这种方法与当前使用的计算方法间的主要不同点是它不需要完整的探空资料，只需要各层的位势高度。
The main difference between this method and the method currently used is that it does not require entire sounding data except geopotential height of each level.
主要结果如下：1位势场的高度主要贡献，集中在准静止长波范围内，并具有明显的季节变化。
The results are as follows:1)The chief contributions of the normal potential field are mainly concentrated at the long quasi-stationary waves and show significant seasonal variations.
主要结果如下：1位势场的高度主要贡献，集中在准静止长波范围内，并具有明显的季节变化。
The results are as follows:1)The chief contributions of the normal potential field are mainly concentrated at the long quasi-stationary waves and show significant seasonal variations.
应用推荐