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Record #152503:

Climatic stability of the geographic origin of Antarctic precipitation simulated by an atmospheric general circulation model / Gilles Delaygue, Valérie Masson, Jean Jouzel.

Title: Climatic stability of the geographic origin of Antarctic precipitation simulated by an atmospheric general circulation model / Gilles Delaygue, Valérie Masson, Jean Jouzel.
Author(s): Delaygue, Gilles.
Masson, Valérie.
Jouzel, Jean.
Date: 1999.
In: Annals of Glaciology. (1999.), Vol. 29 (1999)
Abstract: Estimates moisture origins of Antarctic precipitation with NASA/Goddard Institute of Space Studies atmospheric general circulation model under different climatic conditions. Model indicates subtropical to subglacial latitudinal origin for Antarctic precipitation. Uses different climatic reconstructions, based on CLIMAP, for Last Glacial Maximum, which differ by latitudinal sea-surface temperature gradient and seasonality. Shifting seasonal cycle of oceanic prescribed conditions has important effect on hydrological cycle. Cooler tropical sea-surface temperatures make latitudinal contributions close to modern ones.
Notes:

Annals of Glaciology. Vol. 29 :45-48 (1999).

Sixth International Symposium on Antarctic Glaciology (ISAG-6), 5--9 September 1998, Lanzhou, China, T.H. Jacka (Editor)

Keywords: 551.5 -- Meteorology.
551.513 -- Atmosphere, general circulation.
551.577 -- Precipitation.
551.583.3 -- Climatic changes, Quaternary.
551.326.7 -- Sea ice.
519.673 -- Modelling.
E9 -- Glaciology: meteorology and climatology.
(*7) -- Antarctic regions.
SPRI record no.: 152503

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245 10 ‡aClimatic stability of the geographic origin of Antarctic precipitation simulated by an atmospheric general circulation model /‡cGilles Delaygue, Valérie Masson, Jean Jouzel.
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500 ## ‡aSixth International Symposium on Antarctic Glaciology (ISAG-6), 5--9 September 1998, Lanzhou, China, T.H. Jacka (Editor)
520 3# ‡aEstimates moisture origins of Antarctic precipitation with NASA/Goddard Institute of Space Studies atmospheric general circulation model under different climatic conditions. Model indicates subtropical to subglacial latitudinal origin for Antarctic precipitation. Uses different climatic reconstructions, based on CLIMAP, for Last Glacial Maximum, which differ by latitudinal sea-surface temperature gradient and seasonality. Shifting seasonal cycle of oceanic prescribed conditions has important effect on hydrological cycle. Cooler tropical sea-surface temperatures make latitudinal contributions close to modern ones.
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650 07 ‡a551.513 -- Atmosphere, general circulation.‡2udc
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650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aE9 -- Glaciology: meteorology and climatology.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
700 1# ‡aMasson, Valérie.
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