12 CFR 1710.11 - Board of directors.

Code of Federal Regulations, 2012 CFR

2012-01-01

... member may not vote by proxy. (4) Information. Management of an Enterprise shall provide a board member... time to time. (b) Meetings, quorum and proxies, information, and annual review—(1) Frequency of..., regulations, and guidelines. (2) Non-management board member meetings. Non-management directors of an...

12 CFR 1710.11 - Board of directors.

Code of Federal Regulations, 2011 CFR

2011-01-01

... member may not vote by proxy. (4) Information. Management of an Enterprise shall provide a board member... time to time. (b) Meetings, quorum and proxies, information, and annual review—(1) Frequency of..., regulations, and guidelines. (2) Non-management board member meetings. Non-management directors of an...

12 CFR 1710.11 - Board of directors.

Code of Federal Regulations, 2013 CFR

2013-01-01

... member may not vote by proxy. (4) Information. Management of an Enterprise shall provide a board member... time to time. (b) Meetings, quorum and proxies, information, and annual review—(1) Frequency of..., regulations, and guidelines. (2) Non-management board member meetings. Non-management directors of an...

75 FR 1664 - Self-Regulatory Organizations; NYSE Amex LLC; Notice of Filing and Immediate Effectiveness of...

Federal Register 2010, 2011, 2012, 2013, 2014

2010-01-12

... Discretionary Voting for Election of Directors and on Material Amendments to Investment Advisory Contracts January 5, 2010. Pursuant to Section 19(b)(1) of the Securities Exchange Act of 1934 (``Act'') \\1\\ and... entitled ``Giving Proxies by Member Organization,'' to eliminate broker discretionary voting for the...

Suffrage for People with Intellectual Disabilities and Mental Illness: Observations on a Civic Controversy.

PubMed

Kopel, Charles

Most electoral democracies, including forty-three states in the United States, deny people the right to vote on the basis of intellectual disability or mental illness. Scholars in several fields have addressed these disenfranchisements, including legal scholars who analyze their validity under U.S. constitutional law and international-human-rights law, philosophers and political scientists who analyze their validity under democratic theory, and mental-health researchers who analyze their relationship to scientific categories. This Note reviews the current state of the debate across these fields and makes three contentions: (a) pragmatic political considerations have blurred the distinction between disenfranchisement provisions based on cognitive capacity and those based on personal status; (b) proposals that advocate voting by proxy trivialize the broad civic purpose of the franchise; and (c) the persistence of disenfranchisement on the basis of mental illness inevitably contributes to silencing socially disfavored views and lifestyles. Accordingly, the Note cautions reformers against advocating for capacity assessment or proxy voting, and emphasizes the importance of disassociating the idea of mental illness from voting capacity.

76 FR 10076 - Self-Regulatory Organizations; C2 Options Exchange, Incorporated; Notice of Filing and Order...

Federal Register 2010, 2011, 2012, 2013, 2014

2011-02-23

... election of a member of the board of directors of an issuer (except for a vote with respect to the uncontested election of a member of the board of directors of any investment company registered under the... proxy to vote stock that is registered in its name, unless: (i) Such Permit Holder is the beneficial...

76 FR 6009 - Shareholder Approval of Executive Compensation and Golden Parachute Compensation

Federal Register 2010, 2011, 2012, 2013, 2014

2011-02-02

...)(1) requires that ``[n]ot less frequently than once every 3 years, a proxy or consent or... Exchange Act, requiring that, ``[n]ot less frequently than once every 6 years, a proxy or consent or... determine whether [the say- on-pay vote] will occur every 1, 2, or 3 years.'' \\20\\ As discussed below, this...

A Quantum Proxy Weak Blind Signature Scheme Based on Controlled Quantum Teleportation

NASA Astrophysics Data System (ADS)

Cao, Hai-Jing; Yu, Yao-Feng; Song, Qin; Gao, Lan-Xiang

2015-04-01

Proxy blind signature is applied to the electronic paying system, electronic voting system, mobile agent system, security of internet, etc. A quantum proxy weak blind signature scheme is proposed in this paper. It is based on controlled quantum teleportation. Five-qubit entangled state functions as quantum channel. The scheme uses the physical characteristics of quantum mechanics to implement message blinding, so it could guarantee not only the unconditional security of the scheme but also the anonymity of the messages owner.

75 FR 38576 - Self-Regulatory Organizations; Notice of Filing of Proposed Rule Change by NYSE Arca, Inc. To...

Federal Register 2010, 2011, 2012, 2013, 2014

2010-07-02

... were to be made available on the proxy card) must immediately tender his or her resignation from the.... Under the proposed amendment to the Bylaws, the proxy card would change for an uncontested election, and... director's election (with ``abstentions'' not counted as a vote cast either ``for'' or ``against'' such...

29 CFR 1209.06 - Action necessary to close meetings; record of votes.

Code of Federal Regulations, 2010 CFR

2010-07-01

... 29 Labor 4 2010-07-01 2010-07-01 false Action necessary to close meetings; record of votes. 1209.06 Section 1209.06 Labor Regulations Relating to Labor (Continued) NATIONAL MEDIATION BOARD PUBLIC OBSERVATION OF NATIONAL MEDIATION BOARD MEETINGS § 1209.06 Action necessary to close meetings; record of votes...

45 CFR 614.7 - Record vote.

Code of Federal Regulations, 2012 CFR

2012-10-01

... Regulations Relating to Public Welfare (Continued) NATIONAL SCIENCE FOUNDATION GOVERNMENT IN THE SUNSHINE ACT REGULATIONS OF THE NATIONAL SCIENCE BOARD § 614.7 Record vote. (a) For purposes of this part a vote of the National Science Board is a “record vote” if: (1) It carries by a majority of all those holding office as...

45 CFR 614.7 - Record vote.

Code of Federal Regulations, 2013 CFR

2013-10-01

... Regulations Relating to Public Welfare (Continued) NATIONAL SCIENCE FOUNDATION GOVERNMENT IN THE SUNSHINE ACT REGULATIONS OF THE NATIONAL SCIENCE BOARD § 614.7 Record vote. (a) For purposes of this part a vote of the National Science Board is a “record vote” if: (1) It carries by a majority of all those holding office as...

45 CFR 614.7 - Record vote.

Code of Federal Regulations, 2011 CFR

2011-10-01

... Regulations Relating to Public Welfare (Continued) NATIONAL SCIENCE FOUNDATION GOVERNMENT IN THE SUNSHINE ACT REGULATIONS OF THE NATIONAL SCIENCE BOARD § 614.7 Record vote. (a) For purposes of this part a vote of the National Science Board is a “record vote” if: (1) It carries by a majority of all those holding office as...

45 CFR 614.7 - Record vote.

Code of Federal Regulations, 2010 CFR

2010-10-01

... Regulations Relating to Public Welfare (Continued) NATIONAL SCIENCE FOUNDATION GOVERNMENT IN THE SUNSHINE ACT REGULATIONS OF THE NATIONAL SCIENCE BOARD § 614.7 Record vote. (a) For purposes of this part a vote of the National Science Board is a “record vote” if: (1) It carries by a majority of all those holding office as...

45 CFR 614.7 - Record vote.

Code of Federal Regulations, 2014 CFR

2014-10-01

... Regulations Relating to Public Welfare (Continued) NATIONAL SCIENCE FOUNDATION GOVERNMENT IN THE SUNSHINE ACT REGULATIONS OF THE NATIONAL SCIENCE BOARD § 614.7 Record vote. (a) For purposes of this part a vote of the National Science Board is a “record vote” if: (1) It carries by a majority of all those holding office as...

A Quantum Multi-Proxy Weak Blind Signature Scheme Based on Entanglement Swapping

NASA Astrophysics Data System (ADS)

Yan, LiLi; Chang, Yan; Zhang, ShiBin; Han, GuiHua; Sheng, ZhiWei

2017-02-01

In this paper, we present a multi-proxy weak blind signature scheme based on quantum entanglement swapping of Bell states. In the scheme, proxy signers can finish the signature instead of original singer with his/her authority. It can be applied to the electronic voting system, electronic paying system, etc. The scheme uses the physical characteristics of quantum mechanics to implement delegation, signature and verification. It could guarantee not only the unconditionally security but also the anonymity of the message owner. The security analysis shows the scheme satisfies the security features of multi-proxy weak signature, singers cannot disavowal his/her signature while the signature cannot be forged by others, and the message owner can be traced.

12 CFR 1710.11 - Board of directors.

Code of Federal Regulations, 2010 CFR

2010-01-01

... Enterprise shall meet at regularly scheduled executive sessions without management participation. (3) Quorum... member may not vote by proxy. (4) Information. Management of an Enterprise shall provide a board member... Banks and Banking OFFICE OF FEDERAL HOUSING ENTERPRISE OVERSIGHT, DEPARTMENT OF HOUSING AND URBAN...

7 CFR 1245.102 - Voting.

Code of Federal Regulations, 2011 CFR

2011-01-01

... AND ORDERS; MISCELLANEOUS COMMODITIES), DEPARTMENT OF AGRICULTURE U.S. HONEY PRODUCER RESEARCH... arrangement involving totally independent entities cooperating only to produce U.S. honey or honey products... referendum covering only that producer's share of the ownership of U.S. honey or honey products. (b) Proxy...

75 FR 79417 - Record of Vote of Meeting Closure

Federal Register 2010, 2011, 2012, 2013, 2014

2010-12-20

...] Record of Vote of Meeting Closure I, Isaac Fulwood, of the United States Parole Commission, was present... following Commissioners voted that the meeting be closed: Isaac Fulwood, Cranston J. Mitchell and Patricia K.... Isaac Fulwood, Chairman, U.S. Parole Commission. [FR Doc. 2010-31860 Filed 12-17-10; 8:45 am] BILLING...

36 CFR 1151.4 - Delegations.

Code of Federal Regulations, 2011 CFR

2011-07-01

... 36 Parks, Forests, and Public Property 3 2011-07-01 2011-07-01 false Delegations. 1151.4 Section... BYLAWS § 1151.4 Delegations. (a) Executive Committee. The Board may delegate to the Executive Committee... authorities by two-thirds vote of the members present at a meeting and any proxies. A separate delegation is...

36 CFR 1151.4 - Delegations.

Code of Federal Regulations, 2010 CFR

2010-07-01

... 36 Parks, Forests, and Public Property 3 2010-07-01 2010-07-01 false Delegations. 1151.4 Section... BYLAWS § 1151.4 Delegations. (a) Executive Committee. The Board may delegate to the Executive Committee... authorities by two-thirds vote of the members present at a meeting and any proxies. A separate delegation is...

78 FR 17727 - Self-Regulatory Organizations; International Securities Exchange, LLC; Order Approving Proposed...

Federal Register 2010, 2011, 2012, 2013, 2014

2013-03-22

... and each Exchange Director's underlying business, ISE also stated that it believes that Exchange... Exchange to align its Board structure in accordance with corporate governance best practices guidelines... Services Proxy Voting Guidelines, the CalPERS Core Principles of Accountable Corporate Governance, the TIAA...

5 CFR 2421.15 - Secret ballot.

Code of Federal Regulations, 2012 CFR

2012-01-01

... 5 Administrative Personnel 3 2012-01-01 2012-01-01 false Secret ballot. 2421.15 Section 2421.15... FEDERAL LABOR RELATIONS AUTHORITY MEANING OF TERMS AS USED IN THIS SUBCHAPTER § 2421.15 Secret ballot. Secret ballot means the expression by ballot, voting machine or otherwise, but in no event by proxy, of a...

5 CFR 2421.15 - Secret ballot.

Code of Federal Regulations, 2011 CFR

2011-01-01

... 5 Administrative Personnel 3 2011-01-01 2011-01-01 false Secret ballot. 2421.15 Section 2421.15... FEDERAL LABOR RELATIONS AUTHORITY MEANING OF TERMS AS USED IN THIS SUBCHAPTER § 2421.15 Secret ballot. Secret ballot means the expression by ballot, voting machine or otherwise, but in no event by proxy, of a...

5 CFR 2421.15 - Secret ballot.

Code of Federal Regulations, 2014 CFR

2014-01-01

... 5 Administrative Personnel 3 2014-01-01 2014-01-01 false Secret ballot. 2421.15 Section 2421.15... FEDERAL LABOR RELATIONS AUTHORITY MEANING OF TERMS AS USED IN THIS SUBCHAPTER § 2421.15 Secret ballot. Secret ballot means the expression by ballot, voting machine or otherwise, but in no event by proxy, of a...

5 CFR 2421.15 - Secret ballot.

Code of Federal Regulations, 2010 CFR

2010-01-01

... 5 Administrative Personnel 3 2010-01-01 2010-01-01 false Secret ballot. 2421.15 Section 2421.15... FEDERAL LABOR RELATIONS AUTHORITY MEANING OF TERMS AS USED IN THIS SUBCHAPTER § 2421.15 Secret ballot. Secret ballot means the expression by ballot, voting machine or otherwise, but in no event by proxy, of a...

5 CFR 2421.15 - Secret ballot.

Code of Federal Regulations, 2013 CFR

2013-01-01

... 5 Administrative Personnel 3 2013-01-01 2013-01-01 false Secret ballot. 2421.15 Section 2421.15... FEDERAL LABOR RELATIONS AUTHORITY MEANING OF TERMS AS USED IN THIS SUBCHAPTER § 2421.15 Secret ballot. Secret ballot means the expression by ballot, voting machine or otherwise, but in no event by proxy, of a...

12 CFR 569.1 - Definitions.

Code of Federal Regulations, 2010 CFR

2010-01-01

... 12 Banks and Banking 5 2010-01-01 2010-01-01 false Definitions. 569.1 Section 569.1 Banks and Banking OFFICE OF THRIFT SUPERVISION, DEPARTMENT OF THE TREASURY PROXIES § 569.1 Definitions. As used in this part: (a) Security holder. The term security holder means any person having the right to vote in...

VeryVote: A Voter Verifiable Code Voting System

NASA Astrophysics Data System (ADS)

Joaquim, Rui; Ribeiro, Carlos; Ferreira, Paulo

Code voting is a technique used to address the secure platform problem of remote voting. A code voting system consists in secretly sending, e.g. by mail, code sheets to voters that map their choices to entry codes in their ballot. While voting, the voter uses the code sheet to know what code to enter in order to vote for a particular candidate. In effect, the voter does the vote encryption and, since no malicious software on the PC has access to the code sheet it is not able to change the voter’s intention. However, without compromising the voter’s privacy, the vote codes are not enough to prove that the vote is recorded and counted as cast by the election server.

17 CFR 240.14a-8 - Shareholder proposals.

Code of Federal Regulations, 2010 CFR

2010-04-01

..., the company must also provide in the form of proxy means for shareholders to specify by boxes a choice... held at least $2,000 in market value, or 1%, of the company's securities entitled to be voted on the... writing of any procedural or eligibility deficiencies, as well as of the time frame for your response...

75 FR 68846 - Self-Regulatory Organizations; The NASDAQ Stock Market LLC; Notice of Filing of Proposed Rule...

Federal Register 2010, 2011, 2012, 2013, 2014

2010-11-09

... business combination for which the Company must file and furnish a proxy or information statement subject... combination is being considered. If a shareholder vote on the business combination is held, [(e) Until the... working capital purposes) if the business combination is approved and consummated. A Company may establish...

Religion, Poverty, and Politics: Their Impact on Women's Reproductive Health Outcomes.

PubMed

Kimball, Richard; Wissner, Michael

2015-01-01

This study sought to explore the relationship(s) between U.S. states of selected social determinants of health (SDH) and three women's reproductive health outcomes including abortion, teen births, and infant mortality rates (IMR). The data from multiple population surveys were used to establish on a state-by-state basis, the interactions between selected SDH (religion, voting patterns, child poverty, and GINI) and their policy effects on three women's reproductive health outcomes (abortion, teen births, and IMRs) using publicly available national databases. Child poverty rates and the GINI coefficient were analyzed. Religiosity information was obtained from the Pew Forum's surveys. Voting results were collected from the 2008 congressional and presidential races and were used as proxy measures for conservative- versus liberal-leaning policies and policy makers. Using multiple regression analysis, higher IMRs were associated with higher religiosity scores. Lower abortion rates were associated with voting conservatively and higher income inequality. Higher teen birth rates were associated with higher child poverty rates and voting conservatively. This study shows that selected SDH may have substantial impacts on women's reproductive health outcomes at the state level. Significant inequalities exist between liberal and conservative states that affect women's health outcomes. © 2015 Wiley Periodicals, Inc.

29 CFR 2509.08-2 - Interpretive bulletin relating to the exercise of shareholder rights and written statements of...

Code of Federal Regulations, 2010 CFR

2010-07-01

..., fiduciaries also need to take into account costs when deciding whether and how to exercise their shareholder... into account in determining whether the exercise of such rights (e.g., the voting of a proxy..., statements may need to take into account factors such as the plan's funding policy and its liquidity needs as...

75 FR 66621 - Reporting of Proxy Votes on Executive Compensation and Other Matters

Federal Register 2010, 2011, 2012, 2013, 2014

2010-10-28

... rule and form amendments under the Securities Exchange Act of 1934 and the Investment Company Act of... and the Investment Company Act of 1940 (``Investment Company Act'').\\3\\ The Commission is also proposing a technical amendment to rule 30b1-4 under the Investment Company Act.\\4\\ \\1\\ 15 U.S.C. 78a et seq...

12 CFR 912.6 - Notice of meetings.

Code of Federal Regulations, 2010 CFR

2010-01-01

... Finance Board will publish the notice in the Federal Register. (c) Time—(1) Seven days notice. Except as.... When a majority of the Board of Directors determine by recorded vote that Finance Board business... least a majority of the Board Directors determines by recorded vote that Finance Board business so...

28 CFR 51.50 - Records concerning submissions.

Code of Federal Regulations, 2011 CFR

2011-07-01

... OF SECTION 5 OF THE VOTING RIGHTS ACT OF 1965, AS AMENDED Processing of Submissions § 51.50 Records... available for obtaining copies by the public, pursuant to written request directed to the Chief, Voting Section, Civil Rights Division, United States Department of Justice, Washington, DC. Such written request...

A bill to approve the Keystone XL Pipeline.

THOMAS, 113th Congress

Sen. Hoeven, John [R-ND

2014-05-01

Senate - 11/18/2014 Under the order of 11/12/14, not having achieved 60 votes in the affirmative, failed of passage in Senate by Yea-Nay Vote. 59 - 41. Record Vote Number: 280. (All Actions) Tracker: This bill has the status Failed SenateHere are the steps for Status of Legislation:

Rebuild America Jobs Act

THOMAS, 112th Congress

Sen. Klobuchar, Amy [D-MN

2011-10-31

Senate - 11/03/2011 Motion to proceed to consideration of measure under the order of 11/2/2011, not having achieved 60 votes in the affirmative, was rejected in Senate by Yea-Nay Vote. 51 - 49. Record Vote Number: 195. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Safe Communities, Safe Schools Act of 2013

THOMAS, 113th Congress

Sen. Reid, Harry [D-NV

2013-03-21

Senate - 04/18/2013 Amendment SA 730, under the order of 4/16/13, having achieved 60 votes in the affirmative, was agreed to in Senate by Yea-Nay Vote. 95 - 2. Record Vote Number: 105. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

77 FR 3829 - Self-Regulatory Organizations; NYSE Arca, Inc.; Notice of Filing and Order Granting Accelerated...

Federal Register 2010, 2011, 2012, 2013, 2014

2012-01-25

... SECURITIES AND EXCHANGE COMMISSION [Release No. 34-66192; File No. SR-NYSEArca-2012-02] Self-Regulatory Organizations; NYSE Arca, Inc.; Notice of Filing and Order Granting Accelerated Approval of a Proposed Rule Amendments to NYSE Arca Rule 9.4 and NYSE Equities Inc. Rules 5.3(d) and 9.4 Relating to Discretionary Proxy Voting on Executive...

75 FR 65680 - Self-Regulatory Organizations; International Securities Exchange, LLC; Notice of Filing and Order...

Federal Register 2010, 2011, 2012, 2013, 2014

2010-10-26

... election of a member of the board of directors of an issuer (other than an uncontested election of a... election of a member of the board of directors of an issuer (other than an uncontested election of a... proxy to vote stock that is registered in its name, unless: (i) Such Member is the beneficial owner of...

Representation of layer-counted proxy records as probability densities on error-free time axes

NASA Astrophysics Data System (ADS)

Boers, Niklas; Goswami, Bedartha; Ghil, Michael

2016-04-01

Time series derived from paleoclimatic proxy records exhibit substantial dating uncertainties in addition to the measurement errors of the proxy values. For radiometrically dated proxy archives, Goswami et al. [1] have recently introduced a framework rooted in Bayesian statistics that successfully propagates the dating uncertainties from the time axis to the proxy axis. The resulting proxy record consists of a sequence of probability densities over the proxy values, conditioned on prescribed age values. One of the major benefits of this approach is that the proxy record is represented on an accurate, error-free time axis. Such unambiguous dating is crucial, for instance, in comparing different proxy records. This approach, however, is not directly applicable to proxy records with layer-counted chronologies, as for example ice cores, which are typically dated by counting quasi-annually deposited ice layers. Hence the nature of the chronological uncertainty in such records is fundamentally different from that in radiometrically dated ones. Here, we introduce a modification of the Goswami et al. [1] approach that is specifically designed for layer-counted proxy records, instead of radiometrically dated ones. We apply our method to isotope ratios and dust concentrations in the NGRIP core, using a published 60,000-year chronology [2]. It is shown that the further one goes into the past, the more the layer-counting errors accumulate and lead to growing uncertainties in the probability density sequence for the proxy values that results from the proposed approach. For the older parts of the record, these uncertainties affect more and more a statistically sound estimation of proxy values. This difficulty implies that great care has to be exercised when comparing and in particular aligning specific events among different layer-counted proxy records. On the other hand, when attempting to derive stochastic dynamical models from the proxy records, one is only interested in the relative changes, i.e. in the increments of the proxy values. In such cases, only the relative (non-cumulative) counting errors matter. For the example of the NGRIP records, we show that a precise estimation of these relative changes is in fact possible. References: [1] Goswami et al., Nonlin. Processes Geophys. (2014) [2] Svensson et al., Clim. Past (2008)

Temporary Tax Holiday and Government Reduction Act

THOMAS, 112th Congress

Sen. Heller, Dean [R-NV

2011-11-30

Senate - 12/08/2011 Motion to proceed to consideration of measure, under the order of 12/8/2011, not having achieved the required 60 votes in the affirmative, was rejected in Senate by Yea-Nay Vote. 22 - 76. Record Vote Number: 225. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Middle Class Tax Cut Act of 2011

THOMAS, 112th Congress

Sen. Casey, Robert P., Jr. [D-PA

2011-12-05

Senate - 12/08/2011 Motion to proceed to consideration of measure, under the order of 12/8/2011, not having achieved the required 60 votes in the affirmative, was rejected in Senate by Yea-Nay Vote. 50 - 48. Record Vote Number: 224. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Long-Term Surface Transportation Extension Act of 2011

THOMAS, 112th Congress

Sen. Hatch, Orrin G. [R-UT

2011-11-02

Senate - 11/03/2011 Motion to proceed to consideration of measure under the order of 11/2/2011, not having achieved 60 votes in the affirmative, was rejected in Senate by Yea-Nay Vote. 47 - 53. Record Vote Number: 196. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

A resolution to improve procedures for the consideration of legislation and nominations in the Senate.

THOMAS, 113th Congress

Sen. Reid, Harry [D-NV

2013-01-24

Senate - 01/24/2013 Resolution agreed to in Senate, under the order of 1/24/2012, having achieved 60 votes in the affirmative, without amendment by Yea-Nay Vote. 78 - 16. Record Vote Number: 1. (All Actions) Tracker: This bill has the status Agreed to in SenateHere are the steps for Status of Legislation:

A resolution to permit the waiving of the reading of an amendment if the text and adequate notice are provided.

THOMAS, 112th Congress

Sen. Udall, Mark [D-CO

2011-01-27

Senate - 01/27/2011 Resolution agreed to in Senate, having achieved 60 votes in the affirmative, without amendment by Yea-Nay Vote. 81 - 15. Record Vote Number: 3. (All Actions) Tracker: This bill has the status Agreed to in SenateHere are the steps for Status of Legislation:

Middle Class Tax Cut Act

THOMAS, 112th Congress

Sen. Reid, Harry [D-NV

2012-07-19

Senate - 07/25/2012 Passed Senate without amendment by Yea-Nay Vote. 51 - 48. Record Vote Number: 184. (All Actions) Tracker: This bill has the status Passed SenateHere are the steps for Status of Legislation:

Paycheck Fairness Act

THOMAS, 113th Congress

Sen. Mikulski, Barbara A. [D-MD

2014-04-01

Senate - 09/15/2014 Cloture on the bill not invoked in Senate by Yea-Nay Vote. 52 - 40. Record Vote Number: 262. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

CSA2012

THOMAS, 112th Congress

Sen. Lieberman, Joseph I. [ID-CT

2012-07-19

Senate - 11/14/2012 Upon reconsideration, cloture on the bill not invoked in Senate by Yea-Nay Vote. 51 - 47. Record Vote Number: 202. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Bring Jobs Home Act

THOMAS, 113th Congress

Sen. Walsh, John E. [D-MT

2014-07-08

Senate - 07/30/2014 Cloture on the measure not invoked in Senate by Yea-Nay Vote. 54 - 42. Record Vote Number: 249. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

A resolution to establish as a standing order of the Senate that a Senator publicly disclose a notice of intent to objecting to any measure or matter.

THOMAS, 112th Congress

Sen. Wyden, Ron [D-OR

2011-01-27

Senate - 01/27/2011 Resolution agreed to in Senate, having achieved 60 votes in the affirmative, without amendment by Yea-Nay Vote. 92 - 4. Record Vote Number: 2. (All Actions) Tracker: This bill has the status Agreed to in SenateHere are the steps for Status of Legislation:

75 FR 57295 - Record of Vote of Meeting Closure (Pub. L. 94-409) (5 U.S.C. Sec. 552b)

Federal Register 2010, 2011, 2012, 2013, 2014

2010-09-20

.... 94-409) (5 U.S.C. Sec. 552b) I, Isaac Fulwood, of the United States Parole Commission, was present at... Commissioners voted that the meeting be closed: Isaac Fulwood, Cranston J. Mitchell and Patricia K. Cushwa. In... record to be made available to the public. Dated: September 10, 2010. Isaac Fulwood, Chairman, U.S...

Violence Against Women Reauthorization Act of 2012

THOMAS, 112th Congress

Sen. Leahy, Patrick J. [D-VT

2011-11-30

Senate - 04/26/2012 Passed Senate with an amendment by Yea-Nay Vote. 68 - 31. Record Vote Number: 87. (All Actions) Tracker: This bill has the status Passed SenateHere are the steps for Status of Legislation:

Economic Development Revitalization Act of 2011

THOMAS, 112th Congress

Sen. Boxer, Barbara [D-CA

2011-04-08

Senate - 06/21/2011 Cloture on the bill not invoked in Senate by Yea-Nay Vote. 49 - 51. Record Vote Number: 94. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

76 FR 65750 - Sunshine Act Meeting; Record of Vote of Meeting Closure

Federal Register 2010, 2011, 2012, 2013, 2014

2011-10-24

... Commission, which started at approximately 11 a.m., on Thursday, September 8, 2011, at the U.S. Parole... any other business. Upon motion duly made, seconded, and carried, the following Commissioners voted...

Bipartisan Sportsmen's Act of 2014

THOMAS, 113th Congress

Sen. Hagan, Kay R. [D-NC

2014-05-20

Senate - 07/10/2014 Cloture on the bill not invoked in Senate by Yea-Nay Vote. 41 - 56. Record Vote Number: 220. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Repeal Big Oil Tax Subsidies Act

THOMAS, 112th Congress

Sen. Menendez, Robert [D-NJ

2012-03-19

Senate - 03/29/2012 Cloture on the measure not invoked in Senate by Yea-Nay Vote. 51 - 47. Record Vote Number: 63. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Paycheck Fairness Act

THOMAS, 111th Congress

Sen. Reid, Harry [D-NV

2010-09-13

Senate - 11/17/2010 Cloture on the motion to proceed to the bill not invoked in Senate by Yea-Nay Vote. 58 - 41. Record Vote Number: 249. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Student Loan Affordability Act

THOMAS, 113th Congress

Sen. Reed, Jack [D-RI

2013-05-14

Senate - 06/06/2013 Cloture on the motion to proceed to measure not invoked in Senate by Yea-Nay Vote. 51 - 46. Record Vote Number: 143. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

77 FR 31042 - Sunshine Act Meetings; Record of Vote of Meeting Closure; (Pub. L. 94-409) (5 U.S.C. 552b)

Federal Register 2010, 2011, 2012, 2013, 2014

2012-05-24

...; (Pub. L. 94-409) (5 U.S.C. 552b) I, Isaac Fulwood, Chairman of the United States Parole Commission, was... carried, the following Commissioners voted that the meeting should be closed: Isaac Fulwood, Cranston J... the meeting and authorize this record to be made available to the public. Dated: May 21, 2012. Isaac...

USA FREEDOM Act of 2014

THOMAS, 113th Congress

Sen. Leahy, Patrick J. [D-VT

2014-07-29

Senate - 11/18/2014 Cloture on the motion to proceed to the measure not invoked in Senate by Yea-Nay Vote. 58 - 42. Record Vote Number: 282. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Comprehensive Student Loan Protection Act

THOMAS, 113th Congress

Sen. Coburn, Tom [R-OK

2013-05-21

Senate - 06/06/2013 Cloture on the motion to proceed to measure not invoked in Senate by Yea-Nay Vote. 40 - 57. Record Vote Number: 142. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Bring Jobs Home Act

THOMAS, 112th Congress

Sen. Stabenow, Debbie [D-MI

2012-07-09

Senate - 07/19/2012 Cloture on the motion to proceed to the measure not invoked in Senate by Yea-Nay Vote. 56 - 42. Record Vote Number: 181. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Inferring climate variability from skewed proxy records

NASA Astrophysics Data System (ADS)

Emile-Geay, J.; Tingley, M.

2013-12-01

Many paleoclimate analyses assume a linear relationship between the proxy and the target climate variable, and that both the climate quantity and the errors follow normal distributions. An ever-increasing number of proxy records, however, are better modeled using distributions that are heavy-tailed, skewed, or otherwise non-normal, on account of the proxies reflecting non-normally distributed climate variables, or having non-linear relationships with a normally distributed climate variable. The analysis of such proxies requires a different set of tools, and this work serves as a cautionary tale on the danger of making conclusions about the underlying climate from applications of classic statistical procedures to heavily skewed proxy records. Inspired by runoff proxies, we consider an idealized proxy characterized by a nonlinear, thresholded relationship with climate, and describe three approaches to using such a record to infer past climate: (i) applying standard methods commonly used in the paleoclimate literature, without considering the non-linearities inherent to the proxy record; (ii) applying a power transform prior to using these standard methods; (iii) constructing a Bayesian model to invert the mechanistic relationship between the climate and the proxy. We find that neglecting the skewness in the proxy leads to erroneous conclusions and often exaggerates changes in climate variability between different time intervals. In contrast, an explicit treatment of the skewness, using either power transforms or a Bayesian inversion of the mechanistic model for the proxy, yields significantly better estimates of past climate variations. We apply these insights in two paleoclimate settings: (1) a classical sedimentary record from Laguna Pallcacocha, Ecuador (Moy et al., 2002). Our results agree with the qualitative aspects of previous analyses of this record, but quantitative departures are evident and hold implications for how such records are interpreted, and compared to other proxy records. (2) a multiproxy reconstruction of temperature over the Common Era (Mann et al., 2009), where we find that about one third of the records display significant departures from normality. Accordingly, accounting for skewness in proxy predictors has a notable influence on both reconstructed global mean and spatial patterns of temperature change. Inferring climate variability from skewed proxy records thus requires cares, but can be done with relatively simple tools. References - Mann, M. E., Z. Zhang, S. Rutherford, R. S. Bradley, M. K. Hughes, D. Shindell, C. Ammann, G. Faluvegi, and F. Ni (2009), Global signatures and dynamical origins of the little ice age and medieval climate anomaly, Science, 326(5957), 1256-1260, doi:10.1126/science.1177303. - Moy, C., G. Seltzer, D. Rodbell, and D. Anderson (2002), Variability of El Niño/Southern Oscillation activ- ity at millennial timescales during the Holocene epoch, Nature, 420(6912), 162-165.

Bribery or just desserts? Evidence on the influence of Congressional reproductive policy voting patterns on PAC contributions from exogenous variation in the sex mix of legislator offspring.

PubMed

Conley, Dalton; McCabe, Brian J

2012-01-01

Evidence on the relationship between political contributions and legislators' voting behavior is marred by concerns about endogeneity in the estimation process. Using a legislator's offspring sex mix as a truly exogenous variable, we employ an instrumental variable estimation procedure to predict the effect of voting behavior on political contributions. Following previous research, we find that a legislator's proportion daughters has a significant effect on voting behavior for women's issues, as measured by score in the "Congressional Record on Choice" issued by NARAL Pro-Choice America. In the second stage, we make a unique contribution by demonstrating a significant impact of exogenous voting behavior on PAC contributions, lending further credibility to the hypothesis that Political Action Committees respond to legislators' voting patterns by "rewarding" political candidates that vote in line with the positions of the PAC, rather than affecting those same votes - at least in this high-profile policy domain. Copyright © 2011 Elsevier Inc. All rights reserved.

Joint resolution proposing a balanced budget amendment to the Constitution of the United States.

THOMAS, 112th Congress

Sen. Hatch, Orrin G. [R-UT

2011-03-31

Senate - 12/14/2011 Failed of passage in Senate by Yea-Nay Vote. 47 - 53. Record Vote Number: 229. (All Actions) Tracker: This bill has the status Failed SenateHere are the steps for Status of Legislation:

Emergency Senior Citizens Relief Act of 2010

THOMAS, 111th Congress

Sen. Sanders, Bernard [I-VT

2010-11-29

Senate - 12/08/2010 Cloture on the motion to proceed to the bill not invoked in Senate by Yea-Nay Vote. 53 - 45. Record Vote Number: 267. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Joint resolution proposing a balanced budget amendment to the Constitution of the United States.

THOMAS, 112th Congress

Sen. Udall, Mark [D-CO

2011-08-02

Senate - 12/14/2011 Failed of passage in Senate by Yea-Nay Vote. 21 - 79. Record Vote Number: 228. (All Actions) Tracker: This bill has the status Failed SenateHere are the steps for Status of Legislation:

Withholding Tax Relief Act of 2011

THOMAS, 112th Congress

Sen. McConnell, Mitch [R-KY

2011-10-17

Senate - 10/20/2011 Cloture on the motion to proceed to the bill not invoked in Senate by Yea-Nay Vote. 57 - 43. Record Vote Number: 178. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Medicare Physician Fairness Act of 2009

THOMAS, 111th Congress

Sen. Stabenow, Debbie [D-MI

2009-10-13

Senate - 10/21/2009 Cloture on the motion to proceed to the bill not invoked in Senate by Yea-Nay Vote. 47 - 53. Record Vote Number: 325. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Creating American Jobs and Ending Offshoring Act

THOMAS, 111th Congress

Sen. Durbin, Richard J. [D-IL

2010-09-21

Senate - 09/28/2010 Cloture on the motion to proceed to the bill not invoked in Senate by Yea-Nay Vote. 53 - 45. Record Vote Number: 242. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Emergency Unemployment Compensation Extension Act

THOMAS, 113th Congress

Sen. Reed, Jack [D-RI

2013-12-17

Senate - 02/06/2014 Motion by Senator Reid to reconsider the vote by which second cloture was not invoked on the bill (Record Vote No. 24) made in Senate. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Paying a Fair Share Act of 2012

THOMAS, 112th Congress

Sen. Whitehouse, Sheldon [D-RI

2012-03-22

Senate - 04/16/2012 Cloture on the motion to proceed to the measure not invoked in Senate by Yea-Nay Vote. 51 - 45. Record Vote Number: 65. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Public Safety Employer-Employee Cooperation Act of 2010

THOMAS, 111th Congress

Sen. Reid, Harry [D-NV

2010-11-30

Senate - 12/08/2010 Cloture on the motion to proceed to the bill not invoked in Senate by Yea-Nay Vote. 55 - 43. Record Vote Number: 266. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Energy Savings and Industrial Competitiveness Act of 2014

THOMAS, 113th Congress

Sen. Shaheen, Jeanne [D-NH

2014-04-28

Senate - 05/12/2014 Motion by Senator Reid to reconsider the vote by which cloture was not invoked on the measure (Record Vote No. 142) entered in Senate. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Cut, Cap, and Balance Act of 2011

THOMAS, 112th Congress

Rep. Chaffetz, Jason [R-UT-3

2011-07-15

Senate - 07/22/2011 Motion to table the motion to proceed to the bill agreed to in Senate by Yea-Nay Vote. 51 - 46. Record Vote Number: 116. (All Actions) Tracker: This bill has the status Passed HouseHere are the steps for Status of Legislation:

Removal Clarification Act of 2010

THOMAS, 111th Congress

Rep. Johnson, Henry C. "Hank," Jr. [D-GA-4

2010-05-12

Senate - 12/18/2010 Cloture on the motion to agree to House amendment to Senate amendment numbered 3 not invoked in Senate by Yea-Nay Vote. 55 - 41. Record Vote Number: 278. (All Actions) Tracker: This bill has the status Resolving DifferencesHere are the steps for Status of Legislation:

Minimum Wage Fairness Act

THOMAS, 113th Congress

Sen. Harkin, Tom [D-IA

2014-04-08

Senate - 04/30/2014 Motion by Senator Reid to reconsider the vote by which cloture was not invoked on the motion to proceed to the measure (Record Vote No. 117) entered in Senate. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

A joint resolution relating to the disapproval of obligations under the Emergency Economic Stabilization Act of 2008.

THOMAS, 111th Congress

Sen. Vitter, David [R-LA

2009-01-13

Senate - 01/15/2009 Failed of passage in Senate by Yea-Nay Vote. 42 - 52. Record Vote Number: 5. (All Actions) Tracker: This bill has the status Failed SenateHere are the steps for Status of Legislation:

Teachers and First Responders Back to Work Act of 2011

THOMAS, 112th Congress

Sen. Menendez, Robert [D-NJ

2011-10-17

Senate - 10/20/2011 Cloture on the motion to proceed to the bill not invoked in Senate by Yea-Nay Vote. 50 - 50. Record Vote Number: 177. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Potential for tree rings to reveal spatial patterns of past drought variability across western Australia

NASA Astrophysics Data System (ADS)

O'Donnell, Alison J.; Cook, Edward R.; Palmer, Jonathan G.; Turney, Chris S. M.; Grierson, Pauline F.

2018-02-01

Proxy records have provided major insights into the variability of past climates over long timescales. However, for much of the Southern Hemisphere, the ability to identify spatial patterns of past climatic variability is constrained by the sparse distribution of proxy records. This is particularly true for mainland Australia, where relatively few proxy records are located. Here, we (1) assess the potential to use existing proxy records in the Australasian region—starting with the only two multi-century tree-ring proxies from mainland Australia—to reveal spatial patterns of past hydroclimatic variability across the western third of the continent, and (2) identify strategic locations to target for the development of new proxy records. We show that the two existing tree-ring records allow robust reconstructions of past hydroclimatic variability over spatially broad areas (i.e. > 3° × 3°) in inland north- and south-western Australia. Our results reveal synchronous periods of drought and wet conditions between the inland northern and southern regions of western Australia as well as a generally anti-phase relationship with hydroclimate in eastern Australia over the last two centuries. The inclusion of 174 tree-ring proxy records from Tasmania, New Zealand and Indonesia and a coral record from Queensland did not improve the reconstruction potential over western Australia. However, our findings suggest that the addition of relatively few new proxy records from key locations in western Australia that currently have low reconstruction skill will enable the development of a comprehensive drought atlas for the region, and provide a critical link to the drought atlases of monsoonal Asia and eastern Australia and New Zealand.

Water Isotope Proxy-Proxy and Proxy-Model Convergence for Late Pleistocene East Asian Monsoon Rainfall Reconstructions

NASA Astrophysics Data System (ADS)

Clemens, S. C.; Holbourn, A.; Kubota, Y.; Lee, K. E.; Liu, Z.; Chen, G.

2017-12-01

Confidence in reconstruction of East Asian paleomonsoon rainfall using precipitation isotope proxies is a matter of considerable debate, largely due to the lack of correlation between precipitation amount and isotopic composition in the present climate. We present four new, very highly resolved records spanning the past 300,000 years ( 200 year sample spacing) from IODP Site U1429 in the East China Sea. We demonstrate that all the orbital- and millennial-scale variance in the onshore Yangtze River Valley speleothem δ18O record1 is also embedded in the offshore Site U1429 seawater δ18O record (derived from the planktonic foraminifer Globigerinoides ruber and sea surface temperature reconstructions). Signal replication in these two independent terrestrial and marine archives, both controlled by the same monsoon system, uniquely identifies δ18O of precipitation as the primary driver of the precession-band variance in both records. This proxy-proxy convergence also eliminates a wide array of other drivers that have been called upon as potential contaminants to the precipitation δ18O signal recorded by these proxies. We compare East Asian precipitation isotope proxy records to precipitation amount from a CCSM3 transient climate model simulation of the past 300,000 years using realistic insolation, ice volume, greenhouse gasses, and sea level boundary conditions. This model-proxy comparison suggests that both Yangtze River Valley precipitation isotope proxies (seawater and speleothem δ18O) track changes in summer-monsoon rainfall amount at orbital time scales, as do precipitation isotope records from the Pearl River Valley2 (leaf wax δ2H) and Borneo3 (speleothem δ18O). Notably, these proxy records all have significantly different spectral structure indicating strongly regional rainfall patterns that are also consistent with model results. Transient, isotope-enabled model simulations will be necessary to more thoroughly evaluate these promising results, and to evaluate potentially distinct regional mechanisms linking rainfall amount to precipitation isotopes at orbital and millennial time scales in other monsoon regions. 1 Cheng et al., 10.1038/nature18591 2 Thomas et al., 10.1130/G36289.1 3 Carolin et al., 10.1016/j.epsl.2016.01.028

American Family Economic Protection Act of 2013

THOMAS, 113th Congress

Sen. Mikulski, Barbara A. [D-MD

2013-02-26

Senate - 02/28/2013 Motion by Senator Reid to reconsider the vote by which cloture was not invoked on the motion to proceed to the measure (Record Vote No. 27) entered in Senate. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Democracy is Strengthened by Casting Light on Spending in Elections Act

THOMAS, 111th Congress

Sen. Schumer, Charles E. [D-NY

2010-07-21

Senate - 09/23/2010 Upon reconsideration, cloture on the motion to proceed to the bill (S.3628) not invoked in Senate by Yea-Nay Vote. 59 - 39. Record Vote Number: 240. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Protect Women's Health From Corporate Interference Act of 2014

THOMAS, 113th Congress

Sen. Murray, Patty [D-WA

2014-07-09

Senate - 07/16/2014 Motion by Senator Reid to reconsider the vote by which cloture was not invoked on the motion to proceed to the measure (Record Vote No. 228) entered in Senate. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Brain indices of disagreement with one’s social values predict EU referendum voting behavior

PubMed Central

Sirota, Miroslav; Materassi, Maurizio; Zaninotto, Francesca; Terry, Philip

2017-01-01

Abstract Pre-electoral surveys typically attempt, and sometimes fail, to predict voting behavior on the basis of explicit measures of agreement or disagreement with a candidate or political position. Here, we assessed whether a specific brain signature of disagreement with one’s social values, the event-related potential component N400, could be predictive of voting behavior. We examined this possibility in the context of the EU referendum in the UK. In the 5 weeks preceding the referendum, we recorded the N400 while participants with different vote intentions expressed their agreement or disagreement with pro- and against-EU statements. We showed that the N400 responded to statements incongruent with one’s view regarding the EU. Crucially, this effect predicted actual voting behavior in decided as well as undecided voters. The N400 was a better predictor of voting choice than an explicit index of preference based on the behavioral responses. Our findings demonstrate that well-defined patterns of brain activity can forecast future voting behavior. PMID:28981799

A resolution honoring the victims and heroes of the shooting on January 8, 2011 in Tucson, Arizona.

THOMAS, 112th Congress

Sen. McCain, John [R-AZ

2011-01-25

Senate - 01/26/2011 Resolution agreed to in Senate without amendment and with a preamble by Yea-Nay Vote. 97 - 0. Record Vote Number: 1. (All Actions) Tracker: This bill has the status Agreed to in SenateHere are the steps for Status of Legislation:

FDA Food Safety Modernization Act

THOMAS, 111th Congress

Sen. Durbin, Richard J. [D-IL

2009-03-03

Senate - 11/30/2010 Passed Senate with an amendment by Yea-Nay Vote. 73 - 25. Record Vote Number: 257. (All Actions) Notes: For further action, see H.R.2751, which became Public Law 111-353 on 1/4/2011. Tracker: This bill has the status Passed SenateHere are the steps for Status of Legislation:

A joint resolution disapproving the rule submitted by the Federal Communications Commission with respect to regulating the Internet and broadband industry practices.

THOMAS, 112th Congress

Sen. Hutchison, Kay Bailey [R-TX

2011-02-16

Senate - 11/10/2011 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 46 - 52. Record Vote Number: 200. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

A joint resolution proposing an amendment to the Constitution of the United States relating to contributions and expenditures intended to affect elections.

THOMAS, 113th Congress

Sen. Udall, Tom [D-NM

2013-06-18

Senate - 09/11/2014 Cloture on the joint resolution not invoked in Senate by Yea-Nay Vote. 54 - 42. Record Vote Number: 261. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

A complete representation of uncertainties in layer-counted paleoclimatic archives

NASA Astrophysics Data System (ADS)

Boers, Niklas; Goswami, Bedartha; Ghil, Michael

2017-09-01

Accurate time series representation of paleoclimatic proxy records is challenging because such records involve dating errors in addition to proxy measurement errors. Rigorous attention is rarely given to age uncertainties in paleoclimatic research, although the latter can severely bias the results of proxy record analysis. Here, we introduce a Bayesian approach to represent layer-counted proxy records - such as ice cores, sediments, corals, or tree rings - as sequences of probability distributions on absolute, error-free time axes. The method accounts for both proxy measurement errors and uncertainties arising from layer-counting-based dating of the records. An application to oxygen isotope ratios from the North Greenland Ice Core Project (NGRIP) record reveals that the counting errors, although seemingly small, lead to substantial uncertainties in the final representation of the oxygen isotope ratios. In particular, for the older parts of the NGRIP record, our results show that the total uncertainty originating from dating errors has been seriously underestimated. Our method is next applied to deriving the overall uncertainties of the Suigetsu radiocarbon comparison curve, which was recently obtained from varved sediment cores at Lake Suigetsu, Japan. This curve provides the only terrestrial radiocarbon comparison for the time interval 12.5-52.8 kyr BP. The uncertainties derived here can be readily employed to obtain complete error estimates for arbitrary radiometrically dated proxy records of this recent part of the last glacial interval.

15 CFR 27.115 - IRB records.

Code of Federal Regulations, 2010 CFR

2010-01-01

... in sufficient detail to show attendance at the meetings; actions taken by the IRB; the vote on these...)(5). (b) The records required by this policy shall be retained for at least 3 years, and records...

Sensitivity of Pliocene Arctic climate to orbital forcing, atmospheric CO2 and sea ice albedo parameterisation

USGS Publications Warehouse

Howell, Fergus W.; Haywood, Alan M.; Dowsett, Harry J.; Pickering, Steven J.

2016-01-01

With varying CO2, orbit and sea ice albedo values we are able to reproduce proxy temperature records that lean towards modest levels of high latitude warming, but other proxy data showing greater warming remain beyond the reach of our model. This highlights the importance of additional proxy records at high latitudes and ongoing efforts to compare proxy signals between sites.

75 FR 71147 - Record of Vote of Meeting Closure

Federal Register 2010, 2011, 2012, 2013, 2014

2010-11-22

.... 94-409) (5 U.S.C. Sec. 552b) I, Isaac Fulwood, of the United States Parole Commission, was present at... following Commissioners voted that the meeting be closed: Isaac Fulwood, Cranston J. Mitchell and Patricia K..., 2010. Isaac Fuiwood, Chairman, U.S. Parole Commission. [FR Doc. 2010-29354 Filed 11-19-10; 8:45 am...

Continuing Extension Act of 2010

THOMAS, 111th Congress

Sen. Grassley, Chuck [R-IA

2010-03-23

Senate - 03/25/2010 Motion to proceed to consideration of measure tabled in Senate by Yea-Nay Vote. 59 - 40. Record Vote Number: 106. (All Actions) Notes: For further action, see H.R.4851, which became Public Law 111-157 on 4/15/2010. Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

A joint resolution to disapprove a rule promulgated by the Administrator of the Environmental Protection Agency relating to emission standards for certain steam generating units.

THOMAS, 112th Congress

Sen. Inhofe, James M. [R-OK

2012-02-16

Senate - 06/20/2012 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 46 - 53. Record Vote Number: 139. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

A First Look at Sandra Day O'Connor and the First Amendment.

ERIC Educational Resources Information Center

Schwartz, Thomas A.

First Amendment students were unhappy to see Supreme Court Justice Potter Stewart retire because his voting record demonstrated a favorable attitude toward freedom of speech and press. His replacement, Sandra Day O'Connor, was predicted to be a conservative or moderate who probably would vote consistently with Stewart in other areas, but her…

PATRIOT Sunsets Extension Act of 2011

THOMAS, 112th Congress

Sen. Reid, Harry [D-NV

2011-05-19

Senate - 05/24/2011 Motion to proceed to consideration of measure tabled in Senate by Yea-Nay Vote. 74 - 13. Record Vote Number: 76. (All Actions) Notes: For further action, see H.R.514, which became Public Law 112-3 on 2/25/2011. Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Middle Class Tax Cut Act of 2011

THOMAS, 112th Congress

Sen. Casey, Robert P., Jr. [D-PA

2011-11-28

Senate - 12/01/2011 Motion to proceed to consideration of measure, under the order of 12/1/2011, not having achieved the required 60 votes in the affirmative, was rejected in Senate by Yea-Nay. 51 - 49. Record Vote Number: 219. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

A joint resolution disapproving a rule submitted by the Environmental Protection Agency relating to the mitigation by States of cross-border air pollution under the Clean Air Act.

THOMAS, 112th Congress

Sen. Paul, Rand [R-KY

2011-09-08

Senate - 11/10/2011 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 41 - 56. Record Vote Number: 201. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Establishing the budget for the United States Government for fiscal year 2012 and setting forth appropriate budgetary levels for fiscal years 2013 through 2021.

THOMAS, 112th Congress

Rep. Ryan, Paul [R-WI-1

2011-04-11

Senate - 05/25/2011 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 40 - 57. Record Vote Number: 77. (All Actions) Tracker: This bill has the status Agreed to in HouseHere are the steps for Status of Legislation:

A joint resolution providing for congressional disapproval under chapter 8 of title 5, United States Code, of the rule submitted by the National Mediation Board relating to representation election procedures.

THOMAS, 111th Congress

Sen. Isakson, Johnny [R-GA

2010-05-11

Senate - 09/23/2010 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 43 - 56. Record Vote Number: 239. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Establishing the budget for the United States Government for fiscal year 2013 and setting forth appropriate budgetary levels for fiscal years 2014 through 2022.

THOMAS, 112th Congress

Rep. Ryan, Paul [R-WI-1

2012-03-23

Senate - 05/16/2012 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 41 - 58. Record Vote Number: 98. (All Actions) Tracker: This bill has the status Agreed to in HouseHere are the steps for Status of Legislation:

Transportation, Housing and Urban Development, and Related Agencies Appropriations Act, 2014

THOMAS, 113th Congress

Sen. Murray, Patty [D-WA

2013-06-27

Senate - 08/01/2013 Cloture on the measure not invoked in Senate by Yea-Nay Vote. 54 - 43. Record Vote Number: 199. (All Actions) Notes: For further action, see H.R.3547, which became Public Law 113-76 on 1/17/2014. Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

A concurrent resolution setting forth the congressional budget for the United States Government for fiscal year 2012 and setting forth the appropriate budgetary levels for fiscal years 2013 through 2021.

THOMAS, 112th Congress

Sen. Toomey, Pat [R-PA

2011-05-23

Senate - 05/25/2011 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 42 - 55. Record Vote Number: 79. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

A concurrent resolution setting forth the congressional budget for the United States Government for fiscal year 2013 and setting forth the appropriate budgetary levels for fiscal years 2014 through 2022.

THOMAS, 112th Congress

Sen. Lee, Mike [R-UT

2012-05-08

Senate - 05/16/2012 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 17 - 82. Record Vote Number: 101. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

A concurrent resolution setting forth the congressional budget for the United States Government for fiscal year 2012 and setting forth the appropriate budgetary levels for fiscal years 2013 through 2016.

THOMAS, 112th Congress

Sen. Paul, Rand [R-KY

2011-05-19

Senate - 05/25/2011 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 7 - 90. Record Vote Number: 80. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

A concurrent resolution setting forth the congressional budget for the United States Government for fiscal year 2013, and setting forth the appropriate budgetary levels for fiscal years 2014 through 2022.

THOMAS, 112th Congress

Sen. Toomey, Pat [R-PA

2012-03-29

Senate - 05/16/2012 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 42 - 57. Record Vote Number: 99. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Sophisticated approval voting, ignorance priors, and plurality heuristics: a behavioral social choice analysis in a Thurstonian framework.

PubMed

Regenwetter, Michel; Ho, Moon-Ho R; Tsetlin, Ilia

2007-10-01

This project reconciles historically distinct paradigms at the interface between individual and social choice theory, as well as between rational and behavioral decision theory. The authors combine a utility-maximizing prescriptive rule for sophisticated approval voting with the ignorance prior heuristic from behavioral decision research and two types of plurality heuristics to model approval voting behavior. When using a sincere plurality heuristic, voters simplify their decision process by voting for their single favorite candidate. When using a strategic plurality heuristic, voters strategically focus their attention on the 2 front-runners and vote for their preferred candidate among these 2. Using a hierarchy of Thurstonian random utility models, the authors implemented these different decision rules and tested them statistically on 7 real world approval voting elections. They cross-validated their key findings via a psychological Internet experiment. Although a substantial number of voters used the plurality heuristic in the real elections, they did so sincerely, not strategically. Moreover, even though Thurstonian models do not force such agreement, the results show, in contrast to common wisdom about social choice rules, that the sincere social orders by Condorcet, Borda, plurality, and approval voting are identical in all 7 elections and in the Internet experiment. PsycINFO Database Record (c) 2007 APA, all rights reserved.

Assessing the spatial representability of charcoal and PAH-based paleofire records with integrated GIS, modelling, and empirical approaches

NASA Astrophysics Data System (ADS)

Vachula, R. S.; Huang, Y.; Russell, J. M.

2017-12-01

Lake sediment-based fire reconstructions offer paleoenvironmental context in which to assess modern fires and predict future burning. However, despite the ubiquity, many uncertainties remain regarding the taphonomy of paleofire proxies and the spatial scales for which they record variations in fire history. Here we present down-core proxy analyses of polycyclic aromatic hydrocarbons (PAHs) and three size-fractions of charcoal (63-150, >150 and >250 μm) from Swamp Lake, California, an annually laminated lacustrine archive. Using a statewide historical GIS dataset of area burned, we assess the spatial scales for which these proxies are reliable recorders of fire history. We find that the coherence of observed and proxy-recorded fire history inherently depends upon spatial scale. Contrary to conventional thinking that charcoal mainly records local fires, our results indicate that macroscopic charcoal (>150 μm) may record spatially broader (<25 km) changes in fire history, and as such, the coarsest charcoal particles (>250 μm) may be a more conservative proxy for local burning. We find that sub-macroscopic charcoal particles (63-150 μm) reliably record regional (up to 150 km) changes in fire history. These results indicate that charcoal-based fire reconstructions may represent spatially broader fire history than previously thought, which has major implications for our understanding of spatiotemporal paleofire variations. Our analyses of PAHs show that dispersal mobility is heterogeneous between compounds, but that PAH fluxes are reliable proxies of fire history within 25-50 km, which suggests PAHs may be a better spatially constrained paleofire proxy than sedimentary charcoal. Further, using a linear discriminant analysis model informed by modern emissions analyses, we show that PAH assemblages preserved in lake sediments can differentiate vegetation type burned, and are thus promising paleoecological biomarkers warranting further research and implementation. In sum, our analyses offer new insight into the spatial dimensions of paleofire proxies and constitute a methodology that can be applied to other locations and proxies to better inform site-specific reconstructions.

Enduring Risk? Old Criminal Records and Predictions of Future Criminal Involvement

ERIC Educational Resources Information Center

Kurlychek, Megan C.; Brame, Robert; Bushway, Shawn D.

2007-01-01

It is well accepted that criminal records impose collateral consequences on offenders. Such records affect access to public housing, student financial aid, welfare benefits, and voting rights. An axiom of these policies is that individuals with criminal records--even old criminal records--exhibit significantly higher risk of future criminal…

A concurrent resolution setting forth the President's budget request for the United States Government for fiscal year 2012, and setting forth the appropriate budgetary levels for fiscal years 2013 through 2021.

THOMAS, 112th Congress

Sen. Sessions, Jeff [R-AL

2011-05-19

Senate - 05/25/2011 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 0 - 97. Record Vote Number: 78. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

A concurrent resolution setting forth the President's budget request for the United States Government for fiscal year 2013, and setting forth the appropriate budgetary levels for fiscal years 2014 through 2022.

THOMAS, 112th Congress

Sen. Sessions, Jeff [R-AL

2012-04-17

Senate - 05/16/2012 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 0 - 99. Record Vote Number: 97. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

A joint resolution relating to the disapproval of the President's exercise of authority to suspend the debt limit, as submitted under section 1002(b) of the Continuing Appropriations Act, 2014 on October 17, 2013.

THOMAS, 113th Congress

Sen. McConnell, Mitch [R-KY

2013-10-28

Senate - 10/29/2013 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 45 - 54. Record Vote Number: 220. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

76 FR 13661 - Record of Vote of Meeting Closure; (Pub. L. 94-409) (5 U.S.C. 552b)

Federal Register 2010, 2011, 2012, 2013, 2014

2011-03-14

.... 94-409) (5 U.S.C. 552b) I, Isaac Fulwood, of the United States Parole Commission, was present at a... carried, the following Commissioners voted that the meeting be closed: Isaac Fulwood, Cranston J. Mitchell...: February 18, 2011. Isaac Fulwood, Chairman, U.S. Parole Commission. [FR Doc. 2011-5590 Filed 3-11-11; 8:45...

Providing for consideration of the bill (H.R. 2997) making appropriations for Agriculture, Rural Development, Food and Drug Administration, and Related Agencies programs for the fiscal year ending September 30, 2010, and for other purposes.

THOMAS, 111th Congress

Rep. McGovern, James P. [D-MA-3

2009-07-07

House - 07/08/2009 On motion to reconsider the vote Failed by recorded vote: 170 - 254 (Roll no. 494). (All Actions) Tracker: This bill has the status Agreed to in HouseHere are the steps for Status of Legislation:

A joint resolution providing for congressional disapproval under chapter 8 of title 5, United States Code, of the rule submitted by the National Labor Relations Board relating to representation election procedures.

THOMAS, 112th Congress

Sen. Enzi, Michael B. [R-WY

2012-02-16

Senate - 04/24/2012 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 45 - 54. Record Vote Number: 68. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

A joint resolution relating to the disapproval of the President's exercise of authority to increase the debt limit, as submitted under section 3101A of title 31, United States Code, on August 2, 2011.

THOMAS, 112th Congress

Sen. McConnell, Mitch [R-KY

2011-09-06

Senate - 09/08/2011 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 45 - 52. Record Vote Number: 130. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

A resolution strongly supporting the full implementation of United States and international sanctions on Iran and urging the President to continue to strengthen enforcement of sanctions legislation.

THOMAS, 113th Congress

Sen. Graham, Lindsey [R-SC

2013-02-28

Senate - 05/22/2013 Resolution agreed to in Senate with an amendment and with a preamble by Yea-Nay Vote. 99 - 0. Record Vote Number: 133. (All Actions) Tracker: This bill has the status Agreed to in SenateHere are the steps for Status of Legislation:

The Last Millennium Reanalysis: Improvements to proxies and proxy modeling

NASA Astrophysics Data System (ADS)

Tardif, R.; Hakim, G. J.; Emile-Geay, J.; Noone, D.; Anderson, D. M.

2017-12-01

The Last Millennium Reanalysis (LMR) employs a paleoclimate data assimilation (PDA) approach to produce climate field reconstructions (CFRs). Here, we focus on two key factors in PDA generated CFRs: the set of assimilated proxy records and forward models (FMs) used to estimate proxies from climate model output. In the initial configuration of the LMR [Hakim et al., 2016], the proxy dataset of [PAGES2k Consortium, 2013] was used, along with univariate linear FMs calibrated against annually-averaged 20th century temperature datasets. In an updated configuration, proxy records from the recent dataset [PAGES2k Consortium, 2017] are used, while a hierarchy of statistical FMs are tested: (1) univariate calibrated on annual temperature as in the initial configuration, (2) univariate against temperature as in (1) but calibration performed using expert-derived seasonality for individual proxy records, (3) as in (2) but expert proxy seasonality replaced by seasonal averaging determined objectively as part of the calibration process, (4) linear objective seasonal FMs as in (3) but objectively selecting relationships calibrated either on temperature or precipitation, and (5) bivariate linear models calibrated on temperature and precipitation with objectively-derived seasonality. (4) and (5) specifically aim at better representing the physical drivers of tree ring width proxies. Reconstructions generated using the CCSM4 Last Millennium simulation as an uninformed prior are evaluated against various 20th century data products. Results show the benefits of using the new proxy collection, particularly on the detrended global mean temperature and spatial patterns. The positive impact of using proper seasonality and temperature/moisture sensitivities for tree ring width records is also notable. This updated configuration will be used for the first generation of LMR-generated CFRs to be publicly released. These also provide a benchmark for future efforts aimed at evaluating the impact of additional proxy records and/or more sophisticated physically-based forward models. References: Hakim, G. J., and co-authors (2016), J. Geophys. Res. Atmos., doi:10.1002/2016JD024751 PAGES2K Consortium (2013), Nat. Geosci., doi:10.1038/ngeo1797 PAGES2k Consortium (2017), Sci. Data. doi:10.1038/sdata.2017.88

Neurodynamics of an election.

PubMed

da Rocha, Armando Freitas; Rocha, Fábio Theoto; Burattini, Marcelo Nascimento; Massad, Eduardo

2010-09-10

Variables influencing decision-making in real settings, as in the case of voting decisions, are uncontrollable and in many times even unknown to the experimenter. In this case, the experimenter has to study the intention to decide (vote) as close as possible in time to the moment of the real decision (election day). Here, we investigated the brain activity associated with the voting intention declared 1 week before the election day of the Brazilian Firearms Control Referendum about prohibiting the commerce of firearms. Two alliances arose in the Congress to run the campaigns for YES (for the prohibition of firearm commerce) and NO (against the prohibition of firearm commerce) voting. Time constraints imposed by the necessity of studying a reasonable number (here, 32) of voters during a very short time (5 days) made the EEG the tool of choice for recording the brain activity associated with voting decision. Recent fMRI and EEG studies have shown decision-making as a process due to the enrollment of defined neuronal networks. In this work, a special EEG technique is applied to study the topology of the voting decision-making networks and is compared to the results of standard ERP procedures. The results show that voting decision-making enrolled networks in charge of calculating the benefits and risks of the decision of prohibiting or allowing firearm commerce and that the topology of such networks was vote- (i.e., YES/NO-) sensitive. 2010 Elsevier B.V. All rights reserved.

22 CFR 225.115 - IRB records.

Code of Federal Regulations, 2010 CFR

2010-04-01

... attendance at the meetings; actions taken by the IRB; the vote on these actions including the number of... this policy shall be retained for at least 3 years, and records relating to research which is conducted...

7 CFR 1c.115 - IRB records.

Code of Federal Regulations, 2010 CFR

2010-01-01

... attendance at the meetings; actions taken by the IRB; the vote on these actions including the number of... policy shall be retained for at least 3 years, and records relating to research which is conducted shall...

Actions speak louder: a look at congressional votes on human life issues.

PubMed

Shannon, D; Mazpule, D

1991-01-01

The decision to bring a new life into the world is the most important decision a caring person can make. Many fundamental factors must be considered like: housing, income, food, clothing, etc. The terms pro-choice and pro-life are used to describe both sides of the abortion debate, a debate that is of critical importance when making that decision about new life. While most members of Congress who are pro-choice also support social programs that make raising children easier; most members who are pro-life do not support such social justice programs. It seems paradoxical that someone claiming to be pro-life would then be anti-social justice. To be truly pro-life, a person must not only support a woman's right to choose, but must also support programs and policies that help parents to raise healthy, happy, and productive children. Yet it is the very people who claim to be pro-life that fight equally as hard against choice and against social justice. They fight legal abortion, but they also fight legislation that would make abortion less necessary. This article includes charts of the voting records of all members of the 101st Congress on legislation supported by 7 pro-choice or pro-child organizations. Planned Parenthood Federation of America (PPFA), the Children's Defense Fund (CDF), the Leadership Conference on Civil Rights (LCCR), the National Women's Political Caucus (NWPC), the American Public Health Association (APHA) and the League of Conservation Voters (LCV). The CDF, LCCR, and LCV do not have positions on abortion rights. The voting record of the JustLife Educational Fund are also given. In comparing the voting records, those that supported PPFA at least 75% of the time were labeled pro-choice, those that supported PPFA less than 25% of the time were called anti-choice, and those that supported it 26-74% of the time were called mixed. Once this determination is made, a comparison of their voting records for the other organizations clearly confirm that those who are anti-choice are also against supporting human life.

Mount Logan ice core record of tropical and solar influences on Aleutian Low variability: 500-1998 A.D.

NASA Astrophysics Data System (ADS)

Osterberg, Erich C.; Mayewski, Paul A.; Fisher, David A.; Kreutz, Karl J.; Maasch, Kirk A.; Sneed, Sharon B.; Kelsey, Eric

2014-10-01

Continuous, high-resolution paleoclimate records from the North Pacific region spanning the past 1500 years are rare; and the behavior of the Aleutian Low (ALow) pressure center, the dominant climatological feature in the Gulf of Alaska, remains poorly constrained. Here we present a continuous, 1500 year long, calibrated proxy record for the strength of the wintertime (December-March) ALow from the Mount Logan summit (PR Col; 5200 m asl) ice core soluble sodium time series. We show that ice core sodium concentrations are statistically correlated with North Pacific sea level pressure and zonal wind speed. Our ALow proxy record reveals a weak ALow from circa 900-1300 A.D. and 1575-1675 A.D., and a comparatively stronger ALow from circa 500-900 A.D., 1300-1575 A.D., and 1675 A.D. to present. The Mount Logan ALow proxy record shows strong similarities with tropical paleoclimate proxy records sensitive to the El Niño-Southern Oscillation and is consistent with the hypothesis that the Medieval Climate Anomaly was characterized by more persistent La Niña-like conditions while the Little Ice Age was characterized by at least two intervals of more persistent El Niño-like conditions. The Mount Logan ALow proxy record is significantly (p < 0.05) correlated and coherent with solar irradiance proxy records over various time scales, with stronger solar irradiance generally associated with a weaker ALow and La Niña-like tropical conditions. However, a step-like increase in ALow strength during the Dalton solar minimum circa 1820 is associated with enhanced Walker circulation. Furthermore, rising CO2 forcing or internal variability may be masking the twentieth century rise in solar irradiance.

76 FR 81980 - Sunshine Act Meeting; Record of Vote of Meeting Closure (Pub. L. 94-409) (5 U.S.C. 552b)

Federal Register 2010, 2011, 2012, 2013, 2014

2011-12-29

... (Pub. L. 94-409) (5 U.S.C. 552b) I, Isaac Fulwood, of the United States Parole Commission, was present... following Commissioners voted that the meeting be closed: Isaac Fulwood, Cranston J. Mitchell, Patricia..., 2011. Isaac Fulwood, Chairman, U.S. Parole Commission. [FR Doc. 2011-33524 Filed 12-27-11; 4:15 pm...

A joint resolution disapproving a rule submitted by the Environmental Protection Agency relating to the endangerment finding and the cause or contribute findings for greenhouse gases under section 202(a) of the Clean Air Act.

THOMAS, 111th Congress

Sen. Murkowski, Lisa [R-AK

2010-01-21

Senate - 06/10/2010 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 47 - 53. Record Vote Number: 184. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Relating to the disapproval of the President's exercise of authority to increase the debt limit, as submitted under section 3101A of title 31, United States Code, on January 12, 2012.

THOMAS, 112th Congress

Rep. Reed, Tom [R-NY-29

2012-01-13

Senate - 01/26/2012 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 44 - 52. Record Vote Number: 2. (consideration: CR S95) (All Actions) Tracker: This bill has the status Passed HouseHere are the steps for Status of Legislation:

Reconstructing pre-instrumental streamflow in Eastern Australia using a water balance approach

NASA Astrophysics Data System (ADS)

Tozer, C. R.; Kiem, A. S.; Vance, T. R.; Roberts, J. L.; Curran, M. A. J.; Moy, A. D.

2018-03-01

Streamflow reconstructions based on paleoclimate proxies provide much longer records than the short instrumental period records on which water resource management plans are currently based. In Australia there is a lack of in-situ high resolution paleoclimate proxy records, but remote proxies with teleconnections to Australian climate have utility in producing streamflow reconstructions. Here we investigate, via a case study for a catchment in eastern Australia, the novel use of an Antarctic ice-core based rainfall reconstruction within a Budyko-framework to reconstruct ∼1000 years of annual streamflow. The resulting streamflow reconstruction captures interannual to decadal variability in the instrumental streamflow, validating both the use of the ice core rainfall proxy record and the Budyko-framework method. In the preinstrumental era the streamflow reconstruction shows longer wet and dry epochs and periods of streamflow variability that are higher than observed in the instrumental era. Importantly, for both the instrumental record and preinstrumental reconstructions, the wet (dry) epochs in the rainfall record are shorter (longer) in the streamflow record and this non-linearity must be considered when inferring hydroclimatic risk or historical water availability directly from rainfall proxy records alone. These insights provide a better understanding of present infrastructure vulnerability in the context of past climate variability for eastern Australia. The streamflow reconstruction presented here also provides a better understanding of the range of hydroclimatic variability possible, and therefore represents a more realistic baseline on which to quantify the potential impacts of anthropogenic climate change on water security.

SBIR/STTR Reauthorization Act of 2011

THOMAS, 112th Congress

Sen. Landrieu, Mary L. [D-LA

2011-03-04

Senate - 05/04/2011 Cloture on the bill (S. 493) not invoked in Senate by Yea-Nay Vote. 52 - 44. Record Vote Number: 64. (All Actions) Notes: On 11/29/2011, this bill was incorporated into S. 1867 as S. Amdt. 1115. For further action, see H.R.1540, which became Public Law 112-81 on 12/31/2011. Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

To amend title 49, United States Code, to modify the authority of the Assistant Secretary of Homeland Security (Transportation Security Administration) to issue regulations and security directives using emergency procedures.

THOMAS, 111th Congress

Rep. Mica, John L. [R-FL-7

2009-09-30

House - 10/06/2009 Provisions of measure incorporated into H.R. 2200 as an amendment during House consideration on and adopted by a recorded vote of 219 yeas and 211 noes (Roll Call Vote No. 304).. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

A concurrent resolution setting forth the congressional budget for the United States Government for fiscal year 2013, revising the appropriate budgetary levels for fiscal year 2012, and setting forth the appropriate budgetary levels for fiscal years 2013 through 2022.

THOMAS, 112th Congress

Sen. Paul, Rand [R-KY

2012-04-26

Senate - 05/16/2012 Motion to proceed to consideration of measure rejected in Senate by Yea-Nay Vote. 16 - 83. Record Vote Number: 100. (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

28 CFR 55.21 - Record keeping.

Code of Federal Regulations, 2011 CFR

2011-07-01

... Judicial Administration DEPARTMENT OF JUSTICE (CONTINUED) IMPLEMENTATION OF THE PROVISIONS OF THE VOTING RIGHTS ACT REGARDING LANGUAGE MINORITY GROUPS Minority Language Materials and Assistance § 55.21 Record keeping. The Attorney General's implementation of the Act's provisions concerning language minority groups...

28 CFR 55.21 - Record keeping.

Code of Federal Regulations, 2010 CFR

2010-07-01

... Judicial Administration DEPARTMENT OF JUSTICE (CONTINUED) IMPLEMENTATION OF THE PROVISIONS OF THE VOTING RIGHTS ACT REGARDING LANGUAGE MINORITY GROUPS Minority Language Materials and Assistance § 55.21 Record keeping. The Attorney General's implementation of the Act's provisions concerning language minority groups...

Proxy records of Holocene storm events in coastal barrier systems: Storm-wave induced markers

NASA Astrophysics Data System (ADS)

Goslin, Jérôme; Clemmensen, Lars B.

2017-10-01

Extreme storm events in the coastal zone are one of the main forcing agents of short-term coastal system behavior. As such, storms represent a major threat to human activities concentrated along the coasts worldwide. In order to better understand the frequency of extreme events like storms, climate science must rely on longer-time records than the century-scale records of instrumental weather data. Proxy records of storm-wave or storm-wind induced activity in coastal barrier systems deposits have been widely used worldwide in recent years to document past storm events during the last millennia. This review provides a detailed state-of-the-art compilation of the proxies available from coastal barrier systems to reconstruct Holocene storm chronologies (paleotempestology). The present paper aims (I) to describe the erosional and depositional processes caused by storm-wave action in barrier and back-barrier systems (i.e. beach ridges, storm scarps and washover deposits), (ii) to understand how storm records can be extracted from barrier and back-barrier sedimentary bodies using stratigraphical, sedimentological, micro-paleontological and geochemical proxies and (iii) to show how to obtain chronological control on past storm events recorded in the sedimentary successions. The challenges that paleotempestology studies still face in the reconstruction of representative and reliable storm-chronologies using these various proxies are discussed, and future research prospects are outlined.

Plio-Pleistocene Sea Surface Temperature Variability As Measured by Different Proxies - A Cautionary Tale

NASA Astrophysics Data System (ADS)

Lawrence, K. T.; Woodard, S. C.; Castañeda, I. S.; deMenocal, P. B.; Peterson, L.; Rosenthal, Y.; Bochner, L.; Gorbey, D. B.; Mauriello, H.

2016-12-01

Conflicting interpretations from the application of different sea surface temperature (SST) proxies seeking to characterize past climate conditions of the same region have given rise to a number of controversies about key elements of Pliocene climate. Thus, a detailed look at whether or not different temperature proxies yield consistent results is warranted. Here, we examine Pliocene climate variability at the orbital scale reporting new alkenone-derived SST estimates from ODP Site 1088 (South Atlantic) and ODP Site 846 (Eastern Equatorial Pacific). Using these novel datasets and previously published records from a variety of different sites in a variety of localities, we further examine the consistency of Plio-Pleistocene SST variability and orbital signatures from faunal, Mg/Ca, and TEX86 SST records relative to Uk'37 SST records. We find that many companion SST records produce very similar mean trends and standard deviations as well as absolute temperature estimates that are generally within error of each other. Our analysis also suggests that many companion records, with a few notable exceptions, capture the same dominant Milankovitch periodicities and produce phase estimates relative to benthic oxygen isotope estimates that are within error of each other. However, marked structural differences occur between different proxy records on glacial-interglacial timescales in Uk'37 versus Mg/Ca comparisons and some Uk'37 versus TEX86 comparisons. Therefore, the temperature estimates of individual glacial-interglacial cycles may vary significantly when a specific time slice is explored. Our preliminary investigation suggests that whether or not climate records derived from different paleothermometers yield consistent results depends on the timescale being explored and the study site, which reflects key factors such as seasonality, ecology, and diagenetic regime. Additional work that explores the underlying causes of the differences observed among proxies and uses a more systematic approach to directly compare the results from different paleothermometers is required. Until we have a better and broader sense of where/when proxies perform consistently, we recommend caution in treating SST records from different proxies as interchangeable.

Climatic variability during the last deglaciation: A stalagmite-based multi-proxy record from Mawmluh cave, India

NASA Astrophysics Data System (ADS)

Huguet, C.; Munnuru Singamshetty, K.; Routh, J.; Fietz, S.; Mangini, A.; Ghosh, P.; Lone, M. A.; Rangarajan, R.; Eliasson, J.

2016-12-01

The Mawmluh cave in northeastern India, is affected by global climate patterns displaying glacial-interglacial patterns and also the Indian Summer Monsoon (ISM). Precipitation from the ISM plays a vital role for the local community and thus, understanding the driving forces of ISM fluctuations became a recent focus of a number of paleoclimate studies. Here, we used the stalagmite KM-1 from Mawmluh cave to reconstruct climate variability during the last glacial-interglacial transition from 22 to 6 ka. For the first time, molecular proxy data (TEX86 and MBT/CBT derived from isoprenoid and branched GDGTs respectively) were coupled to stable isotope records (δ13C and δ18O) and compared to other speleothem records in Asia. ISM system abruptly transition between a suppressed and active state which is associated to changes in vegetation and thus shifts in δ13C. The abrupt δ13C shift observed in our record indicate changes to wetter climate in the Holocene, which are coupled to increase in abundance of GDGTs indicating higher production and/or transfer to KM-1. The TEX86-derived temperature roughly follows the glaciation-deglaciation cycle and Holocene changes. The TEX86 results show good correspondence with the δ18O records for temperature highlighting the potential for the use of molecular proxy in speleothem based climate reconstructions. While the MBT/CBT proxy is also defined as a temperature proxy it is not coupled with δ18O patterns, and thus shows no clear temperature signal. A decoupling between MBT/CBT from soils and the connected speleothems as well as a precipitation-moisture effect on this proxy have been previously reported. In this particular case the MBT/CBT seems to be better related to precipitation-monsoon changes, and thus warrant further exploration as a complementary proxy to isotope records for monsoon strength.

Proof-of-Concept Studies in Novel Guided Wave Methods for Metallic Structural Condition

DTIC Science & Technology

2009-03-01

stiffness tensor which is general can be complex (viscoelastic behavior). More details on the compatibility operator can be found in (Gopalakrishnan...structure was in when these AR coefficients were recorded is scored as the " vote " for the unknown condition using that particular input signal. This...signals that are imparted to the structure in its unknown state. The votes for each condition are then summed and the condition with the plurality of

32 CFR 1900.44 - Action by appeals authority.

Code of Federal Regulations, 2010 CFR

2010-07-01

... complete record of the request consisting of the request, the document(s) (sanitized and full text) at... Panel. (c) Decision by the Historical Records Policy Board. In any cases of divided vote by the ARP, any member of that body is authorized to refer the request to the CIA Historical Records Policy Board which...

Reconstruction of spatio-temporal temperature from sparse historical records using robust probabilistic principal component regression

USGS Publications Warehouse

Tipton, John; Hooten, Mevin B.; Goring, Simon

2017-01-01

Scientific records of temperature and precipitation have been kept for several hundred years, but for many areas, only a shorter record exists. To understand climate change, there is a need for rigorous statistical reconstructions of the paleoclimate using proxy data. Paleoclimate proxy data are often sparse, noisy, indirect measurements of the climate process of interest, making each proxy uniquely challenging to model statistically. We reconstruct spatially explicit temperature surfaces from sparse and noisy measurements recorded at historical United States military forts and other observer stations from 1820 to 1894. One common method for reconstructing the paleoclimate from proxy data is principal component regression (PCR). With PCR, one learns a statistical relationship between the paleoclimate proxy data and a set of climate observations that are used as patterns for potential reconstruction scenarios. We explore PCR in a Bayesian hierarchical framework, extending classical PCR in a variety of ways. First, we model the latent principal components probabilistically, accounting for measurement error in the observational data. Next, we extend our method to better accommodate outliers that occur in the proxy data. Finally, we explore alternatives to the truncation of lower-order principal components using different regularization techniques. One fundamental challenge in paleoclimate reconstruction efforts is the lack of out-of-sample data for predictive validation. Cross-validation is of potential value, but is computationally expensive and potentially sensitive to outliers in sparse data scenarios. To overcome the limitations that a lack of out-of-sample records presents, we test our methods using a simulation study, applying proper scoring rules including a computationally efficient approximation to leave-one-out cross-validation using the log score to validate model performance. The result of our analysis is a spatially explicit reconstruction of spatio-temporal temperature from a very sparse historical record.

Vegetation response to southern California drought during the Medieval Climate Anomaly and early Little Ice Age (AD 800–1600)

USGS Publications Warehouse

Heusser, Linda E.; Hendy, Ingrid L.; Barron, John A.

2015-01-01

The presence of xeric vegetation in SBB coincides with major drought events recorded in tree rings and low lake levels elsewhere in California except for the brief drought between AD 1130–1160. Correlative diatom and terrigenous sediment input proxy records from SBB are largely supportive of the pollen record predominantly linking the MCA with drought and La Niña-like conditions and the LIA with wetter (more El Niño-like) conditions. Differences between paleoclimate proxies (pollen, diatoms, and terrigenous sediment) in SBB exist, however, possibly reflecting the temporal and spatial differences in the generation of each proxy record, as well as their individual sensitivity to climate change.

Social voting advice applications-definitions, challenges, datasets and evaluation.

PubMed

Katakis, Ioannis; Tsapatsoulis, Nicolas; Mendez, Fernando; Triga, Vasiliki; Djouvas, Constantinos

2014-07-01

Voting advice applications (VAAs) are online tools that have become increasingly popular and purportedly aid users in deciding which party/candidate to vote for during an election. In this paper we present an innovation to current VAA design which is based on the introduction of a social network element. We refer to this new type of online tool as a social voting advice application (SVAA). SVAAs extend VAAs by providing (a) community-based recommendations, (b) comparison of users' political opinions, and (c) a channel of user communication. In addition, SVAAs enriched with data mining modules, can operate as citizen sensors recording the sentiment of the electorate on issues and candidates. Drawing on VAA datasets generated by the Preference Matcher research consortium, we evaluate the results of the first VAA-Choose4Greece-which incorporated social voting features and was launched during the landmark Greek national elections of 2012. We demonstrate how an SVAA can provide community based features and, at the same time, serve as a citizen sensor. Evaluation of the proposed techniques is realized on a series of datasets collected from various VAAs, including Choose4Greece. The collection is made available online in order to promote research in the field.

Transient coupling relationships of the Holocene Australian monsoon

NASA Astrophysics Data System (ADS)

McRobie, F. H.; Stemler, T.; Wyrwoll, K.-H.

2015-08-01

The northwest Australian summer monsoon owes a notable degree of its interannual variability to interactions with other regional monsoon systems. Therefore, changes in the nature of these relationships may contribute to variability in monsoon strength over longer time scales. Previous attempts to evaluate how proxy records from the Indonesian-Australian monsoon region correspond to other records from the Indian and East Asian monsoon regions, as well as to El Niño-related proxy records, have been qualitative, relying on 'curve-fitting' methods. Here, we seek a quantitative approach for identifying coupling relationships between paleoclimate proxy records, employing statistical techniques to compute the interdependence of two paleoclimate time series. We verify the use of complex networks to identify coupling relationships between modern climate indices. This method is then extended to a set of paleoclimate proxy records from the Asian, Australasian and South American regions spanning the past 9000 years. The resulting networks demonstrate the existence of coupling relationships between regional monsoon systems on millennial time scales, but also highlight the transient nature of teleconnections during this period. In the context of the northwest Australian summer monsoon, we recognise a shift in coupling relationships from strong interhemispheric links with East Asian and ITCZ-related proxy records in the mid-Holocene to significantly weaker coupling in the later Holocene. Although the identified links cannot explain the underlying physical processes leading to coupling between regional monsoon systems, this method provides a step towards understanding the role that changes in teleconnections play in millennial-to orbital-scale climate variability.

Linking Short and Long Term Sediment Delivery to Morphology and Seascape Evolution of Continental Margins

DTIC Science & Technology

1999-09-30

history. OBJECTIVES 1) Is the variability in a river’s sediment load, observed over the last 100 years or less, adequate to provide a proxy for longer-term...experiments, small basins are able to capture in terms of textural proxies , both the natural variability associated with precipitation and temperature...as well as realistic scenarios of abrupt climate change. Open ocean basins, like the Eel River, are less likely to record the proxy record of ambient

45 CFR 46.115 - IRB records.

Code of Federal Regulations, 2010 CFR

2010-10-01

... following: (1) Copies of all research proposals reviewed, scientific evaluations, if any, that accompany the... for Protection of Human Research Subjects § 46.115 IRB records. (a) An institution, or when... voting for, against, and abstaining; the basis for requiring changes in or disapproving research; and a...

Changing climate in a pre-impact world: a multi-proxy paleotemperature reconstruction across the last million years of the Cretaceous

NASA Astrophysics Data System (ADS)

Woelders, L.; Vellekoop, J.; Reichart, G. J.; de Nooijer, L. J.; Sluijs, A.; Peterse, F.; Claeys, P. F.; Speijer, R. P.

2015-12-01

Climate instability during the last million years of the Cretaceous (67-66 Ma) is still poorly documented and not well understood. One of the reasons for this is that in deep time, different proxies are likely to yield different temperatures. This is because the application of calibrations based on present day temperature proxy relationships is affected by source organism evolution, differences in ocean chemistry and non-analogue processes. Only by combining temperature estimates derived from different, independent proxies, the problems with individual proxies can be cancelled out. A quantitative, multi-proxy temperature record from the latest Cretaceous therefore may provide a better insight in climate changes across this time interval. For such a multi-proxy research, sediments are required that yield both well-preserved foraminiferal calcite as well as organic biomarkers. Very few sites are known to provide such sedimentary records, but ODP Leg 174AX Site Bass River (New Jersey Shelf) has proven to be an excellent archive for paleotemperature reconstructions for the Cretaceous and Paleogene. We here present a multi-proxy, quantitative paleotemperature reconstruction of the last million years of the Cretaceous of the Bass River core. Benthic and planktic foraminiferal Mg/Ca and δ18O were determined, as well as the organic geochemical sea surface temperature proxy TEX86. This resulted in a unique coupled surface and bottom water temperature record of the latest Cretaceous. Our data suggest a ~2-6 ˚C bottom water warming and a ~4-6 ˚C surface water warming approximately 300 kyr before the Cretaceous-Paleogene boundary, followed by a cooling trend across the boundary. This warming event appears to coincide with the main phase of the Deccan Traps eruptions and therefore probably represents a global event.

A preliminary study on teak tree ring cellulose δ18O from northwestern Thailand: the potential for developing multiproxy records of Thailand summer monsoon variability

NASA Astrophysics Data System (ADS)

Muangsong, Chotika; Cai, Binggui; Pumijumnong, Nathsuda; Lei, Guoliang; Wang, Fang

2018-05-01

Thailand monsoon is located in the transition zone between the Indian and western North Pacific monsoons. Assuredly, proxy climate data from this area could improve our understanding of the nature of Asian monsoon. Tree rings and stalagmites from this area are two potential materials for high-resolution paleoclimate reconstructions. However, a comprehensive understanding of these multiproxy records is still a challenge. In this study, a 76-year tree ring cellulose oxygen isotope value (δ18O) of a teak tree from northwestern Thailand was developed to test its climatic significance and potential for multiproxy climate reconstruction. The results indicate that the interannual variability of cellulose δ18O can be interpreted as a proxy of rainfall in the early monsoon season (May to July rainfall) as well as a proxy of relative humidity. Comparisons with speleothem proxies from the same locality and tree ring records from wider geographical areas provide a basis for developing a multiproxy approach. The results from a teleconnection analysis reveal that the El Niño-Southern Oscillation (ENSO) is an important climate mode that impacts monsoon rainfall in Thailand. High-quality proxy records covering recent decades are critically important not only to improve proxy data calibrations but also to provide a better understanding of teleconnections within the modern atmosphere. Preliminary findings demonstrated the potential of tree ring stable isotopes from Thai teak to develop multiproxy climate reconstruction.

Bayesian hierarchical models for regional climate reconstructions of the last glacial maximum

NASA Astrophysics Data System (ADS)

Weitzel, Nils; Hense, Andreas; Ohlwein, Christian

2017-04-01

Spatio-temporal reconstructions of past climate are important for the understanding of the long term behavior of the climate system and the sensitivity to forcing changes. Unfortunately, they are subject to large uncertainties, have to deal with a complex proxy-climate structure, and a physically reasonable interpolation between the sparse proxy observations is difficult. Bayesian Hierarchical Models (BHMs) are a class of statistical models that is well suited for spatio-temporal reconstructions of past climate because they permit the inclusion of multiple sources of information (e.g. records from different proxy types, uncertain age information, output from climate simulations) and quantify uncertainties in a statistically rigorous way. BHMs in paleoclimatology typically consist of three stages which are modeled individually and are combined using Bayesian inference techniques. The data stage models the proxy-climate relation (often named transfer function), the process stage models the spatio-temporal distribution of the climate variables of interest, and the prior stage consists of prior distributions of the model parameters. For our BHMs, we translate well-known proxy-climate transfer functions for pollen to a Bayesian framework. In addition, we can include Gaussian distributed local climate information from preprocessed proxy records. The process stage combines physically reasonable spatial structures from prior distributions with proxy records which leads to a multivariate posterior probability distribution for the reconstructed climate variables. The prior distributions that constrain the possible spatial structure of the climate variables are calculated from climate simulation output. We present results from pseudoproxy tests as well as new regional reconstructions of temperatures for the last glacial maximum (LGM, ˜ 21,000 years BP). These reconstructions combine proxy data syntheses with information from climate simulations for the LGM that were performed in the PMIP3 project. The proxy data syntheses consist either of raw pollen data or of normally distributed climate data from preprocessed proxy records. Future extensions of our method contain the inclusion of other proxy types (transfer functions), the implementation of other spatial interpolation techniques, the use of age uncertainties, and the extension to spatio-temporal reconstructions of the last deglaciation. Our work is part of the PalMod project funded by the German Federal Ministry of Education and Science (BMBF).

34 CFR 97.115 - IRB records.

Code of Federal Regulations, 2010 CFR

2010-07-01

... the Secretary, Department of Education PROTECTION OF HUMAN SUBJECTS Federal Policy for the Protection of Human Subjects (Basic ED Policy for Protection of Human Research Subjects) § 97.115 IRB records... in sufficient detail to show attendance at the meetings; actions taken by the IRB; the vote on these...

A review of the South American monsoon history as recorded in stable isotopic proxies over the past two millennia

NASA Astrophysics Data System (ADS)

Vuille, M.; Burns, S. J.; Taylor, B. L.; Cruz, F. W.; Bird, B. W.; Abbott, M. B.; Kanner, L. C.; Cheng, H.; Novello, V. F.

2012-08-01

We review the history of the South American summer monsoon (SASM) over the past ~2000 yr based on high-resolution stable isotope proxies from speleothems, ice cores and lake sediments. Our review is complemented by an analysis of an isotope-enabled atmospheric general circulation model (GCM) for the past 130 yr. Proxy records from the monsoon belt in the tropical Andes and SE Brazil show a very coherent behavior over the past 2 millennia with significant decadal to multidecadal variability superimposed on large excursions during three key periods: the Medieval Climate Anomaly (MCA), the Little Ice Age (LIA) and the current warm period (CWP). We interpret these three periods as times when the SASM's mean state was significantly weakened (MCA and CWP) and strengthened (LIA), respectively. During the LIA each of the proxy archives considered contains the most negative δ18O values recorded during the entire record length. On the other hand, the monsoon strength is currently rather weak in a 2000-yr historical perspective, rivaled only by the low intensity during the MCA. Our climatic interpretation of these archives is consistent with our isotope-based GCM analysis, which suggests that these sites are sensitive recorders of large-scale monsoon variations. We hypothesize that these centennial-scale climate anomalies were at least partially driven by temperature changes in the Northern Hemisphere and in particular over the North Atlantic, leading to a latitudinal displacement of the ITCZ and a change in monsoon intensity (amount of rainfall upstream over the Amazon Basin). This interpretation is supported by several independent records from different proxy archives and modeling studies. Although ENSO is the main forcing for δ18O variability over tropical South America on interannual time scales, our results suggest that its influence may be significantly modulated by North Atlantic climate variability on longer time scales. Finally, our analyses indicate that isotopic proxies, because of their ability to integrate climatic information on large spatial scales, could complement more traditional proxies such as tree rings or documentary evidence. Future climate reconstruction efforts could potentially benefit from including isotopic proxies as large-scale predictors in order to better constrain past changes in the atmospheric circulation.

Synthesizing late Holocene paleoclimate reconstructions: Lessons learned, common challenges, and implications for future research

NASA Astrophysics Data System (ADS)

Rodysill, J. R.

2017-12-01

Proxy-based reconstructions provide vital information for developing histories of environmental and climate changes. Networks of spatiotemporal paleoclimate information are powerful tools for understanding dynamical processes within the global climate system and improving model-based predictions of the patterns and magnitudes of climate changes at local- to global-scales. Compiling individual paleoclimate records and integrating reconstructed climate information in the context of an ensemble of multi-proxy records, which are fundamental for developing a spatiotemporal climate data network, are hindered by challenges related to data and information accessibility, chronological uncertainty, sampling resolution, climate proxy type, and differences between depositional environments. The U.S. Geological Survey (USGS) North American Holocene Climate Synthesis Working Group has been compiling and integrating multi-proxy paleoclimate data as part of an ongoing effort to synthesize Holocene climate records from North America. The USGS North American Holocene Climate Synthesis Working Group recently completed a late Holocene hydroclimate synthesis for the North American continent using several proxy types from a range of depositional environments, including lakes, wetlands, coastal marine, and cave speleothems. Using new age-depth relationships derived from the Bacon software package, we identified century-scale patterns of wetness and dryness for the past 2000 years with an age uncertainty-based confidence rating for each proxy record. Additionally, for highly-resolved North American lake sediment records, we computed average late Holocene sediment deposition rates and identified temporal trends in age uncertainty that are common to multiple lakes. This presentation addresses strengths and challenges of compiling and integrating data from different paleoclimate archives, with a particular focus on lake sediments, which may inform and guide future paleolimnological studies.

Was the Little Ice Age more or less El Niño-like than the Mediaeval Climate Anomaly? Evidence from hydrological and temperature proxy data

NASA Astrophysics Data System (ADS)

Henke, L. M. K.; Lambert, F. H.; Charman, D. J.

2015-11-01

The El Niño-Southern Oscillation (ENSO), an ocean-atmosphere coupled oscillation over the equatorial Pacific, is the most important source of global climate variability on inter-annual time scales. It has substantial environmental and socio-economic consequences such as devastation of South American fish populations and increased forest fires in Indonesia. The instrumental ENSO record is too short for analysing long-term trends and variability, hence proxy data is used to extend the record. However, different proxy sources have produced varying reconstructions of ENSO, with some evidence for a temperature-precipitation divergence in ENSO trends over the past millennium, in particular during the Mediaeval Climate Anomaly (MCA; AD 800-1300) and the Little Ice Age (LIA; AD 1400-1850). This throws into question the stability of the modern ENSO system and its links to the global climate, which has implications for future projections. Here we use a new statistical approach using EOF-based weighting to create two new large-scale ENSO reconstructions derived independently from precipitation proxies and temperature proxies respectively. The method is developed and validated using pseudoproxy experiments that address the effects of proxy dating error, resolution and noise to improve uncertainty estimations. The precipitation ENSO reconstruction displays a significantly more El Niño-like state during the LIA than the MCA, while the temperature reconstruction shows no significant difference. The trends shown in the precipitation ENSO reconstruction are relatively robust to variations in the precipitation EOF pattern. However, the temperature reconstruction suffers significantly from a lack of high-quality, favourably located proxy records, which limits its ability to capture the large-scale ENSO signal. Further expansion of the palaeo-database and improvements to instrumental, satellite and model representations of ENSO are needed to fully resolve the discrepancies found among proxy records.

Evaluating the Effect of Autogenic Sedimentation on the Preservation of Climate Proxy Records: Modeling and Examples from the Paleocene Eocene Thermal Maximum

NASA Astrophysics Data System (ADS)

Trampush, S. M.; Hajek, E. A.

2016-12-01

The stratigraphic record provides a vital opportunity to investigate how changes in climate can impact many different landscapes and seascapes. However, the inherent variability in sedimentation within many depositional environments may mask or remove the signature of climate change. A common solution is to use geochemical proxies - usually collected at regular stratigraphic intervals - to independently identify climate events. This approach doesn't account for the potentially significant variability in deposition and erosion time series resulting from autogenic landscape dynamics. In order to explore how geochemical proxy records could be overprinted by landscape dynamics, we use a 1D stochastic sedimentation model where we mimic fluvial, lacustrine, shallow marine, and deep marine environmental dynamics by varying the frequency-magnitude distributions of sedimentation rates. We find that even conservative estimates of the frequency and magnitude of stochastic sedimentation variability can heavily modify proxy records in characteristic ways by alternately removing, compressing, and expanding portions of the record, regardless of the magnitude or duration of the climatic event. Our model results are consistent with observations of the carbon isotope excursions of the Paleocene Eocene Thermal Maximum (PETM) preserved within both fluvial (e.g. the Bighorn Basin, Wyoming and the Piceance Basin, Colorado) and shallow marine (e.g. the New Jersey shelf) deposits. Our results suggest that we may be able to use existing geochemical proxy records within well studied, global climate events, such as the PETM, to constrain the variability in sedimentation present within different depositional environments.

11 CFR 9410.2 - Definitions.

Code of Federal Regulations, 2010 CFR

2010-01-01

... Vote Act of 2002, 42 U.S.C. 15323. Individual means a citizen of the United States or an alien lawfully... Commission including, but not limited to, his or her education, financial transactions, medical history, and... a photograph. Systems of records means a group of any records under the control of the Commission...

78 FR 36279 - Sunshine Act Meeting

Federal Register 2010, 2011, 2012, 2013, 2014

2013-06-17

... information pertaining to the PRISM-related activities and the Foreign Intelligence Surveillance Act. The...)(1), the Board determined, by recorded vote, that agency business requires that this meeting be...

Validation of a proxy for estrogen receptor status in breast cancer patients using dispensing data.

PubMed

Srasuebkul, Preeyaporn; Dobbins, Timothy A; Pearson, Sallie-Anne

2014-06-01

To assess the performance of a proxy for estrogen receptor (ER) status in breast cancer patients using dispensing data. We derived our proxy using 167 patients. ER+ patients had evidence of at least one dispensing record for hormone therapy during the lookback period, irrespective of diagnosis date and ER- had no dispensing records for hormone therapy during the period. We validated the proxy against our gold standard, ER status from pathology reports or medical records. We assessed the proxy's performance using three lookback periods: 4.5 years, 2 years, 1 year. More than half of our cohort (62%) were >50 years, 54% had stage III/IV breast cancer at recruitment, (46%) were diagnosed with breast cancer in 2009 and 23% were diagnosed before 2006. Sensitivity and specificity were high for the 4.5 year lookback period (93%, 95% CI: 86-96%; and 95%: 83-99%), respectively) and remained high for the 2-year lookback period (91%: 84-95%; and 95%: 83-99%). Sensitivity decreased (83%: 75.2-89%) but specificity remained high (95%: 83-99%) using the 1-year lookback period and the period is long enough to allow sufficient time for hormone therapy to be dispensed. Our proxy accurately infers ER status in studies of breast cancer treatment based on secondary health data. The proxy is most robust with a minimum lookback period of 2 years. © 2012 Wiley Publishing Asia Pty Ltd.

A Fifty-Year Coral Sr/Ca Time Series from Guam, Mariana Islands: In situ Monitoring and Comparison to Observed Pacific Climate

NASA Astrophysics Data System (ADS)

Lander, M.

2016-12-01

Located on the northern edge of the West Pacific Warm Pool, Guam is positioned to obtain uniquely valuable natural records of west Pacific maritime paleoclimate. This study is the first to evaluate the application of the coral Sr/Ca sea surface temperature (SST) proxy to the reconstruction of Guam's climate history. To help test the fidelity of the coral Sr/Ca proxy to actual climate, and how it might be affected by environmental variables—on Guam or elsewhere—the study documented monthly seawater oxygen isotope ratios (δ18O), pH, cation, and nitrate concentrations from September 2009 to December 2010 at a Porites lutea colony in Guam's Apra Harbor. The study site was chosen for its accessibility, so that environmental conditions could be readily monitored. A 50-year Sr/Ca record was carefully compared to instrumental records, the quality and reliability of which were also closely examined. Time series of seawater δ18O, pH, and cation concentrations show some evidence of freshwater input from direct rainfall or stream discharge into the harbor. The Sr/Ca proxy SST results, however, are robust, and do not appear to have been significantly affected. The Sr/Ca proxy reproduces the long-term warming trend observed in the historical records of regional SST and local air temperature. Moreover, it shows remarkable fidelity to regional ocean-atmosphere variations as represented by the indices of the El Niño/Southern Oscillation and the Pacific Decadal Oscillation. The consistency of the results with Guam's historical instrumental records, with previous δ18O results from Guam, and with previous Sr/Ca proxy results in similar environments elsewhere, demonstrate the efficacy of accessible near-shore sites for obtaining reliable Sr/Ca climate proxies, and the utility of Guam as a source for accurate coral records of western Pacific Ocean regional climate.

Arctic temperature and moisture trends during the past 2000 years - Progress from multiproxy-paleoclimate data compilations

NASA Astrophysics Data System (ADS)

Kaufman, Darrell; Routson, Cody; McKay, Nicholas; Beltrami, Hugo; Jaume-Santero, Fernando; Konecky, Bronwen; Saenger, Casey

2017-04-01

Instrumental climate data and climate-model projections show that Arctic-wide surface temperature and precipitation are positively correlated. Higher temperatures coincide with greater moisture by: (1) expanding the duration and source area for evaporation as sea ice retracts, (2) enhancing the poleward moisture transport, and (3) increasing the water-vapor content of the atmosphere. Higher temperature also influences evaporation rate, and therefore precipitation minus evaporation (P-E), the climate variable often sensed by paleo-hydroclimate proxies. Here, we test whether Arctic temperature and moisture also correlate on centennial timescales over the Common Era (CE). We use the new PAGES2k multiproxy-temperature dataset along with a first-pass compilation of moisture-sensitive proxy records to calculate century-scale composite timeseries, with a focus on longer records that extend back through the first millennium CE. We present a new Arctic borehole temperature reconstruction as a check on the magnitude of Little Ice Age cooling inferred from the proxy records, and we investigate the spatial pattern of centennial-scale variability. Similar to previous reconstructions, v2 of the PAGES2k proxy temperature dataset shows that, prior to the 20th century, mean annual Arctic-wide temperature decreased over the CE. The millennial-scale cooling trend is most prominent in proxy records from glacier ice, but is also registered in lake and marine sediment, and trees. In contrast, the composite of moisture-sensitive (primarily P-E) records does not exhibit a millennial-scale trend. Determining whether fluctuations in the mean state of Arctic temperature and moisture were in fact decoupled is hampered by the difficulty in detecting a significant trend within the relatively small number of spatially heterogeneous multi-proxy moisture-sensitive records. A decoupling of temperature and moisture would indicate that evaporation had a strong counterbalancing effect on precipitation and/or that shifting circulation patterns overwhelmed any multi-centennial-scale co-variability.

North Atlantic Oscillation dynamics recorded in shells of a long-lived bivalve mollusk

NASA Astrophysics Data System (ADS)

Schöne, Bernd R.; Oschmann, Wolfgang; Rössler, Jochen; Freyre Castro, Antuané D.; Houk, Stephen D.; Kröncke, Ingrid; Dreyer, Wolfgang; Janssen, Ronald; Rumohr, Heye; Dunca, Elena

2003-12-01

Existing reconstructions of the winter North Atlantic Oscillation (WNAO) are based on terrestrial proxies and historical documents. No direct high-resolution, long-term rec ords from marine settings are available for this major climate-dictating phenomenon, which severely affects a variety of economic aspects of our society. Here we present a 245 yr proxy WNAO index based on shells of the long-lived marine bivalve mollusk Arctica islandica. Variations in annual rates of shell growth are positively correlated with WNAO-related changes in the food supply. Maximum amplitudes in frequency bands of 7 9 and 5 7 yr fall exactly within the range of instrumental and other proxy WNAO indices. These estimates were obtained for specimens collected live, 2000 km apart, in the central North Sea and on the Norwegian Shelf. Hence, the WNAO influences hydrographic regimes of large regions of the ocean. Our study demonstrates that A. islandica can reliably reconstruct WNAO dynamics for time intervals and regions without instrumental records. Our new tool functions as a proxy for the WNAO index prior to the twentieth-century greenhouse forcing and has the potential to further validate other proxy-based WNAO records.

Is Recent Warming Unprecedented in the Common Era? Insights from PAGES2k data and the Last Millennium Reanalysis

NASA Astrophysics Data System (ADS)

Erb, M. P.; Emile-Geay, J.; McKay, N.; Hakim, G. J.; Steig, E. J.; Anchukaitis, K. J.

2017-12-01

Paleoclimate observations provide a critical context for 20th century warming by putting recent climate change into a longer-term perspective. Previous work (e.g. IPCC AR3-5) has claimed that recent decades are exceptional in the context of past centuries, though these statements are usually accompanied by large uncertainties and little spatial detail. Here we leverage a recent multiproxy compilation (PAGES2k Consortium, 2017) to revisit this long-standing question. We do so via two complementary approaches. The first approach compares multi-decadal averages and trends in PAGES2k proxy records, which include trees, corals, ice cores, and more. Numerous proxy records reveal that late 20th century values are extreme compared to the remainder of the recorded period, although considerable variability exists in the signals preserved in individual records. The second approach uses the same PAGES2k data blended with climate model output to produce an optimal analysis: the Last Millennium Reanalysis (LMR; Hakim et al., 2016). Unlike proxy data, LMR is spatially-complete and explicitly models uncertainty in proxy records, resulting in objective error estimates. The LMR results show that for nearly every region of the world, late 20th century temperatures exceed temperatures in previous multi-decadal periods during the Common Era, and 20th century warming rates exceed rates in previous centuries. An uncertainty with the present analyses concerns the interpretation of proxy records. PAGES2k included only records that are primarily sensitive to temperature, but many proxies may be influenced by secondary non-temperature effects. Additionally, the issue of seasonality is important as, for example, many temperature-sensitive tree ring chronologies in the Northern Hemisphere respond to summer or growing season temperature rather than annual-means. These uncertainties will be further explored. References Hakim, G. J., et al., 2016: The last millennium climate reanalysis project: Framework and first results. Journal of Geophysical Research: Atmospheres, 121(12), 6745-6764. http://doi.org/10.1002/2016JD024751 PAGES2k Consortium, 2017: A global multiproxy database for temperature reconstructions of the Common Era. Scientific Data, 1-33. http://doi.org/10.1038/sdata.2017.88

Multiscale combination of climate model simulations and proxy records over the last millennium

NASA Astrophysics Data System (ADS)

Chen, Xin; Xing, Pei; Luo, Yong; Nie, Suping; Zhao, Zongci; Huang, Jianbin; Tian, Qinhua

2018-05-01

To highlight the compatibility of climate model simulation and proxy reconstruction at different timescales, a timescale separation merging method combining proxy records and climate model simulations is presented. Annual mean surface temperature anomalies for the last millennium (851-2005 AD) at various scales over the land of the Northern Hemisphere were reconstructed with 2° × 2° spatial resolution, using an optimal interpolation (OI) algorithm. All target series were decomposed using an ensemble empirical mode decomposition method followed by power spectral analysis. Four typical components were obtained at inter-annual, decadal, multidecadal, and centennial timescales. A total of 323 temperature-sensitive proxy chronologies were incorporated after screening for each component. By scaling the proxy components using variance matching and applying a localized OI algorithm to all four components point by point, we obtained merged surface temperatures. Independent validation indicates that the most significant improvement was for components at the inter-annual scale, but this became less evident with increasing timescales. In mid-latitude land areas, 10-30% of grids were significantly corrected at the inter-annual scale. By assimilating the proxy records, the merged results reduced the gap in response to volcanic forcing between a pure reconstruction and simulation. Difficulty remained in verifying the centennial information and quantifying corresponding uncertainties, so additional effort should be devoted to this aspect in future research.

Suitability of satellite derived and gridded sea surface temperature data sets for calibrating high-resolution marine proxy records

NASA Astrophysics Data System (ADS)

Ouellette, G., Jr.; DeLong, K. L.

2016-02-01

High-resolution proxy records of sea surface temperature (SST) are increasingly being produced using trace element and isotope variability within the skeletal materials of marine organisms such as corals, mollusks, sclerosponges, and coralline algae. Translating the geochemical variations within these organisms into records of SST requires calibration with SST observations using linear regression methods, preferably with in situ SST records that span several years. However, locations with such records are sparse; therefore, calibration is often accomplished using gridded SST data products such as the Hadley Center's HADSST (5º) and interpolated HADISST (1º) data sets, NOAA's extended reconstructed SST data set (ERSST; 2º), optimum interpolation SST (OISST; 1º), and Kaplan SST data sets (5º). From these data products, the SST used for proxy calibration is obtained for a single grid cell that includes the proxy's study site. The gridded data sets are based on the International Comprehensive Ocean-Atmosphere Data Set (ICOADS) and each uses different methods of interpolation to produce the globally and temporally complete data products except for HadSST, which is not interpolated but quality controlled. This study compares SST for a single site from these gridded data products with a high-resolution satellite-based SST data set from NOAA (Pathfinder; 4 km) with in situ SST data and coral Sr/Ca variability for our study site in Haiti to assess differences between these SST records with a focus on seasonal variability. Our results indicate substantial differences in the seasonal variability captured for the same site among these data sets on the order of 1-3°C. This analysis suggests that of the data products, high-resolution satellite SST best captured seasonal variability at the study site. Unfortunately, satellite SST records are limited to the past few decades. If satellite SST are to be used to calibrate proxy records, collecting modern, living samples is desirable.

32 CFR 1908.35 - Action by appeals authority.

Code of Federal Regulations, 2010 CFR

2010-07-01

... consisting of the request, the document(s) (sanitized and full text) at issue, and the findings of the... of the Panel. (b) Action by Historical Records Policy Board. In any cases of divided vote by the ARP, any member of that body is authorized to refer the request to the CIA Historical Records Policy Board...

Stability of ENSO and Its Tropical Pacific Teleconnections over the Last Millennium

NASA Technical Reports Server (NTRS)

Lewis, Sophie; Legrande, A. N.

2015-01-01

Determining past changes in the amplitude, frequency and teleconnections of the El Nio Southern Oscillation (ENSO) is important for understanding its potential sensitivity to future anthropogenic climate change. Palaeo-reconstructions from proxy records provide long-term information of ENSO interactions with the background climatic state through time. However, it remains unclear how ENSO characteristics have changed through time, and precisely which signals proxies record. Proxy interpretations are underpinned by the assumption of stationarity in relationships between local and remote climates, and often utilise archives from single locations located in the Pacific Ocean to reconstruct ENSO histories. Here, we investigate the stationarity of ENSO teleconnections using the Last Millennium experiment of CMIP5 (Coupled Model Intercomparison Project phase 5) (Taylor et al., 2012). We show that modelled ENSO characteristics vary on decadal- to centennial-scales, resulting from internal variability and external forcings, such as tropical volcanic eruptions. Furthermore, the relationship between ENSO conditions and local climates across the Pacific basin varies throughout the Last Millennium. Results show the stability of teleconnections is regionally dependent and proxies may reveal complex changes in teleconnected patterns, rather than large-scale changes in base ENSO characteristics. As such, proxy insights into ENSO likely require evidence to be synthesised over large spatial areas in order to deconvolve changes occurring in the NINO3.4 region from those pertaining to proxy-relevant local climatic variables. To obtain robust histories of the ENSO and its remote impacts, we recommend interpretations of proxy records should be considered in conjunction with palaeo-reconstructions from within the Central Pacific

A fresh look at the Last Glacial Maximum using Paleoclimate Data Assimilation

NASA Astrophysics Data System (ADS)

Malevich, S. B.; Tierney, J. E.; Hakim, G. J.; Tardif, R.

2017-12-01

Quantifying climate conditions during the Last Glacial Maximum ( 21ka) can help us to understand climate responses to forcing and climate states that are poorly represented in the instrumental record. Paleoclimate proxies may be used to estimate these climate conditions, but proxies are sparsely distributed and possess uncertainties from environmental and biogeochemical processes. Alternatively, climate model simulations provide a full-field view, but may predict unrealistic climate states or states not faithful to proxy records. Here, we use data assimilation - combining climate proxy records with a theoretical understanding from climate models - to produce field reconstructions of the LGM that leverage the information from both data and models. To date, data assimilation has mainly been used to produce reconstructions of climate fields through the last millennium. We expand this approach in order to produce a climate fields for the Last Glacial Maximum using an ensemble Kalman filter assimilation. Ensemble samples were formed from output from multiple models including CCSM3, CESM2.1, and HadCM3. These model simulations are combined with marine sediment proxies for upper ocean temperature (TEX86, UK'37, Mg/Ca and δ18O of foraminifera), utilizing forward models based on a newly developed suite of Bayesian proxy system models. We also incorporate age model and radiocarbon reservoir uncertainty into our reconstructions using Bayesian age modeling software. The resulting fields show familiar patterns based on comparison with previous proxy-based reconstructions, but additionally reveal novel patterns of large-scale shifts in ocean-atmosphere dynamics, as the surface temperature data inform upon atmospheric circulation and precipitation patterns.

45 CFR 1703.204 - Public availability of recorded vote to close meeting.

Code of Federal Regulations, 2014 CFR

2014-10-01

...) NATIONAL COMMISSION ON LIBRARIES AND INFORMATION SCIENCE GOVERNMENT IN THE SUNSHINE ACT Procedures... to attend and identifying their affiliation, unless such disclosure would reveal the information that...

45 CFR 1703.204 - Public availability of recorded vote to close meeting.

Code of Federal Regulations, 2010 CFR

2010-10-01

...) NATIONAL COMMISSION ON LIBRARIES AND INFORMATION SCIENCE GOVERNMENT IN THE SUNSHINE ACT Procedures... to attend and identifying their affiliation, unless such disclosure would reveal the information that...

The importance of independent chronology in integrating records of past climate change for the 60-8 ka INTIMATE time interval

NASA Astrophysics Data System (ADS)

Brauer, Achim; Hajdas, Irka; Blockley, Simon P. E.; Bronk Ramsey, Christopher; Christl, Marcus; Ivy-Ochs, Susan; Moseley, Gina E.; Nowaczyk, Norbert N.; Rasmussen, Sune O.; Roberts, Helen M.; Spötl, Christoph; Staff, Richard A.; Svensson, Anders

2014-12-01

This paper provides a brief overview of the most common dating techniques applied in palaeoclimate and palaeoenvironmental studies including four radiometric and isotopic dating methods (radiocarbon, 230Th disequilibrium, luminescence, cosmogenic nuclides) and two incremental methods based on layer counting (ice layer, varves). For each method, concise background information about the fundamental principles and methodological approaches is provided. We concentrate on the time interval of focus for the INTIMATE (Integrating Ice core, MArine and TErrestrial records) community (60-8 ka). This dating guide addresses palaeoclimatologists who aim at interpretation of their often regional and local proxy time series in a wider spatial context and, therefore, have to rely on correlation with proxy records obtained from different archives from various regions. For this reason, we especially emphasise scientific approaches for harmonising chronologies for sophisticated and robust proxy data integration. In this respect, up-to-date age modelling techniques are presented as well as tools for linking records by age equivalence including tephrochronology, cosmogenic 10Be and palaeomagnetic variations. Finally, to avoid inadequate documentation of chronologies and assure reliable correlation of proxy time series, this paper provides recommendations for minimum standards of uncertainty and age datum reporting.

Extending isotopic fractionation in phytoplankton for Phanerozoic pCO2 reconstruction

NASA Astrophysics Data System (ADS)

Witkowski, C. R.; Agostini, S.; Weijers, J.; Schouten, S.; S Sinninghe Damsté, J.

2017-12-01

The atmospheric concentration of carbon dioxide (pCO2) is a keystone in many earth system dynamics, including the biosphere, carbon cycle, and climate. In order to better understand the impact of today's exceptional increases in pCO2 on the future, we look to secular trends in pCO2. Photosynthetic carbon isotopic fractionation (Ɛp), calculated from the difference between the stable carbon isotopic composition (δ13C) of environmental CO2 and biomass, has some of the lowest uncertainty in estimation among CO2 proxies. However, Ɛp is generally applied to species-specific compounds which have an evolution-limited record (e.g. alkenones limited ca. 50 Ma). To extend the use of Ɛp, we explore the general phytoplankton biomarker phytane. As the fossilized side-chain of chlorophyll, phytane is spatially and temporally ubiquitous, with the potential to record pCO2 back to the earliest photoautotrophs in the geologic record. To develop and validate its potential as a pCO2 proxy, we explored phytane in modern environments, in a multi-proxy case study, and in a Phanerozoic reconstruction. As a proof-of-concept, the δ13C of phytane was tested in modern environments at naturally-occurring CO2 vents in Japan and Italy, which showed clear fractionation over the steep CO2 gradient. This was then further tested in a multi-proxy assessment in DSDP site 467 that spans the last 15 Ma, looking at both well-established (i.e. alkenones) and potential (i.e. phytane, steranes, hopanes) pCO2 proxies; phytane represented the average δ13C for these biomarkers. Finally, the δ13C of phytane data over the Phanerozoic was compiled, showing agreement with literature reconstructions of pCO2. Current pCO2 reconstructions are derived from many different types of proxies, which can create incongruities and inconsistencies throughout time, making this single well-constrained proxy that ubiquitously spans the geologic record a useful addition to the palaeo-detective's toolbox.

Finding a Needle in a Climate Haystack

NASA Astrophysics Data System (ADS)

Verosub, K. L.; Medrano, R.; Valentine, M.

2014-12-01

We are studying the regional impact of volcanic eruptions that might have caused global cooling using high-quality annual-resolution proxy records of natural phenomena, such as tree-ring widths, and cultural events, such as the dates of the beginning of grape and rye harvests. To do this we need to determine if the year following an eruption was significantly colder and wetter than preceding or subsequent years as measured by any given proxy and if that year is consistently cold and wet across different proxies. The problem is complicated by the fact that normal inter-annual variations in any given proxy can be quite large and can obscure any volcanological impact and by the fact that inter-annual variations for different proxies will have different means and standard deviations. We address the first problem by assuming that on a regional scale, the inter-annual variations of different proxies are at best only weakly correlated and that, in the absence of a volcanological signal, these variations will average out on a regional scale. We address the second problem by renormalizing each record so that it has the same mean and standard deviation over a given time interval. We then sum the re-normalized records on a year-by-year basis and look for years with significantly higher total scores. The method can also be used to assess the statistical significance of an anomalous value. Our initial analysis of records primarily from the Northern Hemisphere shows that the years 1601 and 1816 were significantly colder and wetter than any others in the past 500 years. These years followed the eruptions of Huayanaputina in Chile and Tambora in Indonesia, respectively, by one year. The years 1698 and 1837 also show up as being climatologically severe although they have not (yet) been associated with specific volcanic eruptions.

Validation and application of a death proxy in adult cancer patients.

PubMed

Mealing, Nicole M; Dobbins, Timothy A; Pearson, Sallie-Anne

2012-07-01

PURPOSE: Fact of death is not always available on data sets used for pharmacoepidemiological research. Proxies may be an appropriate substitute in the absence of death data. The purposes of this study were to validate a proxy for death in adult cancer patients and to assess its performance when estimating survival in two cohorts of cancer patients. METHODS: We evaluated 30-, 60-, 90- and 180-day proxies overall and by cancer type using data from 12 394 Australian veterans with lung, colorectal, breast or prostate cancer. The proxy indicated death if the difference between the last dispensing record and the end of the observational period exceeded the proxy cutoff. We then compared actual survival to 90-day proxy estimates in a subset of 4090 veterans with 'full entitlements' for pharmaceutical items and in 3704 Australian women receiving trastuzumab for HER2+ metastatic breast cancer. RESULTS: The 90-day proxy was optimal with an overall sensitivity of 99.3% (95%CI: 98.4-99.7) and a specificity of 97.6% (95%CI: 91.8-99.4). These measures remained high when evaluated by cancer type and spread of disease. The application of the proxy using the most conservative date of death estimate (date of last dispensing) generally underestimated survival, with estimates up to 3 months shorter than survival based on fact of death. CONCLUSIONS: A 90-day death proxy is a robust substitute to identify death in a chronic population when fact of death is not available. The proxy is likely to be valid across a range of chronic diseases as it relies on the presence of 'regular' dispensing records for individual patients. Copyright © 2011 John Wiley & Sons, Ltd. Copyright © 2011 John Wiley & Sons, Ltd.

Statistical framework for evaluation of climate model simulations by use of climate proxy data from the last millennium - Part 1: Theory

NASA Astrophysics Data System (ADS)

Sundberg, R.; Moberg, A.; Hind, A.

2012-08-01

A statistical framework for comparing the output of ensemble simulations from global climate models with networks of climate proxy and instrumental records has been developed, focusing on near-surface temperatures for the last millennium. This framework includes the formulation of a joint statistical model for proxy data, instrumental data and simulation data, which is used to optimize a quadratic distance measure for ranking climate model simulations. An essential underlying assumption is that the simulations and the proxy/instrumental series have a shared component of variability that is due to temporal changes in external forcing, such as volcanic aerosol load, solar irradiance or greenhouse gas concentrations. Two statistical tests have been formulated. Firstly, a preliminary test establishes whether a significant temporal correlation exists between instrumental/proxy and simulation data. Secondly, the distance measure is expressed in the form of a test statistic of whether a forced simulation is closer to the instrumental/proxy series than unforced simulations. The proposed framework allows any number of proxy locations to be used jointly, with different seasons, record lengths and statistical precision. The goal is to objectively rank several competing climate model simulations (e.g. with alternative model parameterizations or alternative forcing histories) by means of their goodness of fit to the unobservable true past climate variations, as estimated from noisy proxy data and instrumental observations.

The use of Sphagnum cellulose oxygen isotope ratios in ombrotrophic peatlands as a proxy for paleoclimate.

NASA Astrophysics Data System (ADS)

Taylor, M.; Pendall, E.; Jackson, S.; Booth, R. K.; Nichols, J. E.; Huang, Y.

2006-12-01

Developing proxies for discerning paleoclimate that are independent of the pollen record can provide insight into various aspects of climate variability and improve confidence in the interpretation of climate-vegetation interactions. To date, proxies including plant macrofossils, humification indices, testate amoebae, and ratios of n-alkane abundances have been used to infer past climate variability from temperate ombrotrophic peatlands in upper Midwestern North America. These proxies are used to infer past changes in surface-moisture conditions, which in ombrotrophic peatlands is primarily a function of precipitation and temperature. This study investigates the potential uses of stable oxygen isotopes to complement hydrologic proxies. δ18O of surface water and Sphagnum moss cellulose from bogs throughout North America indicates a correlation between average growing season temperatures and δ18O-values. The existence of a modern temperature signal in moss cellulose suggests that δ18O-derived records will not only complement paleohydrological records, but also help assess relative changes in precipitation and temperature. Humification and testate amoebae data from two cores taken from Minden and Irwin Smith Bogs in central and northeastern Michigan have recorded several extreme drought events during the Holocene, including one at 1000 YBP. Comparison of δ18O-values of picked Sphagnum remains to down-core humification and testate amoebae data suggest good temporal correspondence, with the δ18O-values around 1000 YBP indicating a warmer growing season.

12 CFR 544.5 - Federal mutual savings association bylaws.

Code of Federal Regulations, 2013 CFR

2013-01-01

... record at the last address appearing on the books of the association. A similar notice shall be posted in... a method for determining from the books of the association the members entitled to vote. Such date... member, however, shall have the right to inspect or copy any portion of any books or records of a Federal...

12 CFR 544.5 - Federal mutual savings association bylaws.

Code of Federal Regulations, 2014 CFR

2014-01-01

... record at the last address appearing on the books of the association. A similar notice shall be posted in... a method for determining from the books of the association the members entitled to vote. Such date... member, however, shall have the right to inspect or copy any portion of any books or records of a Federal...

The Relationship Between the Zonal Mean ITCZ and Regional Precipitation during the mid-Holocene

NASA Astrophysics Data System (ADS)

Niezgoda, K.; Noone, D.; Konecky, B.

2017-12-01

Characteristics of the zonal mean Tropical Rain Belt (TRB, i.e. the ITCZ + the land-based monsoons) are often inferred from individual proxy records of precipitation or other hydroclimatic variables. However, these inferences can be misleading. Here, an isotope-enabled climate model simulation is used to evaluate metrics of the zonal mean ITCZ vs. regional hydrological characteristics during the mid-Holocene (MH, 6 kya). The MH provides a unique perspective on the relationship between the ITCZ and regional hydrology because of large, orbitally-driven shifts in tropical precipitation as well as a critical mass of proxy records. By using a climate model with simulated water isotopes, characteristics of atmospheric circulation and water transport processes can be inferred, and comparison with isotope proxies can be made more directly. We find that estimations of the zonal-mean ITCZ are insufficient for evaluating regional responses of hydrological cycles to forcing changes. For example, one approximation of a 1.5-degree northward shift in the zonal-mean ITCZ position during the MH corresponded well with northward shifts in maximum rainfall in tropical Africa, but did not match southward shifts in the tropical Pacific or longitudinal shifts in the Indian monsoon region. In many regions, the spatial distribution of water vapor isotopes suggests that changes in moisture source and atmospheric circulation were a greater influence on precipitation distribution, intensity, and isotope ratio than the average northward shift in ITCZ latitude. These findings reinforce the idea that using tropical hydrological proxy records to infer zonal-mean characteristics of the ITCZ may be misleading. Rather, tropical proxy records of precipitation, particularly those that record precipitation isotopes, serve as a guideline for regional hydrological changes while model simulations can put them in the context of zonal mean tropical convergence.

Arctic hydroclimate variability during the last 2000 years: current understanding and research challenges

NASA Astrophysics Data System (ADS)

Linderholm, Hans W.; Nicolle, Marie; Francus, Pierre; Gajewski, Konrad; Helama, Samuli; Korhola, Atte; Solomina, Olga; Yu, Zicheng; Zhang, Peng; D'Andrea, William J.; Debret, Maxime; Divine, Dmitry V.; Gunnarson, Björn E.; Loader, Neil J.; Massei, Nicolas; Seftigen, Kristina; Thomas, Elizabeth K.; Werner, Johannes; Andersson, Sofia; Berntsson, Annika; Luoto, Tomi P.; Nevalainen, Liisa; Saarni, Saija; Väliranta, Minna

2018-04-01

Reanalysis data show an increasing trend in Arctic precipitation over the 20th century, but changes are not homogenous across seasons or space. The observed hydroclimate changes are expected to continue and possibly accelerate in the coming century, not only affecting pan-Arctic natural ecosystems and human activities, but also lower latitudes through the atmospheric and ocean circulations. However, a lack of spatiotemporal observational data makes reliable quantification of Arctic hydroclimate change difficult, especially in a long-term context. To understand Arctic hydroclimate and its variability prior to the instrumental record, climate proxy records are needed. The purpose of this review is to summarise the current understanding of Arctic hydroclimate during the past 2000 years. First, the paper reviews the main natural archives and proxies used to infer past hydroclimate variations in this remote region and outlines the difficulty of disentangling the moisture from the temperature signal in these records. Second, a comparison of two sets of hydroclimate records covering the Common Era from two data-rich regions, North America and Fennoscandia, reveals inter- and intra-regional differences. Third, building on earlier work, this paper shows the potential for providing a high-resolution hydroclimate reconstruction for the Arctic and a comparison with last-millennium simulations from fully coupled climate models. In general, hydroclimate proxies and simulations indicate that the Medieval Climate Anomaly tends to have been wetter than the Little Ice Age (LIA), but there are large regional differences. However, the regional coverage of the proxy data is inadequate, with distinct data gaps in most of Eurasia and parts of North America, making robust assessments for the whole Arctic impossible at present. To fully assess pan-Arctic hydroclimate variability for the last 2 millennia, additional proxy records are required.

Practical experience using speleothem data in multi-proxy climate reconstructions

NASA Astrophysics Data System (ADS)

Graham, N.

2009-04-01

Speleothem records have clear potential to extend and sharpen our understanding of past climate change. Many speleothem records feature both high sample resolution and precision age models, characteristics generally available only in tree-ring records, among terrestrial climate proxies. Speleothem records also avoid some processes that add uncertainty to the interpretation of biological proxy records. At the same time, model results suggest that even if speleothems did provide long and perfect records of meteoric water isotope concentrations, it would not be always be obvious how to interpret the isotopic fluctuations unambiguously in terms of precipitation or temperature variability. Other uncertainties can arise from local hydrologic and speleothem growth processes, as well as sampling and calibration uncertainties. Similar comments apply to other sorts of speleothem-derived records, e.g., verve thickness. These issues of interpretation are especially important in cases where data availability makes calibration to local climate data problematic and when past climate conditions limit the relevance of such calibrations. The presentation will focus broadly on the use of speleothem records together with other sorts of proxy records either to get a general idea of climatic change during some period, or for more formal climate field reconstruction. Examples from few such efforts will be given. Results from simulations with models incorporating stable water isotopes will be discussed, with consideration of what the results imply about the climatic interpretation of speleothem isotope records. The views will be those a climate scientist trying to make better use of speleothem data, a perspective which will highlight 1) where climate researchers would benefit from better understanding of isotope and speleothem processes, and 2) what steps that speleothem researchers could take to tighten the physical interpretation of their records. Convergence on these points will allow us to take better take advantage of the precision and spatial distribution of speleothem records offer for the understanding of past climate.

South American Monsoon variability during the past 2,000 years from stable isotopic proxies and model simulations

NASA Astrophysics Data System (ADS)

Vuille, M.; Cruz, F. W.; Abbott, M.; Bird, B. W.; Burns, S. J.; Cheng, H.; Colose, C. M.; Kanner, L. C.; LeGrande, A. N.; Novello, V. F.; Taylor, B. L.

2012-12-01

The rapidly growing number of high-resolution stable isotopic proxies from speleothems, ice cores and lake sediments, located in the South American summer monsoon (SASM) belt, will soon allow for a comprehensive analysis of climate variability in the South American tropics and subtropics over the past ~ 2000 years. In combination with isotope-enabled General Circulation Models (GCMs) this offers new prospects for better understanding the spatiotemporal dynamics of the South American monsoon system and for diagnosing its sensitivities to external forcing mechanisms (solar, volcanic) and modes of ocean-atmosphere variability (e.g. ENSO and AMO). In this presentation we will discuss the rationale for interpreting isotopic excursions recorded in various proxies from the Andes, northeastern and southeastern Brazil as indicative of changes in monsoon intensity. We will focus on the past 2 millenia when isotopic proxies from the SASM region show a very coherent behavior regardless of the type of archive or their location. All proxies exhibit significant decadal to multidecadal variability, superimposed on large excursions during three key periods, the Medieval Climate Anomaly (MCA), the Little Ice Age (LIA) and the Current Warm Period (CWP). We interpret these three periods as times when the SASM mean state was significantly weakened (MCA and CWP) and strengthened (LIA), respectively. During the LIA each of the proxy archives considered contains the most negative delta-18O values recorded during the entire record length. On the other hand the monsoon strength is currently rather weak in a 2000- year historical perspective, rivaled only by the low intensity during the MCA. One interpretation of these centennial-scale climate anomalies suggests that they were at least partially driven by temperature changes in the northern hemisphere and in particular over the North Atlantic, leading to a latitudinal displacement of the ITCZ and a change in monsoon intensity and degree of rainout upstream of the proxy locations, over the tropical continent. This interpretation is supported by several independent proxy archives and modeling studies. One question that remains, however, is how ENSO, arguably the main forcing factor for delta-18O variability over tropical South America on interannual time scales, interacts with and may be modulated by low-frequency North Atlantic forcing. Our analysis also implies that isotopic proxies, because of their ability to integrate climatic information on large spatial scales, are complementary to more traditional proxies such as tree rings or historical archives, which record in-situ climate variations. Future climate reconstructions therefore should make an effort to include isotopic proxies as large-scale predictors in order to better constrain past changes in the atmospheric circulation.

Elaboration over a Discourse Facilitates Retrieval in Sentence Processing.

PubMed

Troyer, Melissa; Hofmeister, Philip; Kutas, Marta

2016-01-01

Language comprehension requires access to stored knowledge and the ability to combine knowledge in new, meaningful ways. Previous work has shown that processing linguistically more complex expressions ('Texas cattle rancher' vs. 'rancher') leads to slow-downs in reading during initial processing, possibly reflecting effort in combining information. Conversely, when this information must subsequently be retrieved (as in filler-gap constructions), processing is facilitated for more complex expressions, possibly because more semantic cues are available during retrieval. To follow up on this hypothesis, we tested whether information distributed across a short discourse can similarly provide effective cues for retrieval. Participants read texts introducing two referents (e.g., two senators), one of whom was described in greater detail than the other (e.g., 'The Democrat had voted for one of the senators, and the Republican had voted for the other, a man from Ohio who was running for president'). The final sentence (e.g., 'The senator who the {Republican/Democrat}had voted for…') contained a relative clause picking out either the Many-Cue referent (with 'Republican') or the One-Cue referent (with 'Democrat'). We predicted facilitated retrieval (faster reading times) for the Many-Cue condition at the verb region ('had voted for'), where readers could understand that 'The senator' is the object of the verb. As predicted, this pattern was observed at the retrieval region and continued throughout the rest of the sentence. Participants also completed the Author/Magazine Recognition Tests (ART/MRT; Stanovich and West, 1989), providing a proxy for world knowledge. Since higher ART/MRT scores may index (a) greater experience accessing relevant knowledge and/or (b) richer/more highly structured representations in semantic memory, we predicted it would be positively associated with effects of elaboration on retrieval. We did not observe the predicted interaction between ART/MRT scores and Cue condition at the retrieval region, though ART/MRT interacted with Cue condition in other locations in the sentence. In sum, we found that providing more elaborative information over the course of a text can facilitate retrieval for referents, consistent with a framework in which referential elaboration over a discourse and not just local linguistic information directly impacts information retrieval during sentence processing.

Social image quality

NASA Astrophysics Data System (ADS)

Qiu, Guoping; Kheiri, Ahmed

2011-01-01

Current subjective image quality assessments have been developed in the laboratory environments, under controlledconditions, and are dependent on the participation of limited numbers of observers. In this research, with the help of Web 2.0 and social media technology, a new method for building a subjective image quality metric has been developed where the observers are the Internet users. A website with a simple user interface that enables Internet users from anywhere at any time to vote for a better quality version of a pair of the same image has been constructed. Users' votes are recorded and used to rank the images according to their perceived visual qualities. We have developed three rank aggregation algorithms to process the recorded pair comparison data, the first uses a naive approach, the second employs a Condorcet method, and the third uses the Dykstra's extension of Bradley-Terry method. The website has been collecting data for about three months and has accumulated over 10,000 votes at the time of writing this paper. Results show that the Internet and its allied technologies such as crowdsourcing offer a promising new paradigm for image and video quality assessment where hundreds of thousands of Internet users can contribute to building more robust image quality metrics. We have made Internet user generated social image quality (SIQ) data of a public image database available online (http://www.hdri.cs.nott.ac.uk/siq/) to provide the image quality research community with a new source of ground truth data. The website continues to collect votes and will include more public image databases and will also be extended to include videos to collect social video quality (SVQ) data. All data will be public available on the website in due course.

Proxy-to-proxy calibration: Increasing the temporal resolution of quantitative climate reconstructions

PubMed Central

von Gunten, Lucien; D'Andrea, William J.; Bradley, Raymond S.; Huang, Yongsong

2012-01-01

High-resolution paleoclimate reconstructions are often restricted by the difficulties of sampling geologic archives in great detail and the analytical costs of processing large numbers of samples. Using sediments from Lake Braya Sø, Greenland, we introduce a new method that provides a quantitative high-resolution paleoclimate record by combining measurements of the alkenone unsaturation index () with non-destructive scanning reflectance spectroscopic measurements in the visible range (VIS-RS). The proxy-to-proxy (PTP) method exploits two distinct calibrations: the in situ calibration of to lake water temperature and the calibration of scanning VIS-RS data to down core data. Using this approach, we produced a quantitative temperature record that is longer and has 5 times higher sampling resolution than the original time series, thereby allowing detection of temperature variability in frequency bands characteristic of the AMO over the past 7,000 years. PMID:22934132

Evaluation of a chemical proxy for fire intensity: A potential tool for studying fire-climate feedbacks

NASA Astrophysics Data System (ADS)

Hockaday, W. C.; White, J. D.; Von Bargen, J.; Yao, J.

2015-12-01

The legacy of wildfire is recorded in the geologic record, due to the stability of charcoal. Well-preserved charcoal is abundant in paleo-soils and sediments, documenting paleo-fires affecting even the earliest land plants. The dominant role of fire in shaping the biosphere is evidenced by some 40% of the land surface which is occupied by fire-prone and fire-adapted biomes: boreal forest, savanna, grassland, and Mediterranean shrubland. While fire ecologists appreciate the role that fire played in the evolution of these ecosystems, and climate scientists appreciate the role of these biomes in the regulation of Earth's climate, our understanding of the system of fire-vegetation-climate feedbacks is poor. This knowledge gap exists because we lack tools for evaluating change in fire regimes of the past for which climate proxy records exist. Fire regime is a function of fire frequency and fire intensity. Although fire frequency estimates are available from laminated sediment and tree ring records, tools for estimating paleo-fire intensity are lacking. We have recently developed a chemical proxy for fire intensity that is based upon the molecular structure of charcoal, assessed using solid-state nuclear magnetic resonance (NMR) spectroscopy. The molecular dimensions of aromatic domains in charcoal increased linearly (R2 = 0.9) with the intensity (temperature x duration) of heating. Our initial field-based validation in prescribed fires shows a promising correlation (R2 = 0.7) between the proxy-based estimates and thermistor-based measurements of fire intensity. This presentation will discuss the competencies and potential limitations of this novel proxy.

22 CFR 507.5 - Procedures for announcing meetings.

Code of Federal Regulations, 2014 CFR

2014-04-01

..., and the name and phone number of the official designated by the Board to respond to requests for... determine by a recorded vote that such meeting must be called at an earlier date, in which case the Board...

22 CFR 507.5 - Procedures for announcing meetings.

Code of Federal Regulations, 2012 CFR

2012-04-01

..., and the name and phone number of the official designated by the Board to respond to requests for... determine by a recorded vote that such meeting must be called at an earlier date, in which case the Board...

22 CFR 507.5 - Procedures for announcing meetings.

Code of Federal Regulations, 2013 CFR

2013-04-01

..., and the name and phone number of the official designated by the Board to respond to requests for... determine by a recorded vote that such meeting must be called at an earlier date, in which case the Board...

22 CFR 507.5 - Procedures for announcing meetings.

Code of Federal Regulations, 2011 CFR

2011-04-01

..., and the name and phone number of the official designated by the Board to respond to requests for... determine by a recorded vote that such meeting must be called at an earlier date, in which case the Board...

Raising a question of the privileges of the House.

THOMAS, 111th Congress

Rep. Cantor, Eric [R-VA-7

2010-03-18

House - 03/18/2010 On motion to table the measure Agreed to by recorded vote: 232 - 181 (Roll no. 132). (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Raising a question of the privileges of the House.

THOMAS, 111th Congress

Rep. Boehner, John A. [R-OH-8

2010-04-14

House - 04/14/2010 On motion to refer Agreed to by recorded vote: 235 - 157, 17 Present (Roll no. 202). (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Raising a question of the privileges of the House.

THOMAS, 111th Congress

Rep. Carter, John R. [R-TX-31

2009-10-07

House - 10/07/2009 On motion to refer Agreed to by recorded vote: 246 - 153, 19 Present (Roll No. 759). (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Estimating north pacific summer sea-level pressure back to 1600 using proxy climate records from China and North America

NASA Astrophysics Data System (ADS)

Wu, Xiangding; Lough, J. M.

1987-03-01

Sea-level pressure variations over the North Pacific Ocean influence the surface climate conditions of China and western North America. Documentary records of precipitation in China data back to the mid-15th century, and a well-replicated network of tree-ring chronologies from western North America dates to the early 17th century. These proxy climate records are used separately and together to estimate sea-level pressure variations over the North Pacific back to 1600 A.D. The models are calibrated over the period 1899 to 1950 and verified over the independent period, 1951 to 1963. The best estimates, derived from predictors in China and western North America, calibrate 44.7 % of summer sea-level pressure variance. The study demonstrates the potential of combining different proxy data sources to derive estimates of past climate.

Alpine Holocene Tree Ring Isotope Records - A Synthesis of a Multi-Proxy Approach in Dendroclimatology

NASA Astrophysics Data System (ADS)

Ziehmer, Malin Michelle; Nicolussi, Kurt; Schlüchter, Christian; Leuenberger, Markus

2017-04-01

High-resolution climate reconstructions based on tree-ring proxies are often limited by the individual segment length of living trees selected at the defined sampling sites, which mostly results in relatively short multi-centennial proxy series. A potential extension of living wood records comprise the addition of subfossil and archeological wood remains resulting in chronologies and associated climate reconstructions which are able to cover a few millennia in central Europe (e.g. Büntgen et al., 2011). However, existing multi-millennial tree-ring width chronologies in central Europe rank among the longest continuous chronologies world-wide and span the entire Holocene (Becker et al., 1993; Nicolussi et al. 2009). So far, these chronologies have mainly been used for dating subfossil wood samples, floating chronologies and archeological artifacts, but only in parts for reconstructing climate. Finds of Holocene wood remains in glacier forefields, peat bogs and small lakes allow us not only to establish such long-term tree-ring width records; further they offer the possibility to establish multi-millennial proxy records for the entire Holocene by using a multi-proxy approach which includes both tree-ring width and triple stable isotope ratios. As temperature limits tree growth at the Alpine upper tree line, the existing tree-ring width records are currently limited to reconstruct a single environmental variable. In the framework of the project Alpine Holocene Tree Ring Isotope Records, we combine tree-ring width, cellulose content as well as carbon, oxygen and hydrogen isotope series in a multi-proxy approach which allows the reconstruction of past environments by combining both Holocene wood remains and recent tree samples from two Alpine tree-line species. For this purpose, α-cellulose is prepared from 5-year tree ring blocks following the procedure after Boettger et al. (2007) and subsequently crushed by ultrasonic homogenization (Laumer et al., 2009). The cellulose content is determined for each individual sample and carbon, oxygen and hydrogen isotopic ratios are measured simultaneously (Loader et al., 2015). The isotope records of carbon, oxygen and hydrogen show distinct low-frequency trends for the Early- and Mid-Holocene, but the individual series per proxy are often offset in their isotopic signature. As the sampling sites in our study are distributed along a SW-NE transect, the influence of the site conditions (latitude, longitude, elevation, exposition) and the tree species is tested and subsequently a correction is applied to the individual series. In addition, the tree-ring width records operate as a helpful tool in detecting and attributing the influence of larch budmoth outbreaks on the cellulose content and isotope records. We here present a synthesis of the applied multi-proxy approach and its ability to reconstruct Holocene climate variability for the time span from 9000 to 3500 years b2k covering the Early-Holocene (9000 to 7200 years b2k) and Mid-Holocene (7200 to 4200 years b2k) and the transition to the late Holocene (4200 to 3500 years b2k) as well as the recent 400 years including the modern warming. References Becker, B., & Kromer, B. Palaeogeogr. Palaeoclimatol. Palaeoecol., 1993, 103(1): 67-71 Boettger, T., et al. Anal. Chem., 2007, 79: 4603-4612 Büntgen, U. et al. Science, 2011, 331(6017): 578-582 Laumer, W., et al. Rapid Commun. Mass Spectrom., 2009, 23: 1934-1940 Loader, N.J., et al. Anal. Chem., 2015, 87: 376-380 Nicolussi K., et al. The Holocene, 2009, 19(6): 909-920

Impeaching G. Thomas Porteous, Jr., judge of the United States District Court for the Eastern District of Louisiana, for high crimes and misdemeanors.

THOMAS, 111th Congress

Rep. Conyers, John, Jr. [D-MI-14

2010-01-21

Senate - 12/08/2010 The motion to forever disqualify G. Thomas Porteous, Jr. to hold and enjoy any office of honor, trust, or profit under the United States agreed to by Yea-Nay Vote. 94 - 2. Record Vote Number: 265. (All Actions) Notes: Note: On 3/11/2010, the House agreed to the resolution of impeachment. On 12/8/2010, the Senate adjudged G. Thomas Porteous, Jr., guilty as charged in the four Articles of the Impeachment. Tracker: This bill has the status Agreed to in HouseHere are the steps for Status of Legislation:

A High-Resolution Record of Warm Water Inflow and Iceberg Calving in Upernavik Isfjord During the Past 150 Years.

NASA Astrophysics Data System (ADS)

Vermassen, F.; Andresen, C. S.; Sabine, S.; Holtvoeth, J.; Cordua, A. E.; Wangner, D. J.; Dyke, L. M.; Kjaer, K. H.; Kokfelt, U.; Haubner, K.

2016-12-01

There is a growing body of evidence demonstrating that changes in warm water inflow to Greenlandic fjords are linked to the rapid retreat of marine-terminating outlet glaciers. This process is thought to be responsible for a substantial component of the increased mass loss from the Greenland Ice Sheet over the last two decades. Sediment cores from glaciated fjords provide high-resolution sedimentological and biological proxy records which can be used to evaluate the interplay of warm water inflow and glacier calving over recent time scales. In this study, multiple short cores ( 2 m) from Upernavik Isfjord, West Greenland, were analysed to establish a multi-proxy record of glacier behaviour and oceanographic conditions that spans the past 150 years. The down-core variation in the amount of ice-rafted debris reveals periods of increased glacier calving, and biomarker proxies are used to reconstruct variability in the inflow of warm, Atlantic-sourced water to the fjord. Measurements of the sortable silt grain size are used to reconstruct bottom-current strength; periods of vigorous current flow are assumed to be due to enhanced warm water inflow. Finally, a record of glacier terminus position changes, derived from historical observations and satellite imagery, allows comparison of our new proxy records with the retreat of the ice margin from 1849 onwards. We use these data to assess the relative importance of mechanisms controlling the (rapid) retreat of marine-terminating glaciers in Upernavik Isfjord.

Glacial-Interglacial, Orbital and Millennial-Scale Climate Variability for the Last Glacial Cycle at Shackleton Site U1385 based on Dinoflagellate Cysts

NASA Astrophysics Data System (ADS)

Datema, M.

2015-12-01

The Shackleton Site (IODP Expedition 339 Site U1385), located off the West-Portuguese Margin, preserves a continuous high-fidelity record of millennial-scale climate variability for the last several glacial cycles (~1.4 Myr) that can be correlated precisely to patterns observed in polar ice cores. In addition, rapid delivery of terrestrial material to the deep-sea environment allows the correlation of these marine records to European terrestrial climate records. This unique marine-ice-terrestrial linkage makes the Shackleton Site the ideal reference section for studying Quaternary abrupt climate change. The main objective of studying Site U1385 is to establish a marine reference section of Pleistocene climate change. We generated (sub)millennial-scale (~600 year interval) dinoflagellate cyst (dinocyst) assemblage records from Shackleton Site U1385 (IODP Expedition 339) to reconstruct sea surface temperature (SST) and productivity/upwelling over the last 152 kyrs. In addition, our approach allows for detailed land-sea correlations, because we also counted assemblages of pollen and spores from higher plants. Dinocyst SST and upwelling proxies, as well as warm/cold pollen proxies from Site U1385 show glacial-interglacial, orbital and stadial-interstadial climate variability and correlate very well to Uk'37, planktic foraminifer δ18O and Ca/Ti proxies of previously drilled Shackleton Sites and Greenland Ice Core δ18O. The palynological proxies capture (almost) all Dansgaard-Oeschger events of the last glacial cycle, also before ~70 ka, where millennial-scale variability is overprinted by precession. We compare the performance and results of the palynology of Site U1385 to proxies of previously drilled Shackleton Sites and conclude that palynology strengthens the potential of this site to form a multi-proxy reference section for millennial scale climate variability across the Pleistocene-Holocene. Finally, we will present a long-term paleoceanographic perspective down to ~150 ka.

Possible causes of data model discrepancy in the temperature history of the last Millennium.

PubMed

Neukom, Raphael; Schurer, Andrew P; Steiger, Nathan J; Hegerl, Gabriele C

2018-05-15

Model simulations and proxy-based reconstructions are the main tools for quantifying pre-instrumental climate variations. For some metrics such as Northern Hemisphere mean temperatures, there is remarkable agreement between models and reconstructions. For other diagnostics, such as the regional response to volcanic eruptions, or hemispheric temperature differences, substantial disagreements between data and models have been reported. Here, we assess the potential sources of these discrepancies by comparing 1000-year hemispheric temperature reconstructions based on real-world paleoclimate proxies with climate-model-based pseudoproxies. These pseudoproxy experiments (PPE) indicate that noise inherent in proxy records and the unequal spatial distribution of proxy data are the key factors in explaining the data-model differences. For example, lower inter-hemispheric correlations in reconstructions can be fully accounted for by these factors in the PPE. Noise and data sampling also partly explain the reduced amplitude of the response to external forcing in reconstructions compared to models. For other metrics, such as inter-hemispheric differences, some, although reduced, discrepancy remains. Our results suggest that improving proxy data quality and spatial coverage is the key factor to increase the quality of future climate reconstructions, while the total number of proxy records and reconstruction methodology play a smaller role.

Comparison of Geochemical, Grain-Size, and Magnetic Proxies for Rock Flour and Ice- Rafted Debris in the Late Pleistocene Mono Basin, CA

NASA Astrophysics Data System (ADS)

Zimmerman, S. H.; Hemming, S. R.; Kent, D. V.

2008-12-01

Advance and retreat of mountain glaciers are important indicators of climate variability, but the most direct proxy record, mapping and dating of moraines, is by nature discontinous. The Sierra Nevada form the western boundary of the Mono Lake basin, and the proximity of the large Pleistocene lake to the glacial canyons of the Sierra presents a rare opportunity to examine glacial variability in a continuous, well-dated lacustrine sequence. We have applied a geochemical proxy for rock flour to the glacial silts of the late Pleistocene Wilson Creek Formation, but because it is time- and sample-intensive, another method is required for a high-resolution record. Previous microscopic examination, thermomagnetic measurements, XRD analysis, and new isothermal remnant magnetization (IRM) acquisition curves show that the magnetic mineralogy is dominated by fine-grained, unaltered magnetite. Bulk measurements show strong susceptibility (mean ~ 16 x 10- 6 m3/kg) and remanent magnetization (mean IRM ~ 10-2 Am2/kg) compared to diluting components (carbonate, smectite, rhyolitic ash). The Wilson Creek type section sediments also contain a coarse lithic fraction, quantified by counting the >2cm clasts in outcrop and the >425 μm fraction in the bulk sediment. Susceptibility, IRM, and ARM (anhysteretic remnant magnetization) are quite similar throughout the type section, with the abundance of coarse lithic fraction correlative to the ratio k/IRM. Because the magnetic fraction of the rock flour is fine-grained magnetite, IRM should capture the changes in concentration of flour through time, and the major features of the (low-resolution) geochemical flour proxy record are identifiable in the IRM record. Flux-correction of the IRM results in a rock flour proxy record with major peaks between 36 and 48 ka, similar to a rock flour record from neighboring Owens Lake. This regional glacial signal contrasts with peaks in coarse lithics between 58 and 68 ka in the Wilson Creek record; coupled with coeval high lake levels and a lack of geomorphic evidence of glacier-lake interaction, this is taken to indicate that the rafting was due to shore ice, rather than glacial icebergs.

A composite pollen-based stratotype for inter-regional evaluation of climatic events in New Zealand over the past 30,000 years (NZ-INTIMATE project)

NASA Astrophysics Data System (ADS)

Barrell, David J. A.; Almond, Peter C.; Vandergoes, Marcus J.; Lowe, David J.; Newnham, Rewi M.

2013-08-01

Our review of paleoclimate information for New Zealand pertaining to the past 30,000 years has identified a general sequence of climatic events, spanning the onset of cold conditions marking the final phase of the Last Glaciation, through to the emergence to full interglacial conditions in the early Holocene. In order to facilitate more detailed assessments of climate variability and any leads or lags in the timing of climate changes across the region, a composite stratotype is proposed for New Zealand. The stratotype is based on terrestrial stratigraphic records and is intended to provide a standard reference for the intercomparison and evaluation of climate proxy records. We nominate a specific stratigraphic type record for each climatic event, using either natural exposure or drill core stratigraphic sections. Type records were selected on the basis of having very good numerical age control and a clear proxy record. In all cases the main proxy of the type record is subfossil pollen. The type record for the period from ca 30 to ca 18 calendar kiloyears BP (cal. ka BP) is designated in lake-bed sediments from a small morainic kettle lake (Galway tarn) in western South Island. The Galway tarn type record spans a period of full glacial conditions (Last Glacial Coldest Period, LGCP) within the Otira Glaciation, and includes three cold stadials separated by two cool interstadials. The type record for the emergence from glacial conditions following the termination of the Last Glaciation (post-Termination amelioration) is in a core of lake sediments from a maar (Pukaki volcanic crater) in Auckland, northern North Island, and spans from ca 18 to 15.64 ± 0.41 cal. ka BP. The type record for the Lateglacial period is an exposure of interbedded peat and mud at montane Kaipo bog, eastern North Island. In this high-resolution type record, an initial mild period was succeeded at 13.74 ± 0.13 cal. ka BP by a cooler period, which after 12.55 ± 0.14 cal. ka BP gave way to a progressive ascent to full interglacial conditions that were achieved by 11.88 ± 0.18 cal. ka BP. Although a type section is not formally designated for the Holocene Interglacial (11.88 ± 0.18 cal. ka BP to the present day), the sedimentary record of Lake Maratoto on the Waikato lowlands, northwestern North Island, is identified as a prospective type section pending the integration and updating of existing stratigraphic and proxy datasets, and age models. The type records are interconnected by one or more dated tephra layers, the ages of which are derived from Bayesian depositional modelling and OxCal-based calibrations using the IntCal09 dataset. Along with the type sections and the Lake Maratoto record, important, well-dated terrestrial reference records are provided for each climate event. Climate proxies from these reference records include pollen flora, stable isotopes from speleothems, beetle and chironomid fauna, and glacier moraines. The regional composite stratotype provides a benchmark against which to compare other records and proxies. Based on the composite stratotype, we provide an updated climate event stratigraphic classification for the New Zealand region. The stratotype and event classification are not intended to act as definitive statements of paleoclimate history for the New Zealand region, but rather provide a firm baseline against which to compare other records including those from the marine realm.

Growth rates and geochemical proxies in Late Campanian bivalves - New insights from micro-X-ray Fluorescence mapping and numerical growth modelling

NASA Astrophysics Data System (ADS)

de Winter, Niels; Goderis, Steven; van Malderen, Stijn; Vanhaecke, Frank; Claeys, Philippe

2017-04-01

Understanding the Late Cretaceous greenhouse climate is of vital importance for understanding present and future climate change. While a lot of good work has been done to reconstruct climate in this interesting period, most paleoclimatic studies have focused on long-term climate change[1]. Alternatively, multi-proxy records from marine bivalves provide us with a unique opportunity to study past climate on a seasonal scale. However, previous fossil bivalve studies have reported ambiguous results with regard to the interpretation of trace element and stable isotope proxies in marine bivalve shells[2]. One major problem in the interpretation of such records is the bivalve's vital effect and the occurrence of disequilibrium fractionation during bivalve growth. Both these problems are linked to the annual growth cycle of marine bivalves, which introduces internal effects on the incorporation of isotopes and trace elements into the shell[3]. Understanding this growth cycle in extinct bivalves is therefore of great importance for the interpretation of seasonal proxy records in their shells. In this study, three different species of extinct Late Campanian bivalves (two rudist species and one oyster species) that were found in the same stratigraphic interval are studied. Micro-X-Ray Fluorescence line scanning and mapping of trace elements such as Mg, Sr, S and Zn, calibrated by LA-ICP-MS measurements, is combined with microdrilled stable carbon and oxygen isotope analysis on the well-preserved part of the shells. Data of this multi-proxy study is compared with results from a numerical growth model written in the open-source statistics package R[4] and based on annual growth increments observed in the shells and shell thickness. This growth model is used together with proxy data to reconstruct rates of trace element incorporation into the shell and to calculate the mass balance of stable oxygen and carbon isotopes. In order to achieve this goal, 2D mapping of bivalve shell surfaces is combined with high-precision point measurements and linescans to characterize different carbonate facies within the shell and to model changes in proxy data in three dimensions. Comparison of sub-annual variations in growth rate and shell geometry with proxy data sheds light on the degree to which observed seasonal variations in geochemical proxies are dependent on internal mechanisms of shell growth as opposed to external mechanisms such as climatic and environmental change. The use of three different species of bivalve from the same paleoenvironment allows the examination of species-specific responses to environmental change. This study attempts to determine which proxies in which species of bivalve are suitable for paleoenvironmental reconstruction and will aid future paleoseasonality studies in interpreting seasonally resolved multi-proxy records. References 1 DeConto R.M., et al. Cambridge University Press; 2000. 2 Elliot M, et al., PPP 2009. 3 Steuber T. Geology. 1996. 4 R core team, 2004, www.R-project.org

76 FR 10070 - Record of Vote of Meeting Closure (Pub. L. 94-409) (5 U.S.C. Sec. 552b)

Federal Register 2010, 2011, 2012, 2013, 2014

2011-02-23

.... 94-409) (5 U.S.C. Sec. 552b) I, Isaac Fulwood, of the United States Parole Commission, was present at... be closed: Isaac Fulwood, Cranston J. Mitchell, Patricia Cushwa and J. Patricia Wilson Smoot. In... record to be made available to the public. Dated: February 11, 2011. Isaac Fulwood, Chairman, U.S. Parole...

76 FR 39128 - Record of Vote of Meeting Closure (Pub. L. 94-409) (5 U.S.C. 552b)

Federal Register 2010, 2011, 2012, 2013, 2014

2011-07-05

.... 94-409) (5 U.S.C. 552b) I, Isaac Fulwood, of the United States Parole Commission, was present at a... that the meeting be closed: Isaac Fulwood, Cranston J. Mitchell, Patricia Cushwa and J. Patricia Wilson... authorize this record to be made available to the public. Dated: June 21, 2011. Isaac Fulwood, Chairman, U.S...

22 CFR 1004.5 - Procedures for announcing meetings.

Code of Federal Regulations, 2014 CFR

2014-04-01

... of the meeting, whether it is to be open or closed to the public, and the name and phone number of... announcement shall be made unless a majority of the Board of Directors of the IAF determines by a recorded vote...

22 CFR 1004.5 - Procedures for announcing meetings.

Code of Federal Regulations, 2011 CFR

2011-04-01

... of the meeting, whether it is to be open or closed to the public, and the name and phone number of... announcement shall be made unless a majority of the Board of Directors of the IAF determines by a recorded vote...

22 CFR 1004.5 - Procedures for announcing meetings.

Code of Federal Regulations, 2012 CFR

2012-04-01

... of the meeting, whether it is to be open or closed to the public, and the name and phone number of... announcement shall be made unless a majority of the Board of Directors of the IAF determines by a recorded vote...

Raising a question of the privileges of the House.

THOMAS, 111th Congress

Rep. Flake, Jeff [R-AZ-6

2009-02-25

House - 02/25/2009 On motion to table the measure Agreed to by recorded vote: 226 - 182, 12 Present (Roll no. 87). (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

22 CFR 225.115 - IRB records.

Code of Federal Regulations, 2011 CFR

2011-04-01

..., including the following: (1) Copies of all research proposals reviewed, scientific evaluations, if any, that accompany the proposals, approved sample consent documents, progress reports submitted by investigators, and... members voting for, against, and abstaining; the basis for requiring changes in or disapproving research...

Raising a question of the privileges of the House.

THOMAS, 113th Congress

Rep. Kildee, Daniel T. [D-MI-5

2014-03-13

House - 03/13/2014 On motion to table the measure Agreed to by recorded vote: 217 - 173, 10 Present (Roll no. 133). (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Raising a question of the privileges of the House.

THOMAS, 111th Congress

Rep. Flake, Jeff [R-AZ-6

2009-03-05

House - 03/05/2009 On motion to table the measure Agreed to by recorded vote: 222 - 181, 14 Present (Roll no. 105). (All Actions) Tracker: This bill has the status IntroducedHere are the steps for Status of Legislation:

Tobacco Industry Influences in the Oklahoma Legislature.

PubMed

Matheny, James D; Wagener, Theodore L; Anderson, Michael P

2015-11-01

To identify recent tobacco industry influences in the Oklahoma Legislature. Relevant public records were compiled and published online in searchable databases. Activities related to two contested tobacco-related legislative initiatives were analyzed. Analyses of voting behavior controlled for party affiliation. Legislators receiving the largest amounts of campaign contributions and gifts from tobacco lobbyists performed actions necessary to advance tobacco industry objectives. Several significant associations with voting behavior were observed, the strongest of which was between votes on a pro-tobacco industry bill and gifts from tobacco lobbyists. Most lobbyists'gifts were meals. Tobacco industry influence in the Oklahoma Legislature is enhanced through tobacco lobbyists' campaign contributions and gifts. Greater investments are made in legislative leaders, those serving as champions or spokespersons, and others taking key roles in advancing tobacco industry objectives. Exposing such influences may diminish their effects. Given the egregious and uniquely destructive behavior of the tobacco industry, lawmakers could, as an ethical matter of principle, refuse tobacco lobbyists' money and seek to remedy past harms.

Does Internet voting make elections less social? Group voting patterns in Estonian e-voting log files (2013–2015)

PubMed Central

2017-01-01

Remote Internet voting places the control and secrecy of the immediate voting environment on the shoulder of the individual voter but it also turns voting into yet another on-line activity thus endangering the well-known social nature of voting and possibly reducing the crucial sense of civic duty that is important for a healthy democracy. There is however a complete lack of evidence to what degree this actually materializes once electronic voting is introduced. This paper uses individual level log data on Internet voting in Estonian elections between 2013–2015 to inspect if Internet voting retains the social nature of the voting act. We do so by examining if Internet voting in groups takes place and what implications it has for voting speed. We find strong evidence of e-voting in pairs. Same aged male-female pairs seem to be voting in close proximity to each other, consistent with spouses or partners voting together. Also, female-female and female-male pairs with large age differences seem to be voting together, consistent with a parent voting with an adult aged offspring. With regards to voting speed we see the second vote in a vote pair being considerably faster than the first vote, again indicating a shared voting act. We end with a discussion of how the onset of electronic voting does not make elections less social, but does make vote secrecy more a choice rather than a requirement. PMID:28542348

Defense.gov - Special Report: VOTE

Science.gov Websites

Voting Action Plan (pdf) 2013 USMC Voting Action Plan (pdf) 2013 Army Voting Action Plan (pdf) Air Force Voting Plan 2012-13 (pdf) Army Voting Action Plan 2012 (pdf) Marine Corps Voting Action Plan 2012 (pdf ) Navy Voting Action Plan (pdf) Overseas Vote Foundation Project Vote Smart Preparing for the 2012

A review of sea ice proxy information from polar ice cores

NASA Astrophysics Data System (ADS)

Abram, Nerilie J.; Wolff, Eric W.; Curran, Mark A. J.

2013-11-01

Sea ice plays an important role in Earth's climate system. The lack of direct indications of past sea ice coverage, however, means that there is limited knowledge of the sensitivity and rate at which sea ice dynamics are involved in amplifying climate changes. As such, there is a need to develop new proxy records for reconstructing past sea ice conditions. Here we review the advances that have been made in using chemical tracers preserved in ice cores to determine past changes in sea ice cover around Antarctica. Ice core records of sea salt concentration show promise for revealing patterns of sea ice extent particularly over glacial-interglacial time scales. In the coldest climates, however, the sea salt signal appears to lose sensitivity and further work is required to determine how this proxy can be developed into a quantitative sea ice indicator. Methane sulphonic acid (MSA) in near-coastal ice cores has been used to reconstruct quantified changes and interannual variability in sea ice extent over shorter time scales spanning the last ˜160 years, and has potential to be extended to produce records of Antarctic sea ice changes throughout the Holocene. However the MSA ice core proxy also requires careful site assessment and interpretation alongside other palaeoclimate indicators to ensure reconstructions are not biased by non-sea ice factors, and we summarise some recommended strategies for the further development of sea ice histories from ice core MSA. For both proxies the limited information about the production and transfer of chemical markers from the sea ice zone to the Antarctic ice sheets remains an issue that requires further multidisciplinary study. Despite some exploratory and statistical work, the application of either proxy as an indicator of sea ice change in the Arctic also remains largely unknown. As information about these new ice core proxies builds, so too does the potential to develop a more comprehensive understanding of past changes in sea ice and its role in both long and short-term climate changes.

Expression of Aleutian Low variations by a proxy record of precipitation oxygen isotopes in the Matanuska-Susitna region on Cook Inlet, south central Alaska

NASA Astrophysics Data System (ADS)

Finney, B.; Anderson, L.; Engstrom, D. R.

2017-12-01

North Pacific ocean-atmosphere processes strongly influence the climatology of Alaska by altering the strength and position of the Aleutian Low. During the past decade, the development of oxygen isotope proxy records that reflect the isotope composition of precipitation has provided substantial evidence of hydroclimatic variability in Alaska in response to Aleutian Low variations during the Holocene. However, a clear understanding of how the isotopic composition of precipitation reflects Aleutian Low variations remains uncertain because modern and proxy observations and modeling studies provide different predictions for regions (coastal and interior), elevations (0 to 5000 m), and time-scales (seasonal to century) that cannot be adequately tested by existing data. Precipitation isotope proxy records from Mount Logan, Denali, Jellybean Lake and Horse Trail Fen provide valuable perspectives at high elevation and interior (leeward) locations but no data has been available from near sea level on the coastal (windward) side of the Alaska and Chugach Mountain Ranges. Here we present newly recovered marl lake sediment cores from the Matanuska-Susitna region of Knik Arm on Cook Inlet, near Wasilla, 50 km north of Anchorage, AK that provide complete de-glacial and Holocene records of precipitation oxygen isotopes. Geochronology is underway based on identification of known tephras and AMS radiocarbon dating of terrestrial macrofossils. Modern and historic sediments are dated by 210Pb. The groundwater fed site is hydrologically open, unaffected by evaporation, has exceptionally high rates of marl sedimentation and preliminary results indicate clearly defined oxygen isotope excursions in the late 1970's and early 1940's, periods when North Pacific ocean-atmosphere forcing of the Aleutian Low is known to have undergone shifts. These results help to evaluate contrasting models of atmospheric circulation and associated isotope fractionation which is critical for proxy interpretation of paleo-records.

Aligning MIS5 proxy records from Lake Ohrid (FYROM) with independently dated Mediterranean archives: implications for core chronology

NASA Astrophysics Data System (ADS)

Zanchetta, G.; Regattieri, E.; Giaccio, B.; Wagner, B.; Sulpizio, R.; Francke, A.; Vogel, L. H.; Sadori, L.; Masi, A.; Sinopoli, G.; Lacey, J. H.; Leng, M. L.; Leicher, N.

2015-10-01

The DEEP site sediment sequence obtained during the ICDP SCOPSCO project at Lake Ohrid was dated using tephrostratigraphic information, cyclostratigraphy, and orbital tuning through marine isotope record. Although this approach is suitable for the generation of a general chronological framework of the long succession, it is insufficient to resolve more detailed paleoclimatological questions, such as leads and lags of climate events between marine and terrestrial records or between different regions. In this paper, we demonstrate how the use of different tie points can affect cyclostratigraphy and orbital tuning for the period between ca. 140 and 70 ka and how the results can be correlated with directly/indirectly radiometrically-dated Mediterranean marine and continental proxy records. The alternative age model obtained shows consistent differences with that proposed by Francke et al. (2015) for the same interval, in particular at the level of the MIS6-5e transition. According to this age model, different proxies from the DEEP site sediment record support an increase of temperatures between glacial to interglacial conditions, which is almost synchronous with a rapid increase in sea surface temperature observed in the western Mediterranean. The results show how important a detailed study of independent chronological tie points is for synchronizing different records and to highlight asynchronisms of climate events.

Constant Flux Proxies and Pleistocene Sediment Accumulation Rates on the Juan de Fuca Ridge in the Northeast Pacific

NASA Astrophysics Data System (ADS)

Middleton, J. L.; Mukhopadhyay, S.; Langmuir, C. H.; Costa, K.; McManus, J. F.; d'Almeida, M.; Huybers, P. J.; Winckler, G.

2016-12-01

Mass accumulation rates of marine sediments are often employed to constrain deposition rates of important proxies such as terrigenous dust, carbonate, and biogenic opal to quantitatively examine variations in continental aridity, atmospheric transport, and biologic productivity across changing climatic conditions. However, deposition rates that are estimated using traditional mass accumulation rates calculated from sediment core age models can be subject to bias from lateral sediment transport and limited age model resolution. Constant flux proxies, such as extraterrestrial helium-3 (3HeET) and excess thorium-230 (230ThXS), can be used to calculate vertical sediment accumulation rates that are independent of age model uncertainties and the effects of lateral sediment transport. While a short half-life limits analyses of 230ThXS to the past 500 ka, 3HeET is stable and could be used to constrain sedimentary fluxes during much of the Cenozoic. Despite the vast paleoceanographic potential of constant flux proxies, few studies have directly compared the behavior of 230ThXS and 3HeET using measurements from the same samples. Sediment grain size fractionation and local scavenging effects may differentially bias one or both proxy systems and complicate the interpretation of 230ThXS or 3HeET data. We will present a new record of vertical sediment accumulation rates spanning the past 600 ka in the Northeast Pacific constrained using analyses of both 3HeET and 230ThXS in two sediment cores from cruise AT26-19 on the Juan de Fuca Ridge. Such a record allows for intercomparison of both constant flux proxies in the mid-ocean ridge environment and examination of sedimentary behavior across multiple glacial cycles. The 230ThXS-derived accumulation rates typically range from 0.5 to 2 g cm-2 ka-1 over the past 450 ka, with periods of maximum deposition coinciding with glacial maxima. Preliminary results of samples analyzed with both 3HeET and 230ThXS indicate relative consistency between vertical sediment accumulation rates computed from each proxy and encourage the use of these constant flux proxies in other sedimentary records.

Using multi-resolution proxies to assess ENSO impacts on the mean state of the tropical Pacific.

NASA Astrophysics Data System (ADS)

Karamperidou, C.; Conroy, J. L.

2016-12-01

Observations and model simulations indicate that the relationship between ENSO and the mean state of the tropical Pacific is a two-way interaction. On one hand, a strong zonal SST gradient (dSST) in the Pacific (colder cold tongue) increases the potential intensity of upcoming ENSO events and may lead to increased ENSO variance. On the other hand, in a period of increased ENSO activity, large events can warm the cold tongue at decadal scales via residual heating, and thus lead to reduced zonal SST gradient (ENSO rectification mechanism). The short length of the observational record hinders our ability to confidently evaluate which mechanism dominates in each period, and whether it is sensitive to external climate forcing. This question is effectively a question of interaction between two timescales: interannual and decadal. Paleoclimate proxies of different resolutions can help elucidate this question, since they can be independent records of variability in these separate timescales. Here, we use coral proxies of ENSO variability from across the Pacific and multi-proxy records of dSST at longer timescales. Proxies, models, and observations indicate that in periods of increased ENSO activity, dSST is negatively correlated with ENSO variance at decadal timescales, indicating that strong ENSO events may affect the decadal mean state via warming the cold tongue. Using climate model simulations we attribute this effect to residual nonlinear dynamical heating, thus supporting the ENSO rectification mechanism. On the contrary, in periods without strong events, ENSO variance and dSST are positively correlated, which indicates that the primary mechanism at work is the effect of the mean state on ENSO. Our analysis also quantitatively identifies the regions where paleoclimate proxies are needed in order to reduce the existing uncertainties in ENSO-mean state interactions. Hence, this study is a synthesis of observations, model simulations and paleoclimate proxy evidence guided by the fundamental and open question of multi-scale interactions in the tropical Pacific, and illustrates the need for multi-resolution paleoclimate proxies and their potential uses.

A wind proxy based on migrating dunes at the Baltic coast: statistical analysis of the link between wind conditions and sand movement

NASA Astrophysics Data System (ADS)

Bierstedt, Svenja E.; Hünicke, Birgit; Zorita, Eduardo; Ludwig, Juliane

2017-07-01

We statistically analyse the relationship between the structure of migrating dunes in the southern Baltic and the driving wind conditions over the past 26 years, with the long-term aim of using migrating dunes as a proxy for past wind conditions at an interannual resolution. The present analysis is based on the dune record derived from geo-radar measurements by Ludwig et al. (2017). The dune system is located at the Baltic Sea coast of Poland and is migrating from west to east along the coast. The dunes present layers with different thicknesses that can be assigned to absolute dates at interannual timescales and put in relation to seasonal wind conditions. To statistically analyse this record and calibrate it as a wind proxy, we used a gridded regional meteorological reanalysis data set (coastDat2) covering recent decades. The identified link between the dune annual layers and wind conditions was additionally supported by the co-variability between dune layers and observed sea level variations in the southern Baltic Sea. We include precipitation and temperature into our analysis, in addition to wind, to learn more about the dependency between these three atmospheric factors and their common influence on the dune system. We set up a statistical linear model based on the correlation between the frequency of days with specific wind conditions in a given season and dune migration velocities derived for that season. To some extent, the dune records can be seen as analogous to tree-ring width records, and hence we use a proxy validation method usually applied in dendrochronology, cross-validation with the leave-one-out method, when the observational record is short. The revealed correlations between the wind record from the reanalysis and the wind record derived from the dune structure is in the range between 0.28 and 0.63, yielding similar statistical validation skill as dendroclimatological records.

Detecting oscillatory patterns and time lags from proxy records with non-uniform sampling: Some pitfalls and possible solutions

NASA Astrophysics Data System (ADS)

Donner, Reik

2013-04-01

Time series analysis offers a rich toolbox for deciphering information from high-resolution geological and geomorphological archives and linking the thus obtained results to distinct climate and environmental processes. Specifically, on various time-scales from inter-annual to multi-millenial, underlying driving forces exhibit more or less periodic oscillations, the detection of which in proxy records often allows linking them to specific mechanisms by which the corresponding drivers may have affected the archive under study. A persistent problem in geomorphology is that available records do not present a clear signal of the variability of environmental conditions, but exhibit considerable uncertainties of both the measured proxy variables and the associated age model. Particularly, time-scale uncertainty as well as the heterogeneity of sampling in the time domain are source of severe conceptual problems that may lead to false conclusions about the presence or absence of oscillatory patterns and their mutual phasing in different archives. In my presentation, I will discuss how one can cope with non-uniformly sampled proxy records to detect and quantify oscillatory patterns in one or more data sets. For this purpose, correlation analysis is reformulated using kernel estimates which are found superior to classical estimators based on interpolation or Fourier transform techniques. In order to characterize non-stationary or noisy periodicities and their relative phasing between different records, an extension of continuous wavelet transform is utilized. The performance of both methods is illustrated for different case studies. An extension to explicitly considering time-scale uncertainties by means of Bayesian techniques is briefly outlined.

Coral Records of 20th Century Central Tropical Pacific SST and Salinity: Signatures of Natural and Anthropogenic Climate Change

NASA Astrophysics Data System (ADS)

Nurhati, I. S.; Cobb, K.; Di Lorenzo, E.

2011-12-01

Accurate forecasts of regional climate changes in many regions of the world largely depend on quantifying anthropogenic trends in tropical Pacific climate against its rich background of interannual to decadal-scale climate variability. However, the strong natural climate variability combined with limited instrumental climate datasets have obscured potential anthropogenic climate signals in the region. Here, we present coral-based sea-surface temperature (SST) and salinity proxy records over the 20th century (1898-1998) from the central tropical Pacific - a region sensitive to El Niño-Southern Oscillation (ENSO) whose variability strongly impacts the global climate. The SST and salinity proxy records are reconstructed via coral Sr/Ca and the oxygen isotopic composition of seawater (δ18Osw), respectively. On interannual (2-7yr) timescales, the SST proxy record tracks both eastern- and central-Pacific flavors of ENSO variability (R=0.65 and R=0.67, respectively). Interannual-scale salinity variability in our coral record highlights profound differences in precipitation and ocean advections during the two flavors of ENSO. On decadal (8yr-lowpassed) timescales, the central tropical Pacific SST and salinity proxy records are controlled by different sets of dynamics linked to the leading climate modes of North Pacific climate variability. Decadal-scale central tropical Pacific SST is highly correlated to the recently discovered North Pacific Gyre Oscillation (NPGO; R=-0.85), reflecting strong dynamical links between the central Pacific warming mode and extratropical decadal climate variability. Whereas decadal-scale salinity variations in the central tropical Pacific are significantly correlated with the Pacific Decadal Oscillation (PDO; R=0.54), providing a better understanding on low-frequency salinity variability in the region. Having characterized natural climate variability in this region, the coral record shows a +0.5°C warming trend throughout the last century. However, the most prominent feature of the new coral records is an unprecedented freshening trend since the mid-20th century, in line with global climate models (GCMs) projections of enhanced hydrological patterns (wet areas are getting wetter and vice versa) under greenhouse forcing. Taken together, the coral records provide key constraints on tropical Pacific climate trends that may improve regional climate projections in areas affected by tropical Pacific climate variability.
Central Tropical Pacific SST and Salinity Proxy Records

Evidence of multidecadal climate variability and the Atlantic Multidecadal Oscillation from a Gulf of Mexico sea-surface temperature-proxy record

USGS Publications Warehouse

Poore, R.Z.; DeLong, K.L.; Richey, J.N.; Quinn, T.M.

2009-01-01

A comparison of a Mg/Ca-based sea-surface temperature (SST)-anomaly record from the northern Gulf of Mexico, a calculated index of variability in observed North Atlantic SST known as the Atlantic Multidecadal Oscillation (AMO), and a tree-ring reconstruction of the AMO contain similar patterns of variation over the last 110 years. Thus, the multidecadal variability observed in the instrumental record is present in the tree-ring and Mg/Ca proxy data. Frequency analysis of the Gulf of Mexico SST record and the tree-ring AMO reconstruction from 1550 to 1990 found similar multidecadal-scale periodicities (???30-60 years). This multidecadal periodicity is about half the observed (60-80 years) variability identified in the AMO for the 20th century. The historical records of hurricane landfalls reveal increased landfalls in the Gulf Coast region during time intervals when the AMO index is positive (warmer SST), and decreased landfalls when the AMO index is negative (cooler SST). Thus, we conclude that alternating intervals of high and low hurricane landfall occurrences may continue on multidecadal timescales along the northern Gulf Coast. However, given the short length of the instrumental record, the actual frequency and stability of the AMO are uncertain, and additional AMO proxy records are needed to establish the character of multidecadal-scale SST variability in the North Atlantic. ?? 2009 US Government.

A. Bernard Hatch.

ERIC Educational Resources Information Center

Executive Educator, 1984

1984-01-01

Bernard Hatch, the aggressive superintendent of schools in Dayton, Ohio, was voted out by the board of education despite an excellent record of accomplishments. His fate bodes ill for urban school districts in general, where those with the integrity and grit to do what is necessary often become unpopular. (TE)

49 CFR 11.115 - IRB records.

Code of Federal Regulations, 2011 CFR

2011-10-01

..., including the following: (1) Copies of all research proposals reviewed, scientific evaluations, if any, that... members voting for, against, and abstaining; the basis for requiring changes in or disapproving research... continuing review activities. (4) Copies of all correspondence between the IRB and the investigators. (5) A...

49 CFR 11.115 - IRB records.

Code of Federal Regulations, 2010 CFR

2010-10-01

..., including the following: (1) Copies of all research proposals reviewed, scientific evaluations, if any, that... members voting for, against, and abstaining; the basis for requiring changes in or disapproving research... continuing review activities. (4) Copies of all correspondence between the IRB and the investigators. (5) A...

7 CFR 1c.115 - IRB records.

Code of Federal Regulations, 2011 CFR

2011-01-01

..., including the following: (1) Copies of all research proposals reviewed, scientific evaluations, if any, that... members voting for, against, and abstaining; the basis for requiring changes in or disapproving research... continuing review activities. (4) Copies of all correspondence between the IRB and the investigators. (5) A...

45 CFR 2505.6 - What are the procedures for making a public announcement of a meeting?

Code of Federal Regulations, 2013 CFR

2013-10-01

... (a) of this section may be reduced only if— (1) The Board determines by recorded vote that Board... preceding, and the name and phone number of the official designated by the agency to respond to requests for...

On the construction of a time base and the elimination of averaging errors in proxy records

NASA Astrophysics Data System (ADS)

Beelaerts, V.; De Ridder, F.; Bauwens, M.; Schmitz, N.; Pintelon, R.

2009-04-01

Proxies are sources of climate information which are stored in natural archives (e.g. ice-cores, sediment layers on ocean floors and animals with calcareous marine skeletons). Measuring these proxies produces very short records and mostly involves sampling solid substrates, which is subject to the following two problems: Problem 1: Natural archives are equidistantly sampled at a distance grid along their accretion axis. Starting from these distance series, a time series needs to be constructed, as comparison of different data records is only meaningful on a time grid. The time series will be non-equidistant, as the accretion rate is non-constant. Problem 2: A typical example of sampling solid substrates is drilling. Because of the dimensions of the drill, the holes drilled will not be infinitesimally small. Consequently, samples are not taken at a point in distance, but rather over a volume in distance. This holds for most sampling methods in solid substrates. As a consequence, when the continuous proxy signal is sampled, it will be averaged over the volume of the sample, resulting in an underestimation of the amplitude. Whether this averaging effect is significant, depends on the volume of the sample and the variations of interest of the proxy signal. Starting from the measured signal, the continuous signal needs to be reconstructed in order eliminate these averaging errors. The aim is to provide an efficient identification algorithm to identify the non-linearities in the distance-time relationship, called time base distortions, and to correct for the averaging effects. Because this is a parametric method, an assumption about the proxy signal needs to be made: the proxy record on a time base is assumed to be harmonic, this is an obvious assumption because natural archives often exhibit a seasonal cycle. In a first approach the averaging effects are assumed to be in one direction only, i.e. the direction of the axis on which the measurements were performed. The measured averaged proxy signal is modeled by following signal model: -- Δ ∫ n+12Δδ- y(n,θ) = δ- 1Δ- y(m,θ)dm n-2 δ where m is the position, x(m) = Δm; θ are the unknown parameters and y(m,θ) is the proxy signal we want to identify (the proxy signal as found in the natural archive), which we model as: y(m, θ) = A +∑H [A sin(kωt(m ))+ A cos(kωt(m ))] 0 k=1 k k+H With t(m): t(m) = mTS + g(m )TS Here TS = 1/fS is the sampling period, fS the sampling frequency, and g(m) the unknown time base distortion (TBD). In this work a splines approximation of the TBD is chosen: ∑ g(m ) = b blφl(m ) l=1 where, b is a vector of unknown time base distortion parameters, and φ is a set of splines. The estimates of the unknown parameters were obtained with a nonlinear least squares algorithm. The vessel density measured in the mangrove tree R mucronata was used to illustrate the method. The vessel density is a proxy for the rain fall in tropical regions. The proxy data on the newly constructed time base showed a yearly periodicity, this is what we expected and the correction for the averaging effect increased the amplitude by 11.18%.

Marine sediment cores database for the Mediterranean Basin: a tool for past climatic and environmental studies

NASA Astrophysics Data System (ADS)

Alberico, I.; Giliberti, I.; Insinga, D. D.; Petrosino, P.; Vallefuoco, M.; Lirer, F.; Bonomo, S.; Cascella, A.; Anzalone, E.; Barra, R.; Marsella, E.; Ferraro, L.

2017-06-01

Paleoclimatic data are essential for fingerprinting the climate of the earth before the advent of modern recording instruments. They enable us to recognize past climatic events and predict future trends. Within this framework, a conceptual and logical model was drawn to physically implement a paleoclimatic database named WDB-Paleo that includes the paleoclimatic proxies data of marine sediment cores of the Mediterranean Basin. Twenty entities were defined to record four main categories of data: a) the features of oceanographic cruises and cores (metadata); b) the presence/absence of paleoclimatic proxies pulled from about 200 scientific papers; c) the quantitative analysis of planktonic and benthonic foraminifera, pollen, calcareous nannoplankton, magnetic susceptibility, stable isotopes, radionuclides values of about 14 cores recovered by Institute for Coastal Marine Environment (IAMC) of Italian National Research Council (CNR) in the framework of several past research projects; d) specific entities recording quantitative data on δ18O, AMS 14C (Accelerator Mass Spectrometry) and tephra layers available in scientific papers. Published data concerning paleoclimatic proxies in the Mediterranean Basin are recorded only for 400 out of 6000 cores retrieved in the area and they show a very irregular geographical distribution. Moreover, the data availability decreases when a constrained time interval is investigated or more than one proxy is required. We present three applications of WDB-Paleo for the Younger Dryas (YD) paleoclimatic event at Mediterranean scale and point out the potentiality of this tool for integrated stratigraphy studies.

Munchausen Syndrome by Proxy: A Family Affair.

ERIC Educational Resources Information Center

Mehl, Albert L.; And Others

1990-01-01

The article reports on a case of Munchausen syndrome by proxy in which chronic illicit insulin was administered to a one-year-old child by her mother. Factitious illnesses continued despite psychiatric intervention. Retrospective review of medical records suggested 30 previous episodes of factitious illness within the family. (DB)

Elaboration over a Discourse Facilitates Retrieval in Sentence Processing

PubMed Central

Troyer, Melissa; Hofmeister, Philip; Kutas, Marta

2016-01-01

Language comprehension requires access to stored knowledge and the ability to combine knowledge in new, meaningful ways. Previous work has shown that processing linguistically more complex expressions (‘Texas cattle rancher’ vs. ‘rancher’) leads to slow-downs in reading during initial processing, possibly reflecting effort in combining information. Conversely, when this information must subsequently be retrieved (as in filler-gap constructions), processing is facilitated for more complex expressions, possibly because more semantic cues are available during retrieval. To follow up on this hypothesis, we tested whether information distributed across a short discourse can similarly provide effective cues for retrieval. Participants read texts introducing two referents (e.g., two senators), one of whom was described in greater detail than the other (e.g., ‘The Democrat had voted for one of the senators, and the Republican had voted for the other, a man from Ohio who was running for president’). The final sentence (e.g., ‘The senator who the {Republican/Democrat}had voted for…’) contained a relative clause picking out either the Many-Cue referent (with ‘Republican’) or the One-Cue referent (with ‘Democrat’). We predicted facilitated retrieval (faster reading times) for the Many-Cue condition at the verb region (‘had voted for’), where readers could understand that ‘The senator’ is the object of the verb. As predicted, this pattern was observed at the retrieval region and continued throughout the rest of the sentence. Participants also completed the Author/Magazine Recognition Tests (ART/MRT; Stanovich and West, 1989), providing a proxy for world knowledge. Since higher ART/MRT scores may index (a) greater experience accessing relevant knowledge and/or (b) richer/more highly structured representations in semantic memory, we predicted it would be positively associated with effects of elaboration on retrieval. We did not observe the predicted interaction between ART/MRT scores and Cue condition at the retrieval region, though ART/MRT interacted with Cue condition in other locations in the sentence. In sum, we found that providing more elaborative information over the course of a text can facilitate retrieval for referents, consistent with a framework in which referential elaboration over a discourse and not just local linguistic information directly impacts information retrieval during sentence processing. PMID:27014172

Gulf of Mexico Climate-History Calibration Study

USGS Publications Warehouse

Spear, Jessica W.; Poore, Richard Z.

2010-01-01

Reliable instrumental records of past climate are available for about the last 150 years only. To supplement the instrumental record, reconstructions of past climate are made from natural recorders such as trees, ice, corals, and microfossils preserved in sediments. These proxy records provide information on the rate and magnitude of past climate variability, factors that are critical to distinguishing between natural and human-induced climate change in the present. However, the value of proxy records is heavily dependent on calibration between the chemistry of the natural recorder and of the modern environmental conditions. The Gulf of Mexico Climate and Environmental History Project is currently undertaking a climate-history calibration study with material collected from an automated sediment trap. The primary focus of the calibration study is to provide a better calibration of low-latitude environmental conditions and shell chemistry of calcareous microfossils, such as planktic Foraminifera.

A Tale of Two Lakes: Catchment-Specific Responses to Late Holocene Cooling in Northwest Iceland

NASA Astrophysics Data System (ADS)

Crump, S. E.; Florian, C. R.; Miller, G. H.; Geirsdottir, A.; Zalzal, K.

2015-12-01

Lake sediments are frequently utilized for reconstructing paleoclimate in the Arctic, particularly in Iceland, where high sedimentation rates and abundant tephra layers allow for the development high-resolution, well-dated records. However, when developing climate records using biological proxies, catchment-specific processes must be understood and separated from the primary climate signal in order to develop accurate reconstructions. In this study, we compare proxy records (biogenic silica [BSi], C:N, ∂13C, and algal pigments) of the last 2 ka from two nearby lakes in northwest Iceland in order to elucidate how different catchments respond to similar climate history. Torfdalsvatn and Bæjarvötn are two coastal lakes located 60 km apart; mean summer temperatures are highly correlated between the two sites over the instrumental record, and likely for the past 2 ka as well. Consistent with other Icelandic records, both lakes record cooling as decreasing aquatic productivity (BSi) over the last 2 ka. Both sediment cores also record the onset of landscape destabilization, reflected by increased terrestrial input (C:N and ∂13C), which suggests an intensification of cooling. However, the timing and magnitude of this shift differ markedly between lakes. Biological proxies indicate gradual landscape destabilization beginning ~900 AD at Torfdalsvatn in contrast to a sharper, more intense landscape destabilization at ~1400 AD at Bæjarvötn. Because temperatures at the two lakes are well correlated, contrasting proxy responses are likely the result of catchment-specific thresholds and processes. Specifically, a steeper catchment at Bæjarvötn may allow for a more pronounced influx of terrestrial material as the critical shear stress for soil erosion is surpassed more readily. The impact of human colonization on erosion rates is also critical to assess, and recent developments in lipid biomarkers will allow for more precise reconstructions of human activity in each catchment.

Fidelity of the Sr/Ca proxy in recording ocean temperature in the western Atlantic coral Siderastrea siderea

NASA Astrophysics Data System (ADS)

Kuffner, Ilsa B.; Roberts, Kelsey E.; Flannery, Jennifer A.; Morrison, Jennifer M.; Richey, Julie N.

2017-01-01

Massive corals provide a useful archive of environmental variability, but careful testing of geochemical proxies in corals is necessary to validate the relationship between each proxy and environmental parameter throughout the full range of conditions experienced by the recording organisms. Here we use samples from a coral-growth study to test the hypothesis that Sr/Ca in the coral Siderastrea siderea accurately records sea-surface temperature (SST) in the subtropics (Florida, USA) along 350 km of reef tract. We test calcification rate, measured via buoyant weight, and linear extension (LE) rate, estimated with Alizarin Red-S staining, as predictors of variance in the Sr/Ca records of 39 individual S. siderea corals grown at four outer-reef locations next to in-situ temperature loggers during two, year-long periods. We found that corals with calcification rates < 1.7 mg cm-2 d-1 or < 1.7 mm yr-1 LE returned spuriously high Sr/Ca values, leading to a cold-bias in Sr/Ca-based SST estimates. The threshold-type response curves suggest that extension rate can be used as a quality-control indicator during sample and drill-path selection when using long cores for SST paleoreconstruction. For our corals that passed this quality control step, the Sr/Ca-SST proxy performed well in estimating mean annual temperature across three sites spanning 350 km of the Florida reef tract. However, there was some evidence that extreme temperature stress in 2010 (cold snap) and 2011 (SST above coral-bleaching threshold) may have caused the corals not to record the temperature extremes. Known stress events could be avoided during modern calibrations of paleoproxies.