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Last modified
7/14/2009 5:02:35 PM
Creation date
5/22/2009 4:46:38 PM
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Template:
UCREFRP
UCREFRP Catalog Number
9385
Author
Hawkins, J.
Title
Responses by Flaming Gorge Technical Integration Team to April 4, 2000, Minority Report from John Hawkins
USFW Year
2000.
USFW - Doc Type
Flow and Temperature Recommendations for Endangered Fishes in the Green River Downstream of Flaming Gorge Dam (hereafter the Flow Report.
Copyright Material
NO
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<br />In addition to mainstem dams, small off-channel flow depletion projects can <br />have cumulative impacts which may be superimposed on the mainstem response <br />to upstream reservoirs. Butler (1988a) indicated that both large water projects <br />and cumulative impacts of smaller projects in the upper basins have the potential <br />to alter the sediment supply to downstream river reaches through streamflow <br />regulation. <br /> <br />A number of reports discuss the potential impacts related to water resource <br />development in the Little Snake River, Yampa River and Green River basins. <br />Andrews (1978) projected an increase in sediment yield due to a potential increase <br />in coal surface mining but confined his analysis to the Yampa River basin. He <br />analyzed suspended sediment measurements collected at the Maybell and Lily <br />Gages as well as the sediment records for 16 other gages in the Yampa River <br />basin. Andrews concluded that the impact of increased sediment load will depend <br />on where in the basin it enters the river channel. <br /> <br />In 1980, Andrews published an important paper on effective and bankfull <br />discharge in the Yampa River basin which used his 1978 data base (Andrews <br />1978). This study addressed the concept of effective discharge and it's <br />significance to the river channels in the Yampa River basin. The premise of the <br />paper, as introduced by Wolman and Miller (1960), was that channel morphology <br />characteristics, particularly meander length and channel width, were formed by <br />relatively frequent flows and not by rare catastrophic events. Recurrence intervals <br />for the effective discharges ranged from 1.18 to 3.26 years for 15 selected gaging <br />stations. <br /> <br />Based on a Little Snake River cross section surveyed near Dixon, WY, <br />Andrews (1980) determined that the effective and bankfull discharges were in <br />close agreement and concluded that the stream channels were adjusted to the <br /> <br />31 <br />
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