The Sensitivity of Heavy Precipitation to Horizontal Resolution, Domain Size, and Rain Rate Assimilation: Case Studies with a Convection-Permitting Model

<div>The TSA and BS of hourly rainfalls from different model configurations from 7 UTC 9 January 2011 to 12 UTC 10 January 2011 using E210 as “truth.” (a) Shows TSA of E210 (CTL), E210RP1, E210RP2, E210ICR1, E210ICR2, and ENSM, (b) shows TSA of E210, E110, E100, E211, E221, E220, E310, E320, E321, E340, and E440, and (c) shows BS of all experiments.</div>

Advances in Meteorology

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Figure 16

Figure 16: The Sensitivity of Heavy Precipitation to Horizontal Resolution, Domain Size, and Rain Rate Assimilation: Case Studies with a Convection-Permitting Model 

Figure 16 | The Sensitivity of Heavy Precipitation to Horizontal Resolution, Domain Size, and Rain Rate Assimilation: Case Studies with a Convection-Permitting Model 