Role of the Greenland-Scotland Ridge in Neogene Climate Changes
Abstract Cenozoic climates are marked by long-term cooling since the early Eocene that evolved into the large amplitude glacial/interglacial cycles of the late Pleistocene. Circulation models (both atmospheric and oceanic) have simulated these changes by altering the concentration of atmospheric tra...
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Format: | Book Part |
Language: | unknown |
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Oxford University PressNew York, NY
1998
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Online Access: | http://dx.doi.org/10.1093/oso/9780195112450.003.0009 https://academic.oup.com/book/chapter-pdf/52433466/isbn-9780195112450-book-part-9.pdf |