Spatial and Temporal Features of the Frequency of Cloud Occurrence over China Based on CALIOP

<table class="figure-group"><tr class="fig-image" id="a"><td><object data="https://static.hindawi.com/articles/amete/volume-2017/4548357/figures/4548357.fig.005a.svgz" name="4548357.fig.005a" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(a) </b>Cloud top temperature (°C)</td></tr><tr class="fig-image" id="b"><td><object data="https://static.hindawi.com/articles/amete/volume-2017/4548357/figures/4548357.fig.005b.svgz" name="4548357.fig.005b" type="image/svg+xml"></object></td></tr><tr class="fig-caption"><td><b>(b) </b></td></tr></table>

<div>(a) Horizontal distribution of the cloud top temperature of single-layer cloud over China and surrounding areas; (b) PDF of the cloud top temperature of single-layer cloud over Tibetan Plateau (TP) and East China (EA). The shaded part indicates that the surface elevation is above 3.1 km (680 hpa).</div>

Advances in Meteorology

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Figure 5

Figure 5: Spatial and Temporal Features of the Frequency of Cloud Occurrence over China Based on CALIOP 