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Journal article

An aerial view of 80 years of climate-related glacier fluctuations in southeast Greenland

From

University of Copenhagen1

National Space Institute, Technical University of Denmark2

Geodesy, National Space Institute, Technical University of Denmark3

Geological Survey of Denmark and Greenland4

Ohio State University5

Aarhus University6

Widespread retreat of glaciers has been observed along the southeastern margin of Greenland. This retreat has been associated with increased air and ocean temperatures. However, most observations are from the satellite era; presatellite observations of Greenlandic glaciers are rare. Here we present a unique record that documents the frontal positions for 132 southeast Greenlandic glaciers from rediscovered historical aerial imagery beginning in the early 1930s.

We combine the historical aerial images with both early and modern satellite imagery to extract frontal variations of marine- and land-terminating outlet glaciers, as well as local glaciers and ice caps, over the past 80 years. The images reveal a regional response to external forcing regardless of glacier type, terminal environment and size.

Furthermore, the recent retreat was matched in its vigour during a period of warming in the 1930s with comparable increases in air temperature. We show that many land-terminating glaciers underwent a more rapid retreat in the 1930s than in the 2000s, whereas marine-terminating glaciers retreated more rapidly during the recent warming.

Both marine- and land-terminating glaciers in southeast Greenland have experienced dramatic recent retreat. An 80-year record of historical aerial photographs and satellite imagery shows that many land-terminating glaciers in this region retreated more rapidly in the 1930s than today, whereas marine-terminating glaciers have retreated faster in the 2000s.

Language: English
Publisher: Nature Publishing Group
Year: 2012
Pages: 427-432
ISSN: 17520908 and 17520894
Types: Journal article
DOI: 10.1038/NGEO1481
ORCIDs: Khan, Shfaqat Abbas , 0000-0002-4919-792X , 0000-0002-8871-5179 , 0000-0002-8700-7023 , 0000-0002-8557-5131 and 0000-0002-7636-0470

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