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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...

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Bibliographic Details
Main Authors: Wataru Ohfuchi, Nobumasa Komori, Bunmei Taguchi, Akira Kuwano-yoshida, Masami Nonaka, Mayumi K. Yoshioka, Hidenori Aiki
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
atmosphere–ocean interaction
sea surface temperature front
oceanic Rossby wave
sea ice variability
typhoon
Arctic
Pacific
Sea ice
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
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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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