Scattering phase function for particulates-in-water: modeling and validation

S. Sahu, P. Shanmugam
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引用次数: 8

Abstract

Scattering phase function plays a crucial role in studies and calculations based on radiative transfer theory in water as well as atmosphere. A model based on Mie theory is developed for estimating the particulates-in-water scattering phase function for forward angles (0.1° - 90°). Particle size distribution (PSD) slope (ξ) and bulk refractive index (n) are chosen as key inputs for this proposed model. The PSD slope can be estimated from the attenuation spectrum measured directly in-situ and the bulk refractive index can be calculated by an inversion model using measured backscattering ratio (BP) and PSD slope. The attenuation spectrum and backscattering ratio can be easily measured in-situ using commercially available instruments in real time. The entire range of forward angles is divided into two ranges and phase function is modeled separately in the ranges 0.1° - 5° and 5° - 90°, from numerically calculated Volume Scattering Function (VSF) using Mie theory. The division boundary is decided owing to the fact that the scattering phase functions, for different oceanic conditions, exhibit a change in slope at approximately 5°. Performance of the present model is evaluated by comparing with existing empirical and analytical models as well as measured phase functions. The proposed phase function model shows a considerable improvement upon existing models, and will have important applications in remote sensing applications and underwater studies.
水中粒子的散射相函数:建模和验证
散射相函数在水和大气辐射传输理论的研究和计算中起着至关重要的作用。建立了一种基于Mie理论的水粒子散射相函数模型,用于估计前向角(0.1°~ 90°)下的水中粒子散射相函数。选择粒径分布(PSD)、斜率(ξ)和体折射率(n)作为该模型的关键输入。PSD斜率可以直接从原位测量的衰减谱中估计出来,体折射率可以通过测量后向散射比(BP)和PSD斜率的反演模型计算出来。衰减谱和后向散射比可以很容易地使用市售仪器实时测量。利用Mie理论,从数值计算的体积散射函数(VSF)出发,将整个前向角范围划分为两个范围,分别在0.1°~ 5°和5°~ 90°范围内建立相函数模型。划分边界的确定是由于在不同的海洋条件下,散射相函数的斜率变化约为5°。通过与已有的经验模型和分析模型以及实测相函数的比较,对模型的性能进行了评价。所提出的相函数模型在现有模型的基础上有很大的改进,将在遥感应用和水下研究中具有重要的应用价值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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