Stronger ocean circulation and increased melting under Pine Island Glacier ice shelf
Glacier showed that the ice shelf buttressing the glacier was melting rapidly1. This melting was attributed to the presence of relatively warm, deep water on the Amundsen Sea continental shelf. Heat, salt and ice budgets along with ocean modelling provided steady-state calving and melting rates2,3....
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.470.7849 2023-05-15T13:23:59+02:00 Stronger ocean circulation and increased melting under Pine Island Glacier ice shelf Stanley S. Jacobs* Adrian Jenkins The Pennsylvania State University CiteSeerX Archives 2011 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.470.7849 http://xa.yimg.com/kq/groups/18383638/94278695/name/ngeo1188.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.470.7849 http://xa.yimg.com/kq/groups/18383638/94278695/name/ngeo1188.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://xa.yimg.com/kq/groups/18383638/94278695/name/ngeo1188.pdf text 2011 ftciteseerx 2016-01-08T07:16:26Z Glacier showed that the ice shelf buttressing the glacier was melting rapidly1. This melting was attributed to the presence of relatively warm, deep water on the Amundsen Sea continental shelf. Heat, salt and ice budgets along with ocean modelling provided steady-state calving and melting rates2,3. Subsequent satellite observations and modelling have indicated large system imbalances, including ice-shelf thinning and more intense melting, glacier acceleration and drainage basin drawdown4–10. Here we combine our earlier data with measurements taken in 2009 to show that the temperature and volume of deep water in Pine Island Bay have increased. Ocean transport and tracer calculations near the ice shelf reveal a rise in meltwater production by about 50 % since 1994. The faster melting seems to result mainly from stronger sub-ice-shelf circulation, as thinning ice has increased the gap Text Amundsen Sea Ice Shelf Pine Island Bay Pine Island Glacier Unknown Amundsen Sea Pine Island Glacier ENVELOPE(-101.000,-101.000,-75.000,-75.000) Island Bay ENVELOPE(-109.085,-109.085,59.534,59.534) Pine Island Bay ENVELOPE(-102.000,-102.000,-74.750,-74.750) |
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Open Polar |
collection |
Unknown |
op_collection_id |
ftciteseerx |
language |
English |
description |
Glacier showed that the ice shelf buttressing the glacier was melting rapidly1. This melting was attributed to the presence of relatively warm, deep water on the Amundsen Sea continental shelf. Heat, salt and ice budgets along with ocean modelling provided steady-state calving and melting rates2,3. Subsequent satellite observations and modelling have indicated large system imbalances, including ice-shelf thinning and more intense melting, glacier acceleration and drainage basin drawdown4–10. Here we combine our earlier data with measurements taken in 2009 to show that the temperature and volume of deep water in Pine Island Bay have increased. Ocean transport and tracer calculations near the ice shelf reveal a rise in meltwater production by about 50 % since 1994. The faster melting seems to result mainly from stronger sub-ice-shelf circulation, as thinning ice has increased the gap |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Stanley S. Jacobs* Adrian Jenkins |
spellingShingle |
Stanley S. Jacobs* Adrian Jenkins Stronger ocean circulation and increased melting under Pine Island Glacier ice shelf |
author_facet |
Stanley S. Jacobs* Adrian Jenkins |
author_sort |
Stanley S. Jacobs* Adrian Jenkins |
title |
Stronger ocean circulation and increased melting under Pine Island Glacier ice shelf |
title_short |
Stronger ocean circulation and increased melting under Pine Island Glacier ice shelf |
title_full |
Stronger ocean circulation and increased melting under Pine Island Glacier ice shelf |
title_fullStr |
Stronger ocean circulation and increased melting under Pine Island Glacier ice shelf |
title_full_unstemmed |
Stronger ocean circulation and increased melting under Pine Island Glacier ice shelf |
title_sort |
stronger ocean circulation and increased melting under pine island glacier ice shelf |
publishDate |
2011 |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.470.7849 http://xa.yimg.com/kq/groups/18383638/94278695/name/ngeo1188.pdf |
long_lat |
ENVELOPE(-101.000,-101.000,-75.000,-75.000) ENVELOPE(-109.085,-109.085,59.534,59.534) ENVELOPE(-102.000,-102.000,-74.750,-74.750) |
geographic |
Amundsen Sea Pine Island Glacier Island Bay Pine Island Bay |
geographic_facet |
Amundsen Sea Pine Island Glacier Island Bay Pine Island Bay |
genre |
Amundsen Sea Ice Shelf Pine Island Bay Pine Island Glacier |
genre_facet |
Amundsen Sea Ice Shelf Pine Island Bay Pine Island Glacier |
op_source |
http://xa.yimg.com/kq/groups/18383638/94278695/name/ngeo1188.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.470.7849 http://xa.yimg.com/kq/groups/18383638/94278695/name/ngeo1188.pdf |
op_rights |
Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
_version_ |
1766376800193085440 |