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

<div>(a) Spatial distribution of OISST averaged over the period of 2000–2014. The contoured interval is 1 K. The shading denotes the horizontal SST gradient (K/100 km). (b) As in Figure <a href="../fig12/#a">12(a)</a> but for horizontally smoothed OISST.</div>

Advances in Meteorology

fig12

Figure 12

Figure 12: Dynamical Modulation of Wintertime Synoptic-Scale Cyclone Activity over the Japan Sea due to Changbai Mountain in the Korean Peninsula 