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Adaptive semianalytical inversion of ocean color radiometry in optically complex waters

机译:光学复杂水中海洋颜色辐射度的自适应半解析反演

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摘要

To address the challenges of the parameterization of ocean color inversion algorithms in optically complex waters, we present an adaptive implementation of the linear matrix inversion method (LMI) [J. Geophys. Res. 101, 16631 (1996)], which iterates over a limited number of model parameter sets to account for naturally occurring spatial or temporal variability in inherent optical properties (IOPs) and concentration specific IOPs (SIOPs). LMI was applied to a simulated reflectance dataset for spectral bands representing measured water properties of a macrotidal embayment characterized by a large variability in the shape and amplitude factors controlling the IOP spectra. We compare the inversion results for the single-model parameter implementation to the adaptive parameterization of LMI for the retrieval of bulk IOPs, the IOPs apportioned to the optically active constituents, and the concentrations of the optically active constituents. We found that ocean color inversion with LMI is significantly sensitive to the a priori selection of the empirical parameters g_(0) and g_(1) of the equations relating the above-surface remote-sensing reflectance to the IOPs in the water column [J. Geophys. Res. 93, 10909 (1988)]. When assuming the values proposed for open-ocean applications for g_(0) and g_(1) [J. Geophys. Res. 93, 10909 (1988)], the accuracy of the retrieved IOPs, and concentrations was substantially lower than that retrieved with the parameterization developed for coastal waters [Appl. Opt. 38, 3831 (1999)] because the optically complex waters analyzed in this study were dominated by particulate and dissolved matter. The adaptive parameterization of LMI yielded consistently more accurate inversion results than the single fixed SIOP model parameterizations of LMI. The adaptive implementation of LMI led to an improvement in the accuracy of apportioned IOPs and concentrations, particularly for the phytoplankton-related quantities. The adaptive parameterization encompassing wider IOP ranges were more accurate for the retrieval of bulk IOPs, apportioned IOPs, and concentration of optically active constituents.
机译:为了解决光学复杂水域中海洋颜色反演算法参数化的挑战,我们提出了线性矩阵反演方法(LMI)的自适应实现。地理学。 Res。 101,16631(1996)],它在有限数量的模型参数集上进行迭代,以解决固有光学特性(IOP)和浓度特定IOP(SIOP)中自然发生的空间或时间变化。将LMI应用于模拟反射率数据集的光谱带,该光谱带表示测量到的潮汐带水域水质特征,其特征在于控制IOP光谱的形状和幅度因子存在较大差异。我们将单模型参数实现的反演结果与LMI的自适应参数化进行比较,以获取大块IOP,分配给旋光成分的IOP以及旋光成分的浓度。我们发现,使用LMI进行海洋颜色反演对将地表遥感反射率与水柱中IOP相关的方程的经验参数g_(0)和g_(1)的先验选择非常敏感[J] 。地理学。 Res。 93,10909(1988)]。假设为g_(0)和g_(1)的海洋应用建议了值[J.地理学。 Res。 93,10909(1988)],取回的IOPs和浓度的准确度明显低于为沿海水域开发的参数化所取回的准确度[Appl。Chem。,93,10909(1988)]。选择。 38,3831(1999)],因为在这项研究中分析的光学复杂水主要是颗粒和溶解物质。与LMI的单个固定SIOP模型参数化相比,LMI的自适应参数化始终产生更准确的反演结果。 LMI的自适应实施导致分配的IOP和浓度的准确性有所提高,尤其是与浮游植物有关的数量。包含更宽的IOP范围的自适应参数化对于散装IOP,分摊的IOP和光学活性成分的浓度更准确。

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