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12-14 September, 2011, Lucknow - Earth Science India

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National Conference on <strong>Science</strong> of Climate Change and <strong>Earth</strong>’s Sustainability: Issues and Challenges ‘A Scientist-People Partnership’<br />

<strong>12</strong>-<strong>14</strong> <strong>September</strong>, <strong>2011</strong>, <strong>Lucknow</strong><br />

assessment of total water resources in the basin and the water requirement for different<br />

purposes is not precisely estimated. Discharge is considered as the basic unit for water<br />

availability estimations which may be affected by a number of basin parameters and<br />

developmental activities such as population, industrialization, change in the irrigated<br />

areas, improvement in irrigation efficiencies, availability and development of<br />

groundwater, change in land use (increase/decrease in forest area, urban land, barren<br />

land etc.), change in the climate of the region (increase/decrease in temperature,<br />

precipitation etc.), construction of hydraulic structures etc. Therefore, a need was felt to<br />

develop a detailed model to assess various components of the hydrological cycle in a<br />

river basin and to estimate the demands for various purposes.<br />

To evaluate various components of the hydrological cycle at the basin scale, a<br />

conceptual spatially distributed water balance model has been developed. In this model,<br />

focus is given to incorporate spatial variation of land-use, soil type, rainfall, evapotranspiration,<br />

physiographic characteristics, cropping pattern, irrigation development,<br />

groundwater conditions, river network and hydraulic structures in a river basin. GIS is<br />

employed to link the spatial data with the simulation model and to project the model<br />

results in map form for easy visualization. The basin is divided into grids of uniform<br />

size (~ 1 km) and model computes various components of hydrologic cycle such as<br />

actual evapo-transpiration, overland flow, groundwater recharge, and residual soil water<br />

content at monthly time step for each grid. The model brings out total water availability<br />

in the basin; water consumed by different uses; and water storage in different hydraulic<br />

structures, in soil water zone, and in groundwater aquifer in a river basin.<br />

The present paper gives a brief description of the developed model. Using this<br />

model, it is possible to simulate various past, present or future hydrological scenarios in<br />

a river basin.<br />

UTTAR PRADESH STATE ACTION PLAN ON CLIMATE<br />

CHANGE: WATER MISSION<br />

Ravindra Kumar<br />

State Water Resources Agency, <strong>Lucknow</strong>.<br />

email: ravindra53@yahoo.co.in<br />

While more and more of the natural flow is stored, used or diverted out of the<br />

river, we looked for a set of ameliorative measures that would be implemented to<br />

mitigate impacts of climate change on water resources of the state. These measures<br />

would be scheduled to begin with ensuring 50% water in rivers for maintenance of<br />

minimum flow for ecological and livelihood water requirement, no encroachment in<br />

river flood plain within 500 m (as per HC, Allahabad Orders) towards the quality and<br />

36

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