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Atmospheric Correction Performance of Hyperspectral Airborne Imagery over a Small Eutrophic Lake under Changing Cloud Cover

机译:变化的云量下小富营养化湖泊高光谱航空影像的大气校正性能

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摘要

Atmospheric correction of remotely sensed imagery of inland water bodies is essentialudto interpret water-leaving radiance signals and for the accurate retrieval of water quality variables.udAtmospheric correction is particularly challenging over inhomogeneous water bodies surrounded byudcomparatively bright land surface. We present results of AisaFENIX airborne hyperspectral imageryudcollected over a small inland water body under changing cloud cover, presenting challenging butudcommon conditions for atmospheric correction. This is the first evaluation of the performance ofudthe FENIX sensor over water bodies. ATCOR4, which is not specifically designed for atmosphericudcorrection over water and does not make any assumptions on water type, was used to obtainudatmospherically corrected reflectance values, which were compared to in situ water-leavingudreflectance collected at six stations. Three different atmospheric correction strategies in ATCOR4udwas tested. The strategy using fully image-derived and spatially varying atmospheric parametersudproduced a reflectance accuracy of �0.002, i.e., a difference of less than 15% compared to the in situudreference reflectance. Amplitude and shape of the remotely sensed reflectance spectra were in generaludaccordance with the in situ data. The spectral angle was better than 4.1� for the best cases, in theudspectral range of 450–750 nm. The retrieval of chlorophyll-a (Chl-a) concentration using a popularudsemi-analytical band ratio algorithm for turbid inland waters gave an accuracy of ~16% or 4.4 mg/m3udcompared to retrieval of Chl-a from reflectance measured in situ. Using fixed ATCOR4 processingudparameters for whole images improved Chl-a retrieval results from ~6 mg/m3 difference to referenceudto approximately 2 mg/m3. We conclude that the AisaFENIX sensor, in combination with ATCOR4udin image-driven parametrization, can be successfully used for inland water quality observations.udThis implies that the need for in situ reference measurements is not as strict as has been assumed anduda high degree of automation in processing is possible.
机译:内陆水体遥感图像的大气校正对于解释留水辐射信号和准确获取水质变量至关重要。对于大气比较明亮的陆地所包围的非均质水体,大气校正尤其具有挑战性。我们介绍了在变化的云层覆盖下的小内陆水体上收集的AisaFENIX机载高光谱图像的结果,提出了具有挑战性但不常见的大气校正条件。这是对FENIX传感器在水体上性能的首次评估。 ATCOR4不是专门为水上的大气非校正设计的,并且没有对水的类型做出任何假设,用于获得大气压校正的反射率值,并将其与在六个站点收集的原位留水非反射率进行了比较。测试了ATCOR4 ud中的三种不同的大气校正策略。使用完全源自图像并在空间上变化的大气参数的策略得出的反射率精度为±0.002,即与原位/参考反射率的差异小于15%。遥感反射光谱的幅度和形状一般与原位数据不符。在450-750 nm的超光谱范围内,最佳情况下的光谱角优于4.1°。使用常见的 udsemi-analytical能谱比算法对内陆浑浊的水域中的叶绿素a(Chl-a)浓度进行反演,其准确度约为16%或4.4 mg / m3 ud,与通过在C1a中测得的反射率反演Chl-a相比原地。对整个图像使用固定的ATCOR4处理超参数可改善Chl-a检索结果,从〜6 mg / m3到参考值的ud ud至大约2 mg / m3。我们得出的结论是,AisaFENIX传感器与ATCOR4 udin图像驱动的参数化结合可以成功地用于内陆水质观测。 ud这意味着对原位参考测量的要求并不像以前设想的那么严格。高度自动化的处理是可能的。

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