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.
(a)
(b)