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首页> 外文期刊>ISPRS Journal of Photogrammetry and Remote Sensing >Improved atmospheric correction and chlorophyll-a remote sensing models for turbid waters in a dusty environment
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Improved atmospheric correction and chlorophyll-a remote sensing models for turbid waters in a dusty environment

机译:改进的大气校正和叶绿素-多尘环境中浑浊水域的遥感模型

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This study presents a comprehensive assessment of the performance of the commonly used atmospheric correction models (NIR, SWIR, NIR-SWIR and FM) and ocean color products (OC3 and OC2) derived from MODIS images over the Arabian Gulf, Sea of Oman, and Arabian Sea. The considered atmospheric correction models have been used to derive MODIS normalized water-leaving radiances (nL(w)), which are compared to in situ water nL(w)(lambda) data collected at different locations by Masdar Institute, United Arab of Emirates, and from AERONET-OC (the ocean color component of the Aerosol Robotic Network) database. From this comparison, the NIR model has been found to be the best performing model among the considered atmospheric correction models, which in turn shows disparity, especially at short wavelengths (400-500 nm) under high aerosol optical depth conditions (AOT (869) > 0.3) and over turbid waters. To reduce the error induced by these factors, a modified model taking into consideration the atmospheric and water turbidity conditions has been proposed. A turbidity index was used to identify the turbid water and a threshold of AOT (869) = 0.3 was used to identify the dusty atmosphere. Despite improved results in the MODIS nL(w)(2) using the proposed approach, Chl-a models (OC3 and OC2) show low performance when compared to the in situ Chl-a measurements collected during several field campaigns organized by local, regional and international organizations. This discrepancy might be caused by the improper parametrization of these models or/and the improper selection of bands. Thus, an adaptive power fit algorithm (R-2 = 0.95) has been proposed to improve the estimation of Chl-a concentration from 0.07 to 10 mg/m(3) by using a new blue/red MODIS band ratio of (443,488)/645 instead of the default band ratio used for OC3(443,488)/547. The selection of this new band ratio (443,488)/645 has been based on using band 645 nm which has been found to represent both water turbidity and algal absorption. (C) 2017 International Society for Photogrammetry and Remote Sensing, Inc. (ISPRS). Published by Elsevier B.V. All rights reserved.
机译:这项研究对从阿拉伯海湾,阿曼海和阿联酋的MODIS影像得出的常用大气校正模型(NIR,SWIR,NIR-SWIR和FM)和海洋色彩产品(OC3和OC2)的性能进行了全面评估。阿拉伯海。考虑的大气校正模型已用于导出MODIS归一化的放水辐射率(nL(w)),并将其与阿拉伯联合酋长国马斯达尔研究所在不同地点收集的现场水nL(w)(lambda)数据进行比较,以及来自AERONET-OC(Aerosol机器人网络的海洋颜色组件)数据库。通过这种比较,已发现在考虑的大气校正模型中,NIR模型是性能最佳的模型,这反过来又显示出差异,尤其是在高气溶胶光学深度条件下(AOT(869))在短波长(400-500 nm)下> 0.3)和浑浊的水域。为了减少这些因素引起的误差,提出了一种考虑大气和水浊度条件的改进模型。使用浊度指数来识别浑浊的水,使用AOT阈值(869)= 0.3来识别尘土飞扬的气氛。尽管使用建议的方法在MODIS nL(w)(2)中获得了改进的结果,但与在本地,区域性组织的几次野战中收集的现场Chl-a测量值相比,Chl-a模型(OC3和OC2)显示出较低的性能。和国际组织。这种差异可能是由于这些模型的参数化不当或/和频段选择不当造成的。因此,提出了一种自适应功率拟合算法(R-2 = 0.95),通过使用新的蓝/红MODIS谱带比(443,488)将Chl-a浓度的估计值从0.07提高到10 mg / m(3)。 / 645,而不是OC3(443,488)/ 547使用的默认带宽比率。选择新的谱带比(443,488)/ 645是基于使用645 nm谱带,已发现该谱带既代表水浊度又代表藻类吸收。 (C)2017国际摄影测量与遥感学会(ISPRS)。由Elsevier B.V.发布。保留所有权利。

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