My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FLOOD06898
CWCB
>
Floodplain Documents
>
Backfile
>
6001-7000
>
FLOOD06898
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/25/2010 7:10:16 PM
Creation date
10/5/2006 2:34:57 AM
Metadata
Fields
Template:
Floodplain Documents
County
Statewide
Basin
Statewide
Title
Managing Floodplain Development in Approximate Zone A Areas
Date
4/1/1995
Prepared By
FEMA
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.
/
152
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 />Guide Por Approximate Zone A Areas <br /> <br />Developing BPEs <br /> <br />I <br />, <br /> <br />I <br />r <br />I <br />t <br />l <br />I <br />, <br /> <br />Detailed Methods <br /> <br />I <br />I <br />~ <br />r <br />I <br /> <br />Three essential factors must be determined either by hand <br />calculations or by computer model to determine a BFE by' <br />detailed methods. These factors are: 1) floodplain geometry <br />(topography); 2) flood discharge and/or volume (hydrology); <br />and 3) flood height (hydraulics). <br /> <br />Topography involves the measurement of the geometry of a cross <br />section(s) of the floodplain, which includes horizontal and <br />vertical coordinates. The vertical coordinate, or elevation, <br />is related to a vertical datum, such as the National Geodetic <br />Vertical Datum of 1929 or North American Vertical Datum of <br />1988. The horizontal coordinate, or station, is measured from <br />a reference point along the cross section to establish actual <br />ground points. <br /> <br />Hydrology for the particular location along a stream involves <br />the determination of the peak rate of stream flow [usually <br />measured in cubic feet per second (cfs)] that will occur <br />during a flood (for purposes of determining the BFE, the 100- <br />year flood). When determining lake or pond elevations, a 100- <br />year flood hydrograph is required to determine the BFE. <br /> <br />Hydraulics involves the determination of the water-surface <br />elevation that will occur during a flood (for purposes of <br />determining the BFE, the 100-year flood), the selection of a <br />method to relate the flood discharge to a flood depth, and the <br />selection of Manning's roughness coefficients or "n" values. <br />These "n" values vary depending on the type of materials; <br />degree of irregularity; variation of shape, obstructions, and <br />vegetation; and degree of meandering related to the channel <br />and the floodplain of a stream. <br /> <br />The following sections discuss various methods for determining <br />the topography, hydrology, and hydraulics for a particular <br />location in order to determine a BFE. <br /> <br />TODoaraDhv <br /> <br />Existing Topographic Maps <br /> <br />Before initiating field surveys, determine if there is <br />existing detailed topographic mapping that can be used to <br />generate cross-section data. To adequately describe a <br />floodplain and for use with a hydraulic method to calculate a <br />BFE, topographic map scales and contour intervals must be the <br />same as, or more detailed than, those used to prepare the <br /> <br />V-ll <br />
The URL can be used to link to this page
Your browser does not support the video tag.