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

给出改进的场方式反演方法,利用该方法从卫星散计测量的后向散强度的数据中唯反演出大尺度海洋风场。

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

垂直气流速度是根据落速变化算出,把它用在天气系统分析是初次尝试。