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Normalized radar backscattering cross-section and Doppler shifts of the sea surface in Ka-band

机译:Ka波段归一化雷达后向散射截面和海面多普勒频移

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Field data taken from the Black Sea Research platform during 2009-2015 are used to develop a dual-co-polarized (VV and HH) empirical model for the sea surface normalized radar cross-section (NRCS) and Doppler Velocity (DV) in the Ka-band. A fitting function for the NRCS is the standard truncated Fourier series in azimuth with polynomial coefficients dependent on incidence angle and wind speed. The data are corrected for the angular antenna pattern, which is measured in special calibration procedures. The resulting NRCS model is consistent with other rare Ka-band measurements and agrees well with Ku-band geophysical model functions, in contrast with previously proposed Ka-band models. Surface is subtracted from measured DV using either propeller current meter measurements or surface video recording. The resulting DV model consists of constant and wave-induced (WIDV) parts. The constant part is evaluated based on the time mean of Instantaneous DV (IDV), which is close to the Bragg wave phase speed. The WIDV part is analyzed in terms of Modulation Transfer Function (MTF) for which a separate empirical model is proposed.
机译:从黑海研究平台(Black Sea Research Platform)在2009年至2015年期间获取的现场数据用于为海平面归一化雷达横截面(NRCS)和多普勒速度(DV)开发双共极化(VV和HH)经验模型。嘉乐队NRCS的拟合函数是方位角的标准截断傅立叶级数,其多项式系数取决于入射角和风速。校正了角天线方向图的数据,该角方向图是通过特殊的校准程序测量的。与先前提出的Ka波段模型相比,最终的NRCS模型与其他罕见的Ka波段测量结果一致,并且与Ku波段地球物理模型函数非常吻合。使用螺旋桨电流计测量或地面视频记录从测得的DV中减去地面。所得的DV模型由常数和波感应(WIDV)组成。根据瞬时DV(IDV)的时间平均值评估常数部分,该时间平均值接近布拉格波的相速度。 WIDV部分根据调制传递函数(MTF)进行了分析,为此提出了单独的经验模型。

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