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TR(BR)-112 : Forecasting of low flows for river Narmada at Mortakka

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dc.contributor.author Kumar, Rakesh
dc.contributor.author Singh, R. D.
dc.date.accessioned 2019-05-21T09:52:27Z
dc.date.available 2019-05-21T09:52:27Z
dc.date.issued 1993
dc.identifier.uri http://117.252.14.250:8080/xmlui/handle/123456789/2431
dc.description.abstract For development of our agriculture based economy and to meet the demands of the growing population; in terms of irrigation, drinking water, hydropower generation and indu-3trial use etc. modelling and forecasting of river flows during non-monsoon months is essential. Efficient management of existing water resources projects and optimal planning of the future projects also attach great importance to low flow modelling and forecasting. Ideally, a distributed model based on the principle of physical laws representing the movement of water through its different phases should be developed for any modelling exercise for low flow forecast. However, it remains a fact that the physical laws for representing the formation and propagation of runoff through its various processes have not yet been perfected. No doubt, for the more complicated problems the use of physically based models acquires a great importance. But the physically based models require extensive data input and enormous computational facilities. On the other hand, there are many problems for which necessary solutions can be obtained with desired degree of accuracy required for the purpose, with relatively less sophisticated, lumped, conceptual or statistical models, which require very limited data generally available in the field. In this study, a statistical model has been used to forecast the low flows (November to May) for the river Narmada at Mortakka, using the monthly data of previous month. To begin with, the forecast of flow from the month of November to May is formulated on the basis of observed data of October for a specific year. The forecast is updated after each month when additional data become available. The observed discharge and forecasts have been compared for the four test years and percentage errors between them have been computed. en_US
dc.language.iso en en_US
dc.publisher National Institute of Hydrology en_US
dc.relation.ispartofseries ;TR(BR)-112
dc.subject Forecasting of low flows en_US
dc.subject Narmada -low flows en_US
dc.subject Narmada at Mortakka en_US
dc.title TR(BR)-112 : Forecasting of low flows for river Narmada at Mortakka en_US
dc.type Technical Report en_US


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