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Retrieval of short ocean wave slope using polarimetric imaging

机译:极化成像反演海浪短坡

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摘要

We present a passive optical remote sensing technique for recovering shape information about a water surface, in the form of a two-dimensional slope map. The method, known as polarimetric slope sensing (PSS), uses the relationship between surface orientation and the change in polarization of reflected light to infer the instantaneous two-dimensional slope across the field-of-view of an imaging polarimeter. For unpolarized skylight, the polarization orientation and degree of linear polarization of the reflected skylight provide sufficient information to determine the local surface slope vectors. A controlled laboratory experiment was carried out in a wave tank with mechanically generated gravity waves. A second study was performed from a pier on the Hudson River, near Lamont-Doherty Earth Observatory. We demonstrated that the two-dimensional slope field of short gravity waves could be recovered accurately without interfering with the fluid dynamics of the air or water, and water surface features appear remarkably realistic. The combined field and laboratory results demonstrate that the polarimetric camera gives a robust characterization of the fine-scale surface wave features that are intrinsic to wind-driven air-sea interaction processes.
机译:我们以二维斜率图的形式介绍了一种用于恢复水面形状信息的无源光学遥感技术。该方法称为极化斜率感应(PSS),它使用表面方向与反射光的偏振变化之间的关系来推断成像偏振计视场上的瞬时二维斜率。对于非偏振天窗,反射天窗的偏振方向和线性偏振度可提供足够的信息来确定局部表面坡度矢量。在带有机械产生的重力波的波浪罐中进行了受控的实验室实验。第二项研究是在拉蒙特·多尔蒂地球观测台附近的哈德逊河上的一个码头上进行的。我们证明了短重力波的二维斜场可以在不干扰空气或水的流体动力学的情况下准确地恢复,并且水表面特征显得非常逼真。野外和实验室结果的结合表明,偏振相机可以很好地表征风表面相互作用的固有尺度,即细尺度的表面波特征。

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