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ABSTRACT <br />The present study investigates changes in channel morphology and potential losses of <br />fish habitat in reaches of the Colorado River near Grand Junction, Colorado. We have <br />used aerial photographs, discharge records, and field studies to evaluate the significance <br />of historical changes in flow regime and the effects of more recent flow events. Our <br />analysis of aerial photographs indicates there have been measurable decreases in the <br />amount of backwater habitat, although this vanes with the specific time period. A <br />preliminary analysis of peak flow data from several gaging stations in the region <br />indicates that in the last 30 years there has been a 19% decrease in the average peak <br />discharge of the Colorado River in the study area. This coincides with the time when <br />most of the major reservoirs in the upper basin were constructed. Peak flows on <br />unregulated tributary streams have remained stationary over the last 60 years. Field <br />studies conducted in 1993 during a period of higher than average runoff reveal minor <br />changes in channel morphology. Results from flow modeling are consistent with this <br />observation: model results indicate that the peak flow in 1993 was just sufficient to cause <br />significant movement of cobble and gravel bed material. <br />INTRODUCTION <br />There are currently four species of fish in the upper Colorado River which are listed as <br />endangered. These fish are the bonytail chub, the humpback chub, the Colorado squawfish, and <br />the razorback sucker. The latter two species were once plentiful in the reaches of the Colorado <br />River near Grand Junction, Colorado. Several factors appear to have contributed to the decline of <br />these fish, including competition with non-native species, deterioration in water quality, and a loss <br />of habitat due to river channelization and flow regulation. The present study focuses on the issue <br />of habitat loss. Biologists have suggested that backwaters are an important habitat for these fish <br />(Tyus and Karp, 1989), and that these habitats have been lost over time because of changes in the <br />flow regime of the Colorado River (Osmundson and Kaeding, 1991; Kaeding and Osmundson, <br />1989). It is reasonable to assume that a reduction in peak flows will result in changes in channel <br />morphology (Andrews, 1986; Williams and Wolman, 1984; Schumm, 1969), and thus, the U.S. <br />Fish and Wildlife Service has recommended that more water be released from upstream reservoirs <br />to improve in-channel habitat and enhance the recovery of these fish (Osmundson and Kaeding, <br />1991). However, it is not clear exactly how high these flows should be or how long they should <br />last. The present study was undertaken to detem- ine the extent of historical changes in riverine <br />habitat and to improve our understanding of the processes of habitat formation.