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- W2374420393 abstract "Using the Simple Ocean Data Assimilation(SODA) climatological data,we compared the climatological oceanic stratification around the Antarctic and the Antarctic Circumpolar Current(ACC) region to conduct a pre-liminary study on the reasonable oceanic boundary condition of Antarctic ice sheet melting.Our results indicate freshwater flux induced by ice-melting will advect along the surface path in the East Atlantic and Indian Ocean,while in the West Atlantic and Pacific Ocean,the meridional motion path of freshwater flux depends on the intensity of freshwater flux itself.When there appears intense ice-melting of Antarctic,freshwater will travel along the sur-face path;when ice-melting is relatively generous,subsurface path will be preferred by freshwater flux.On the ba-sis of these analyses,we quantitatively assessed the threshold state guaranteeing freshwater flux moving along sur-face path,and further analyzed the rationality of simulation of Antarctic ice-melting with idealized freshwater flux in most of current climate models,in order to providing neccessary reference for the selection of modeling strategy simulating the Antarctic ice-melting scenario." @default.
- W2374420393 created "2016-06-24" @default.
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- W2374420393 date "2011-01-01" @default.
- W2374420393 modified "2023-09-26" @default.
- W2374420393 title "A preliminary study on the oceanic boundary condition of an idealized Antarctic ice sheet melting scheme" @default.
- W2374420393 hasPublicationYear "2011" @default.
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