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ANALYSIS OF WIND FIELD FOR TYPHOON RUSA IN SOUTH KOREA: BASED ON WIND DIRECTION OF TYPHOON MODEL

机译:韩国台风rusa风场分析:基于台风模型的风向

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Synthetic Aperture Radar (SAR) images are more and more widely used in ocean wind monitoring. We present a method for the estimation of wind directions from synthetic aperture radar (SAR) images of the ocean. The method is based on winds of QuikSCAT scatterometer and Typhoon Surface Wind Model (PVM, KORDI) for the region of eye wall that the wind direction does not appear as streaks in SAR images of the ocean. Within the eye wall, the wind speed reaches its maximum and the most damaging winds and intense rainfall is found. A RADARSAT-SAR image of TY RUSA acquired on August 30, 2002 at 2112 UTC seems like the center where the NRCS is quite low, but belongs to the eye wall. To retrieve wind speeds, CMOD5 was originally developed for the scatterometer aboard ERS-1 and 2 operating at VV polarization and consequently requires modification if applied to HH-polarized SAR data. However, because the Extended High mode used here has comparatively high incidence angles of 54.24° - 57.31°, the polarization ratio in a hybrid model function is supposed to be 1. The retrieved SAR wind is compared with the result of the typhoon model with a fine computing grid of 1/60 degrees. It is shown that wind structure of eye wall can be described by using SAR based on wind directions from QuikSCAT.
机译:合成孔径雷达(SAR)图像在海风监测中越来越广泛使用。我们提出了一种从海洋的合成孔径雷达(SAR)图像估计风向的方法。该方法基于Quikscat散射仪和台风表面风模型(PVM,Kordi)的风向,用于眼壁的区域,风向不会在海洋的SAR图像中出现条纹。在眼墙内,风速达到其最大值,最损坏的风和强烈的降雨量。 2002年8月30日收购的Ty Rusa的Radarsat-SAR图像在2112 UTC中似乎是NRC非常低的中心,但属于眼墙。为了检索风速,最初为在VV偏振中操作的散射计的散射计,并且如果应用于HH偏振SAR数据,则最初为散射计的散射仪和2开发的CMOD5。然而,由于这里使用的扩展高模式具有54.24° - 57.31°的相对高的发射角度,因此混合模型函数中的偏振比应该是1.检索到的SAR风与台风模型的结果进行比较精细计算网格为1/60度。结果表明,眼壁的风结构可以通过基于Quikscat的风向使用SAR来描述。

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