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Record #122284:

Deglaciation triggered by the resumption of North Atlantic Deep Water / James D. Wright.

Title: Deglaciation triggered by the resumption of North Atlantic Deep Water / James D. Wright.
Author(s): Wright, James D.
Date: 1993.
In: Eos : transactions, American Geophysical Union. (1993.), Vol. 74(2) (1993)
Abstract: Changes in distribution of solar radiation received on Earth are known to be pacemaker of Pleistocene climate change, but cannot account, by themselves, for waxing and waning of ice ages. Reviews new evidence which clearly defines role of deep ocean circulation during last deglaciation and supports stronger connection between deep ocean circulation changes and warming trends.
Notes:

Eos : transactions, American Geophysical Union. Vol. 74(2) :24 (1993).

Keywords: 551.336 -- Ice ages.
551.791 -- Pleistocene.
551.338 -- Ice ages, theories of causation.
551.583.3 -- Climatic changes, Quaternary.
551.461.8 -- Palaeo-oceanography.
551.465 -- Oceanography, dynamics.
551.465.71 -- Ocean dynamics, solar and terrestrial effects.
E7 -- Glaciology: glacial geology and ice ages.
SPRI record no.: 122284

MARCXML

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520 3# ‡aChanges in distribution of solar radiation received on Earth are known to be pacemaker of Pleistocene climate change, but cannot account, by themselves, for waxing and waning of ice ages. Reviews new evidence which clearly defines role of deep ocean circulation during last deglaciation and supports stronger connection between deep ocean circulation changes and warming trends.
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650 07 ‡a551.338 -- Ice ages, theories of causation.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.461.8 -- Palaeo-oceanography.‡2udc
650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc
650 07 ‡a551.465.71 -- Ocean dynamics, solar and terrestrial effects.‡2udc
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