Identifying the natural flow regime and the relationship with riparian vegetation for two contrasting western Australian rivers

The natural flow regime and the relationship between flows and riparian vegetation are described for sites on both the Blackwood River in south‐western Australia and the Ord River in north‐western Australia. Analysis of long‐term flow data showed the historic mean monthly river discharge for the Blackwood River is strongly seasonal and highly predictable with generally low variability each month. The Ord River showed a strong seasonality of flows with about 92% of the (total) yearly flow occurring between December and March. Flow variability was very high (e.g. coefficient of variation >100% for all months) but highly predictable, with this mostly attributed to low but constant dry‐season flows. Water depth, duration of flood events and the number of flood events per year show a significant correlation with aspects of the riparian vegetation within experimental vegetation plots. Results highlight the strong relationship between floristics, life form structure and population dynamics with stream hydrology. On the Blackwood River, species richness and cover of shrubs reduced with increased duration and frequency of flooding, while cover of exotic species and annual herbs increased with increased flooding. Germination of tree seedlings was not influenced by flood regime but size class of tree species increased with flooding frequency. On the Ord River, species richness was not influenced by flooding regime. However, cover of perennial grasses increased with flooding frequency whilst cover of shrubs decreased. There was no relationship between flooding and seedling establishment whilst tree size class decreased with increased flooding. The methods described here can be used to compare the response of different components of the riparian vegetation to different fluvial regimes (e.g. because of impoundment and abstraction). This technique can be expanded for the management of riparian zones and planning rehabilitation programmes. It may also be useful for improving the ecological knowledge base for setting environmental flows in regulated systems. Copyright © 2001 John Wiley & Sons, Ltd.     

Effects of stream flow intermittency on riparian vegetation of a semiarid region river (San Pedro River,Arizona)

The San Pedro River in the southwestern United States retains a natural flood regime and has several reaches with perennial stream flow and shallow ground water. However, much of the river flows intermittently. Urbanization‐linked declines in regional ground‐water levels have raised concerns over the future status of the riverine ecosystem in some parts of the river, while restoration‐linked decreases in agricultural ground‐water pumping are expected to increase stream flows in other parts. This study describes the response of the streamside herbaceous vegetation to changes in stream flow permanence. During the early summer dry season, streamside herbaceous cover and species richness declined continuously across spatial gradients of flow permanence, and composition shifted from hydric to mesic species at sites with more intermittent flow. Hydrologic threshold values were evident for one plant functional group: Schoenoplectus acutus, Juncus torreyi, and other hydric riparian plants declined sharply in cover with loss of perennial stream flow. In contrast, cover of mesic riparian perennials (including Cynodon dactylon, an introduced species) increased at sites with intermittent flow. Patterns of hydric and mesic riparian annuals varied by season: in the early summer dry season their cover declined continuously as flow became more intermittent, while in the late summer wet season their cover increased as the flow became more intermittent. Periodic drought at the intermittent sites may increase opportunities for establishment of these annuals during the monsoonal flood season. During the late summer flood season, stream flow was present at most sites, and fewer vegetation traits were correlated with flow permanence; cover and richness were correlated with other environmental factors including site elevation and substrate nitrate level and particle size. Although perennial‐flow and intermittent‐flow sites support different streamside plant communities, all of the plant functional groups are abundant at perennial‐flow sites when viewing the ecosystem at broader spatial and temporal scales: mesic riparian perennials are common in the floodplain zone adjacent to the river channel and late‐summer hydric and mesic annuals are periodically abundant after large floods. Copyright © 2005 John Wiley & Sons, Ltd.     

Impacts of water surface area of watershed on design flood简

In order to analyze the impact of the water surface area of a watershed on the design flood, the watershed was classified into a land watershed and a water surface watershed for flood flow calculation at the same time interval. Then, the design flood of the whole watershed was obtained by adding the two flood flows together. Using this method, we calculated design floods with different water surface areas of three reservoirs and analyzed the impact of water surface area on the flood volume and peak flow. The results indicate that larger water surface areas lead to greater impacts on the flood volume and peak flow. For the same watershed area, the impact of water surface area on the flood volume and peak flow is positively proportional to the flood frequency, i.e., the higher the frequency, the greater the impact becomes.     

Changes in riparian vegetation communities below a large dam in a monsoonal region: Futase Dam,Japan

This paper examines the effects of a dam reservoir flood control on riparian plant communities in an Asian monsoon area subjected to large summer floods under natural conditions. We compared riparian plant communities downstream of the Futase Dam located on the Arakawa River, with communities on the Nakatsu River, a tributary of the Arakawa River with no dam. Historical changes in spatial distribution of riparian vegetation communities were analysed using aerial photographs. Stand ages and flood history were also examined to analyse the likelihood of tree erosion in scenarios with and without flood control. Comparison of the two reaches shows that the reduced flood peaks below the Futase Dam led to the expansion of riparian forest area and an increase in species diversity. Reduction in the flood peaks below the dam means that the toppling moment of the trees is no longer exceeded. The result is that the riparian forest below the dam is able to develop into later successional stages. Copyright © 2004 John Wiley & Sons, Ltd.     

Impact of regulated releases on periphyton and macroinvertebrate communities: The dynamic relationship between hydrology and geomorphology in frequently flooded rivers.

Flood‐type disturbances affect both periphyton and macroinvertebrate communities depending on their frequency, magnitude and duration, but some impacts can be mitigated by geomorphic constraints. We studied four rivers in the Adirondack Mountains; the Indian River experienced regulated flow releases creating bank‐full floods four times/week whereas other study sites provided a continuum of control conditions for comparison. We sampled periphyton and macroinvertebrate communities in each river along with channel hydrology, hydraulics and geomorphology. Periphyton abundance varied seasonally and among rivers depending on nitrate concentrations and scour. Flow releases created a static mosaic of patches consisting of heavily scoured bed sediment in the thalweg (high shear stress areas—HSS) which had very low periphyton abundance; boulders and rocky shoals created low shear stress areas (LSS) supporting mats of filamentous algae. Macroinvertebrate densities were highest in HSS areas whereas LSS areas had lower macroinvertebrate densities that were more similar to reference rivers, although both LSS and HSS areas had the lowest species diversity and richness. Macroinvertebrate composition in HSS areas was dominated by filter‐feeders, whereas LSS areas had more gatherers and scrapers. While all rivers had high boulder densities, the Indian River could be considered geomorphically moribund—its substrate was immobile and the channel experienced no adjustments in spite of high flood frequencies. These physical characteristics help mitigate the severe hydrologic conditions that releases create because the static mosaic of low and HSS patches allow certain macroinvertebrates adapted to this level of disturbance to persist. This static mosaic is different from the shifting mosaic pattern often observed in streams following flood‐type disturbances. Geomorphically moribund rivers may lack ecological sensitivity to hydrologic disturbances, and decisions to limit flow modification (e.g. recreational flow releases, hydropower generation) should consider whether assumed ecological impacts are likely to occur given local geomorphic conditions and constraints. Copyright © 2010 John Wiley & Sons, Ltd.     

The importance for birds of the riparian woodlands within the alluvial corridor of the river garonne,S.W. France

Communities of nesting birds were studied in four distinct biotopes within the alluvial corridor of the River Garonne: 50 terrace woodlands, 17 riparian woodlands, one poplar plantation, and one slope woodland. A total of 400 stations were investigated, consisting of eight distinct classes of forest size for the terrace woodlands and four for the riparian woodlands. The distribution of 64 species of birds, observed by means of 20 minute listening point surveys, was related to three main factors: forest size, site wetness, and the wooded space marginality (forests, woods, copses, hedges, trees). Indices of mean richness and of mean abundance show that the riparian woodlands were the richest and the most densely populated. The surface area of woodlands has a strong effect on the structure of the bird community on terraces but less in the riparian environment. Multivariate analysis contrasted the species from the open islands within closed environments with the species from the closed islands within an open environment. The effect upon the nesting bird communities of the fragmentation of the original forest within the alluvial corridor of the River Garonne is demonstrated by a grouping of two characteristics: the connectivity of the riparian woodlands and the insularity of the terrace woodlands. The conservation of a continuous ribbon of riparian woodlands is shown to be an important condition for maintaining a rich community of nesting birds.     

Changes to herbaceous plant communities on a regulated desert river

Riparian plant communities are shaped by gradients of disturbance intensity and frequency and resource availability. Reservoir operation can alter the composition and abundance of riparian vegetation by changing the flood regime and by trapping fine sediments and associated nutrients within the reservoir system. We examined differences in herbaceous species richness, abundance and composition in Populus‐Salix stands along an unregulated and regulated reach of a river in semi‐arid Arizona, contrasted flood inundation frequency and edaphic conditions (soil moisture, nutrients and texture) between the reaches, and interpreted the vegetation differences in light of observed differences in environmental conditions. Flooding frequency was similar between reaches, but the proportion of fine textured soils in the unregulated reach was nearly double that of the regulated reach and soil nutrient levels were up to three times higher in the unregulated reach. Herbaceous cover and richness were consistently lower in the regulated reach, with between‐reach differences greatest during dry seasons. These patterns suggest that an edaphic‐based change in resource availability is the principal pathway by which river damming is altering herbaceous vegetation in this system. Our results demonstrate that sediment transport within riparian corridors is important for maintenance of herbaceous communities and that restoration of flow regimes alone may be insufficient to restore herbaceous flora on some regulated reaches. Copyright © 2008 John Wiley & Sons, Ltd.     

Simulating the effect of environmental flow duration on seedling emergence from riparian seed banks of the Upper Hunter River,New South Wales

Passive riparian revegetation techniques are important tools in river rehabilitation. However, the utility of the sediment seed bank as a passive riparian regeneration option is poorly understood. After modelling a range of flows for field‐surveyed cross sections, a glasshouse seedling emergence experiment was undertaken to compare the effects of simulated flow duration on seedling emergence of desirable riparian species that occur on benches of the gravel‐bedded Hunter River near Muswellbrook, New South Wales. The duration of inundation did have an effect (although not always significant) on seed germination for most species. The most successful simulated flood conditions differed among species, with the control treatment (no inundation) resulting in the most germination for only two of the 10 species examined. These findings suggest that although environmental flows for the sole purpose of stimulating the riparian seed bank in order to facilitate regeneration of desirable riparian species would be largely ineffective and complicated by differing inundation responses among species, seed bank stimulation using environmental flows could be a value‐added benefit from flows allocated for other purposes. As such, consideration of flow duration is worthy of inclusion in environmental flow allocation planning.     

Hydrogeomorphic and Biotic Drivers of Instream Wood Differ Across Sub‐basins of the Columbia River Basin,USA

Instream wood promotes habitat heterogeneity through its influence on flow hydraulics and channel geomorphology. Within the Columbia River Basin, USA, wood is vital for the creation and maintenance of habitat for threatened salmonids. However, our understanding of the relative roles of the climatic, geomorphic, and ecological processes that source wood to streams is limited, making it difficult to identify baseline predictions of instream wood and create targets for stream restoration. Here, we investigate how instream wood frequency and volume differ between seven sub‐basins of the interior Columbia River Basin and what processes shape these differences within these sub‐basins. We collected data on wood volume and frequency, discharge and stream power, and riparian and watershed forest structure for use in modelling wood volume and frequency. Using random forest models, we found that mean annual precipitation, riparian tree cover, and the individual watershed were the most important predictors of wood volume and frequency. Within sub‐basins, we used linear models, finding that some basins had unique predictors of wood. Discharge, watershed area, or precipitation often combined with forest cover, riparian conifer, and/or large tree cover in models of instream large wood volume and frequency. In many sub‐basins, models showed at least one hydrologic variable, indicative of transport competence and one ecological variable, indicative of the reach or upstream watershed's capability to grow measurable instream wood. We conclude that basin‐specific models yield important insights into the hydrologic and ecological processes that influence wood loads, creating tractable hypotheses for building predictive models of instream wood. Copyright © 2015 John Wiley & Sons, Ltd.     

VEGETATION–LANDFORM ASSEMBLAGES ALONG SELECTED RIVERS IN THE CZECH REPUBLIC,A DECADE AFTER A 500‐YEAR FLOOD EVENT

Rivers with a natural flow regime strongly influence the dynamics of riparian plant communities through hydrological and geomorphological processes. In this study, associations between fluvial landforms and vegetation are investigated on three near‐natural rivers in the Czech Republic a decade after a 500‐year return period flood in July 1997. This extreme disturbance destroyed the anthropogenically modified river channels and created suitable conditions for a range of ecosystems with high diversity and ecological stability. Field surveys were conducted on fluvial landforms (bars, islands, banks, floodplains and terraces) along three ‘renaturalized’ rivers, where no technical modifications had subsequently been made to their channels outside urban areas and the floodplains had been left in a post‐flood state. Vegetation species abundance and 13 environmental variables (topographical, hydrological and soil) were investigated in summer 2007, 10 years after the extreme flood disturbance. The results suggest that the recently created fluvial geomorphic forms are key environmental determinants of riparian vegetation distribution patterns. A range of statistical analyses illustrate that some plant species show predictable patterns of occurrence that correspond with the fluvial forms, supporting a fourfold grouping of herbaceous and woody species and the identification of typical plant communities associated with gravel bars, islands, banks, floodplains and terraces. An investigation of the species richness found on different fluvial landforms showed that the highest number of species occurred on the floodplain and decreased gradually towards the channel bed and towards terraces. Investigation of existing conditions in reaches of rivers with natural dynamics of fluvial processes provides valuable information that can be used as an effective tool for planning restoration strategies and precise management. However, the most important finding of this study is the remarkable establishment of complex river corridor vegetation–landform associations within 10 years of a 500‐year flood that removed the heavily cultivated landscape that had existed before the event. Copyright © 2011 John Wiley & Sons, Ltd.     

How do instream flow increase and gravel augmentation impact biological communities in large rivers: A case study on the Upper Rhine River

Actions are being developed to address the adverse consequences of engineering works on large European rivers by developing and implementing restoration activities in order to enhance the functionality and biodiversity of fluvial hydrosystems. However, as has frequently been mentioned in the scientific literature, quantitative and qualitative evaluation of the project benefits, if any, and their sustainability are hindered by the difficulty in assessing the responses of aquatic and riparian communities to the methods employed. A case study was conducted on a by‐passed section of the Upper Rhine River (France and Germany) to investigate the effects of instream flow increase and gravel augmentation on selected aquatic and riparian communities (macroinvertebrates, macrophytes, and riparian plants). This paper presents the results of a 6‐year interdisciplinary, before‐after control‐impact design monitoring study. The complexity of the study lies in carrying out a separate assessment of the cumulative effects on a site‐based, project‐specific basis. The results showed that (a) the instream flow increase resulted in greater richness of macrophyte species in the newly created backwaters, (b) the artificial gravel bar favoured the recruitment of pioneer species, including invasive species, although gravel redistribution by floods prevented their development, and (c) gravel augmentation tended to promote the taxonomic richness of macroinvertebrate communities with the appearance of species adapted to the new substrate areas. These findings should help to fill the knowledge gaps in large‐scale restoration and contribute key responses to the most frequently arising issues in this area, especially those concerning the efficiency and sustainability of river restoration projects.     

EFFECT OF A MAJOR FLOOD ON BREEDING AND HABITAT OF THE CRIMSON FINCH (NEOCHMIA PHAETON): A RIPARIAN SPECIALIST

Riparian specialists, such as the Crimson Finch (Estrildidae: Neochmia phaeton), are vulnerable to declines in habitat quality, including alterations of flow regime associated with dam construction. Crimson Finches persisted and bred in substantial numbers following two large floods in the Isaac–Connors catchment in early 2008. Major flooding was not detrimental to nesting and breeding success, although the immediate post‐flood period was identified as a bottleneck in the availability of riparian grass seed. Crimson Finches nested at 16 m or more above the normal river level (compared with an average of 2–3 m elsewhere in Northern Australia); indicating that they have adapted to the extreme flood peaks in the Fitzroy River basin. The tall river‐associated grass Chionachne cyathopoda was a key habitat plant, retaining seed well into the dry season when most other grasses are expended. It also provided abundant seeds following floods, coinciding with peaks in abundance of dependent young finches. The adaptations of both Crimson Finches and Chionachne suggest that increased flooding, predicted by climate change, is unlikely to be a problem. In contrast, a proposed dam on the Connors River may be a threat. River regulation that reduces peaks of major floods may favour introduced riparian grasses over flood adapted native grasses such as Chionachne. Any change in the quantity of this species could be detrimental to persistence of Crimson Finches. Environmental managers should carefully consider the ecology of Chionachne when making decisions about river flows. Copyright © 2013 John Wiley & Sons, Ltd.     

The influence of major dams on hydrology through the drainage network of the Sacramento River basin,California

This paper reports basinwide patterns of hydrograph alteration via statistical and graphical analysis from a network of long‐term streamflow gauges located various distances downstream of major dams and confluences in the Sacramento River basin in California, USA. Streamflow data from 10 gauging stations downstream of major dams were divided into hydrologic series corresponding to the periods before and after dam construction. Pre‐ and post‐dam flows were compared with respect to hydrograph characteristics representing frequency, magnitude and shape: annual flood peak, annual flow trough, annual flood volume, time to flood peak, flood drawdown time and interarrival time. The use of such a suite of characteristics within a statistical and graphical framework allows for generalising distinct strategies of flood control operation that can be identified without any a priori knowledge of operations rules. Dam operation is highly dependent on the ratio of reservoir capacity to annual flood volume (impounded runoff index). Dams with high values of this index generally completely cut off flood peaks thus reducing time to peak, drawdown time and annual flood volume. Those with low values conduct early and late flow releases to extend the hydrograph, increasing time to peak, drawdown time and annual flood volume. The analyses reveal minimal flood control benefits from foothill dams in the lower Sacramento River (i.e. dissipation of the down‐valley flood control signal). The lower part of the basin is instead reliant on a weir and bypass system to control lowland flooding. Data from a control gauge (i.e. with no upstream dams) suggest a background signature of global climate change expressed as shortened flood hydrograph falling limbs and lengthened flood interarrival times at low exceedence probabilities. This research has implications for flood control, water resource management, aquatic and riparian ecosystems and for rehabilitation strategies involving flow alteration and/or manipulation of sediment supplies. Copyright © 2006 John Wiley & Sons, Ltd.     

渭河华县段漫滩洪水变异特征及其生态效用探析

以渭河华县段漫滩洪水为研究对象,首先运用ToB(Top of Bank)方法确定不同历史大断面下的河道漫滩水位,采用水位流速法计算并统计渭河华县段1965-2010年间漫滩洪水发生的次数、淹没持续时间及漫滩期最大流量,并进一步分析其演变趋势。其次,以漫滩洪水发生次数和淹没持续时间为评估指标,应用变化范围法(RVA)对漫滩洪水的变异程度进行评估,从侧面探讨漫滩洪水变化对滨河生态系统的潜在影响。计算结果显示,渭河华县段1965-2010年间累计发生漫滩洪水34次,年均仅0.74次,且漫滩洪水次数、淹没持续时间、漫滩最大流量在时域上均呈显著下降趋势。尤其是20世纪90年代以后,受来水量减少和渭河下游泥沙淤积的共同影响,漫滩洪水多为小流量洪水,较以前其流速和流量都有所减弱,生态效果有限。而RVA评价结果则表明渭河华县段漫滩洪水的淹没次数和持续时间两个指标均发生了高度变异,缩减严重,对滨河生态环境有较大的潜在威胁。建议管理部门制定相应措施,适时人造漫滩洪水,以保障滨河湿地、滩地的生态平衡与安全。     

黄河无定河流域“2017.7.26”洪水泥沙来源辨析

2017年7月25—26日无定河流域降大到暴雨,支流大理河发生建站以来的最大洪水,无定河下游形成高含沙洪水。为深入认识“7.26”暴雨无定河流域产沙和输沙等情况,选择典型小流域进行了侵蚀调查和淤地坝拦沙观测,对城区淤积及河道冲刷进行了调查和测量,采用不同方法对坡面和沟谷产沙进行分析。结果表明,无定河“2017.7.26”暴雨分布集中,单站最大24 h降雨量近100年一遇,无定河白家川水文站洪峰流量为建站以来第二大值,相应最大含沙量873 kg/m3; 洪水期输沙量64.1%来自大理河流域; 以闷葫芦淤地坝拦沙分析为依据,推算“2017.7.26”暴雨期无定河流域侵蚀产沙量约为1.249亿t,其中70%~85%来自沟谷坡,在泥沙沿程输移过程中,淤地坝拦沙对减少河道输沙入黄起重要作用。     

DECLINE AND RECOVERY OF SMALL MAMMALS AFTER FLOODING: IMPLICATIONS FOR PEST MANAGEMENT AND FLOODPLAIN COMMUNITY DYNAMICS

Floodplains often are managed both for agriculture and as habitat for native species. On the Sacramento River, farmers have expressed concern that natural areas may harbour small mammals in greater abundance than occurs on farms, which could make them sources of pests to adjoining farmlands. Concern over this has generated some opposition to riparian restoration. To better understand the issue, we studied small mammals at agricultural sites, young and older riparian restoration sites and remnant natural areas through live trapping and visual surveys over three successive years. Significant flooding occurred during the second winter of the study. We found that young riparian restoration sites (3–4 years since planting) did not harbour agricultural pests (e.g. California ground squirrel, Botta's pocket gopher) in greater abundance than agricultural sites, with the exception of California voles. Although voles were common at young sites, they declined dramatically as the sites matured, and neither 12‐ to 15‐year‐old sites nor remnant riparian habitats had higher abundances of any small mammal pest species than agricultural sites. All species except the arboreal western gray squirrel experienced significant population declines following the flood and remained at depressed levels for at least a full year thereafter. Native species were not less susceptible to flooding than exotic species. California vole was the first species to recover. Our study suggests that frequent winter flooding may be desirable from an agricultural pest management perspective. It illustrates a valuable ecosystem service, small mammal pest control, which is provided by flooding, an important natural disturbance process. Copyright © 2011 John Wiley & Sons, Ltd.     

温德河流域暴雨洪水时空特征及模拟分析

受降雨和地形影响,吉林省温德河流域季节性洪灾频繁。为了解温德河流域暴雨洪水规律,利用2017年7—8月3次山洪灾害的暴雨洪水监测资料,采用自主研发模块化小流域分布式水文模型模拟了流域的洪水过程,取得较高的模拟精度。并结合研究区春登河、西阳河及五里河等三个主要河段的模拟流量和暴雨时空分布特征,分析三场暴雨时空分布对洪水造成的影响,总结了该流域2017年山洪灾害产生原因。结果表明:①温德河流域三场超标准洪水由短历时强降雨引起,"雨洪同向"的降雨锋面移动特点使洪峰呈现陡涨陡落之势;②"7·13"和"7·19"洪水的降雨时空集中程度和暴雨中心分布的差异影响两场洪水洪峰峰型、流量和各河段的洪量贡献比,造成温德河流域不同程度的灾害。     

ASSESSMENT OF RIPARIAN VEGETATION SENSITIVITY TO RIVER HYDROLOGY DOWNSTREAM OF A MAJOR TEXAS DAM

Dams may impact the health of downstream riparian vegetation communities through flow modifications such as decreased flood frequency and duration. Without historical vegetation data, however, it is difficult to relate changes in vegetation composition to hydrology patterns downstream of dams. We studied bottomland hardwood forests downstream of Toledo Bend Dam on the Sabine River in Texas and Louisiana to determine their sensitivity to minor changes in river hydrology with a particular focus on floods. Current riparian vegetation was characterized within three topographic zones at three selected sites below the dam. Using 80 years of hydrologic records from two gauging stations downstream of the dam, we evaluated trends in flood frequency, flood duration, peak discharge and total flood discharge in those periods before (1926?1965) and after (1971?2005) dam construction, as well as related flood stage to floodplain elevations to link topography to flood frequency. Plant species diversity in this system is highly dependent on minor changes in elevation, and the proportion of wetland‐dependent species changes rapidly with only a few centimeters difference in elevation. Although 50% of trees, shrubs and herbs in the sloughs were wetland adapted, their numbers were only 21% in the levees (74–284 cm higher in elevation) and 14% in the mid‐floodplains. Since dam construction, total flood discharge and duration at the most upstream gauge on the Sabine River decreased by 49%. At both gauges, mean discharge was also altered with higher summer flows. Patterns of tree regeneration point to less recruitment by wetland‐dependent species in the years following dam construction. These results suggest that minor changes in flood magnitude might limit occurrence of wetland species to the lowest topographic zones and illustrate the need to analyse sensitivity of plants to minor changes in flood characteristics when historical data for the vegetation community are lacking. Copyright © 2012 John Wiley & Sons, Ltd.     

Dam reverse flow events influence limnological variables and fish assemblages of a downstream tributary in a Neotropical floodplain

We used a dam‐free tributary (the Baía River) in the upper Paraná River floodplain downstream of a major dam in the Paraná River, Brazil to investigate the effects of dam‐regulated reverse flow on limnological variables and fish. We tested the hypotheses that limnological variables in tributaries change based on flow direction and that fish assemblages respond to this variation. Sampling sites were determined considering flow direction (normal or reverse) and position (near or far from the river mouth). Limnological variables showed higher values for transparency, oxygen, pH, and electrical conductivity at sites near the mouth of the Baía River during reverse flow. Species richness and evenness differed significantly in relation to position, with higher values closer to the Paraná River. The average standard length of fish species was higher near the mouth of the Baía River and during the reverse flow period. No significant differences in species abundance were found. Reverse flow into the Baía River brought nutrient‐poor water from the dammed Paraná River, thereby altering the limnological variables. This flow condition impelled the entry of species with higher average standard lengths. However, increased species richness and low evenness were due to the increase in species dispersal rates under all flow conditions. Our results emphasize that the effects of dams can extend several kilometres into the floodplain, provide basic knowledge on the effects of major dams on downstream pristine tributaries, and highlight the need for further studies to understand the wider influences.     

Increasing River Flow Expands Riparian Habitat: Influences of Flow Augmentation on Channel Form,Riparian Vegetation and Birds Along the Little Bow River,Alberta

With river regulation, water withdrawal is common, reducing instream flows. The opposite alteration, flow augmentation, is less common and could reveal a mechanistic coordination between flow regime, channel form, and riparian ecosystems. The Little Bow River, a naturally intermittent prairie stream in Southern Alberta, has experienced flow augmentation since the late 1890s, and the Little Bow/Highwood Project of 2004 enabled a tripling of diversion flows from 2.9 to 8.5 m³/s. We investigated the subsequent responses by assessing the channel form and riparian vegetation based on aerial photographs taken in 2000 versus 2010, and riparian birds were assessed between 2005 and 2013 to investigate associations with riparian vegetation. Following recent flow augmentation, the mean channel width increased from 12.2 to 13.5 m, while sinuosity was relatively unchanged. Streamside zones with true willows (especially Salix exigua and Salix bebbiana) increased from 7 to 11% of the river corridor, and the facultative riparian wolf willow (Elaeagnus commutata) zones increased from 16 to 20%, while grassy zones decreased from 64 to 52%. Avian species richness and Shannon–Wiener index increased, while species evenness was relatively unaltered, suggesting an increase of rarer bird species in response to the increased habitat structure and diversity following the expansion of riparian shrubs and woodland. This study revealed responses to the recent flow augmentation over the first decade of implementation, and alterations following flow augmentation would likely continue for decades until the river and riparian zones adjust to the new flow regime. Copyright © 2016 John Wiley & Sons, Ltd.