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

<div>(a) Climatological mean December distribution of the maximum Eady growth rate for the CTL run. The shading interval is 0.1 day<sup>−1</sup>. (b) As in Figure <a href="../fig3/">3</a>(a) but for the MOD run. (c) Difference in the maximum Eady growth rate between the MOD and CTL runs (former minus latter).</div>

Advances in Meteorology

fig3

Figure 3

Figure 3: Dynamical Modulation of Wintertime Synoptic-Scale Cyclone Activity over the Japan Sea due to Changbai Mountain in the Korean Peninsula 