The results also show that the centre of the heavy snow lay in the positive area to the western severe gradient of MPV 1 zero line and also in the negative area to the northern severe gradient of MPV 2 zero line.
英
美
- 大降雪中心位于MPV1 零線(xiàn)西側強梯度帶的正值區內 ,它也位于 MPV2 零線(xiàn)北側強梯度帶的負值區內。 冬季在對流穩定層結下 ,當 MPV2 值為負時(shí) ,垂直渦度才能得到較大的增長(cháng) ,導致上升運動(dòng) ,產(chǎn)生大降雪天氣