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We have conducted high-resolution simulations with primitive equation or non-hydrostatic atmospheric, oceanic and coupled models in order to understand mechanisms of variations of the atmosphere–ocean system with relatively small spatial scales in the oceanic part. We report in this paper decadal va...
Main Authors: | , , , , , , |
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Other Authors: | |
Format: | Text |
Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.405.5008 http://www.jamstec.go.jp/esc/publication/annual/annual2009/pdf/2project/chapter1/p011_Ohfuchi.pdf |
Summary: | We have conducted high-resolution simulations with primitive equation or non-hydrostatic atmospheric, oceanic and coupled models in order to understand mechanisms of variations of the atmosphere–ocean system with relatively small spatial scales in the oceanic part. We report in this paper decadal variations in the North Pacific, Kuroshio Extension Current fluctuations, sea-ice variations in the Arctic Sea, and typhoon development. |
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