有无台风影响下陕西西北涡暴雨特征对比分析
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彭力 1,2,4( ), 赵强 3,4, 乔丹杨 4,5, 张雄 1,2, 徐浩天 1,2, 倪闻 1,2
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Comparative analysis on characteristics of rainstorms caused by northwest vortex in Shaanxi with and without influence of typhoon
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PENG Li 1,2,4( ), ZHAO Qiang 3,4, QIAO Danyang 4,5, ZHANG Xiong 1,2, XU Haotian 1,2, NI Wen 1,2
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图6. 2010—2020年陕西西北涡暴雨有(a、b)和无(c、d)台风影响时 (实线,单位:K)与湿位涡(MPV1)(虚线,单位: 10-6 m2·s-1·K·kg-1)沿110°E(a)及109°E(c)的纬度-高度剖面和沿38°N(b)及37°N(d)的经度-高度剖面
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Fig.6. The latitude-height profiles along 110°E (a) and 109°E (c) and longitude-height profiles along 38°N (b) and 37°N (d) of pseudo-equivalent potential temperature (solid lines, Unit: K) and moist potential vorticity (MPV1) (dashed lines, Unit:10-6 m2·s-1·K·kg-1) during rainstorm processes caused by northwest vortex with (a, b) and without (c, d) typhoon influence in Shaanxi from 2010 to 2020
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