Ice cores and SeaRISE: What we do (and don't) know
Ice core analyses are needed in SeaRISE to learn what the West Antarctic ice sheet and other marine ice sheets were like in the past, what climate changes led to their present states, and how they behave. The major results of interest to SeaRISE from previous ice core analyses in West Antarctic are...
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ftnasantrs:oai:casi.ntrs.nasa.gov:19910017265 2023-05-15T13:42:52+02:00 Ice cores and SeaRISE: What we do (and don't) know Alley, Richard B. Unclassified, Unlimited, Publicly available May 1, 1991 application/pdf http://hdl.handle.net/2060/19910017265 unknown Document ID: 19910017265 Accession ID: 91N26579 http://hdl.handle.net/2060/19910017265 No Copyright CASI OCEANOGRAPHY NASA. Goddard Space Flight Center, West Antarctic Ice Sheet Initiative. Volume 2: Discipline Reviews; p 111-130 1991 ftnasantrs 2015-03-15T05:16:45Z Ice core analyses are needed in SeaRISE to learn what the West Antarctic ice sheet and other marine ice sheets were like in the past, what climate changes led to their present states, and how they behave. The major results of interest to SeaRISE from previous ice core analyses in West Antarctic are that the end of the last ice age caused temperature and accumulation rate increases in inland regions, leading to ice sheet thickening followed by thinning to the present. Other/Unknown Material Antarc* Antarctic ice core Ice Sheet NASA Technical Reports Server (NTRS) Antarctic West Antarctic Ice Sheet |
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Open Polar |
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NASA Technical Reports Server (NTRS) |
op_collection_id |
ftnasantrs |
language |
unknown |
topic |
OCEANOGRAPHY |
spellingShingle |
OCEANOGRAPHY Alley, Richard B. Ice cores and SeaRISE: What we do (and don't) know |
topic_facet |
OCEANOGRAPHY |
description |
Ice core analyses are needed in SeaRISE to learn what the West Antarctic ice sheet and other marine ice sheets were like in the past, what climate changes led to their present states, and how they behave. The major results of interest to SeaRISE from previous ice core analyses in West Antarctic are that the end of the last ice age caused temperature and accumulation rate increases in inland regions, leading to ice sheet thickening followed by thinning to the present. |
format |
Other/Unknown Material |
author |
Alley, Richard B. |
author_facet |
Alley, Richard B. |
author_sort |
Alley, Richard B. |
title |
Ice cores and SeaRISE: What we do (and don't) know |
title_short |
Ice cores and SeaRISE: What we do (and don't) know |
title_full |
Ice cores and SeaRISE: What we do (and don't) know |
title_fullStr |
Ice cores and SeaRISE: What we do (and don't) know |
title_full_unstemmed |
Ice cores and SeaRISE: What we do (and don't) know |
title_sort |
ice cores and searise: what we do (and don't) know |
publishDate |
1991 |
url |
http://hdl.handle.net/2060/19910017265 |
op_coverage |
Unclassified, Unlimited, Publicly available |
geographic |
Antarctic West Antarctic Ice Sheet |
geographic_facet |
Antarctic West Antarctic Ice Sheet |
genre |
Antarc* Antarctic ice core Ice Sheet |
genre_facet |
Antarc* Antarctic ice core Ice Sheet |
op_source |
CASI |
op_relation |
Document ID: 19910017265 Accession ID: 91N26579 http://hdl.handle.net/2060/19910017265 |
op_rights |
No Copyright |
_version_ |
1766173729098825728 |