Extreme rain heads for California's burn scars, raising the risk of mudslides – this is what cascading climate disasters look like
- Written by Amir AghaKouchak, Professor of Civil & Environmental Engineering and Earth System Science, University of California, Irvine
Two powerful storm systems known as atmospheric rivers[1] are heading for northern California and Oregon, a region in the midst of an historic drought.
While the storms will bring much-needed water to a parched region and should significantly lower the wildfire risk, they also bring dangerous new flood and mudslide risks, particularly in areas recovering from wildfires[2].
Wildfires strip away vegetation and leave the soil less able to absorb water. A downpour on these vulnerable landscapes can quickly erode the ground as fast-moving water carries debris and mud with it.
The National Weather Service has warned of ash and debris flows[3] from Oct. 21-26 in several burned areas, including the site of the nearly 1-million-acre Dixie Fire[4] in the Sierra Nevada.
I study cascading hazards like this, in which consecutive events lead to human disasters[5]. Studies show climate change is raising the risk of multiple compound disasters, and it’s clear that communities and government agencies aren’t prepared.
When storms hit burn scars
California has experienced this kind of cascading disaster before.
In early 2017, following years of drought, the region had a wet winter that fueled dense growth of vegetation and shrubs. An unusually warm and dry spring and summer followed, and it dried out the vegetation, turning it into fuel ready to burn. That fall, extreme Santa Ana and Diablo winds – known for their sustained low humidity – created the perfect conditions for wildfires[6].
The Thomas Fire[7] began near Santa Barbara in December 2017 and burned over 280,000 acres. The following January, extreme rainfall hit the region, including the burn scar left by the fire, and caused the deadliest mudslide-debris flow event[8] in California’s history. More than 400 homes were destroyed in about two hours[9], and 23 people died.
These kinds of cascading events aren’t unique to California. Australia’s Millennium Drought (1997-2009) also ended with devastating floods[11] that inundated urban areas and breached levees[12]. A study linked some of the levee and dike failures to earlier drought conditions, such as cracks forming because of exposure to heat and dryness.
Individually, they might not have been disasters
When multiple hazards, such as droughts, heat waves, wildfires and extreme rainfall, interact, human disasters often result.
The individual drivers might not be very extreme on their own, but combined they can become lethal. These types of events are broadly referred to as compound events – for example, a drought and heat wave hitting at the same time. Their combined impact can be harder to forecast. A cascading event involves compound events in succession[13], like wildfires followed by downpours and mudslides.
Video shows how quickly a mudslide overtakes a town.While the drivers and physical mechanisms behind compound and cascading events are not fully understood, they are often linked to large-scale circulation patterns like the El Niño-Southern Oscillation (ENSO). Meanwhile, lack of preparedness and high degrees of vulnerability at the local level can also increase the impacts of multiple connected events.
With compound and cascading events likely to become more common in a warming world, being able to prepare for and manage multiple hazards will be increasingly essential.
Climate change intensifies the risk
Several[14] research studies[15] have shown that compound events with both drought and heat waves have become more severe and frequent[16] in recent years. One study[17] attributed the increase in the risk of these dry-warm events in California to human-caused global warming and projected that the increased risk of dry-warm conditions will continue in the future.
An important physical process responsible for increases in compound drought and heat is land-atmosphere interactions. Evaporation from soil cools down the land surface, similar to how the human body cools down by sweating. During droughts, the lack of moisture limits soil evaporation[18], which increases the surface temperature and eventually the air temperature in the area. Data shows temperatures during droughts are rising in many parts[19] of the United States, including the Southwest – a pattern that is expected to continue in the future[20].
Numerous studies have also shown that droughts and heat waves increase[22] the likelihood of wildfires[23]. And wildfires can trigger other cascading hazards, turning otherwise unexceptional events into human disasters[24].
At the same time, extreme rainfall events are expected to intensify[25] in a warming climate[26]. A warmer atmosphere can hold more moisture, leading to wetter storms. This means there will likely be more burned acres exposed to potentially extreme rainfall events in a warmer world.
[You’re smart and curious about the world. You can read The Conversation daily by subscribing to our newsletter[27].]
Cascading hazards are not limited to rain over burned areas[29]. Soot and ash deposits on snowpack[30] can increase snowmelt, change the timing of runoff and cause snow-driven flooding. Fires are not only increasing in size and severity, they are also occurring at higher elevations and well above the snow line[31].
It’s also important to recognize that human activities and local infrastructure can also affect extreme events. Urbanization and deforestation, for example, can intensify flooding and worsen mud or debris flow events and their impacts.
Managing multiple disasters and climate change
Despite the high risk when extreme rainfall and droughts interact, most research in this area focuses on only one or the other. Different government agencies oversee flood and drought monitoring, warning and management, even though both are extremes of the same hydrological cycle[32].
Recent studies and disasters show a strong need to integrate management and risk reduction[34] strategies of droughts and flood. Focusing on one hazard by one agency can potentially have unintended consequences[35] for another hazard. For example, maximizing reservoir storage[36] when expecting a drought can increase the flood risk.
As a society, we cannot prevent cascading hazards from happening. But we can become better prepared for plausible cascading hazards in a changing climate.
References
- ^ atmospheric rivers (www.noaa.gov)
- ^ recovering from wildfires (theconversation.com)
- ^ warned of ash and debris flows (twitter.com)
- ^ Dixie Fire (inciweb.nwcg.gov)
- ^ consecutive events lead to human disasters (doi.org)
- ^ perfect conditions for wildfires (doi.org)
- ^ Thomas Fire (www.fire.ca.gov)
- ^ mudslide-debris flow event (doi.org)
- ^ two hours (youtu.be)
- ^ AghaKouchak et al., Annual Review of Earth and Planetary Sciences, 2020 (doi.org)
- ^ devastating floods (doi.org)
- ^ levees (doi.org)
- ^ events in succession (doi.org)
- ^ Several (doi.org)
- ^ research studies (doi.org)
- ^ become more severe and frequent (doi.org)
- ^ One study (doi.org)
- ^ lack of moisture limits soil evaporation (doi.org)
- ^ rising in many parts (doi.org)
- ^ continue in the future (doi.org)
- ^ NOAA/NDIS (www.drought.gov)
- ^ droughts and heat waves increase (doi.org)
- ^ likelihood of wildfires (doi.org)
- ^ human disasters (doi.org)
- ^ expected to intensify (doi.org)
- ^ in a warming climate (doi.org)
- ^ You can read The Conversation daily by subscribing to our newsletter (theconversation.com)
- ^ National Wildfire Coordinating Group (maps.nwcg.gov)
- ^ rain over burned areas (doi.org)
- ^ deposits on snowpack (doi.org)
- ^ elevations and well above the snow line (doi.org)
- ^ hydrological cycle (theconversation.com)
- ^ Justin Sullivan/Getty Images (www.gettyimages.com)
- ^ integrate management and risk reduction (doi.org)
- ^ unintended consequences (doi.org)
- ^ maximizing reservoir storage (doi.org)
Authors: Amir AghaKouchak, Professor of Civil & Environmental Engineering and Earth System Science, University of California, Irvine
