2016
DOI: 10.1061/(asce)wr.1943-5452.0000701
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Synthetic Drought Scenario Generation to Support Bottom-Up Water Supply Vulnerability Assessments

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Cited by 87 publications
(69 citation statements)
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“…In this study the Classification and Regression Tree (CART) method (Breiman et al, ) was used for scenario discovery. Alternative scenario discovery methods include the Patient Rule Induction Method (PRIM) (Guivarch et al, ; Kwakkel, ; Kwakkel & Jaxa‐Rozen, ), support vector classification (Herman et al, ), and logistic regression (Quinn, ). Lempert et al () provide a detailed description of CART and PRIM and evaluate their performance for different test cases.…”
Section: Methodology and Exploratory Modelingmentioning
confidence: 99%
“…In this study the Classification and Regression Tree (CART) method (Breiman et al, ) was used for scenario discovery. Alternative scenario discovery methods include the Patient Rule Induction Method (PRIM) (Guivarch et al, ; Kwakkel, ; Kwakkel & Jaxa‐Rozen, ), support vector classification (Herman et al, ), and logistic regression (Quinn, ). Lempert et al () provide a detailed description of CART and PRIM and evaluate their performance for different test cases.…”
Section: Methodology and Exploratory Modelingmentioning
confidence: 99%
“…Natural variability is commonly represented as synthetic climate time-series data obtained from a stochastic weather generator (Steinschneider & Brown, 2013). However, in some cases, it can be desirable to sample natural variability in hydrological conditions directly using a synthetic streamflow generator (Borgomeo, Farmer, & Hall, 2015;Henley, 2012;Herman et al, 2010) , 1979). LHS samples are be obtained by dividing the continuous uncertainty range of each factor into n equal intervals and generating an n x m matrix, where each factor interval is sampled exactly once.…”
Section: Phase 2: Vulnerability Analysismentioning
confidence: 99%
“…Reporting metrics of risk requires extensive and explicit simulation of hydrological variability, extending well beyond historic droughts to include worse than observed conditions. The methodologies are available to do this either via stochastic streamflow (Borgomeo et al, ; Herman et al, ) and groundwater (Mackay et al, ; Prudhomme et al, ) simulation, or via regional climate simulations (Guillod et al, ) or weather generators (Glenis et al, ; Steinschneider & Brown, ) coupled with rainfall‐runoff and groundwater models. For spatially extensive systems this will involve consideration of spatial variability in the simulations (Serinaldi, ).…”
Section: The Frameworkmentioning
confidence: 99%