Summer transport estimates of the Kamchatka Current derived as a variational inverse of hydrophysical and surface drifter data

Panteleev, G.G.; Stabeno, P.; Luchin, V.A. et al.

Geophysical Research Letters, 2006, 33(9), L09609

Permalink : https://hdl.handle.net/2115/14407

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アクセス権	open access
URI	https://hdl.handle.net/2115/14407
タイトル	Summer transport estimates of the Kamchatka Current derived as a variational inverse of hydrophysical and surface drifter data
著者	Panteleev, G.G. ; Stabeno, P. ; Luchin, V.A. ; Nechaev, D.A. ; Ikeda, M.
著者名 Panteleev, G.G.
著者名 Stabeno, P.
著者名 Luchin, V.A.
著者名 Nechaev, D.A.
著者名 Ikeda, M. 池田, 元美
言語	英語
発行日	2006-05-12
出版者	AMERICAN GEOPHYSICAL UNION
収録物名	Geophysical Research Letters
巻(号)	33(9)
ページ	L09609
抄録	The quasistationary summer Bering Sea circulation is reconstructed as a variational inverse of the hydrographic and atmospheric climatologies, transport estimates through the Bering Strait, and surface drifter data. Our results indicate the splitting of the Kamchatka Current in the vicinity of the Shirshov Ridge. This branching is in agreement with independent ARGO drifter observations. It was also found, that transport of the Kamchatka Current gradually increases downstream from 14 Sv in the Olyutorsky Gulf to 24 Sv in the Kamchatka Strait, which is twice higher than previous estimates.
資源タイプ	学術雑誌論文
出版タイプ	Version of Record
権利情報	An edited version of this paper was published by AGU. Copyright 2006 American Geophysical Union.
PISSN	0094-8276
関連情報 (isIdenticalTo)	出版社版DOI https://doi.org/10.1029/2005GL024974, 2006