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 6

(a, b, c, d, e, f) Differences between the accumulated SEED and NOSEED precipitation (mm; SEED − NOSEED) from the start of model run until (a) 1330 LST and (b) 1430 LST in EXP1, (c) 1700 LST and (d) 1900 LST in EXP2, and (e) 1600 LST and (f) 2000 LST in EXP3. (g, h, i) Accumulated precipitation in NOSEED run from the start of model run until (g) 1430 LST in EXP1, (h) 1900 LST in EXP2, and (i) 2000 LST in EXP3.