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during the winter of 1996-1997 did not dismantle ice cover or promote formation of frazil ice <br />and ice jams. Whatever the cause, it is likely that ice jams form at several locations on the <br />middle Green River nursery area in most years. <br />As a result of stage changes, ice jams, and frazil ice formation, young fish redistribute to <br />more suitable habitats. Young Colorado pikeminnow prefer low-velocity backwater habitats, <br />and when these habitats are inundated, the fish abandon them and move to other low-velocity <br />habitats, sometimes to other backwaters several miles away and sometimes to low-velocity <br />micro-habitats within close proximity of the inundated backwater from which they re-inhabit <br />once the stage recedes. <br />When stage changes inundate nursery habitats and transform them into flow-through <br />environments, resident fish are flushed into the surrounding system and incur increased risk of <br />injury, predation, and metabolic costs associated with the search for another suitable nursery <br />area. Body weight and condition decline faster when fish activity is increased because energetic <br />reserves must be used to offset the cost of higher metabolic rate. The result may be higher <br />overwinter mortality. <br />A-xi