Fig. 9: Atmospheric vertical velocity and humidity in CTL experiment and its response to regional climate change. | npj Climate and Atmospheric Science

Fig. 9: Atmospheric vertical velocity and humidity in CTL experiment and its response to regional climate change.

From: Response and mechanisms of sub-daily precipitation over the Tibetan Plateau to regional climate change

Fig. 9

Vertical cross section of the water vapour mixing ratio (shading, units: g kg−1) and the vertical circulation vectors (zonal winds and 1000 times of vertical velocity, units: 10−3 m/s), which are latitudinal averaged over TP during 0800–1400 BST (a, c) and 1400–2000 BST (b, d) for CTL experiment (a, b) and the difference between CTL and NoRCC experiment (c, d).

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