The lower atmosphere has convective stability ( MPV 1> 0) in hail area, but the development of moist slantwise vorticity ( MPV 2 < 0) could be a favorable condition to the severe convection there.

  • 在降雹区低层为对流稳定的层结下(MPV1>0),有MPV2<0,使湿斜压不稳定增强,倾斜涡度得以发展;

  • 互联网摘选 2025-01-20 11:39:50

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