|
<br />largest stream in the region, has been transformed from a free-flowing, dynamic
<br />waterway to a string of storage pools. Its stream flow has been greatly reduced and
<br />only rarely reaches the Colorado River delta. Multiple impoundments also disrupt
<br />patterns of water and sediment flow on major and minor tributaries of the,Colo~do
<br />River (Graf, 1999). Diversion structures, including Granite Reef Dam on the Salt River,
<br />and New Waddell Dam on Arizona's Agua Fria River, completely reroute stream flow
<br />into canals, leaving dry river beds below (Graf, 1982; Springer et al., 1999). Other
<br />streams, such as the Santa Cruz in Arizona, have been. dewatered as a result
<br />of ground-water pumping. l:iround-water mining, stream flow diversion, and damming
<br />in combination have caused ground-water tables along a portion of the Gila River
<br />to plummet by 200 m in the last century Qudd et al., 1971). Concentrations of
<br />dissolved solids (salinity levels) have increased in many streams, a result of high rates
<br />of evaporation from expansive, shallow impoundments, and run-off from agricul-
<br />tural fields. Vast areas of flood plains have been converted to agricultural fields and
<br />urban settlements, necessitating construction of dikes and levees to constrain flood ~
<br />,
<br />waters. ~
<br />These physical changes have led to biological losses and various types of biological ~
<br />change (Rood & Mahoney, 1990; Patten, 1998; Johnson, 1.998). Al~ng ~ome. reaches in i
<br />which floods have been suppressed but stream flows not diverted, npanan biomass has I Success rates for effecting desired ecosystem changes vary widely. Our ability to
<br />increas. ed. For example, riparian vegetation has increased significantl. y along the Bill I' restore riparian ecosystems sometimes falls short of our desire, despite some assertions
<br />Williams River, a small tributary to the Colorado, since closure of Alamo Dam in 1968. . to the contrary (Hey & Phillipi, 1999). Sometimes, efforts fail because of an
<br />Most of the new vegetation, however, is composed of the exotic woody plant Tamarix' inability to implement or sustain necessary changes. In other cases, the. failure lies with
<br />ramosissima and the dense riparian forests have become fire-prone (Busch, 1995; ~ inadequate scientific recommendations. Too often, restoration efforts fail because
<br />Shafroth, 1999). Along the Colorado River, narrow strips of marshland and riparian i the underlying factors that caused the riparian degradation are not addressed (Briggs,
<br />forest have developed in areas of the narrow Glen Marble and Grand Canyon reaches ~ 1996; Briggs et al., 1994; Hobbs & Norton, 1996; Alpert et al., 1999). For example,
<br />that formerly were scoured by annual floods (Stevens et al., 1994). Along much of the l a decade ago in the south-western United States, riparian restoration was synonymous
<br />lower Colorado River and major tributaries, however, riparian vegetation has declined I with cottonwood pole planting. Many of these planting efforts failed, because
<br />and the vegetation mosaic in the flood plain has simplified. Much of the lower Colorado j no-one asked, 'What factors caused the loss of the cottonwoods?'. Today, removal of
<br />River flood plain is now vegetated by Tamarix ramosissima and Pluchea sericea (Ohmart 1 exotic plant species seemingly has become a restoration panacea, but again, few are
<br />et al., 1988). Both are reproductively opportunistic; stress-tolerant shrubs, that can ; asking 'What factors have allowed for establishment of the exotics?'. Additions or
<br />withstand saline soils, drought, and repeated burning. Near the delta of the Colora.do ) removals of plants can sometimes suffice as the sole restoration effort. More
<br />River, the cumulative effects of river use have nearly obliterated the most extensIve" frequently, though, th,ere is a need to 'dig deeper' to identify and reverse the root causes
<br />wetlands in the south-western United States and northern Mexico, leaving only a few j of ecosystem degradation (Wissmar & Beschta, 1998). Because we do not yet have all
<br />scattered ecological remnants amidst an expanse of dry, salty, unvegetated land (Glenn ~ the answers, restoration projects should be designed as science-based experiments or at
<br />et al., 1992, 1996; Briggs & Cornelius, 1998). i least integrate some degree of experimentation. Adaptive research and management
<br />Generally, in arid regions, riparian species diversity is lower along stre~s that ~o n?tl policies should be integral to the process. .
<br />flow perennially (fabacchi et a/., 1996). As streams are dewatered, spec~es decline In, Primary root causes of riparian loss and degradation are alteration of herbIVOry
<br />number because the wetland to upland species continuum is truncated: obligate wetland .; regimes, disruption of hydrologic regimes, and direct conversion to irrigated cropland
<br />species that depend upon shallow water tables or perennial stream flows decline, while! and urban areas. Restoration measures to reverse impacts of livestock grazing generally
<br />upland species that grow on drier portions of the flood plain may be unaffected orj require exclusion of the grazing animals or large declines in their stocking rates in
<br />expand into areas once occupied by riparian obligates (Stromberg et al., 1996). Lo~er~d; riparian zones as well as upland sites throughout the watershed (Williams et al., 19~7).
<br />ground water levels have killed phreatophytic riparian plants alon~ the. Ca~el Ri~er In ,\ Active intervention may be required to reverse l~ng-term effec~ of ~)Ver~mg,
<br />California, Coal Creek in Colorado, and the Santa Cruz and Gila Rivers In Arizona, ~ such as compacted soils and lowered water-tables. With respect to direct dlsrupno.ns of
<br />among others (Bryan, 1928; Rea, 1983; Groene~eld & ~riepeI?trog, 198?; Scott ~t a.l.,I. hydrologic regimes, there is growing recognition that res~oring na~ fl~w ~epmes,
<br />1999). Fremont cottonwood (Populus fremonui)-Godding willow (SallX. gooddln~t) ; including natural patterns of flood disturbance and flUVIal dynarmsm, .IS CDtI;cal to
<br />forest associations, dependent on ample amounts of fresh water and speCific flooding .l restoration success (Briggs, 1996; Middleton, 1999; Graf et al., 2001)'. ProJects With the
<br />patterns, have become globally imperiled (Fenner et al.) 1985; Busch & Smith, 1995)..: greatest chance for sustainable improvement encompass an 'ecosystem managem~nt
<br />Riverine marshlands have become rare (Hendrickson & Minckley, 1984): .~ Ilgenda' of restoring ecological processes, as a basis for restoring ecosystem co~pleXlty
<br />Declines in species diversity also can occur if flood disturbance becomes Infrequent or .~ (Whisenant, 1999). Active restoration techniques such as planting trees or shapmg land
<br />if the temporal and spatial diversity of flood disturbance declines (pollock et al., 1998). ~ forms sometimes are used to jumpstart the recovery but the ultimate goal is to allow
<br />Flood suppression may be a key reason why plant diversity is low in the dense thickets of t, process restoration to naturally drive ecosystem recovery (Kauffman et ai., 1997).
<br />Tamarix that develop on flow-regulated streams (Brock, 1994). Although theseJ One such ecosystem management effort is underway in California. Los Angel~s
<br />declines have been attributed to changes produced by Tamarix, the ultimate cause may;, Department of Water and Power, in conjunction with Mono County, is involved In
<br />be river damming and flood suppression. Plant biodiversity levels can be equally high in! II multi-year effort to restore the Owens River gorge. Restoration of flood pulses and
<br />
<br />18
<br />
<br />J. C. STROMBERG
<br />
<br />RESTORATION Of RIPARIAN VEGETATION OF FLOW REGIME
<br />
<br />19
<br />
<br />understories of the patchy forests of Populus and Tamarix that occur along free-flowing
<br />streams (Stromberg, 1998a).
<br />The combined effects of physical and vegetational changes in riparian habitats
<br />has endangered many riparian-dependent animal species, including south-western wil-
<br />low flycatcher (Empidonax traillii extimus), Yuma clapper rail (Rallus longirostris
<br />yumanensis), and least Bell's vireo (Vireo bellii pusillus). Large percentages of native fish
<br />species have become endangered or extinct (Minckley & Deacon, 1991; Richteret al.,
<br />1997 a). Restoration of habitat for endangered speci~s has been one, impetus Jor restora-
<br />tion projects in the south-western U.S.A. (Kus, 1998). Other restoration goals expressed
<br />by managers of Nature Conservancy preserves, National Wildlife Refuges, flood control
<br />districts, and other sites, include increasing the abundance of rare native riparian
<br />vegetation types, shifting dominance from exotic plant communities to native, improv-
<br />ing wildlife habitat and recreational amenities, and reducing the size of flood peaks that
<br />have increased due to activities such as road construction and urbanization.
<br />
<br />C;)
<br />C?
<br />W
<br />I-~
<br />""
<br /><:::::>
<br />
<br />Approaches to riparian ecosystem recovery
<br />
|