而中尺度低压及其特有的动力热力结构与该暴雨过程直接相关。
The mesoscale typhoon low pressure and its specific dynamical and thermodynamical structures were directly related to this heavy rainfall event.
所分析的地面低压中心位于中（尺度）气旋之东约8公里处。
The analyzed low-pressure center at the surface was located ~8 km east of the mesocyclone.
四种积云对流参数化方案模拟的海平面气压场差别较大，其中GR方案较好地模拟出造成这次暴雨的高低压系统和中尺度气旋。
The simulative sea level pressure of four CPSs showed large difference, in which the GR scheme had better simulated the high, low systems and mesoscale cyclone.
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