Pervasive ice sheet mass loss reflects competing ocean and atmosphere processes

Author:

Smith Ben1ORCID,Fricker Helen A.2ORCID,Gardner Alex S.3ORCID,Medley Brooke4ORCID,Nilsson Johan3ORCID,Paolo Fernando S.3ORCID,Holschuh Nicholas56ORCID,Adusumilli Susheel2ORCID,Brunt Kelly7ORCID,Csatho Bea8ORCID,Harbeck Kaitlin9ORCID,Markus Thorsten4ORCID,Neumann Thomas4ORCID,Siegfried Matthew R.10ORCID,Zwally H. Jay47ORCID

Affiliation:

1. Polar Science Center, Applied Physics Laboratory, University of Washington, Seattle, WA, USA.

2. Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA, USA.

3. Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, USA.

4. Cryospheric Science Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA.

5. Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA.

6. Department of Geology, Amherst College, Amherst, MA, USA.

7. Earth System Science Interdisciplinary Center, University of Maryland, College Park, MD, USA.

8. Department of Geological Sciences, University at Buffalo, Buffalo, NY, USA.

9. KBR, Greenbelt, MD, USA.

10. Department of Geophysics, Colorado School of Mines, Golden, CO, USA.

Abstract

Taking stock of our losses Earth's ice sheets are melting and sea levels are rising, so it behooves us to understand better which climate processes are responsible for how much of the mass loss. Smith et al. estimated grounded and floating ice mass change for the Greenland and Antarctic ice sheets from 2003 to 2019 using satellite laser altimetry data from NASA's ICESat and ICESat-2 satellites. They show how changing ice flow, melting, and precipitation affect different regions of ice and estimate that grounded-ice loss averaged close to 320 gigatons per year over that period and contributed 14 millimeters to sea level rise. Science , this issue p. 1239

Funder

National Aeronautics and Space Administration

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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