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首页> 外文期刊>Journal of Geophysical Research, C. Oceans: JGR >Remote sensing of salinity from satellite-derived CDOM in the Changjiang River dominated East China Sea
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Remote sensing of salinity from satellite-derived CDOM in the Changjiang River dominated East China Sea

机译:来自长江以东海为主的卫星CDOM的盐度遥感

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[1] Defining highly variable freshwater plume area from space is important for characterizing the dynamics of biogeochemical properties and understanding the effects of climate change and human activities on plume-related processes. The absorption coefficient of colored dissolved organic matter (aCDOM) from satellite ocean color data can be used to estimate the salinity and thus the plume area in coastal oceans if a robust conservative salinity and aCDOM relationship and an accurate satellite aCDOM algorithm can be established. In this paper, tight relationships between surface water salinity and in situ aCDOM were found during several cruises covering all seasons and the full salinity range in the East China Sea. Thus, a salinity inversion model from aCDOM was developed and validated with an independent data set, in which 73.6% of the data were within the absolute salinity error of ±1 and 87.1% were within ±1.5. Factors influencing the conservative behavior of colored dissolved organic matter are analyzed, with a particular focus on the effect of the phytoplankton-induced autochthonous colored dissolved organic matter. In addition, several satellite aCDOM algorithms were compared and validated with our in situ data. Monthly satellite-derived salinity images were mapped in August from 2008 to 2010 and showed the significant interannual variability in the plume coverage. This study demonstrated that the salinity derived from satellite-derived aCDOM can provide a reliable and good synoptic view of the plume area, and help with biogeochemical studies, in particular, those properties related to the interannual variability of plume coverage, although the development of a localized satellite algorithm of aCDOM is still desirable.
机译:[1]从太空中定义高度变化的淡水羽流区域对于表征生物地球化学特性的动力学以及理解气候变化和人类活动对羽流相关过程的影响非常重要。如果可以建立稳健的保守盐度和aCDOM关系以及精确的卫星aCDOM算法,那么来自卫星海洋颜色数据的有色溶解有机物(aCDOM)的吸收系数可用于估算盐度,从而估算沿海海洋的羽流面积。在本文中,在涵盖东海所有季节和整个盐度范围的几次航行中,发现了地表水盐度与原位aCDOM之间的紧密关系。因此,开发了aCDOM的盐度反演模型并使用独立的数据集进行了验证,其中73.6%的数据在绝对盐度误差内为±1,87.1%的数据在±1.5之内。分析了影响有色溶解有机物保守行为的因素,特别关注浮游植物诱导的自生有色溶解有机物的影响。此外,还比较了几种卫星aCDOM算法,并用我们的现场数据进行了验证。从2008年至2010年8月,绘制了每月一次的卫星盐度图像,这些图像显示出羽流覆盖率的年际变化很大。这项研究表明,源自卫星的aCDOM所获得的盐度可以提供可靠且良好的羽流区域概要信息,并有助于进行生物地球化学研究,特别是与羽流覆盖率年际变化有关的那些特性,虽然仍然需要aCDOM的本地化卫星算法。

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