Yet another winter storm is slated to send more rain to Southern California this week and we at RedZone think it warrants a little inside info on the risks of post-fire debris flows. Winter rains mean a higher potential for land-moving rainfall rates in areas where fires have scorched the landscape. After 2018’s tragic events that occurred in the Thomas fire burn scar, officials have not taken the potential of these continued storms lightly. Last winter, residents were evacuated near the Holy, Thomas, Cranston, Napa/Sonoma, and Woolsey fires (all burn scars from the last couple years).
Although vegetation grows back in approximately five years after a fire, researchers estimate that it takes up to two decades for a hillside’s soil to be restored to pre-fire conditions. Strong rains that happen during that five-year window bring a heightened chance that debris flows could occur. This is best explained by NOAA’s “Flood After Fire Fact Sheet”.
Rain after Fire can equal Debris Flows
Large-scale wildfires dramatically alter the terrain and ground conditions. Normally, vegetation resides across the landscape and absorbs any rainfall, reducing runoff. However, wildfires leave the ground charred, barren, and unable to absorb water, creating conditions ripe for flash flooding and mudflow. Steeper the terrain and closer to the runoff zones the higher the debris flow risk is until the vegetation is restored.
Flooding after fire is often more severe, as debris and ash left from the fire can form mudflows. As rainwater moves across charred and denuded ground, it can also pick up soil and sediment and carry it in a stream of floodwaters. These mudflows can cause significant damage.
This blog was originally posted on February 13, 2019. It has been updated by RedZone December 24th, 2019.