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Dual-polarized Doppler radar measurements of oceanic fronts

机译:海洋前沿的双极化多普勒雷达测量

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This paper presents high-resolution, dual-polarized Doppler radar measurements of oceanic fronts made from a shipborne platform along the northern boundary of the Gulf Stream during the second Office of Naval Research (ONR)/Naval Research Laboratory (NRL) High Resolution Remote Sensing Experiment (HIRES-II). Average radial scatterer velocity and consecutive short-time Doppler spectra are computed from the coherent backscatter data. These are compared with in-situ current records obtained with an Acoustic Doppler Current Profiler (ADCP) and visually detected whitecap events recorded with a closed-circuit video camera. For the case in which dominant waves are propagating toward the radar, the change in the across-front radial scatterer velocity for vertical polarization shows reasonable agreement with current variations observed with the ADCP. Conversely, for the case in which the radar line-of-sight direction is orthogonal to the direction of propagation of the dominant waves, the radial scatterer velocity is sensitive to changes in the wave propagation direction caused by wave-current interaction at the front. For both polarizations, the shape of the Doppler spectrum shows significant variation across fronts, particularly for horizontal polarization. These spectral variations occur coincidentally with changes in the number of visually detected whitecap events per minute obtained from the closed-circuit video recordings. These results demonstrate the potential of dual-polarized Doppler radars operating in the low grazing angle regime for remotely sensing the current variability and the occurrence of wave breaking across oceanic fronts as well as the effect of fronts on wave propagation.
机译:本文介绍了第二次海军研究办公室(ONR)/海军研究实验室(NRL)高分辨率遥感过程中,从沿墨西哥湾北部边界的船载平台对海洋前沿进行的高分辨率,双极化多普勒雷达测量。实验(HIRES-II)。从相干反向散射数据计算平均径向散射速度和连续的短时多普勒光谱。将这些与通过声多普勒电流剖面仪(ADCP)获得的现场电流记录进行比较,并与通过闭路摄像机记录的视觉检测到的白浪事件进行比较。对于主波向雷达传播的情况,垂直极化的跨前径向散射速度的变化与ADCP观测到的电流变化显示出合理的一致性。相反,在雷达视线方向与主波传播方向正交的情况下,径向散射速度对前方波流相互作用引起的波传播方向变化敏感。对于这两种极化,多普勒光谱的形状在整个前沿都表现出明显的变化,特别是对于水平极化而言。这些光谱变化与从闭路视频记录获得的每分钟视觉检测到的白帽事件数量的变化同时发生。这些结果表明,双极化多普勒雷达在低掠角范围内运行的潜力,可用于远程感测当前的变化性和跨越海洋前沿的波的发生以及前沿对波传播的影响。

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