地震造成的水平加速峰值是从大坝坝基向坝顶急剧增加的。
在水库蓄满水的时候，正如人们所预料的，坝顶加速峰值会更大一些。
Peak accelerations, as expected, at the crest are greater with full reservoirs.
在林带上部，有林带间的阻滞减速区和林带后的涡旋减速区，在林带顶后部有集流加速区。
In the upper layer, there are the blocking speed-down zone inter-belt, the whirling speed-down zone behind the belt, the conflux accelerating zone just behind the top of shelterbelt.
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