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7/14/2009 5:02:37 PM
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5/20/2009 3:21:58 PM
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UCREFRP
UCREFRP Catalog Number
9617
Author
Scott, M. L., M. A. Wondzell and G. T. Auble
Title
Hydrograph Characteristics Relevant to the Establishment and Growth of Western Riparian Vegetation
USFW Year
1993
USFW - Doc Type
Hydrology Days Publications
Copyright Material
NO
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<br />INTRODUCTION <br /> <br />Riparian zones or bottomlands are water courses and <br />associated areas of alluvial sediments. In arid and <br />semi-arid regions of North America, riparian <br />woodlands bordering streams and rivers are <br />distinctive features representing topographic <br />positions that are consistently moist enough to <br />support the growth of trees in a .landscape that is <br />otherwise too dry. Riparian zones represent important <br />transitional areas between upland and aquatic <br />ecosystems (Gregory et ale 19~1) and provide <br />essential habitat for a wide diversity of vertebrate <br />species (Brinson et ale 1981, Knopf 1985). <br /> <br />Western riparian ecosystems, particularly at lower <br />elevations, are often dominated by~species of po~lar <br />and willow. These early successional speC1es, <br />including plains cottonwood (Populus deltoides subsp. <br />monilifera (Aiton) Eckenwalder) 'are adapted to <br />relatively frequent, intense disturbances produced by <br />the energy of flowing water in riparian environments <br />(Osterkamp and Costa 1987). streamflow in most large <br />western rivers and streams is now influenced br <br />management activities including agricultura <br />diversion and damming for power generation and flood <br />control. Such activities have; caused dramatic <br />changes in the diversity, structure~ and organization <br />of riparian vegetation throughout western North <br />America. Changes in the magnitu~e and timing of <br />flows have led to marked declineslin the extent of <br />riparian vegetation in some river systems (Johnson et <br />ale 1976, Fenner et ale 1984, Rood.and Mahoney 1990). <br />However, in situations where natural flow <br />fluctuations historically prevented establishment of <br />vegetation, the moderating e.ffects of water <br />development have led to at least tem~orary increases <br />in the extent of riparian vegetat10n (Nadler and <br />Schumm 1981, Williams and Wolman 1984). <br /> <br />Ha,nagement of riparian resources within a larger <br />framework of water management will require clear <br />articulation of flow characteristics relevant to <br />riparian vegetation. In this paper we discuss stream <br />hydrograph characteristics critical to conditions <br />required for establishment, growth, and survival of <br />native riparian vegetation. <br /> <br />ECOLOGICAL REQUIREMENTS <br /> <br />The capacity of moving water to erode, transport, and <br />deposit alluvial materials is central to the <br />structuring and maintenance of western riparian <br />ecosystems (Brinson et ale 1981). Early successional <br />species, like many riparian willows and poplars, <br />possess a number of ecological characteristics that <br />make them particularly well-suited to physical <br />conditions in riparian zones. We discuss the <br />ecological requirements for germination, <br />establishment, growth, and long-term survival of <br />riparian vegetation, using plains cottonwood as an <br />example. <br /> <br />238 <br />
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