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Upper Catchment (upper + catchment)

Distribution by Scientific Domains

Life Sciences	40%
Earth and Environmental Science	40%

Selected Abstracts

Instream and catchment characteristics affecting the occurrence and population density of brown trout, Salmo trutta L., in forest brooks of a boreal river basin

FISHERIES MANAGEMENT & ECOLOGY, Issue 6 2001
E. Jutila
The occurrence and density of , 1+ brown trout, Salmo trutta L., and their relationship with prevailing instream and catchment characteristics were studied in 50 small forest streams, partially dredged for forest ditching. The occurrence of trout at a stream site was largely determined by the abundance of pools, size of upper catchment and water pH. Moreover, at sites where trout occurred, the abundance of pools was lower at dredged locations than at those in a natural state. In riffles in a natural state, there was a positive relationship between trout density and three instream variables: the abundance of stream pools, cascades and instream vegetation, while an inverse relationship was found with the abundance of substratum of 2,10 cm in diameter. Of the catchment variables, correspondingly, the proportion of forest in the upper catchment was positively related and the proportion of peatland negatively related to trout density. No significant regression model could be fitted for dredged riffles. The possibility of enhancing trout populations in dredged riffles is discussed. [source]

Source,sink dynamics sustain central stonerollers (Campostoma anomalum) in a heavily urbanized catchment

FRESHWATER BIOLOGY, Issue 10 2008
ERIC R. WAITS
Summary 1. The influence of spatial structure on population dynamics within river,stream networks is poorly understood. Utilizing spatially explicit analyses of temporal genetic variance, we tested whether persistence of central stonerollers (Campostoma anomalum) reflects differences in habitat quality and location within a highly modified urban catchment in southwestern Ohio, U.S.A. 2. Estimates of genetic diversity did not vary with habitat quality. Nevertheless, evidence of weak but temporally stable genetic structure, location-dependent effective population sizes and rates of immigration among sites, together suggest that persistence of central stonerollers within the catchment may be attributable to source,sink dynamics driven by habitat heterogeneity. 3. Under this scenario, migrant-pool colonization from areas of relatively high habitat quality in the upper catchment sustains the presence of central stonerollers at degraded sites in the main stem and dampens population subdivision within the catchment. However, because intact habitat is restricted to the upper portion of the catchment, it is not possible to preclude net downstream dispersal as a mechanism contributing to source,sink dynamics. The slight genetic structure that persists appears to reflect weak isolation by distance diminished by high rates of immigration. 4. This study suggests that without a systems perspective of the conditions that sustain populations in degraded waterways, environmental assessments may underestimate levels of impairment. Conservation and management of stream fishes could be improved by maintaining habitat in areas that are net exporters of migrants or by remediation of impaired habitat. [source]

Ecohydrology of a seasonal wetland in the Rift Valley: ecological characterization of Lake Solai

AFRICAN JOURNAL OF ECOLOGY, Issue 3 2009
Tanguy De Bock
Abstract The following research describes through an ecohydrological approach, the first assessment of the ecology of Lake Solai, with a particular emphasis on the vegetation. Lake Solai is located 50 km north of Nakuru in the Rift Valley in Kenya at E36°80,,36°84, to N00°05,,00°08,. It is a shallow lake that follows a very peculiar seasonal water regime, and that faces conflicts between agriculture and conservation water users. In the upper catchment, an overview of the agricultural practices was implemented and river water uses were identified to assess river flows. Crops/grassland and woodland/shrubland were the major land uses, covering c. 65% of the catchment. Closer to the lake, vegetation samples were collected around the lake together with samples of environmental factors such as soil and water quality. Thirteen vegetation communities were identified within four main zonations: forest, grassland, river inlet and rocky outcrop. These communities showed abundance, distribution and diversity determined mostly by the human pressures, the flooding periods and the salinity. Cynodon, Cyperus and Sporobolus genera were the most abundant. Résumé La recherche suivante décrit, par une approche éco-hydrologique, la première évaluation de l'écologie du lac Solai, en insistant particulièrement sur la végétation. Le lac Solai est situéà 50 km au nord de Nakuru, dans la vallée du Rift kényane, et ses coordonnées sont 36°80,,36°84E à 00°05,,00°08,N. C'est un lac peu profond qui est soumis à un régime hydrique saisonnier très particulier et qui est confrontéà des conflits entre acteurs agricoles et de conservation de la nature. En amont du bassin, une étude des pratiques agricoles a été effectuée, puis les utilisations de l'eau identifiées pour évaluer les débits des rivières. Les cultures/prairies et les forêts/broussailles étaient les principales utilisations des terres et couvraient environ 65% du bassin versant. Plus en aval, des échantillons de végétation ont été récoltés le long du lac, en même temps que des échantillons de facteurs environnementaux tels que le sol et l'eau. Treize communautés végétales ont été identifiées au sein de quatre zones principales: forêt, prairie, rivière entrante et affleurement rocheux. Ces communautés présentaient une abondance, une distribution et une diversité qui étaient principalement déterminées par les pressions humaines, les périodes d'inondation et la salinité. Les genres Cynodon, Cyperus et Sporobolusétaient les plus abondants. [source]

Community cooperation with natural flood management: a case study in the Scottish Borders

AREA, Issue 3 2009
Olivia Ruth Howgate
The cooperation of communities and landowners in the upper catchment is vital for the successful implementation of natural flood management (NFM) projects as few incentives are in place to reward them to host such projects. The aim of this paper is to initiate an exploration of the issues that affect a community's decision to cooperate. The results of a case study in Scotland show that willingness to cooperate is affected by concern about alternative flood management techniques, a sense of responsibility to help connected communities at risk of flooding and the expectation of beneficial impacts from the project. Indeed, these issues appeared to over-ride the hostility generated towards the project as a result of poor communication and engagement with the community from organisations associated with the proposed project. The results of the research suggest that if NFM projects are to proliferate, close attention must be paid to community attitudes towards flood management and related communities at risk, and that NFM projects must be developed and implemented according to well-established principles of public participation. [source]

Hydro-meteorological variability in the greater Ganges,Brahmaputra,Meghna basins

INTERNATIONAL JOURNAL OF CLIMATOLOGY, Issue 12 2004
MD. Rashed Chowdhury
Abstract The flows of the Ganges, Brahmaputra and Meghna (GBM) are highly seasonal, and heavily influenced by monsoon rainfall. As a result, these rivers swell to their banks and often overflow during the monsoon months. This is most pronounced in the downstream regions, particularly in Bangladesh, which is the lowest riparian country. The objective of this paper is to study this hydro-meteorological variability in the greater GBM regions, including the headwater regions in India and their role in streamflows in Bangladesh, and explore the large-scale oceanic factors affecting this hydro-meteorological variability. Global precipitation data, Bangladesh rainfall and streamflow records have been analysed and related to large-scale climate patterns, including upstream rainfall, regional atmospheric circulation and patterns of sea-surface temperature. The findings have quantified how the streamflows of these rivers in Bangladesh are highly correlated with the rainfall in the upper catchments with typically a lag of about 1 month. Therefore, streamflows in Bangladesh could be reasonably estimated for 1 to 3 months in advance (especially for the Ganges and Brahmaputra rivers) by employing simple correlation, if rainfall data from countries further up are available on a real-time and continuous basis. In the absence of rainfall data, streamflow forecasts are still possible from unusually warm or cold sea-surface temperatures in the tropics. The study concludes that hydro-meteorological information flow between Bangladesh and other neighbouring countries is essential for developing a knowledge base for evaluating the potential implications of seasonal streamflow forecast in the GBM basins in Bangladesh. Copyright © 2004 Royal Meteorological Society [source]