Changes in ITCZ location and cross-equatorial heat transport at the Last Glacial Maximum, Heinrich Stadial 1, and the mid-Holocene-Reference-Cited by-同舟云学术

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Changes in ITCZ location and cross-equatorial heat transport at the Last Glacial Maximum, Heinrich Stadial 1, and the mid-Holocene

Published:2014-03 Issue: Volume:390 Page:69-79
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

McGee David,Donohoe Aaron,Marshall John,Ferreira David

Funder

U.S. Department of Energy

National Center for Atmospheric Research

National Science Foundation

National Oceanic and Atmospheric Administration

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference62 articles.

1. The “African humid period” and the record of marine upwelling from excess 230Th in Ocean Drilling Program Hole 658C;Adkins;Paleoceanography,2006

2. Meridional shifts of the Atlantic intertropical convergence zone since the Last Glacial Maximum;Arbuszewski;Nat. Geosci.,2013

3. Rapid interhemispheric climate links via the Australasian monsoon during the last deglaciation;Ayliffe;Nat. Commun.,2013

4. Hydrological impact of Heinrich events in the subtropical northeast Atlantic;Bard;Science,2000

5. Rates of thermohaline recovery from freshwater pulses in modern, Last Glacial Maximum, and greenhouse warming climates;Bitz;Geophys. Res. Lett.,2007

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