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.004a.svgz" name="206016.fig.004a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Stratiform rain percentage</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/ijas/volume-2015/206016/figures/206016.fig.004b.svgz" name="206016.fig.004b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b>Convective rain percentage</td></tr></table>

<div>Spatial patterns of stratiform (a) and convective (b) percentage of the WG (left panel of each figure) and MWC (right panel of each figure). Pixels where the total precipitation is &lt;0.15 mm/h are deleted from these and all the following percentage plots. Orographic contours are as in Figure <a href="../fig2/">2</a>.</div>

International Journal of Atmospheric Sciences

fig4

Figure 4

Figure 4: Characteristics of Summer Precipitation around the Western Ghats and the Myanmar West Coast 