However, the simulated rainfall rate in BILIS is higher than observed, the errors are possible due to some deficiencies in the model physics and the simulated intensity was stronger than observed.
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释义
降水分布方面,模拟同样能掌握风切下游的降水量皆高于上游之特性,但碧利斯的模拟降水量稍高于观测,可能是碧利斯结果中台风强度过强或模式物理不够完整所造成。
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