Dust: A Diagnostic of the Hydrological Cycle during the Last Glacial Maximum

2010507010023 天文所 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 w...

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Bibliographic Details
Main Author: Yung YL;Lee T;Wang CH;Shieh YT
Other Authors: 李太楓
Format: Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science 1996
Subjects:
30
Online Access:http://nthur.lib.nthu.edu.tw/dspace/handle/987654321/53812
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spelling ftnthuniv:oai:nthur.lib.nthu.edu.tw:987654321/53812 2023-05-15T13:31:11+02:00 Dust: A Diagnostic of the Hydrological Cycle during the Last Glacial Maximum Yung YL;Lee T;Wang CH;Shieh YT 李太楓 1996 109 bytes text/html http://nthur.lib.nthu.edu.tw/dspace/handle/987654321/53812 En eng American Association for the Advancement of Science Science 16 February 1996,Vol. 271 no. 5251 pp. 962-963 GENERAL-CIRCULATION MODEL;DESERT DUST;ICE;ATMOSPHERE 30 Journal 1996 ftnthuniv 2014-12-17T20:53:52Z 2010507010023 天文所 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. Journal/Newspaper Antarc* Antarctica Greenland National Tsing Hua University Institutional Repository (NTHUR) Greenland
institution Open Polar
collection National Tsing Hua University Institutional Repository (NTHUR)
op_collection_id ftnthuniv
language English
topic GENERAL-CIRCULATION MODEL;DESERT DUST;ICE;ATMOSPHERE
30
spellingShingle GENERAL-CIRCULATION MODEL;DESERT DUST;ICE;ATMOSPHERE
30
Yung YL;Lee T;Wang CH;Shieh YT
Dust: A Diagnostic of the Hydrological Cycle during the Last Glacial Maximum
topic_facet GENERAL-CIRCULATION MODEL;DESERT DUST;ICE;ATMOSPHERE
30
description 2010507010023 天文所 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.
author2 李太楓
format Journal/Newspaper
author Yung YL;Lee T;Wang CH;Shieh YT
author_facet Yung YL;Lee T;Wang CH;Shieh YT
author_sort Yung YL;Lee T;Wang CH;Shieh YT
title Dust: A Diagnostic of the Hydrological Cycle during the Last Glacial Maximum
title_short Dust: A Diagnostic of the Hydrological Cycle during the Last Glacial Maximum
title_full Dust: A Diagnostic of the Hydrological Cycle during the Last Glacial Maximum
title_fullStr Dust: A Diagnostic of the Hydrological Cycle during the Last Glacial Maximum
title_full_unstemmed Dust: A Diagnostic of the Hydrological Cycle during the Last Glacial Maximum
title_sort dust: a diagnostic of the hydrological cycle during the last glacial maximum
publisher American Association for the Advancement of Science
publishDate 1996
url http://nthur.lib.nthu.edu.tw/dspace/handle/987654321/53812
geographic Greenland
geographic_facet Greenland
genre Antarc*
Antarctica
Greenland
genre_facet Antarc*
Antarctica
Greenland
op_relation Science 16 February 1996,Vol. 271 no. 5251 pp. 962-963
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