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dc.contributor國立臺灣師範大學海洋環境科技研究所zh_tw
dc.contributor.authorTseng, C.-M.en_US
dc.contributor.authorG. T. F. Wongen_US
dc.contributor.authorI-I Linen_US
dc.contributor.authorC.-R. Wuen_US
dc.contributor.authorK.-K. Liuen_US
dc.date.accessioned2014-12-02T06:42:33Z-
dc.date.available2014-12-02T06:42:33Z-
dc.date.issued2005-04-01zh_TW
dc.identifierntnulib_tp_C1001_01_002zh_TW
dc.identifier.urihttp://rportal.lib.ntnu.edu.tw/handle/77345300/42845-
dc.description.abstractA distinctive seasonal pattern in phytoplankton biomass was observed at the South East Asian Time-series Study (SEATS) station (18°N, 116°E) in the northern South China Sea (SCS). Surface chlorophyll-a, depth-integrated chlorophyll-a and primary production were elevated to 0.3 mg/m3, ∼35 mg/m2 and 300 mg-C/m2/d, respectively, in the winter but stayed low, at ≤0.1 mg/m3, ∼15 mg/m2 and 110 mg-C/m2/d as commonly found in other low latitude waters, in the rest of the year. Concomitantly, soluble reactive phosphate and nitrate+nitrite in the mixed layer also became readily detectable in the winter. The elevation of phytoplankton biomass coincided approximately with the lowest sea surface temperature and the highest wind speed in the year. Only the combined effect of convective overturn by surface cooling and wind-induced mixing could have enhanced vertical mixing sufficiently to make the nutrients in the upper nutricline available for photosynthetic activities and accounted for the higher biomass in the winter.en_US
dc.description.urihttp://phyoce.geos.ntnu.edu.tw/pdf/GRL_A%20unique%20seasonal%20pattern%20in%20phytoplankton%20biomass%20in%20low-latitude%20waters%20in%20the%20South%20China%20Sea.pdfzh_TW
dc.languageen_USzh_TW
dc.relationGeophysical Research Letters, 32(8), L08608.en_US
dc.relation.urihttp://dx.doi.org/10.1029/2004GL022111zh_TW
dc.titleA unique seasonal pattern in phytoplankton biomass in low-latitude waters in the South China Seaen_US
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