My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FLOOD10338
CWCB
>
Floodplain Documents
>
DayForward
>
1
>
FLOOD10338
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/26/2010 10:13:04 AM
Creation date
10/19/2007 1:03:36 PM
Metadata
Fields
Template:
Floodplain Documents
County
Statewide
Basin
Statewide
Title
TR-20 Computer Program for Project Formulation Hydrology
Date
5/1/1983
Floodplain - Doc Type
Educational/Technical/Reference Information
Jump to thumbnail
< previous set
next set >
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
332
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 />TECHNICAL RELEASE 20 <br />COMPUTER PROGRAM FOR PROJECT FORMULATION <br /> <br />HYDROLOGY <br /> <br />CHAPTER 2. PROGRAM DESCRIPTION <br /> <br />This chapter provides an understanding of the TR-20 computer program <br />organization and features. Terminology-in general usage by engineers is <br />used without definition. Terminology and acronyms used solely for this <br />computer program are defined the first time they are used and in the <br />Glossary. <br /> <br />To use this program effectively, an understanding of the procedures <br />described in SCS National Engineering Handbook, Section 4 (hereafter <br />referred to as NEH-4) is suggested. <br /> <br />2.1 METHODOLOGY FOR HYDROLOGY AND HYDRAULICS <br /> <br />~ <br /> <br />Subwatershed Delineation <br />The watershed should be divided into as many subwatersheds as required <br />to define hydrologic and alternative structural effects. Hydrologic <br />effects are influenced by entrance of tributaries, watershed shape, <br />valley slope changes, homogeneity of the runoff curve number and existing <br />or proposed water impoundment structures. Each subwatershed is assumed <br />to be hydrologically homogeneous. See Chapter 6, NEH-4. <br /> <br />Rainfall Distribution <br />Either actual or synthetic cumulative rainfall distributions may be <br />used. Rain~fall distributions (mass time-depth data) must be represen- <br />tative of the watershed area under study. This could be individual <br />subwatersheds or the entire watershed. <br /> <br />. <br /> <br />Runoff Volume <br />A mass curve of runoff is developed for each subwatershed. The runoff <br />curve number (CN), rainfall volume and rainfall distribution are the <br />input variables needed to determine this mass curve. CN's are determined <br />by the user for each subwatershed based on soil, land use, and hydrologic <br />condition information, as described in Chapters 7, 8, and 9, NEH-4. <br />
The URL can be used to link to this page
Your browser does not support the video tag.