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风浪谱模型在高度计风速反演中的应用
引用本文:程永存,刘玉光,徐青,荣增瑞,殷晓斌,宗海波,修鹏.风浪谱模型在高度计风速反演中的应用[J].高技术通讯,2007,17(8):858-862.
作者姓名:程永存  刘玉光  徐青  荣增瑞  殷晓斌  宗海波  修鹏
作者单位:1. 中国人民解放军理工大学气象学院,南京,211101;中国海洋大学物理海洋实验室,青岛,266003
2. 中国人民解放军理工大学气象学院,南京,211101
3. 香港中文大学太空与地球信息科学研究所,香港
基金项目:国家重点基础研究发展计划(973计划)
摘    要:依据粗糙海面电磁波镜面散射理论,将根据全波数范围内的风浪谱模型计算的标准化雷达后向散射截面与T/P卫星高度计测得的雷达后向散射截面(Ku波段)进行比较,实现了对高度计风速的反演.研究表明,在所选浮标附近海域,波龄因子对高度计风速反演存在较大影响.与目前高度计业务化算法相比,考虑波龄因子影响后,根据谱模型反演获得的风速与中国近海浮标风速之间均方根误差和平均偏差更小.由于波龄因子可以根据高度计测得有效波高以及业务化算法获得的风速得到,因此根据风浪谱模型反演获得的风速具有广泛的适用性.

关 键 词:高度计风速  风浪谱模型  反演  雷达后向散射截面  波龄
收稿时间:2006-07-03
修稿时间:2006年7月3日

Application of wind wave spectrum model in altimeter wind speed retrieval
Cheng Yongcun,Liu Yuguang,Xu Qing,Rong Zengrui,Yin Xiaobin,Zong Haibo,Xiu Peng.Application of wind wave spectrum model in altimeter wind speed retrieval[J].High Technology Letters,2007,17(8):858-862.
Authors:Cheng Yongcun  Liu Yuguang  Xu Qing  Rong Zengrui  Yin Xiaobin  Zong Haibo  Xiu Peng
Affiliation:1Institute of Meteorology, PLA University of Science and Technology, Nanjing 211101;2.Physical Oceanography Laboratory, Ocean University of China, Qingdao 266003;3. Institute of Space and Earth Information Science,The Chinese University of Hong Kong, Hong Kong
Abstract:Based on the specular reflection theory of electromagnetic waves at rough sea surface and the spectral model of wind waves with a wave age factor, the sea surface wind speeds were retrieved from the normalized radar backscatter cross section measured by TOPEX/Poseidon Ku-band altimeter using the mean square slope calculated from the spectral models of the wind waves and the gravity-capillary waves. The study showed that the wave age factor has a significant influence on retrieving altimeter wind speeds. Compared with the empirical algorithms in operational use for altimeter winds retrieval, after considering the effects of wave age factor, both the bias and the root mean square error between wind speeds retrieved by the proposed analytical algorithm and buoy measured wind speeds in Eastern China Sea decrease significantly. The relationship between the wave age and non-dimensional wave height can be used to calculate the wave age factor based on altimeter measured significant wave height and wind speeds. Thus, the algorithm proposed in this study has a comprehensive applicability.
Keywords:altimeter wind speed  wind wave spectrum model  retrieval  normalized radar backscatter cross section  wave age
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