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Ocean Cooling Pattern at the Last Glacial Maximum
Joint Authors
Zhuang, Kelin
Giardino, John R.
Source
Issue
Vol. 2012, Issue 2012 (31 Dec. 2012), pp.1-8, 8 p.
Publisher
Hindawi Publishing Corporation
Publication Date
2012-12-13
Country of Publication
Egypt
No. of Pages
8
Main Subjects
Abstract EN
Ocean temperature and ocean heat content change are analyzed based on four PMIP3 model results at the Last Glacial Maximum relative to the prehistorical run.
Ocean cooling mostly occurs in the upper 1000 m depth and varies spatially in the tropical and temperate zones.
The Atlantic Ocean experiences greater cooling than the rest of the ocean basins.
Ocean cooling is closely related to the weakening of meridional overturning circulation and enhanced intrusion of Antarctic Bottom Water into the North Atlantic.
American Psychological Association (APA)
Zhuang, Kelin& Giardino, John R.. 2012. Ocean Cooling Pattern at the Last Glacial Maximum. Advances in Meteorology،Vol. 2012, no. 2012, pp.1-8.
https://search.emarefa.net/detail/BIM-455039
Modern Language Association (MLA)
Zhuang, Kelin& Giardino, John R.. Ocean Cooling Pattern at the Last Glacial Maximum. Advances in Meteorology No. 2012 (2012), pp.1-8.
https://search.emarefa.net/detail/BIM-455039
American Medical Association (AMA)
Zhuang, Kelin& Giardino, John R.. Ocean Cooling Pattern at the Last Glacial Maximum. Advances in Meteorology. 2012. Vol. 2012, no. 2012, pp.1-8.
https://search.emarefa.net/detail/BIM-455039
Data Type
Journal Articles
Language
English
Notes
Includes bibliographical references
Record ID
BIM-455039