Uncertainty in Sediment Yield from a Semi-Arid Watershed

From the Proceedings of the 1974 Meetings of the Arizona Section - American Water Resources Assn. and the Hydrology Section - Arizona Academy of Science - April 19-20, 1974, Flagstaff, Arizona === The paper presents a stochastic model for the prediction of sediment yield in a semi -arid watershed ba...

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Main Authors: Smith, J. M., Fogel, M., Duckstein, L.
Other Authors: Systems & Industrial Engineering, University of Arizona, Tucson, Arizona 85721
Language:en_US
Published: Arizona-Nevada Academy of Science 1974
Subjects:
Online Access:http://hdl.handle.net/10150/300468
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spelling ndltd-arizona.edu-oai-arizona.openrepository.com-10150-3004682015-10-23T05:24:29Z Uncertainty in Sediment Yield from a Semi-Arid Watershed Smith, J. M. Fogel, M. Duckstein, L. Systems & Industrial Engineering, University of Arizona, Tucson, Arizona 85721 Watershed Management and Systems & Industrial Engineering, University of Arizona, Tucson, Arizona 85721 Hydrology -- Arizona. Water resources development -- Arizona. Hydrology -- Southwestern states. Water resources development -- Southwestern states. Planning Land management Land use Water resources Land development Conservation Land classification Land resources Natural resources Evaluation Land appraisals Systems analysis Simulation analysis Social aspects Decision making Economics Land use planning From the Proceedings of the 1974 Meetings of the Arizona Section - American Water Resources Assn. and the Hydrology Section - Arizona Academy of Science - April 19-20, 1974, Flagstaff, Arizona The paper presents a stochastic model for the prediction of sediment yield in a semi -arid watershed based on rainfall data and watershed characteristics. Uncertainty stems from each of the random variables used in the model, namely, rainfall amount, storm duration, runoff, and peak flow. Soil Conservation Service formulas are used to compute the runoff and peak flow components of the Universal Soil Loss Equation. A transformation of random variables is used to obtain the distribution function of sediment yield from the joint distribution of rainfall amount and storm duration. The model has applications in the planning of reservoirs and dams where the effective lifetime of the facility may be evaluated in terms of storage capacity as well as the effects of land management on the watershed. Experimental data from the Atterbury watershed is used to calibrate the model and to evaluate uncertainties associated with our uncertain knowledge of the parameters of the joint distribution of rainfall and storm duration. 1974-04-20 text Proceedings 0272-6106 http://hdl.handle.net/10150/300468 Hydrology and Water Resources in Arizona and the Southwest en_US Copyright ©, where appropriate, is held by the author. Arizona-Nevada Academy of Science
collection NDLTD
language en_US
sources NDLTD
topic Hydrology -- Arizona.
Water resources development -- Arizona.
Hydrology -- Southwestern states.
Water resources development -- Southwestern states.
Planning
Land management
Land use
Water resources
Land development
Conservation
Land classification
Land resources
Natural resources
Evaluation
Land appraisals
Systems analysis
Simulation analysis
Social aspects
Decision making
Economics
Land use planning
spellingShingle Hydrology -- Arizona.
Water resources development -- Arizona.
Hydrology -- Southwestern states.
Water resources development -- Southwestern states.
Planning
Land management
Land use
Water resources
Land development
Conservation
Land classification
Land resources
Natural resources
Evaluation
Land appraisals
Systems analysis
Simulation analysis
Social aspects
Decision making
Economics
Land use planning
Smith, J. M.
Fogel, M.
Duckstein, L.
Uncertainty in Sediment Yield from a Semi-Arid Watershed
description From the Proceedings of the 1974 Meetings of the Arizona Section - American Water Resources Assn. and the Hydrology Section - Arizona Academy of Science - April 19-20, 1974, Flagstaff, Arizona === The paper presents a stochastic model for the prediction of sediment yield in a semi -arid watershed based on rainfall data and watershed characteristics. Uncertainty stems from each of the random variables used in the model, namely, rainfall amount, storm duration, runoff, and peak flow. Soil Conservation Service formulas are used to compute the runoff and peak flow components of the Universal Soil Loss Equation. A transformation of random variables is used to obtain the distribution function of sediment yield from the joint distribution of rainfall amount and storm duration. The model has applications in the planning of reservoirs and dams where the effective lifetime of the facility may be evaluated in terms of storage capacity as well as the effects of land management on the watershed. Experimental data from the Atterbury watershed is used to calibrate the model and to evaluate uncertainties associated with our uncertain knowledge of the parameters of the joint distribution of rainfall and storm duration.
author2 Systems & Industrial Engineering, University of Arizona, Tucson, Arizona 85721
author_facet Systems & Industrial Engineering, University of Arizona, Tucson, Arizona 85721
Smith, J. M.
Fogel, M.
Duckstein, L.
author Smith, J. M.
Fogel, M.
Duckstein, L.
author_sort Smith, J. M.
title Uncertainty in Sediment Yield from a Semi-Arid Watershed
title_short Uncertainty in Sediment Yield from a Semi-Arid Watershed
title_full Uncertainty in Sediment Yield from a Semi-Arid Watershed
title_fullStr Uncertainty in Sediment Yield from a Semi-Arid Watershed
title_full_unstemmed Uncertainty in Sediment Yield from a Semi-Arid Watershed
title_sort uncertainty in sediment yield from a semi-arid watershed
publisher Arizona-Nevada Academy of Science
publishDate 1974
url http://hdl.handle.net/10150/300468
work_keys_str_mv AT smithjm uncertaintyinsedimentyieldfromasemiaridwatershed
AT fogelm uncertaintyinsedimentyieldfromasemiaridwatershed
AT ducksteinl uncertaintyinsedimentyieldfromasemiaridwatershed
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