Global Glacier Mass Loss During the GRACE Satellite Mission (2002-2016)

Frontiers in Earth Science

Bert Wouters²  Alex S. Gardner³  Geir Moholdt⁴ 

[1] Department of Physics, Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, Netherlands;Faculty of Civil Engineering and Geosciences, Delft University of Technology, Delft, Netherlands;Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA, United States;Norwegian Polar Institute, Fram Centre, Tromsø, Norway;

关键词: GRACE;    glaciers;    ice caps;    sea level;    mass balance;   

DOI  :  10.3389/feart.2019.00096

来源: DOAJ

【 摘 要 】

Glaciers outside of the ice sheets are known to be important contributors to sea level rise. In this work, we provide an overview of changes in the mass of the world's glaciers, excluding those in Greenland and Antarctica, between 2002 and 2016, based on satellite gravimetry observations of the Gravity Recovery and Climate Experiment (GRACE). Glaciers lost mass at a rate of 199 ± 32 Gt yr−1 during this 14-yr period, equivalent to a cumulative sea level contribution of 8 mm. We present annual mass balances for 17 glacier regions, that show a qualitatively good agreement with published estimates from in situ observations. We find that annual mass balance varies considerably from year to year, which can in part be attributed to changes in the large-scale circulation of the atmosphere. These variations, combined with the relatively short observational record, hamper the detection of acceleration of glacier mass loss. Our study highlights the need for continued observations of the Earth's glacierized regions.

【 授权许可】

Unknown