Warmth of the Subpolar North Atlantic Ocean During Northern Hemisphere Ice-Sheet Growth
Two 10,000-year periods of Northern Hemisphere continental ice-sheet growth stand out prominently within the last full interglacial-to-glacial cycle. During the first half of each rapid ice-growth phase, the subpolar North Atlantic from 40°N to 60°N maintained warm sea-surface temperatures comparabl...
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Language: | English |
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American Association for the Advancement of Science (AAAS)
1979
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Online Access: | http://dx.doi.org/10.1126/science.204.4389.173 https://www.science.org/doi/pdf/10.1126/science.204.4389.173 |
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craaas:10.1126/science.204.4389.173 2024-06-09T07:46:46+00:00 Warmth of the Subpolar North Atlantic Ocean During Northern Hemisphere Ice-Sheet Growth Ruddiman, W. F. McIntyre, A. 1979 http://dx.doi.org/10.1126/science.204.4389.173 https://www.science.org/doi/pdf/10.1126/science.204.4389.173 en eng American Association for the Advancement of Science (AAAS) Science volume 204, issue 4389, page 173-175 ISSN 0036-8075 1095-9203 journal-article 1979 craaas https://doi.org/10.1126/science.204.4389.173 2024-05-16T12:54:46Z Two 10,000-year periods of Northern Hemisphere continental ice-sheet growth stand out prominently within the last full interglacial-to-glacial cycle. During the first half of each rapid ice-growth phase, the subpolar North Atlantic from 40°N to 60°N maintained warm sea-surface temperatures comparable to those of today's ocean. The juxtaposition at latitudes 50°N to 60°N of an "interglacial" ocean alongside a "glacial" land mass, particularly along eastern North America, is regarded as an optimal configuration for delivering moisture to the growing ice sheets. Article in Journal/Newspaper Ice Sheet North Atlantic AAAS Resource Center (American Association for the Advancement of Science) Science 204 4389 173 175 |
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Open Polar |
collection |
AAAS Resource Center (American Association for the Advancement of Science) |
op_collection_id |
craaas |
language |
English |
description |
Two 10,000-year periods of Northern Hemisphere continental ice-sheet growth stand out prominently within the last full interglacial-to-glacial cycle. During the first half of each rapid ice-growth phase, the subpolar North Atlantic from 40°N to 60°N maintained warm sea-surface temperatures comparable to those of today's ocean. The juxtaposition at latitudes 50°N to 60°N of an "interglacial" ocean alongside a "glacial" land mass, particularly along eastern North America, is regarded as an optimal configuration for delivering moisture to the growing ice sheets. |
format |
Article in Journal/Newspaper |
author |
Ruddiman, W. F. McIntyre, A. |
spellingShingle |
Ruddiman, W. F. McIntyre, A. Warmth of the Subpolar North Atlantic Ocean During Northern Hemisphere Ice-Sheet Growth |
author_facet |
Ruddiman, W. F. McIntyre, A. |
author_sort |
Ruddiman, W. F. |
title |
Warmth of the Subpolar North Atlantic Ocean During Northern Hemisphere Ice-Sheet Growth |
title_short |
Warmth of the Subpolar North Atlantic Ocean During Northern Hemisphere Ice-Sheet Growth |
title_full |
Warmth of the Subpolar North Atlantic Ocean During Northern Hemisphere Ice-Sheet Growth |
title_fullStr |
Warmth of the Subpolar North Atlantic Ocean During Northern Hemisphere Ice-Sheet Growth |
title_full_unstemmed |
Warmth of the Subpolar North Atlantic Ocean During Northern Hemisphere Ice-Sheet Growth |
title_sort |
warmth of the subpolar north atlantic ocean during northern hemisphere ice-sheet growth |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
1979 |
url |
http://dx.doi.org/10.1126/science.204.4389.173 https://www.science.org/doi/pdf/10.1126/science.204.4389.173 |
genre |
Ice Sheet North Atlantic |
genre_facet |
Ice Sheet North Atlantic |
op_source |
Science volume 204, issue 4389, page 173-175 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.204.4389.173 |
container_title |
Science |
container_volume |
204 |
container_issue |
4389 |
container_start_page |
173 |
op_container_end_page |
175 |
_version_ |
1801376758073655296 |