My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FLOOD07910
CWCB
>
Floodplain Documents
>
Backfile
>
7001-8000
>
FLOOD07910
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/25/2010 7:13:08 PM
Creation date
10/5/2006 3:18:04 AM
Metadata
Fields
Template:
Floodplain Documents
Designation Number
314
County
Broomfield
Community
Broomfield
Basin
South Platte
Title
Flood Insurance Study - Broomfield, Colorado, Adams, Boulder and Jefferson Counties
Date
8/1/1988
Designation Date
3/1/1991
Floodplain - Doc Type
Historic FEMA Regulatory Floodplain Information
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
72
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 />. <br /> <br />. <br /> <br />3.0 <br /> <br />. <br /> <br />. <br /> <br />Nissen Channel flows southeasterly through central <br />Broomfield and is narrow and relatively shallow. The <br />average slope is 56.9 feet per mile. For approximately <br />1,400 feet, the stream flows down East 7th Avenue between <br />Ash and Birch Streets. Runoff from West Lake and Gay <br />Reservoir basins, located in northeastern Broomfield, flows <br />through shallow, poorly defined channels that have average <br />slopes of 68,3 feet per mile. <br /> <br />Flooding in Broomfield is generally caused by heavy local <br />rainstorms. Flooding occurred in various parts of the city <br />in June 1965, July 1965, and May 1973. Scenes of the <br />May 1973 flood are shown in Figures 2 through 8. <br /> <br />2.4 <br /> <br />Flood Protection Measures <br /> <br />The City has purchased various parcels to be developed into <br />parks. In 1975, zoning ordinances were passed to prohibit <br />construction of structures within the floodplains and to <br />prevent flood damage. <br /> <br />Other flood protection measures include the construction of <br />a levee and channel improvements along Gay Reservoir <br />Channel. <br /> <br />ENGINEERING METHODS <br /> <br />For the flooding sources studied by detailed methods in the <br />community, standard hydrologic and hydraulic study methods were <br />used to determine the flood hazard data required for this study. <br />Flood events of a magnitude which are expected to be equaled or <br />exceeded once on the average during any 10-, 50-, 100-, or 500- <br />year period (recurrence interval) have been selected as having <br />special significance for flood- plain management and for flood <br />insurance rates. These events, commonly termed the 10-, 50-, <br />100-, and 500-year floods, have a 10-, 2-, 1-, and 0.2-percent <br />chance, respectively, of being equaled or exceeded during any <br />year. Although the recurrence interval represents the long-term <br />average period between floods of a specific magnitude, rare floods <br />could occur at short intervals or even within the same year, The <br />risk of experiencing a rare flood increases when periods greater <br />than 1 year are considered. For example, the risk of having a <br />flood which equals or exceeds the 100-year flood (1 percent chance <br />of annual exceedence) in any 50-year period is approximately 40 <br />percent (4 in 10), and, for any 90-year period, the risk increases <br />to approximately 60 percent (6 in 10). The analyses reported <br />herein reflect flooding potentials based on conditions existing in <br />the community at the time of completion of this study. Maps and <br />flood elevations will be amended periodically to ~eflect future <br />changes. <br /> <br />5 <br />
The URL can be used to link to this page
Your browser does not support the video tag.