Dust: A Diagnostic of the Hydrologic Cycle During the Last Glacial Maximum
Dust concentrations in ice of the last glacial maximum (LGM) are high in ice cores from Greenland and Antarctica. The magnitude of the enhancements can be explained if the strength of the hydrologic cycle during the LGM was about half of that at present. This notion is consistent with a large decrea...
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American Association for the Advancement of Science (AAAS)
1996
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Online Access: | http://dx.doi.org/10.1126/science.271.5251.962 https://www.science.org/doi/pdf/10.1126/science.271.5251.962 |
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craaas:10.1126/science.271.5251.962 2024-04-21T07:49:13+00:00 Dust: A Diagnostic of the Hydrologic Cycle During the Last Glacial Maximum Yung, Yuk L. Lee, Typhoon Wang, Chung-Ho Shieh, Ying-Tzung 1996 http://dx.doi.org/10.1126/science.271.5251.962 https://www.science.org/doi/pdf/10.1126/science.271.5251.962 en eng American Association for the Advancement of Science (AAAS) Science volume 271, issue 5251, page 962-963 ISSN 0036-8075 1095-9203 Multidisciplinary journal-article 1996 craaas https://doi.org/10.1126/science.271.5251.962 2024-03-27T07:41:07Z Dust concentrations in ice of the last glacial maximum (LGM) are high in ice cores from Greenland and Antarctica. The magnitude of the enhancements can be explained if the strength of the hydrologic cycle during the LGM was about half of that at present. This notion is consistent with a large decrease (5°C) in ocean temperature during the LGM, as recently deduced from measurements of strontium and calcium in corals. Article in Journal/Newspaper Antarc* Antarctica Greenland AAAS Resource Center (American Association for the Advancement of Science) Science 271 5251 962 963 |
institution |
Open Polar |
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AAAS Resource Center (American Association for the Advancement of Science) |
op_collection_id |
craaas |
language |
English |
topic |
Multidisciplinary |
spellingShingle |
Multidisciplinary Yung, Yuk L. Lee, Typhoon Wang, Chung-Ho Shieh, Ying-Tzung Dust: A Diagnostic of the Hydrologic Cycle During the Last Glacial Maximum |
topic_facet |
Multidisciplinary |
description |
Dust concentrations in ice of the last glacial maximum (LGM) are high in ice cores from Greenland and Antarctica. The magnitude of the enhancements can be explained if the strength of the hydrologic cycle during the LGM was about half of that at present. This notion is consistent with a large decrease (5°C) in ocean temperature during the LGM, as recently deduced from measurements of strontium and calcium in corals. |
format |
Article in Journal/Newspaper |
author |
Yung, Yuk L. Lee, Typhoon Wang, Chung-Ho Shieh, Ying-Tzung |
author_facet |
Yung, Yuk L. Lee, Typhoon Wang, Chung-Ho Shieh, Ying-Tzung |
author_sort |
Yung, Yuk L. |
title |
Dust: A Diagnostic of the Hydrologic Cycle During the Last Glacial Maximum |
title_short |
Dust: A Diagnostic of the Hydrologic Cycle During the Last Glacial Maximum |
title_full |
Dust: A Diagnostic of the Hydrologic Cycle During the Last Glacial Maximum |
title_fullStr |
Dust: A Diagnostic of the Hydrologic Cycle During the Last Glacial Maximum |
title_full_unstemmed |
Dust: A Diagnostic of the Hydrologic Cycle During the Last Glacial Maximum |
title_sort |
dust: a diagnostic of the hydrologic cycle during the last glacial maximum |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
1996 |
url |
http://dx.doi.org/10.1126/science.271.5251.962 https://www.science.org/doi/pdf/10.1126/science.271.5251.962 |
genre |
Antarc* Antarctica Greenland |
genre_facet |
Antarc* Antarctica Greenland |
op_source |
Science volume 271, issue 5251, page 962-963 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.271.5251.962 |
container_title |
Science |
container_volume |
271 |
container_issue |
5251 |
container_start_page |
962 |
op_container_end_page |
963 |
_version_ |
1796931435002593280 |