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<br />4. STANDARD PROJECT STORM. The Standard Project Storm (SPS) is defined as that <br />combination of severe meteorological events that gives the maximum precipnation <br />reasonably characteristic of the geographic region of interest, excluding extremely rare <br />events, Since the SPS is an infrequent event, no specnic frequency can be assigned to <br />n. It may range from a return interval of a few hundred years to a few thousand years, <br />The SPS has been used by the Corps of Engineers as a design storm in which only a <br />small degree of risk of exceedance can be tolerated such as in the design of an urban <br />f1oodwall, It is usually used for comparison wnh the recommended protection for a <br />particular project, Because the Standard Project Storm (SPS) is used mainly wnhin the <br />Corps of Engineers, only a limned number of publications describe its derivation and use, <br />in contrast to materials available on hypothetical-frequency storms and the Probable <br />Maximum Stonn, EM 1110-2-1411 describes the SPS derivation for the Unned States east <br />of 1050 longitude, SPS development for the remainder of the Unned States must be <br />based on various published and unpublished Corps District reports and procedures, <br /> <br />5. PROBABLE MAXIMUM STORM. <br /> <br />The Probable Maximum Storm (PMS) is defined as the most severe combination <br />of meteorological occurrences considered reasonably possible in a particular region, It is <br />felt to be an upper limit of flood-producing rainfall (or snowpack melting when applicable) <br />and is used as a design storm where virtually no risk of flooding can be tolerated, The <br />PMS has historically been used in dam design to ensure the adequacy of spillways and <br />top-of-dam elevations for high dams, <br /> <br />As wnh the hypothetical frequency storms, one set of generalized criteria is applied <br />to the majorny of the U.S" and a variety of regional crneria, accounting primarily for <br />orographic effects, to the balance, Details for constructing a PMS for a particular region <br />are given in the various Hydrometeorological Reports and Technical Papers listed in the <br />references, The reports, HMR-51 and HMR-52, for the Unned States east of the 105th <br />meridian, apply generally to the eastern plains portion of Colorado, The mechanics of <br />stonn breakdown and arrangement presented in these reports are similar to methods for <br />the western Unned Stated presented in other publications, <br /> <br />5.1. PMS FOR EAST OF THE '103rd MERIDIAN. The steps for deriving a PMS, <br />using Probable Maximum Precipitation data from HMR-51 and data for the detennination <br />of shape, orientation, and distribution from HMR-52, <br /> <br />5.1.1. Determine isohyetal Probable Maximum Precipnation (PMP) values for the <br />study area for desired drainage area sizes (10,100,200, 1,000,5,000, 10,000,20,000 <br />square miles) and for corresponding storm durations (6-, 12-,24-,48-, and 72"hours) using <br />the appropriate plates from the report, <br /> <br />5.1.2, Plot a family of duration curves (6-, 12-, 24-, 48-, and 72-holJrs) for PMP <br /> <br />Colorado Flood <br />Hydrology Manual <br /> <br />DRAFT <br /> <br />7,11 <br />