International Conference: Recent submissions

  • 27-Modeling Urban Flooding from Storm Sewers Using Dynamic Wave Theory. 
    Mukhopadhyay, Biswajit; Dutta, Aniruddha; Nouri, Fariborz; Kaushik, Chitranjan (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    Traditionally, urban storm sewers, meant to convey excess runoff from impervious covers efficiently, are designed with the applications of rational formula of hydrology with all of the conceptual limitations of the method. ...
  • 28-Numerical Modeling for Floodway Assessment—A Case Study. 
    Panu, U. S.; McKenna, Dominic; Tomlinson, Daniel (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    Vitality of the Neebing-Mclntyre Floodway based on a variety of climatic and geometrical boundary conditions has been evaluated. A numerical hydraulic model of the floodway was developed. Sensitivity analysis of the floodway ...
  • 29-Development of Interface for Daily Runoff Assessment from a Watershed. 
    Dhore, K. A.; Khare, Deepak; Chaube, U. C.; Garg, P. K. (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    Surface runoff is one of the major components in watershed hydrology. The amount of runoff generated from any watershed depends on the many watershed characteristics such as land use, soil type and its physical properties, ...
  • 30-Quantification of Urban Runoff Reaching to the Upper Bhopal Lake, M.P., India . 
    Dwivedi, Vijay K.; Ojha, C. S. P.; Choubey, V. K. (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    The Upper Bhopal Lake in the city of Bhopal in the State of Madhya Pradesh of India is the only source of water for the city of Bhopal. Economic as well as recreational activities of the city of Bhopal is dependent on the ...
  • 31-Modeling Rainfall-Runoff Process Using Grey System Theory with Two Solution Procedures. 
    Trivedi, Harsh V.; Singh, J. K. (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    Rainfall-runoff is a nonlinear process and can be modeled with a nonlinear modeling framework. The process of rainfall to runoff transformation involves a complex mechanism and it is quite difficult to understand too. To ...
  • 32-Genetic Algorithm Based Unit Hydrograph. 
    Rai, R. K.; Gundekar, H. G.; Sarkar, S.; Mathur, B. S. (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    Unit hydrograph approach is one of the commonly used techniques employed for the determination of flood hydrographs. For this purpose various distribution functions have been utilized in the past. The suitability of the ...
  • 33-Impacts of Urbanization on Streamflow. 
    Rudra, Ramesh P.; Dickinson, Trevor; Ahmed, Syed I. (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    This study has concentrated on the temporal and spatial changes in streamflow patterns due to urbanization and/or rainfall trends within the watershed. The analyses were conducted by using the rainfall data from two stations, ...
  • 34-The Development of a Flood Risk Model for Romania. 
    Bachu, Murthy; Jadhav, Kunal; Chendes, Viorel (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    Spatially explicit hydrodynamic flood models can play an important role in natural hazard risk reduction. A key element of these models that make them suitable for risk reduction is the ability to provide inundation ...
  • 35-Mathematical Model of River Mandarmani, Purba Midnapore—A Case Study. 
    Dolai, D. P.; Roy, Shyamal Kumar (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    Jalda Kuthi is a traditional fish landing centre situated on the bank of Mandarmani River at the confluence of Bay of Bengal in Purba Midnapur District of West Bengal. Due to siltation at the confluence of the river, the ...
  • 36-Experimental Evidences on the Run-on Process. 
    Corradini, Corrado; Morbidelli, Renato; Saltalippi, Carla; Flammini, Alessia; Govindaraju, Rao S. (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    Experimental evidence of infiltration of excess water that moves downslope over unsaturated areas, usually called run-on process, is provided in laboratory. The experiments were carried out using a laboratory slope ...
  • 37-Melt-Runoff Delaying Characteristics of Gangotri Glacier. 
    Arora, Manohar; Singh, R. D.; Kumar, Amit; Singh, Pratap (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    Most of the Himalayan basins have considerable snow and glacier covered areas. The melt contribution in such rivers augments their flows in the lean season, thereby reducing the variation in water availability. Depending ...
  • 38-Role of Snow and Glacier Melt Runoff Modelling in Hydropower Projects in the Himalayan Region. 
    Singh, Pratap; Polglase, Larry; Wilson, David (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    At present the installed capacity of Indian hydropower projects is about 35900 MW, which represents 25% of the total installed capacity of India (1,43,000 MW). The share of hydropower generated in the Himalayan region is ...
  • 39-Estimation of SWE and Surface Energy Balance for a Snow Cover in Pir-Panjal Range of N-W Himalaya. 
    Datt, Prem; Pooja; Srivastava, P. K.; Negi, P. S. (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    Melting of seasonal snowpack in mountainous ranges of Indian Himalaya contributes significantly to the rivers flowing in the mountain valley. The melting of snow starts in late winter, i.e., from April onwards and produces ...
  • 40-Snow Harvesting for Drinking and Irrigation Water - A Case Study. 
    Negi, P. S.; Sethi, D. N.; Mathur, P. (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    In the recent past due to global warming and change in climate, the snow fall pattern has changed considerably. The late snow fall, frequent avalanche activity and fast snow melting reduces the frequency of contact time ...
  • 41-Suspended Sediment Transfer in a Himalayan Headwater Stream - Glacier vs Monsoon. 
    Thayyen, Renoj J.; Gergan, J. T.; Dobhal, D. P. (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    Sediment load in the Himalayan rivers are many fold than the world average. Being the youngest and tectonically active mountains, increased erosion during the monsoon is sited as one the reasons for the higher erosion rate. ...
  • 42-Rainfall Contribution in Bhagirathi River near Gangotri Glacier Snout, Gomukh, Western Himalayas, India, Using Stable Isotope. 
    Rai, S. P.; Kumar, Bhishm; Singh, Pratap (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    Gomukh is the snout of Gangotri Glacier located at an altitude of 4000 m from where the snow/glacier meltwater stream known as Bhagirathi river emerges out. Stream and rainfall samples were collected for stable isotopes ...
  • 43-Development versus Sustainable Development of Ground Water Resources in Indian Context. 
    Rai, S. N. (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    The accelerated growth in population, industries and agriculture has brought about many fold increase in the water supply. Groundwater contributes significantly to meet the ever increasing demand of water supply. Massive ...
  • 44-A Protocol for Groundwater Recharge Capability Assessment Using Multi-Themati Parameters - An Example from a Semi-Arid Region of Rajasthan, India. 
    Roy, S. Sinha (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    The shallow to middle level aquifer systems in semi-arid regions of central Rajasthan, India, are depleted of groundwater resources, showing a steady fall in the water table, due to an imbalance in recharge and abstraction. ...
  • 45-Forecasting Spatiotemporal Water Levels of Tabriz Aquifer. 
    Nourani, V.; Moghaddam, A. A.; Nadiri, A. O.; Singh, V. P. (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    This paper evaluates the feasibility of using an Artificial Neural Networks (ANNs) methodology for estimating the groundwater level in some piezometers placed in an aquifer in northwestern Iran. This aquifer is complex and ...
  • 46-Analysis of Natural Recharge and Groundwater Dynamics in Alluvial Aquifer Systems . 
    Jha, Madan K.; Roshni, T.; Kamii, Yasumori (Allied Publishers Pvt. Ltd., New Delhi, 2009)
    Proper knowledge of groundwater recharge is essential for the management and protection of valuable groundwater resources. Natural groundwater recharge is a very complex and dynamic phenomenon, and its determination ...

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