Research Article
Dynamical Modulation of Wintertime Synoptic-Scale Cyclone Activity over the Japan Sea due to Changbai Mountain in the Korean Peninsula
Figure 11
(a) Composite differences in the 850 hPa poleward eddy heat flux between the MOD and CTL runs (former minus latter) based on the three typical cases. The shading interval is 250 K m s−1. (b) As in Figure 11(a) but for the local deepening rate (LDR). The shading interval is 0.1 hPa hr−1.
| (a) Eddy heat flux |
| (b) LDR |