Results show a need to revise existing methods for calculating flood risk
Desert Research Institute
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 infrastructure design, dam safety analysis, and flood mapping in flood-prone areas.
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
U.S., 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."
The
study team hopes that this research is useful to engineers, who rely on
accurate estimates of flood frequencies when building bridges and other
infrastructure. Although many engineers realize that there is a problem with
the conventional way of estimating flood frequencies, this study provides new
insights into the level of inaccuracy that results.
"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." length.