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Estimating Additional Water Yield From Changes in Management of National Forests in the North Platte Basin
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Estimating Additional Water Yield From Changes in Management of National Forests in the North Platte Basin
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3/29/2013 2:57:42 PM
Creation date
3/6/2013 10:50:04 AM
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Water Supply Protection
Description
An Independent Report Prepared for the Platte River EIS Office U.S. Department of the Interior Related to Platte River Endangered Species Partnership (aka Platte River Recovery Implementation Program or PRRIP),
State
CO
NE
WY
Basin
North Platte
Water Division
6
Date
5/12/2000
Author
Charles A. Troendle, Matcom Corporation & James M. Nankervis, Blue Mountain Consultants
Title
Estimating Additional Water Yield from Changes in Management of Ntional Forests in the North Platte Bains, Final Report
Water Supply Pro - Doc Type
Report/Study
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Fool Creek, the small (714 acre) experimental watershed on the Fraser <br />Experimental Forest, described earlier, represents one of the most definitive <br />data sets world -wide; documenting both the initial effect of timber harvest <br />on increasing water yield, and the more subtle reduction in the initial <br />increase in water yield that occurs as the vegetation recovers or re -grows <br />over time. Figure 9 represents a double -mass plot (Anderson 1955) of <br />cumulative flow from Fool Creek (the treated watershed) plotted over the <br />cumulative flow from East St. Louis Creek (the control watershed). The <br />data for the period 1943 -1955 (Point A to B on figure 9) represents the pre - <br />harvest, or calibration, period and as can be noted, the relationship is linear <br />(follows a very straight line), and a regression line has been fitted to the <br />calibration data and extended to point C (equality, or a 1:1 relationship, is <br />not required). In 1954 -1956, 40 percent of the watershed area was harvested <br />on Fool Creek and resulted in an average increase in flow of 40 percent. <br />The increase in flow from Fool Creek began immediately. This abrupt <br />change in the relationship between Fool Creek and East St. Louis Creek, as a <br />result of the increase in flow from Fool Creek, can be evidenced by the <br />change in the trajectory of the double -mass plot at point B. Flow increased <br />on Fool Creek (Y -axis) relative to that for East St. Louis Creek (X -axis) <br />causing the relationship to deflect upward. Since 1956, the clear cuts on the <br />Fool Creek watershed have gradually recovered naturally. By 1984, <br />approximately one -third of the original vegetation biomass had returned. By <br />1995, approximately one -half or more of the original increase in flow had <br />been lost as a result of regrowth. Regrowth can be documented by the <br />gradual, almost imperceptible, arc present in the double -mass plot between <br />points B and C (figure 9) as the flow returns to the relationship that existed <br />prior to harvest. Eventually, we would expect the double -mass plot to <br />parallel the regression (solid) line fitted to the pre - harvest data. If the <br />recovery- line "over compensates ", it would imply the younger, more <br />vigorous stand is using more water than the original stand. <br />The Fool Creek watershed experiment sets the standard in the snow zone for <br />hydrologic comparisons that document the effect of forest disturbance on <br />stream flow response both in terms of initial response and the recovery. <br />Data from highly controlled experimental watersheds, such as Fool Creek, <br />are usually more definitive in demonstrating response than are landscape <br />scale watersheds, normally monitored with less rigor and for largely <br />forecasting purposes. <br />1 <br />1 17 <br />
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