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<br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br /> <br />2. A W A Team Study Approach <br /> <br />The approach taken by the A W A team to determine site-specific PMP values for <br />the Cherry Creek drainage is as follows: <br /> <br />1. Adhere to the published definition ofPMP. <br />2. Use a storm based analysis approach, incorporating the concepts of storm <br />maximization, storm transposition, elevation and barrier moisture adjustments, <br />and temporal and spatial envelopment. Emphasis is placed on using only storms <br />that can be transpositioned over the northern slopes of the Palmer Divide. This <br />constraint also applies to the use of methods, procedures and techniques that are <br />consistent with storm characteristics of transpositionable storms, Implicit storm <br />transpositioning is not used. Methods and techniques that attempt to address <br />orographic effects in PMP analyses must be valid for storms that can occur over <br />the Cherry Creek basin. When validated methods are not available, conservative <br />assumptions are used. <br />3. Computer based Geographic Information System (GIS) technologies are <br />incorporated to support accepted analysis methods and procedures. Emphasis is <br />placed on incorporating as much objectivity as possible, following procedures as <br />explicitly as possible and producing reproducible results. <br /> <br />) <br />} <br />The A W A team recognizes that the procedures used in the determination of PMP <br />values for the Cherry Creek drainage basin must I) be physically possible and 2) replicate <br />storm characteristics consistent with extreme storms that can occur over the northern <br />slopes of the Palmer Divide. All assumptions made during the analysis need to be <br />physically consistent with each other and with the atmospherics physics of an extreme <br />rainfall storm environment over the Cherry Creek basin. The assumptions used in this <br />study are presented in the following sections, <br /> <br />7 <br />