Glacial/Interglacial Paleoclimate

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Glacial/Interglacial Paleoclimate
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N. American cold winds affected N. Atlantic SST
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Size of ice sheets controlled climate in mid- and
high-latitude regions
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Paleoclimate of the Last Glacial Maximum
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Climap reconstruction of SST
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Climap reconstructions of ice thickness do not
match recent glacial reconstructions
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Today precipitation and temperature control the
distribution of vegetation in the Midwest.
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Model simulations verified that colder conditions
forced a change in vegetation, although these
simulations do not fully capture proxy data.
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Melting of southward- floating icebergs.
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Tropical cooling during the LGM
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Climaps SST reconstructions for low latitudes is
based on small differences
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