황해 중앙부해역에서의 수온약층을 통한 영양염 공급 OTHER

DC Field Value Language
dc.contributor.author Wei Hao -
dc.contributor.author Wang Lei -
dc.contributor.author Lin Yian -
dc.contributor.author 정창수 -
dc.date.accessioned 2020-04-21T07:40:07Z -
dc.date.available 2020-04-21T07:40:07Z -
dc.date.created 2020-01-16 -
dc.date.issued 2002 -
dc.identifier.issn 1671-6647 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/5806 -
dc.description.abstract The difference between the temperature in the upper and lower mixing layers in the Yellow Sea in the stratified season is much greater than that in other coastal areas, but there is still the mass transport across the strong thermocline by means of turbulent entrainment. Based on a mixing layer lodel, the entraninment velocities in the upper and lower layers in the Yellow Sea were calculated, and the observed data during 3 cruises were used to quantatively estimate the nutrient transport across the thermocline in the stratified season. It is shown from the calculation results that the lower layer water is the storage pool of nutrient for the photic zone, which can bring about 15, 9 mgC/m2/d new production to the upper layer in summer and replenish the upper layer with nutrients within half a month. -
dc.description.uri 1 -
dc.language Chinese -
dc.publisher ADVANCES IN MARINE SCIENCE -
dc.title 황해 중앙부해역에서의 수온약층을 통한 영양염 공급 -
dc.title.alternative Nutrient transport across the thermocline in the central Yellow Sea -
dc.type Article -
dc.citation.endPage 20 -
dc.citation.startPage 15 -
dc.citation.title Advances in Marine Science -
dc.citation.volume 20 -
dc.citation.number 3 -
dc.identifier.bibliographicCitation Advances in Marine Science, v.20, no.3, pp.15 - 20 -
dc.description.journalClass 1 -
dc.description.isOpenAccess N -
dc.description.journalRegisteredClass other -
Appears in Collections:
Marine Environmental & Climate Research Division > Marine Environmental Research Center > 1. Journal Articles
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