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Mapping radar-derived sea surface currents with a variational method

机译:用变分方法绘制雷达衍生的海面流

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摘要

High-frequency radars measure projections of surface velocity vectors on the directions of the radar beams. A variational method for reconstruction of the 2d velocity field from such observations is proposed. The interpolation problem is regularized by penalizing high-frequency variability of the surface vorticity and divergence fields. Twin-data experiments are used to assess the method's skill and compare it with two well-known approaches to HFR data processing: conventional local interpolation and more sophisticated non-local scheme known as open-boundary modal analysis (OMA). It is shown that the variational method and OMA have a significant advantage over local interpolation because of their ability to reconstruct the velocity field within the gaps in data coverage, near the coastlines and in the areas covered only by one radar. Compared to OMA, the proposed variational method appears to be more flexible in processing gappy observations and more accurate at noise levels below 30%. (C) 2009 Elsevier Ltd. All rights reserved.
机译:高频雷达测量表面速度矢量在雷达波束方向上的投影。提出了一种从这种观测结果重建二维速度场的变分方法。通过惩罚表面涡度和发散场的高频变化来规范内插问题。双数据实验用于评估该方法的技能,并将其与两种著名的HFR数据处理方法进行比较:常规局部插值和更复杂的非局部方案,称为开放边界模态分析(OMA)。结果表明,由于变分方法和OMA能够重建数据覆盖范围内,海岸线附近和仅由一个雷达覆盖的区域内的速度场,因此具有优于局部插值的显着优势。与OMA相比,拟议的变分方法在处理零碎的观测结果时似乎更灵活,并且在低于30%的噪声水平下更准确。 (C)2009 Elsevier Ltd.保留所有权利。

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