An Oceanic Cold Reversal
of the Younger Dryas (a warming in inland Antarctic records at 12.5 ky B.P., when Greenland cools abruptly) is consistent with the idea of a seesaw behavior of the Atlantic thermohaline circulation (6 ), caused by a massive discharge of ice cap meltwater, which shut down thermohaline circulation, re...
Main Authors: | , , , , , , , , |
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Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.7.9972 http://www.climate.unibe.ch/pdf/Stenni_et_al.pdf |