2021
DOI: 10.1016/j.atmosres.2021.105571
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Potential of stochastic methods for improving convection-permitting ensemble forecasts of extreme events over the Western Mediterranean

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Cited by 8 publications
(13 citation statements)
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“…Stanford et al (2019) showed that perturbing the ice microphysics parameters involved in mass-size and fallspeed-size relationships using the SPP (Stochastically Perturbed Parameterization; Ollinaho et al, 2017) scheme resulted in significant impacts on the variability of ice cloud optical depth, rain-rate and precipitation in ensemble simulations of deep convection events. Similarly, Hermoso et al (2021) demonstrated that the Random Parameters (RP) scheme (McCabe et al, 2016) applied to several microphysics parameters in a two-moment bulk microphysics scheme significantly increased ensemble variability of convective storm evolution for the studied case. Thompson et al (2021) reported important localized impacts on the precipitation properties including changes to maximum hail-size from perturbing only two microphysics parameters using the SPP scheme.…”
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confidence: 85%
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“…Stanford et al (2019) showed that perturbing the ice microphysics parameters involved in mass-size and fallspeed-size relationships using the SPP (Stochastically Perturbed Parameterization; Ollinaho et al, 2017) scheme resulted in significant impacts on the variability of ice cloud optical depth, rain-rate and precipitation in ensemble simulations of deep convection events. Similarly, Hermoso et al (2021) demonstrated that the Random Parameters (RP) scheme (McCabe et al, 2016) applied to several microphysics parameters in a two-moment bulk microphysics scheme significantly increased ensemble variability of convective storm evolution for the studied case. Thompson et al (2021) reported important localized impacts on the precipitation properties including changes to maximum hail-size from perturbing only two microphysics parameters using the SPP scheme.…”
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confidence: 85%
“…The PR scheme (Hermoso et al, 2021;McCabe et al, 2016) assumes no spatial variability of the parameters and makes use of the uniform distribution for the stochastic variability according to , where 𝐴𝐴 𝐴𝐴 * would be a large value applicable to all parameters. The RP scheme and this configuration are not exact equivalents due to approximating the uniform distribution by the Normal with a large variance, but the correspondence would be close for all practical purposes assuming application of the appropriate boundary conditions (the range of parameter values).…”
Section: Appendix A: Relationship Between Generalized Linear Gaussian...mentioning
confidence: 99%
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“…As a result, the SP schemes produce physically-based and physically-consistent stochastic variability to the tendencies of the resolved states. Evaluations of the SP schemes in global and regional models have shown positive impacts on the ensemble prediction skill of various degrees depending on the prediction time range, the modeling system, and verification variables (Christensen et al, 2015;Hermoso et al, 2021;Jankov et al, 2017;Leutbecher et al, 2017;McCabe et al, 2016;Ollinaho et al, 2017;Stanford et al, 2019;Thompson et al, 2021;Wang et al, 2019). In comparison to the SPPT, the impacts of the SP schemes on ensemble spread were found to be smaller, but adding value when the two approaches were combined (Christensen et al, 2015;Hermoso et al, 2021;Jankov et al, 2019;Ollinaho et al, 2017).…”
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confidence: 99%