Strengthening of the Northeast Monsoon over the Flores Sea, Indonesia, at the time of Heinrich event 1
Paleoclimate evidence from South America and Asia has been interpreted to indicate that tropical rainfall migrated southward during the Northern Hemisphere cooling associated with Heinrich stadial 1 (HS1), an event of massive iceberg discharge to the North Atlantic ca. 18–15 ka. Although arid condit...
Main Authors: | , , , |
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Format: | Text |
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Columbia University
2012
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Online Access: | https://dx.doi.org/10.7916/d8h13bqq https://academiccommons.columbia.edu/doi/10.7916/D8H13BQQ |