Inorganic nutrient distributions in association with thermocline at KOMO station in the northeast equatorial Pacific Ocean during 1995-2002 SCOPUS KCI

DC Field Value Language
dc.contributor.author Son, S.-K. -
dc.contributor.author Son, J.-W. -
dc.contributor.author Kim, K.-H. -
dc.contributor.author Kang, J.-H. -
dc.contributor.author Chi, S.-B. -
dc.contributor.author Yoo, C.M. -
dc.contributor.author Park, C.-K. -
dc.contributor.author Kim, W.-S. -
dc.date.accessioned 2020-04-20T15:40:21Z -
dc.date.available 2020-04-20T15:40:21Z -
dc.date.created 2020-01-28 -
dc.date.issued 2004 -
dc.identifier.issn 1598-141X -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/5347 -
dc.description.abstract Annual variations of inorganic nutrients such as nitrate(+nitrite), phosphate and silicate in association with thermocline were investigated in the upper 200 m of the water column at KODES Long-term Monitoring (KOMO) station in the northeast equatorial Pacific from 1995 to 2002. Global climatic disturbances such as El Niño and La Niña, should have affected KODES area during the study period. In 1995-97 and 2000-2002, a thermocline where temperatures rapidly decrease with depth, was formed at 50-70 m water depth. Nutrient depletion, specially for nitrate and phosphate, was extended down to approximately 50 m depth, which coincided with the surface mixed layer depth. In 1998 and 1999, however a very fluctuating thermocline was observed at 20-100 m water depth. In the photic zone (up to 100 m depth), depth integration of nitrate, phosphate and silicate ranged from 2.02 to 23.14 gN/m2, from 0.87 to 4.05 gP/m2 and from 35.67 to 176.21 gSi/m2, respectively. As a result of changes in the water column structures, nutrient concentrations also showed fluctuation parallel to the changes of thermocline in the study area. -
dc.description.uri 1 -
dc.language Korean -
dc.publisher Korea Ocean Research and Development Institute -
dc.subject annual variation -
dc.subject inorganic matter -
dc.subject nutrient dynamics -
dc.subject thermocline -
dc.subject water column -
dc.subject Pacific Ocean -
dc.subject Pacific Ocean (Equatorial) -
dc.title Inorganic nutrient distributions in association with thermocline at KOMO station in the northeast equatorial Pacific Ocean during 1995-2002 -
dc.type Article -
dc.citation.endPage 384 -
dc.citation.startPage 377 -
dc.citation.title Ocean and Polar Research -
dc.citation.volume 26 -
dc.citation.number 2 -
dc.identifier.bibliographicCitation Ocean and Polar Research, v.26, no.2, pp.377 - 384 -
dc.identifier.doi 10.4217/OPR.2004.26.2.377 -
dc.identifier.scopusid 2-s2.0-3543055845 -
dc.type.docType Article -
dc.identifier.kciid ART000952161 -
dc.description.journalClass 1 -
dc.subject.keywordPlus annual variation -
dc.subject.keywordPlus inorganic matter -
dc.subject.keywordPlus nutrient dynamics -
dc.subject.keywordPlus thermocline -
dc.subject.keywordPlus water column -
dc.subject.keywordPlus Pacific Ocean -
dc.subject.keywordPlus Pacific Ocean (Equatorial) -
dc.subject.keywordAuthor KOMO -
dc.subject.keywordAuthor Nutrient -
dc.subject.keywordAuthor Pacific -
dc.subject.keywordAuthor Thermocline -
dc.description.journalRegisteredClass scopus -
dc.description.journalRegisteredClass kci -
Appears in Collections:
Marine Resources Research Division > Deep-sea Mineral Resources Research Center > 1. Journal Articles
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