SAR observation on sea surface wind caused by rain cell

Xiaomin Ye, Ding Jing, Yongjun Jia, Xinzhe Yuan, Yi Zhang, Liming Cui, Ying Xu, Xuetong Xie
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Abstract

Rain cells or convective rain, the dominant form of rain in the tropics and subtropics, can be easy detected by Synthetic Aperture Radar (SAR) images with high horizontal resolution. The footprints of rain cells on SAR images are caused by the scattering and attenuation of the rain drops, as well as the downward airflow. In this study, we extracted sea surface wind structure caused by rain cells by using a RADARSAT-2 SAR image with a spatial resolution of 100 m for case study. We extracted the sea surface wind speed from SAR image by using CMOD4 geophysical model function with outside wind directions of NCEP final operational global analysis data and microwave scattermeter onboard Chinese HY-2 satellite, respectively. The root-mean-square errors (RMSE) of these SAR wind speeds, validated against NCEP and HY-2, are 1.48 m/s and 2.14 m/s, respectively. Circular signature patterns with brighter on one side and darker on the opposite side on SAR image were interpreted as the sea surface wind speed (or sea surface roughness) variety caused by downdarft associated with rain cell. The wind speed taken from the transect profile which superposes to the wind ambient vectors and go through the center of the circular footprint of rain cell can be fitted as a cosine or sine curve in high linear correlation with the values of no less than 0.80. The background wind speed, the wind speed cause by rain cell and the diameter of footprint of the rain cell with kilometers or tens of kilometers can be acquired by fitting curve. Eight cases interpreted and analysed in this study all showed the same conclusion.
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雨单体引起海面风的SAR观测
雨单体或对流雨是热带和亚热带地区的主要降雨形式,可以通过高水平分辨率的合成孔径雷达(SAR)图像很容易地探测到。雨点在SAR图像上的足迹是由雨滴的散射和衰减以及向下的气流造成的。本研究以100 m空间分辨率的RADARSAT-2 SAR图像为例,提取了由雨单体引起的海面风结构。利用CMOD4地球物理模型函数,利用NCEP最终业务全球分析数据和中国海2星微波散射计数据,分别从SAR影像中提取海面风速。经NCEP和HY-2验证,这些SAR风速的均方根误差(RMSE)分别为1.48 m/s和2.14 m/s。在SAR图像上,一面较亮,一面较暗的圆形特征模式被解释为与雨细胞相关的下气流引起的海面风速(或海面粗糙度)变化。经风环境矢量叠加的样条剖面的风速可拟合为余弦或正弦曲线,其线性相关值不小于0.80。通过拟合曲线可以得到背景风速、雨点引起的风速以及雨点在公里或几十公里范围内的足迹直径。本研究分析的8个案例均得出了相同的结论。
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