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Last modified
1/26/2010 10:10:21 AM
Creation date
10/5/2006 4:37:09 AM
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Floodplain Documents
County
Statewide
Basin
Statewide
Title
Colorado Statewide Drainage Floodplain Management Criteria Manual
Date
8/1/2002
Prepared By
CWCB & WRC Engineering Inc
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br />. <br /> <br /> <br />COLORADO STATEWIDE <br />DRAINAGE AND FLOODPLAIN MANAGEMENT CRITERIA MANUAL <br /> <br />. <br /> <br />. <br /> <br />CHAPTER 5 <br />HYDROLOGY <br /> <br />SECTION 1.0 <br />RAINFALL <br /> <br />CHAPTER 5 <br />HYDROLOGY <br /> <br />SECTION 1.0 <br />RAINFALL <br /> <br />1.1 INTRODUCTION <br /> <br />Due to the complexity of the natural terrain, orographic effects of the Rocky <br />Mountains, and semi-arid climate of the region, the type and duration of rainstorms <br />can vary substantially within the State of Colorado. However, rainstorm events can <br />be generally defined as short duration convective storms or long duration general <br />rainstorms. <br /> <br />The short duration convective storms (cloudbursts/thunderstorms) can produce high <br />rainfall intensities for a short period and generally cover watershed areas of less than <br />200 square miles. Convective storms are commonly known to be responsible for high <br />peak flows and flooding problems for many small drainage basins. The long duration <br />general rainstorms can produce rain coverage over a large watershed area for a <br />period in excess of six hours up to several days. General rainstorms can produce <br />large amount of total rainfall runoffs and sometimes generate higher peak flows than <br />the convective storms. Depending on the purpose of the hydrologic analysis, it may <br />be necessary to analyze both types of rainstorms in order to estimate the high peak <br />flow rate and the high runoff volume for a given drainage basin. <br /> <br />The information presented in this section is the state-of-art information available at <br />the time of preparation of this manual and should be updated as better techniques <br />and new rainfall data become available in the future. <br /> <br />1.2 RAINFALL DATA <br /> <br />The rainfall data published by National Oceanic and Atmospheric Administration <br />(NOM) in their "Precipitation-Frequency Atlas of the Westem United States, Volume <br />III - Colorado, 1973" should be used to perform necessary hydrologic calculations <br />within the State of Colorado, unless site-specific <br />rainfall studies have been performed and adopted <br />by the local govemment agency having <br />jurisdiction over the study area. <br /> <br />The NOM Atlas 6-hour and 24-hour precipitation <br />frequency maps for various storm events for the <br />State of Colorado are included as Figures CH5- <br />F101 through CH5-F112. The 6-hr and 24-hr point <br />precipitation values can be estimated directly from <br />Figures CH5-F101 through CH5-F112, and these <br />point rainfall values can then be used to develop <br />5-minute, 10-minute, 15-minute, 30-minute, 1- <br />hour, 2-hour, 3-hour, and 12-hour rainfall depths <br />using the procedures outlined in this section. <br /> <br />AUGUST 2002 <br /> <br />RAINFALL <br /> <br />The Rational Method can <br />be used for drainage <br />basins with a total <br />contributing area of less <br />than 160 acres. <br /> <br />For drainage basins with <br />an area greater than 90 <br />acres, CHUP and/or <br />HEC-1 computer models <br />should be used to <br />estimate the runoff data. <br /> <br />CH5-1 03 <br />
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