Growth of Greenland ice sheet - Interpretation
An observed 0.23 m/year thickening of the Greenland ice sheet indicates a 25 percent to 45 percent excess ice accumulation over the amount required to balance the outward ice flow. The implied global sea-level depletion is 0.2 to 0.4 mm/year, depending on whether the thickening is only recent (5 to...
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ftnasantrs:oai:casi.ntrs.nasa.gov:19900033212 2023-05-15T16:26:50+02:00 Growth of Greenland ice sheet - Interpretation Zwally, H. Jay Unclassified, Unlimited, Publicly available Dec 22, 1989 http://ntrs.nasa.gov/search.jsp?R=19900033212 unknown http://ntrs.nasa.gov/search.jsp?R=19900033212 Accession ID: 90A20267 Copyright Other Sources 46 Science; 246; 1589-159 1989 ftnasantrs 2012-02-15T18:25:16Z An observed 0.23 m/year thickening of the Greenland ice sheet indicates a 25 percent to 45 percent excess ice accumulation over the amount required to balance the outward ice flow. The implied global sea-level depletion is 0.2 to 0.4 mm/year, depending on whether the thickening is only recent (5 to 10 years) or longer term (less than 100 years). If there is a similar imbalance in the northern 60 percent of the ice-sheet area, the depletion is 0.35 to 0.7 mm/year. Increasing ice thickness suggests that the precipitation is higher than the long-term average; higher precipitation may be a characteristic of warmer climates in polar regions. Other/Unknown Material Greenland Ice Sheet NASA Technical Reports Server (NTRS) Greenland |
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Open Polar |
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NASA Technical Reports Server (NTRS) |
op_collection_id |
ftnasantrs |
language |
unknown |
topic |
46 |
spellingShingle |
46 Zwally, H. Jay Growth of Greenland ice sheet - Interpretation |
topic_facet |
46 |
description |
An observed 0.23 m/year thickening of the Greenland ice sheet indicates a 25 percent to 45 percent excess ice accumulation over the amount required to balance the outward ice flow. The implied global sea-level depletion is 0.2 to 0.4 mm/year, depending on whether the thickening is only recent (5 to 10 years) or longer term (less than 100 years). If there is a similar imbalance in the northern 60 percent of the ice-sheet area, the depletion is 0.35 to 0.7 mm/year. Increasing ice thickness suggests that the precipitation is higher than the long-term average; higher precipitation may be a characteristic of warmer climates in polar regions. |
format |
Other/Unknown Material |
author |
Zwally, H. Jay |
author_facet |
Zwally, H. Jay |
author_sort |
Zwally, H. Jay |
title |
Growth of Greenland ice sheet - Interpretation |
title_short |
Growth of Greenland ice sheet - Interpretation |
title_full |
Growth of Greenland ice sheet - Interpretation |
title_fullStr |
Growth of Greenland ice sheet - Interpretation |
title_full_unstemmed |
Growth of Greenland ice sheet - Interpretation |
title_sort |
growth of greenland ice sheet - interpretation |
publishDate |
1989 |
url |
http://ntrs.nasa.gov/search.jsp?R=19900033212 |
op_coverage |
Unclassified, Unlimited, Publicly available |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Ice Sheet |
genre_facet |
Greenland Ice Sheet |
op_source |
Other Sources |
op_relation |
http://ntrs.nasa.gov/search.jsp?R=19900033212 Accession ID: 90A20267 |
op_rights |
Copyright |
_version_ |
1766015839816908800 |