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作 者:JIANG GuoYing XU JiYao YUAN Wei NING BaiQi WAN WeiXing HU LianHuan
机构地区:[1]State Key Laboratory of Space Weather,Center for Space Science and Applied Research,Chinese Academy of Sciences,Beijing 100190,China [2]Beijing National Observatory of Space Environment,Institute of Geology and Geophysics,Chinese Academy of Sciences Beijing 100029,China
出 处:《Science China(Technological Sciences)》2012年第5期1245-1250,共6页中国科学(技术科学英文版)
基 金:supported by the National Natural Science Foundation of China (Grant Nos. 40804037, 40890165, and 40921063);the National Important Basic Research Project of China (Grant No. 2011CB811405);the Chinese Meridian Project and the Specialized Research Fund for State Key Laboratories
摘 要:In this paper, winds derived from OH Meinel 892.0 nm detection by an FPI (Fabry-Perot Interferometer) are compared with the simultaneous wind measurements from a meteor radar during April-May of 2010. The peak height of OH Meinel 892.0 nm is about 87 km. The variations of FPI wind at 87 km mostly have the similar track to meteor radar wind at 87 km, and the data values of FPI wind mainly fall into the range of meteor radar wind. However, there are still quantitative differences between the observations of the two systems. The best cross-correlation occurs in rneridional winds from two systems in April of 2010. An obvious wave signal with 0.2 cycle/d frequency is found in meridional winds observed by both FPI and meteor radar.
关 键 词:FPI meteor radar mesospheric wind
分 类 号:P618.130.8[天文地球—矿床学] TN959.74[天文地球—地质学]
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