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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
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Water Supply Protection
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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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thus resulting in what appear to be relatively young stands. Second, we <br />assumed that as we subtracted 20-'years from the current age of each stand, it <br />remained in the same size class (and hydrologic condition) unless the new <br />stand age fell below the midpoint in the range in years between the current <br />size class and the next younger size class. Once past the mid -point between <br />two age classes, the stand was moved to the next lower age class. If a size <br />class was non - stocked, it was assumed that 20 -years earlier it was a <br />sawtimber stand and the pattern repeated. In this way, the current size <br />classes were projected back in time, at 20 -year intervals, to the year 1860. <br />We did not account for stand evolution or changes in specie composition <br />that might also have occurred over time. We also had to assume there was <br />compatibility between the field survey derived estimates of stand age for the <br />4 classes and the GIS based estimates of area in each size class. Finally, it <br />was assumed that the hydrologic model, WRENSS, could be used to <br />characterize the annual water yield for the forest conditions characterized at <br />20 -year increments from 1860 to 2000. <br />Any trends in the water yields simulated for the forest condition assumed to <br />exist at successive increments of time is assumed to reflect the effect of <br />forest cover changes on water yield. This phase of the analysis was <br />performed on all national forest forested land in the North Platte River <br />Basin. The estimate of total acres in each of the 4 size classes for the period <br />1860 to 2000 is presented in table 3. <br />At first glance, the projections in table 3 seem erratic. For example, we can <br />pretty well assume there were more than zero non - stocked acres in 1940 and <br />that some sawtimber stands were present in 1920; contradicting the numbers <br />presented in table 3. However, these discontinuities or discrepancies are a <br />result of working with age class means, size class means, perhaps with the <br />choice of a time increment, and with the assumption that one size class is <br />reduced to its preceding size class at the mid -point in years between the two <br />size classes. Discontinuity is a problem that occurs whenever discrete <br />values are used to describe continuous, and often non- linear functions. The <br />value of the information in table 3 is in the trends it expresses. Currently <br />(year 2000) over 50 percent of the forested area is occupied by relatively <br />young sawtimber stands that were quite young in 1860. <br />29 <br />
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