Increasing riverine heat influx triggers Arctic sea ice decline and oceanic and atmospheric warming-Reference-Cited by-同舟云学术

Increasing riverine heat influx triggers Arctic sea ice decline and oceanic and atmospheric warming

Published:2020-11-06 Issue:45 Volume:6 Page:
ISSN:2375-2548
Container-title:Science Advances
language:en
Short-container-title:Sci. Adv.

Author:

Park Hotaek¹²^ORCID,Watanabe Eiji¹^ORCID,Kim Youngwook³⁴^ORCID,Polyakov Igor⁵⁶^ORCID,Oshima Kazuhiro⁷^ORCID,Zhang Xiangdong⁸^ORCID,Kimball John S.³^ORCID,Yang Daqing⁹

Affiliation:

1. Institute of Arctic Climate and Environmental Research, JAMSTEC, Yokosuka, Japan.

2. Institute for Space-Earth Environmental Research, Nagoya University, Nagoya, Japan.

3. Numerical Terradynamic Simulation Group, WA Franke College of Forestry and Conservation, The University of Montana, Missoula, MT 59812, USA.

4. Department of Biology, College of Science United Arab Emirates University P.O. Box 15551, Al Ain, United Arab Emirates.

5. International Arctic Research Center and College of Natural Science and Mathematics, University of Alaska Fairbanks, 930 Koyukuk Drive, Fairbanks, AK, 99775, USA.

6. Finnish Meteorological Institute, Erik Palménin aukio 1, Helsinki, Finland.

7. Faculty of Software and Information Technology, Aomori University, Aomori, Japan.

8. International Arctic Research Center and Department of Atmospheric Sciences, University of Alaska Fairbanks, Fairbanks, AK 99775, USA.

9. Environment and Climate Change Canada, Victoria, Canada.

Abstract

Positive river heat–sea ice feedback doubles the river heat effect on declining Arctic sea ice.

Funder

U.S. Department of Energy

NSF Office of the Director

NASA

The Research Council of Norway

Scientific Research of Japan Society for the Promotion of Science