lf, a decrease with Allerød cooling, and a recovery through the ttersrelationship with the millennial perturbations of NADW flux to the deep Southern Ocean. The data indicate that the baseline intensity of NADW reaching the Cape Basin is paced by Northern Hemisphere insolation and that North Atlanti...

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Bibliographic Details
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2004
Subjects:
thermohaline circulation
deep water
deglacial
neodymium
Younger Dryas
last glacial
Southern Ocean
NADW
North Atlantic
Sea ice
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.548.7252
http://www.ldeo.columbia.edu/~peter/Resources/Seminar/readings/Piotrowski_etal_EPSL04.pdf
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Summary:lf, a decrease with Allerød cooling, and a recovery through the ttersrelationship with the millennial perturbations of NADW flux to the deep Southern Ocean. The data indicate that the baseline intensity of NADW reaching the Cape Basin is paced by Northern Hemisphere insolation and that North Atlantic sea ice coverage acts as a major amplifying link between the oceans and the atmosphere.

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