Officials issuedevacuationorders for people living downhill from several of California’s wildfire burn scars on Oct. 24, 2021, as a powerful storm system known as an atmospheric river began to drench the West Coast.
While the storm brings much-needed water to a region in the midst of an historic drought, and should significantly lower the wildfire risk after a destructive fire year, it also brings dangerous new flood and mudslide risks, particularly in areas recovering from wildfires.
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 issued flash flood warnings and warned of ash and debris flows through Oct. 26 in several areas that recently burned, including the sites of the Alisal Fire near Santa Barbara, California, and the nearly 1-million-acre Dixie Fire in the Sierra Nevada. Near San Jose, two counties ordered evacuations near large areas that burned in the Santa Cruz Mountains in 2020.
I study cascading hazards like this, in which consecutive events lead to human disasters. 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.
The Thomas Fire 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 in California’s history. More than 400 homes were destroyed in about two hours, 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 that inundated urban areas and breached levees. 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, like wildfires followed by downpours and mudslides.
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
Severalresearch studies have shown that compound events with both drought and heat waves have become more severe and frequent in recent years. One study 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, which increases the surface temperature and eventually the air temperature in the area. Data shows temperatures during droughts are rising in many parts of the United States, including the Southwest – a pattern that is expected to continue in the future.
At the same time, extreme rainfall events are expected to intensifyin a warming climate. 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.
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.