Climate Science Glossary

Term Lookup

Enter a term in the search box to find its definition.


Use the controls in the far right panel to increase or decrease the number of terms automatically displayed (or to completely turn that feature off).

Term Lookup


All IPCC definitions taken from Climate Change 2007: The Physical Science Basis. Working Group I Contribution to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, Annex I, Glossary, pp. 941-954. Cambridge University Press.

Home Arguments Software Resources Comments The Consensus Project Translations About Support

Twitter Facebook YouTube Mastodon MeWe

RSS Posts RSS Comments Email Subscribe

Climate's changed before
It's the sun
It's not bad
There is no consensus
It's cooling
Models are unreliable
Temp record is unreliable
Animals and plants can adapt
It hasn't warmed since 1998
Antarctica is gaining ice
View All Arguments...

New? Register here
Forgot your password?

Latest Posts


Coping with fire-scorched land more prone to mudslides

Posted on 28 December 2020 by Guest Author

This is a re-post from Yale Climate Connections by Daisy Simmons

After a fire, rain can feel like a refreshing mercy. But it also spells fresh danger in fire-struck areas made newly vulnerable to mudslides. Amidst recovering from the trauma of a wildfire, people in hillside homes across much of the western U.S., in particular, must now be ready to evacuate when threatening heavy rains appear in the forecast.

That’s because fires do more to the physical environment than level buildings and fell trees. They also alter the makeup of the soil, making it less likely it will absorb rainwater, especially during a downpour.

“The same intensity of rain can generate overland flows more than 10 times greater in areas recently burned compared to those without fire,” Arizona State University (ASU) environmental engineer Mikhail Chester said in Popular Science.

To explain why fire-scorched land is more prone to mudslides, and what communities can do about it, let’s begin with the basics.

What causes a debris flow?

On a typical hillside not recently burned, vegetation helps trap the soil in place. When rain pours down in a major storm, trees, shrubs, grasses, and leaf litter all help protect the soil from a heavy downpour, giving water more time to soak into the ground.

As much as 5 years after the raging embers have cooled, resulting mudflows can pose still more threats.

But when fire destroys that vegetation, there can be little left to keep soil and sediment from flowing down a steep hill, much less retain water there. What’s more, parched, fire-charred soil can become hydrophobic, which means it actually repels water, just as pavement does.

Wildfire burn graphic(Source: National Weather Service)

When intense rain falls on water-repellant ground, the water runs downhill quickly – more than double its usual rate – forming a river of mud and other debris. All the while, the expanding flow can pick up whatever it encounters along the way, from mud, rock, and sediment, to larger debris like fallen trees and limbs and boulders, depending on the severity of the rain and vulnerability of the soil.

The California Department of Water Resources advises that fast-moving debris flows can rock homes off their foundations and sweep away vehicles, creating life-threatening dangers.

The results can be tragic, as was the case in Montecito, California, in 2018, shortly after the deadly Thomas Fire laid bare much of the landscape. A half-inch of rain fell in just 15 minutes, unleashing a debris flow that was an estimated 25 to 30 feet deep, moving at roughly 10-15 mph, and capable of carrying boulders as big as a tow truck. The catastrophe claimed at least 21 lives, destroyed more than 100 homes, and shut down Highway 101, a major north-south route, for almost two weeks.

How fire-struck communities can mitigate the risk

Looking ahead, the likelihood of post-fire debris and mud flow is likely to increase, in large part because climate change is already leading to the intensity of more fires across the West. A joint study by ASU and University of California, Los Angeles researchers found that the chances of post-fire debris flow risk will generally increase as climate change intensifies.

To protect people and property from this growing threat, communities should first and foremost be aware of the risks they and their populations face. The California Department of Conservation advises that residents of fire-struck areas be prepared for potential debris flows for as long as two to five years after major fires.

From there, communities that have recently experienced wildfire should consider the following safety tips:

  • Understand the risk at a local level. Visit the USGS’s post-fire debris-flow hazard assessments page for data-driven estimates on the probability and volume of debris flows in the aftermath of major fires in the western U.S. Beyond that, heed CDC to just “assume” that steep, burned hills will be more vulnerable to debris flows.
  • Be prepared to evacuate. Make sure you have an emergency evacuation plan. Listen to weather reports, and be ready to leave the area if heavy rains are on the way and you live on a hillside or downslope area that may be susceptible to mud or debris flows.
  • Know the signs of an impending debris flow. According to CDC, warning signs include sudden changes in water level of a stream or creek, or trickling mud or rumbling sounds that might indicate approaching flow. Visit the Red Cross website for more detail on what to do before and during a mud or debris flow.

Take proactive measures to defend against future mudflow. The California Conservation Corps’ Paradise Erosion Control Project is one example of how a community can take preventive actions. There, to mitigate the loss of ground cover caused by the Camp Fire, volunteers placed wattles, sandbags, silt socks, and drainage inlet treatments to help slow runoff and erosion in vulnerable areas around the town of Paradise in the Sierra Nevada foothills above the northeastern Sacramento Valley.

Colorado State University’s extension service offers more detailed post-fire soil erosion control strategies, ranging from spreading straw mulch to protect soil and reseeding efforts, to creating log terraces that help slow the velocity of the runoff.

Like so many other difficult climate-related impacts, the risk of mudslides in fire-scorched areas is a problem more communities will be facing in the years ahead. By staying actively informed and prepared, people in these vulnerable areas can help keep themselves, and their neighbors and communities, ahead of the threat.

0 0

Printable Version  |  Link to this page


There have been no comments posted yet.

You need to be logged in to post a comment. Login via the left margin or if you're new, register here.

The Consensus Project Website


(free to republish)

© Copyright 2023 John Cook
Home | Translations | About Us | Privacy | Contact Us