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Polarization of light in shallow waters

机译:浅水区光的极化

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Measurements of the upwelling polarized radiance in relatively shallow waters of varying depths and benthic conditions are compared to simulationsrevealing the depolarizing nature of the seafloor. Significant correlations between simulations and measurements are attained when the appropriate unpolarized, Lambertian bottoms are included in the radiative transfer model. The bottoms used in this study produce realistic upwelling radiance distributions as well as ranges of the degree of linear polarization (DoLP) that peak between 10 and 30%. This study specifically finds that polarization in upwelling radiance is best preserved at long wavelengths in clear waters and also at short wavelengths in phytoplankton- and CDOM-rich waters. These results can thus facilitate the detection of benthic materials as well as future studies of camouflage by benthic biota.The DoLPwas found to be highly sensitive to benthic reflectance, but the angle of polarization (AoLP), which quantifies the orientation of polarization, is independent of it. The AoLP could therefore be used to communicate and sense direction underwater.
机译:比较不同深度和弯曲条件的相对较浅的水中的上升偏振辐射的测量与模拟海底的去极化性质。当适当的不偏振,朗伯底部包括在辐射转移模型中,实现模拟和测量之间的显着相关性。本研究中使用的底部产生了现实的上升辐射发布,以及达到10至30%之间的线性偏振度(DOLP)的范围。本研究具体地发现,在透明水域中的长波长和富含富富植物中的短波长,最佳地保存了上升辐射的极化。因此,这些结果可以促进底栖物质的检测以及底栖生物群的未来研究。发现的Dolpwas对底栖反射率非常敏感,但偏振(AOLP)的角度,这量化了极化方向,是独立的它。因此,AOLP可以用于在水下进行通信和感应方向。

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