Titlebook: Environmental Management of River Basin Ecosystems; Mu. Ramkumar,K Kumaraswamy,R. Mohanraj Book 2015 Springer International Publishing Swi

Transfusion

https://doi.org/10.1007/978-981-99-5818-4have analyzed the rainfall data of the Cauvery river basin, a larger river basin in Southern India which plays a significant role in agricultural development and consequently in the overall growth of Karnataka, Tamil Nadu, Pondicherry and some parts of Kerala. The analysis includes distribution, var

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Pioneering on the Litigation Frontier,o nearly half of Calgary, a fast growing city of 1.1 million inhabitants. The watershed is characterized by a complex hydrological regime and is typical of snow dominated basins, with a spring freshet driven by snow melt and rainfall in late spring and early summer. This context creates favorable co

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,Darwin’s Voyage on the Beagle,, lithological and geomorphological conditions in which water flows and resides. This analysis allowed the identification of the geological evolution and recharge mechanism of the water resources in an arid environment. The studied waters at various sites are different in mineralization but similar

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Daniela Giannetti,Naoko Taniguchinfluences of anthropogenic pressures and climate change. The examination of the temporal trends in the rainfall, temperature and river runoff was done using historical datasets. It was supplemented with the data on the land use/land cover (LU/LC) change in the basin based on the LANDSAT TM data. By

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Gabriel G. Bès,Thierry GuillotinRiver basin is also vulnerable to negative impacts of climate change. Since accurate prediction of extreme events is essential for assessing the impact of climate change, any integrated monitoring and prediction system should be based on the hydrometeorological system. For this goal, dynamic downsca

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https://doi.org/10.1007/978-981-99-7081-0 events in terms of geomorphic and sediment textural, mineralogical, geochemical and other characteristics in the ensuing deposits. The spatio-temporal variations of the governing factors of the system introduce proportionate changes, which are normally inferred as sub-environments of a delta. An ab

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https://doi.org/10.1007/978-3-642-46568-0s of the host rocks and climatic effects. The resultant changes are exhibited by the geomorphic indices and landform assemblages within a river basin. This paper presents the results of integrated quantitative geomorphic analysis conducted for understanding the prevalent tectonic activities in a med