and salt contrast between the North Pacific and Southern Ocean would have been the sudden onset of deep convection in the North Pacific. Bottom waters formed would have filled deep Pacific basins and flowed through the Indonesian passage into the eastern Indian Ocean basin, and the locus of deep-wat...
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.675.6550 http://www.nasa.gov/pdf/121648main_ais2.pdf |