The Characteristics of Marine Environment around the Ieodo in Aug. 2016

DC Field Value Language
dc.contributor.author 최은지 -
dc.contributor.author 김성현 -
dc.contributor.author 김응 -
dc.contributor.author 김병남 -
dc.contributor.author 최복경 -
dc.date.accessioned 2020-07-15T13:32:07Z -
dc.date.available 2020-07-15T13:32:07Z -
dc.date.created 2020-02-11 -
dc.date.issued 2017-12-11 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/23520 -
dc.description.abstract The sea area around Ieodo is analyzed from the CTD data and the S-ADCP data observed in 23 Aug. 2016. Ieodo, an underwater reef, is located 149 km southwest of Marado in Republic of Korea. It has 4 peaks and is about 4.6 meter below sea level. It stretches about 600m north to south and 750m east to west from its top. It has the same geographical characteristics as the seamount.In the sea area around Ieodo, the northward flow appeared during the ebb tide, the southward flow appeared during the flood tide. The strong stratification formed in summer seems to change the depth depending on the sea water current. The thermocline depth becomes deeper at the north of the Ieodo when the northward current flows and theupwelling flow occurs. And the thermocline depth becomes shallower at the south when the southward current flows and the downwelling flow occurs. In this way, the upwelling and downwelling seems to be according to the tide’s direction.el. It stretches about 600m north to south and 750m east to west from its top. It has the same geographical characteristics as the seamount.In the sea area around Ieodo, the northward flow appeared during the ebb tide, the southward flowappeared during the flood tide. The strong stratification formed in summer seems to change the depth depending on the sea water current. The thermocline depth becomes deeper at the north of the Ieodo when the northward current flows and theupwelling flow occurs. And the thermocline depth becomes shallower at the south when the southward current flows and the downwelling flow occurs. In this way, the upwelling and downwelling seems to be according to the tide’s direction. -
dc.description.uri 1 -
dc.language English -
dc.publisher American Geophysical Union -
dc.relation.isPartOf American Geophysical Union 2017 Fall Meeting -
dc.title The Characteristics of Marine Environment around the Ieodo in Aug. 2016 -
dc.type Conference -
dc.citation.conferencePlace US -
dc.citation.endPage 1 -
dc.citation.startPage 1 -
dc.citation.title American Geophysical Union 2017 Fall Meeting -
dc.contributor.alternativeName 최은지 -
dc.contributor.alternativeName 김성현 -
dc.contributor.alternativeName 김응 -
dc.contributor.alternativeName 김병남 -
dc.contributor.alternativeName 최복경 -
dc.identifier.bibliographicCitation American Geophysical Union 2017 Fall Meeting, pp.1 -
dc.description.journalClass 1 -
Appears in Collections:
Sea Power Enhancement Research Division > Marine Domain & Security Research Department > 2. Conference Papers
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