Research Article

Numerical Simulations of Airborne Glaciogenic Cloud Seeding Using the WRF Model with the Modified Morrison Scheme over the Pyeongchang Region in the Winter of 2016

Figure 10

(a, b, c) Distribution of the 1-hour vertical accumulation of cloud water mixing ratio (g kg−1) from the seeding start time and (d, e, f) time series of the hourly liquid water path for the NOSEED simulation in EXP1 (a, d), EXP2 (b, e), and EXP3 (c, f). The blue and red lines in (d), (e), and (f) indicate the values at A and B in (a), (b), and (c), respectively.