GOCI, AVHRR, MODIS, VIIRS 등을 이용한 동해안 냉수대의 시공간적인 변화분석

DC Field Value Language
dc.contributor.author 윤석 -
dc.contributor.author 양현 -
dc.date.accessioned 2020-07-15T20:34:32Z -
dc.date.available 2020-07-15T20:34:32Z -
dc.date.created 2020-02-11 -
dc.date.issued 2016-09-27 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/24596 -
dc.description.abstract This study relates various environment changes to cold water zone in summer season in the East/Japan Sea. Cold water means the sea area where average sea surface temperature (SST) is 5°C lower than its surroundings. Data analysis was performed based on the divers environment factors using satellite data and in-situ data from summer to fall during the period of 2011~2016. We used daily SST data derived from the AVHRR, the MODIS, and the VIIRS to located cold water area. We also used daily chlorophyll concentration (chl) data from the Geostationary Ocean color Imager (GOCI), geostrophic current data from the AVISO, and wind speed data from the WindSat to the influnce of life a cold water zone. As a result we studied that the cycle of life a cold water zone is repeated in summer season. Also, we found out that the cold water tends to occurred at the end of Jun and disappeared at the end of August. It sees that the chl increment from September to November although after the cold water zone disappeared. On the other hand We found see that this phenomenon comes from inertial influence of cold water zone.rmed based on the divers environment factors using satellite data and in-situ data from summer to fall during the period of 2011~2016. We used daily SST data derived from the AVHRR, the MODIS, and the VIIRS to located cold water area. We also used daily chlorophyll concentration (chl) data from the Geostationary Ocean color Imager (GOCI), geostrophic current data from the AVISO, and wind speed data from the WindSat to the influnce of life a cold water zone. As a result we studied that the cycle of life a cold water zone is repeated in summer season. Also, we found out that the cold water tends to occurred at the end of Jun and disappeared at the end of August. It sees that the chl increment from September to November although after the cold water zone disappeared. On the other hand We found see that this phenomenon comes from inertial influence of cold water zone. -
dc.description.uri 1 -
dc.language English -
dc.publisher Korea -
dc.relation.isPartOf International GOCI Symposium 2016 -
dc.title GOCI, AVHRR, MODIS, VIIRS 등을 이용한 동해안 냉수대의 시공간적인 변화분석 -
dc.title.alternative Temporal and Spatial Variation Analysis of Cold Water in the East/Japan Sea Using GOCI, AVHRR, MODIS and VIIRS -
dc.type Conference -
dc.citation.conferencePlace KO -
dc.citation.endPage 65 -
dc.citation.startPage 65 -
dc.citation.title International GOCI Symposium 2016 -
dc.identifier.bibliographicCitation International GOCI Symposium 2016, pp.65 -
dc.description.journalClass 1 -
Appears in Collections:
Ocean Research, Operations & Support Department > Korea Ocean Satellite Center > 2. Conference Papers
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