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A portion of Arizona's San Pedro River is managed as a National Riparian Conservation Area but is potentially affected by ground-water withdrawals beyond the conservation area borders. We applied an assessment model to the Conservation Area as a basis for monitoring long-term changes in riparian ecosystem condition resulting from changes in river water availability, and collected multi-year data on a subset of the most sensitive bioindicators. The assessment model is based on nine vegetation bioindicators that are sensitive to changes in surface water or ground water. Site index scores allow for placement into one of three condition classes, each reflecting particular ranges for site hydrology and vegetation structure. We collected the bioindicator data at 26 sites distributed among 14 reaches that had similar stream flow hydrology (spatial flow intermittency) and geomorphology (channel sinuosity, flood-plain width). Overall, 39% of the riparian corridor fell within condition class 3 (the wettest condition), 55% in condition class 2, and 6% in the driest condition class. Condition class 3 reaches have high cover of herbaceous wetland plants (e.g., Juncus and Schoenoplectus spp.) along the perennial stream channel and dense, multi-aged Populus-Salix woodlands in the flood plain, sustained by shallow ground water in the stream alluvium. In condition class 2, intermittent stream flows result in low cover of streamside wetland herbs, but Populus-Salix remain abundant in the flood plain. Perennial wetland plants are absent from condition class 1, reflecting highly intermittent stream flows; the flood plain is vegetated by Tamarixa small tree that tolerates the deep and fluctuating ground water levels that typify this reach type. Abundance of herbaceous wetland plants and growth rate of Salix gooddingii varied between years with different stream flow rates, indicating utility of these measures for tracking short-term responses to hydrologic change. Repeat measurement of all bioindicators will indicate long-term trends in hydro-vegetational condition.

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Riparian fire studies in the American Southwest have focused on flow-regulated rivers and typically show increase in introduced Tamarix, a species with high resprout capacity, and declines in Populus. Effects of fire, however, can vary with environmental setting. We examined riparian fire along the free-flowing Upper San Pedro River (Arizona) by making temporal comparisons supplemented by spatial contrasts between burned and unburned sites. Pre-fire, Populus fremontii and Salix gooddingii were dominant species, with Tamarix sparse in the understory. Species differed in mortality and resprout rates, producing post-fire vegetation change. Mortality was highest for Tamarix, intermediate for Salix, and lowest for Populus, and also varied among size classes. Resprout rate was low for Populus, high for Salix, and also high for the few surviving Tamarix. The net effect was changes in population size structure (relative shifts towards larger Populus but smaller individuals of other species) and forest composition (decreased abundance of Tamarix relative to Populus and Salix), and in spatial distribution of stems. Tamarix's low ability to survive fire resulted from competitive suppression by Populus and Salix, with their dominance a product of the site's flow regime. Results indicate that post-fire outcomes within the riparian Southwest are variable and context-dependent.

Land-use and land-cover change affect the biogeochemistry of stream ecosystems in numerous ways, both direct and indirect. Changes result from hydrologic modifications, including direct alterations of flow regimes and hydrologic flowpaths and indirect changes in hydrologic patterns via increased impervious cover in contributing areas of watersheds. Direct changes to channel morphology (i.e., reduced complexity) and to floodplains of streams and rivers also influence biogeochemistry, for example, by eliminating surface water-groundwater exchange. The nature of and strength of connections between the stream and its watershed may be altered by large-scale changes such as those brought about by urban and suburban development. Finally, in urban and agricultural areas, elevated nutrient loading is exacerbated by land-cover changes that increase the potential for erosion or overland flow, and decrease the opportunities for nutrient retention. Using comparative analysis based on published work, mined public data, and new research, we evaluate urbanization effects on stream ecosystems in the Sonoran Desert region of central Arizona. Five key characteristics of non-urban desert streams-nitrogen limitation, a flashy hydrologic regime that initiates succession, extensive groundwater-surface water interaction, episodic terrestrial-aquatic interactions, and high capacity for nutrient retentionare both dramatically altered and scarcely affected by urbanization. The similarities exhibited by aridland streams and their urban counterparts arise from large-scale constraints (e.g., episodic terrestrial-aquatic interaction is imposed by the climatic regime in both stream types), whereas the differences, like interrupted flowpath continuity in the urban landscape, likely result from the myriad direct modifications of streams and catchment land cover in cities.