“A view of the 2 nd and 3 rd August COPE cases using storm-permitting ensemble MOGREPS-UK” S. Dey Supervisors: R. Plant, N. Roberts and S. Migliorini COPE.

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Presentation transcript:

“A view of the 2 nd and 3 rd August COPE cases using storm-permitting ensemble MOGREPS-UK” S. Dey Supervisors: R. Plant, N. Roberts and S. Migliorini COPE science meeting 29/04/2014

Cases [mm/hr] 2 nd August 16Z3 nd August 18Z – Nimrod radar derived rain rates

MOGREPS-UK – 2.2km resolution – Convection permitting – 12 members – Downscaled from MOGREPS-G – Methods not specific to MOGREPS Methods of ensemble characterization 1.Spatial 2.Vertical correlations

Ensemble mean – Not physically representative Motivation cv Scale dependence – Faster error growth at smaller scales (Hohenegger and Schär 2007, BAMS) – Need ensembles at convective scale Individual forecasts Ensemble mean Physical meaning

Method 1: spatial analysis Over what spatial scales are the forecasts acceptably similar? ?=?= L A B – Varies point by point – Measure of spatial agreement – Apply to different variables and different vertical levels.

Spatial comparisons [ km] [mm/hr] Ensemble scalesRadar rain rates Ensemble-radar scales 2 nd August 16Z 3 nd August 14Z

Method 12 3D variables (A,B) Horizontal divergence Horizontal wind speed Cloud fraction in each layer Specific humidity Temperature Surface Rain rates- Temporal correlations ( C ) ABC z

Correlations: 2 nd August, 14Z Convergence Divergence -ve correlation +ve correlation 1 grid points (2.2km)13x13 grid points (28.6km)21x21 grid points (46.2km)

Summary >32 Mesoscale Convective System 27/07/2013 Scattered convection 29/07/2013 Bands of thunderstorms 23/07/ th JulyOrganized thunderstorms (NOT COPE CASE) 23 rd JulyBands of thunderstorms (IOP 5) 27 th JulyMCS (IOP 7) 29 th JulyConvective showers (IOP 9) 2 nd AugustConvection along SW peninsula (IOP 10) 3 rd AugustConvection along SW peninsula (IOP 11)

Main questions Can we develop scale appropriate, multivariate and physically meaningful methods for obtaining information from convection permitting ensembles? Techniques useful for assessing model changes – Increased membership by time lagging? – Including the UKV forecast in the ensemble? – Global ensemble – More statistical approach Other interesting investigations? – Verification of spatial scales for different variables – Comparison of correlation results with observations