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

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/amete/volume-2017/6216032/figures/6216032.fig.0013a.svgz" name="6216032.fig.0013a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>SS run</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/amete/volume-2017/6216032/figures/6216032.fig.0013b.svgz" name="6216032.fig.0013b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>SS run minus CTL run</td></tr></table>

<div>(a) Climatological mean December precipitation during 2000–2014 for the SS run. (b) Difference in precipitation between the SS and CTL runs (former minus latter).</div>

Advances in Meteorology

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Figure 13

Figure 13: Dynamical Modulation of Wintertime Synoptic-Scale Cyclone Activity over the Japan Sea due to Changbai Mountain in the Korean Peninsula 