Systematic Errors in Weather and Climate Models: Nature, Origins, and Way Forward
Bulletin of the American Meteorological Society (2017)
Stochastic representations of model uncertainties at ECMWF: state of the art and future vision
Quarterly Journal of the Royal Meteorological Society Wiley 143:707 (2017) 2315-2339
Abstract:
Members in ensemble forecasts differ due to the representations of initial uncertainties and model uncertainties. The inclusion of stochastic schemes to represent model uncertainties has improved the probabilistic skill of the ECMWF ensemble by increasing reliability and reducing the error of the ensemble mean. Recent progress, challenges and future directions regarding stochastic representations of model uncertainties at ECMWF are described in this paper. The coming years are likely to see a further increase in the use of ensemble methods in forecasts and assimilation. This will put increasing demands on the methods used to perturb the forecast model. An area that is receiving a greater attention than 5 to 10 years ago is the physical consistency of the perturbations. Other areas where future efforts will be directed are the expansion of uncertainty representations to the dynamical core and to other components of the Earth system as well as the overall computational efficiency of representing model uncertainty.Evaluation of Thunderstorm Predictors for Finland Using Reanalyses and Neural Networks
Journal of Applied Meteorology and Climatology American Meteorological Society 56:8 (2017) 2335-2352
The impact of stochastic parametrisations on the representation of the Asian summer monsoon
Climate Dynamics Springer 50:5-6 (2017) 2269-2282
Abstract:
The impact of the stochastic schemes Stochastically Perturbed Parametrisation Tendencies (SPPT) and Stochastic Kinetic Energy Backscatter Scheme (SKEBS) on the representation of interannual variability in the Asian summer monsoon is examined in the coupled climate model CCSM4. The Webster–Yang index, measuring anomalies of a specified wind-shear index in the monsoon region, is used as a metric for monsoon strength, and is used to analyse the output of three model integrations: one deterministic, one with SPPT, and one with SKEBS. Both schemes show improved variability, which we trace back to improvements in the El Niño-Southern Oscillation (ENSO) and the Indian Ocean Dipole (IOD). SPPT improves the representation of ENSO and through teleconnections thereby the monsoon, supporting previous work on the benefits of this scheme on the model climate. SKEBS also improves monsoon variability by way of improving the representation of the IOD, in particular by breaking an overly strong coupling to ENSO.Introducing independent patterns into the Stochastically Perturbed Parametrisation Tendencies (SPPT) scheme
Quarterly Journal of the Royal Meteorological Society Wiley 143:706 (2017) 2168-2181