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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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 |
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en_US |
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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 |
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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 |
_version_ |
1718105827372433408 |