We introduce a modified model approach to estimate the unique synoptic oceanic wind field from backscatter of spaceborne scatterometer.

给出了一种改进的反演法,利用该法从卫星散计测量的后向散强的数据中唯一反演出大尺海洋风。

The vertical velocity is calculated directly from the raw dropsonde data, it is a preliminary attempt to use the vertical velocity for synoptic analysis.

垂直气是根据探空仪落变化算出,把它用在天气系统分析是初次尝试。