Diurnal Variation Characteristics of Raindrop Size Distribution Observed by a Parsivel² Disdrometer in the Ili River Valley

Figure 11

Scatter plots of Z (mm⁶·m⁻³) versus R (mm·h⁻¹) for stratiform and convective rain types. The solid blue lines indicate the fitting power-law relationships in Zhaosu. The black solid line and black dashed line, respectively, represent the empirical relationships (Z = 200R^1.60 for stratiform rain type and Z = 300R^1.40 for convective rain type).

(a)

(b)