My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FLOOD04822
CWCB
>
Floodplain Documents
>
Backfile
>
4001-5000
>
FLOOD04822
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/25/2010 6:47:23 PM
Creation date
10/5/2006 1:04:17 AM
Metadata
Fields
Template:
Floodplain Documents
County
El Paso
Community
Colorado Springs
Stream Name
Plum Creek, Mason Reservoir
Basin
Arkansas
Title
Site-Specific Probable Maximum Precipitation for Mason Reservoir
Date
1/1/1997
Prepared For
Black and Veatch
Prepared By
Henz Meteorological Services
Floodplain - Doc Type
Floodplain Report/Masterplan
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
80
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
Show annotations
View images
View plain text
<br />1.0 Introduction <br /> <br />Henz Meteorological Services (HMS) was retained by Black & Veatch (BV) to <br />prepare a review of existing Mason Rese/voir Probable Maximum Precipitation <br />(PMP) studies, evaluate the validity of the existing Hydrometeorological Report <br />(HMR)-based PMP assumptions as they apply to Mason Reservoir and prepare <br />a site-specific PMP for the Mason Reservoir drainage basin, Special <br />considerations were made for the unique location of Mason Reservoir which is <br />influenced both by the rolling High Plains to the east and by the surrounding <br />topography of the Rocky Mountains to the south through north. <br /> <br />Mason Reservoir is located at an elevation of 11,600 feet immediately south and <br />east of the base of Pikes Peak which towers just west of Colorado Springs, <br />Colorado and is presented in Figure 1. Its drainage basin elevations range from <br />11,100 feet to 13,500 feet and its area is less than 10 square miles in size, It is <br />located in a high alpine area which consists of mostly rock outcroppings above <br />12,500 feet and a combination of bristle cone pine, spruce, Douglas fir, aspen <br />and pines in alpine meadows at lower elevations, <br /> <br />The task of determining the site-specific F'IVIP for Mason Reservoir consisted of <br />four steps which were split into two phases: <br /> <br />Phase I: <br /> <br />1. HMS evaluated the BV local storm and geneml storm PMP calculations <br />for Mason Reservoir and the HMR 55A assumptions used to calc:ulate <br />them. HMS evaluated the use of these historically accepted <br />methodologies and identified opportunities tel combine them with new <br />technologies and methodologies (i.E~., the HMS Convective Storm <br />Methodology) in a manner which allowed continuity with previollls <br />accepted studies while providing incremental improvements where <br />enhanced data sets and new technolclgical adlvances allowed. <br /> <br />Phase I of this study, a preliminary site-speGific PMP evaluation, was begun in <br />February 1995. During this Phase HMS evaluated the prior BV site-specific PMP <br />calculations which had been completed for the Mason Reservoir basin, An <br />internal memorandum was issued in April, 1995 which summarized the results of <br />meteorological and analytical evaluations of the standard HMR 55A <br />methodologies which are used to prepare site-specific PMP's relative to both <br />enhanced data sets and new technologies and the high elevation of Mason <br />Reservoir, The conclusion of Phase I recommended that an enhanced site- <br />specific PMP which makes use of these new data sets and methodologies <br />should be undertaken. <br />
The URL can be used to link to this page
Your browser does not support the video tag.