West Antarctica's sensitivity to natural and human‐forced climate change over the Holocene-Reference-Cited by-同舟云学术

West Antarctica's sensitivity to natural and human‐forced climate change over the Holocene

Published:2012-12-14 Issue:1 Volume:28 Page:40-48
ISSN:0267-8179
Container-title:Journal of Quaternary Science
language:en
Short-container-title:J. Quaternary Sci.

Author:

Mayewski P. A.¹²,Maasch K. A.¹²,Dixon D.¹²,Sneed S. B.¹,Oglesby R.³,Korotkikh E.¹²,Potocki M.¹²,Grigholm B.¹²,Kreutz K.¹²,Kurbatov A. V.¹²,Spaulding N.¹²,Stager J. C.¹⁴,Taylor K. C.⁵,Steig E. J.⁶,White J.⁷,Bertler N. A. N.⁸,Goodwin I.⁹,Simões J. C.¹⁰,Jaña R.¹¹,Kraus S.¹²,Fastook J.¹¹³

Affiliation:

1. Climate Change Institute, University of Maine, Orono, ME, USA

2. Department of Earth Sciences, University of Maine, Orono, ME, USA

3. Department of Earth and Atmospheric Sciences and School of Natural Resources, University of Nebraska, Lincoln, NE, USA

4. Natural Sciences, Paul Smith's College, Paul Smiths, NY, USA

5. Desert Research Institute, University/Community College System Nevada, Reno, NV, USA

6. Quaternary Research Center, University of Washington, Seattle, WA, USA

7. Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO, USA

8. Joint Antarctic Institute, Victoria University and GNS Science, Wellington, New Zealand

9. Department of Environment and Geography, Macquarie University, NSW, Australia

10. Centro Polar e Climático, Universidade Federal do Rio Grande do Sul, Porto Alegre, Brazil

11. Instituto Antártico Chileno (INACH), Punta Arenas, Chile

12. Servicio Nacional de Geología y Minería (SERNAGEOMIN), Santiago, Chile

13. Department of Computer Sciences, University of Maine, Orono, ME, USA

Publisher

Wiley

Subject

Paleontology,Earth and Planetary Sciences (miscellaneous),Arts and Humanities (miscellaneous)

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.2593

Reference56 articles.

1. Mechanisms of Holocene palaeoenvironmental change in the Antarctic Peninsula region

2. Snow chemistry across Antarctica

3. Cold conditions in Antarctica during the Little Ice Age — Implications for abrupt climate change mechanisms

4. Asynchrony of Antarctic and Greenland climate change during the last glacial period

5. Timing of millennial-scale climate change at Siple Dome, West Antarctica, during the last glacial period

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