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Floods are the most widely occurring and costly natural hazard in the United States. Although maps of theoretical floods associated with given recurrence intervals or exceedance probabilities for a town are often available in the form of Flood Insurance Rate Maps (FIRMs), flood inundation maps show the inundated area for actual and forecast flood stages—filling the gap between maps made for regulatory purposes and maps delineating floods in real time. Flood inundation maps make current flood stages provided by the U.S. Geological Survey, and peak-forecast flood stages projected by the National Weather Service relevant to the public; assist emergency-management workers to evaluate risk, prioritize relief efforts for people and property in flood-prone areas, and are a powerful tool for use in response, mitigation, and damage assessments.

Introduction

Severe flooding occurred in northern Maine from April 28 to May 1, 2008, and damage was extensive in the town of Fort Kent (Lombard, 2010). Aroostook County was declared a Federal disaster area on May 9, 2008. The extent of flooding on both the Fish and St. John Rivers during this event showed that the current Federal Emergency Management Agency (FEMA) Flood Insurance Study (FIS) and Flood Insurance Rate Map (FIRM) (Federal Emergency Management Agency, 1979) were out of date. The U.S. Geological Survey (USGS) conducted a study to develop a flood inundation map library showing the areas and depths for a range of flood stages from bankfull to the flood of record for Fort Kent to complement an updated FIS (Federal Emergency Management Agency, in press).

Hydrologic analyses that support the maps include computer models with and without the levee and with various depths of backwater on the Fish River. This fact sheet describes the methods used to develop the maps and describes how the maps can be accessed.

Inputs Necessary for Flood Inundation Mapping

Flood surveying and documentation (Lombard, 2010) and the field work for a new FEMA FIS and FIRM provided many of the elements needed to develop flood inundation maps.

Lidar Elevation Data

Light detection and ranging (lidar) technology supports the rapid collection of high-accuracy elevation data for large areas. Lidar uses an airplane equipped with laser range finders that pulse tens of thousands of times a second and a

River

high-precision global positioning system (GPS). The result is topographic data with a vertical accuracy equivalent to 2-foot contour intervals. Topographic maps with this level of detail provide elevation data for the banks and flood plains along a river for both hydraulic models and flood mapping.

Surveyed Elevation Data

High water marks were surveyed following the flood; the survey provided calibration points for updating the hydraulic models of these rivers. Additional field data included elevation data measured with a total-station theodolite and underwater depths measured with an Acoustic Doppler Current Profiler (ADCP) referenced to the elevation of the water surface at the time of the survey. Underwater and channel-bank field-survey data were merged with lidar data to create a final base map of high-precision elevation data.

Lidar data for Fort Kent, Maine, 2009. (Lidar, light detection and ranging)

Figure 2. Lidar data for Fort Kent, Maine, 2009. (Lidar, light detection and ranging)

Flood-Forecast Streamgages

The gages on the St. John River below the Fish River at Fort Kent (USGS streamgage 01014000, not shown on fig.

1) and on the Fish River near Fort Kent

(USGS streamgage 01013500) are both used as flood-forecast streamgages by the National Weather Service (National Oceanic and Atmospheric Administration, 2010). The current and forecasted water levels are linked to the flood-inundation maps.

Interaction of St. John and Fish Rivers

Flood inundation maps for Fort Kent include flood inundation boundaries and depths for both the St. John and Fish Rivers. Backwater from the St. John River affects flood elevations on the Fish River, with the greatest interaction at the mouth. The flood inundation map library consists of a set of maps developed at 1-foot contour intervals for a total of nine stages (20.6 to 28.6 feet) at the St. John River streamgage in Fort Kent (01014000) and for a total of seven stages (8.3 to 14.3 feet) at the Fish River streamgage at Fort Kent (01013500). The user can select the map that best matches current or forecast stages at the St. John and Fish River streamgages to see the areal extent of expected inundation.

U.S. Geological Survey National Flood Inundation Mapper showing Fort Kent, Maine, and accessed at http://wim.usgs.gov/FIMI/.

Figure 3. U.S. Geological Survey National Flood Inundation Mapper showing Fort Kent, Maine, and accessed at http://wim.usgs.gov/FIMI/.

Maps Available in Multiple Formats

The flood inundation map library for Fort Kent is available to water managers and the public in multiple formats: downloadable geographic information system (GIS) file format, keyhole markup language (KML) format, and portable document format (PDF). The Fort Kent flood inundation map library is also available through the USGS Flood Inundation Mapper at http://wim.usgs.gov/FIMI/(fig. 3). This interactive tool allows the user to select maps according to flood stages at USGS streamgaging stations or NWS flood-warning forecasts. All maps and supporting documentation are available at: http://water.usgs.gov/osw/flood_inundation/projects/fort-kent/.

References Cited

Federal Emergency Management Agency, 1979, Flood insurance study, Town of Fort Kent, Aroostook County, Maine: Washington, D.C., December 1979, 19 p.

Lombard, P.J., 2010, Flood of April and May 2008 in northern Maine: U.S. Geological Survey Scientific Investigations Report 2010–5003, 17 p. (Also available at http://pubs.usgs.gov/sir/2010/5003/.)

Lombard, P.J., 2011, Flood inundation maps for the St. John and Fish Rivers in Fort Kent, Maine: U.S. Geological Survey Scientific Investigations Map 3157, 8 p.

National Oceanic and Atmospheric Administration, 2010, National Weather Service Advanced Hydrologic Prediction Service, accessed October 10, 2010 at http://water.weather.gov/ahps/.

U.S. Army Corps of Engineers, 2001, Hydrologic Engineering Center, River Analysis System (HEC–RAS), version 4.0. —By Pamela J. Lombard

For more information, please contact:

Robert Lent, Director USGS Maine Water Science Center 196 Whitten Road Augusta, Maine 04330 Telephone: (207) 622-8201 E-mail: dc_me@usgs.gov

Where this page came from

This page was imported from U.S. Geological Survey. Published by the U.S. Geological Survey and, as a work of the United States government, in the public domain.

Nobody has written it yet — it is the source material at a new address, which is why search engines are asked to skip it and why no one earns from it. It is up for grabs: take it on, and it is yours to rewrite and to earn from.

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Licence: CC0 1.0 (public domain) · Adapted from pubs.usgs.gov

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