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Modeling water surface reflectance signatures and in-water irradiance profiles in shallow tropical waters influenced by bottom reflectance

机译:底部反射率影响水面反射率及水面反射率和水中辐照曲线

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The two flow equations have been solved using Cauchy type boundary conditions so as to form a pair of coupled equations for use in a coupled atmosphere-water-bottom reflectance optical model to simulate the surface or subsurface reflectance, in-water irradiance profiles and in-water reflectance profiles in optically shallow or deep waters with or without a wind roughened surface. The model results presented utilize clear water absorption and backscatter coefficients, and bottom reflectance as a function of wavelength. The bottom reflectance is characteristic of a tropical sea grass, sand and silt and Elkhorn coral, and a dead reef system in order to evaluate the nature of the underwater light climatology. The analytical model results are compared to a hyper-spectral Monte-Carlo model. The Monte Carlo model also suggests a subsurface maximum in the intensity of light in optically shallow waters which is predicted by the analytical model.
机译:使用Cauchy型边界条件解决了两个流动方程,以便形成一对耦合方程,用于耦合大气压 - 水底反射光学模型,以模拟表面或地下反射率,水中辐照度轮廓和 - 在具有或没有风力粗糙表面的光学浅或深水区中的水反射曲线。呈现的模型结果利用清晰的吸水和反向散射系数,以及作为波长的函数的底部反射率。底部反射率是热带海草,沙子和淤泥和埃尔科恩珊瑚的特征,以及死礁系统,以评估水下光气球的性质。将分析模型结果与超光谱蒙特卡罗模型进行比较。 Monte Carlo模型还提出了通过分析模型预测的光学浅水中的光强度的地下最大值。

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