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Accelerating changes in ice mass within Greenland, and the ice sheet’s sensitivity to atmospheric forcing

Author(s): Bevis, Michael; Harig, Christopher; Khan, Shfaqat A; Brown, Abel; Simons, Frederik J; et al

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Abstract: From early 2003 to mid-2013, the total mass of ice in Greenland declined at a progressively increasing rate. In mid-2013, an abrupt reversal occurred, and very little net ice loss occurred in the next 12–18 months. Gravity Recovery and Climate Experiment (GRACE) and global positioning system (GPS) observations reveal that the spatial patterns of the sustained acceleration and the abrupt deceleration in mass loss are similar. The strongest accelerations tracked the phase of the North Atlantic Oscillation (NAO). The negative phase of the NAO enhances summertime warming and insolation while reducing snowfall, especially in west Greenland, driving surface mass balance (SMB) more negative, as illustrated using the regional climate model MAR. The spatial pattern of accelerating mass changes reflects the geography of NAO-driven shifts in atmospheric forcing and the ice sheet’s sensitivity to that forcing. We infer that southwest Greenland will become a major future contributor to sea level rise.
Publication Date: 5-Feb-2019
Citation: Bevis, Michael, Christopher Harig, Shfaqat A. Khan, Abel Brown, Frederik J. Simons, Michael Willis, Xavier Fettweis et al. "Accelerating changes in ice mass within Greenland, and the ice sheet’s sensitivity to atmospheric forcing." Proceedings of the National Academy of Sciences 116, no. 6 (2019): 1934-1939. doi:10.1073/pnas.1806562116.
DOI: doi:10.1073/pnas.1806562116
ISSN: 0027-8424
EISSN: 1091-6490
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Pages: 1934 - 1939
Language: eng
Type of Material: Journal Article
Journal/Proceeding Title: Proceedings of the National Academy of Sciences of the United States of America
Version: Final published version. This is an open access article.
Notes: Related Item links to supplemental information.

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