Research Article
Influence of Ice Nuclei Parameterization Schemes on the Hail Process
Figure 6
Variation of the regional (118.7°E–120.2°E, 29.4°N–30.4°N) average mixing ratio ((a) unit: mg·kg−1) and the number concentrations ((b) unit: 103 L−1) of ice crystals with time and the variation of the regional average mixing ratio with height from the hail cloud generation to the extinction period ((c) unit: mg·kg−1).
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