But when the baroclinicity of low level vortex was strengthened and when warm air came into being, all the rain belts lay in the left and the front of southeast low level jet.

 
  • 當低渦的斜壓性加大,出現暖空氣的作用時(shí),暴雨區均出現于西南風(fēng)急流的左前方。
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