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Characteristics of mesozooplankton sound-scattering layer in the Pacific Summer Water, Arctic Ocean

Cited 7 time in wos
Cited 8 time in scopus

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DC Field Value Language
dc.contributor.authorLa, Hyoung Sul-
dc.contributor.authorKang, Myounghee-
dc.contributor.authorDahms, Hans-Uwe-
dc.contributor.authorHa, Ho Kyung-
dc.contributor.authorYang, Eun Jin-
dc.contributor.authorLee, Hyungbeen-
dc.contributor.authorKim, Young-Nam-
dc.contributor.authorChung, Kyung Ho-
dc.contributor.authorKang, Sung-Ho-
dc.coverage.spatialCananda Basin-
dc.coverage.spatialArctic Ocean-
dc.coverage.spatialCanada Basin-
dc.date.accessioned2017-08-03T13:41:48Z-
dc.date.available2017-08-03T13:41:48Z-
dc.date.issued2015-
dc.description.abstractThis study investigated the variations in the sound-scatteringlayer(SSL) that were reflected from the mesozooplankton communities around the Northwind Ridge in the western Arctic Ocean.A multi-frequency acoustic survey was conducted to reveal the SSL distribution dominated by Arctic copepodsin the early summer of 2010.The SSL distribution was well correlated with the salinity,nutrients and chlorophyll <em>a</em> (chl-α) associated with the features of the Pacific Summer Water(PSW).TheSSL was observed primarily in the upper most100m of the PSW,which provided a desirable habitat for Arctic copepods due to high nutrients and phytoplankton biomass.The highest density SSL was observed in the eddy-like structure of the PSW,which is most likely because of the high nutrients and chl-α. High regional densities in the SSL indicated that Arctic copepods provide a large portion of the biomass and contribution to the foodwebs in the PSW,in the western Arctic Ocean.-
dc.languageEnglish-
dc.subjectOceanography-
dc.subject.classificationAraon-
dc.titleCharacteristics of mesozooplankton sound-scattering layer in the Pacific Summer Water, Arctic Ocean-
dc.typeArticle-
dc.identifier.bibliographicCitationLa, Hyoung Sul, et al. 2015. "Characteristics of mesozooplankton sound-scattering layer in the Pacific Summer Water, Arctic Ocean". <em>Deep-Sea Research II</em>, 120: 114-123.-
dc.citation.titleDeep-Sea Research II-
dc.citation.volume120-
dc.citation.page114-123.-
dc.citation.conferenceDate3890m-
dc.identifier.doi10.1016/j.dsr2.2015.01.005-
dc.coverage.x75ºN-
dc.coverage.x75.002°N-
dc.coverage.x75.216°N-
dc.coverage.x75.992°N-
dc.coverage.y160ºE-
dc.coverage.y157.508'E-
dc.coverage.y156.047°E-
dc.coverage.y156.992°E-
dc.coverage.z2000m-
dc.coverage.z1300m-
dc.coverage.z940m-
dc.coverage.z3890m-
dc.subject.keywordArctic Ocean-
dc.subject.keywordCanada Basin-
dc.subject.keywordNorthwind Ridge-
dc.subject.keywordSound-scattering layer-
dc.subject.keywordArctic copepods-
dc.subject.keywordEddy-
dc.subject.keywordPacific Summer Water-
dc.subject.keywordAraon-
dc.coverage.degreeX75.002-
dc.coverage.degreeX75.216-
dc.coverage.degreeX75.992-
dc.coverage.degreeX75-
dc.coverage.degreeY157.508-
dc.coverage.degreeY156.047-
dc.coverage.degreeY156.992-
dc.coverage.degreeY160-
dc.identifier.scopusid2-s2.0-84942192753-
dc.identifier.wosid000362610700012-
Appears in Collections  
2011-2016, Korea Polar Ocean in Rapid Transition (K-PORT) / Kang, Sung-Ho (PM11080; PM12020; PM13020; PM14040; PM14040; PM15040)
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