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Spectral signature of highly turbid waters application with SPOT data to quantify suspended particulate matter concentrations

机译:使用SPOT数据对高浊水应用的光谱特征进行量化,以量化悬浮颗粒物的浓度

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摘要

An experimental method for determining water composition from "ocean colour" satellite data, in visible and near-infrared (("1IR) wavelengths, is applied to highly turbid waters. Numerous spectroradiometric measurements are carried out in the Gironde estuary, for suspended particulate matter (SPM) concentrations ranging between 35 and more than 2000 mg l{sup}(-1). Empirical relationships are established between remote-sensing reflectance (R{sub}(rs)) in SPOT-HRV bands and SPM concentration through these numerous in situ measurements. We observed that remote-sensing reflectance increases with SPM concentration and that the SPOT bands saturate at the highest turbidities. The best correlations are obtained for the NIR band X53 (790-890 nm) and for the reflectance ratios: R{sub}(rs)(XS3)/R{sub}(rs)(XS1) and R{sub}(rs)(XS3)/R{sub}(rs)(XS2). The XS1 and XS2 visible bands are only used to determine SPM concentrations in the lower pan of the estuary (where the SPM concentrations are lower). As a result, SPM concentrations within the surface waters in the estuary are estimated up to 2000 mg l{sup}(-1) with an accuracy better than ±35%. The algorithm is finally applied to a SPOT scene. Satellite data are corrected for atmospheric effects using a radiative transfer code and in situ reflectance measurements; as a result, the horizontal distribution of SPM is retrieved. Moreover, the high spatial resolution HRV-SPOT sensor shows detailed sedimentary flows, especially in the visible XS1 and XS2 spectral bands.
机译:一种用于根据“海洋颜色”卫星数据确定可见光和近红外(“ 1IR”波长)水成分的实验方法,该方法适用于浑浊度很高的水。在吉伦特河口进行了许多分光光度法测量悬浮颗粒物(SPM)浓度在35到2000 mg l {sup}(-1)之间,通过这些大量的SPOT-HRV波段的遥感反射率(R {sub}(rs))和SPM浓度之间建立了经验关系我们观察到,遥感反射率随SPM浓度的增加而增加,SPOT谱带在最高浊度时饱和。对于NIR谱带X53(790-890 nm)和反射率比,R {{ sub}(rs)(XS3)/ R {sub}(rs)(XS1)和R {sub}(rs)(XS3)/ R {sub}(rs)(XS2)。仅XS1和XS2可见带用于确定河口下部平底锅(其中SPM浓度较低)中的SPM浓度。结果,估计河口地表水中SPM的浓度高达2000 mg l {sup}(-1),准确度优于±35%。该算法最终应用于SPOT场景。使用辐射传输代码和原位反射率测量对卫星数据进行大气影响校正;结果,检索了SPM的水平分布。此外,高空间分辨率HRV-SPOT传感器显示出详细的沉积流,特别是在可见的XS1和XS2光谱带中。

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