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Tracking down the origin of NWP model uncertainty : coarse-graining studies
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dc.contributor.authorShutts, Glennes_ES
dc.contributor.authorCallado Pallarés, Alfonses_ES
dc.date.accessioned2017-08-02T07:41:32Z-
dc.date.available2017-08-02T07:41:32Z-
dc.date.issued2011-
dc.identifier.citationWorkshop on representing model uncertainty and error in numerical weather and climate prediction (2011)es_ES
dc.identifier.urihttp://hdl.handle.net/20.500.11765/7373-
dc.descriptionPonencia presentada en: Workshop on representing model uncertainty and error in numerical weather and climate prediction celebrado del 20 al 24 de junio de 2011 en Reading, Inglaterra.es_ES
dc.description.abstractCurrent implementations of the perturbed parametrization tendency method for representing uncertainty rely on ad hoc assumptions about its magnitude and its spatial and temporal correlation scales. Ideally one would use observational data to ascertain the statistical character of parametrization tendency errors and use the resulting probability distribution functions to devise and calibrate the perturbed tendency approach. The reality is that observations rarely have the coverage, representativity and accuracy to form a useful comparison with model data. A less satisfactory alternative is to use high resolution modelling to provide a ‘truth’ simulation and then compare this with an equivalent but lower resolution simulation. Tendency fields from both simulations are coarse-grained to a resolution compatible with the assumed horizontal correlation scale in the perturbed tendency method and the bias-corrected differences between them are used to quantify statistical uncertainty. Early results using the ECMWF IFS forecasts appear to show that the variance of the coarse-grained tendency differences is proportional to the tendency in the lower-resolution forecast. However the current perturbed parametrization tendency scheme at ECMWF assumes that the standard deviation of the perturbations is proportional to the tendency itself. Probability distribution functions of the high-resolution model tendency, sub-sampled by narrow ranges of the low-resolution model tendency, seem to be consistent with an underlying Poisson process.es_ES
dc.language.isoenges_ES
dc.rightsLicencia CC: Reconocimiento–NoComercial–SinObraDerivada CC BY-NC-NDes_ES
dc.subjectParametrizationes_ES
dc.subjectNumerical weather predictiones_ES
dc.subjectEnsemble forecastinges_ES
dc.titleTracking down the origin of NWP model uncertainty : coarse-graining studieses_ES
dc.typeinfo:eu-repo/semantics/conferenceObjectes_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
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