Over the past three months, the United States has been inundated by a series of wintertime floods unusual in their scope and severity. Especially hard hit were California and the Pacific Northwest around the year-end holidays and the Ohio Valley in early March. Total damage is in the billions, and dozens of people have been killed. More trouble may be on the way. With an extremely heavy winter snowpack beginning to melt this spring, the Red River Valley of North Dakota and Minnesota is bracing for what is expected to be its worst flooding on record.
What seasonal weather patterns have placed so much of the country at risk for flooding? How does society exacerbate flooding and its dangers? What is the difference between a flash flood and a river flood? To help you answer these and other questions, below is some background information on U.S. flood risk from a newly published report by Roger Pielke, Jr., of the National Center for Atmospheric Research (NCAR) in Boulder, Colorado. Also below is a list of flood and flash-flood experts and some relevant World Wide Web sites. NCAR is operated by the University Corporation for Atmospheric Research (UCAR) under sponsorship by the National Science Foundation.
---Experts on flooding
Roger Pielke, Jr. 303-497-8111 firstname.lastname@example.org
NCAR/Environmental and Societal Impacts Group
Specialty: Societal aspects of extreme weather events, including flooding
A political scientist, Pielke has completed "Midwest Flood of 1993: Weather, Climate, and Societal Impacts," an in-depth study of the U.S. flood hazard that uses the Midwest flood to examine how society deals with its vulnerability to flooding (see p. 3, Background). The report is one of a series being prepared for the Extreme Mesoscale Events and Impacts project.
Matthew Kelsch 303-497-6719 email@example.com
National Oceanic and Atmospheric Administration (NOAA)/Forecast Systems Laboratory, Boulder, Colorado
Kelsch, a meteorologist, is one of the lead instructors for an April course at UCAR that will train National Weather Service (NWS) personnel in state-of-the-art forecast techniques. He has tested and evaluated software that uses NWS/WSR-88D radar returns to estimate rainfall accumulations.
Bob Davis 412-262-1591, ext. 401 firstname.lastname@example.org
Specialty: Software to assess runoff from heavy rain and subsequent flash-flood risk
Davis, a meteorologist, has created a program called AMBER (Annual Mean Basin Estimated Rainfall) which combines rainfall data from the NWS/WSR-88D radar network with geographic information system (GIS) data bases. The program is being developed for nationwide use by NWS offices to estimate flood risk in stream basins as small as five square miles.
Eve Gruntfest 719-262-3513 email@example.com
University of Colorado at Colorado Springs/Department of Geography
Specialty: Flash flood mitigation; disaster mitigation; societal impacts of warnings and responses
Gruntfest, a geographer, has participated in on-site surveys of a number of major flood disasters, including Colorado's Big Thompson Canyon flood of 1976 and the Midwest floods of 1993.
Mary Fran Myers 303-492-2150 firstname.lastname@example.org
University of Colorado/Natural Hazards Research and Applications Information Center
Specialty: Policy responses to floods and other natural hazards
Myers, codirector of the Natural Hazards Center, is an expert on the National Flood Insurance Program and other federal policies regarding flood control and management.
---World Wide Web sites for information on flooding
Monthly summary of national water conditions
U.S. Geological Survey
Flood story ideas and relevant links NWS Office of Public Affairs
Bibliography of research on water resources
U.S. Geological Survey/Colorado District
Flood plain management
U.S. Army Corps of Engineers/Flood Plain Management Services Program
Background on flood hazards, insurance, and mitigation
Federal Emergency Management Agency
http://www.fema.gov/fema/finifp.html (home page)
(National Flood Insurance Program)
---Background information on flooding
The Web links above, and much of the information below, come from "Midwest Flood of 1993: Weather, Climate, and Societal Impacts," by Roger Pielke, Jr. The 160-page report summarizes the history of U.S. flood policy, vulnerability, and response and examines the 1993 flood in that context. It is available from NCAR's Environmental and Societal Impacts Group (303-497-8117, email@example.com).
What are the elements of a flash flood and a river flood?
Flash floods are short-term inundations of small areas such as a town or parts of a city, usually by tributaries and creeks. Heavy rain in a few hours can produce flash flooding even in places where little rain has fallen for weeks or months. If heavy rainfall occurs repeatedly over a wide area, then river or mainstem flooding becomes more likely, in which the main rivers of a region swell and inundate large areas, sometimes well after rainfall has ended. The 1993 Midwest floods were caused by 77 events over several months where rainfall of greater than one inch occurred over areas 100 to 200 miles wide and 400 to 600 miles long. Both flash flooding and river flooding threaten life and property, although the former causes more deaths and the latter more property damage.
Are the death tolls from U.S. floods increasing?
On average, U.S. flooding kills more than 100 people a year--
more than any other single weather hazard, including tornadoes and hurricanes. The average flooding toll has increased in recent decades while deaths from tornadoes and hurricanes have dropped. Almost half of all flash-flood deaths are connected to stream crossings or highway travel. Victims often underestimate the power of water when driving into flooded areas. It takes only 18 inches of water to float a typical automobile.
How can a 100-year flood occur more than once in a short period?
A 100-year flood is one that has a one-percent chance of being exceeded in a given year. Few locations have rainfall records of more than a century, so 100-year flood values are estimates rather than certainties. Changes in watershed management, land use, and the like can affect streamflow characteristics and alter the likelihood of a given flood. Moreover, climatic patterns themselves can change. There is nothing to prevent more than one "100-year flood" from occurring at a given spot over a century.
Is global warming causing more floods?
Because flood risk is the result of both environmental and societal factors, it is difficult to single out the impact of climate variations. According to the United Nations Intergovernmental Panel on Climate Change, the average global temperature at the surface has increased about 1.0 degree Fahrenheit this century. At the same time, according to NOAA, there has been a steady increase in the area of the United States affected by extreme precipitation events (more than two inches of rain in one day, or the equivalent in snow). However, flood reports have not increased uniformly across the country. For instance, streamflows in the Colorado River basin have decreased over the past 60 years. Any alteration of global climate can bring either an increase or decrease in precipitation or flood events at a given location. Current computer models of climate are unable to project local variations with certainty.
Are societal choices increasing flood risk?
According to a report by the U.S. Congress's Office of Technology Assessment, "despite recent efforts, vulnerability to flood damages is likely to continue to grow." The factors cited include
--growing populations in and near flood-prone regions
--the loss of flood-moderating wetlands
--increased runoff from paving over soil
--new development in areas insufficiently mapped for flood risk
--the deterioration of decades-old dams and levees
--policies such as subsidies that encourage development in flood plains.
Find this press release on the World Wide Web at http://www.ucar.edu/ucargen/press/flooding.html
To receive UCAR and NCAR press releases by e-mail,
telephone 303-497-8601 or e-mail firstname.lastname@example.org
Materials provided by University Corporation for Atmospheric Research. Note: Content may be edited for style and length.
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