The Indo-Pacific warm pool was much dryer during the last ice age than today, because lower sea level exposed the Sunda Shelf. The large landmass, in place of the warm ocean, altered the atmospheric circulation, shifting convection further west into the Indian Ocean. These findings by scientists at the International Pacific Research Center, University of Hawaii at Manoa, and Woods Hole Institute of Oceanography, appear in the May 19, online edition of Nature Geoscience.
Fuente : http://www.eurekalert.org/pub_releases/2013-05/uoh…
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