Vertical structure and dynamical properties during snow events in middle latitudes of china from observations by the c-band vertically pointing radar

Data from the continuous observations of four shallow snow events (echo top < 8 km) and two deep events (> 10 km) were obtained using the C-band vertically pointing radar with frequency-modulation continuous-wave technology with extremely high resolution during the winter of 2015 – 2016 in middle latitudes of China. Snow-generating cells (GCs) were found near the cloud top in each event. Reflectivity (Z ), radial velocity (V ), and the vertical gradients of Z (dZ/dh, where h is the vertical distance) and V (dV /dh) showed different vertical distribution characteristics between the upper GC and lower stratiform regions (St regions). Fall streaks (FSs) associated with GCs were embedded in the St regions. In the deep events, the proportions of GC regions were slightly larger, but the average contributions to the growth of Z (33 %) were lower than those in the shallow events (42 %). The average d Z /dh values were usually two to three times larger inside GCs and FSs compared to outside. Bimodal Doppler spectra were used to establish the relationships between Z and the reflectivity-weight-ed particle fall speed (V) for the two regions. The vertical air velocity (W ) and V were then retrieved, and the results showed that both the updraft and the downdraft were alternately observed in GC regions. GC locations were usually accompanied by strong upward air motion, with average speeds mostly distributed around 1.2 m s, whereas downward air motion often appeared between GCs. In the St regions, the speeds of W were mainly within 0.5 m s. The upper areas of the St regions consisted primarily of weak upward motion, whereas weak downward motion dominated the lower areas. There was no apparent difference in W inside and outside the FSs. The average V was slightly larger inside GCs and FSs compared to outside, with a difference of 0.1–0.3 m s and 0.2–0.4 m s, respectively.