High sensitivity of Bering Sea winter sea ice to winter insolation and carbon dioxide over the last 5500 years

Author:

Jones Miriam C.1ORCID,Berkelhammer Max2ORCID,Keller Katherine J.13ORCID,Yoshimura Kei4ORCID,Wooller Matthew J.5ORCID

Affiliation:

1. Florence Bascom Geoscience Center, U.S. Geological Survey, Reston, VA 20192, USA.

2. Department of Earth and Environmental Sciences Chicago, University of Illinois at Chicago, Chicago, IL 60607, USA.

3. Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, USA.

4. Institute of Industrial Science, University of Tokyo, Tokyo, Japan.

5. Alaska Stable Isotope Facility, College of Fisheries and Ocean Sciences and Institute of Northern Engineering, University of Alaska Fairbanks, Fairbanks, AK 99775, USA.

Abstract

Anthropogenic CO 2 emissions and long-term winter insolation forcing drive Bering Sea ice extent to lowest in the last 5,500 years.

Funder

National Science Foundation

U.S. Geological Survey

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference50 articles.

1. F. Fetterer M. Savoie S. Helfrich P. Clemente-Colón Multisensor Analyzed Sea Ice Extent - Northern Hemisphere (MASIE-NH) Version 1 [Sea ice extent]. NSIDC: National Snow and Ice Data Center Boulder Colorado USA (2010); https://doi.org/10.7265/N5GT5K3K.

2. Observed Arctic sea-ice loss directly follows anthropogenic CO 2 emission

3. Return of warm conditions in the southeastern Bering Sea: Physics to fluorescence

4. D. G. Vaughan J.C. Comiso I. Allison J. Carrasco G. Kaser R. Kwok P. Mote T. Murray F. Paul J. Ren E. Rignot O. Solomina K. Steffen T. Zhang Observations: Crysophere in Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change T. F. Stocker D. Qin G.-K. Plattner M. Tignor S. K. Allen J. Boschung A. Nauels Y. Xia V. Bex P. M. Midgley Eds. (Cambridge Univ. Press Cambridge United Kingdom and New York NY USA 2013).

5. The Aleutian Low, storm tracks, and winter climate variability in the Bering Sea

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