本文对双多普勒天气雷达反演大气三维风场进行了初步探讨。
In this paper it is primarily discussed that the retrieval of the atmospheric three-dimensional wind field by Dual-Doppler radar.
该资料是用双多普勒天气雷达同步立体扫描数据，通过MUSCAT技术，反演出风场。
The wind field retrieval data are obtained by plied MUSCAT technique to transact the rude radial velocity data which were observed by dual-Doppler radar volume scans.
该文提出一些解决办法，但在应用双多普勒天气雷达风场反演数据时，还必须进行可靠性分析。
When wind fields derived from dual-Doppler radar observation are used, their reliability must been analyzed.
双多普勒天气雷达反演风场是以直接合成法为基础，垂直速度通过连续方程得到，反演天气系统的三维风场。
Wind field retrieval from dual-Doppler radar data USES synthesis technique, and the vertical velocity is obtained by using continuity equation, then the three-dimensional wind fields are retrieved.
双多普勒天气雷达反演风场是以直接合成法为基础，垂直速度通过连续方程得到，反演天气系统的三维风场。
Wind field retrieval from dual-Doppler radar data USES synthesis technique, and the vertical velocity is obtained by using continuity equation, then the three-dimensional wind fields are retrieved.
应用推荐