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

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cess, miniaturized semiconductor devices derived from various technologies and meeting an ever-changing demand kept emerging. As most of us learned in the later stage of studying semiconductor physics and circuits, integrated circuits comprised of different technologies and configurations require DC

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transdermal

Bjarke Christensen,Jens Nielsenrole in advancement toward the intricate approach for solving various real-life problems. One such initiation is the simulation analysis. The major advantage of this approach is the reduction in the utilization of natural resources for physical modeling. The present investigation is aimed at applica

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innovation

C. J. Dyde,M. F. Barkworth,K. D. Rehm for the region. Marathwada region of Maharashtra state, India is selected for this study. Marathwada region is facing extremely dry conditions again and again over the period. Marathwada region has 8 districts and 76 blocks. This study provides a blockwise characterization of meteorological drought

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Eric Reid,J. D. Robinson,Ian D. Wilsonbeen used for rainfall predictions. One of such tools which have been developed in recent times to promote the study of hydrological modelling and rainfall forecasting is by using fuzzy logic and ANN. The present study has been done out to analyze and compare the fuzzy logic and ANN based analysis f

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Frank Carey,Duncan Haworth,Robert A. Forder Mahanadi river basin. To identify the flooding events a flood disaster database Dartmouth Flood Observatory is used and archives from this source were examined and flooding years were identified as 1994, 2005 and 2007. To verify the flood events derived from the database, data of streamflow is used

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Eric Reid,J. D. Robinson,Ian D. Wilsonpractical application of water in domestic, industrial, and irrigation applications, especially in the hilly Himalayan region of India. Lightly substantial declines in the spring flows from any source can affect the flow activity of rivers in the Himalayan regions. In the Himachal Pradesh and Ladakh