Fig. 6
From: Simulation study of low-level disturbances affecting near surface inversion events in Urumqi


shows the meridional-vertical distribution of vertical velocity after 2Â h of integration (a), the meridional-vertical distribution of temperature after 2Â h of integration (b), the meridional-vertical distribution of vertical velocity after 2Â h of integration (c), the meridional-vertical distribution of temperature after 3Â h of integration (d), the meridional-vertical distribution of temperature after 3Â h of integration (e), and the meridional-vertical distribution of vertical velocity after 3Â h of integration (f).