Research Article
Dynamical Modulation of Wintertime Synoptic-Scale Cyclone Activity over the Japan Sea due to Changbai Mountain in the Korean Peninsula
Figure 5
(a) Difference in the 850 hPa poleward eddy heat flux for December between the MOD and CTL runs (former minus latter). The shading interval is 0.3 K m s−1. (b) As in Figure 5(a) but for the local deepening rate (LDR). Shading interval is 3 hPa/month.
| (a) Eddy heat flux |
| (b) LDR |