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

<div>The accumulated AgI number concentration (m<sup>−3</sup>) for the SEED simulations from the surface to 3,000 m (MSL) for EXP1 (a, b), EXP2 (c, d), and EXP3 (e, f). The vector represents the wind field at the seeding heights.</div>

Advances in Meteorology

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Figure 4

Figure 4: 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 4 | 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 