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Last modified
11/23/2009 10:51:24 AM
Creation date
10/4/2006 9:35:57 PM
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Template:
Floodplain Documents
County
Statewide
Community
State of Colorado
Title
Colorado Flood Hydrology Manual - Section 22 Program
Date
9/1/1993
Prepared For
CWCB
Prepared By
US Army Corps of Engineers
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br /> <br />that the 1-hour percentages based on this time distribution have occasionally been <br />found to give rainfall values that are not sufficiently conservative, particularly in the <br />Southwestern Division of the Corps of Engineers (SWD). <br /> <br />5. PROBABLE MAXIMUM STORM. <br /> <br />The Probable Maximum Storm (PMS) is defined as the most severe <br />,combination of meteorological occurrences considered reasonably possible in a <br />particular region. It is felt to be an upper limit of flood-producing rainfall (or snowpack <br />melting when applicable) and is used as a design storm where virtually no risk of <br />flooding can be tolerated. The PMS has historically been used in dam designto ensure <br />the adequacy of spillways and top-of-dam elevations for high dams. <br /> <br />As with the hypothetical frequency storms, one set of generalized criteria <br />is applied to the majority of the U.S., and a variety of regional criteria, accounting <br />primarily for orographic effects, to the balance. Details for constructing a PMS for a <br />particular region are given in the various Hydrometeorological Reports and Technical <br />Papers listed in the references. The reports, HMR-51 and HMR-52, for the United <br />States east of the 105th meridian, apply to most of the country and are discussed <br />further here. The mechanics of storm breakdown and arrangement presented in these <br />reports are similar to methods for the western United Stated presented in other <br />publications. <br /> <br />5.1. PMS FOR THE EASTERN AND CENTRAL UNITED STATES. The <br />steps for deriving a PMS, using Probable Maximum Precipitation data from HMR-51 <br />and data for the determination of shape, orientation, and distribution from HMR-52. <br /> <br />5.1.1. Determine isohyetal Probable Maximum Precipitation (PMP) values <br />for the study area for desired drainage area sizes (10, 100, 200, 1,000, 5,000, <br />10,000,20,000 square miles) and for corresponding storm durations (6-,12-,24-,48- <br />, and 72-hours) using the appropriate plates from the report. <br /> <br />5.1.2. Plot 11 family of duration curves (6-, 12-, 24-, 48-, and 72-hours) <br />for PMP intensities versus drainage area size on semi-logarithmic paper. <br /> <br />5.1.3. Interpolate for the desired storm area, determine PMP intensities <br />for each duration and plot on ordinary graph paper. <br /> <br />5.1.4. Determine rainfall in each 6-hour time interval by interpolation, <br />then increment the rainfall by successive subtractions. The PMP will be the maximum <br />value for the selected storm area only; areas greater or less than the selected storm <br />area will show smaller values of PMP. Considerable trail and error computations will <br />normally be required to determine the storm area which maximizes average <br /> <br />7-19 <br /> <br />. <br /> <br />
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