首页> 外文期刊>ISPRS Journal of Photogrammetry and Remote Sensing >Dynamics of chromophoric dissolved organic matter in Mandovi and Zuari estuaries — A study through in situ and satellite data
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Dynamics of chromophoric dissolved organic matter in Mandovi and Zuari estuaries — A study through in situ and satellite data

机译:Mandovi和Zuari河口发色团溶解的有机物的动力学—通过原位和卫星数据进行的研究

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The spatial and temporal distribution of absorption of chromophoric dissolved organic matter at 440 nm (a_(CDOM) (440)) in the Mandovi and Zuari estuaries situated along the west coast of India, has been analysed. The study was carried out using remotely sensed data, obtained from the Ocean Colour Monitor (OCM) on board the Indian Remote Sensing satellite - P4, together with in situ data during the period January to December 2005. Satellite retrieval of CDOM absorption was carried out by applying an algorithm developed for the site. A good correlation (R = 0.98) was obtained between satellite derived CDOM and in situ data. Time series analysis revealed that spatial distribution of CDOM has a direct link with the seasonal hydrodynamics of the estuaries. The effect of remnant fresh water on CDOM distribution could be analysed by delineating a plume in the offshore region of the Zuari estuary. Though fresh water flux from terrestrial input plays a major role in the distribution of CDOM throughout the Mandovi estuary, its role in the Zuari estuary is significant up to the middle zone. Other processes responsible for feeding CDOM in both the estuaries are coastal advection, in situ production and resuspension of bottom settled sediments. The highest value of a_(Cdom)(440) was observed in the middle zone of the Mandovi estuary during the post-monsoon season. The relation between a_(cdom)(440) and S (spectral slope coefficient of CDOM) could differentiate CDOM introduced in to estuaries through multiple sources. The algorithm developed for the Mandovi estuary is S = 0.003 [a_(cdom) (440)~-0.7091 ] while for the Zuari estuary, S = 0.0031 [a_(CDOM)(440)~-0.777], respectively.
机译:分析了位于印度西海岸的曼多维河和祖阿里河口在440 nm(a_(CDOM)(440))上发色溶解的有机物吸收的时空分布。该研究使用了从印度遥感卫星-P4上的海洋色彩监测器(OCM)获得的遥感数据以及2005年1月至12月期间的原位数据进行。对CDOM吸收的卫星进行了检索通过应用针对该站点开发的算法。卫星导出的CDOM与原位数据之间具有良好的相关性(R = 0.98)。时间序列分析表明,CDOM的空间分布与河口的季节性水动力有直接联系。剩余淡水对CDOM分布的影响可以通过在Zuari河口近海区域划出羽状流来进行分析。尽管来自陆地输入的淡水通量在整个Mandovi河口的CDOM分布中起着主要作用,但它在Zuari河口直到中部地区的作用都很大。在这两个河口中喂食CDOM的其他过程是海岸平流,原位生产和底部沉降沉积物的重新悬浮。季风后季节,在曼多维河口中部观测到a_(Cdom)(440)的最大值。 a_(cdom)(440)和S(CDOM的光谱斜率系数)之间的关系可以区分通过多个源引入河口的CDOM。为Mandovi河口开发的算法分别为S = 0.003 [a_(cdom)(440)〜-0.7091],而对于Zuari河口,开发的算法分别为S = 0.0031 [a_(CDOM)(440)〜-0.777]。

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