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Validation of shallow-water reflectance model for remote sensing of water depth and bottom type by radiative transfer simulation

机译:辐射传输模拟在浅水反射模型遥感水深和底型中的验证

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摘要

Lyzenga proposed a shallow-water reflectance model that describes the exponential relationship between the remote-sensing reflectance (R) and water depth [Appl. Opt. 17, 379383 (1978)]. The model has been widely used in remote sensing of water depth to estimate the depth from R, and in remote sensing of bottom type to remove the effect of depth from R. Although it was derived from radiative transfer theory ignoring internal reflection at the water surface, no study has quantitatively validated it following the theory. In this study, we examine its accuracy under various conditions using Monte Carlo radiative transfer simulations. Although internal reflection contributed significantly to R in some cases, the model, if fitted to (calibrated with) data covering the entire target depth range, described the relationship between R and depth reasonably accurately (R~2 > 0.9935). This was because the internally reflected component of R, as well as the other component, decreases exponentially with depth. However, because the sum of two exponentially decreasing functions is not strictly exponential, the model does not accurately estimate the depth using R when the calibration data did not cover the entire depth range of interest: the model significantly underestimated the depth when used for extrapolation.
机译:Lyzenga提出了一种浅水反射率模型,该模型描述了遥感反射率(R)与水深之间的指数关系[Appl。选择。 17,379383(1978)]。该模型已广泛用于遥感水深以估算R的深度,以及用于底部类型的遥感以消除R的深度的影响。尽管它是从辐射转移理论推导而忽略了水面的内部反射,没有任何研究根据该理论对其进行定量验证。在这项研究中,我们使用蒙特卡洛辐射转移模拟研究了其在各种条件下的准确性。尽管在某些情况下内部反射对R的影响很大,但是如果该模型适合(校准)覆盖整个目标深度范围的数据,则可以合理准确地描述R与深度之间的关系(R〜2> 0.9935)。这是因为R的内部反射分量以及其他分量随深度呈指数下降。但是,由于两个指数递减函数的总和不是严格的指数关系,因此当校准数据未涵盖感兴趣的整个深度范围时,该模型无法使用R准确估算深度:当用于外推时,该模型大大低估了深度。

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