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<br />~each <br /> <br />1 the supplemented- <br />nced by localized, in- <br />This is indicated by <br />between tree chro- <br />reach and the lack of <br />models for the reach <br />1989). This contrasts <br />Lches, where one site <br />'lume. had a primary <br />growth. Trees in the <br />each were not limited <br />,cted given the high <br />,ased into the stream. <br />s that may influence <br />, reach include vary- <br />.ition over time and <br />the extent of soil sat- <br />o conditions. The de- <br />me trees during very <br />at prolonged satura- <br />, growth and vigor of <br />,. Other human im- <br />haps including soil <br />; the old age of most <br />:ontribute to the low <br />,ite. The question of <br />th response of trees <br />modified. flow-sup- <br />'ares to that of trees <br />)wing streams awaits <br /> <br />JGMENTS <br /> <br />lifornia Edison, Incor- <br />ancial support and hy- <br />, go to three reviewers <br />~ws of the manuscript. <br /> <br />o as reconstructed <br />'2. <br /> <br />variations in past <br />-144. <br />~ impact of water <br />and S. J. SaLtveit, <br /> <br />nd riparian vegc- <br />California, USA. <br /> <br />ment on riparian <br />l.1anagement 11(4): <br /> <br />January 1991 <br /> <br />~L)[)OS5 <br /> <br />Hess, J. W., and S. D. Smith. 1987. Isotopic analysis of Bishop Creek hydrology and vegetation <br />water sources. Pages 6-8 in D. Patten. editor. Sierran riparian confermce procudings. Pleas- <br />anton, CA.. Available from: Duncan Patten, Center for Environmental Studies, Arizona <br />State University. <br />Kondolf, G. M., J. W. Webb, M. J. Sale, and T. Felando. 1987. 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Wash- <br />ington, DC: U.S. Geological Sorvey (Professional Paper 1286). <br /> <br />Rt'cdl!eJ. 1~ Mall 1990 <br />Accepted: 15 Scpt('ntb~r 199U <br />Di:;Cll~siOlr VPl'lI Imtll 1 AlIgust /991 <br /> <br />II II~ <br /> <br />J. C. Stromberg and D. T. Patten <br />