My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FLOOD08201
CWCB
>
Floodplain Documents
>
Backfile
>
7001-8000
>
FLOOD08201
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/25/2010 7:13:55 PM
Creation date
10/5/2006 3:27:47 AM
Metadata
Fields
Template:
Floodplain Documents
County
Statewide
Community
State of Colorado
Basin
Statewide
Title
The NWS Dambrk Model Quick Users Guide
Date
6/20/1988
Prepared By
National Weather Service
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.
/
33
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 />Appendix A-12 <br /> <br />Note: <br /> <br />(33) <br /> <br />*(34) <br /> <br />*(35) <br /> <br />*(36) <br /> <br />Card (33) is omitted if KFLP <br /> <br />0, (card (2)). <br /> <br />[ <br /> <br />SNC(K,I) - 8 F 10.0 Format <br /> <br />I <br /> <br />SNC(I) <br /> <br />Sinuosity coefficient (channel flow-path length/ <br />floodplain flow-path length) corresponding to each <br />elevation HS (K,I) for each of the (NS-l) <br />reaches. If left blank, SNC (K,I) is assumed to be <br />1.0; however, it cannot be omitted if KFLP=l. <br /> <br />I <br /> <br />I <br /> <br />DXM(I) - 8 F 10.0 Format <br /> <br />I <br /> <br />DXM(I) <br /> <br />Minimum bx distance (mi) between cross sections used <br />in the computations. If DXM(I) is less than the <br />distance between two adjacent cross sections among <br />the NS cross sections read-in, then intermediate <br />cross sections are created within the program via a <br />linear interpolation procedure. (NS-l) values of <br />D~(I) are entered on one or more cards (8 values <br />to a card); maximum no. of DXM(I) values is limited <br />to 89; val'~es assigned to DXM(I) sho'lid not res'lIt <br />in more than 200 cross sections produced by the <br />interpolation procedure. (DXM values should be <br />determined by the relationship C times bt,where C <br />is the approximate speed of the flood wave.) If <br />left blank, program will try to automatically <br />determine the proper value. If a DXM value is <br />entered, program will use DXM but will print out a <br />suggested computed value for a later run. Some DXM <br />values may be specified while others are left <br />blank, in which case the blank values are computed <br />and used along with the specified values. <br /> <br />.-' <br /> <br />I <br /> <br />I <br /> <br />'- <br /> <br />I <br /> <br />I <br /> <br />FK:(I) - 8 F 10.0 Format <br /> <br />FKC ( I) <br /> <br />I <br /> <br />Expansion/contraction coefficient; contraction values <br />vary from 0,1 to 0.3, expansion values vary from <br />-0,1 to -1.0; if expansion/contraction effects are <br />negligible, enter 0.0 for FKC(I); (NS-l) values of <br />FKC(I) are entered on one or more cards (8 values <br />to a card); maxim'lID no. of FKC(I) values is limited <br />to 89. <br /> <br />I <br /> <br />I <br /> <br />QMAXD, QLL, DTHM, YDN, SOM, F1I, EPSY, TFI - 8 F 10.0 Format <br /> <br />QMAXD <br /> <br />Estimated maximum discharge (cfs) at downstream <br />extremity of channel/valley reach; can be read in <br />as 0.0 for initial run; subseq~ent runs can have a <br />value of Q~AXD as determined by the routing <br /> <br />I <br /> <br />I <br /> <br />r <br />
The URL can be used to link to this page
Your browser does not support the video tag.