Near collapse of the meridional SST gradient in the eastern equatorial Pacific during Heinrich Stadial 1-Reference-Cited by-同舟云学术

Near collapse of the meridional SST gradient in the eastern equatorial Pacific during Heinrich Stadial 1

Published:2013-11-25 Issue:4 Volume:28 Page:663-674
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Kienast Stephanie S.¹,Friedrich Tobias²,Dubois Nathalie³,Hill Paul S.¹,Timmermann Axel²,Mix Alan C.⁴,Kienast Markus¹

Affiliation:

1. Department of Oceanography; Dalhousie University; Halifax Nova Scotia Canada

2. International Pacific Research Center, SOEST; University of Hawaii; Honolulu Hawaii USA

3. Woods Hole Oceanographic Institution; Woods Hole Massachusetts USA

4. College of Earth, Ocean and Atmospheric Sciences; Oregon State University; Corvallis Oregon USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

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4. Partitioning of eolian and hemipelagic sediment in eastern equatorial Pacific core TR163-31B and the late Quaternary climate of the northern Andes;Boven;J. Sediment. Res.,1998

5. Diatom productivity in the Equatorial Pacific Ocean from the Last Glacial Maximum to the present: A test of the silicic acid leakage hypothesis;Bradtmiller;Paleoceanography,2006

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