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Improved turbidity estimates in complex inland waters using combined NIR-SWIR atmospheric correction approach for Landsat 8 OLI data

机译:使用Landsat 8 OLI数据的组合NIR-SWIR大气校正方法改进复杂内陆水域的浊度估算

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Turbidity is one of the important water quality parameters, essentially a proxy to assess eutrophication state in inland coastal systems. In this article, a method of combined near-infrared-shortwave infrared (NIR-SWIR) atmospheric correction for Landsat 8 (L8) Operational Land Imager data is proposed to improve the turbidity retrieval in optically complex waters. From the extremely turbid to moderately turbid waters, the relative ranges in water-leaving reflectance in band 3 (rho(3)(w)) are found to be 19-92% and 31-79% in band 4 (rho(4)(w)). The SWIR reflectances in rho(4)(w) and rho(3)(w) are 57% and 66% higher than that of standard NIR correction in extremely turbid waters. However, this method has resulted in similar to 30% higher reflectances than the NIR method in relatively less turbid waters; the latter method is still good in moderately turbid waters. Using Rayleigh corrected reflectances, a turbidity index, T-ind (865; 1610), was computed to discriminate the productive and/or turbid waters. The SWIR method was applied for water having T-ind 1.5 threshold and the NIR method in the other regions. A new turbidity algorithm has been developed using L8 two band ratio (rho(4)(w) = rho(3)(w)) optimized with in situ turbidity data from four data buoys for 2014. The Landsat 8 band-weighted in situ reflectances for bands 3 and 4 are used to derive turbidity using the present algorithm and validated against in situ turbidity, providing a good coefficient of determination of R-2 = 0.87. As compared to the NIR-based correction, the turbidity obtained from the combined (NIR + SWIR) correction in extremely turbid waters is around 80-90% (absolute percentage difference (APD)) different. Whereas in the moderately turbid waters, the APD between the two corrections was around 50-75%. There are no obvious data discontinuities in using the combined approach. Comparisons were made with available single-band turbidity algorithms and found that the present turbidity algorithm performed well in the optically complex lagoon environment.
机译:浊度是重要的水质参数之一,本质上是评估内陆沿海系统富营养化状态的指标。本文提出了一种结合Landsat 8(L8)陆地成像仪数据的近红外-短波红外(NIR-SWIR)大气校正方法,以改善光学复杂水中的浊度反演。从极浑浊的水到中等浑浊的水,发现频带3(rho(3)(w))中的离水反射率的相对范围在频带4(rho(4)中为19-92%和31-79% (w))。在极端浑浊的水中,rho(4)(w)和rho(3)(w)的SWIR反射率比标准NIR校正分别高57%和66%。但是,在相对浑浊的水中,这种方法的反射率比NIR方法高出近30%。后一种方法在中度浑浊的水域中仍然很好。使用瑞利校正的反射率,计算浊度指数T-ind(865; 1610)来区分生产水和/或浊水。 SWIR方法应用于T-ind> 1.5阈值的水,其他区域采用NIR方法。已经开发了一种新的浊度算法,该算法使用L8的两个波段比率(rho(4)(w)= rho(3)(w))进行了优化,并使用来自四个数据浮标的2014年现场浊度数据进行了优化。Landsat 8波段加权原位使用本算法,将波段3和波段4的反射率用于得出浊度,并针对原位浊度进行验证,从而提供了良好的R-2 = 0.87的确定系数。与基于NIR的校正相比,在极浑浊的水中,通过组合(NIR + SWIR)校正获得的浊度大约相差80-90%(绝对百分比差(APD))。而在中度浑浊的水中,两次校正之间的APD约为50-75%。使用组合方法没有明显的数据不连续性。与可用的单波段浊度算法进行了比较,发现本浊度算法在光学复杂的泻湖环境中表现良好。

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