The Cryosphere
The extreme melt across the Greenland ice sheet in 2012
Article first published online: 27 OCT 2012
DOI: 10.1029/2012GL053611
©2012. American Geophysical Union. All Rights Reserved.
Additional Information
How to Cite
, , , , , , , , and (2012), The extreme melt across the Greenland ice sheet in 2012, Geophys. Res. Lett., 39, L20502, doi:10.1029/2012GL053611.
Publication History
- Issue published online: 27 OCT 2012
- Article first published online: 27 OCT 2012
- Manuscript Accepted: 26 SEP 2012
- Manuscript Revised: 25 SEP 2012
- Manuscript Received: 24 AUG 2012
- Abstract
- Article
- References
- Cited By
Keywords:
- Greenland ice sheet;
- Oceansat-2 scatterometer;
- Summit;
- extreme melt
[1] The discovery of the 2012 extreme melt event across almost the entire surface of the Greenland ice sheet is presented. Data from three different satellite sensors – including the Oceansat-2 scatterometer, the Moderate-resolution Imaging Spectroradiometer, and the Special Sensor Microwave Imager/Sounder – are combined to obtain composite melt maps, representing the most complete melt conditions detectable across the ice sheet. Satellite observations reveal that melt occurred at or near the surface of the Greenland ice sheet across 98.6% of its entire extent on 12 July 2012, including the usually cold polar areas at high altitudes like Summit in the dry snow facies of the ice sheet. This melt event coincided with an anomalous ridge of warm air that became stagnant over Greenland. As seen in melt occurrences from multiple ice core records at Summit reported in the published literature, such a melt event is rare with the last significant one occurring in 1889 and the next previous one around seven centuries earlier in the Medieval Warm Period. Given its rarity, the 2012 extreme melt across Greenland provides an exceptional opportunity for new studies in broad interdisciplinary geophysical research.

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