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<br />I <br />t <br /> <br />growth responses to streamflow. Growth <br />of cottonwoods in both reach types in- <br />creased in response to increased flow vol- <br />ume. although volume of flow explained <br />slightly more of the variance in annual <br />growth for trees in the effluent reach. The <br />instream flow models indicate that a great. <br />er volume of flow should be released to <br />maintain healthy cottonwoods in the efflu- <br />ent reach. These results suggest that stream <br />?iversion adversely affects riparian popu- <br />lations in effluent and influent reaches, but <br />to a lesser extent in effluent reaches. The <br />rate of groundwater discharge 10 lhe stream <br />in the influent reach has not been sufficient <br />to alleviate moisture stress and prevent <br />growth reduction during low-flow years. <br />However, further data are needed on this <br />topic, particularly because rales of ground- <br />water discharge at the study sites were not <br />measured, <br />Within the effluent reach. the black cot- <br />tonwood population showed a sharper <br />growth response to streamflow than did <br />the Fremont cottonwood. The young age <br />of the black cottonwoods in this reach (an <br />unavoidable consequence of the limited <br />availability of trees) may have contributed <br />to this response. Young cottonwoods at an- <br />other eastern Sierra Nevada stream, Rush <br />Creek. also had more annual growth vari- <br />ance explained by present-year streamflow <br />than by prior-year variables in com parison <br />to mature trees (Stromberg and Patten <br />1990). Growth in juvenile trees appears to <br />be buffered to a lesser degree by prior-vear <br />photosynthate allocation. and it appears to <br />be more responsive to present-year envi- <br />ronmental conditions. <br /> <br />000084 <br /> <br />Supplemented-flow Reach <br /> <br />Growth of trees in the supplemented- <br />now reach was influenced bv localized in- <br />dividualistic factors. This i~ indicated by <br />the low correlations between tree chro- <br />nologies within the reach and the lack of <br />significant instream models for the reach <br />(Fritts and Swetnam 1989). This contrasts <br />with the diverted reaches, where one site <br />factor, streamflow volume. had a primary <br />Influence on annual growth. Trees in the <br />supplemented-flow reach were not limited <br />by moisture, as expected given the high <br />volumes of water released into the stream. <br />Individualized factors that may influence <br />annual growth in the reach include vary- <br />ing levels of competition over time and <br />annual differences in the extent of soil sat- <br />uration and anaerobic conditions. The de- <br />cline in growth by some trees during very <br />wet years suggests that prolonged satura- <br />tion negatively affects growth and vigor of <br />some trees at the site. Other human im- <br />pacts at the site. perhaps including soil <br />compaction, as well as the old age of most <br />of the trees. also may contribute to the low <br />canopy vigor at the site. The question of <br />how closely the growth response of trees <br />in this hydrologically modified. flow-sup- <br />plemented reach compares to that of trees <br />in unregulated, free-flowing streams awaits <br />further study. <br /> <br />ACKNOWLEDGMENTS <br /> <br />We thank Southern California Edison, Incor- <br />porate~, for providing financial support and hy- <br />drologiC data. Thanks also go to three reviewers <br />for their constructive reviews of the m"nuscript. <br /> <br />REFERENCES <br /> <br />Cook, E. R., and G. C. Jacoby. 1983. Potomac River streamflow since ]730 as reconstructed <br />by tree rings. Journal of ClJmate and Applied Meteorology 22(10):1659-1672. <br />Fritts, H. C. 1976. Tree rmgs and climate. New York: Academic Press. <br />_, and T. W. Swetnam. 1989. Dendroecology: A tool for evaluating variations in past <br />and present forest environments. Advances in Ecological Research ]9:11]-144. <br />Gustard, A. 1984. The characterization of flow regimes for assessing the impact of water <br />resource management on river ecology. Pages 53-60 in A. Lillehammer and S. ]. Saltveit, <br />editors. Regulated rivers. New York: Columbia University Press. <br />Harris,.R. R. 1988.. Associations between .st~eam valley geomorphology and riparian vege- <br />tation as a baSIS for landscape analYSIS In the eastern Sierra Nevada, California, USA. <br />Environmt.'nlal Management 12(2):219-228. <br />_, c.~. F~x, and.R. Risser. 1987. Impacts of hydroelectric development on riparian <br />vegetation In the Sierra Nevada region, California, USA. Environmental Management 11(4): <br />519-527. <br /> <br />I~ 10 <br /> <br />January 1991 <br /> <br />Rivers. Volume 2, Number I <br /> <br />- <br /> <br />Hess,]. W.,andS <br />water sourCE <br />anton, CA. l <br />State Univel <br />Kondol!, G. M.. <br />assessing im <br />the eastern ~ <br />Kulik. B. 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