1961—2019年青藏高原中东部夏季强降水与大尺度环流的关系
曹瑜,游庆龙,蔡子怡

Relationship between the summer extreme precipitation in the Qinghai-Tibet Plateau and large-scale circulations from 1961 to 2019
Yu CAO,Qinglong YOU,Ziyi CAI
图7 1961—2019年青藏高原中东部夏季200 hPa位势高度距平场(等值线,gpm)、500 hPa波作用通量(箭头,m2·s-2)及其散度(阴影,m·s-2)距平和500 hPa风暴轴(阴影,dagpm2
Fig.7 The composite anomalous on the eastern and central Qinghai-Tibetan Plateau during 1961-2019 of 500 hPa storm track (shaded, dagpm2) (a) the positive year of R95p (c) the negative year of R95p; 200 hPa geopotential height (contour, gpm) and TN wave flux (arrows, m2·s-2) and it divergence (shaded, m·s-2) (b) the positive year of R95p (d) the negative year of R95p