Titlebook: Advanced Modelling and Innovations in Water Resources Engineering; Select Proceedings o Chintalacheruvu Madhusudana Rao,K. C. Patra,Sangee

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Reiner Westermeier,Angelika G?rgural catastrophe. The main input parameter for any hydrodynamic modeling is river geometry. A discussion of a method to create river geometry by using the Cartosat-1 Digital Elevation Model (DEM) has been carried out. Many difficulties in distinguishing arise in hydraulic features, which requires pr

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https://doi.org/10.1007/978-3-8274-2156-2he way for drastic changes in the riverine ecosystem. Any disruption in the river‘s natural flow regime can alter the entire river ecosystem and socio-economic activities. Environmental flows are mainly defined based on hydrologic, hydraulic, and ecological conditions of a river system. Given the ch

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https://doi.org/10.1007/978-3-8274-2156-2), simple linear regression (SLR), Kendall rank correlation (KRC), Mann–Kendall (MK), and modified MK (MMK) methods to investigate the magnitude (size of trend) and trend in annual, seasonal, and monthly streamflow of Naula and Kedar hydrological stations. Both stations are placed in the upper catch

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DNA, RNA und IHRE Amplifikation,ate descriptors. The landscape descriptors such as land use/land cover (LU/LC), geomorphologic, soil property and geology, and the climate descriptor of the river basin are estimated for Upper Baitarani river basin in India to identify the characteristic features of this basin. The required data is

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Lecture Notes in Civil Engineeringhttp://image.papertrans.cn/a/image/145993.jpg