Literature DB >> 33362988

Assessing development and climate variability impacts on water resources in the Zambezi River basin: Initial model calibration, uncertainty issues and performance.

D A Hughes1, S Mantel1, F Farinosi2.   

Abstract

STUDY REGION: : The Zambezi River basin, one of the most important water resources in sub-Saharan Africa from both a water supply and hydro-power generation perspective. STUDY FOCUS: : Calibration of two hydrological models (Pitman and WEAP) that have been established for 76 sub-basins covering the total basin area of about 1 350 000 km2. The longer-term purpose of establishing the models is to facilitate scenario analyses of future conditions related to changes in water use and management as well as climate change. NEW HYDROLOGICAL INSIGHTS FOR THE REGION: : While there are many (inevitable) uncertainties in the data used, as well as the models and calibrated parameter sets themselves, the results suggest that the models are generally fit for purpose in terms of evaluating future changes. There are, however, some parts of the basin where the reduction of identified uncertainties would lead to improved models and greater confidence in their future use. One of sources of uncertainty relates to the existence of several large wetland areas that have impacts on downstream flows, but are difficult to simulate due to the relatively poor existing understanding of the dynamics of water exchange between the river channels and the wetland storage areas.
© 2020 The Author(s).

Entities:  

Keywords:  Calibration; Hydrological models; Model uncertainties; Zambezi River basin

Year:  2020        PMID: 33362988      PMCID: PMC7756318          DOI: 10.1016/j.ejrh.2020.100765

Source DB:  PubMed          Journal:  J Hydrol Reg Stud        ISSN: 2214-5818


  1 in total

1.  A global streamflow reanalysis for 1980-2018.

Authors:  Lorenzo Alfieri; Valerio Lorini; Feyera A Hirpa; Shaun Harrigan; Ervin Zsoter; Christel Prudhomme; Peter Salamon
Journal:  J Hydrol X       Date:  2020-01
  1 in total

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