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首页> 外文期刊>TAO: Terrastrial, atmospheric, and oceanic sciences >NOTES AND CORRESPONDENCE Unique Dispersal of the Changjiang-Diluted Water Plume in the East China Sea Revealed from Satellite Monitoring of Colored Dissolved Organic Matter (CDOM)
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NOTES AND CORRESPONDENCE Unique Dispersal of the Changjiang-Diluted Water Plume in the East China Sea Revealed from Satellite Monitoring of Colored Dissolved Organic Matter (CDOM)

机译:注释和对应从有色溶解有机物(CDOM)卫星监测中揭示的东海长江稀水流的独特扩散

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The optical properties of colored dissolved organic matter (CDOM) in the Changjiang (Yangtze River) plume water were investigated during the summer of 2009 and 2010. The absorption coefficient of CDOM at 325 nm (aCDOM) increased inversely with decreasing sea-surface salinity (SSS), implying that aCDOM can be used as a natural tracer of Changjiang-diluted water (CDW). This aCDOM vs. SSS relationship, however, differed between 2009 and 2010. For mapping the CDW plume, the aCDOM was retrieved from an ocean-color satellite. Values of SSS were also derived from the satellite-retrieved aCDOM using field-based SSS vs. aCDOM relationships. Satellite observations revealed the temporary variable eastward extension of a high aCDOM, low SSS CDW plume in the central East China Sea (ECS) during the summer. The CDW plume during the summer of 2010 extended southeastward from the mouth of the Changjiang (Yangtze River) to almost 26°N. Moreover, the branch of this southeastward CDW plume was seen to extend northeastward to the eastern ECS where the Kuroshio Current flows northeastward along the shelf break. Subsequently, this branch was distributed around southern Kyushu. Satellite observations revealed this unique dispersal of the CDW plume, which illustrates that the aCDOM and SSS from ocean-color satellite data are useful for monitoring the dispersal of this river-water plume.
机译:研究了2009年夏季和2010年夏季长江羽水中有色溶解有机物(CDOM)的光学性质。CDOM在325 nm(aCDOM)的吸收系数与海表盐度的降低成反比( SSS),这意味着aCDOM可以用作长江稀释水(CDW)的天然示踪剂。但是,aCDOM与SSS的关系在2009年和2010年之间有所不同。为了绘制CDW羽流,从海洋彩色卫星中检索了aCDOM。 SSS的值也使用基于现场的SSS与aCDOM关系从卫星检索的aCDOM中得出。卫星观测结果显示,夏季,东中国海(ECS)中高aCDOM,低SSS CDW羽流向东临时扩展。 CDW羽流在2010年夏季从长江(长江)河口向东南延伸至近26°N。此外,该CDW烟羽向东南延伸的分支被认为是向东北延伸到东部ECS,在那里黑潮潮流沿架子断裂向东北流动。随后,该分支机构分布在九州南部。卫星观测揭示了CDW羽流的这种独特散布,这说明来自海洋彩色卫星数据的aCDOM和SSS可用于监视这种河水羽流的散布。

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