Across the Southeastern United States, hundreds of roads are closed, power outages continue to be reported and catastrophic flooding devastated mountain towns as the fallout from Hurricane Helene swept through parts of Georgia, the Carolinas and Virginia this weekend.
Majid Shafiee-Jood, a research assistant professor of civil and environmental engineering at the University of Virginia, discusses how and why this is happening. Shafiee-Jood researches decision-making based on hazardous weather information, including hurricane bulletins, flash-flood warnings and evacuation orders.
Q. Why are we seeing spinoff storms as a result of hurricanes further south?
A. Hurricanes are rapidly rotating storms systems with strong winds and a spiral arrangement of thunderstorms. Hurricanes typically contain massive amounts of moisture, which could lead to heavy rainfall. Depending on the size or speed of the storm, they can generate massive flooding. These are typically referred to as flash floods – flood events that occur in a short period after a storm, typically within six hours and often within three hours of the storm. This is different than flooding seen in coastal areas induced by storm surge, known as coastal flooding.
Flash floods happen because you have significant rainfall in one region in a short period of time. It can happen anywhere. In urban areas with significant development, it can happen because the rain doesn’t have much space to penetrate into the ground. In the mountainous areas with steep slopes, especially when soils are saturated, intense rainfall can rapidly turn into flash floods, which are sometimes accompanied by mudslides and landslides. That’s what we’re witnessing right now in western North Carolina and parts of Virginia.