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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Format: | Text |
Language: | English |
Published: |
2004
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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 |
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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