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首页> 外文期刊>Applied optics >Radiance-irradiance inversion algorithm for estimating the absorption and backscattering coefficients of natural waters: vertically stratified water bodies
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Radiance-irradiance inversion algorithm for estimating the absorption and backscattering coefficients of natural waters: vertically stratified water bodies

机译:辐射-辐射反演算法,用于估计天然水的吸收和反向散射系数:垂直分层水体

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摘要

A full multiple-scattering algorithm for inverting profiles of the upwelling and down welling irradiances to yield profiles of the absorption and backscattering coefficients in a vertically stratified water body is described and tested with simulated data. The algorithm does not require knowledge of the scattering phase function of the medium. The results are better the closer the phase function assumed in the retrievals is to the true phase function, although excellent retrievals of the absorption coefficient can still be obtained with an inaccurate phase function. Simulations show that the algorithm is capable of determining the vertical structure of a stratified water body and usually provides the absorption coefficient profile with an error less than or similar to 2% and the backscattering coefficient profile with an error less than or similar to 10%, as long as the spacing between pseudodata samples is sufficiently small that the necessary derivatives of the irradiances can be accurately computed. The performance is only slightly degraded when the upwelling radiance (nadir viewing) is substituted for the upwelling irradiance. (C) 1998 Optical Society of America. [References: 16]
机译:描述了一个完整的多重散射算法,该算法用于反转上升流和下降阱辐照度的分布,以产生垂直分层水体中吸收系数和反向散射系数的分布,并使用模拟数据进行了测试。该算法不需要了解介质的散射相位函数。尽管假设不准确的相位函数仍然可以获得出色的吸收系数检索结果,但在检索中假设的相位函数越接近真实相位函数,结果越好。仿真表明,该算法能够确定分层水体的垂直结构,并且通常提供误差小于或等于2%的吸收系数曲线和误差小于或等于10%的反向散射系数曲线,只要伪数据样本之间的间隔足够小,就可以精确计算出辐照度的必要导数。当用上升流辐射(天底观测)代替上升流辐照度时,性能只会稍微降低。 (C)1998年美国眼镜学会。 [参考:16]

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