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Spectral slopes of the absorption coefficient of colored dissolved and detrital material inverted from UV-visible remote sensing reflectance

机译:紫外可见遥感反射率反演的有色溶解和碎屑物质吸收系数的光谱斜率

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摘要

The spectral slope of the absorption coefficient of colored dissolved and detrital material (CDM), Scdm (units: nm−1), is an important optical parameter for characterizing the absorption spectral shape of CDM. Although highly variable in natural waters, in most remote sensing algorithms, this slope is either kept as a constant or empirically modeled with multiband ocean color in the visible domain. In this study, we explore the potential of semianalytically retrieving Scdm with added ocean color information in the ultraviolet (UV) range between 360 and 400 nm. Unique features of hyperspectral remote sensing reflectance in the UV-visible wavelengths (360–500 nm) have been observed in various waters across a range of coastal and open ocean environments. Our data and analyses indicate that ocean color in the UV domain is particularly sensitive to the variation of the CDM spectral slope. Here, we used a synthesized data set to show that adding UV wavelengths to the ocean color measurements will improve the retrieval of Scdm from remote sensing reflectance considerably, while the spectral band settings of past and current satellite ocean color sensors cannot fully account for the spectral variation of remote sensing reflectance. Results of this effort support the concept to include UV wavelengths in the next generation of satellite ocean color sensors.
机译:有色溶解和碎屑物质(CDM)的吸收系数Scdm的光谱斜率(单位:nm -1 )是表征CDM吸收光谱形状的重要光学参数。尽管在自然水域中变化很大,但是在大多数遥感算法中,该斜率要么保持不变,要么在可见域中用多波段海洋颜色进行经验建模。在这项研究中,我们探索了在360至400 nm的紫外线(UV)范围内半解析检索Scdm以及添加海洋颜色信息的潜力。在一系列沿海和远洋环境的各种水域中,已经观察到了紫外线可见波长(360-500 nm)中的高光谱遥感反射率的独特特征。我们的数据和分析表明,UV域中的海洋颜色对CDM光谱斜率的变化特别敏感。在这里,我们使用了一个综合数据集来表明,将紫外线波长添加到海洋颜色测量中将大大改善遥感反射率对Scdm的检索,而过去和当前的卫星海洋颜色传感器的光谱带设置无法完全说明光谱遥感反射率的变化。这项努力的结果支持了将紫外线波长包括在下一代卫星海洋颜色传感器中的概念。

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