The hail fall of the hail cloud which domain of the initial potential temperature perturbation is located in lee slope is 6 times as large as in windward slope.

 
  • 當初始位溫擾動(dòng)在背風(fēng)坡時(shí)冰雹云的降雹量約為當初始位溫擾動(dòng)在迎風(fēng)坡時(shí)冰雹云降雹量的6倍。
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