HIGHLIGHTS
SUMMARY
The authors focus on the "fire effect" in the new WRF simlations, which refers to the difference between FIRE and NOFIRE runs hereinafter. When it comes to the difference between WRF-FIRE and WRF-NOFIRE, however, it is very small; Fig 2 shows the differences (FIRE-NOFIRE) in the spatial patterns of monthly accumulated surface rainfall (Fig 2a) and the time series of precipitation rates in the three regions (Fig 2b-d). Indeed, the FIRE-NOFIRE differences in area-mean monthly total rainfall (mm) is on the order of 100 (mm), which is much . . .
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