Research Article
The Sensitivity of Heavy Precipitation to Horizontal Resolution, Domain Size, and Rain Rate Assimilation: Case Studies with a Convection-Permitting Model
Figure 3
(a) Surface (shading, in Kelvin) and horizontal wind at 1 km height, (b) East-west vertical cross section of 29S–25S averaged and () vector at 12 UTC 9 January 2011.
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