SEASONAL VARIATION OF SURFACE AND DEEP CURRENTS IN THE JAPAN SEA
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- TRUSENKOVA Olga
- V.I. Il'ichev Pacific Oceanological Institute, Russian Academy of Science
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- ISHIDA Hajime
- Dept. of Civil Engineering, Kanazawa University
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Abstract
As simulated with the MHI oceanic model (Shapiro, 1998), surface gradient currents in the entire Japan Sea strengthen (weaken) in late summer (winter), with the highest (lowest) velocity in August (February), in line with altimetry data (Morimoto and Yanagi, 2001). The simulated patterns of the surface circulation are in line with those derived from satellite imagery (Nikitin and Kharchenko, 2002). In particular, a northern meander of the East Korean Warm Current is simulated near the North Korea coast in October, caused by local anticyclonic wind stress curl. The simulated deep circulation is geostrophic and reaches the highest (lowest) velocity in April (November), after 2 to 3 months of the extreme surface velocity.
Journal
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- Doboku Gakkai Ronbunshu
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Doboku Gakkai Ronbunshu 2005 (796), 796_93-796_111, 2005
Japan Society of Civil Engineers
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Keywords
Details 詳細情報について
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- CRID
- 1390282680578801920
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- NII Article ID
- 10015604385
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- NII Book ID
- AN10014020
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- ISSN
- 18827187
- 02897806
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- NDL BIB ID
- 7461725
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- Text Lang
- en
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- Data Source
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- JaLC
- NDL
- Crossref
- CiNii Articles
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- Abstract License Flag
- Disallowed