동중국해에서 태풍에 대한 해양반응 큰에디모사

DC Field Value Language
dc.contributor.author 민홍식 -
dc.contributor.author 강석구 -
dc.date.accessioned 2020-07-16T13:31:39Z -
dc.date.available 2020-07-16T13:31:39Z -
dc.date.created 2020-02-11 -
dc.date.issued 2012-02-23 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/27903 -
dc.description.abstract A large eddy simulation (LES) model is used to examine an ocean response to a typhoon in the East China Sea. Wind stresses and wave fields at the right of the route where the typhoon Kompasu passes are applied for surface forcing, and temperature and salinity structures observed before the typhoon is used as an initial ocean condition. The LES model shows that turbulent intensity increases and surface mixed layer deepens during the typhoon as expected. In contrast to the vertical component of the turbulent intensity which is high in the middle of the mixed layer, its horizontal component is high very near the surface. Besides near the surface, the downwind direction component of the turbulent intensity is high near the bottom of the surface mixed layer while the crosswind direction component is low. With the comparison experiment to examine the effect of wind direction change, it is found that the change of wind direction influences the velocity field not only in the mixed layer but also below the thermocline.emperature and salinity structures observed before the typhoon is used as an initial ocean condition. The LES model shows that turbulent intensity increases and surface mixed layer deepens during the typhoon as expected. In contrast to the vertical component of the turbulent intensity which is high in the middle of the mixed layer, its horizontal component is high very near the surface. Besides near the surface, the downwind direction component of the turbulent intensity is high near the bottom of the surface mixed layer while the crosswind direction component is low. With the comparison experiment to examine the effect of wind direction change, it is found that the change of wind direction influences the velocity field not only in the mixed layer but also below the thermocline. -
dc.description.uri 1 -
dc.language English -
dc.publisher American Geophysical Union -
dc.relation.isPartOf Ocean Sciences Meeting 2012 -
dc.title 동중국해에서 태풍에 대한 해양반응 큰에디모사 -
dc.title.alternative Large Eddy Simulation of Ocean Response to a Typhoon in the East China Sea -
dc.type Conference -
dc.citation.conferencePlace US -
dc.citation.endPage 319 -
dc.citation.startPage 319 -
dc.citation.title Ocean Sciences Meeting 2012 -
dc.contributor.alternativeName 민홍식 -
dc.contributor.alternativeName 강석구 -
dc.identifier.bibliographicCitation Ocean Sciences Meeting 2012, pp.319 -
dc.description.journalClass 1 -
Appears in Collections:
Marine Environmental & Climate Research Division > Ocean Circulation Research Center > 2. Conference Papers
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