2023
DOI: 10.5194/gmd-16-2055-2023
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Evaluation of bias correction methods for a multivariate drought index: case study of the Upper Jhelum Basin

Abstract: Abstract. Bias correction (BC) is often a necessity to improve the applicability of global and regional climate model (GCM and RCM, respectively) outputs to impact assessment studies, which usually depend on multiple potentially dependent variables. To date, various BC methods have been developed which adjust climate variables separately (univariate BC) or jointly (multivariate BC) prior to their application in impact studies (i.e., the component-wise approach). Another possible approach is to first calculate … Show more

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Cited by 4 publications
(2 citation statements)
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References 98 publications
(118 reference statements)
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“…For example, the eqm is a non‐parametric method using empirical CDFs, whereas the gpqm and the pqm are the parametric methods employing probability distributions (e.g., generalized Pareto, gamma, and Gaussian) for the CDFs. The dqm initially removes a long‐term linear trend before applying standard quantile mapping to detrended data (Cannon et al, 2015); the qdm is similar to the dqm but it preserves the model‐projected relative changes and apply quantile mapping to correct the remaining biases (Ansari et al, 2022). Other methods (i.e., loci, mva, ptr, scaling, and variance) employ linear transformation or scaling factors to match the statistical properties (i.e., mean, variance or standard deviation) for bias correction (Cannon et al, 2015; Fang et al, 2015; Teutschbein & Seibert, 2012).…”
Section: Methodsmentioning
confidence: 99%
“…For example, the eqm is a non‐parametric method using empirical CDFs, whereas the gpqm and the pqm are the parametric methods employing probability distributions (e.g., generalized Pareto, gamma, and Gaussian) for the CDFs. The dqm initially removes a long‐term linear trend before applying standard quantile mapping to detrended data (Cannon et al, 2015); the qdm is similar to the dqm but it preserves the model‐projected relative changes and apply quantile mapping to correct the remaining biases (Ansari et al, 2022). Other methods (i.e., loci, mva, ptr, scaling, and variance) employ linear transformation or scaling factors to match the statistical properties (i.e., mean, variance or standard deviation) for bias correction (Cannon et al, 2015; Fang et al, 2015; Teutschbein & Seibert, 2012).…”
Section: Methodsmentioning
confidence: 99%
“…This approach has the advantage of circumventing the difficulties associated with correcting the dependence between different climate variables, which is not accounted for by univariate BC methods. Some studies use this method to calculate indices such as the SPEI (Standardized Precipitation Evapotranspiration Index; Ansari et al 2022) or the FWI (Fire Weather Index; Casanueva et al 2018), which…”
Section: 4mentioning
confidence: 99%