Program Description and User Manual for SSAR Streamflow Synthesis and Reservoir Regulation PDF Download

Author:
Publisher:
ISBN:
Category : Reservoirs
Languages : en
Pages : 188

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Book Description

Author: Etats-Unis.Army Engineer Division.North Pacific
Publisher:
ISBN:
Category :
Languages : en
Pages : 188

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Book Description

Author: U.S. Army Engineer Division, North Pacific
Publisher:
ISBN:
Category :
Languages : en
Pages : 201

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Book Description

Author: United States. Army. Corps of Engineers
Publisher:
ISBN:
Category : Reservoirs
Languages : en
Pages : 188

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Book Description

Author: United States. Army. Corps of Engineers. North Pacific Division
Publisher:
ISBN:
Category : Reservoirs
Languages : en
Pages : 236

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Book Description

Author: United States. Army. Corps of Engineers. North Pacific Division
Publisher:
ISBN:
Category : Reservoirs
Languages : en
Pages : 188

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Book Description

Author: Kenneth N. Brooks
Publisher:
ISBN:
Category : Hydrology
Languages : en
Pages : 188

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Book Description

Author: David M. Rockwood
Publisher:
ISBN:
Category : COSSARR (Computer program)
Languages : en
Pages : 108

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Book Description

Author: United States. Army. Corps of Engineers
Publisher:
ISBN:
Category :
Languages : en
Pages : 200

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Book Description

Author: Maria Margaretha de Groen
Publisher: CRC Press
ISBN: 9789058093783
Category : Science
Languages : en
Pages : 240

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Book Description
The book presents improved equations for monthly water resources models, in particular for interception and transpiration. Most of the existing monthly models do not make a distinction between interception and transipiration, while this distinction is very important for management purposes. Interception is direct feedback to the atmosphere, important to sustain rainfall. Transpiration is a good indicator for plant growth and biomass production. This distinction also contributes to the estimation of recharge and therewith of runoff.;The derivations are based on the Markov theory for the occurrence of rain-days. The methodology can be used on the basis of an analysis of a few time series of daily data, at a spatial scale of 300km and not necessarily of the same period as the monthly data. Zimbabwe served as the case study, but derived equations can be used worldwide as long as the relationship between the monthly rainfall and the mean number of rain-days can be established.