Characteristics of Summer Precipitation around the Western Ghats and the Myanmar West Coast

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/ijas/volume-2015/206016/figures/206016.fig.005a.svgz" name="206016.fig.005a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Stratiform rain frequency (%)</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/ijas/volume-2015/206016/figures/206016.fig.005b.svgz" name="206016.fig.005b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Convective rain frequency (%)</td></tr></table>

<div>Distributions of rainfall characteristics over the WG (left panels) and MWC (right panels) regions: (a) stratiform rain frequency, (b) convective rain frequency. Rain frequency here is defined as ratio of number of rain samples to number of total samples expressed in percentage. Total sample includes stratiform, convective, other, and no rain. Orographic contours are as in Figure <a href="../fig2/">2</a>.</div>

International Journal of Atmospheric Sciences

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Figure 5

Figure 5: Characteristics of Summer Precipitation around the Western Ghats and the Myanmar West Coast 