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dc.contributor.authorLin, IIen_US
dc.contributor.authorWen, LSen_US
dc.contributor.authorLiu, KKen_US
dc.contributor.authorTsai, WTen_US
dc.contributor.authorLiu, AKen_US
dc.date.accessioned2014-12-08T15:42:24Z-
dc.date.available2014-12-08T15:42:24Z-
dc.date.issued2002-05-15en_US
dc.identifier.issn0094-8276en_US
dc.identifier.urihttp://dx.doi.org/10.1029/2001GL014039en_US
dc.identifier.urihttp://hdl.handle.net/11536/28789-
dc.description.abstract[1] Near simultaneously (within 2 hours) acquired ERS-2 Synthetic Aperture Radar (SAR) and Sea-viewing Wide Field-of-view Scanner (SeaWiFS) data over an upwelling region shows remarkable similarity in feature's location, scale, and boundary. Under uniform wind and sea states, reduction of Normalised Radar Cross Section (NRCS) from SAR is found highly correlated with the increase of SeaWiFS Chlorophyll-a (Chl-a) concentration. Typically, 1 mg/m3 of chlorophyll-a is correspondent with a 5 dB reduction of NRCS. This relationship is supported by simultaneously collected in situ sea truth measurements. This work provides a direct evidence and exceptional quantification of the relationship between radar backscatter and ocean colour that has long been speculated.en_US
dc.language.isoen_USen_US
dc.titleEvidence and quantification of the correlation between radar backscatter and ocean colour supported by simultaneously acquired in situ sea truthen_US
dc.typeArticleen_US
dc.identifier.doi10.1029/2001GL014039en_US
dc.identifier.journalGEOPHYSICAL RESEARCH LETTERSen_US
dc.citation.volume29en_US
dc.citation.issue10en_US
dc.citation.epageen_US
dc.contributor.department交大名義發表zh_TW
dc.contributor.departmentNational Chiao Tung Universityen_US
dc.identifier.wosnumberWOS:000178888300042-
dc.citation.woscount9-
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