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Estimation of Turbidity in Coastal Waters using Satellite Data

机译:利用卫星数据估算沿海水域的浊度

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摘要

The assessment of water clarity of any regional water body is particularly important from ecological and water quality perspectives, especially in the regions which are highly influenced by sediment run-off and seasonal fluctuations in turbidity. The ocean colour remote sensing has played a significant role in monitoring the turbidity level in marine and inland water bodies. However, algorithms to accurately estimate the turbidity in such optically complex waters are scarce or limited by high level of uncertainty due to various issues. The present study proposes a simple, two band algorithm to estimate turbidity in both turbid and clear waters. It was found that the band ratio of remote sensing reflectance (R_(rs)(670)/R_(rs)(670)+R_(rs)(555)) represents the proxy of TSS (Total suspended sediment) and therefore, positively correlates to turbidity. The new algorithm is based on the assumption that light reflected in these two vital bands contains the essential information regarding the total suspended matter in the water column. The statistical results showed that the percent mean relative error between the predicted turbidity and the measured turbidity was within ±20%. To further demonstrate the robustness of the present algorithm, the spatial grid contours for the measured and the predicted turbidity was generated for the month of January 2014, August 2013 and May 2012 for the coastal waters in Bay of Bengal (Point Calimere, located in the southeast coast of India). The close consistency between the predicted and measured turbidity spatial patterns revealed that the present algorithm can be applied with high confidence to predict turbidity in both coastal and inland waters.
机译:从生态和水质的角度,评估任何区域水体的水净度尤其重要,尤其是在受到泥沙径流和浊度季节性波动影响较大的地区。海洋颜色遥感在监测海洋和内陆水体的浊度水平方面发挥了重要作用。然而,由于各种问题,用于光学上复杂的水中的浊度的准确估计算法很少或受到高度不确定性的限制。本研究提出了一种简单的两波段算法来估算浑浊和清澈海水中的浊度。发现遥感反射率的谱带比(R_(rs)(670)/ R_(rs)(670)+ R_(rs)(555))代表了TSS(总悬浮泥沙)的代表,因此正与浊度相关。新算法基于这样的假设:在这两个生命带中反射的光包含有关水柱中总悬浮物的基本信息。统计结果表明,预计浊度和测得浊度之间的平均相对误差百分比在±20%之内。为了进一步证明本算法的鲁棒性,针对2014年1月,2013年8月和2012年5月的孟加拉湾沿岸水域(Point Calimere,位于印度东南海岸)。预测和测得的浊度空间模式之间的紧密一致性表明,本算法可以高度可靠地应用于预测沿海和内陆水域的浊度。

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