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Following impoundment, NHWZ vegetation cover increased by nearly 400% in GIS reach 5, <br />despite a significant, flood-related decrease in vegetation cover in the early 1980s. This result <br />indicates how productive riparian habitats can be in the absence of frequent flooding. <br />The OHWZ in GIS reach 5 appears to exhibit a trend of increased vegetation cover in 1984, <br />which may relate to the flood conditions that occurred during the early 1980s. High flows may <br />have supplied mesquites with much-needed water for growth. Analysis of OHWZ patterns <br />within the five other GIS reaches will help to determine if this trend is a larger-scale pattern <br />of response throughout Grand Canyon. <br />One of the environmental variables, depositional environment, may also influence vegetation <br />cover along the Colorado River. Consistently less NHWZ vegetation cover was present in the <br />mile below the Little Colorado River than in the mile above this tributary between 1965 and <br />1984; however, this pattern is reversed by 1992. Although vegetation cover increases both above <br />and below this tributary from pre-dam times to the present, these data suggest that the rate <br />of increase is greater below the Little Colorado River. A substantial influx of sediments from <br />the Little Colorado River may be providing additional colonizable substrate for vegetation in this <br />otherwise sediment-limited river system. We will measure vegetation patterns upstream and <br />downstream from other tributaries, including the Paria River, Nankoweap Creek, and Tepeats <br />Creek, to determine the extent of this preliminary finding. <br />This research will also relate to the demography of one riparian species, Goodding willow, which <br />may be negatively affected by river regulation, over the last 30 years. Currently, little evidence <br />of recruitment in this species exists within Grand Canyon; most individuals are mature or <br />decadent. Large populations have become established recently at the end of Grand Canyon on <br />Lake Mead and represent an enormous recruitment event for Goodding willow. We will <br />establish the timing and basis of this event'in the course of determining the age distribution of <br />this species' populations through the canyon. Goodding willow's range is restricted to the <br />southwestern United States. The Goodding willow - Fremont cottonwood association in Arizona <br />is listed as threatened by the Nature Conservancy. <br />A thorough analysis of riparian vegetation responses to river regulation will be provided by this <br />study. As a result of this work, nearly 30 years of data on georeferenced vegetation cover will <br />be available for 50% of all GCES/GIS reaches. This study will provide valuable insights into the <br />impact of river regulation on riparian vegetation, will produce a permanent, quantitative record <br />that can be included in all fixture research and monitoring efforts involving riparian vegetation <br />along the Colorado River, and will serve as a comparison for other river systems. <br />The fourth and final study to be included in this report was contributed by the U.S. Geological <br />Survey and discusses how they are using existing GCES/GIS topographic and newly created <br />bathymetric data to generate flow, sediment-transport, and bed-evolution models to predict <br />sand accumulation or losses. <br />28