Surface-atmosphere decoupling limits accumulation at Summit, Greenland

Author:

Berkelhammer Max123,Noone David C.234,Steen-Larsen Hans Christian256,Bailey Adriana237ORCID,Cox Christopher J.238,O’Neill Michael S.28,Schneider David29,Steffen Konrad210ORCID,White James W. C.111213

Affiliation:

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

2. Cooperative Institute for Research in Environmental Sciences, University of Colorado, Boulder, CO 80309, USA.

3. Department of Atmospheric and Oceanic Sciences, University of Colorado, Boulder, CO 80309, USA.

4. College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA.

5. Laboratoire des Sciences du Climat et de l’Environnement, UMR CEA-CNRS-UVSQ/IPSL 8212, Gif-sur-Yvette, France.

6. Center for Ice and Climate, University of Copenhagen, Copenhagen, Denmark.

7. Joint Institute for the Study of the Atmosphere and Ocean, University of Washington, Seattle, WA 98195, USA.

8. National Oceanic and Atmospheric Administration, Boulder, CO 80305, USA.

9. National Center for Atmospheric Research, Boulder, CO 80305, USA.

10. Swiss Federal Research Institute WSL, Birmensdorf, Switzerland.

11. Department of Geological Sciences, University of Colorado, Boulder, CO 80309, USA.

12. Environmental Studies Program, University of Colorado, Boulder, CO 80309, USA.

13. Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO 80309, USA.

Abstract

The surface of the Greenland ice sheet becomes isolated from the atmosphere during the winter, which acts to conserve ice mass.

Funder

National Science Foundation

Danish Council for Independent Research

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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