Dynamical Modulation of Wintertime Synoptic-Scale Cyclone Activity over the Japan Sea due to Changbai Mountain in the Korean Peninsula

<div>(a) Frequency distribution of synoptic-scale cyclone tracks during 2000–2014 for the CTL run. (b) As in Figure <a href="../fig4/">4</a>(a) but for the MOD run. (c) Difference in cyclone track frequency between the MOD and CTL runs (former minus latter).</div>

Advances in Meteorology

fig4

Figure 4

Figure 4: Dynamical Modulation of Wintertime Synoptic-Scale Cyclone Activity over the Japan Sea due to Changbai Mountain in the Korean Peninsula 