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Last modified
7/14/2009 5:02:36 PM
Creation date
5/22/2009 5:27:49 PM
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UCREFRP
UCREFRP Catalog Number
9532
Author
Anderson, R. and G. Stewart.
Title
Riverine Fish Flow Investigations.
USFW Year
2000.
USFW - Doc Type
Fort Collins.
Copyright Material
NO
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<br />bottom is on private property and is used for grazing or hay fields. In 1999 the river channel <br /> <br />was mapped from RM 63.1 to RM 62.5 for a total of 1.0-km. A 2.7-km reach was electro- <br /> <br />fished in 1999, from RM 63.9 to 62.2. In 1998 the surveyed site was less (0.8 km), but a <br /> <br />larger section of the river (6.1-km) was electro-fished last year, from RM 66.0 to 62.2. <br /> <br />The Duffy site is centered near River Mile 109.5, in the lower part of Little Yampa <br /> <br />Canyon (Figure 1). Little Yampa Canyon extends from about RM 105 to RM 121. Here one <br /> <br />side of the river is usually on a canyon wall and the BLM is the primary landowner. In some <br /> <br />sections large boulders provide instream cover in pool and run habitats. A 2.2-km section of <br /> <br />river channel was mapped in 1999, from RM 110.25 to 108.9. The electrofishing station <br /> <br />shifted upstream about 0.5 mile in 1999 compared to last year, and was from RM 110.5 to RM <br /> <br />105.5 (8.0 km). It was from RM 109.9 to RM 104.8 (8.1 km) in 1998. This upstream shift <br /> <br />was due to the fact that the size of channel surveyed was enlarged both up' and downstream. <br />"\ <br /> <br />Flows at Sevens (RM 63) were based on the Maybell gage located at RM 85.8. The Maybell <br /> <br />gage has been in continuous operation since May 1, 1916. During the irrigation season, flows <br /> <br />recorded at Sevens may be somewhat higher, due to return flows from lands irrigated by the <br /> <br />Maybell Canal diverted at RM 89. Flows at Duffy (RM 109) were determined by combining <br /> <br />records from the Craig gage (RM 140) with the gage at the confluence of the Williams Fork <br /> <br />(RM 127). <br /> <br />Peak flow for 1998 was 10,040 cfs and it was 9,980 cfs for 1999, which rank 44th and <br /> <br /> <br />39th, respectively for the Maybell gage 84-year period of record. The median peak flow for <br /> <br />v~ the, 84 -year period is 10,000 cfs. Prior to 1999 there were four consecutive yearswit1fpeakslEl..~" <br /> <br />above the median, indicating the hydrograph in recent years has been in a wetter than normal <br /> <br />cycle and the last two years are medial (Figure 2). In contrastto the peak flows, base flows <br /> <br />4 <br />
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