Quadrant-Averaged Structure and Evolution Mechanisms of a Northeast Cold Vortex during Its Mature Stage  | 
	
|   Figure 2   a-d Vorticity units: 10 -5  s -1 , e-h divergence units: 10 -5  s -1 , i-l vertical velocity units: cm s -1  at 500 hPa, and m-p whole-atmosphere precipitable water PW units: kg m -2  during the mature stage of the NCCV 0000 UTC 3 July to 1800 UTC 3 July 2013, where the dashed circles stand for the effective region of the cyclone. Panels q-t show quadrant-averaged divergence units: 10 -5  s -1 , vorticity units: 10 -5  s -1 , PW units: kg m -2 , and vertical velocity cm s -1 , respectively. Typical regions for divergence and ascending motions are marked with dotted areas.  | 
	![]()  |