여름철 황해남동부 지역에서 냉수와 태풍이 SCM 형성에 미치는 영향

DC Field Value Language
dc.contributor.author 장풍국 -
dc.contributor.author 신경순 -
dc.contributor.author 이석 -
dc.contributor.author 차형곤 -
dc.contributor.author 권오윤 -
dc.contributor.author 강정훈 -
dc.date.accessioned 2020-07-16T03:34:27Z -
dc.date.available 2020-07-16T03:34:27Z -
dc.date.created 2020-02-11 -
dc.date.issued 2014-10-01 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/26002 -
dc.description.abstract To study the influences of physical process on phytoplankton biomass in the shallow marginal sea, spatial and temporal variations in physiochemical parameters in southeastern Yellow Sea (YS) were investigated in summer of 2010 to 2013. The temperature of surface waters mostly were over 25oC except for 2011 when it mostly around 20oC. The low salinity (<31) of surface water were observed in 2012 and 2013. The subsurface chlorophyll maximum (SCM) layer become shallow from open sea to coastal sea and formed within thermocline and over nitracline, which may be related with tidal fronts in the southeastern YS. Of the environmental parameters in 2011 when the strong typhoon passed through the center of Yellow Sea three days ago, before measured, the concentration of nutrient and chlorophyll-a (Chl-a) in the upper layer was demonstrated to be present at the high levels compared to that in other years. The Yellow Sea Cold Water (YSCW) may rapidly lead to natural recover of water stability after the passage of typhoon in the YS, which may be an important parameter in the distribution of Chl-a concentration after the summer typhoon. These results suggest that the distribution of nutrients and chlorophyll-a concentration in the YS may be mainly affected on the formed front between warm and cold water masses, and the path of typhoon during summer.temperature of surface waters mostly were over 25oC except for 2011 when it mostly around 20oC. The low salinity (<31) of surface water were observed in 2012 and 2013. The subsurface chlorophyll maximum (SCM) layer become shallow from open sea to coastal sea and formed within thermocline and over nitracline, which may be related with tidal fronts in the southeastern YS. Of the environmental parameters in 2011 when the strong typhoon passed through the center of Yellow Sea three days ago, before measured, the concentration of nutrient and chlorophyll-a (Chl-a) in the upper layer was demonstrated to be present at the high levels compared to that in other years. The Yellow Sea Cold Water (YSCW) may rapidly lead to natural recover of water stability after the passage of typhoon in the YS, which may be an important parameter in the distribution of Chl-a concentration after the summer typhoon. These results suggest that the distribution of nutrients and chlorophyll-a concentration in the YS may be mainly affected on the formed front between warm and cold water masses, and the path of typhoon during summer. -
dc.description.uri 1 -
dc.language English -
dc.publisher The -
dc.relation.isPartOf Asian Marine Biology Symposium -
dc.title 여름철 황해남동부 지역에서 냉수와 태풍이 SCM 형성에 미치는 영향 -
dc.title.alternative The effect of cold water and typhoon on the formation of subsurface chlorophyll maximum in the southeastern Yellow Sea during summer from 2010 to 2013 -
dc.type Conference -
dc.citation.conferencePlace KO -
dc.citation.endPage 230 -
dc.citation.startPage 230 -
dc.citation.title Asian Marine Biology Symposium -
dc.contributor.alternativeName 장풍국 -
dc.contributor.alternativeName 신경순 -
dc.contributor.alternativeName 이석 -
dc.contributor.alternativeName 차형곤 -
dc.contributor.alternativeName 권오윤 -
dc.contributor.alternativeName 강정훈 -
dc.identifier.bibliographicCitation Asian Marine Biology Symposium, pp.230 -
dc.description.journalClass 1 -
Appears in Collections:
South Sea Research Institute > Ballast Water Research Center > 2. Conference Papers
South Sea Research Institute > Risk Assessment Research Center > 2. Conference Papers
Ocean Climate Solutions Research Division > Ocean Circulation & Climate Research Department > 2. Conference Papers
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