My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
Estimating Additional Water Yield from Changes in Management
CWCB
>
Water Supply Protection
>
DayForward
>
2001-3000
>
Estimating Additional Water Yield from Changes in Management
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/26/2010 4:41:08 PM
Creation date
7/22/2009 12:50:22 PM
Metadata
Fields
Template:
Water Supply Protection
File Number
8461.250
Description
Water Issues
State
CO
Basin
South Platte
Water Division
1
Date
5/12/2000
Author
Charles A. Troendle, James M. Nankervis
Title
Estimating Additional Water Yield from Changes in Management
Water Supply Pro - Doc Type
Report/Study
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
54
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 />Coon Creek. The calibration relationship, as well as pre- and post-harvest <br />seasonal flow values are presented in figure 8. Flow was significantly <br />increased as a result of timber harvest, but it should be noted seasonal <br />increases in flow only slightly exceeded the significance detection limit. <br />Genera ly, it has been assumed that 20-25 percent of the vegetation on a <br />fully forested small watersheds has to be harvested in order to generate a <br />detectable response at the streamgage. Approximately 24 percent of the <br />vegetation on the Coon Creek watershed was harvested and the increase is <br />slightly above the detection limit. In addition, in an attempt to harvest as <br />much of the area as possible, many of the clear cuts crossed interior ridges, <br />as they did on the Upper Basin at Deadhorse Creek, causing a certain degree <br />of wind scour. Snow pack accumulation in the openings was not increased <br />on Coon Creek (Troendle et al. 1998) and there may be actual decreases in <br />net accumulation on the watershed in wetter years as a result of exposure to <br />wind. (Troendle and Meiman (1984) observed that once slash or roughness, <br />filled with snow, retention efficiency in openings decreased). <br />28 <br />c <br />? <br />3 <br />? <br />p <br />0 <br />a <br />v <br />cn <br />x <br />a? <br />? <br />U <br />c <br />0 <br />0 <br />U <br />26 <br />24 <br />22 <br />20 <br />1$ <br />16 <br />14 <br />12 <br />10 <br />09, <br />/,? <br />i _-•?? <br />? <br />,••? <br />o ? ?'.?•.-?"i <br />i <br />? , <br />? ? -'"i ? ? • 0 1983-1990 + t + 1991-1992 <br />?"i ? o? 0 1993-1997 Fit for 1983-1990 <br />? -• Lower 95°/a CI for Mean --• Upper 95% CI for Mean <br />-- Lower 95% CI for 1 Pred -- Upper 95% CI for 1 Pred <br />6 8 10 12 14 16 18 20 22 24 26 28 <br />Upper East Fork Seasonal Flow (in) <br />Figire 8: Seasonal water.yield for Coon Creek watershed (harvested) plotted over that for the <br />Upper EastFork (control). Pre-harvest, harvest, and post-harvest data are ptesemed. <br />Understanding the dynamics of stream flow response to timber harvest is <br />critical to evaluating the opportunity to increase flow via timber harvest and <br />equally critical in assessing the effects of forest regrowth on historic flows. <br />16
The URL can be used to link to this page
Your browser does not support the video tag.