检查季节性波浪处理设置和浅水对波浪测量的影响

C. Evans, H. Roarty, J. Kohut, S. Glenn
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引用次数: 3

摘要

当将SeaSonde高频雷达软件应用于美国东海岸大陆架时,推导波浪测量值是具有挑战性的。浅水深度具有饱和一阶和二阶布拉格的能力,不可避免地导致对波高条件的不精确估计。本文旨在研究在新泽西州海岸附近的前几个范围内水深小于30米的环境中,在SeaSonde中定义的设置。波浪测量数据来自13mhz标准范围CODAR(海岸海洋动力学应用雷达)天线,并与NDBC(国家数据浮标中心)位于纽约港和特拉华湾外的3米讨论浮标进行比较。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Examination of the SeaSonde wave processing settings and the effects of shallow water on wave measurements
Derivation of wave measurements from the SeaSonde high frequency (HF) radar software is challenging when applied to the U.S. East Coast continental shelf. Shallow water depths have the capability of saturating the 1st and 2nd order Bragg, inevitably leading to imprecise estimates of the wave height conditions. This paper looks to examine the settings defined in the SeaSonde in an environment where water depth is less than 30 m within the first few range cells off of the coast of New Jersey. Wave measurements were taken from a 13 MHz standard range CODAR (Coastal Ocean Dynamics Applications Radar) antenna and compared with NDBC (National Data Buoy Center) 3-meter discuss buoys located outside New York Harbor and Delaware Bay.
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