改进的海风卫星散射计飓风风速算法

I. Adams, W. Jones, Jun-Dong Park, T. Kasparis, S. Chen, J. Tenerelli
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引用次数: 0

摘要

在标准产品(例如QuikSCAT L2B)中给出的卫星微波散射计风速反演严重低估了热带气旋的峰值风速。一个重要的原因是在处理算法中忽略了降水对归一化雷达截面sigma-0的影响。本文介绍了第一次尝试提供sigma-0修正的结果,该修正解释了雨的大气衰减。大气透射率是由QuikSCAT辐射计(QRAD)的过量亮度温度与sigma-0测量同时得出的。当应用时,检索到的风速与数值飓风模型(PSU/NCAR MM5)在中到高降雨量的情况下显示出更好的一致性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Improved hurricane wind speed algorithm for the seawinds satellite scatterometer
Satellite microwave scatterometer wind retrievals, given in the standard product (e.g., QuikSCAT L2B), badly underestimate the peak wind speed in tropical cyclones. One important reason is that the effects of precipitation on the normalized radar cross section sigma-0 are neglected in the processing algorithms. This paper presents results of a first attempt to provide sigma-0 corrections, which account for the atmospheric attenuation of the rain. Atmospheric transmissivity is derived from the QuikSCAT Radiometer (QRAD) excess brightness temperatures taken simultaneously with sigma-0 measurements. When applied, retrieved wind speeds show improved agreement with numerical hurricane models (PSU/NCAR MM5) where there is moderate to high rainfall.
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