of sea level rise." This statement appeared nearly 19 years ago in bold print at the top of the page in a brief article published in Shore and Beach (Galvin,1990). The term "sea level rise" was defined in 1990 as follows: "In this statement, "sea level rise" has the meaning that the average person on the street usually attaches to that term. That is, sea level is rising; not, as in some places like the Mississippi River delta, land level is sinking." While still a subject of controversy, it is now (2008) increasingly plausible (Tornqvist et al,2008) that damage from Hurricane Katrina was significantly worse on the Mississippi River delta because floodwaters exploited wetlands and levees whose elevations had been lowered by decades of compaction in the underlying soil. (1) "Sea level" commonly appears in the literature as "relative sea level rise", occurring that way in 711 publications between 1980 and 2009 (GeoRef database on 8 Sep 08). "Relative sea level rise" does not appear in the 2005 AGI Glossary. The nearest Glossary term is "relative change in sea level", but that term occurs in only 12 publications between 1980 and 2009. The Glossary defines this term in a sequence stratigraphy sense, which infers that "relative sea level rise" is the sum of bottom subsidence and eustatic sea level rise. In plain English, "relative sea level rise" means "water depth increase". For present day coastal environments, "relative sea level rise" is commonly used where eustatic sea level rise is less than subsidence, that is, where the magnitude of actual sea level rise is smaller than the magnitude of subsidence. In that situation, "relative sea level rise" misleads both the average person and the scientist who is not a coastal geologist. Thus, the first challenge is to abandon "relative sea level rise" in favor of "water depth increase", in order that the words accurately descibe what happens. It would further clarify popular understanding if the term "actual sea level rise" were used in place of "eustatic sea level rise". (2)Geologists have approximated the the practice of paleontologists and biologists in establishing type examples of important geological features. This is a useful practice. A graduate geologist holds in mind clear conceptions of "beach cusps", "drumlin fields", "birdfoot deltas", and "igneous sills" based on seeing field examples accepted by professional geologists as representative of these features. However, although publications frequently report that sea level rise erodes a particular beach, no one identifies a type beach where that cause has been proven to produce the alleged effect. At the type beach, it is necessary to show that sea level is rising, and that the beach erodes primarily from this sea level rise, rather than from interrupted longshore transport. Thus, the second challenge is to identify a type ocean beach proven to erode because of sea level rise.

Galvin, C.

2008-12-01

223

7 CFR 1437.310 - Sea grass and sea oats.  

Code of Federal Regulations, 2010 CFR

...Sea grass and sea oats are value loss crops and eligibility...2) of this section, the value of: (1) Seed will be...Have readily identifiable boundaries; and (3) Be managed and...commodities having any dollar value after the disaster shall...

2010-01-01

224

Holocene sea surface temperature and sea ice extent in the Okhotsk and Bering Seas  

NASA Astrophysics Data System (ADS)

Accurate prediction of future climate requires an understanding of the mechanisms of the Holocene climate; however, the driving forces, mechanisms, and processes of climate change in the Holocene associated with different time scales remain unclear. We investigated the drivers of Holocene sea surface temperature (SST) and sea ice extent in the North Pacific Ocean, and the Okhotsk and Bering Seas, as inferred from sediment core records, by using the alkenone unsaturation index as a biomarker of SST and abundances of sea ice-related diatoms (F. cylindrus and F. oceanica) as an indicator of sea ice extent to explore controlling mechanisms in the high-latitude Pacific. Temporal changes in alkenone content suggest that alkenone production was relatively high during the middle Holocene in the Okhotsk Sea and the western North Pacific, but highest in the late Holocene in the eastern Bering Sea and the eastern North Pacific. The Holocene variations of alkenone-SSTs at sites near Kamchatka in the Northwest Pacific, as well as in the western and eastern regions of the Bering Sea, and in the eastern North Pacific track the changes of Holocene summer insolation at 50°N, but at other sites in the western North Pacific, in the southern Okhotsk Sea, and the eastern Bering Sea they do not. In addition to insolation, other atmosphere and ocean climate drivers, such as sea ice distribution and changes in the position and activity of the Aleutian Low, may have systematically influenced the timing and magnitude of warming and cooling during the Holocene within the subarctic North Pacific. Periods of high sea ice extent in both the Okhotsk and Bering Seas may correspond to some periods of frequent or strong winter-spring dust storms in the Mongolian Gobi Desert, particularly one centered at ?4-3 thousand years before present (kyr BP). Variation in storm activity in the Mongolian Gobi Desert region may reflect changes in the strength and positions of the Aleutian Low and Siberian High. We suggest that periods of eastward displacement or increased intensity of the Aleutian Low correspond with times of increased extent of sea ice in the western Okhotsk Sea and eastern Bering Sea.

Harada, Naomi; Katsuki, Kota; Nakagawa, Mitsuhiro; Matsumoto, Akiko; Seki, Osamu; Addison, Jason A.; Finney, Bruce P.; Sato, Miyako

2014-08-01

225

Spectacled Eiders Wintering in Northern Bering Sea  

USGS Multimedia Gallery

Large flock of Spectacled Eiders aggregated in a sea ice lead in the northern Bering Sea, south of St. Lawrence Island, Alaska.  Aerial photograph from a helicopter deployed from the USCG Cutter Polar Sea....

226

Spectacled Eiders Wintering in Northern Bering Sea  

USGS Multimedia Gallery

Large flock of Spectacled Eiders aggregated in a sea ice lead at sunset in the northern Bering Sea, south of St. Lawrence Island, Alaska.  Aerial photograph from a helicopter deployed from the USCG Cutter Polar Sea....

227

Spectacled Eiders Wintering in Northern Bering Sea  

USGS Multimedia Gallery

Large flock of Spectacled Eiders aggregated in a sea ice lead in the northern Bering Sea, south of St. Lawrence Island, Alaska.  Aerial photograph from a helicopter deployed from the USCG Cutter Polar Sea. ...

228

Sea modeling and rendering  

NASA Astrophysics Data System (ADS)

More and more defence and civil applications require simulation of marine synthetic environment. Currently, the "Future Anti-Surface-Guided-Weapon" (FASGW) or "anti-navire léger" (ANL) missile needs this kind of modelling. This paper presents a set of technical enhancement of the SE-Workbench that aim at better representing the sea profile and the interaction with targets. The operational scenario variability is a key criterion: the generic geographical area (e.g. Persian Gulf, coast of Somalia,...), the type of situation (e.g. peace keeping, peace enforcement, anti-piracy, drug interdiction,...)., the objectives (political, strategic, or military objectives), the description of the mission(s) (e.g. antipiracy) and operation(s) (e.g. surveillance and reconnaissance, escort, convoying) to achieve the objectives, the type of environment (Weather, Time of day, Geography [coastlines, islands, hills/mountains]). The paper insists on several points such as the dual rendering using either ray tracing [and the GP GPU optimization] or rasterization [and GPU shaders optimization], the modelling of sea-surface based on hypertextures and shaders, the wakes modelling, the buoyancy models for targets, the interaction of coast and littoral, the dielectric infrared modelling of water material.

Cathala, Thierry; Latger, Jean

2010-10-01

229

ROC Sampling Deep Sea Urchin  

USGS Multimedia Gallery

Images of the remotely operated vehicle Jason2 sampling a sea urchin in a deep sea mussel community found near a gas seep on the U.S. outer continental shelf. Images courtesy Deepwater Canyons 2013 - Pathways to the Abyss expedition, NOAA-OER/BOEM/USGS....

230

How SeaBirds Dine  

Microsoft Academic Search

As I have ascertained that the following fact is not well known, I send you this account in the hope that it may be of interest to naturalists and to the general public. Anyone who lives in the Western Hebrides will have often watched on a calm day the sea-birds feeding with noisy clamour in the sea-lochs and about the

1888-01-01

231

Probability of sea level rise  

SciTech Connect

The report develops probability-based projections that can be added to local tide-gage trends to estimate future sea level at particular locations. It uses the same models employed by previous assessments of sea level rise. The key coefficients in those models are based on subjective probability distributions supplied by a cross-section of climatologists, oceanographers, and glaciologists.

Titus, J.G.; Narayanan, V.K.

1995-10-01

232

Glass Munchers Under the Sea  

NSDL National Science Digital Library

This NASA Astrobiology Institute article documents recent findings of bacterial life beneath the sea floor. These newly discovered bacteria are thought to live as far down as 500 meters beneath the sea floor and eat through volcanic rock, leaving behind burrows. The article contains hyperlinks to websites explaining some key vocabulary, related websites, and color photos and maps.

Leslie Mullen

233

Connecting the Seas of Norden  

NASA Astrophysics Data System (ADS)

The Nordic Seas are highly sensitive to environmental change and have been extensively monitored and studied across a broad range of marine disciplines. For these reasons, the Nordic seas may serve as a pilot area for integrated policy development in response to ongoing climate change.

Paasche, Øyvind; Österblom, Henrik; Neuenfeldt, Stefan; Bonsdorff, Erik; Brander, Keith; Conley, Daniel J.; Durant, Joël M.; Eikeset, Anne M.; Goksøyr, Anders; Jónsson, Steingrímur; Kjesbu, Olav S.; Kuparinen, Anna; Stenseth, Nils Chr.

2015-02-01

234

Dead sea asphalts: historical aspects  

Microsoft Academic Search

Asphalts are present in the Dead Sea basin in three forms: (1) huge blocks, up to 100 tons in weight, composed of extremely pure (>99.99%) solid asphalt occasionally found floating on the lake, (2) veins, seepages, and cavity and fissure fillings in Lower Cretaceous to Holocene rocks, and (3) ozocerite veins on the eastern shore of the lake. Dead Sea

Nissenbaum

1978-01-01

235

Salton: A Sea of Controversy  

NSDL National Science Digital Library

The Salton Sea is an accidental lake that receives used irrigation water from the Colorado River. Humans have profoundly altered the area's ecosystems. The sea is important for wildlife and recreation but is now saltier than the ocean. How might it be sav

Kristin B. Vessey

2000-09-01

236

Evidence of Ice Free Seas  

NSDL National Science Digital Library

In this activity, students make a model sea floor sediment core using two types of buttons to represent fossil diatoms. They then compare the numbers of diatom fossils in the sediment at different depths to determine whether the seas were free of ice while the diatoms were alive.

LuAnn Dahlman

237

The Barbados Sea Level Record  

NASA Astrophysics Data System (ADS)

Additional offshore drill cores, nearly 100 new radiometric dates, and more than 1000 kilometers of Multibeam mapping greatly enhance the Barbados Sea Level record. Extensive Multibeam mapping around the entire island covers approximately 2650 km2 of the sea bottom and now integrates the offshore reef topography and Barbados Sea Level Record with the unparalleled onshore core collection, digital elevation maps, and Pleistocene sea level record spanning the past one million years. The reef crest coral, Acropora palmata, remains the stalwart indicator of sea level for many reasons that are validated by our redundant sea level records and redundant dating via Th/U and Pa/U analyses. Microanalysis and densitometry studies better explain why Acropora palmata is so well preserved in the Pleistocene reef records and therefore why it is the species of choice for sea level reconstructions and radiometric dating. New drill cores into reefs that formed during Marine Isotope Stage 3 lead us to a model of diagenesis that allows us to better prospect for unaltered coral samples in older reefs that may be suitable for Th/U dating. Equally important, our diagenesis model reinforces our rigorous sample quality criteria in a more quantitative manner. The Barbados Sea Level record has a sampling resolution of better than 100 years throughout much of the last deglaciation showing unprecedented detail in redundant drill cores. The Melt Water Pulses (MWP1A and MWP1B) are well resolved and the intervening interval that includes the Younger Dryas reveals sea level changes in new detail that are consistent with the terrestrial records of ice margins (see Abdul et al., this section). More than 100 paired Th/U and radiocarbon ages place the Barbados Sea Level Record unambiguously on the radiocarbon time scale for direct comparisons with the terrestrial records of ice margin changes.

Fairbanks, R. G.; Mortlock, R. A.; Abdul, N. A.; Wright, J. D.; Cao, L.; Mey, J. L.

2013-12-01

238

The Aral Sea: Then and Now  

NSDL National Science Digital Library

This lesson plan asks students to consider what happens when a sea shrinks and to compare pictures of the Aral Sea at different times. They will conclude by pretending to be residents of the Aral Sea region, drawing before and after pictures of how changes to the sea have affected their lives. Students will conduct an experiment to see whether salt evaporates with water; hypothesize what might happen to people, animals, and plants living near a shrinking sea; compare satellite images of the Aral Sea from 1973 and 1999; match problems in the Aral Sea region with statements about these problems in the Aral Sea family activity; discuss changes that are occurring in the Aral Sea region; and create drawings depicting the lives of people in the Aral Sea region before and after the sea began to shrink.

239

Beneath the Sea  

NSDL National Science Digital Library

This site contains videos from the "Beneath the Sea" television episode, related website articles and student activities, and an interactive ocean game that tests knowledge of what creatures live at what depth. The videos feature technologies that have opened up the farthest reaches of the ocean and a remote submarine as it dives to the unexplored middle depths of the ocean off Monterey, California, revealing a spectacular variety of new life forms. The videos total approximately one hour in length. The articles explore how life survives in dark hot ocean vents and how this may shed light on the origin of life on Earth; evidence in support of the flood in the biblical story of Noah; and what deep-ocean research has revealed about continental drift, plate tectonics, and the formation of the Earth.

240

Deep Sea Duel  

NSDL National Science Digital Library

This Android app for the Illuminations online game Deep Sea Duel card game helps users develop mental computation skills by finding sums of 3 or 4 numbers. A student and the opponent, Okta the octopus take turns selecting cards. The first one to reach the target sum with 3 cards (in the 9-card game) or 4 cards (in the 16-card game) wins the game. You can choose how many cards are presented (9 or 16), what types of numbers they display (small integers through tricky decimals), and Okta's level of strategy. The game is not timed but depends on strategic planning in order to defend against Okta's moves while trying to collect a winning group of cards.

2012-08-29

241

Deep Sea Duel  

NSDL National Science Digital Library

This iOS app for the Illuminations online card game Deep Sea Duel (cataloged separately) helps users develop mental computation skills by finding sums of 3 or 4 numbers. A student and the opponent, Okta the octopus take turns selecting cards. The first one to reach the target sum with 3 cards (in the 9-card game) or 4 cards (in the 16-card game) wins the game. You can choose how many cards are presented (9 or 16), what types of numbers they display (small integers through tricky decimals), and Okta's level of strategy. The game is not timed but depends on strategic planning in order to defend against Okta's moves while trying to collect a winning group of cards.

2012-08-02

242

Late Glacial to Holocene benthic foraminifera in the Marmara Sea: implications for Black Sea^Mediterranean Sea  

E-print Network

Late Glacial to Holocene benthic foraminifera in the Marmara Sea: implications for Black Sea^Mediterranean by the Mediterranean at V12 ka, allowing saline waters to penetrate the Marmara Sea. These saline waters reached Sea connections following the last deglaciation Michael A. Kaminski a;b;Ã , Ali Aksu c , Matthew Box a

Kaminski, Michael A.

243

Variability and forcing of the East Australian Current Melissa M. Bowen1  

E-print Network

Zealand [Nilsson and Cresswell, 1981]. [3] At times the EAC can extend along the coast well south into the Tasman Sea, others of which move northeastward to coalesce with the main current [Nilsson and Cresswell

Wilkin, John

244

RESEARCHERS TEACHERS Niiler, P., N. Maximenko and J. McWilliams,  

E-print Network

Zealand New Zealand Met. Service Climate & Forecast Tasman Sea & S. Pac SST & P South Africa South African Weather Service Climate & Forecast S. Atl SST, P, & W UK UKMET Ocean Forecast N. Atl SST, P, &W US Coast

245

Sea Star Succumbing to Sea Star Wasting Disease  

USGS Multimedia Gallery

Unlike their smiling cartoon brethren on television, since 2013, real-life sea stars have been suffering from a wasting disease epidemic in which they lose limbs and literally disintegrate in a matter of days. ...

246

Sea level variation in the eastern Asia  

Microsoft Academic Search

Mean sea level variations in the eastern Asia region during 1950 to 1991 are investigated with the use of observed sea level data at 16 stations. It is suggested from the data analysis, that the main cause of long-term sea level variation in this region may be the plate tectonic processes. The mean sea levels along the eastern coasts of

Tetsuo Yanagi; Tatsuya Akaki

1994-01-01

247

Structural Degradation in Mediterranean Sea Food Webs  

E-print Network

Structural Degradation in Mediterranean Sea Food Webs: Testing Ecological Hypotheses Using-Central Adriatic and South Catalan Sea) and two time periods (mid-late 1970s and 1990s) in the Mediterranean Sea to species removal; Niche model; Ecopath model; Mediterranean Sea. INTRODUCTION Degradation of marine

Myers, Ransom A.

248

Influences of sea ice on eastern Bering Sea phytoplankton  

NASA Astrophysics Data System (ADS)

The influence of sea ice on the species composition and cell density of phytoplankton was investigated in the eastern Bering Sea in spring 2008. Diatoms, particularly pennate diatoms, dominated the phytoplankton community. The dominant species were Grammonema islandica (Grunow in Van Heurck) Hasle, Fragilariopsis cylindrus (Grunow) Krieger, F. oceanica (Cleve) Hasle, Navicula vanhoeffenii Gran, Thalassiosira antarctica Comber, T. gravida Cleve, T. nordenskiöeldii Cleve, and T. rotula Meunier. Phytoplankton cell densities varied from 0.08×104 to 428.8×104 cells/L, with an average of 30.3×104 cells/L. Using cluster analysis, phytoplankton were grouped into three assemblages defined by ice-forming conditions: open water, ice edge, and sea ice assemblages. In spring, when the sea ice melts, the phytoplankton dispersed from the sea ice to the ice edge and even into open waters. Thus, these phytoplankton in the sea ice may serve as a "seed bank" for phytoplankton population succession in the subarctic ecosystem. Moreover, historical studies combined with these results suggest that the sizes of diatom species have become smaller, shifting from microplankton to nannoplankton-dominated communities.

Zhou, Qianqian; Wang, Peng; Chen, Changping; Liang, Junrong; Li, Bingqian; Gao, Yahui

2015-03-01

249

SEA GRANT AT A GLANCE February 2014 National Sea Grant Office's  

E-print Network

:40pm ­ 11:10am Lake Champlain Sea Grant (Garber) #12;SEA GRANT AT A GLANCE ­ February 2014 3 11:10am at a glance USC Sea Grant at a glance TEXAS Sea Grant at a glance LAKE CHAMPLAIN Sea Grant at a glance

250

Trans-Tasman migration: New Zealanders' explanations for their move  

Microsoft Academic Search

This study investigates why New Zealanders move to Australia. A survey of New Zealanders living in Australia found 'pull' factors, notably greater opportunities and better climate, were the most common reasons. While desire for change or sense of adventure was important, dissatisfaction with life in New Zealand was also a factor. Results indicated a form of transnationalism as migrants felt

Alison E. Green; Mary R. Power; Deannah M. Jang

2008-01-01

251

Supervising Doctorates at a Distance: Three Trans-Tasman Stories  

ERIC Educational Resources Information Center

Purpose: The purpose of this paper is to describe the challenges of post-traditional, distance PhD supervision and suggest pedagogical interventions to bridge the distance. The paper investigates the skills and understandings necessary for mediating the supervisor-supervisee dyad within faceless encounters. Design/methodology/approach: Grounded in…

Andrew, Martin

2012-01-01

252

Sea salt CCN contribution  

NASA Astrophysics Data System (ADS)

Volatility measurements (Twomey 1971; Hudson and Da 1996) showed that most CCN over the ocean are not NaCl. However, other reports indicate NaCl as a major CCN component. Here we contrast cloud condensation nuclei (CCN) spectral volatility (thermal fractionation) measurements from three aircraft field projects to provide insight into the relative contribution of sea salt. The most remote location, PASE (mid-Pacific), had the highest average CCN concentrations (NCCN) probably because it was the least cloudy whereas the less remote, but more cloudy,RICO(Caribbean)had the lowest average NCCN (Hudson and Noble 2009). In RICO particle concentrations in all size ranges larger than 0.3 micrometers were well correlated with wind speed (R ~ 0.87) but uncorrelated with NCCN (Fig. 1A). Smaller particles in RICO were correlated with NCCN but uncorrelated with wind speed. In PASE only particles larger than 10 micrometers were correlated with wind speed and concentrations in these size ranges were uncorrelated with NCCN. Particles smaller than 10 micrometers in PASE were uncorrelated with wind speed but well correlated with NCCN. In both projects particle concentrations smaller than these respective sizes were highly correlated with NCCN, at all S in PASE but mainly with NCCN at high S in RICO. CCN volatility measurements showed high correlations between refractory NCCN and wind speed, especially for low supersaturation (S) NCCN, and no correlation of volatile NCCN at all S with wind speed. In PASE there was only a weak positive correlation between refractory NCCN and wind and also no correlation between volatile NCCN and wind. These results indicate that in clean maritime air the wind originated component of NCCN can be substantial (i.e., > 30% for wind > 14 m/s) but that in maritime air with higher NCCN the wind derived CCN component is probably less than 10%. The contrast in cloudiness between the two projects was responsible for many of the differences noted between them. A third project (POST) showed appropriately intermediate results to those of RICO and PASE. The results indicate that the effects of clouds on NCCN play a major role in the relative influence of sea salt on NCCN and ultimately on climate. Hudson, J.G. and S. Noble, 2009: Geophys. Res. Let., 36, L13812, Hudson, J.G. and X. Da, 1996: J. Geophys. Res., 101, 4435-4442. Twomey, S.: 1971: J. Atmos. Sci., 28, 377-381.

Hudson, J. G.; Jha, V.; Noble, S.

2011-12-01

253

Deep Sea Vents Web List  

NSDL National Science Digital Library

This student-friendly list has eight web sites that relate to deep sea vents. A short description follows each site, listing the reference materials, interactive tools, videos, sound recordings, photo archives, or other resources that can be found there.

254

A Can of Sea Worms  

ERIC Educational Resources Information Center

A comprehensive discussion of the free-living worms that inhabit the beaches and subtidal bottoms of the Cape Cod shoreline is presented. Methods for the location, collection, preservation, and identification of sea worms are identified. (BT)

Zinn, Donald J.

1977-01-01

255

Antarctic Ice: Sea Level Change  

NSDL National Science Digital Library

This video segment, adapted from a NOVA broadcast, explains what might happen to global sea level if atmospheric warming caused the collapse and melting of the West Antarctica Ice Sheet. The segment is three minutes nineteen seconds in length.

256

Arctic Sea Ice Satellite Observations  

NSDL National Science Digital Library

In this interactive activity produced for Teachers' Domain, learn how Arctic sea ice has changed over the past 25 years in terms of maximum winter extent, concentration, and the timing of breakup each spring.

WGBH Educational Foundation

2008-01-17

257

Doppler characteristics of sea clutter.  

SciTech Connect

Doppler radars can distinguish targets from clutter if the target's velocity along the radar line of sight is beyond that of the clutter. Some targets of interest may have a Doppler shift similar to that of clutter. The nature of sea clutter is different in the clutter and exo-clutter regions. This behavior requires special consideration regarding where a radar can expect to find sea-clutter returns in Doppler space and what detection algorithms are most appropriate to help mitigate false alarms and increase probability of detection of a target. This paper studies the existing state-of-the-art in the understanding of Doppler characteristics of sea clutter and scattering from the ocean to better understand the design and performance choices of a radar in differentiating targets from clutter under prevailing sea conditions.

Raynal, Ann Marie; Doerry, Armin Walter

2010-06-01

258

The Kemps Ridley Sea Turtle  

NSDL National Science Digital Library

This video adapted from Texas Parks and Wildlife Department describes how humans are helping restore safe nesting grounds for the critically endangered Kemp's ridley sea turtle to ensure its successful repopulation.

WGBH Educational Foundation

2007-08-09

259

Sea Turtle Protection and Conservation  

NSDL National Science Digital Library

This extensive site describes the population status of each U.S. sea turtle species and how they are protected by law. Each species' scientific name, biology, threatened or endangered status, description, human impacts, population trends, distribution, and photos are documented. Read the downloadable Recovery Plans for each species, as well as learn about turtle legislation. Site also features reports and proceedings from various sea turtle symposia and conferences.

260

Mapping Deep-sea Habitats  

NSDL National Science Digital Library

In this lesson students investigate bathymetric mapping of deep-sea habitats to see how deep-sea areas of the northwestern Hawaiian Islands can be mapped to facilitate their exploration with a manned submersible. Students will create a two-dimensional topographic map from bathymetric survey data, a three-dimensional model of landforms from a two-dimensional topographic map, and will interpret two- and three-dimensional topographic data.

Mel Goodwin

261

Sea Turtle First Aid Investigation  

NSDL National Science Digital Library

This activity (located on page 4 of the PDF) is a full inquiry investigation into testing a repair material. Groups of learners perform “first aid” on a cut orange, which represents propeller damage on the back of a leatherback sea turtle. Learners use a variety of repair materials and predict how well various treatments will work, then observe treated, untreated, and uncut control oranges for 4 days. Relates to linked video, DragonflyTV GPS: Sea Turtles.

Twin Cities Public Television, Inc.

2007-01-01

262

Earthwatch Radio: Sea Lamprey Resurgence  

NSDL National Science Digital Library

This radio broadcast describes efforts to control the population of sea lampreys in the Great Lakes. Sea lampreys, an invasive species from the Atlantic Ocean, have populated the lakes for years, but have recently increased in numbers despite efforts to control them. A hole in a dam on the Manistique River on the northern edge of Lake Michigan is thought to have caused the problem. The clip is 2 minutes in length and may be downloaded in MP3 format.

Kalinowski, Laura

263

SeaWIFS: Teacher Resources  

NSDL National Science Digital Library

The SeaWIFS project uses space technology to study phytoplankton. Site contains: The Living Ocean Teacher's Guide, a guide for grades 9-10 that discusses satellites, ocean color, phytoplankton, the carbon cycle, and greenhouse effect; Classic CZCS Scenes, a tutorial about ocean color using some of the more interesting CZCS images; and Monitoring the Earth from Space with SeaWiFS, an presentation about ocean color; and several other remote sensing resources.

264

Impacts into oceans and seas  

Microsoft Academic Search

Impacts of cosmic bodies into oceans and seas lead to the formation of very high waves. Numerical simulations of 3-km and 1-km comets impacting into a 4 km depth ocean with a velocity of 20 km\\/sec have been conducted. For a 1-km body, depth of the interim crater in the sea bed is about 8 km below ocean level, and

I. V. Nemtchinov; T. V. Loseva; A. V. Teterev

1996-01-01

265

Intermittent sea-level acceleration  

NASA Astrophysics Data System (ADS)

Using instrumental observations from the Permanent Service for Mean Sea Level (PSMSL), we provide a new assessment of the global sea-level acceleration for the last ~ 2 centuries (1820-2010). Our results, obtained by a stack of tide gauge time series, confirm the existence of a global sea-level acceleration (GSLA) and, coherently with independent assessments so far, they point to a value close to 0.01 mm/yr2. However, differently from previous studies, we discuss how change points or abrupt inflections in individual sea-level time series have contributed to the GSLA. Our analysis, based on methods borrowed from econometrics, suggests the existence of two distinct driving mechanisms for the GSLA, both involving a minority of tide gauges globally. The first effectively implies a gradual increase in the rate of sea-level rise at individual tide gauges, while the second is manifest through a sequence of catastrophic variations of the sea-level trend. These occurred intermittently since the end of the 19th century and became more frequent during the last four decades.

Olivieri, M.; Spada, G.

2013-10-01

266

Polar Sea Ice Processes  

NSDL National Science Digital Library

The goal of this NASA Earth Science Enterprise-funded project is to increase the use of satellite data in high school and college science classrooms by developing classroom materials linked to guided inquiry computer exercises. This Polar Sea Ice Processes module is one of four Studying Earth's Environment from Space (SEES) modules. Each module consists of three sections: Class Resources, Computer Lab Resources and a Glossary and Acronym List. Class Resources is an electronic lecture viewable by a Web browser. Computer Lab Resources contains an instructor's guide, data and software. The instructor's guide contains exercises for using the data and software. The public domain software, a version of NIH-Image for the Macintosh that was modified by NASA Goddard Space Flight Center especially for SEES, is for data display, analysis and tutorial of satellite data. The software will also work on Windows machines with a Mac emulator. Image2000, a cross-platform Java version of the software, is expected to be available by the end of the year 2000. Each module section can stand-alone (e.g. you don't have to use the Class Resources in order to complete the Computer Lab Resources). Students and instructors may continue their own scientific discovery by accessing archived and current data from various NASA Earth Science data centers.

Elizabeth Smith

267

From Shore to Sea  

NSDL National Science Digital Library

As the dog days of summer begin to set in, humans tend to flock like seagulls to the sun and sand of the shore and sea. This Topic in Depth examines several topics of interest from food chain on a beach to coral reefs.The first site (1), from the National Park Service, offers a look at the exceptionally beautiful Canaveral National Seashore. The site gives information about the flora and fauna found at the seashore as well a great photo gallery. The second link(2) leads to a white paper by Peter Entnoyer, Chad Nelson, and Kevin Ranker of the Surfider Foundation on the value of beach sand in the food chain. At the third site (3) from Mother Jones, visitors will find an article about the status of coral reefs. The fourth site, (4) from Ask a Scientist provides several questions and answers about plants and algae. The next link leads to the Online Marine Picture Book (5), a great resource for great photos from everything from crabs to starfish. The last site, from SUNY Stony Brook(6), provides a great glossary of marine biology related terms from Abyssal Plain to Zooxanthellae.

268

Correlation at sea  

NASA Astrophysics Data System (ADS)

This paper discusses an optical correlator interfaces to a FLIR and laser rangefinder to aid aircraft landing aboard an aircraft carrier. The purpose was to recognize aircraft and provide precision track in spite of the engine plume which is visible in IR images. Toward the end of the program, an opportunity arose to piggyback on tests of a Navy FLIR system, on board the USS Enterprise. The Navy's developmental FLIR and laser rangefinder were mounted on the carrier and provided excellent imagery with concurrent range data. The correlator performed a limited set of experiments at sea, tracking an aircraft from 8000 feet until almost touchdown. The challenges to the correlator we operation in a harsh environment and real time interfacing with other hardware. Real time range information controlled a series of filters in the correlator. The system fit into a standard panel rack and utilized remote alignment. The system operated during the chock of aircraft launch and landing, with no need to open up the optical box.

Hartman, Richard L.; Farr, Keith B.; McColgan, Michele W.; Smith, Ralph G.

1997-03-01

269

North Sea platforms revamped  

SciTech Connect

Many of the early North Sea platforms are reaching their end-of-field life. Most are still equipped with their original drilling package. In a few cases the package has either been removed or decommissioned. The early installations were designed for much simpler and less demanding wells than the horizontal, extended-reach or designer wells common today. Extended-reach wells now can be drilled realistically from ageing platforms, without incurring massive capital expenditure. This can be achieved using the existing drilling package to the limit of its capabilities and supplementing where necessary with relatively minor upgrades or the use of temporary equipment. Drilling even a few more wells from existing platforms not only prolongs field life, it enables any surplus processing capacity to be made available to develop near-field potential with extended-reach drilling (ERD) or by tying back subsea satellite wells, or for processing third-party fluids. The paper describes well design, surface equipment, mud pumps, shakers and solids control equipment, drill cuttings disposal systems, derrick and hoisting system, top drive and drillstring, downhole equipment, well planning, casing wear, logistics, rig preparations, and ERD vs. subsea tie-backs.

O'Hare, J.

1999-12-01

270

Research papers The genesis of sea level variability in the Barents Sea  

E-print Network

, University of Miami, and Atlantic Oceanographic and Meteorological Laboratory, NOAA, Miami, FL, USA, b Jet 1­3 month phase lag between the annual cycles of sea level in the Barents Sea and in the Nordic seas

271

State estimation of the Labrador Sea with a coupled sea ice-ocean adjoint model  

E-print Network

Sea ice (SI) and ocean variability in marginal polar and subpolar seas are closely coupled. SI variability in the Labrador Sea is of climatic interest because of its relationship to deep convection/mode water formation, ...

Fenty, Ian Gouverneur

2010-01-01

272

Variability In The Solomon Sea From Altimetric Sea Level Data  

NASA Astrophysics Data System (ADS)

In the southwest tropical Pacific, subtropical waters from the SEC flow in the Solomon Sea, mainly through the western boundary New Guinea Coastal Undercurrent, and join the equatorial western Pacific by three narrow straits. The NGCU transports part of the spiciness anomalies generated in the South East Pacific and subducted in the thermocline. Because the NGCU is a primary source of the EUC, variations of its characteristics are expected to play a role in the equatorial thermocline features and more generally on decadal climate variability. Therefore, the study of the Solomon Sea is a key issue of the SPICE program. In this study, we focus on the variability of the Solomon Sea in term of sea level. The Solomon Sea is semi closed with a complex topography and numerous islands. Thus, the use of classical gridded altimetric products is inadequate. Consequently, this work is based on original along track Topex/Poseidon data. New data processing (CTOH/LEGOS) has been applied to recover proper data and to gain more information on the altimetric signal in this region. A track-by-track specific and customized post processing has been used to finalize the dataset. These new altimetric data have been assessed against tide gauge data. The analysis of the resulting sea level anomalies exhibits the highest variability observed in the tropical Pacific in an area centred near 8°S and expanding from each side of the Solomon Islands, outside of the WBC. Sea level variability presents a wide temporal spectrum, from intraseasonal to interannual ranges with the notable influence of the monsoon and of ENSO. In the Solomon Sea, three frequencies emerge : 60, 365 and 2000 days. The 60-days frequency seems particularly important in the Solomon Sea compared with the surrounding waters and an EOF analysis is used to understand its features. We also depict the signature of the New Guinea Coastal Current (NGCC), the western boundary current flowing north along the eastern coast of Papua New Guinea, which is particularly important for the connection to the equator. In parallel to this study, a hierarchy of high resolution (1/4°, 1/12°) regional models is also being built. The altimetric dataset will be used to perform a realistic simulation of the region circulations through data assimilation.

Melet, A.; Gourdeau, L.; Kessler, W.; Verron, J.

2007-12-01

273

Effects of sea ice dynamics on the Antarctic sea ice distribution in a coupled ocean atmosphere model  

Microsoft Academic Search

Impact of sea ice dynamics on the Southern Ocean sea ice distribution is investigated using a coupled ocean-sea ice-atmosphere general circulation model (OAGCM) and a separate offline sea ice model driven by monthly mean climatological boundary conditions. Sea ice dynamics considerably affects sea ice distribution of the OAGCM as well as of the offline model. When sea ice dynamics (advection)

T. Ogura; A. Abe-Ouchi; H. Hasumi

2004-01-01

274

Magnetohydrodynamic sea water propulsion  

SciTech Connect

An experimental and theoretical investigation of a large scale MHD propulsor has been undertaken whose objectives are to (1) investigate the transient and steady state performance of the thruster over operating parameter ranges that are compatible with achievement of high efficiency, (2) to quantify the principal loss mechanisms within the thruster and (3) to obtain preliminary hydroacoustic data. The performance of the thruster was first investigated theoretically with a 3-D code to quantify the loss mechanisms and identify experimental parameter ranges of interest. The loss mechanisms of interest are ohmic losses within the channel and those resulting from electrical currents at the entrance and exit of the thruster, and enhanced frictional losses. The analysis indicated that the relative importance of the loss mechanisms was a function of the thruster design and operating parameters. The experimental investigation of the large scale propulsor is being conducted on a sea water test facility that was designed to match the capabilities of a large 6-T superconducting magnet. The facility design was such that {approximately}90{degrees} of all losses occurred within the propulsion test train (inlet nozzle, propulsor and diffuser) thus facilitating isolation of the loss mechanisms. The test thruster itself is heavily instrumented to provide local measurements of velocity, pressure, and electric fields. The predicted overall thruster performance and value of the loss mechanisms will be compared with measured values. Comparisons will also be presented of the voltage gradients between electrodes, overall thruster efficiency, axial pressure gradients across the propulsor, change in velocity profiles, axial and vertical current distributions and exit distribution of the electrolytic gases.

Petrick, M.; Thomas, A.; Genens, L.; Libera, J.; Nietert, R.; Bouillard, J.; Pierson, E.; Hill, D.; Picologlou, B.; Ohlsson, O.; Kasprzyk, T.; Berry, G.

1991-01-01

275

Magnetohydrodynamic sea water propulsion  

SciTech Connect

An experimental and theoretical investigation of a large scale MHD propulsor has been undertaken whose objectives are to (1) investigate the transient and steady state performance of the thruster over operating parameter ranges that are compatible with achievement of high efficiency, (2) to quantify the principal loss mechanisms within the thruster and (3) to obtain preliminary hydroacoustic data. The performance of the thruster was first investigated theoretically with a 3-D code to quantify the loss mechanisms and identify experimental parameter ranges of interest. The loss mechanisms of interest are ohmic losses within the channel and those resulting from electrical currents at the entrance and exit of the thruster, and enhanced frictional losses. The analysis indicated that the relative importance of the loss mechanisms was a function of the thruster design and operating parameters. The experimental investigation of the large scale propulsor is being conducted on a sea water test facility that was designed to match the capabilities of a large 6-T superconducting magnet. The facility design was such that {approximately}90{degrees} of all losses occurred within the propulsion test train (inlet nozzle, propulsor and diffuser) thus facilitating isolation of the loss mechanisms. The test thruster itself is heavily instrumented to provide local measurements of velocity, pressure, and electric fields. The predicted overall thruster performance and value of the loss mechanisms will be compared with measured values. Comparisons will also be presented of the voltage gradients between electrodes, overall thruster efficiency, axial pressure gradients across the propulsor, change in velocity profiles, axial and vertical current distributions and exit distribution of the electrolytic gases.

Petrick, M.; Thomas, A.; Genens, L.; Libera, J.; Nietert, R.; Bouillard, J.; Pierson, E.; Hill, D.; Picologlou, B.; Ohlsson, O.; Kasprzyk, T.; Berry, G.

1991-12-31

276

SeaWinds - Greenland  

NASA Technical Reports Server (NTRS)

The frequent coverage provided by NASA's SeaWinds instrument on the QuikScat satellite provides unprecedented capability to monitor daily and seasonal changes in the key melt zones of Greenland, which is covered with a thick ice sheet that resulted from snow accumulating over tens of thousands of years. The thickness of the snow layers reveals details about the past global climate, and comparing snow accumulation and snow melting can provide insight into climate change and global warming. In particular, the extent of summer melting of snow in Greenland is considered a sensitive indicator of global change.

Earlier scatterometer data has suggested that Greenland has experienced significantly more melting in recent years. This figure compares the melting observed over 15 days during July 1999 in Greenland. The red areas around the central blue and white areas are the main melt zones and have lower radar back scatter because of water on the surface that saturates the surface snow. As the days warm up, the melt extent dramatically increases. Comparing this data with computer models and past scatterometer data will help scientists evaluate the inter-annual variability of the melting as a step toward understanding potential climate change.

The world's large ice sheets in Greenland and Antarctica act as vast storehouses of freshwater. Summer season melting releases large quantities of freshwater into the ocean, and year-to-year variations can have a significant impact on global sea level. Furthermore, long-term changes in the patterns and extent of melting on the large ice sheets reflect the effects of climate variability; thus Greenland is considered a sensitive indicator of global warming.

Satellite microwave radars are extremely sensitive to melting and can provide the only effective means of accurately measuring the year-round picture of the extent and variability in ice sheet melting. Daily mean images were produced from QuikScat data collected over the Greenland ice sheet at the height of the present summer melt period. In the top row, four images are shown at intervals of 5 days, for (a) day 203, (b) 208,(c) 213, and (d) 218 in 1999. Blue and white colors indicate surfaces which are cold and dry, while read and black indicate wet snow surfaces experiencing melting. The coastal regions are lower in elevation and begin to melt first. As summer progresses, the area of melting expands inland and northwards along the western coast of Greenland as air temperatures warm. A large pale and dark blue region in the central, high-elevation part of the ice sheet survives each summer without experiencing any melting. This is known as the dry snow region, and its area is a measure of the stability of the central part of the ice sheet. The line dividing the melt area and the dry snow is very sensitive to climate conditions and monitoring this line will help scientists determine whether the Earth's climate is changing.

The lower series of four images shows the daily variability in the radar data within each image. White patches in these images identify regions where the most rapid changes are taking place. Air temperature and precipitation variations are responsible for the patterns, with the greatest impact over the southern tip of Greenland occurring from storms originating over the Atlantic. Note that the red areas of central and northern Greenland experience much smaller or slower changes, with the central ice sheet showing little change during this summer period.

With its frequent coverage, the SeaWinds instrument is a power and unique tool for monitoring the health of the large ice sheets. The continuing time-series of data is a valuable contribution to assessments of the effects and impact of global change in the polar regions.

NASA's Earth Science Enterprise is a long-term research and technology program designed to examine Earth's land, oceans, atmosphere, ice and life as a total integrated system. JPL is a division of the California Institute of Technology, Pasadena

1999-01-01

277

Sea Ice, an Antarctic Habitat  

NSDL National Science Digital Library

A 'click-and-learn' sub site hosted by the Alfred Wegener Institute Foundation for Polar and Marine Research (AWI), this is a succinct, educational tour of sea-ice and its associated ecological communities. Short synopses introduce the dynamics of sea-ice formation, the microstructure of sea-ice (including crystal structure, brine channels, and ice algae), the effects of ice melt on resident organisms, the logistics of sea-ice research, and _land fast-ice_ and platelet ice habitats. Introductions also exist for the following organisms: krill; whales (i.e., Orcas, southern bottlenosesd dolphins, minke whales); sea birds (i.e., skuas and snow petrals), penguins (i.e., emperor, adelie, and chinstraps), and seals (i.e., weddell, crabeater, leopard, and ross.) Enlargeable thumbnail images accompany the habitat and inhabitant descriptions. Further investigations (at an accelerated level) are prompted with the inclusion of bibliographic references and scientific research presentations (in PDF format) on fast-ice and platelet ice, as well as links to the main site for the AWI.

278

Internal and external forcing of sea level variability in the Black Sea  

NASA Astrophysics Data System (ADS)

The variability of sea level in the Black Sea is forced by a combination of internal and external processes of atmospheric, oceanic, and terrestrial origin. We use a combination of satellite altimetry and gravity, tide gauge, river discharge, and atmospheric re-analysis data to provide a comprehensive up-to-date analysis of sea level variability in the Black Sea and to quantify the role of different environmental factors that force the variability. The Black Sea is part of a large-scale climatic system that includes the Mediterranean and the North Atlantic. The seasonal sea level budget shows similar contributions of fresh water fluxes (precipitation, evaporation, and river discharge) and the Black Sea outflow, while the impact of the net surface heat flux is smaller although not negligible. We find that the nonseasonal sea level time series in the Black and Aegean seas are significantly correlated, the latter leading by 1 month. This lag is attributed to the adjustment of sea level in the Black Sea to externally forced changes of sea level in the Aegean Sea and to the impact of river discharge. The nonseasonal sea level budget in the Black Sea is dominated by precipitation and evaporation over the sea itself, but external processes such as river discharge and changes in the outflow can also cause some large synoptic-scale sea level anomalies. Sea level is strongly coupled to terrestrial water storage over the Black Sea drainage basin, which is modulated by the North Atlantic Oscillation (NAO). We show that during the low/high NAO southwesterly/northeasterly winds near the Strait of Gibraltar and southerly/northerly winds over the Aegean Sea are able to dynamically increase/decrease sea level in the Mediterranean and Black seas, respectively.

Volkov, Denis L.; Landerer, Felix W.

2015-02-01

279

ConcepTest: Effect of Rain on Sea Level  

NSDL National Science Digital Library

A majority of Earth's water is in the oceans. Predict what would happen to sea level if rain fell continuously all over the world's oceans. a. Sea level would rise b. Sea level would fall c. Sea level ...

280

Future sea-level rise in the Mediterranean Sea  

NASA Astrophysics Data System (ADS)

Secular sea level variations in the Mediterranean Sea are the result of a number of processes characterized by distinct time scales and spatial patterns. Here we predict the future sea level variations in the Mediterranean Sea to year 2050 combining the contributions from terrestrial ice melt (TIM), glacial isostatic adjustment (GIA), and the ocean response (OR) that includes the thermal expansion and the ocean circulation contributions. The three contributions are characterized by comparable magnitudes but distinctly different sea-level fingerprints across the Mediterranean basin. The TIM component of future sea-level rise is taken from Spada et al. (2013) and it is mainly driven by the melt of small glaciers and ice caps and by the dynamic ice loss from Antarctica. The sea-level fingerprint associated with GIA is studied using two distinct models available from the literature: ICE-5G(VM2) (Peltier, 2004) and the ice model progressively developed at the Research School of Earth Sciences (RSES) of the National Australian University (KL05) (see Fleming and Lambeck, 2004 and references therein). Both the GIA and the TIM sea-level predictions have been obtained with the aid of the SELEN program (Spada and Stocchi, 2007). The spatially-averaged OR component, which includes thermosteric and halosteric sea-level variations, recently obtained using a regional coupled ocean-atmosphere model (Carillo et al., 2012), vary between 2 and 7 cm according to scenarios adopted (EA1B and EA1B2, see Meehl at al., 2007). Since the sea-level variations associated with TIM mainly result from the gravitational interactions between the cryosphere components, the oceans and the solid Earth, and long-wavelength rotational variations, they are characterized by a very smooth global pattern and by a marked zonal symmetry reflecting the dipole geometry of the ice sources. Since the Mediterranean Sea is located in the intermediate far-field of major ice sources, TIM sea-level changes have sub-eustatic values (i.e. they do not exceed the global average) and show little (but still significant) variations across the basin associated with the subsidence driven by the meltwater load. For year 2050, TIM calculations predict a sea-level rise of ~10 and ~30 cm for the mid range and the high end scenarios, respectively. Mainly because of the distinct mantle viscosity profiles adopted in ICE-5G(VM2) and KL05, the GIA patterns differ significantly and, in contrast with the TIM fingerprint, are both characterized by strong variations across the Mediterranean Sea, showing maximum values in the bulk of the basin. For the OR component, a significant geographical variation is observed across the Mediterranean sub-basins, corresponding to different Atlantic boundary conditionsAccording to this study, the total future sea-level rise for year 2050 will reach maximum values for the extreme scenario (hig-hend prediction for TIM, KL05 for GIA and EA1B2 for OR) of ˜ 27 cm in average with peak of ˜ 30 cm in the central sub-basins. Our results show that when these three components of future sea-level rise are simultaneously considered, the spatial variability is enhanced because of the neatly distinct geometry of the three fingerprints. References: Carillo, A., Sannino, G., Artale, V., Ruti, P., Calmanti, S., DellAquila, A., 2012, Clim. Dyn. 39 (9-10), 2167-2184; Fleming, K. and Lambeck, K., 2004, Quat. Sci. Rev. 23 (9-10), 1053-1077; Meehl, G.A., and 11 others, 2007, in Climate Change 2007: The Physical Science Basis, Cambridge University Press; Peltier W.R., 2004, Annu. Rev. Earth Pl. Sc., 32, 111-149; Spada, G. and Stocchi, P., 2007, Comput. and Geosci., 33(4), 538-562; Spada G., Bamber J. L., Hurkmans R. T. W. L., 2013, Geophys. Res. Lett., 1-5, 40.

Galassi, Gaia; Spada, Giorgio

2014-05-01

281

Orientation and open-sea navigation in sea turtles  

PubMed

Loggerhead sea turtle hatchlings (Caretta caretta L.) emerge from underground nests, scramble to the sea and begin a transoceanic migration by swimming away from their natal beach and into the open ocean. Evidence suggests that hatchlings sequentially use three different sets of cues to maintain orientation during their initial migration offshore. While on the beach, hatchlings find the ocean by crawling towards the lower, brighter seaward horizon and away from the dark, elevated silhouettes of vegetation and dunes. Upon entering the ocean, turtles initially orient seawards by swimming into waves, which can be detected as orbital movements from under water. Laboratory experiments have demonstrated that turtles can transfer a course initiated on the basis of waves or visual cues to a course mediated by a magnetic compass. Thus, by setting a magnetic course on the basis of nearshore cues that indicate the seaward direction, hatchlings may continue on offshore headings after entering deep water beyond sight of land. Sea turtles may use the earth's magnetic field not only as a cue for compass orientation but also as a source of world-wide positional information. Recent experiments have demonstrated that loggerheads can detect subtle differences in magnetic field inclination and intensity, two geomagnetic features that vary across the surface of the earth. Because most nesting beaches and oceanic regions are marked by a unique combination of these features, these findings raise the possibility that adult sea turtles navigate using a bicoordinate magnetic map. PMID:9317364

Lohmann; Lohmann

1996-01-01

282

SeaWorld Snack Shop - SeaWorld Classroom Activity  

NSDL National Science Digital Library

In this problem-solving activity, challenges students to take on the role of a Food Services Manager placing orders for a snack shop at Sea World. To solve the problem they will use data and proportional reasoning to make predictions and communicate findings.

Sea World - Just for Teachers

2012-05-06

283

Sea Otter Pup Wants the Worm  

USGS Multimedia Gallery

A sea otter pup watches eagerly as its mother eats a fat innkeeper worm in Monterey Bay, California. USGS scientists study sea otters in efforts to help the threatened species continue to recover from near extinction....

284

The quest for sea-floor integrity  

NASA Astrophysics Data System (ADS)

The status of sea floors is an important part of healthy marine ecosystems and intact coastlines. We need laws and a sea-floor management regime to make the exploitation of marine resources sustainable.

Markus, Till; Huhn, Katrin; Bischof, Kai

2015-03-01

285

Isotopic Composition and Origin of the Red Sea and Salton Sea Geothermal Brines  

Microsoft Academic Search

Deuterium and oxygen-18 measurements show that the Red Sea and Salton Sea brines are the results of a single process, the leaching of sediments by surface water circulating downward to a geothermal reservoir. The Salton Sea brine is derived from local precipitation but the Red Sea brine originates 1000 kilometers south of its basin, on the shallow sill which controls

H. Craig

1966-01-01

286

Revisions to the Steller Sea Lion Protection Measures for the Bering Sea and Aleutian Islands  

E-print Network

Revisions to the Steller Sea Lion Protection Measures for the Bering Sea and Aleutian Islands of the environmental, social, and economic effects of alternatives to the Steller sea lion protection measures and Pacific cod fisheries. The western distinct population segment (WDPS) of Steller sea lion is listed

287

Geophysical Aspects of Sea-ice Nomenclatures  

NSDL National Science Digital Library

This reference discusses the evolution of nomenclature for sea ice, originally developed for polar travel, and how it is seen from a geophysical perspective, particularly ocean-ice-atmosphere interaction or remote sensing. The site includes links to a number of student papers on sea-ice geophysics that provide background and material for discussion on the geophysical aspects of sea-ice nomenclatures. There is also a link to a pictorial glossary of sea ice terms and evolution.

288

Phytoplankton blooms beneath the sea ice in the Chukchi sea  

NASA Astrophysics Data System (ADS)

In the Arctic Ocean, phytoplankton blooms on continental shelves are often limited by light availability, and are therefore thought to be restricted to waters free of sea ice. During July 2011 in the Chukchi Sea, a large phytoplankton bloom was observed beneath fully consolidated pack ice and extended from the ice edge to >100 km into the pack. The bloom was composed primarily of diatoms, with biomass reaching 1291 mg chlorophyll a m-2 and rates of carbon fixation as high as 3.7 g C m-2 d-1. Although the sea ice where the bloom was observed was near 100% concentration and 0.8-1.2 m thick, 30-40% of its surface was covered by melt ponds that transmitted 4-fold more light than adjacent areas of bare ice, providing sufficient light for phytoplankton to bloom. Phytoplankton growth rates associated with the under-ice bloom averaged 0.9 d-1 and were as high as 1.6 d-1. We argue that a thinning sea ice cover with more numerous melt ponds over the past decade has enhanced light penetration through the sea ice into the upper water column, favoring the development of these blooms. These observations, coupled with additional biogeochemical evidence, suggest that phytoplankton blooms are currently widespread on nutrient-rich Arctic continental shelves and that satellite-based estimates of annual primary production in waters where under-ice blooms develop are ~10-fold too low. These massive phytoplankton blooms represent a marked shift in our understanding of Arctic marine ecosystems.

Arrigo, Kevin R.; Perovich, Donald K.; Pickart, Robert S.; Brown, Zachary W.; van Dijken, Gert L.; Lowry, Kate E.; Mills, Matthew M.; Palmer, Molly A.; Balch, William M.; Bates, Nicholas R.; Benitez-Nelson, Claudia R.; Brownlee, Emily; Frey, Karen E.; Laney, Samuel R.; Mathis, Jeremy; Matsuoka, Atsushi; Greg Mitchell, B.; Moore, G. W. K.; Reynolds, Rick A.; Sosik, Heidi M.; Swift, James H.

2014-07-01

289

[Multiple scattering of visible and infrared light by sea fog over wind driving rough sea surface].  

PubMed

The present paper is concerned with computing the multiple scattering characteristics of a sea fog-sea surface couple system within this context. The single scattering characteristics of sea fog were studied by Mie theory, and the multiple scattering of sunlight by single sea fog layer was studied by radiative transfer theory. The reflection function of a statistically rough ocean surface was obtained using the standard Kirchhoff formulation, with shadowing effects taken into account. The reflection properties of the combined sea fog and ocean surface were obtained employing the adding method, and the results indicated that the reflected light intensity of sea fog increased with the sea background. PMID:24159849

Sun, Xian-Ming; Wang, Hai-Hua; Lei, Cheng-Xin; Shen, Jin

2013-08-01

290

Isotopic composition and origin of the red sea and salton sea geothermal brines.  

PubMed

Abstract. Deuterium and oxygen-18 measurements show that the Red Sea and Salton Sea brines are the results of a single process, the leaching of sediments by surface water circulating downward to a geothermal reservoir. The Salton Sea brine is derived from local precipitation but the Red Sea brine originates 1000 kilometers south of its basin, on the shallow sill which controls the circulation of the Red Sea. On this sill sea water penetrates a thick evaporite sequence to a depth of 2000 meters, and, driven by its increased density relative to sea water, flows northward to emerge in the brine-filled deeps. PMID:17807292

Craig, H

1966-12-23

291

Salish Sea Act3vity Book  

E-print Network

Salish Sea Act3vity Book #12;Salish Sea . Salish sea is the traditional name for the inland stars (sometimes called starfish) are found along the northwest coast than anywhere else in the world in the quieter tidepools. Urchins eat algae, seaweed, and plankton (tiny floating plants). #12;The Giant Pacific

292

Sea Turtle Tracks at Nesting Site  

USGS Multimedia Gallery

A morning photo depicts evidence of a sea turtle nesting the previous night (from the sea, left; return to sea, right). The protective stakes mark a nest from an earlier week as part of a county research program that marks and records every eighth nest....

293

Environmental changes in the central Baltic Sea  

E-print Network

Environmental changes in the central Baltic Sea during the past 1000 years: inferences from Leibniz Institute for Baltic Sea Research Warnem¨unde (IOW), Seestrasse 15, D­18119 Warnem¨unde, Germany. Dippner, S. Hille et al. Ice Age), the environmental conditions of the central Baltic Sea were distinctly

Dippner, Joachim W.

294

Sea Ice Yearly Minimum in the Arctic  

NSDL National Science Digital Library

This series of visualizations show the annual Arctic sea ice minimum from 1979 to 2010. The decrease in Arctic sea ice over time is shown in an animation and a graph plotted simultaneously, but can be parsed so that the change in sea ice area can be shown without the graph.

GSFC/Science Visualization Studio

295

33 CFR 2.32 - High seas.  

Code of Federal Regulations, 2010 CFR

...2010-07-01 2010-07-01 false High seas. 2.32 Section 2.32 Navigation...JURISDICTION Jurisdictional Terms § 2.32 High seas. (a) For purposes of special...States as defined in 18 U.S.C. 7, high seas means all waters seaward of...

2010-07-01

296

Sea Grant: Enhancing K-12 Education.  

ERIC Educational Resources Information Center

Sea Grant is a major contributor to marine and aquatic education in K-12 classrooms through curriculum development, teacher education, school programs at field sites, and educational research. Describes Sea Grant's efforts in these areas. Specific programs outlined include Operation Pathfinder, Ohio Sea Grant Partnerships for Great Lakes…

Fortner, Rosanne W.

1998-01-01

297

AMSR-E Algorithm Theoretical Basis Document: Sea Ice Products  

E-print Network

1 AMSR-E Algorithm Theoretical Basis Document: Sea Ice Products Thorsten Markus and Donald J 20771 1. Overview The AMSR-E sea ice standard level 3 products include sea ice concentration, sea ice temperature, and snow depth on sea ice. The AMSR-E standard sea ice concentration product is generated using

Waliser, Duane E.

298

The Impact of Sea Surface Temperature Front on Stratus-Sea Fog over the Yellow and East China Seas  

NASA Astrophysics Data System (ADS)

A stratus-sea fog event occurred on 3 June 2011 over the Yellow and East China Seas (as shown in figure) is investigated observationally and numerically. Emphasis is put on the influences of the sea surface temperature front (SSTF) and of the synoptic circulations on the transition of stratus to sea fog. The southerly winds from a synoptic high pressure transport water vapor from the East China Sea to the Yellow Sea, while the subsidence induced by the high contributes to the formation of the temperature inversion on the top of the stratus or stratocumulus that appears mainly over the warm flank of a sea surface temperature front in the East China Sea. Forced by the SSTF, there is a secondary cell within the atmospheric boundary layer (ABL), with a sinking branch on the cold flank and a rising one on the warm flank of the SSTF. This sinking branch, in phase with the synoptic subsidence, forces the stratus or stratocumulus to lower in the elevation getting close to the sea surface as these clouds move northward driven by the southerly winds. The cloud droplets can either reach to the sea surface directly or evaporate into water vapor that may condense again when coming close to the cold sea surface to form fog. In this later case, the stratus and fog may separate. The cooling effect of cold sea surface counteracts the adiabatic heating induced by the subsidence and thus helps the transition of stratus to sea fog in the southern Yellow Sea. By smoothing the SSTF in the numerical experiment, the secondary cell weakens and the sea fog patches shrink obviously over the cold flank of the SSTF though the synoptic subsidence and moist advection still exist. A conceptual model is suggested for the transition of stratus to sea fog in the Yellow and East China Seas, which is helpful for the forecast of sea fog over these areas. The satellite visible image of the stratus-fog event. The fog appears in the Yellow Sea and the stratocumulus in the East China Sea.

Zhang, S.; Li, M.; Liu, F.

2013-12-01

299

Ploughing the deep sea floor.  

PubMed

Bottom trawling is a non-selective commercial fishing technique whereby heavy nets and gear are pulled along the sea floor. The direct impact of this technique on fish populations and benthic communities has received much attention, but trawling can also modify the physical properties of seafloor sediments, water–sediment chemical exchanges and sediment fluxes. Most of the studies addressing the physical disturbances of trawl gear on the seabed have been undertaken in coastal and shelf environments, however, where the capacity of trawling to modify the seafloor morphology coexists with high-energy natural processes driving sediment erosion, transport and deposition. Here we show that on upper continental slopes, the reworking of the deep sea floor by trawling gradually modifies the shape of the submarine landscape over large spatial scales. We found that trawling-induced sediment displacement and removal from fishing grounds causes the morphology of the deep sea floor to become smoother over time, reducing its original complexity as shown by high-resolution seafloor relief maps. Our results suggest that in recent decades, following the industrialization of fishing fleets, bottom trawling has become an important driver of deep seascape evolution. Given the global dimension of this type of fishery, we anticipate that the morphology of the upper continental slope in many parts of the world’s oceans could be altered by intensive bottom trawling, producing comparable effects on the deep sea floor to those generated by agricultural ploughing on land. PMID:22951970

Puig, Pere; Canals, Miquel; Company, Joan B; Martín, Jacobo; Amblas, David; Lastras, Galderic; Palanques, Albert

2012-09-13

300

Great Lakes Region Sea Grant  

NSDL National Science Digital Library

Site dedicated to the Great Lakes Sea Grant program. Information on GLSG priorities and initiatives. Topics of increased importance to the Great Lakes include fisheries and invasive species. Links to sites featuring publications and photos of Great Lakes storms and seiches and wildlife.

301

Great Lakes Region Sea Grant  

NSDL National Science Digital Library

This site is dedicated to the Great Lakes Sea Grant program. It provides information on the GLSG's priorities and initiatives. Topics of increased importance to the Great Lakes include fisheries and invasive species. Links to sites featuring publications and photos of Great Lakes storms and wildlife.

302

Sea Lamprey, an Invasive Fish  

USGS Multimedia Gallery

Invasive sea lamprey prey on commercially important fish species such as lake trout, living off of the blood and body fluids of adult fish.  It is one of many fish species that USGS scientists study from the USGS Research Vessel Muskie. These lamprey belong to the Great Lakes Fisheries Com...

303

Sea Lamprey, an Invasive Fish  

USGS Multimedia Gallery

Invasive sea lamprey prey on commercially important fish species such as lake trout, living off of the blood and body fluids of adult fish. It is one of many fish species that USGS scientists study from the USGS Research Vessel Muskie. These lamprey belong to the Great Lakes Fisheries Commissio...

304

Scour in the North Sea  

Microsoft Academic Search

Scour or seabed erosion around drilling and production platform legs and pipelines in the North Sea can be a major environmental problem because of the combination of shallow water depths, fast tidal currents, and mobile sand waves and banks. Considerable progress has been made in recent years toward understanding the mechanism of seabed scour around offshore platforms, but the North

T. N. Watson

1974-01-01

305

Tuna Sea Shell Pasta Ingredients  

E-print Network

Tuna Sea Shell Pasta Ingredients: 8 ounces pasta shells 12 ounces tuna in water, canned 1 onion 2. Cut the ends off of the onion, and peel off the brown layers. Run under water to remove any dirt. Cut the onion in half lengthwise, and place the flat side on the cutting board. Slice across the onion, from one

Liskiewicz, Maciej

306

Navigating the Seas of Policy.  

ERIC Educational Resources Information Center

As the sun, moon, and stars helped sea captains to navigate, policy (defined as a formalized idea to encourage change) indicates general direction and speed but does not establish a specific approach to achieve implementation. Formal and informal policies have advantages and disadvantages. These are steps in navigating policy formation: identify…

Cunningham, Stephanie; Kennedy, Steve; McAlonan, Susan; Hotchkiss, Heather

307

A Deep-Sea Simulation.  

ERIC Educational Resources Information Center

Describes an activity that simulates exploration techniques used in deep-sea explorations and teaches students how this technology can be used to take a closer look inside volcanoes, inspect hazardous waste sites such as nuclear reactors, and explore other environments dangerous to humans. (DDR)

Montes, Georgia E.

1997-01-01

308

Past and present Aral Sea  

NASA Astrophysics Data System (ADS)

The tragedy of disappearing of Aral Sea is well known to the World. Before and after collapse of Soviet Union, a huge quantity of scientific and popular editions described with grief the situation around the Aral Sea. After the NIS states became independent, World Bank, UNDP, UNEP in proper competition with each other had provided some assessment of the situation through presentation of some small and medium grants, but after 2000, the local population remained alone with own problems. Although on the eyes of the present generation a unique transformation of great water body into deserts took place, the global scientific community did not find forces and financing for real and detail investigation of the processes accompanying the Sea shrinking and land formation. We should acknowledge and give big respect to NATO, later to German Government that through GTZ (now GIZ) - German International Collaboration Agency - and GFZ (Potzdam) paid attention to this area of environment crisis and organized scientific and protective design in the so-called Priaralie - the territory around the drying Sea and delta of the two rivers - Amudarya and Syrdarya. Thank to this assistance, the local specialists in collaboration with limited a number of foreign scientists (N.Aladin, P.Zavialov, Joop de Schutter, Hans Wilps, Hedi Oberhansli) organized significant works for detail socioeconomic, ecological and hydrological assessment situation in Priaralie and on the Aral sea coast. On this base, Ministry of Agriculture and Water resources of Uzbekistan and State Committee of Water resources of Kazakhstan developed a plan of rehabilitation of Amudarya and Syrdarya deltas and started implementation of these projects. If Kazakh water authority moved ahead in wetland restoration faster, a forestation of delta and drying bed of Aral Sea got big success in Uzbek territory. 244 thousands hectares of saxsaul and tamarix were planted for protection of the Priaralie. By request of GTZ SIC, ICWC organized in 2005-2009 sixth expeditions for complex remote sensing and ground investigations Aral Sea former bottom that were complemented in 2010 -2011 by two expeditions with GFZ. As a result, the landscape, soils and environment mapping was done with determination of ecologically unstable zones and assessment total change of lands situation compared with the pre-independence time. Moreover - methodic of monitoring water, environment and hydro geological indicators on the all deltas area was elaborated, organized its testing and combined with remote sensing data on Amudarya delta for 2009-2012. It permits to SIC ICWC to organize systematic permanent (decadal) monitoring and recording of size, volume and level of water in Aral Sea. Since the beginning of regular observations over the Aral Sea level, 2 periods can be emphasized: 1. Conditionally natural period - 1911-1960 - characterized by a relatively stable hydrological regime, with fluctuations in the level around 53 m and the range of inter-annual fluctuations at no more than 1 m., when the sea received annually about a half of the run-off in the Syrdarya and Amudarya Rivers, i.e. 50-60 km3/yr. 2. Intensive anthropogenic impact period - since the 1960s, a vast extension of irrigable land was carried out in Central Asia that resulted in intensive diversion of river run-off. Since then, the sea level has been falling steadily, causing a dramatic reduction in the water surface area, a decrease in water volume and depths, great changes in shoreline configuration and an expansion of the desert areas adjacent to the Aral Sea. From 1960-1985, when the sea was an integral water body, slight lowering in the sea level took place until the 1970s, when the sea-level decreased with the mean level lowering 1 m. The desiccation process accelerated visibly from the mid 1970s. In 1975-1980, the level decreased by 0.65 m a year on average. Moreover, the level dropped greatly, when the run-off of the Amudarya did not reach the Aral Sea any more (1980-1990). Kokaral was the first of the large islands becoming a peninsula, separa

Dukhovniy, Viktor; Stulina, Galina; Eshchanov, Odylbek

2013-04-01

309

TROPICAL ATLANTIC/ Warmer sea surface  

E-print Network

in atmospheric pressure and its associated impacts are known as the North Atlantic Oscillation (NAO). #12;-south contrast in sea level pressure over the North Atlantic Ocean, with low pressure in the north near Iceland and high pressure in the south near the Azores. The pressure contrast drives surface winds and wintertime

310

SEA K-12 Lesson Plans  

NSDL National Science Digital Library

Award-winning ideas from SEA Semester's educators. This collection of over 25 lesson plans covers topics in marine biology, coastal ecology, chemical and physical oceanography, seafloor geology and nautical science. Each plan includes target grades, keywords, introduction and background, advice on how to best integrate the activities into classroom curriculum, instructions and tips, materials list, procedures, suggestions for evaluation, extensions.

311

Alaska SeaLife Center  

NSDL National Science Digital Library

Located in Seward, Alaska, the Alaska SeaLife Center is a non-profit marine science facility dedicated to understanding and maintaining the integrity of the marine ecosystem of Alaska through research, rehabilitation and public education. The Center's research and rehabilitation facilities and naturalistic exhibits immerse visitors in the dynamic marine ecosystems of Alaska. Includes links to additional resources for students and teachers.

312

Global Sea SurfaceTemperature  

NSDL National Science Digital Library

This illustration of Earth's sea surface temperature was obtained from two weeks of infrared observations by the Advanced Very High Resolution Radiometer (AVHRR), an instrument on board NOAA-7, during July 1984. Temperatures are color coded with red being warmest and decreasing through oranges, yellows, greens, and blues. The caption provides a brief description of the features seen in the image.

313

Tides of the British Seas  

ERIC Educational Resources Information Center

Examines the gravitational effects and the way that local conditions interact with these effects to produce the tides characteristic of the British seas. Presents some effects of tides including the possibility of harnessing tidal energy and the effect of tidal friction on the use of the earth as a clock. (GS)

Sandon, Frank

1975-01-01

314

Sea Grant Nonindigenous Species (SGNIS)  

NSDL National Science Digital Library

Sea Grant's award winning, comprehensive exotic species resource center with everything from educational materials to research findings on a variety of exotic species. Site features peer-reviewed literature, unreviewed publications, and the outreach section includes a searchable database of reference material covering all aspects of nonindigenous species, including individual exotic species. Also features an outstanding kid's section containing games and information on exotics.

315

Sea Lion Skeleton (Gliding Joint)  

NSDL National Science Digital Library

Sea lions are vertebrates with both backbones and ribs. The backbone is a gliding joint, allowing the animal to be flexible, while the ribs main function is to protect it's inner organs. The short tail helps to balance the animal while walking on land.

Ketan Patel (California State University, Fullerton; Student, B)

2007-07-14

316

Westward intensification in marginal seas  

NASA Astrophysics Data System (ADS)

An idealized model was used to examine why the strong western boundary current (WBC) is observed in the South China Sea (SCS) but not in the Gulf of Mexico (GOM) and Japan/East Sea (JES). Results suggested that the stronger WBC in the SCS is mainly attributed to the direct contribution of the inflow and the strong monsoon. Although the Gulf Stream transports a large amount of water into the GOM, the passage in the southeast corner guides the inflow out of the gulf and inhibits the inflow from intensifying the WBC. Meanwhile, the wind stress in the GOM is weakest among the three marginal seas. The meridional ocean ridge and the particular layout of the continental slope of JES prevent the whole basin from participating in the westward intensification. Besides, the throughflow has adverse effects on the formulation of WBC in JES. The variation of Coriolis parameter with latitude leads to the westward intensification in marginal seas. However, a strong WBC cannot be observed in the absence of reasonable collocation of wind, inflow, and topography.

Chen, Gengxin; Xue, Huijie

2014-03-01

317

Distribution characteristics of marine litter on the sea bed of the East China Sea and the South Sea of Korea  

NASA Astrophysics Data System (ADS)

The types, quantities, and distribution of marine litter found on the sea bed of the East China Sea and the South Sea of Korea are surveyed. Surveys were evaluated using bottom trawl nets during 1996-2005 cruises. Mean distribution densities were high in coastal seas, especially in the South Sea of Korea offshore from Yeosu, with 109.8 kg km -2, and low in the East China Sea, with densities of 30.6 kg km -2. Fishing gear, such as pots, nets, octopus jars, and fishing lines, accounted for about 42-72% and 37-62% of litter items in the East China Sea and the South Sea of Korea, respectively, whereas the contributions of rubber, vinyl, metal, plastic, glass, wood, and clothing were below 30% mainly. Rope and drum composition fluctuated greatly, between 54% and 0%. Eel and net pots dominated the marine debris of the South Sea of Korea, and some vinyl, plastics, and fishing gear made in Korea, China, and Japan were collected in abundance in the East China Sea. Fishing gear was probably discarded into the sea, deliberately or inadvertently, by fishing operations. A comprehensive joint approach by Korea, China, and Japan is needed for the continuous monitoring of input sources, the actual conditions, and the behavior of marine litter for protection against litter pollution and fisheries resource management in this area.

Lee, Dae-In; Cho, Hyeon-Seo; Jeong, Sun-Beom

2006-10-01

318

Facing up to sea rise.  

PubMed

A milder and less extreme climate, abundance of fish and mollusks, transport and communication, and fertile land at low altitudes have drawn humans to coastal areas and river valleys for centuries. More than 60% of the world's population occupy the 150 km closest to the coast. Millions of tourists come to coastlines and small tropical islands for recreation. About 80% of the global fish supply originates from the 19 km closest to the shore. Fish are the only protein source for the rapidly growing populations in many developing countries. Global climate change is increasing the sea level so much that by 2050, the mean increase will be about 38 cm (24-52 cm). The Intergovernmental Panel on Climate Change (IPCC) notes that the effects of sea level rise will differ from place to place. Direct effects are flooding of low-lying coastal areas and increased erosion rates. An indirect effect includes higher water tables and intrusion of saline water into aquifers, resulting in loss of fresh ground water resources. These effects may make coastal areas less suitable for settlement and agriculture. Coral sand settled on top of coral reefs makes up the unstable, small atoll islands of the Pacific and Indian Oceans. People on these islands depend almost entirely on the sea for their livelihood and on the small amount of fresh water with which they grow root crops and drink. Rising sea levels also threaten low lying countries, e.g., Bangladesh, and densely populated deltas, e.g., the Nile. Changes in the frequency and severity of flooding will increase Bangladesh's dependence on foreign aid. IPCC sees 3 possible responses to the rising sea level: defense, retreat, and accommodation. Accommodation is the only practical choice for many developing countries. A switch from rice cultivation to mariculture of prawns and fish is an example of accommodation. We need to more completely understand the natural processes in coastal environments to be better prepared for climate change. PMID:12287486

Pernetta, J

1994-01-01

319

Management of the Wadden Sea  

NASA Astrophysics Data System (ADS)

The Wadden Sea situated along the North Sea coasts of Denmark, the Federal Republic of Germany and The Netherlands represents one of the world's largest bar-built type of estuaries. The area is a typical sedimentation and mineralization basin, with a large influx of organic matter from the adjoining North Sea, consequently a delicate oxygen balance and a rich benthic macrofauna, poor in species, which serves as food for juveniles of some commercially important North Sea fishes and for large numbers of migrating and wintering waders and waterfowl. Past and present activities of the human society in the area include fisheries (mainly for shrimp and mussels, semi-culture), shipping, land reclamation, recreation, dredging for sand and shells, and waste discharge from industries and human communities. Until the present these activities, although sometimes conflicting, did not fundamentally affect the area and its biota (pollution excluded), but future claims, including the construction of large deep-sea harbours, drilling for natural gas and oil, large-scale land reclamation and increased industrialization etc., might gradually induce degradation. For instance, area reduction by continued land reclamation could lead to irreversible losses of specific biotopes (e. g. salt-marshes, mud-flats), which could affect the size of bird and fish populations in a much wider region. Increased pollution, which has already inflicted damage on bird and seal populations, could reduce the fauna and hence the value of the area as a natural sanctuary. In the event of a proposal for a new human activity in the area, the present standing practice in the countries concerned requires an evaluation of its safety and economic aspects and its environmental impact. However, the various plans are considered separately and there is a general need for integrated management of the area.

Wolff, W. J.; Zijlstra, J. J.

1980-03-01

320

Thermal biology of sea snakes and sea kraits.  

PubMed

Temperature probably had no direct effect on the evolution of sea kraits within their center of origin, a geologically stable thermal zone straddling the equator, but may have indirectly affected expansions and contractions in distributions beyond that zone through global fluctuations that caused alternation of higher and lower sea levels. The northern limit of the Laticauda colubrina complex seems to be the 20°C isotherm; in the south, the range does not reach that isotherm because there is no land (also a habitat requirement of sea kraits) within the zone of suitable temperature. The relationship of temperature to the pattern of geographic variation in morphology supports either the hypothesis of peripheral convergence or the developmental hypothesis but does not distinguish between them. Quadratic surfaces relating cumulative scores for coloration and morphological characters to global position showed a strong latitudinal component and an even stronger longitudinal one in which the direction of the latitudinal effect was reversed between east and west. A multivariate analysis revealed that while morphological characters vary significantly by location and climate when tested separately, when the influence of location on morphology is taken into account, no residual relationship between climate and morphology remains. Most marine snakes have mean upper temperature tolerances between 39°C and 40°C and operate at temperatures much nearer their upper thermal limits than their lower limits but still avoid deleterious extremes by diving from excessively hot water to deeper, cooler strata, and by surfacing when water is cold. At the surface in still water in sunlight, Pelamis can maintain its body temperature slightly above that of the water, but whether this is significant in nature is questionable. As temperature falls below 18-20°C, survival time is progressively reduced, accompanied by the successive occurrence of cessation of feeding, cessation of swimming, and failure to orient. Acclimation does not seem to be in this species' repertoire. In the water column, marine snakes track water temperature; on land, sea kraits can thermoregulate by basking, selecting favorable locations, and by kleptothermy. Laticauda colubrina adjusts its reproductive cycle geographically in ways that avoid breeding in the coldest months. Mean voluntary diving time is not temperature-dependent within the normal range of temperatures experienced by marine snakes in the field, but is reduced in water colder than 20°C. On land, much as while diving in the sea, sea kraits maintain long periods of apnea; intervals between breaths are inversely related to temperature. PMID:22669175

Heatwole, Harold; Grech, Alana; Monahan, John F; King, Susan; Marsh, Helene

2012-08-01

321

Flavor Structure of Intrinsic Nucleon Sea  

NASA Astrophysics Data System (ADS)

The concept of intrinsic charm suggested by Brodsky et al. is extended to lighter quarks. Extraction of the intrinsic ?, d¯, and s¯ seas is obtained from an analysis of the d¯ - ?, s + s¯, and ? + d¯ - s -s¯ distributions. The connection between the intrinsic/extrinsic seas and the connected/disconnected seas in lattice QCD is also examined. It is shown that the connected and disconnected components for the ?(x) + d¯(x) sea can be separated. The striking x-dependence of the [s(x) + s¯(x)]/[?(x) + d¯(x)] ratio is interpreted as an interplay between the connected and disconnected seas.

Peng, Jen-Chieh; Chang, Wen-Chen; Cheng, Hai-Yang; Liu, Keh-Fei

2015-01-01

322

Ecological consequences of sea-ice decline.  

PubMed

After a decade with nine of the lowest arctic sea-ice minima on record, including the historically low minimum in 2012, we synthesize recent developments in the study of ecological responses to sea-ice decline. Sea-ice loss emerges as an important driver of marine and terrestrial ecological dynamics, influencing productivity, species interactions, population mixing, gene flow, and pathogen and disease transmission. Major challenges in the near future include assigning clearer attribution to sea ice as a primary driver of such dynamics, especially in terrestrial systems, and addressing pressures arising from human use of arctic coastal and near-shore areas as sea ice diminishes. PMID:23908231

Post, Eric; Bhatt, Uma S; Bitz, Cecilia M; Brodie, Jedediah F; Fulton, Tara L; Hebblewhite, Mark; Kerby, Jeffrey; Kutz, Susan J; Stirling, Ian; Walker, Donald A

2013-08-01

323

Global Warming and Caspian Sea Level Fluctuations  

E-print Network

Coastal regions have a high social, economical and environmental importance. Due to this importance the sea level fluctuations can have many bad consequences. In this research the correlation between the increasing trend of temperature in coastal stations due to Global Warming and the Caspian Sea level has been established. The Caspian Sea level data has been received from the Jason-1 satellite. It was resulted that the monthly correlation between the temperature and sea level is high and also positive and almost the same for all the stations. But the yearly correlation was negative. It means that the sea level has decreased by the increase in temperature.

Ardakanian, Reza

2013-01-01

324

On the cloudiness and cloud types around the Black Sea, Caspian Sea and Aral Sea regions  

NASA Astrophysics Data System (ADS)

Ten years (2000-2010) of cloud ground observations from 332 synoptic stations (with 3h time resolution) for the regions around the Black Sea, the Caspian Sea and the Aral Sea were analyzed. The considered variables were: total cloud cover (TCLD), cloud cover from low or middle clouds (LMCLD), low cloud type (LCLD), middle cloud type (MCLD) and high cloud type (HCLD). Data analyses were carried out for the whole dataset and several subsets: cloudless observations, 1-layer observations, and multi-layer observations. For the whole dataset, the analyses included frequency of cloudy observations, frequency of multilayer observations, and mean TCLD. We studied also frequency of 1-layer of clouds only, and frequency of each type of clouds (low, middle, high). Results show a large spatial and seasonal variability with respect to TCLD, cloud types and the frequency of multilayer cloud observations. Moreover, over the ten-year period, the evolution of the annual mean TCLD is investigated, showing a positive trend in the northern region of the Black Sea. Acknowledgements: This work has been undertaken within the frame and support of the CLIMSEAS project FP7-IRSES-2009 (ref. 247512).

Badosa, J.; Dmitrieva, L. R.; Shatunova, M.; Chumako, M.; Khan, V.; Calbó, J.; González, J.-A.

2012-04-01

325

The distribution and diversity of sea cucumbers in the coral reefs of the South China Sea, Sulu Sea and Sulawesi Sea  

NASA Astrophysics Data System (ADS)

A study on the distribution and diversity of sea cucumbers in the coral reefs of the South China Sea, Sulu Sea and Sulawesi Sea was carried out in July 2009. The survey was done using wandering transect underwater with SCUBA. Twelve species of sea cucumber were found from four different families and nine genera. The most dominant family was Holothuriidae (five species), followed by Stichopodidae (three species), Synaptidae (three species) and Cucumariidae with only one species. The most dominant species found around the island was Pearsonothuria graffei, which can be found abundantly on substrate of dead corals in a wide range of depth (6-15 m). The Sulawesi Sea showed a higher diversity of sea cucumber with seven different species compared to the South China Sea with only six different species and Sulu Sea with only two species. Ordination by multidimensional scaling of Bray-Curtis similarities clustered the sampling locations to three main clusters with two outgroups. Previous studies done indicated a higher diversity of sea cucumber as compared to this study. This can be indication that the population and diversity of sea cucumbers in the reef is under threat.

Woo, Sau Pinn; Yasin, Zulfigar; Ismail, Siti Hasmah; Tan, Shau Hwai

2013-11-01

326

Sea ice as a source of sea salt aerosol: A trajectory study of 25 years of year-round sea salt aerosol record at Neumayer, Antarctica  

Microsoft Academic Search

Recently it was recognized that sea ice is a source of sea salt aerosols in coastal Antarctica, playing a more important role than open ocean during winter time. Frost flowers which grow on the surface of newly-formed sea ice are considered to contribute to the generation of sea salt aerosols. The exact mechanism of the release of sea salt aerosols

X. Tian-Kunze; L. Kaleschke; R. Weller; G. König-Langlo; D. Wagenbach; S. Rast; G. Santos; A. Richter; M. Begoin

2009-01-01

327

Alkenone production in the East Sea/Japan Sea  

NASA Astrophysics Data System (ADS)

To test the applicability of alkenones as a proxy for past sea surface temperature (SST) in the East Sea (Japan Sea), this study investigated the season and depth of alkenone production in the area. Surface and subsurface seawater samples were collected from the East Sea during cruises carried out by the National Fisheries Research and Development Institute of Korea in 2008-2010. Surface samples were filtered for suspended material at two-month intervals. Subsurface samples were collected at water depths of 20, 50, 70 and 100 m by CTD bottle casts at two stations, one a coastal station and the other an offshore station. The results of alkenone analysis show that the concentration of total C37 alkenones was generally high in the surface mixed layer and decreased with depth, indicating that alkenones were most likely produced in or close to the surface mixed layer. Alkenone concentration varied seasonally: high in spring to fall and significantly reduced in winter. Comparisons of alkenone-based temperatures with in situ seawater temperatures show that alkenone temperatures measured from suspended particles in the surface waters were close to in situ SST in summer but were lower in winter. During winter, when alkenone production is significantly reduced, alkenones may be suspended for relatively long times and are likely to be advected from the north by eddies from Subpolar Front meanders. In summer when new production of alkenones increases, the settling velocity of alkenones appears to increase and residence time becomes shorter than in winter, suggesting that particles are less likely to be significantly advected at that time. Importantly, at the offshore station, coretop alkenone temperature corresponds to annual-averaged SST, while at the coastal station it corresponds to summer-to-fall averaged SST.

Lee, Kyung Eun; Lee, Sunghye; Park, Yonggi; Lee, Ho Jin; Harada, Naomi

2014-02-01

328

Cabled ocean observatories in Sea of Oman and Arabian Sea  

NASA Astrophysics Data System (ADS)

An ocean observatory—consisting of a real-time, cabled array in the Sea of Oman and an internally recording, autonomous mooring array recently upgraded to a cabled array in the northern Arabian Sea—celebrated more than 2500 days of continuous operation in July 2012. The observatory, which measures a range of properties, such as water current velocities, temperature, salinity, pressure, dissolved oxygen, and turbidity, is part of the Lighthouse Ocean Research Initiative (LORI) project [du Vall et al., 2011], which was designed as a pilot project and installed in 2005 in the region off Abu Bakara (Figures 1a and 1b). The initial goal of the project was to prove that an in situ, cabled ocean observatory can return high-quality scientific data on a real-time basis over longer time periods than conventional moored systems. That same year, an autonomous array was deployed off Ras al Hadd and on Murray Ridge in the Arabian Sea (Figure 1a).

DiMarco, Steven F.; Wang, Zhankun; Jochens, Ann; Stoessel, Marion; Howard, Matthew K.; Belabbassi, Leila; Ingle, Stephanie; du Vall, Ken

2012-07-01

329

Variability and Trends in Sea Ice Extent and Ice Production in the Ross Sea  

NASA Technical Reports Server (NTRS)

Salt release during sea ice formation in the Ross Sea coastal regions is regarded as a primary forcing for the regional generation of Antarctic Bottom Water. Passive microwave data from November 1978 through 2008 are used to examine the detailed seasonal and interannual characteristics of the sea ice cover of the Ross Sea and the adjacent Bellingshausen and Amundsen seas. For this period the sea ice extent in the Ross Sea shows the greatest increase of all the Antarctic seas. Variability in the ice cover in these regions is linked to changes in the Southern Annular Mode and secondarily to the Antarctic Circumpolar Wave. Over the Ross Sea shelf, analysis of sea ice drift data from 1992 to 2008 yields a positive rate of increase in the net ice export of about 30,000 sq km/yr. For a characteristic ice thickness of 0.6 m, this yields a volume transport of about 20 cu km/yr, which is almost identical, within error bars, to our estimate of the trend in ice production. The increase in brine rejection in the Ross Shelf Polynya associated with the estimated increase with the ice production, however, is not consistent with the reported Ross Sea salinity decrease. The locally generated sea ice enhancement of Ross Sea salinity may be offset by an increase of relatively low salinity of the water advected into the region from the Amundsen Sea, a consequence of increased precipitation and regional glacial ice melt.

Comiso, Josefino; Kwok, Ronald; Martin, Seelye; Gordon, Arnold L.

2011-01-01

330

Micromechanics of Sea Urchin Spines  

PubMed Central

The endoskeletal structure of the Sea Urchin, Centrostephanus rodgersii, has numerous long spines whose known functions include locomotion, sensing, and protection against predators. These spines have a remarkable internal microstructure and are made of single-crystal calcite. A finite-element model of the spine’s unique porous structure, based on micro-computed tomography (microCT) and incorporating anisotropic material properties, was developed to study its response to mechanical loading. Simulations show that high stress concentrations occur at certain points in the spine’s architecture; brittle cracking would likely initiate in these regions. These analyses demonstrate that the organization of single-crystal calcite in the unique, intricate morphology of the sea urchin spine results in a strong, stiff and lightweight structure that enhances its strength despite the brittleness of its constituent material. PMID:22984468

Tsafnat, Naomi; Fitz Gerald, John D.; Le, Hai N.; Stachurski, Zbigniew H.

2012-01-01

331

Journey to Deep Sea Vents  

NSDL National Science Digital Library

This fun Web article is part of OLogy, where kids can collect virtual trading cards and create projects with them. Here, they learn about deep sea vents. Kids are introduced to these underwater geysers and to the Alvin submersible by Ro Kinzler, an Earth scientist at the Museum. They then have the opportunity to travel to the bottom of the ocean aboard a virtual submersible, learning about the zones they pass through and their inhabitants. A game allows kids to explore and collect specimens from one of the mineral chimneys found at a deep sea vent. When they have collected all nine living things at the vent, they are rewarded with a desktop image.

332

Swimming with Sea Cows: Manatees  

NSDL National Science Digital Library

When manatees were first seen by Columbus, he thought they were mermaids..but he had been at sea for a long time! Today these gentle marine mammals are threatened by loss of habitat and collisions with boats. This video segment explores the endangered manatees of Florida and their struggle to survive, as well as some of the people who are working to save them. Please see the accompanying lesson plan for educational objectives, discussion points and classroom activities.

2012-07-19

333

Fracture of multiyear sea ice  

Microsoft Academic Search

The fracture and flow of multiyear sea ice was investigated under triaxial compression and uniaxial tension in the temperature range -40 ø to -3.5øC, for strain rates from 10 -7 to 10 -2 s -1, and for confining pressures up to 30 MPa using 40 mm diameter specimens. Specimens both in the horizontal plane of the multiyear floe and perpendicular

P. R. Sammonds; S. A. F. Murrell; M. A. Rist

1998-01-01

334

Fracture of multiyear sea ice  

Microsoft Academic Search

The fracture and flow of multiyear sea ice was investigated under triaxial compression and uniaxial tension in the temperature range -40° to -3.5°C, for strain rates from 10-7 to 10-2s-1, and for confining pressures up to 30 MPa using 40 mm diameter specimens. Specimens both in the horizontal plane of the multiyear floe and perpendicular to this plane were tested.

P. R. Sammonds; S. A. F. Murrell; M. A. Rist

1998-01-01

335

Fracture of multiyear sea ice  

NASA Astrophysics Data System (ADS)

The fracture and flow of multiyear sea ice was investigated under triaxial compression and uniaxial tension in the temperature range -40° to -3.5°C, for strain rates from 10-7 to 10-2s-1 and for confining pressures up to 30 MPa using 40 mm diameter specimens. Specimens both in the horizontal plane of the multiyear floe and perpendicular to this plane were tested. The results of short-rod fracture toughness tests on multiyear and first-year sea ice at temperatures -20°C are also reported. The multiyear sea ice came from an unridged portion of a single floe about 7 m thick, which was found to be massive and not blocky with large voids. The ice had low salinity and high porosity. The inelastic deformation of multiyear sea ice was found to be strongly dependent upon strain rate, temperature, and confining pressure. In compression, four main types of deformation were observed. (1) Under uniaxial compression, completely brittle fracture at high strain rates (of 10-3 to 10-2 s-1) was characterized by multiple axial splitting. (2) Application of even a small confining pressure inhibited splitting, and fracture took place by the formation of a narrow shear fault inclined at 45±3°. (3) At higher confining pressures, plastic deformation accompanied substantial cracking activity. (4) However, at still higher confining pressures, cracking was completely inhibited and deformation was entirely plastic. At -20°C, shear fracture occurred according to a maximum shear stress criterion and hence was pressure independent, with crack nucleation dominating the fracture behavior. At -40°C, however, the shear fracture stress was found to be strongly pressure dependent up to 14 MPa and could be described in terms of a Coulombic failure envelope. The unusual 45° orientation of ice shear fractures, together with the unusual pressure dependencies of ice peak strengths, may be explained by the fact that low-stress slip and cleavage occurs in the basal planes of ice crystals.

Sammonds, P. R.; Murrell, S. A. F.; Rist, M. A.

1998-09-01

336

NOAA Teacher At Sea Program  

NSDL National Science Digital Library

Are you a teacher who is interested in oceanographic research? Does the idea of living aboard an ocean-going research vessel intrigue you? Would you like to work as a crew member on a one to three week scientific cruise? NOAA is looking for motivated teachers (K-16) with a desire to do scientific research at sea and share that experience with students and colleagues.

337

Primary productivity in the sea  

SciTech Connect

Recent progress in primary productivity is discussed in the book based on 27 symposia texts and 19 poster abstracts. Most papers deal with particular cellular processes in pelagic phytoplankton and their relationship to whole plant photosynthesis and growth. In addition, presentations on the productivity of the seaweed, Laminaria, zooxanthellae and whole corals are included. Other articles discuss predictive modeling, new developments in remote sensing, nutrient regeneration within the sea, grazing effects, and carbon cycling. (JMT)

Falkowski, P.G.

1980-01-01

338

Medusa Sea Floor Monitoring System  

NASA Technical Reports Server (NTRS)

The objective of the research described in this poster presentation is to develop technologies to enable fundamental research into understanding the potential for and limits to chemolithoautotrophic life. The Medusa Isosampler (isobaric sampler), for sampling fluids eminating from deep sea hydrothermal vents and cold seep sites analogous to extraterrestrial environments, is described by the presentation. The following instruments are integrated with the isosampler, and also described: in situ flow-through chemical sensor, intrinsic fluorescent-based microbial detector, isotope ratio spectral detector.

Flynn, Michael

2004-01-01

339

Salton Sea solar pond project  

NASA Technical Reports Server (NTRS)

The feasibility of constructing salt gradient solar ponds within the Salton Sea is being studied. These ponds would serve a dual purpose: (1) become a depository for unwanted salt and (2) supply thermal energy for driving turbine electric power systems. Under present circumstances, the rise in salinity is expected to eliminate fish life and create other unfavorable conditions. The proposed concept would have a power generation potential of 600 MWe.

French, R. L.; Meitlis, I.

1980-01-01

340

Ice Sheets and Sea Level  

NSDL National Science Digital Library

In this exercise, learners use basic arithmetic to determine the amount that sea level would rise around the globe with the melting of the Greenland and Antarctic ice sheets. Basic data for this calculation is provided. This resource is from PUMAS - Practical Uses of Math and Science - a collection of brief examples created by scientists and engineers showing how math and science topics taught in K-12 classes have real world applications.

2012-08-03

341

Arctic sea ice minimum extent  

NASA Astrophysics Data System (ADS)

The extent of Arctic sea ice dropped to 3.41 million square kilometers on 16 September, 760,000 square kilometers below the minimum ice extent in 2007, which had been the low mark since the satellite record began in 1979, the National Snow and Ice Data Center (NSIDC) announced. Overall ice extent is 50% below where it was in the 1970s, NSIDC research scientist Walt Meier said during a 19 September briefing. He added that there is also a decrease in ice thickness. Meier said that sea ice varies from year to year with lots of ups and downs. “We wouldn't expect it to keep going down, straight off the map so to speak,” he said. “Typically after a record low, we've seen it rebound.” Meier added that the general long-term trend is for the Arctic to continue to become generally ice free. He said it is difficult to know how long it will take for that condition to be reached; because of strong variations, Arctic sea ice extent could plateau for some time.

Showstack, Randy

2012-10-01

342

MODIS Global Sea Surface Temperature  

NASA Technical Reports Server (NTRS)

Every day the Moderate-resolution Imaging Spectroradiometer (MODIS) measures sea surface temperature over the entire globe with high accuracy. This false-color image shows a one-month composite for May 2001. Red and yellow indicates warmer temperatures, green is an intermediate value, while blues and then purples are progressively colder values. The new MODIS sea surface temperature product will be particularly useful in studies of temperature anomalies, such as El Nino, as well as research into how air-sea interactions drive changes in weather and climate patterns. In the high resolution image, notice the amazing detail in some of the regional current patterns. For instance, notice the cold water currents that move from Antarctica northward along South America's west coast. These cold, deep waters upwell along an equatorial swath around and to the west of the Galapagos Islands. Note the warm, wide currents of the Gulf Stream moving up the United States' east coast, carrying Caribbean warmth toward Newfoundland and across the Atlantic toward Western Europe. Note the warm tongue of water extending from Africa's east coast to well south of the Cape of Good Hope. MODIS was launched in December 1999 aboard NASA's Terra satellite. For more details on this and other MODIS data products, please see NASA Unveils Spectacular Suite of New Global Data Products from MODIS. Image courtesy MODIS Ocean Group, NASA GSFC, and the University of Miami

2002-01-01

343

Biogeochemistry in Sea Ice: CICE model developments  

SciTech Connect

Polar primary production unfolds in a dynamic sea ice environment, and the interactions of sea ice with ocean support and mediate this production. In spring, for example, fresh melt water contributes to the shoaling of the mixed layer enhancing ice edge blooms. In contrast, sea ice formation in the fall reduces light penetration to the upper ocean slowing primary production in marine waters. Polar biogeochemical modeling studies typically consider these types of ice-ocean interactions. However, sea ice itself is a biogeochemically active medium, contributing a significant and, possibly, essential source of primary production to polar regions in early spring and fall. Here we present numerical simulations using the Los Alamos Sea Ice Model (CICE) with prognostic salinity and sea ice biogeochemistry. This study investigates the relationship between sea ice multiphase physics and sea ice productivity. Of particular emphasis are the processes of gravity drainage, melt water flushing, and snow loading. During sea ice formation, desalination by gravity drainage facilitates nutrient exchange between ocean and ice maintaining ice algal blooms in early spring. Melt water flushing releases ice algae and nutrients to underlying waters limiting ice production. Finally, snow loading, particularly in the Southern Ocean, forces sea ice below the ocean surface driving an upward flow of nutrient rich water into the ice to the benefit of interior and freeboard communities. Incorporating ice microphysics in CICE has given us an important tool for assessing the importance of these processes for polar algal production at global scales.

Jeffery, Nicole [Los Alamos National Laboratory; Hunke, Elizabeth [Los Alamos National Laboratory; Elliott, Scott [Los Alamos National Laboratory; Turner, Adrian [Los Alamos National Laboratory

2012-06-18

344

Sea level anomalies exacerbate beach erosion  

NASA Astrophysics Data System (ADS)

Sea level anomalies are intra-seasonal increases in water level forced by meteorological and oceanographic processes unrelated to storms. The effects of sea level anomalies on beach morphology are unknown but important to constrain because these events have been recognized over large stretches of continental margins. Here, we present beach erosion measurements along Onslow Beach, a barrier island on the U.S. East Coast, in response to a year with frequent sea level anomalies and no major storms. The anomalies enabled extensive erosion, which was similar and in most places greater than the erosion that occurred during a year with a hurricane. These results highlight the importance of sea level anomalies in facilitating coastal erosion and advocate for their inclusion in beach-erosion models and management plans. Sea level anomalies amplify the erosive effects of accelerated sea level rise and changes in storminess associated with global climate change.

Theuerkauf, Ethan J.; Rodriguez, Antonio B.; Fegley, Stephen R.; Luettich, Richard A.

2014-07-01

345

Microplastic pollution in deep-sea sediments.  

PubMed

Microplastics are small plastic particles (<1 mm) originating from the degradation of larger plastic debris. These microplastics have been accumulating in the marine environment for decades and have been detected throughout the water column and in sublittoral and beach sediments worldwide. However, up to now, it has never been established whether microplastic presence in sediments is limited to accumulation hot spots such as the continental shelf, or whether they are also present in deep-sea sediments. Here we show, for the first time ever, that microplastics have indeed reached the most remote of marine environments: the deep sea. We found plastic particles sized in the micrometre range in deep-sea sediments collected at four locations representing different deep-sea habitats ranging in depth from 1100 to 5000 m. Our results demonstrate that microplastic pollution has spread throughout the world's seas and oceans, into the remote and largely unknown deep sea. PMID:24035457

Van Cauwenberghe, Lisbeth; Vanreusel, Ann; Mees, Jan; Janssen, Colin R

2013-11-01

346

First biological measurements of deep-sea corals from the Red Sea  

PubMed Central

It is usually assumed that metabolic constraints restrict deep-sea corals to cold-water habitats, with ‘deep-sea’ and ‘cold-water’ corals often used as synonymous. Here we report on the first measurements of biological characters of deep-sea corals from the central Red Sea, where they occur at temperatures exceeding 20°C in highly oligotrophic and oxygen-limited waters. Low respiration rates, low calcification rates, and minimized tissue cover indicate that a reduced metabolism is one of the key adaptations to prevailing environmental conditions. We investigated four sites and encountered six species of which at least two appear to be undescribed. One species is previously reported from the Red Sea but occurs in deep cold waters outside the Red Sea raising interesting questions about presumed environmental constraints for other deep-sea corals. Our findings suggest that the present understanding of deep-sea coral persistence and resilience needs to be revisited. PMID:24091830

Roder, C.; Berumen, M. L.; Bouwmeester, J.; Papathanassiou, E.; Al-Suwailem, A.; Voolstra, C. R.

2013-01-01

347

Historical Antarctic mean sea ice area, sea ice trends, and winds in CMIP5 simulations  

E-print Network

In contrast to Arctic sea ice, average Antarctic sea ice area is not retreating but has slowly increased since satellite measurements began in 1979. While most climate models from the Coupled Model Intercomparison Project ...

Mahlstein, Irina

348

A study of mobile trough genesis over the Yellow Sea - East China Sea region  

E-print Network

The purpose of this study was to understand the mechanisms responsible for the formation of mobile troughs over a prolific source region in the Yellow Sea and East China Sea. Two mobile troughs which intensified significantly after formation were...

Komar, Keith Nickolas

1997-01-01

349

Marine environments in the China Seas and their prediction  

SciTech Connect

The China Seas surround the China continent to its south and east, and connect with the Pacific Ocean. In this paper, marine environmental elements in the China Seas such as marine climate, storm surge, sea wave, sea temperature, sea ice, tsunami and red tide, are analyzed. The predication of marine environments, especially oceanic disasters with good accuracy are also given in this paper.

Bao, C. [National Research Center for Marine Environment Forecasts, Beijing (China)

1993-12-31

350

Recent state of the Aral sea from regular satellite observations  

Microsoft Academic Search

The Aral Sea disaster is one of the most significant examples of ecological catastrophe caused by mismanagement of water resources. Aral sea level dropped on 22 meters for the last 35 years. The sea separated in to two independent parts , the Large Sea(Southern) and the Small Sea (Northern), loosing more than 90% of its original water masses. After the

S. Stanichny; A. Davidov; S. Djenidi; U. Horstmann; R. Stanichnaya; D. Soloviev

2004-01-01

351

Flood Vulnerability and Flood Protection North and Baltic Seas  

E-print Network

G G G G Flood Vulnerability and Flood Protection North and Baltic Seas Meteorological Forcings NorthSea/BalticSeaMeteorologicalForcingsforDCSM28April2009 1 #12;G G G G Overview GLAMEPS Harmonie G G G G NorthSea/BalticSeaMeteorologicalForcingsforDCSM28April2009 2 #12;G G G G DCSM and Hirlam History

Vries, Hans de

352

The role of sea ice dynamics in global climate change  

NASA Technical Reports Server (NTRS)

The topics covered include the following: general characteristics of sea ice drift; sea ice rheology; ice thickness distribution; sea ice thermodynamic models; equilibrium thermodynamic models; effect of internal brine pockets and snow cover; model simulations of Arctic Sea ice; and sensitivity of sea ice models to climate change.

Hibler, William D., III

1992-01-01

353

Ecological Role of Sea Lions as Predators, Competitors, and Prey  

E-print Network

Ecological Role of Sea Lions as Predators, Competitors, and Prey · Sea Lion Species · California Sea Lions (not listed) - increasing · Steller Sea Lions eDPS (threatened) ­ increasing (delisting review under way, June 2010) · Steller Sea Lions wDPS (endangered) - decreasing · Predators ­ varied diet

354

Anchovy fisheries in the Adriatic Sea  

Microsoft Academic Search

SUMMARY: Anchovy (Engraulis encrasicolus, L.) is one the most important commercial species of the Adriatic Sea. With a surface area of 138,000 km2, about one twentieth of the Mediterranean Sea, the Adriatic Sea produced about 13,000 tonnes of anchovy in 1991, equal to 19% of the Mediterranean anchovy catches. The value of Adriatic anchovy catches has been estimated at about

NANDO CINGOLANI; GIANFRANCO GIANNETTI; ENRICO ARNERI

355

Sea Surface Salinity : Research Challenges and Opportunities  

NASA Technical Reports Server (NTRS)

Sea surface salinity (SSS) can be important in regulating sea surface temperature (SST). Two technological breakthrough satellite SSS missions, Aquarius and Soil Moisture and Ocean Salinity (SMOS), are currently producing high-quality SSS data. This paper provides an overview of the importance of SSS for weather and climate applications and describes the Aquarius and SMOS missions. The newness of adequately sampled SSS data prompted a first-time at-sea field campaign devoted to improved understanding of SSS variations.

Halpern, David; Lagerloef, Gary; Font, Jordi

2012-01-01

356

Journey to the Deep Sea Vents  

NSDL National Science Digital Library

This six-day unit provides an in-depth look at the dynamic forces at work on the sea floor. Throughout the unit, students collect their findings in a portfolio. The comprehensive curriculum materials include teacher tools such as individually downloadable readings and detailed daily breakdowns of tasks, a hands-on experiment, three activities about how scientists find deep sea vents and two activities about the thriving ecosystems found in deep sea vents.

357

Caribbean Conservation Corporation/ Sea Turtle Survival League  

NSDL National Science Digital Library

Contains sources of information on sea turtles, tropical birds, and other species in the Caribbean basin and the Costa Rica rainforests. Site includes information on satellite telemetry, satellite-tracked sea turtles data and maps, and sea turtle legislation. Directions, data, and other materials available allow you to create your own maps. Free printable publications available. Also information on grants, workshops, donations, and volunteer opportunities.

358

The International Arctic Seas Assessment Project  

SciTech Connect

The International Arctic Seas Assessment Project (IASAP) was initiated in 1993 to address widespread concern over the possible health and environmental impacts associated with the radioactive waste dumped into the shallow waters of the Arctic Seas. This article discusses the project with these general topics: A brief history of dumping activities; the international control system; perspectives on arctic Seas dumping; the IASAP aims and implementation; the IASAP work plan and progress. 2 figs.

Linsley, G.S.; Sjoeblom, K.L.

1994-07-01

359

Hubbs-Sea World Research Institute  

NSDL National Science Digital Library

Describes the Research Institute's use of science in developing solutions for conservation challenges facing marine ecosystems and species. Overviews of research projects in ecology, physiology, bioacoustics and aquaculture. Species studied include: marine mammals, sea turtles, whale shark, white sea bass and others. Explains how satellite tracking technology is used to study survival needs of endangered species (leatherback sea turtle, Hawaiian monk seal). Outlines educational objectives and contributions, news and events. Appropriate for grades 8 and up.

360

Steriod dynamics in immature sea turtles  

E-print Network

numbers of adult and im- mature individuals in a given sea turtle population. In some animals, evidence indicates that early experi- ences greatly influence the physiology and the behavior of the adult. Such influences may exist for sea turtles...: Biology STEROID DYNAMICS IN IMMATURE SEA TURTLES A Thesis by YUKI ANN MORRIS Approved as to styie and content by: David W. Owens (Chairman of Committee) Heimut W. Sauer (Head of Department) Robert C. Bur hardt (Member) Max S. Amoss (Member...

Morris, Yuki A

1982-01-01

361

Lena River Delta and East Siberian Sea  

NASA Technical Reports Server (NTRS)

The winter sea ice in the east Siberian Sea is looking a bit like a cracked windshield in these true-color Moderate Resolution Imaging Spectroradiometer (MODIS) images from June 16 and 23, 2002. North of the thawing tundra, the sea ice takes on its cracked, bright blue appearance as it thins, which allows the reflection of the water to show through. Numerous still-frozen lakes dot the tundra. Credit: Jacques Descloitres, MODIS Land Rapid Response Team, NASA/GSFC

2002-01-01

362

Arctic sea ice as a granular plastic  

Microsoft Academic Search

An important consideration in understanding sea ice mechanics is the integration of observed sea ice behavior on a floe neighborhood scale (1-10 km) into ice dynamics on a regional scale O(50km). We investigate sea ice kinematics from October 1993 through April 1994 using relative motions from 13 drifting buoys with Global Positioning System navigation in a 20-km array centered on

James E. Overland; S. Lyn McNutt; Sigrid Salo; Joanne Groves; Shusun Li

1998-01-01

363

South China Sea WWW Virtual Library  

NSDL National Science Digital Library

The South China Sea WWW Virtual Library is a new subsection of the Asian Studies WWW Virtual Library edited by David Rosenberg, professor of political science at Middlebury College (Vermont). This site will serve as a centralized resource for students, researchers, and policymakers interested in South China Sea regional development, environment, and security issues. The South China Sea WWW VL links to online publications, databases, maps, images, related institutions, and a print bibliography.

Rosenburg, David

364

Climate Change and Sea Level Rise  

NSDL National Science Digital Library

This module looks at how increasing temperatures due to climate change have affected sea level rise and what effects scientist expect in the future, given rising greenhouse gas emissions. The various mechanisms of sea level rise are discussed, as well as the tools and research used to study this topic. The module also discusses how countries and communities are preparing for future increases in sea levels.

COMET

2012-08-14

365

Correlating the shallow and the deep 3D-structure of the Barents Sea/ Kara Sea  

NASA Astrophysics Data System (ADS)

The Barents Sea and Kara Sea continental shelf region is located in the northern European Arctic. The crustal configuration of the Barents Sea/Kara Sea region exhibits a complex architecture of the sedimentary cover which implies the influence of diverse causative geological processes. The narrow and deep basins of the southwestern Barents Sea characterise rift basins which have been filled with thick sediments predominantly Mesozoic in age. In contrast, the eastern Barents Sea and the southern Kara Sea are marked by a wide and deep basin architecture which indicates basin formation mechanisms apart from rifting. There, the sedimentary succession yields Paleozoic and Mesozoic sediments. Cenozoic deposits are restricted to the southwesternmost parts of the Barents Sea and the oceanic domain. The lack of sediments on the shelf is attributed to strong Pleistocene uplift, subsequent erosion and recurring ice sheet coverage of the Barents Sea/Kara Sea region. The modelled area covers about 5 million km² with a maximum longitudinal and latitudinal extent of 2180 and 2400 km, respectively, and comprises regions beyond the Barents Sea and Kara Sea such as parts of Greenland, Fennoscandia and western Siberia. This study presents the lithospheric density configuration below the greater Barents Sea/ Kara Sea region. Thereby, five sedimentary megasequences are differentiated across the entire study area. Each unit is modelled with matrix densities and depth dependent porosities to calculate the bulk densities. The respective compaction curves reflect that strong late Cenozoic erosion and ice sheet coverage removed particularly less dense sediments on Svalbard and Novaya Zemlya, while in the eastern Barents Sea and the southern Kara Sea erosion was less effective. Thus, the obtained sedimentary bulk densities vary laterally distinctively. The density setup of the subsedimentary lithosphere beneath the Barents shelf is defined by a high-resolution, velocity-converted density grid. This dataset is tested the first time against gravity to further constrain the 3D density model. Interestingly, region that experienced weaker Cenozoic erosion are underlain by a heavier mantle density composition.

Klitzke, Peter; Faleide, Jan Inge; Sippel, Judith; Scheck-Wenderoth, Magdalena

2013-04-01

366

Changes in Extremes of Relative Sea-level: the Baltic Sea case study  

NASA Astrophysics Data System (ADS)

Long records of relative sea-level heights from coastal tide gauge stations provide valuable information on regional variability. The analysis of such records is usually focused on the estimation of linear slopes by ordinary least squares regression. However, sea-level variability can include not only changes in the mean but also changes in the shape and spread of the sea-level values distribution over time. These variations can be more important than changes in mean sea-level - in particular, changes in extreme high waters can impact considerably coastal locations and populations. In this study, this issue is addressed by analyzing the variability of extreme sea-levels in the Baltic Sea through quantile regression. This method allows to derive slopes, along with corresponding uncertainties, for different quantiles of the sea-level distribution. A total of 70 tide gauges along the Baltic sea coastlines are considered. The results show that in the eastern part of the Baltic Sea, including the Gulf of Bothnia and the Gulf of Finland, the rate of change of relative sea-level is significantly higher at the 0.9 quantile (corresponding to the largest 10% of sorted sea-level values) than at the mean. The Baltic Sea is a shallow, semi-enclosed sea. Relative sea-level heights are directly influenced by land uplift, which varies considerably along the Baltic Sea coastlines and by the exchange of water through the Danish Straits, mainly determined by meteorological conditions (particularly winds and atmospheric pressure). The distinct rate of change of high-waters in the upper Baltic Sea seems to be associated with corresponding changes in atmospheric conditions, particularly westerly winds.

Silva, M.; Barbosa, S. M.

2007-12-01

367

Predicting the Impact of Sea-Level Rise on Caribbean Sea Turtle Nesting Habitat  

Microsoft Academic Search

Abstract: Th ep rojected rise in sea level is likely to increase the vulnerability of coastal zones in the Caribbean, which,are already under,pressure from,a combination,of anthropogenic,activities and,natural processes. One of the major effects will be a loss of beach habitat, which provides nesting sites for endangered sea turtles. To assess the potential impacts of sea-level rise on sea turtle nesting

MARIANNE R. FISH; ISABELLE M. COTE; JENNIFER A. GILL; ANDREW P. JONES; SASKIA RENSHOFF; ANDREW R. WATKINSON

2005-01-01

368

Population status of California sea otters  

SciTech Connect

The main objective of the study was to develop a simulation model to facilitate analysis of the risk of oil spills to the threatened California sea otter population. Existing data on the dynamics and demography of the population were synthesized. The additional data needed for model development were collected through radiotelemetry studies of sea otters in Alaska and California. The simulation model contains four interrelated stochastic submodels: a short-term population model, a long-term population model, a sea otter distribution model, and a sea otter movement model. The report includes a detailed description of the model, the data on which it is based, and an operating manual.

Not Available

1988-11-30

369

Sea level rise and its coastal impacts  

NASA Astrophysics Data System (ADS)

Global warming in response to accumulation of human-induced greenhouse gases inside the atmosphere has already caused several visible consequences, among them increase of the Earth's mean temperature and ocean heat content, melting of glaciers, and loss of ice from the Greenland and Antarctica ice sheets. Ocean warming and land ice melt in turn are causing sea level to rise. Sea level rise and its impacts on coastal zones have become a question of growing interest in the scientific community, as well as in the media and public. In this review paper, we summarize the most up-to-date knowledge about sea level rise and its causes, highlighting the regional variability that superimposes the global mean rise. We also present sea level projections for the 21st century under different warming scenarios. We next address the issue of the sea level rise impacts. We question whether there is already observational evidence of coastal impacts of sea level rise and highlight the fact that results differ from one location to another. This suggests that the response of coastal systems to sea level rise is highly dependent on local natural and human settings. We finally show that in spite of remaining uncertainties about future sea levels and related impacts, it becomes possible to provide preliminary assessment of regional impacts of sea level rise.

Cazenave, Anny; Cozannet, Gonéri Le

2014-02-01

370

Biogeochemistry of the Salton Sea, California  

NASA Astrophysics Data System (ADS)

The Salton Sea is a saline, closed basin lake 70 meters below MSL in the southern desert of California. It is the largest lake in California with a surface area of 945 km2 and an annual inflow of 1,600 million m3. The Sea is hypereutrophic due to nutrient inputs from farm runoff, and anaerobic conditions in the bottom water result in summer and fall releases of hydrogen sulfide and fish kills. The salinity of the Sea is 47 g/L and rising, with an annual salt load of 4 million metric tons. Plans are being developed for construction of a salt repository to control salinization, improve water quality, and maintain the Sea as a refuge for migratory waterfowl. We estimate 700,000 metric tons of calcite are precipitating in the Sea each year, along with 7,000 tons of iron sulfide minerals. Potentially, 70,000 metric tons of hydrogen sulfide are produced in the Sea each year. Measurements of hydrogen sulfide production, reoxidation in the water column, and atmospheric releases will be reported. Hydrodynamic modeling of the current Sea, and the proposed smaller Sea, indicate that partitioning the Sea could lead to persistent stratification and episodic releases of hydrogen sulfide during fall mixing.

Amrhein, C.; Reese, B. K.; Anderson, M. A.

2006-12-01

371

Parasites in the Wadden Sea food web  

NASA Astrophysics Data System (ADS)

While the free-living fauna of the Wadden Sea has received much interest, little is known on the distribution and effects of parasites in the Wadden Sea food web. However, recent studies on this special type of trophic interaction indicate a high diversity of parasites in the Wadden Sea and suggest a multitude of effects on the hosts. This also includes effects on specific predator-prey relationships and the general structure of the food web. Focussing on molluscs, a major group in the Wadden Sea in terms of biomass and abundance and an important link between primary producers and predators, we review existing studies and exemplify the ecological role of parasites in the Wadden Sea food web. First, we give a brief inventory of parasites occurring in the Wadden Sea, ranging from microparasites (e.g. protozoa, bacteria) to macroparasites (e.g. helminths, parasitic copepods) and discuss the effects of spatial scale on heterogeneities in infection levels. We then demonstrate how parasites can affect host population dynamics by acting as a strong mortality factor, causing mollusc mass mortalities. In addition, we will exemplify how parasites can mediate the interaction strength of predator-prey relationships and affect the topological structure of the Wadden Sea food web as a whole. Finally, we highlight some ongoing changes regarding parasitism in the Wadden Sea in the course of global change (e.g. species introduction, climate change) and identify important future research questions to entangle the role of parasites in the Wadden Sea food web.

Thieltges, David W.; Engelsma, Marc Y.; Wendling, Carolin C.; Wegner, K. Mathias

2013-09-01

372

Permanent Service for Mean Sea Level  

NSDL National Science Digital Library

The Permanent Service for Mean Sea Level (PSMSL), hosted by the Proudman Oceanographic Laboratory (POL), is the global data bank for long term sea level change information from tide gauges. The PSMSL data set is the main source of information on long term changes in global sea level during the last two centuries. This site contains data sets, and information on other services such as vertical land movements and air pressure. There are answers to frequently asked questions about sea level changes, packets on data use available, annual reports, and other contacts for more information.

373

Extreme 2008: A Deep Sea Adventure  

NSDL National Science Digital Library

This website, designed for K-12 teachers and students, offers materials and activities based on the "Extreme 2008: A Deep Sea Adventure" mission to explore deep-sea hydrothermal vents. Students can step into the shoes of deep-sea scientists as they follow the expedition and listen to recordings of student communications with the researchers via e-mail and telephone calls placed directly to Alvin, a research submersible, as it made its way deep into the Pacific. Topics include sea creatures, geology, plate tectonics, and chemistry of the deep ocean. Video clips are also provided to help students visualize the underwater experience.

2004-08-08

374

Coastal Consequences of Sea Level Rise  

NSDL National Science Digital Library

This self-paced tutorial explores the evidence for sea level rise related to global climate change and the consequences for humanity, especially for coastal-dwelling populations. Learners explore how a warming climate contributes to sea level rise, examine how satellites collect sea level data, and analyze interactive data to understand the potential consequences of climate change on sea level in different parts of the world. Multimedia educational resources including video clips and glossary links to vocabulary are included. This is the seventh of ten self-paced professional development modules providing opportunities for teachers to learn about climate change through first-hand data exploration.

2012-10-18

375

Coastal eolian landforms and sea level fluctuations  

NASA Astrophysics Data System (ADS)

This paper is dedicated to correlation of the formation of coastal marine landforms with sea level fluctuations and climate changes in the last millennium using the southeastern Baltic region as an example. The morphological analysis of spits and historical evidence reveal three sea level oscillations in its evolution. It is shown that the sea level rise against the background of the sandy material excess in the coastal zone and optimum angle of the prevailing land-directed wind are the main factors responsible for accumulation of the thickest sandy formations. The recent climate warming and related sea level rise provoke global destabilization of coastal dune massifs.

Badyukova, E. N.; Solovieva, G. D.

2015-02-01

376

Interannual Extremes in New Zealand Precipitation Linked to Modes of Southern Hemisphere Climate Variability  

Microsoft Academic Search

Interannual extremes in New Zealand rainfall and their modulation by modes of Southern Hemisphere climate variability are examined in observations and a coupled climate model. North Island extreme dry (wet) years are characterized by locally increased (reduced) sea level pressure (SLP), cold (warm) sea surface temperature (SST) anomalies in the southern Tasman Sea and to the north of the island,

Caroline C. Ummenhofer; Matthew H. England

2007-01-01

377

Bayesian Hierarchical Air-Sea Interaction Modeling: Application to the Labrador Sea  

NASA Technical Reports Server (NTRS)

The objectives are to: 1) Organize data from 26 MINIMET drifters in the Labrador Sea, including sensor calibration and error checking of ARGOS transmissions. 2) Produce wind direction, barometer, and sea surface temperature time series. In addition, provide data from historical file of 150 SHARP drifters in the Labrador Sea. 3) Work with data interpretation and data-modeling assimilation issues.

Niiler, Pearn P.

2002-01-01

378

Temporal and spatial variations of sea surface temperature in the East China Sea  

Microsoft Academic Search

Sea surface temperature of the East China Sea (ECS) were analyzed using the NOAA\\/AVHRR SST images. These satellite images reveal surface features of ECS including mainly the Kuroshio Current, Kuroshio Branch Current, Taiwan Warm Current, China coastal water, Changjiang diluted water and Yellow Sea mixed cold water. The SST of ECS ranges from 27 to 29°C in summer; some cold

Chente Tseng; Chiyuan Lin; Shihchin Chen; Chungzen Shyu

2000-01-01

379

A numerical experiment on the sedimentation processes in the Yellow Sea and the East China Sea  

Microsoft Academic Search

Sedimentation processes of suspended matter supplied from the Huanghe (Yellow River) and the Changjiang are investigated with the use of a three-dimensional numerical model of the Yellow Sea and the East China Sea which includes the tidal current, residual flow and wind waves. Suspended matter supplied from the Huanghe mainly deposits in the Bohai Sea and that from the old

Tetsuo Yanagi; Koh-ichi Inoue

1995-01-01

380

NOAA's Deep Sea Coral Research and Technology Program Deep-Sea Coral Ecosystems  

E-print Network

and Technology Program is to provide sound scientific information needed to conserve and manage deep-sea coralNOAA's Deep Sea Coral Research and Technology Program Deep-Sea Coral Ecosystems Research over activities that disturb the seafloor. Recovery from damage may take decades, or even centuries, as most deep

381

NOAA's Deep Sea Coral Research and Technology Program Deep-Sea Coral Ecosystems  

E-print Network

NOAA's Deep Sea Coral Research and Technology Program Deep-Sea Coral Ecosystems Deep-sea corals can and pipelines, and other human activities that disturb the seafloor. Recovery from damage may take decades Act. · Produces sound science to support NOAA's role in the management of fishing impacts

382

Tides in the Weddell Sea Robertson et al., 1998 TIDES IN THE WEDDELL SEA  

E-print Network

Tides in the Weddell Sea Robertson et al., 1998 TIDES IN THE WEDDELL SEA Robin Robertson, Laurie of baroclinic tides. Model results indicate that tides play a significant role in the circulation and heat flux in the Weddell Sea. We discuss the influence of tides on mean flow through the modified effective bot- tom drag

Robertson, Robin

383

Territorial behavior in juvenile red sea bream Pagrus major and crimson sea bream Evynnis japonica  

Microsoft Academic Search

The territorial behavior of juvenile red sea bream Pagrus major and crimson sea bream Evynnis japonica was examined at Morode Cove, Ehime Prefecture. Four exclusive types of behavior (attack, mutual attack, head down threat and mutual display) and one escaping behavior (fleeing) were observed in both species. Juvenile of the two sea bream could discriminate between each other and change

Takaya KUDOH; Kosaku YAMAOKA

2004-01-01

384

SEA TURTLE RESEARCH INTERNSHIPS Karen Beasley Sea Turtle Rescue and Rehabilitation Center  

E-print Network

SEA TURTLE RESEARCH INTERNSHIPS Karen Beasley Sea Turtle Rescue and Rehabilitation Center Sponsors of North Carolina Wilmington North Carolina Museum of Natural Sciences KAREN BEASLEY SEA TURTLE RESCUE AND REHABILITATION CENTER MISSION STATEMENT · The conservation and protection of all species of marine turtles, both

Southwood Williard, Amanda

385

Sea Turtles: Navigating with Young sea turtles use the Earth's magnetic field as a source of  

E-print Network

Sea Turtles: Navigating with Magnetism Young sea turtles use the Earth's magnetic field as a source satellite telemetry has now demonstrated for the first time that adult turtles also navigate using the Earth's magnetic field. Kenneth J. Lohmann The ability of sea turtles to navigate across vast expanses of seemingly

Lohmann, Kenneth J.

386

SEAS Lab Safety Officer Orientation Welcome to the SEAS Safety Committee.  

E-print Network

_streeto@harvard.edu Sid Paula, Biosafety Manager, spaula@mcb.harvard.edu Xiaowei Yan, Manager of Laser Safety, xiaoweiSEAS Lab Safety Officer Orientation Welcome to the SEAS Safety Committee. We appreciate your Officer list · SEAS/EHS Safety Tools ­ How often do I update ... ? · Lab Inspection Schedule, and Peer

387

POSSIBLE LUNAR TIDE EFFECTS ON CLIMATE AND ECOSYSTEM VARIABILITY IN THE NORDIC SEAS AND THE BARENTS SEA  

Microsoft Academic Search

The inflow of North Atlantic Water to the Norwegian Sea and the Barents Sea has a major influence on northern Europe climate and ecosystem dynamics in the Nordic Seas and the Barents Sea. In the period from 1900 to 2005, the temperature variability of North Atlantic Water and the Barents Sea temperature was correlated with the 18.6 year amplitude tide

Harald Yndestad

388

ADVANCES IN ATMOSPHERIC SCIENCES, VOL. 22, NO. 1, 2005, 120 Seasonal Variability of the Yellow Sea/East China Sea  

E-print Network

ADVANCES IN ATMOSPHERIC SCIENCES, VOL. 22, NO. 1, 2005, 1­20 Seasonal Variability of the Yellow Sea Oceanographic Observation Data Set (MOODS) for the Yellow Sea/East China Sea (YES) to investigate and water mass properties, we divide YES into five regions: East China Sea (ECS) shelf, Yellow Sea (YS

Chu, Peter C.

389

An evaluation of MODIS and SeaWiFS bio-optical algorithms in the Baltic Sea  

E-print Network

An evaluation of MODIS and SeaWiFS bio-optical algorithms in the Baltic Sea Miroslaw Dareckia) and Sea-viewing Wide Field-of-view Sensor (SeaWiFS) ocean color (in-water) algorithms in the Baltic Sea these standard algorithms inadequate for pigment determinations in the Baltic. Although new parameterization

Stramski, Dariusz

390

Unlocking a Sea Ice Secret  

SciTech Connect

Dr. Rachel Obbard and her research group from Dartmouth College traveled to the Antarctic to collect samples of sea ice. Next stop: the GeoSoilEnviroCARS x-ray beamline at the Advanced Photon Source at Argonne National Laboratory in Illinois. This U.S. Department of Energy Office of Science synchrotron x-ray research facility gave the Obbard team the frontier scientific tools they needed to study the path bromide takes as it travels from the ocean to the atmosphere.

Dr. Rachel Obbard

2013-04-22

391

Solar distillation of sea water  

SciTech Connect

Indian coastal and fishing villages suffer from scarcity of potable water. Solar distillation could provide a solution to this problem by adopting the following criteria: (1) Integration of distillation and storage systems with the house design. (2) Public supply of sea water and a public drain pipe system to periodically drain away the concentrated brine. (3) Harvest and store rain water to tide over cloudy rainy periods. In India there has been a thrust towards centralized non-conventional energy systems. Decentralized non-conventional energy devices and centralized service support units may offer a better solution. 1 fig.

Subramanyam, S. (Kakatiya Institute of Technology and Science, Warangal (India))

1989-01-01

392

UN adopts Law of Sea  

NASA Astrophysics Data System (ADS)

After more than 8 years of diplomatic wrangling, the United Nations Convention on the Law of the Sea was adopted on April 30 by a vote of 130 to 4. The United States, Israel, Turkey, and Venezuela voted against the treaty; 17 nations—including the Soviet Union, West Germany, and Britain—abstained.The treaty, which would give nations the exclusive rights to natural resources in the continental shelf up to approximately 650 km offshore, will be signed in December. The treaty becomes effective 1 year after at least 60 nations ratify it.

Richman, Barbara T.

393

Aral Sea, Kazakhstan,CIS  

NASA Technical Reports Server (NTRS)

Situated in the middle of an immense desert, much like the Great Salt Lake of Utah, the Aral Sea (45.0N, 59.0E) is landlocked in the center of a broad basin. Rivers flow in but not out; water escapes only by evaporation. In recent years, river water has been diverted for agricultural irrigation and the lake level has fallen 40 to 50 ft., its surface has shrunk by almost 40 % and the salinity has almost tripled. Twenty species of fish are now extinct.

1992-01-01

394

The electrolysis of sea water  

E-print Network

). t ~ Is & ~ ( I ~ d ~ loxl '-. sl y )V' 1. 1 ':. 5 d ~ & I ~ I & o ~ 1 ~ 1', 7 ~ (& &C ~ 167, 1. . lxlo 'xl . . . xls- ~3 ~ 3 0 ~ 6P IG ~ . ~ 7 ~o:I. -;. ' . -e water of no~el corn. o ition t-. maxitue value 2' or the recovery..., s of but a few people. In abstract form there are reported the following having to do with the electroly- sis of sea watero 2" 8 SOLUTION A ? CELLULOSE ACETATE TUBE B ? LUCITE DISKS C ? GLASS TUBING D ? GRAPHITE ANODE E ? RUBBER STOPPER F ? STEEL...

Stoddard, William Bull

1952-01-01

395

Processes driving sea ice variability in the Bering Sea in an eddying ocean/sea ice model: Mean seasonal cycle  

NASA Astrophysics Data System (ADS)

The seasonal cycle of sea ice variability in the Bering Sea, together with the thermodynamic and dynamic processes that control it, are examined in a fine resolution (1/10°) global coupled ocean/sea-ice model configured in the Community Earth System Model (CESM) framework. The ocean/sea-ice model consists of the Los Alamos National Laboratory Parallel Ocean Program (POP) and the Los Alamos Sea Ice Model (CICE). The model was forced with time-varying reanalysis atmospheric forcing for the time period 1970-1989. This study focuses on the time period 1980-1989. The simulated seasonal-mean fields of sea ice concentration strongly resemble satellite-derived observations, as quantified by root-mean-square errors and pattern correlation coefficients. The sea ice energy budget reveals that the seasonal thermodynamic ice volume changes are dominated by the surface energy flux between the atmosphere and the ice in the northern region and by heat flux from the ocean to the ice along the southern ice edge, especially on the western side. The sea ice force balance analysis shows that sea ice motion is largely associated with wind stress. The force due to divergence of the internal ice stress tensor is large near the land boundaries in the north, and it is small in the central and southern ice-covered region. During winter, which dominates the annual mean, it is found that the simulated sea ice was mainly formed in the northern Bering Sea, with the maximum ice growth rate occurring along the coast due to cold air from northerly winds and ice motion away from the coast. South of St Lawrence Island, winds drive the model sea ice southwestward from the north to the southwestern part of the ice-covered region. Along the ice edge in the western Bering Sea, model sea ice is melted by warm ocean water, which is carried by the simulated Bering Slope Current flowing to the northwest, resulting in the S-shaped asymmetric ice edge. In spring and fall, similar thermodynamic and dynamic patterns occur in the model, but with typically smaller magnitudes and with season-specific geographical and directional differences.

Li, Linghan; McClean, Julie L.; Miller, Arthur J.; Eisenman, Ian; Hendershott, Myrl C.; Papadopoulos, Caroline A.

2014-12-01

396

Climate and sea ice variability in the SW Labrador Sea during the late Holocene  

NASA Astrophysics Data System (ADS)

The recent rapid decline in Arctic sea ice cover has increased the need to improve the accuracy of the sea ice components in climate models and to provide detailed long-term sea ice records based on proxy data. Recently, the highly branched isoprenoid IP25 has emerged as a potential sea ice specific proxy for past sea ice cover, found in marine sediments underlying seasonal sea ice. We tested the reliability of this biomarker against observational sea ice data off Newfoundland (SW Labrador Sea), where box cores covering the last ca. 100-150 years were collected. Based on the results, IP25 proved to be a robust and reliable proxy for reconstructing variability in past sea ice concentrations in the area. After having successfully validated the proxy in the SW Labrador Sea, we further analysed IP25 from a sediment core NE of Newfoundland covering the last ca. 5000 years, providing the southernmost multi-millennial record of this proxy to date. Based on this record and on diatom and dinoflagellate cyst data and alkenone-based sea surface temperatures (SSTs) from the same core, we reconstructed climatic conditions in and Arctic sea ice export to the SW Labrador Sea area: Alkenone-based SSTs show a clear albeit variable decline after the Holocene Climate Optimum, while at the same time diatom and dinoflagellate cyst data suggest decreased melt water export from the Arctic. The IP25 record reveals increased sea ice export from the Baffin and Hudson Bays starting ca 1500 yr cal. BP, accelerating ca. 800 yr cal. BP and culminating at the height of the Little Ice Age. Sea ice export during the last century is comparable to the export during the Medieval Climate Anomaly.

Weckström, Kaarina; Massé, Guillaume; Collins, Lewis; Sicre, Marie-Alexandrine; Bouloubassi, Ioanna; Seidenkrantz, Marit-Solveig; Olsen, Jesper; Kuijpers, Antoon

2014-05-01

397

SciFeatureSciFeature SEA-MONKEYS AND ALIENS?  

E-print Network

SciFeatureSciFeature MSU SEA-MONKEYS® AND ALIENS? What is the connection between Sea-Monkeys® and aliens? Believe it or not NASA scientists think it is possible that some alien life might resemble Sea

398

46 CFR 42.30-30 - Enclosed seas.  

Code of Federal Regulations, 2014 CFR

... Summer: April 1 to October 31. (b) Black Sea. This sea is included in the Summer Zones. (1) However...29. Summer: March 1 to November 30. (c) Mediterranean. This sea is included in the Summer Zones....

2014-10-01

399

Melting Ice, Rising Seas - Duration: 4:32.  

NASA Video Gallery

Sea level rise is an indicator that our planet is warming. Much of the world's population lives on or near the coast, and rising seas are something worth watching. Sea level can rise for two reason...

400

50 CFR 648.109 - Sea turtle conservation.  

Code of Federal Regulations, 2013 CFR

... 2013-10-01 2013-10-01 false Sea turtle conservation. 648.109 Section 648.109...the Summer Flounder Fisheries § 648.109 Sea turtle conservation. Sea turtle regulations are found at 50 CFR parts 222 and...

2013-10-01

401

50 CFR 648.109 - Sea turtle conservation.  

Code of Federal Regulations, 2011 CFR

... 2011-10-01 2011-10-01 false Sea turtle conservation. 648.109 Section 648.109...the Summer Flounder Fisheries § 648.109 Sea turtle conservation. Sea turtle regulations are found at 50 CFR parts 222 and...

2011-10-01

402

50 CFR 648.109 - Sea turtle conservation.  

Code of Federal Regulations, 2012 CFR

... 2012-10-01 2012-10-01 false Sea turtle conservation. 648.109 Section 648.109...the Summer Flounder Fisheries § 648.109 Sea turtle conservation. Sea turtle regulations are found at 50 CFR parts 222 and...

2012-10-01

403

50 CFR 648.109 - Sea turtle conservation.  

Code of Federal Regulations, 2014 CFR

... 2014-10-01 2014-10-01 false Sea turtle conservation. 648.109 Section 648.109...the Summer Flounder Fisheries § 648.109 Sea turtle conservation. Sea turtle regulations are found at 50 CFR parts 222 and...

2014-10-01

404

50 CFR 648.106 - Sea Turtle conservation.  

Code of Federal Regulations, 2010 CFR

... 2010-10-01 2010-10-01 false Sea Turtle conservation. 648.106 Section 648.106...the Summer Flounder Fisheries § 648.106 Sea Turtle conservation. Sea turtle regulations are found at 50 CFR parts 222 and...

2010-10-01

405

50 CFR 223.202 - Steller sea lion.  

Code of Federal Regulations, 2013 CFR

... 2013-10-01 false Steller sea lion. 223.202 Section 223.202 Wildlife...Anadromous Species § 223.202 Steller sea lion. (a) General prohibitions. ...to the eastern population of Steller sea lions: (1) No discharge of...

2013-10-01

406

50 CFR 223.202 - Steller sea lion.  

Code of Federal Regulations, 2010 CFR

... 2010-10-01 false Steller sea lion. 223.202 Section 223.202 Wildlife...Anadromous Species § 223.202 Steller sea lion. (a) General prohibitions. ...to the eastern population of Steller sea lions: (1) No discharge of...

2010-10-01

407

50 CFR 223.202 - Steller sea lion.  

Code of Federal Regulations, 2012 CFR

... 2012-10-01 false Steller sea lion. 223.202 Section 223.202 Wildlife...Anadromous Species § 223.202 Steller sea lion. (a) General prohibitions. ...to the eastern population of Steller sea lions: (1) No discharge of...

2012-10-01

408

50 CFR 223.202 - Steller sea lion.  

Code of Federal Regulations, 2011 CFR

... 2011-10-01 false Steller sea lion. 223.202 Section 223.202 Wildlife...Anadromous Species § 223.202 Steller sea lion. (a) General prohibitions. ...to the eastern population of Steller sea lions: (1) No discharge of...

2011-10-01

409

Remote Sensing of Sea Ice in the Northern Sea Route: Studies and Applications  

NASA Astrophysics Data System (ADS)

Given the rapid changes that are under way in Arctic sea ice extent, Remote Sensing of Sea Ice in the Northern Sea Route is a timely work. The Northern Sea Route (NSR), along the Arctic coast of Russia, has a long history, dating back to 1932, when the Soviet Union established the NSR administration to develop hydrometeorological services. Shipping along the sea route peaked in the 1980s, but there is renewed interest associated with a lengthening ice-free season and mineral exploitation. Since July 1991, the NSR has been open to all merchant vessels.

Barry, Roger G.

2008-07-01

410

Mapping of sea bottom topography  

NASA Technical Reports Server (NTRS)

Under suitable conditions the bottom topography of shallow seas is visible in remote sensing radar imagery. Two experiments were performed to establish which remote sensing technique or combination yields optimal imaging of bottom topography and which hydro-meteorological conditions are favorable. A further goal is to gain experience with these techniques. Two experiments were performed over an area in the North Sea near the measuring platform Meetpost Noordwijk (MPN). The bottom topography in the test area is dominated by sand waves. The crests of the sand waves are perpendicular to the coast line and the dominating (tidal-)current direction. A 4x4 sq km wide section of the test area was studied in more detail. The first experiment was undertaken on 16 Aug. 1989. During the experiment the following remote sensing instruments were used: Landsat-Thematic Mapper, and NASA/JPL Airborne Imaging Radar (AIR). The hydro-meteorological conditions; current, wind, wave, and air and water temperature were monitored by MPN, a ship of Rijkswaterstaat (the OCTANS), and a pitch-and-roll WAVEC-buoy. The second experiment took place on 12 July 1992. During this experiment data were collected with the NASA/JPL polarimetric synthetic aperture radar (SAR), and a five-band helicopter-borne scatterometer. Again the hydro-meteorological conditions were monitored at MPN and the OCTANS. Furthermore, interferometric radar data were collected.

Calkoen, C. J.; Wensink, G. J.; Hesselmans, G. H. F. M.

1992-01-01

411

North Sea development activity surges  

SciTech Connect

This paper reports that operators in the North Sea have reported a burst of upstream activity. Off the U.K.: Amoco (U.K.) Exploration Co. installed three jackets in its North Everest and Lomond fields. It also completed laying the Central Area Transmission System (CATS) pipeline, which will carry the fields' gas to shore. BP Exploration Operating Co. Ltd. installed the jacket for it Unity riser platform 5 {1/2} km from its Forties Charlie platform. Conoco (U.K.) Ltd. tested a successful appraisal well in Britannia field in Block 15/30, about 130 miles northeast of Aberdeen. In the Norwegian North Sea, Saga Petroleum AS placed Snorre oil and gas field on production 6 weeks ahead of schedule and 1.5 billion kroner under budget at a cost of 16.6 billion kroner; and downstream off the U.K., Phillips Petroleum Co. (U.K.) Ltd. awarded Allseas Marine Contractors SA, Essen, Belgium, a pipelay and trenching contract for its Ann field development project in Block 49/6a.

Not Available

1992-08-10

412

Studies on sea snake venom  

PubMed Central

Erabutoxins a and b are neurotoxins isolated from venom of a sea snake Laticauda semifasciata (erabu-umihebi). Amino acid sequences of the toxins indicated that the toxins are members of a superfamily consisting of short and long neurotoxins and cytotoxins found in sea snakes and terrestrial snakes. The short neurotoxins to which erabutoxins belong act by blocking the nicotinic acetylcholine receptor on the post synaptic membrane in a manner similar to that of curare. X-ray crystallography and NMR analyses showed that the toxins have a three-finger structure, in which three fingers made of three loops emerging from a dense core make a gently concave surface of the protein. The sequence comparison and the location of essential residues on the protein suggested the mechanism of binding of the toxin to the acetylcholine receptor. Classification of snakes by means of sequence comparison and that based on different morphological features were inconsistent, which led the authors to propose a hypothesis “Evolution without divergence.” PMID:21422738

TAMIYA, Nobuo; YAGI, Tatsuhiko

2011-01-01

413

4, 47374776, 2004 Sea salt in snow on  

E-print Network

ACPD 4, 4737­4776, 2004 Sea salt in snow on Arctic sea ice and in coastal regions F. Domine et al and Physics Discussions The origin of sea salt in snow on Arctic sea ice and in coastal regions F. Domine 1, 4737­4776, 2004 Sea salt in snow on Arctic sea ice and in coastal regions F. Domine et al. Title Page

Paris-Sud XI, Université de

414

Solution notches, earthquakes, and sea level, Haiti  

Microsoft Academic Search

Shortly after the 12 January 2010 Haiti earthquake, we installed an array of five tide gauges to determine sea level and its variability in the region of uplifted corals on the coast SW of Leogane, Haiti, that had been uplift <=30 cm during the earthquake. Each gauge consists of a pressure transducer bolted 50-80 cm below mean sea level, which

C. R. Schiffman; B. S. Mildor; R. G. Bilham

2010-01-01

415

Earthquakes and secular sea level rise  

Microsoft Academic Search

By means of a model of global postseismic deformation we have computed the cumulative residual vertical displacement, the geoid heigth changes and the relative sea level variations due to all the M>=7 earthquakes of the last century. Our aim is to ascertain if earthquakes could play a role in the assessment of the trend of sea level rise observed by

D. Melini; A. Piersanti; G. Spada; E. Casarotti

2003-01-01

416

Sea Scallop Shell Lab Teacher's Guide  

NSDL National Science Digital Library

Used in combination with the Sea Scallop Lab handout, students will examine sea scallop shells to determine their size, approximate age, and meat yield. This lab activity is complete with objectives, math and science standards, materials list, procedure, and extensions. The handout is available from the COSEE-NE OSEI resource site.

417

Atlantic Air-Sea Interaction Revisited  

NASA Astrophysics Data System (ADS)

INTRODUCTION DATA AND MODELS THE ANALYSIS METHOD ATMOSPHERIC FORCING OF NORTH ATLANTIC SEA SURFACE TEMPERATURES NORTH ATLANTIC SEA SURFACE TEMPERATURE FORCING OF THE ATMOSPHERE Observational Evidence Model Results POTENTIAL SEASONAL PREDICTABILITY BASED ON THE ATMOSPHERE GENERAL - CIRCULATION MODEL CONCLUSIONS AND DISCUSSION REFERENCES

Rodwell, M. J.

418

Scientific reticence and sea level rise  

Microsoft Academic Search

I suggest that a ‘scientific reticence’ is inhibiting the communication of a threat of a potentially large sea level rise. Delay is dangerous because of system inertias that could create a situation with future sea level changes out of our control. I argue for calling together a panel of scientific leaders to hear evidence and issue a prompt plain-written report

J. E. Hansen

2007-01-01

419

Metagenomic Sequencing of Two Salton Sea Microbiomes  

PubMed Central

The Salton Sea is the largest inland body of water in California, with salinities ranging from brackish freshwater to hypersaline. The lake experiences high nutrient input, and its surface water is exposed to temperatures up to 40°C. Here, we report the community profiles associated with surface water from the Salton Sea. PMID:24459270

Hawley, Erik R.; Schackwitz, Wendy

2014-01-01

420

Optical properties of the Kara Sea  

Microsoft Academic Search

This study was motivated by the need to understand dispersion processes which affect the redistribution of nuclear wastes in the Arctic from dump sites in the Kara Sea and in the rivers which flow into the Kara Sea. We focus on vertical profiles of light beam transmission and fluorometry made over the delta region fronting the Ob and Yenisey Rivers

Donald R. Johnson; Vernon Asper; Thomas McClimans; Alan Weidemann

2000-01-01

421

Estimating Diet Composition in Sea Lions  

E-print Network

Estimating Diet Composition in Sea Lions: Which Technique to Choose? Dominic Tollit and Susan Columbia, Canada Abstract Reliable estimates of diets are vital to monitor impacts of sea lion popu, coupled with preferen- tial regurgitation and enumeration biases, can confound accurate diet

422

Sea Stars Underwater Offshore Northern California  

USGS Multimedia Gallery

Three sea stars on a rock, surrounded by a sandy seafloor littered with broken shells. Each sea star is approx. 10 - 15 cm (4-6 inches) across. Image acquired 4.5 km (3 miles) offshore Pigeon Point, southern San Mateo County, California at a depth of 52 meters....

423

Potential collapse of North Sea cod stocks  

Microsoft Academic Search

In common with many fish stocks in the North Sea, cod are heavily exploited with as much as 60% of the fishable stock being removed annually1. The International Council for the Exploration of the Sea (ICES), which advises fishery managers on the state of fish stocks in the northeast Atlantic, has recommended that exploitation rates be reduced considerably and immediately,

R. M. Cook; A. Sinclair; G. Stefánsson

1997-01-01

424

Sea level change: a philosophical approach  

Microsoft Academic Search

The present Cenozoic era is an icehouse episode characterized by a low sea level. Since the beginning of the industrial revolution, the human race has been emitting greenhouse gases, increasing the global atmospheric temperature, and causing a rise in sea level. If emissions continue to increase at the present rate, average global temperatures may rise by 1.5°C by the year

R. Leinfelder; H. Seyfried

1993-01-01

425

Frazil deposition under growing sea ice  

Microsoft Academic Search

Platelet ice may be an important component of Antarctic landfast sea ice. Typically, it is found at depth in first-year landfast sea ice cover, near ice shelves. To explain why platelet ice is not commonly observed at shallower depths, we consider a new mechanism. Our hypothesis is that platelet ice eventually appears due to the sudden deposition of frazil ice

M. J. McGuinness; M. J. M. Williams; P. J. Langhorne; C. Purdie; J. Crook

2009-01-01

426

Analysis of explosives in sea water  

Microsoft Academic Search

Summary A rapid method for the analysis of the explosives, TNT, RDX, and tetryl in sea water present in the part per billion to part per trillion range by vapor phase chromatography with the nickel-63 electron capture detector is described. Results of the analyses of sea water samples near two munitions dumping areas are given.

John C. Hoffsommer; Jerome M. Rosen

1972-01-01

427

Overview of Radioactive Waste Disposal at Sea  

Microsoft Academic Search

For hundreds of years, the seas have been used as a place to dispose of wastes from human activities. Although no high level radioactive waste has been disposed of into the sea, variable amounts of packaged low level radioactive wastes have been dumped at 47 sites in the northern part of the Atlantic and Pacific Oceans. in 1946 the first

Dominique Calmet

1992-01-01

428

Factors Affecting Sea Lamprey Egg Survival  

Microsoft Academic Search

Factors that affect recruitment of sea lampreys Petromyzon marinus are not well understood; for example, the majority (85%) of sea lamprey eggs are washed out of the nest, and the survival rate of these eggs is unknown. We examined the role of predation and substrate on egg survival in the laboratory and egg predation and dispersion of eggs outside the

Stephen J. Smith; J. Ellen Marsden

2009-01-01

429

Searching the Ocean for Deep Sea Vents  

NSDL National Science Digital Library

This Web-based slide show walks students through the painstaking and difficult search for deep sea vents. In pictures and text, it provides an overview of the subject explaining the process whereby the location of deep sea vents can be discovered from the surface using indirect methods.

430

Aquarius: Sea Surface Salinity from Space  

NSDL National Science Digital Library

Online in 2009, the Aquarius instrument will measure sea surface salinity. Site provides background information about salinity, salinity lesson plans, and salinity data and tools. Activities include relating salt to density, conductivity, buoyancy, and understanding the effect of the water cycle on salinity. View figures of sea surface salinity and temperature as they change from month to month and more.

431

California Sea Grant College Program Strategic Plan  

E-print Network

2014­2017 California Sea Grant College Program Strategic Plan 1 #12;The National Sea Grant College://nsgl.gso.uri.edu. University of California CASG College Program 9500 Gilman Dr., Dept. 0232 La Jolla, CA 92093-0232 (858) 534-4440 http://www.csgc.ucsd.edu Report No. P­010 Design: www.SharonBelknapDesign.com San Diego, California

Jaffe, Jules

432

Forward electromagnetic scattering models for sea ice  

Microsoft Academic Search

Recent advances in forward modeling of the electromagnetic scattering properties of sea ice are presented. In particular, the principal results include the following: (1) approximate calculations of electromagnetic scattering from multilayer random media with rough interfaces, based on the distorted Born approximation and radiative transfer (RT) theory; (2) comprehensive theory of the effective complex permittivity of sea ice based on

K. M. Golden; M. Cheney; Kung-Hau Ding; A. K. Fung; Thomas C. Grenfell; D. Isaacson; Jin Au Kong; S. V. Nghiem; J. Sylvester; P. Winebrenner

1998-01-01

433

Twentieth-century sea surface temperature trends  

Microsoft Academic Search

An analysis of historical sea surface temperatures provides evidence for global warming since 1900, in line with land-based analyses of global temperature trends, and also shows that over the same period, the eastern equatorial Pacific cooled and the zonal sea surface temperature gradient strengthened. Recent theoretical studies have predicted such a pattern as a response of the coupled ocean-atmosphere system

M. A. Cane; A. C. Clement; A. Kaplan

1997-01-01

434

Sea surface temperature measurements with AIRS  

NASA Technical Reports Server (NTRS)

The comparison of global sea surface skin temperature derived from cloud-free AIRS super window channel at 2616 cm-1 (sst2616) with the Real-Time Global Sea Surface Temperature for September 2002 shows surprisingly small standard deviation of 0.44K.

Aumann, H.

2003-01-01

435

Improvements on the Sea Gravimeter Gss2  

Microsoft Academic Search

ß Abstract. Several improvements made on the Askania 'Sea Gravimeter Gss2 after Graf' have considerably widened the scope of application of this instrument. Some of these altera- tions are described. The phenomena resulting from the heavier damping used are treated in detail. In the laboratory, the sea gravimeter was subjected to accelerations up to ñ100,000 mgal. It was found that

Anton Graf; Reinhard Schulze

1961-01-01

436

6, 1105111066, 2006 Sea ice, frost flowers  

E-print Network

ACPD 6, 11051­11066, 2006 Sea ice, frost flowers and halogen activation W. R. Simpson et al. Title than potential frost flower contact W. R. Simpson 1 , D. Carlson 1 , G. Hoenninger 1,2, , T. A. Douglas. Simpson (ffwrs@uaf.edu) 11051 #12;ACPD 6, 11051­11066, 2006 Sea ice, frost flowers and halogen activation

Paris-Sud XI, Université de

437

Paleoclimatic studies with Dead Sea Sediments  

E-print Network

evaluation of the global warming effects. DeadSea Saharo-Arabian desert belt ITCZ July Dead Sea basin Maximum and its late Quaternary climate history reflect global shifts of the major ocean- atmospheric systems dust washed to the lake by the winter floods. It provides information on the dust sources and mode

Shepard, Kenneth

438

Seismogeodynamics of the Caspian Sea Region  

Microsoft Academic Search

Results of studies of fluctuations in seismic regime of the Caspian Sea and adjacent area are ana- lyzed in order to reveal the correlation of anomalous variations in the sea level with seismicity of the region. The inferred regularities indicate that these phenomena have a common origin. A seismogeodynamic model of the region under consideration is discussed.

1999-01-01

439

Ocean Currents and Sea Surface Temperature  

NSDL National Science Digital Library

In this classroom activity, students access sea surface temperature and wind speed data from a NASA site, plot data, compare data, and draw conclusions about surface current and sea surface temperature and link their gained understanding to concerns about global climate change.

2007-01-01

440

Tritium level along Romanian Black Sea Coast  

SciTech Connect

Establishing the tritium level along the Romanian Black Sea Coast, after 10 years of exploitation of the nuclear power plant from Cernavoda, is a first step in evaluating its impact on the Black Sea ecosystem. The monitoring program consists of tritium activity concentration measurement in sea water and precipitation from Black Sea Coast between April 2005 and April 2006. The sampling points were spread over the Danube-Black Sea Canal - before the locks Agigea and Navodari, and Black Sea along the coast to the Bulgarian border. The average tritium concentration in sea water collected from the sampling locations had the value of 11.1 {+-} 2.1 TU, close to tritium concentration in precipitation. Although an operating nuclear power plant exists in the monitored area, the values of tritium concentration in two locations are slightly higher than those recorded elsewhere. To conclude, it could be emphasized that until now, Cernavoda NPP did not had any influence on the tritium concentration of the Black Sea Shore. (authors)

Varlam, C.; Stefanescu, I.; Popescu, I.; Faurescu, I. [National Inst. for Cryogenic and Isotopic Technologies, PO Box 10, Rm. Valcea, 24050 (Romania)

2008-07-15

441

Mailman seas Administrator's Guide 1.2  

E-print Network

: listname@lists.seas.upenn.edu The email will include instructions, a password and the URL for your list Options Administrative Interface (requires password) Administration page http://lists.seas.upenn.edu/mailman/admin/your-list passwords twice. Managing member lists Configuration Categories Membership Management View list members

Plotkin, Joshua B.

442

Ocean Currents and Sea Surface Temperature  

NSDL National Science Digital Library

In this classroom activity, students access sea surface temperature and wind speed data from a NASA site, plot and compare data, draw conclusions about surface current and sea surface temperature, and link their gained understanding to concerns about global climate change.

Joan Carter

443

SeaWiFS: North Pacific Storm  

NASA Technical Reports Server (NTRS)

An extratropical storm can be seen swirling over the North Pacific just south of Alaska. This SeaWiFS image was collected yesterday at 23:20 GMT. Credit: Provided by the SeaWiFS Project, NASA/Goddard Space Flight Center, and ORBIMAGE

2002-01-01

444

Metagenomic sequencing of two salton sea microbiomes.  

PubMed

The Salton Sea is the largest inland body of water in California, with salinities ranging from brackish freshwater to hypersaline. The lake experiences high nutrient input, and its surface water is exposed to temperatures up to 40°C. Here, we report the community profiles associated with surface water from the Salton Sea. PMID:24459270

Hawley, Erik R; Schackwitz, Wendy; Hess, Matthias

2014-01-01

445

The application of ERTS imagery to monitoring Arctic sea ice. [mapping ice in Bering Sea, Beaufort Sea, Canadian Archipelago, and Greenland Sea  

NASA Technical Reports Server (NTRS)

The author has identified the following significant results. Because of the effect of sea ice on the heat balance of the Arctic and because of the expanding economic interest in arctic oil and minerals, extensive monitoring and further study of sea ice is required. The application of ERTS data for mapping ice is evaluated for several arctic areas, including the Bering Sea, the eastern Beaufort Sea, parts of the Canadian Archipelago, and the Greenland Sea. Interpretive techniques are discussed, and the scales and types of ice features that can be detected are described. For the Bering Sea, a sample of ERTS-1 imagery is compared with visual ice reports and aerial photography from the NASA CV-990 aircraft. The results of the investigation demonstrate that ERTS-1 imagery has substantial practical application for monitoring arctic sea ice. Ice features as small as 80-100 m in width can be detected, and the combined use of the visible and near-IR imagery is a powerful tool for identifying ice types. Sequential ERTS-1 observations at high latitudes enable ice deformations and movements to be mapped. Ice conditions in the Bering Sea during early March depicted in ERTS-1 images are in close agreement with aerial ice observations and photographs.

Barnes, J. C. (principal investigator); Bowley, C. J.

1974-01-01

446

22 Years of Sea Surface Temperatures  

NSDL National Science Digital Library

This NOAA visualization video on YouTube shows the seasonal variations in sea surface temperatures and ice cover for the 22 years prior to 2007 based on data collected by NOAA polar-orbiting satellites (POES). El NiÃo and La NiÃa are easily identified, as are the trends in decreasing polar sea ice.

NOAA (National Oceanic and Atmospheric Administration) Visualizations

447

Inverse electromagnetic scattering models for sea ice  

Microsoft Academic Search

Inverse scattering algorithms for reconstructing the physical properties of sea ice from scattered electromagnetic field data are presented. The development of these algorithms has advanced the theory of remote sensing, particularly in the microwave region, and has the potential to form the basis for a new generation of techniques for recovering sea ice properties, such as ice thickness, a parameter

K. M. Goldenl; D. Borup; M. Cheney; E. Cherkaeva; M. S. Dawson; Kung-Hau Ding; A. K. Fung; D. Isaacson; S. A. Johnson; Arthur K. Jordan; Jin Au Kong; Ronald Kwok; Son V. Nghiem; Robert G. Onstott; J. Sylvester; D. P. Winebrenner; I. H. H. Zabel

1998-01-01

448

Sea Change Part 2: In the Lab  

NSDL National Science Digital Library

This video is the second of a three-video series in the Sea Change project, which follows the work of Dr. Maureen Raymo, paleogeologist at Columbia University's Lamont-Doherty Earth Observatory, who travels with fellow researchers to Australia in search of evidence of sea level that was once higher than it is today.

Daniel Grossman

449

Monsters of the Deep: Deep Sea Bioluminescence  

NSDL National Science Digital Library

This award-winning Sea and Sky website uses creative graphics to explore deep sea bioluminescence. It defines the phenomenon of bioluminescence, explains the chemical reactions involved, describes organisms with this adaptation, and investigates possible reasons for this dazzling light show. Links direct users to similar pages about hydrothermal vents, ocean layers, and more.

J.D. Knight

450

Color Difference in Bering Sea Phytoplankton Blooms  

NASA Technical Reports Server (NTRS)

There is considerable color variation in the phytoplankton blooms in the Bering Sea -- from the aquamarine west of Nunivak Island to the almost reddish patch west of St. Matthew Island to the green eddy astride the International dateline at 60 North latitude and 178 East longitude. Credit: Provided by the SeaWiFS Project, NASA/Goddard Space Flight Center, and ORBIMAGE

2002-01-01

451

More on Sea Turtles and Seaweed  

ERIC Educational Resources Information Center

"Sea turtle" and "seaweed"--otherwise known as "returnee from abroad" and "unemployed from abroad," respectively-- are a pair of popular new terms that are innately connected. In this article, the author discusses the common plight faced by "sea turtles" and "seaweeds" who returned from abroad to work in China. The author describes the experiences…

Xin, Tian

2005-01-01

452

Teaching Wide Sargasso Sea in New Jersey  

ERIC Educational Resources Information Center

High school teacher Susan Arpajian Jolley emphasizes experience and understanding by using the related novels "Wide Sargasso Sea" and "Jane Eyre" to help her students travel into unfamiliar cultural territory. "Wide Sargasso Sea" relates to Caribbean history and culture, feminism, race relations, colonialism, and personal identity.

Jolley, Susan Arpajian

2005-01-01

453

Petroleum geology of the Black Sea  

Microsoft Academic Search

The Black Sea comprises two extensional basins formed in a back-arc setting above the northward subducting Tethys Ocean, close to the southern margin of Eurasia. The two basins coalesced late in their post-rift phases in the Pliocene, forming the present single depocentre. The Western Black Sea was initiated in the Aptian, when a part of the Moesian Platform (now the

A. G. Robinson; J. H. Rudat; C. J. Banks; R. L. F. Wiles

1996-01-01

454

20,000 Microbes Under the Sea  

NSDL National Science Digital Library

This website contains the introduction to a Discover Magazine article about bacteria found living under the floor of the Black Sea. The sea floor core, taken in 2001, contained a cubic meter of bacteria. The full article is available to Discover Magazine Subscribers or may be purchased online.

Robert Kunzig

455

Long-term projection: Initializing sea level  

NASA Astrophysics Data System (ADS)

Long-term climate change and sea-level rise in model projections have been primarily determined by external forcing of climate conditions. Now, research shows that centennial projections of the dynamic sea level are also sensitive to the ocean's initial conditions.

Yin, Jianjun

2015-04-01

456

Sea Change Part 1: In the Field  

NSDL National Science Digital Library

This video is the first of a three-video series from the Sea Change project. It features the field work of scientists from the US and Australia looking for evidence of sea level rise during the Pliocene era when Earth was (on average) about 2 to 3 degrees Celsius hotter than it is today.

Daniel Grossman

457

Sea Level: On the Rise Lesson Plan  

NSDL National Science Digital Library

"Sea Level: On the Rise" is designed to teach middle-school students about the relationship between climate change and sea-level rise. It is a lesson plan created for the Environmental Protection Agency's Student's Guide to Global Climate Change.

Environmental Protection Agency

458

Sea Change Part III: Interpreting the Results  

NSDL National Science Digital Library

This video is the third in a three-part series by the Sea Change project, about scientists' search for Pleiocene beaches in Australia and elsewhere to establish sea level height during Earth's most recent previous warm period. This segment features the research of Jerry Mitrovica, Harvard geophysicist.

Daniel Grossman

459

The wind sea and swell waves climate in the Nordic seas  

NASA Astrophysics Data System (ADS)

A detailed climatology of wind sea and swell waves in the Nordic Seas (North Sea, Norwegian Sea, and Barents Sea), based on the high-resolution reanalysis NORA10, developed by the Norwegian Meteorological Institute, is presented. The higher resolution of the wind forcing fields, and the wave model (10 km in both cases), along with the inclusion of the bottom effect, allowed a better description of the wind sea and swell features, compared to previous global studies. The spatial patterns of the swell-dominated regional wave fields are shown to be different from the open ocean, due to coastal geometry, fetch dimensions, and island sheltering. Nevertheless, swell waves are still more prevalent and carry more energy in the Nordic Seas, with the exception of the North Sea. The influence of the North Atlantic Oscillation on the winter regional wind sea and swell patterns is also presented. The analysis of the decadal trends of wind sea and swell heights during the NORA10 period (1958-2001) shows that the long-term trends of the total significant wave height (SWH) in the Nordic Seas are mostly due to swell and to the wave propagation effect.

Semedo, Alvaro; Vettor, Roberto; Breivik, Øyvind; Sterl, Andreas; Reistad, Magnar; Soares, Carlos Guedes; Lima, Daniela

2015-02-01

460

Ocean primary production estimation of China Bohai Sea and Yellow Sea by HY-COCTS  

NASA Astrophysics Data System (ADS)

China Bohai Sea and Yellow Sea are semi-enclosed sea which locate between China continent and Korea peninsula, and affected by high turbid runoffs and strong monsoon. With the significant seasonal variation in temperate zone and local interests about fishery and ecosystem security in Margin Sea, China Bohai Sea and Yellow Sea is a good place for ocean primary production observation and researches. China has its own ocean satellite HY-1A in year 2002, and accumulated nearly two years of ocean color data, which can apply to marine environmental protection and resources management. Utilized the data of HY-1A aboard sensor, COCTS, ocean primary production of China Bohai Sea and Yellow Sea from July, 2002 to July, 2003 was estimated with a local primary production model. The seasonal evolution of algal biomass and external environmental changes, like depth of euphotic layer (Zeu), photosynthetic available radiation (PAR), and sea surface temperature (SST), affect the primary production in a complex way. Based on the input parameters of algorithm, spatial and temporal variation of primary production in China Bohai Sea and Yellow Sea was analyzed, revealing a maximum in summer, and a minimum in winter, and the offshore maximum front of primary production is significantly observed, under the balance of available light and nutrient limitation. The application of China ocean satellite data shows its good performance in the retrieval of compound biological and chemical parameters.

Bai, Yan; Pan, Delu; He, Xianqiang; Gong, Fang

2005-10-01

461

75 FR 38935 - Fisheries of the Northeastern United States; Black Sea Bass Fishery; 2010 Black Sea Bass...  

Federal Register 2010, 2011, 2012, 2013, 2014

...Fisheries of the Northeastern United States; Black Sea Bass Fishery; 2010 Black Sea Bass Specifications; Emergency Rule Extension...extending the emergency action to increase the 2010 black sea bass specifications (i.e., commercial...

2010-07-07

462

75 FR 6586 - Fisheries of the Northeastern United; Black Sea Bass Fishery; 2010 Black Sea Bass Specifications...  

Federal Register 2010, 2011, 2012, 2013, 2014

...100120036-0038-01] Fisheries of the Northeastern United; Black Sea Bass Fishery; 2010 Black Sea Bass Specifications; Emergency Rule AGENCY...rule NMFS is implementing increases to the 2010 black sea bass specifications (i.e., commercial...

2010-02-10

463

75 FR 59154 - Fisheries of the Northeastern United States; Black Sea Bass Fishery; 2010 Black Sea Bass...  

Federal Register 2010, 2011, 2012, 2013, 2014

...0648-XT99 Fisheries of the Northeastern United States; Black Sea Bass Fishery; 2010 Black Sea Bass Specifications; Emergency Rule Extension...extend the emergency action to increase the 2010 black sea bass specifications. The preamble text of...

2010-09-27

464

Caspian Sea surface circulation variability inferred from satellite altimeter and sea surface temperature  

NASA Astrophysics Data System (ADS)

Multiyear (1993-2007) satellite-derived Sea Level Anomaly (SLA), Sea Surface Temperature (SST), and model-derived mean dynamic topography were used together to analyze climatological and interannual variations of the Caspian Sea surface circulation. Constructed geostrophic currents are in good agreement with the known circulation features of the Caspian Sea, obtained from models and verified by some drifter observations. It is shown that the climatological surface circulation of the Middle Caspian Sea (MCS) is dominated by a basin-wide cyclonic circulation in winter, switching to an anticyclonic circulation in summer. A dipole pattern (an anticyclonic eddy near 39.5°N and a cyclonic one near 38°N) exist in the Southern Caspian Sea (SCS) (stronger from September to January). Evaluation of the multiyear geostrophic velocities shows that the Caspian Sea surface circulation exhibits strong interannual variations, with the location and intensity of the circulation patterns changing from one year to another.

Gunduz, Murat

2014-02-01

465

Quantifying the influence of sea ice on ocean microseism using observations from the Bering Sea, Alaska  

NASA Astrophysics Data System (ADS)

Microseism is potentially affected by all processes that alter ocean wave heights. Because strong sea ice prevents large ocean waves from forming, sea ice can therefore significantly affect microseism amplitudes. Here we show that this link between sea ice and microseism is not only a robust one but can be quantified. In particular, we show that 75-90% of the variability in microseism power in the Bering Sea can be predicted using a fairly crude model of microseism damping by sea ice. The success of this simple parameterization suggests that an even stronger link can be established between the mechanical strength of sea ice and microseism power, and that microseism can eventually be used to monitor the strength of sea ice, a quantity that is not as easily observed through other means.

Tsai, Victor C.; McNamara, Daniel E.

2011-11-01

466

Potential for rapid transport of contaminants from the Kara Sea.  

PubMed

Export of sea ice from the Kara Sea may redistribute contaminants entrained from atmospheric, marine and riverine sources. Ice exiting the Kara Sea ice to the north, will influence the Fram Strait, Svalbard and Barents Sea regions. Kara Sea ice may also be exported to the Barents Sea through straits north and south of Novaya Zemlya. Some ice from the Kara Sea makes its way into the Laptev Sea to the north and south of Severnaya Zemlya. Data on ice exchange and contaminant levels are not adequate to assess contaminant flux. PMID:9241881

Pfirman, S L; Kögeler, J W; Rigor, I

1997-08-25

467

Volga River Delta and Caspian Sea  

NASA Technical Reports Server (NTRS)

This true-color MODIS image from May 10, 2002, captures Russia's Volga River (running south through the center) emptying into the northern portion of the Caspian Sea. The waters of the Caspian Sea are quite murky in this image, highlighting the water quality problems plaguing the sea. The sea is inundated with sewage and industrial and agricultural waste, which is having measurable impact on human health and wildlife. According reports from the Department of Energy, in less than a decade the sturgeon catch dropped from 30,000 tons to just over 2,000 tons. National and international groups are currently joining together to find strategies of dealing with the environmental problems of the Caspian Sea. Credit: Jacques Descloitres, MODIS Land Rapid Response Team, NASA/GSFC

2002-01-01

468

Global Ups and Downs, Changing Sea Level  

NSDL National Science Digital Library

This unitfocuses on the concept that changes in sea level have occurred in the past, are occurring now, and will continue to occur. The unit provides an inquiry-based exploration of the lines of evidence for periodic melting of ice and resulting sea level rise: glacial evidence, geologic evidence, fossil evidence, and isotopic evidence. Students learn about the worldwide effects of sea level changes in the past and then use a study on topography and sea level to demonstrate their understanding of impact of sea level change on flora, fauna, and human society. Details about the supported concepts and standards, lessons with activities organized into teachable units, and a section describing the online resources used in the unit are provided for ready reference.

2005-01-01

469

Geothermal development and the Salton Sea  

NASA Astrophysics Data System (ADS)

The paper examines the relationship of the Salton Sea, a key element of the Imperial Valley water system, to potential geothermal development. Both water quantity and quality considerations suggest that the Salton Sea cannot be used as a repository for large amounts of geothermal brine. Diversion of some of the inflow to the Sea will have the beneficial effect of lowering the surface level, but will also tend to increase the salinity level. For the cooling water diversion to a 100 MW power plant, both effects are small; for a 1000 MW power plant, the effects are substantial. The use of Salton Sea water for injection fluid to maintain geothermal reservoir pressure will lower the elevation of the Sea and reduce its salinity.

Goldsmith, M.

1976-12-01

470

Early Spring Dust over the Mediterranean Sea  

NASA Technical Reports Server (NTRS)

The Sea-viewing Wide Field-of-view Sensor (SeaWiFS) observed this large cloud of dust (brownish pixels) blowing from northern Africa across the Mediterranean Sea on March 4, 2002. The dust can be seen clearly blowing across Southern Italy, Albania, Greece, and Turkey-all along the Mediterranean's northeastern shoreline. Notice that there also appears to be human-made aerosol pollution (greyish pixels) pooling in the air just south of the Italian Alps and blowing southeastward over the Adriatic Sea. The Alps can be easily identified as the crescent-shaped, snow-capped mountain range in the top center of this true-color scene. There also appears to be a similar haze over Austria, Hungary, and Yugoslavia to the north and east of Italy. Image courtesy the SeaWiFS Project, NASA/Goddard Space Flight Center, and ORBIMAGE

2002-01-01

471

Wind-driven circulation in Titan's seas  

NASA Astrophysics Data System (ADS)

Circulation in Titan's seas forced by wind is simulated by an ocean circulation model using surface wind data predicted by a global circulation model. Wind-driven circulation is insignificant throughout much of the annual cycle but becomes significant from late spring to late summer, when the wind stress becomes strong. The large-scale circulation in summer is predominantly southward near the sea surface and northward near the sea bottom. The sea surface current can get as fast as 5 cms-1 in some areas. Titan's rotation affects the vertical structure of sea currents in the form of an Ekman spiral if the wind is strong. The maximum wind setup at the shores is of the same order of magnitude as the tidal range. Wind stirring may reduce thermal stratification in summer but may be unable to destroy stratification of methane-rich liquids on top of ethane-rich liquids that can result from imbalances between evaporation and precipitation.

Tokano, Tetsuya; Lorenz, Ralph D.

2015-01-01

472

Brine-ecosystem interactions in sea ice  

NASA Astrophysics Data System (ADS)

Microalgae grow in brine inclusions in sea ice. Previous sea ice-ecosystem models neglect brine-microalgae interactions, prescribing the location of the microbial communities. In this study, a sea ice model with explicit brine dynamics coupled to a simple nutrient-phytoplankton (N-P) module (diatoms and dissolved silicates) is introduced. The model predicts bottom and surface microalgal populations. In fall, brine convection in cooling ice supplies nutrients, which favors microalgal growth. In early summer, the vertical brine density profile in warmer ice stabilizes, nutrient supply shuts off, which prevents further biomass building. Sensitivity tests in an idealized Antarctic pack ice configuration suggest that mode of microalgal transport within brine (passive or active) induces important population differences. This study is a step toward a more realistic sea ice-ecosystem model, which is required to understand the role of sea ice and associated ecosystems in global biogeochemical cycles.

Vancoppenolle, M.; Bitz, C. M.; Fichefet, T.; Goosse, H.; Lancelot, C.; Tison, J.

2010-12-01

473

Ice core records as sea ice proxies: An evaluation from the Weddell Sea region of Antarctica  

NASA Astrophysics Data System (ADS)

Ice core records of methanesulfonic acid (MSA) from three sites around the Weddell Sea are investigated for their potential as sea ice proxies. It is found that the amount of MSA reaching the ice core sites decreases following years of increased winter sea ice in the Weddell Sea; opposite to the expected relationship if MSA is to be used as a sea ice proxy. It is also shown that this negative MSA-sea ice relationship cannot be explained by the influence that the extensive summer ice pack in the Weddell Sea has on MSA production area and transport distance. A historical record of sea ice from the northern Weddell Sea shows that the negative relationship between MSA and winter sea ice exists over interannual (˜7-year period) and multidecadal (˜20-year period) timescales. National Centers for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) reanalysis data suggest that this negative relationship is most likely due to variations in the strength of cold offshore wind anomalies traveling across the Weddell Sea, which act to synergistically increase sea ice extent (SIE) while decreasing MSA delivery to the ice core sites. Hence our findings show that in some locations atmospheric transport strength, rather than sea ice conditions, is the dominant factor that determines the MSA signal preserved in near-coastal ice cores. A cautious approach is thus required in using ice core MSA for reconstructing past sea ice conditions, including the need for networks of ice core records and multiproxy studies to assess the significance of past MSA changes at different locations around Antarctica.

Abram, Nerilie J.; Mulvaney, Robert; Wolff, Eric W.; Mudelsee, Manfred

2007-08-01

474

Coherent sea level variation in and around the Sea of Okhotsk  

NASA Astrophysics Data System (ADS)

We investigated the seasonal and interannual variations of the sea level in and around the Sea of Okhotsk and their causes, based on tide gauge and satellite altimeter data. The sea level all along the coastal region of the Sea of Okhotsk is found to be dominated by the seasonal variation with a maximum in winter and a minimum in summer, which cannot be explained by the annual cycle of atmospheric heat flux and pressure. This sea level variation appears to reflect ocean current variations. Both the Arrested Topographic Waves (ATWs) caused by alongshore wind stress and the Sverdrup transport by wind stress curl show corresponding seasonal variations. Seasonal amplitude of the sea level is relatively large along Sakhalin Island with a tendency of a larger amplitude toward the south. This meridional dependence is consistent with the ATWs, but not with the Sverdrup transport in the Sea of Okhotsk. Seasonal variation of the geostrophic current velocity expected from the sea level variation is comparable to that of the observed nearshore current and is consistent with the theoretical ATW transport. It is also revealed that, on an interannual timescale, the wintertime sea level fluctuates quite coherently all around the Sea of Okhotsk and further along the East Kamchatka and Oyashio coasts in the North Pacific. The altimeter data clearly show that this coherent sea level variation is trapped over the coastal and continental shelf regions with depths shallower than 1000 m. The wintertime sea levels have a higher correlation with the ATW transport than with the Sverdrup transport in the Sea of Okhotsk and the upstream East Kamchatka coast. All these suggest that the interannual sea level variation along the coastal and shelf regions in winter, as well as the seasonal variation, is mainly caused by the ATWs (coastal trapped current forced by the alongshore wind stress). The wintertime Sverdrup transport, raised by the previous studies, is the secondary contributor to these variations.

Nakanowatari, Takuya; Ohshima, Kay I.

2014-08-01

475

Sea ice-albedo climate feedback mechanism  

SciTech Connect

The sea ice-albedo feedback mechanism over the Arctic Ocean multiyear sea ice is investigated by conducting a series of experiments using several one-dimensional models of the coupled sea ice-atmosphere system. In its simplest form, ice-albedo feedback is thought to be associated with a decrease in the areal cover of snow and ice and a corresponding increase in the surface temperature, further decreasing the area cover of snow and ice. It is shown that the sea ice-albedo feedback can operate even in multiyear pack ice, without the disappearance of this ice, associated with internal processes occurring within the multiyear ice pack (e.g., duration of the snow cover, ice thickness, ice distribution, lead fraction, and melt pond characteristics). The strength of the ice-albedo feedback mechanism is compared for several different thermodynamic sea ice models: a new model that includes ice thickness distribution., the Ebert and Curry model, the Mayjut and Untersteiner model, and the Semtner level-3 and level-0 models. The climate forcing is chosen to be a perturbation of the surface heat flux, and cloud and water vapor feedbacks are inoperative so that the effects of the sea ice-albedo feedback mechanism can be isolated. The inclusion of melt ponds significantly strengthens the ice-albedo feedback, while the ice thickness distribution decreases the strength of the modeled sea ice-albedo feedback. It is emphasized that accurately modeling present-day sea ice thickness is not adequate for a sea ice parameterization; the correct physical processes must be included so that the sea ice parameterization yields correct sensitivities to external forcing. 22 refs., 6 figs., 1 tab.

Schramm, J.L.; Curry, J.A. [Univ. of Colorado, Boulder, CO (United States); Ebert, E.E. [Bureau of Meterology Research Center, Melbourne (Australia)

1995-02-01

476

Geomagnetic Navigation in Sea Turtles  

NASA Astrophysics Data System (ADS)

Young loggerhead sea turtles (Caretta caretta) from eastern Florida undertake a transoceanic migration in which they gradually circle the north Atlantic Ocean before returning to the North American coast. Newly hatched turtles (hatchlings) begin the migration with a 'magnetic map' in which regional magnetic fields function as navigational markers and elicit changes in swimming direction at crucial geographic boundaries. In laboratory experiments, young turtles that had never before been in the ocean were exposed to fields like those that exist at various, widely separated locations along their transoceanic migratory route. Turtles responded by swimming in directions that would, in each case, help them remain within the North Atlantic gyre currents and advance along the migratory pathway. The results demonstrate that turtles can derive both longitudinal and latitudinal information from the Earth's field, and provide strong evidence that hatchling loggerheads inherit a remarkably elaborate set of responses that function in guiding them along their open-sea migratory route. For young sea turtles, couplings of oriented swimming to regional magnetic fields appear to provide the fundamental building blocks from which natural selection can sculpt a sequence of responses capable of guiding first-time ocean migrants along complex migratory routes. The results imply that hatchlings from different populations in different parts of the world are likely to have magnetic navigational responses uniquely suited for the migratory routes that each group follows. Thus, from a conservation perspective, turtles from different populations are not interchangeable. From an evolutionary perspective, the responses are not incompatible with either secular variation or magnetic polarity reversals. As Earth's field gradually changes, strong selective pressure presumably acts to maintain an approximate match between the responses of hatchlings and the fields that exist at critical points along the migratory pathway at any point in time. Although responses to regional fields might be rendered useless during occasional periods of rapid field change associated with magnetic polarity reversals or excursions, these sporadic events do not preclude the evolution of magnetic responses during the intervening and usually much longer intervals when Earth's field changes more slowly and is relatively stable.

Lohmann, K.; Putman, N.; Lohmann, C.

2011-12-01

477

Sea level change: a philosophical approach  

NASA Astrophysics Data System (ADS)

The present Cenozoic era is an ‘icehouse’ episode characterized by a low sea level. Since the beginning of the industrial revolution, the human race has been emitting greenhouse gases, increasing the global atmospheric temperature, and causing a rise in sea level. If emissions continue to increase at the present rate, average global temperatures may rise by 1.5°C by the year 2050, accompanied by a rise of about 30 cm in sea level. However, the prediction of future climatic conditions and sea level is hampered by the difficulty in modelling the interactions between the lithosphere, kryosphere, biosphere and atmosphere; in addition, the buffering capacity of our planet is still poorly understood. As scientists cannot offer unambiguous answers to simple questions, sorcerer's apprentices fill in the gaps, presenting plans to save planet without inconveniencing us. The geological record can help us to learn about the regulation mechanisms of our planet, many of which are connected with or expressed as sea level changes. Global changes in sea level are either tectono-eustatic or glacioeustatic. Plate tectonic processes strongly control sea levels and climate in the long term. There is a strong feed-back mechanism between sea level and climate; both can influence and determine each other. Although high sea levels are a powerful climatic buffer, falling sea levels accelerate climatic accentuation, the growth of the polar ice caps and will hence amplify the drop in sea level. Important sources of fossil greenhouse gases are botanic CO2 production, CO2 released by volcanic activity, and water vapour. The latter is particularly important when the surface area of the sea increases during a rise in sea level (‘maritime greenhouse effect’). A ‘volcanogenic greenhouse effect’ (release of volcanogenic CO2) is possibly not equally important, as intense volcanic activity may take place both during icehouse episodes as well as during greenhouse episodes. The hydrosphere, land vegetation and carbonate platforms are major CO2 buffers which may both take up and release CO2. CO2 can be released from the ocean due to changes in the pCO2 caused by growth of coral reefs and by uptake of CO2-rich freshwater from karst provinces. Efficient sinks of CO2 are the weathering products of silicate rocks; long-term sinks are organic deposits caused by regional anoxic events which preferrably develop during sea level rises and highstands; and coal-bearing strata. Deposition of limestone also removes CO2 from the atmospheric-hydrospheric cycle at a long term. Biotic crises are often related to either sea-level lows or sea-level highs. Long-term sea-level lows, characteristic of glacial periods, indicate cooling as major cause of extinction. During verly long-lasting greenhouse episodes the sea level is very high, climate and circulation systems are stable and biotic crises often develop as a consequence of oxygen depletion. On land, niche-splitting, complex food web structures and general overspecialization of biota will occur. Whether the crisis is caused by a single anoxic event (e.g. in the Late Devonian) or a disturbance by an asteroid impact (e.g. the Cretaceous/Tertiary boundary), it will only trigger total collapse of an ecosystem if a large part of it was already in decline. The regulatory mechanisms and buffers are thermodynamically extremely efficient if they are given sufficient time in which to deploy their power. However, after major catastrophes the re-establishment of successful ecosystems will take millions of years. The present rate of sea level and associated temperature rise is much too fast to be compensated and buffered by the network of natural controls. It is likely that the transitional time towards a new steady state will be an extremely variable and chaotic episode of unpredictable duration.

Leinfelder, R.; Seyfried, H.

1993-07-01

478

Review of critical factors for SEA implementation  

SciTech Connect

The implementation process involved in translating Strategic Environmental Assessment (SEA) intention into action is vital to an effective SEA. Many factors influence implementation and thus the effectiveness of an SEA. Empirical studies have identified and documented some factors influencing the implementation of an SEA. This research is fragmented, however, and it is still not clear what are the most critical factors of effective SEA performance, and how these relate to different stages of the implementation process or other contextual circumstances. The paper takes its point of departure in implementation theory. Firstly, we introduce implementation theory, and then use it in practice to establish a more comprehensive model related to the stages in the implementation process. Secondly, we identify the critical factors in order to see how they are related to the different stages of SEA or are more general in character. Finally we map the different critical factors and how they influence the overall results of an SEA. Based on a literature review, we present a comprehensive picture of the critical factors and where they are found in the process. We conclude that most of the critical factors identified are of a more general character influencing the SEA process as such, while only one out of four of these factors relates to the specific stages of the SEA. Based on this mapping we can sketch a picture of the totality of critical factors. In this study 266 notions of critical factors were identified. Seen at the level of notions of critical factors, only 24% of these relate to specific stages while for 76% the critical factors are of a more general nature. These critical factors interact in complex ways and appear in different combinations in different stages of the implementation process so tracing the cause and effect is difficult. The pervasiveness of contextual and general factors also clearly suggests that there is no single way to put SEA into practice. The paper identifies some of the critical factors for effective SEA implementation, but further research is still needed to conclude which factors are more critical than others, just as the contingencies on which they depend are not easy to unravel. - Highlights: Black-Right-Pointing-Pointer The research on critical factors influencing SEA implementation is fragmented. Black-Right-Pointing-Pointer The critical factors are used to discuss 'hot-spots' in the implementation process. Black-Right-Pointing-Pointer Critical factors are just as broad as the concept of effectiveness. Black-Right-Pointing-Pointer Both stage and general factors are relevant in explaining the effectiveness of SEA.

Zhang Jie, E-mail: jasmine@plan.aau.dk; Christensen, Per; Kornov, Lone

2013-01-15

479

Current Tropical Sea Surface Temperatures  

NSDL National Science Digital Library

This animation shows the most recent Sea Surface Temperature (SST) data available for the Gulf of Mexico and the Atlantic Coast region. Users can see the progression of warm waters (shown in yellow, orange, and red) slowly filling the Gulf of Mexico. This natural annual warming contributes to the possible formation of hurricanes in the Gulf. The animation updates every 24 hours, and still images of the data are also available. There is also imagery of the most recent 10-day average of SST anomalies in the Pacific Ocean, which is used by scientists for studying El Nino and La Nina. Warmer colors (yellow, red, orange) indicate positive anomalies (temperatures above normal). The imagery is from the Advanced Microwave Scanning Radiometer for EOS (AMSR-E) aboard the National Aeronautics and Space Administration's (NASA) Aqua satellite.

480

Find the Deep Sea Vent  

NSDL National Science Digital Library

This interactive tool helps students grasp the difficult task of locating deep sea vents by allowing them to virtually "survey" a portion of the Juan de Fuca Ridge in the Pacific Ocean. Students begin by using a CTD (Conductivity - Temperature - Depth) package to take a number of initial water-temperature readings. They then focus on a 40-kilometer (24.8-mile) path, taking up to 55 temperature readings along it. Based on their readings, they narrow in on a specific segment and select five points to survey, using the CTD package in its vertical mode. Finally, they select one of these points and send a submersible down to determine if they have truly found a hydrothermal vent.

481

Family conflicts in the sea.  

PubMed

In sexually reproducing organisms, conflicts of interest among family members are inevitable. The intensity of these conflicts depends upon the opportunities for parents and offspring to interact and the level of promiscuity. Despite the acknowledged role of family conflict in the evolutionary ecology of terrestrial organisms, its influence in the marine realm has largely been ignored. Nevertheless, marine organisms exhibit a wide range of reproductive and developmental modes through which sexual, sibling, and parent-offspring conflicts can manifest. Moreover, the existence of multiple mating in these species increases the likelihood, as well as the degree, of these conflicts. Consequently, many puzzling aspects of evolution in the sea, from life-history variation to diversification, could be clarified through the lens of conflict theory. PMID:20557975

Kamel, Stephanie Jill; Grosberg, Richard K; Marshall, Dustin J

2010-08-01

482

Plastic litter in the sea.  

PubMed

On June 2013 a workshop at the University of Siena (Italy) was organized to review current knowledge and to clarify what is known, and what remains to be investigated, concerning plastic litter in the sea. The content of the workshop was designed to contribute further to the European Marine Strategy Framework Directive (MSFD) following an inaugural workshop in 2012. Here we report a number of statements relevant to policymakers and scientists that was overwhelming agreement from the participants. Many might view this as already providing sufficient grounds for policy action. At the very least, this early warning of the problems that lie ahead should be taken seriously, and serve as a stimulus for further research. PMID:24157269

Depledge, M H; Galgani, F; Panti, C; Caliani, I; Casini, S; Fossi, M C

2013-12-01

483

Chemical Composition of Sea Fog Water Along the South China Sea  

NASA Astrophysics Data System (ADS)

The chemical and microphysical properties of sea fog were measured during a field experiment on Donghai Island, Zhanjiang of China from March 15 to April 18, 2010. The average pH and electrical conductivity (EC) value of the six sea fog cases during the experiment was 5.2 and 1,884 ?S/cm. The observed total ion concentration of sea fog was four orders of magnitude higher than those in the North Pacific and other sea areas of China. The dominant anion and cation in all sea fog water samples were Cl- and Na+, respectively. From backward trajectory analysis and ion loading computation, it can be concluded that the ions in the samples were transported either from pollutants in distant industrial cities or from local ion deposition processes. The concentration of Ca2+ in the sea fog water samples in Case 2 suggested that a dust storm in the Inner Mongolia, a northern region of China several thousand kilometers away, could reach the South China Sea. The data also showed that the sea fog droplet spectrum over the South China Sea is unimodal. Through relationship analysis, it is illustrated that the evolution of microphysics (such as droplet concentration, diameter, and liquid water content) during fog process could affect the chemical properties of sea fog.

Yue, Yanyu; Niu, Shengjie; Zhao, Lijuan; Zhang, Yu; Xu, Feng

2012-12-01

484

Polar Seas Oceanography: An Integrated Case Study of the Kara Sea  

NASA Astrophysics Data System (ADS)

What strikes first when browsing through this book is that the main title is misleading. Polar Seas Oceanography is, first of all, a book on ``an integrated case study of the Kara Sea,'' as the subtitle says. For readers who are interested more generally in polar oceanography, the book is probably the wrong choice. The Kara Sea is a rather shallow shelf sea within the Arctic Ocean, located between the Barents Sea to the west and the Laptev Sea to the east. The importance of the Kara Sea is manifold: climate change issues like ice formation and freshwater runoff, environmental problems from dumping of radioactive waste or oil exploitation, and finally, the Northern Sea route, which crosses large parts of the Kara Sea, underline the economical and ecological relevance of that region. In spite of severe climate conditions, the Kara Sea is relatively well investigated. This was achieved through intense oceanographic expeditions, aircraft surveys, and polar drift stations. Russian scientists from the Arctic and Antarctic Research Institute (AARI) carried out a major part of this outstanding work during the second half of the last century.

Harms, Ingo

2004-02-01

485

Regional Long-Term Sea Level and Sea Surface Temperature Characteristics from Satellite Observations  

NASA Astrophysics Data System (ADS)

For a the large portion of the world's population liv ing in coastal zones forecasts of long- term sea lev el change is importan t for a var iety of environmen tal and socio- economic r easons. Satellite altimetry offers a unique opportunity for improving our knowledge about glob al and r egional sea level change on bo th global and reg ional scale. Joint TOPEX/PO SEIDON(T/P) +JASON-1 sea level observations and Reyno lds AVH RR sea surface temperature observ ations over th e most recen t 12 years hav e qualitativ ely been used to study regional correlations between long-term changes in sea level and sea surface temper ature. Long-term is here tak en to be lin ear signals in the 12-year time per iod Consistent in creases in both sea level and sea surface temp eratures ar e found in large parts of the world's oceans over this per iod. In the Indian Ocean and particularly th e Pacif ic Ocean , the trends in both sea level and temper ature are domin ated by the larg e changes associated w ith th e El N iño Southern Oscillation (ENSO) . Co mparison with similar trend estimates u sing only 8 years of satellite data shows the incr eased decoupling with ENSO and th e imp act of inter-annual variability on sea lev el tr end estimates.

Andersen, O. B.; Knudsen, P.; Beckley, B.

2006-07-01

486

Putting SEA in context: A discourse perspective on how SEA contributes to decision-making  

SciTech Connect

Over the last couple of years there is an ongoing debate in the environmental assessment literature about the contribution of Strategic Environmental Assessment (SEA) to public decision-making and how this can be understood and enhanced by better incorporating insights from policy analysis, planning theory and political sciences. By explicitly framing SEA as an element in a process where stakeholders with diverging interests struggle, acceptability of SEA processes and results by stakeholders has become an important element in SEA evaluation. In addition, the importance of other context variables, such as the institutional organisation, and the need for SEA to adapt to this context, is stressed. Thus far, publications in this area have been dealing with the operationalisation of SEA's 'contribution', typologies of roles that SEA can or should play in different policy settings and on factors that stimulate or impede SEA to play these roles. In this paper an alternative approach is suggested that starts from the deliberative processes around a particular policy issue or decision supported by SEA. Of particular interest are 'discourses': the frames through which groups of actors give meaning to aspects of the policy issues and decisions that are supported by SEA. Discourses do not only reflect conflicts of interests and power play, but also the ways in which actors perceive and understand aspects of the world. Decision-making is conceptualised as a 'system of competing discourse coalitions and their struggles to 'control shared meanings' and to gain acceptance of their framing of a policy issue' [Durning D. A review of Fischer and Forrester (1993) The argumentative turn in policy analysis and planning. Policy Sci 1995;28(1):102-8]. SEA is one of the events in this process that may impact upon dominant discourses. Discourse analysis allows for an understanding of arguments that are considered legitimate for (not) incorporating particular elements of SEA. In addition it opens the door to relatively new strategies for SEA professionals to enhance their contribution to decision-making.

Runhaar, Hens [Copernicus Institute for Sustainable Development and Innovation, Utrecht University, P.O. Box 80115, 3508 TC Utrecht (Netherlands)], E-mail: h.runhaar@geo.uu.nl

2009-04-15

487

Mean sea surface topography in the Baltic Sea and its transition area to the North Sea: A geodetic solution and comparisons with oceanographic models  

NASA Astrophysics Data System (ADS)

A consistent height system designed for comparisons between geodesy and oceanography is presented for the Baltic Sea area. Mean sea surface topography is computed geodetically in this height system at 42 reliable long-term sea level stations, connected by high-precision levelings, along the coasts of the Baltic Sea, the Kattegat, the Skagerrak, and the adjacent part of the North Sea. Based on this, a map is drawn of the mean sea surface topography in the Baltic Sea and its transition area to the North Sea. The general agreement between our geodetic solution and recent oceanographic models turns out to be excellent; the discrepancies rarely exceed 2-3 cm. Hence the mean sea surface topography in the Baltic Sea area to a dominating extent is caused by the distribution of salinity. There are two main characteristics of the sea surface topography found here. First, there is a continuous increase of the sea surface height from the North Sea into the Baltic Sea, the height difference between the inner part of the Gulf of Bothnia and the Skagerrak amounting to 35-40 cm. The main reason behind this is the considerable difference in salinity, close to the maximum possible one. Second, there is a steep sea level gradient in the border zone between the Kattegat and the Skagerrak, reaching 2 cm per 10 km. This reflects the salinity front there, separating the brackish Baltic Sea water from the saline North Sea water, and the associated Baltic current. A local maximum in the sea surface can be seen in the Oslo Fiord, reflecting an accumulation of low-salinity water there. An area where there is still no oceanographic model agreeing sufficiently with the geodetic solution is the Belt Sea/southwestern Kattegat.

Ekman, Martin; MäKinen, Jaakko

1996-05-01

488

Galapagos Islands: Sea Cucumbers at Risk  

NSDL National Science Digital Library

Over the past weeks, heightened tensions have again placed the future of marine life of the Galapagos Islands into question. Beloved to students of evolution the world around, the Galapagos Islands -- and its unique wildlife -- are threatened by human population growth, invader species, and commercial fishing. Recently, the fishing of a rare variety of sea cucumber, Ischitopus fuscus, has gained international attention. The demand for sea cucumbers, which are used in cuisine in France and China, has risen over the past decade, resulting in the export of millions of sea cucumbers. In 1992, the Ecuadorian government imposed a ban on the fishing of sea cucumbers, but poaching continued at an alarming rate. In 1995, armed sea cucumber fishermen took over the ecologically famous Charles Darwin Research Station, forcing the return of the sea cucumber harvest. In 1998, the Ecuadorian government passed a series of sweeping protective measures (The Galapagos Conservation Law) for the Galapagos Islands. Despite enthusiasm from the international community, the new laws again seem uncertain in their effectiveness. This week's In The News chronicles recent events in the Galapagos, and the eight resources listed provide background information on the Galapagos and sea cucumbers.

Payne, Laura X.

489

Dissolved organic matter in the Baltic Sea  

NASA Astrophysics Data System (ADS)

Several factors highlight the importance of dissolved organic matter (DOM) in coastal ecosystems such as the Baltic Sea: 1) DOM is the main energy source for heterotrophic bacteria in surface waters, thus contributing to the productivity and trophic state of bodies of water. 2) DOM functions as a nutrient source: in the Baltic Sea, more than one-fourth of the bioavailable nutrients can occur in the dissolved organic form in riverine inputs and in surface water during summer. Thus, DOM also supports primary production, both directly (osmotrophy) and indirectly (via remineralization). 3) Flocculation and subsequent deposition of terrestrial DOM within river estuaries may contribute to production and oxygen consumption in coastal sediments. 4) Chromophoric DOM, which is one of the major absorbers of light entering the Baltic Sea, contributes highly to water color, thus affecting the photosynthetic depth as well as recreational value of the Baltic Sea. Despite its large-scale importance to the Baltic Sea ecosystem, DOM has been of minor interest compared with inorganic nutrient loadings. Information on the concentrations and dynamics of DOM in the Baltic Sea has accumulated since the late 1990s, but it is still sporadic. This review provides a coherent view of the current understanding of DOM dynamics in the Baltic Sea.

Hoikkala, L.; Kortelainen, P.; Soinne, H.; Kuosa, H.

2015-02-01

490

Climate, Ocean, and Sea Ice Modeling Project  

NSDL National Science Digital Library

This site provides an overview of the Climate, Ocean and Sea Ice Modeling Project (COSIM) and its mission to develop sea ice and ocean models which can be applied to coupled climate models. Research areas include polar processes, thermohaline circulation, ocean biogeochemistry, and eddy resolving ocean simulations. Available models include the Parallel Ocean Program (POP), the Los Alamos Sea Ice Model, and eventually the hybrid vertical coordinate version of POP. In addition, COSIM researchers have provided substantial input and development to the Miami Isopycnal Coordinate Ocean Model and its hybrid vertical coordinate equivalent Hybrid Coordinate Ocean Model. Links to these model pages contain model downloads, documentation and data.

Los Alamos National National Laboratory

491

Shelf Sea Oceanography and Meteorology Research Group  

NSDL National Science Digital Library

The Shelf Sea Oceanography and Meteorology Research Group, located at the University of Plymouth, furnishes summaries and reports of its current and recent research projects dealing with mesoscale physical processes, sediment transport, and other shelf and coastal oceanographic and meteorological challenges. Along with discovering the objectives of the endeavors, users can download the final report of the Black Sea Ecosystem Recovery Project, which quantified "shelf-deep transport of water masses and exchanges of nutrients by mesoscale activity at the North West Black Sea shelf break." Researchers can learn about past and upcoming seminars, conferences, and other events. The website offers links to abstracts of many of the group's publications as well.

492

District cooling in Stockholm using sea water  

SciTech Connect

In May this year Stockholm Energi started supplying properties in central Stockholm with cooling for comfort and for various processes from its new district cooling system. The project is unique in that most of the cooling energy is produced using cold water from the Baltic Sea. The following article describes the system and provides a summary of the considerations that resulted in venturing to invest in sea-water cooling for such a large project. There is also a description of the hydrological conditions that made the system feasible in Stockholm and some speculations about the possibilities to use cooled sea water elsewhere in the world.

Fermbaeck, G. [Stockholm Energie (Sweden)

1995-12-31

493

Quantile trends in Baltic sea level  

NASA Astrophysics Data System (ADS)

Quantile regression is applied for characterizing long-term sea-level variability in the Baltic Sea from long tide gauge records. The approach allows to quantify not only variability in the mean but also in extreme heights and thus provides a more complete description of regional sea-level variability. In the Baltic, slopes in minima are similar to the classical mean-based ordinary least squares slope, but maxima exhibit larger trends, particularly at the northernmost stations, in the Gulf of Bothnia, likely associated with changes in north Atlantic atmospheric circulation and particularly regional wind patterns.

Barbosa, Susana M.

2008-11-01

494

The summer climatology of Weddell Sea waters  

E-print Network

to the south by heavy ice cover (Owen 1941). Captain C. A, Larsen of Norway explored the region to the east of the Antarctic Peninsula in 1893. Today the ice shelf in that area bears his name. It was largely through this man' s efforts that whaling.... HISTORY OF THE EXPLORATION OF THE WEDDELL SEA III. OVERVIEW OF WEDDELL SEA OCEA NOGRAPHY 16 Wind-driven Surface Currents 16 Ice 19 Water Masses and Subsurface Circulation 23 The Southern Ocean 23 The Weddell Sea 27 The Antarctic Bottom Water...

Patterson, Steven Leroy

1972-01-01

495

Sea Ice, Climate and Fram Strait  

NASA Technical Reports Server (NTRS)

When sea ice is formed the albedo of the ocean surface increases from its open water value of about 0.1 to a value as high as 0.8. This albedo change effects the radiation balance and thus has the potential to alter climate. Sea ice also partially seals off the ocean from the atmosphere, reducing the exchange of gases such as carbon dioxide. This is another possible mechanism by which climate might be affected. The Marginal Ice Zone Experiment (MIZEX 83 to 84) is an international, multidisciplinary study of processes controlling the edge of the ice pack in that area including the interactions between sea, air and ice.

Hunkins, K.

1984-01-01

496

Effects of Mackenzie River discharge and bathymetry on sea ice in the Beaufort Sea  

NASA Astrophysics Data System (ADS)

Mackenzie River discharge and bathymetry effects on sea ice in the Beaufort Sea are examined in 2012 when Arctic sea ice extent hit a record low. Satellite-derived sea surface temperature revealed warmer waters closer to river mouths. By 5 July 2012, Mackenzie warm waters occupied most of an open water area about 316,000 km2. Surface temperature in a common open water area increased by 6.5°C between 14 June and 5 July 2012, before and after the river waters broke through a recurrent landfast ice barrier formed over the shallow seafloor offshore the Mackenzie Delta. In 2012, melting by warm river waters was especially effective when the strong Beaufort Gyre fragmented sea ice into unconsolidated floes. The Mackenzie and other large rivers can transport an enormous amount of heat across immense continental watersheds into the Arctic Ocean, constituting a stark contrast to the Antarctic that has no such rivers to affect sea ice.

Nghiem, S. V.; Hall, D. K.; Rigor, I. G.; Li, P.; Neumann, G.

2014-02-01

497

Effects of Mackenzie River Discharge and Bathymetry on Sea Ice in the Beaufort Sea  

NASA Technical Reports Server (NTRS)

Mackenzie River discharge and bathymetry effects on sea ice in the Beaufort Sea are examined in 2012 when Arctic sea ice extent hit a record low. Satellite-derived sea surface temperature revealed warmer waters closer to river mouths. By 5 July 2012, Mackenzie warm waters occupied most of an open water area about 316,000 sq km. Surface temperature in a common open water area increased by 6.5 C between 14 June and 5 July 2012, before and after the river waters broke through a recurrent landfast ice barrier formed over the shallow seafloor offshore the Mackenzie Delta. In 2012, melting by warm river waters was especially effective when the strong Beaufort Gyre fragmented sea ice into unconsolidated floes. The Mackenzie and other large rivers can transport an enormous amount of heat across immense continental watersheds into the Arctic Ocean, constituting a stark contrast to the Antarctic that has no such rivers to affect sea ice.

Nghiem, S. V.; Hall, D. K.; Rigor, I. G; Li, P.; Neumann, G.

2014-01-01

498

Movement of Sea Lamprey in the Lake Champlain Basin  

Microsoft Academic Search

Sea lamprey (Petromyzon marinus) are a nuisance aquatic species in the Great Lakes and Lake Champlain that have devastated native fish populations and hampered the restoration of sport fisheries. This study examined inter-basin movement of sea lamprey in Lake Champlain to identify tributaries that contribute parasitic-phase sea lamprey and provide information for prioritizing those tributaries for sea lamprey control. A

Eric A. Howe; J. Ellen Marsden; Wayne Bouffard

2006-01-01

499

Climate change impact on the Mediterranean Sea circulation  

E-print Network

Climate change impact on the Mediterranean Sea circulation: a regional modelling approach Samuel. In the Mediterranean Sea, many authors have also described a THC driven by heat and water losses at the sea surface getting into the Mediterranean Sea across the Gibraltar Strait at the surface and salty and cold water

Ribes, Aurélien

500

Food Consumption by Sea Lions: Existing Data and Techniques  

E-print Network

Food Consumption by Sea Lions: Existing Data and Techniques Arliss J. Winship, Andrea M.J. Hunter the quantity of prey that sea lions consume is a prerequisite for assessing the role of sea lions in aquatic that have been used to estimate the food requirements for the six spe- cies of sea lions. We reviewed data