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Uncertain Hydrological Modelling: Application of the Pitman Model in the Great Ruaha River Basin, Tanzania

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dc.creator Tumbo, Madaka
dc.creator Hughes, D. A.
dc.date 2016-05-26T09:11:10Z
dc.date 2016-05-26T09:11:10Z
dc.date 2015
dc.date.accessioned 2018-04-18T11:18:00Z
dc.date.available 2018-04-18T11:18:00Z
dc.identifier Tumbo, M. and Hughes, D.A., 2015. Uncertain hydrological modelling: application of the Pitman model in the Great Ruaha River basin, Tanzania. Hydrological Sciences Journal, 60(11), pp.2047-2061.
dc.identifier http://hdl.handle.net/20.500.11810/2257
dc.identifier 10.1080/02626667.2015.1016948
dc.identifier.uri http://hdl.handle.net/20.500.11810/2257
dc.description Uncertainty analysis has become the standard approach to hydrological modelling, but has yet to be effectively used in practical water resources assessment. This study of the Great Ruaha River basin in Tanzania is based on the use of regional estimates of mean runoff, groundwater recharge and three flow points on flow duration curves (FDCs) to constrain ensemble outputs from the Pitman monthly model using Monte Carlo parameter sampling. The constraint bounds were quantified from gauged data available for 26 sub-basins together with assumptions about the spatial variations in hydrological response using limited physical sub-basin property and climate data. The results are encouraging in that the simulated FDC ranges bracket the observed curves at two gauging stations downstream of many ungauged sub-basins that are important sites for water resources development decision making. Further work is required to refine the constraint bounds, the input parameter sets and climate data and achieve a more robust model of the basin.
dc.language en
dc.publisher Taylor and Francis
dc.subject Uncertainty
dc.subject Hydrological modelling
dc.subject Southern Africa
dc.subject Hydrological constraints
dc.title Uncertain Hydrological Modelling: Application of the Pitman Model in the Great Ruaha River Basin, Tanzania
dc.type Journal Article, Peer Reviewed


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