Differences in Cloud Vertical Structures between the Tibetan Plateau and Eastern China Plains during Rainy Season as Measured by CloudSat/CALIPSO

<div>Cross sections of depression of the dew point and vertical velocity along longitude (a) averaged between 30°N and 35°N and latitude (b) averaged between 80°E and 95°E and (c) averaged between 110°E and 120°E. A scale of vertical velocity is shown on the lower-right of the figure, and its units is Pa/s. The thick dashed line represents dynamic tropopause.</div>

Advances in Meteorology

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Figure 10

Figure 10: Differences in Cloud Vertical Structures between the Tibetan Plateau and Eastern China Plains during Rainy Season as Measured by CloudSat/CALIPSO 

Figure 10 | Differences in Cloud Vertical Structures between the Tibetan Plateau and Eastern China Plains during Rainy Season as Measured by CloudSat/CALIPSO 