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Last modified
7/14/2009 5:02:32 PM
Creation date
5/20/2009 11:01:52 AM
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UCREFRP
UCREFRP Catalog Number
8065
Author
Vaill, J. E.
Title
Computation of Selected Hydraulic Variables for the Lower Yampa River in Northwestern Colorado.
USFW Year
1997.
USFW - Doc Type
Denver, Colorado.
Copyright Material
NO
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<br />105 <br /> <br />::iii <br />::> <br />I- <br />C!i1oo <br />>- <br />a: <br />< <br />a: <br />~ 95 <br />a: <br />< <br />w <br />> <br />g 90 <br />< <br />I- <br />W <br />W <br />U. <br />~ 85 <br />Z <br />o <br />i= <br />~80 <br />w <br />...J <br />W <br /> <br />7~20 <br /> <br />CROSS SECTION 6 <br /> <br /> <br />-10 <br /> <br />10 <br /> <br />30 <br /> <br />o <br /> <br />20 <br /> <br />CROSS SECTION 7 <br />102 <br /> <br />20 30 40 50 60 <br />STATIONING, IN FEET FROM LEFT BANK <br /> <br />Figure 5. Cross-section geometry for the downstream cross sections in Cross Mountain Canyon. <br /> <br />::iii <br />::>100 <br />!;( <br />C <br />~ 98 <br />~ <br />~ 96 <br />a: <br />< <br />~94 <br />o <br />In <br />~ 92 <br />w <br />w <br />u. <br />~90 <br />Z <br />Qee <br />!;( <br />> <br />~86 <br />w <br /> <br /> <br />~20 <br /> <br />o <br /> <br />10 <br /> <br />-10 <br /> <br />The WSPRO computations were performed for <br />cross sections in the three stream reaches (the Patrick <br />Sweeney diversion structure, the Maybell Canal <br />diversion structure, and the two subreaches in Cross <br />Mountain Canyon) assuming streamflows ranging <br />from 50 to 400 ft3/s. This range of streamflows was <br />chosen for analysis based on the assumption by State <br />and Federal biologists (Modde and Smith, 1995) and <br />CRWCD personnel that streamflows less than 50 ft3/s <br />would always present adverse conditions to squawfish <br /> <br />40 <br /> <br />50 <br /> <br />60 <br /> <br />70 <br /> <br />80 <br /> <br />90 <br /> <br />100 <br /> <br /> <br />90 <br /> <br />100 <br /> <br />70 <br /> <br />80 <br /> <br />migration and that streamflows greater than <br />400 ft3/s would always present favorable conditions. <br />Five percent of the streamflow being analyzed was <br />assigned to a stream tube based on equal conveyance <br />in accordance with the assumption of one-dimensional <br />flow. Stream tubes are imaginary tubes bounded by <br />streamlines. Because the streamflow between stream- <br />lines is constant, each stream tube carries a constant <br />streamflow along its length. The WSPRO output <br />data listed in the appendixes of this report include <br /> <br />MODEL DESCRIPTION AND APPLICATION 7 <br />
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