My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FLOOD10141
CWCB
>
Floodplain Documents
>
Backfile
>
9001-10000
>
FLOOD10141
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/26/2010 10:12:05 AM
Creation date
10/5/2006 4:55:40 AM
Metadata
Fields
Template:
Floodplain Documents
County
Statewide
Community
Nationwide
Basin
Statewide
Title
Guidelines for Determining Flood Flow Frequency Bulletin 17A
Date
3/1/1977
Prepared By
USWRC
Floodplain - Doc Type
Educational/Technical/Reference Information
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
172
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 />Floods developed from precipitation estimates can be used to adjust <br />frequency curves, including extrapolation beyond experienced values. <br />Because of the many variables, no specific procedure is recommended at <br />this time. Analysts making use of such procedures should first standardize <br />methods for computing the flood to be used and then evaluate its probability <br />of occurrence based upon flood and storm experience in a hydrologically <br />and lreteorologically lx:rrogeneous region. Plotting of the flocxl. at the <br />exceedance probability thus determined provides a guide for adjusting <br />and extrapolating the frequency curve. Any adjustments must recognize <br />the relative accuracy of the flood estimate and the other flood data. <br /> <br />VI. Reliability Application <br /> <br />The preceding sections have presented recommended procedures for <br />determination of the flood frequency curve at a gaged location. When <br />applying these curves to the solution of water resource problems, there <br />are certain additional considerations which must be kept in mind. These <br />are discussed in this section. <br />It is useful to make a distinction in hydrology between the concepts <br />of risk and uncertainty (18). <br />Risk is a permanent population property of any random phenomenon <br />such as floods. If the population distribution were known for floods, <br />then the risk would be exactly known. The risk is stated as the probability <br />that a specified flood magnitude will be exceeQed in a specified period <br />of years. Risk is inherent in the phenomenon itself and cannot be <br />avoided. <br />Because use is made of data which are deficient, or biased, and <br />because population properties must be estimated from these data by some <br />technique, various errors and information losses are introduced into the <br />flood frequency determination. Differences between the population <br />properties and estimates of these properties derived from sample data <br />constitute uncertainties. Risk can be decreased or minimized by various <br />water resources developments and measures, while uncertainties can be <br />decreased only by obtaining more or better data and by using better <br />statistical techniques. <br /> <br />20 <br />
The URL can be used to link to this page
Your browser does not support the video tag.