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Flood frequency analysis is a technique used to estimate flood risk, providing statistics such as the ‘100-year flood’ or ‘500-year flood’ that are critical to flood risk management and resilience; including infrastructure design, dam safety analysis, and flood mapping. But the method used to calculate these flood frequencies is due for an update, according to a new study by scientists from the Desert Research Institute (DRI), University of Wisconsin-Madison, and Colorado State University.

Floods, even in a single watershed, are known to be caused by a variety of sources, including  rainfall, snowmelt, or ‘rain-on-snow’ events in which rain falls on existing snowpack. However, flood frequencies have traditionally been estimated under the assumption these flood drivers, or root causes, are unimportant.

In a new open-access paper in Geophysical Research Letters, a team led by Guo Yu, Ph.D., of DRI examined the most common drivers (rainfall, snowmelt, and rain-on-snow events) of historic floods for 308 watersheds in the Western US, and investigated the impact of different flood types on the resulting flood frequencies.

Their findings showed that most (64 percent) watersheds frequently experienced two or three flood types throughout the study period, and that rainfall-driven floods, including rain-on-snow, tended to be substantially larger than snowmelt floods across watershed sizes.  

Further analysis showed that by neglecting the unique roles of each flood type, conventional methods for generating flood frequency estimates tended to result in under-estimation of flood frequency at more than half of sites, especially at the 100-year flood and beyond.

“In practice, the role of different mechanisms has often been ignored in deriving the flood frequencies,” said Yu, a Maki postdoctoral research associate at DRI. “This is partly due to the lack of physics-based understanding of historic floods. In this study, we showed that neglecting such information can result in uncertainties in estimated flood frequencies which are critical for infrastructure.”

The study findings have important implications for estimating flood frequencies into the future, as climate change pushes conditions in snowmelt-dominated watersheds toward increased rainfall.

“How the 100-year flood will evolve in the future due to climate change is one of the most important unanswered questions in water resources management,” said Wright, an associate professor in Civil and Environmental Engineering at University of Wisconsin-Madison. “To answer it, we need to focus on the fundamental science of how the water cycle, including extreme rainstorms and snow dynamics, are and will continue to change in a warming climate.”

“This study shows that taking into account different physical processes can improve flood risk assessment,” said Frances Davenport, Ph.D., postdoctoral research fellow at Colorado State University. “Importantly, this result suggests both a need and opportunity to develop new methods of flood frequency assessment that will more accurately reflect flood risk in a warming climate.”

The full study, Diverse Physical Processes Drive Upper-Tail Flood Quantiles in the US Mountain West, is available from Geophysical Research Letters: 

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