The effects of geothermal heating on the East Sea

DC Field Value Language
dc.contributor.author 박영규 -
dc.contributor.author 박재훈 -
dc.contributor.author 이호진 -
dc.contributor.author 민홍식 -
dc.date.accessioned 2020-07-16T09:31:46Z -
dc.date.available 2020-07-16T09:31:46Z -
dc.date.created 2020-02-11 -
dc.date.issued 2013-05-09 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/27083 -
dc.description.abstract Geothermal heating intensifies the bottom flows but the simulated flows are not as strong as the observed ones suggesting we still are missing important factors. Reduction in deep stratification strengthens deep water mass formation, intensifying cyclonic circulations located over this area, so the effects of the heating extend to the surfaceifying cyclonic circulations located over this area, so the effects of the heating extend to the surface -
dc.description.uri 1 -
dc.language English -
dc.publisher 2nd KIOST-US Joint Symposium on Climate and Ocean -
dc.relation.isPartOf 2nd KIOST-US Joint Symposium on Climate and Ocean -
dc.title The effects of geothermal heating on the East Sea -
dc.type Conference -
dc.citation.conferencePlace US -
dc.citation.endPage 1 -
dc.citation.startPage 1 -
dc.citation.title 2nd KIOST-US Joint Symposium on Climate and Ocean -
dc.contributor.alternativeName 박영규 -
dc.contributor.alternativeName 박재훈 -
dc.contributor.alternativeName 민홍식 -
dc.identifier.bibliographicCitation 2nd KIOST-US Joint Symposium on Climate and Ocean, pp.1 -
dc.description.journalClass 1 -
Appears in Collections:
Ocean Climate Solutions Research Division > Ocean Circulation & Climate Research Department > 2. Conference Papers
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