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Characteristics of Convective Storm Top Altitudes in Summer over the Tibetan Plateau by GPM

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Figure

Figure 2. Samples for different storm top altitudes that the rain rate is greater than 0.2 mm/h in June (a), July (b) and August (c) over the Tibetan Plateau and surrounding regions
Figure 3. Distributions of deep convection frequency over the Tibetan Plateau and surrounding regions
Figure 5. PDF of deep convections in June (a), July (b), August (c), and JJA (d) over the Tibetan Plateau and surrounding region.
Figure 7. Mean precipitation profiles and reflectivity profiles of convective precipitation in summer

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