Changes in Typhoon Activities and Regional Precipitation Variability over the Korean Peninsula according to Different Phases of El Niño

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/amete/volume-2015/983268/figures/983268.fig.001a.svgz" name="983268.fig.001a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Five major river basins in Korea</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/amete/volume-2015/983268/figures/983268.fig.001b.svgz" name="983268.fig.001b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Distribution of seasonal precipitation</td></tr></table>

<div>Distribution of seasonal precipitation (June–September) in Korea during the 1966–2007 periods. (a) Five major river basins in Korea. (b) Distribution of seasonal precipitation. The annual long-term average precipitation was noted with the number for each histogram. The fraction of seasonal precipitation and TC-induced precipitation is expressed in percentage.</div>

Advances in Meteorology

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Figure 1

Figure 1: Changes in Typhoon Activities and Regional Precipitation Variability over the Korean Peninsula according to Different Phases of El Niño 