COPS - FRANCE

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COPS - FRANCE COPS - FRANCE A, Toulouse PSL, Paris NRM, Toulouse aMP, Clermont-Ferrand A A N N R R Agence nationale de la recherche

description

A N R. Agence nationale de la recherche. COPS - FRANCE. LA, Toulouse IPSL, Paris CNRM, Toulouse LaMP, Clermont-Ferrand. Meso-NH IOP 8B. COPS - France. Instrumentation on supersite V Lidar Juan Cuesta Radar Joël Van Baelen Reinforcement of the GPS network Cédric Champollion - PowerPoint PPT Presentation

Transcript of COPS - FRANCE

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COPS - FRANCECOPS - FRANCE

LA, ToulouseIPSL, ParisCNRM, ToulouseLaMP, Clermont-Ferrand

AANNRRAgence nationale de la

recherche

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COPS - France Instrumentation on supersite V

Lidar Juan Cuesta Radar Joël Van Baelen

Reinforcement of the GPS network Cédric Champollion

Safire Falcon / Leandre II operation Cyrille Flamant

Numerical modelling Jean-Pierre Chaboureau Evelyne Richard

High-resolution assimilation Pierre Brousseau Olivier Caumont

Meso-NHMeso-NH

IOP 8BIOP 8B

Other case studies …see ChaboureauOther case studies …see Chaboureau

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DLR Poldirad at Waltenheim sur Zorn

14:00 UTC14:00 UTC 14:20 UTC14:20 UTC 14:40 UTC14:40 UTC 15:00 UTC15:00 UTC

15:20 UTC15:20 UTC 15:40 UTC15:40 UTC 16:00 UTC16:00 UTC

IOP 8B : 15 July 2007IOP 8B : 15 July 2007

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Montancy radar observationsMontancy radar observations

(2dBz contour – PPI 1°)(2dBz contour – PPI 1°)

Meso-NH (2km - ECMWF driven)Meso-NH (2km - ECMWF driven)

(0.1 mm precip contour)(0.1 mm precip contour)

12:15 – 13:0012:15 – 13:0013:15 – 14:0013:15 – 14:00

14:15 – 15:0014:15 – 15:0015:15 – 16:0015:15 – 16:00

Time evolution : Time evolution : Observation versus simulationObservation versus simulation

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12:15 – 13:0012:15 – 13:0013:15 – 14:0013:15 – 14:00

14:15 – 15:0014:15 – 15:0015:15 – 16:0015:15 – 16:00

Time evolution :Time evolution :Observation versus simulationObservation versus simulation

Meso-NHMeso-NH (2km - ARPEGE driven) (2km - ARPEGE driven)(0.1 mm precip contour)(0.1 mm precip contour)

Montancy radarMontancy radar observations observations(2dBz contour – PPI 1°)(2dBz contour – PPI 1°)

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Montancy radarMontancy radar observations observations

(2dBz contour – PPI 1°)(2dBz contour – PPI 1°)

Meso-NH Meso-NH ((2km2km - ECMWF driven) - ECMWF driven)

(0.1 mm precip contour)(0.1 mm precip contour)

12:15 – 13:0012:15 – 13:0013:15 – 14:0013:15 – 14:00

14:15 – 15:0014:15 – 15:0015:15 – 16:0015:15 – 16:00

Time evolution (close up view) : Time evolution (close up view) : Observation versus Observation versus simulationsimulation

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Montancy radarMontancy radar observations observations

(2dBz contour – PPI 1°)(2dBz contour – PPI 1°)

Meso-NHMeso-NH ( (500m500m - ECMWF driven) - ECMWF driven)

(0.1 mm precip contour)(0.1 mm precip contour)

12:15 – 13:0012:15 – 13:0013:15 – 14:0013:15 – 14:00

14:15 – 15:0014:15 – 15:0015:15 – 16:0015:15 – 16:00

Time evolution : Time evolution : Observation versus simulationObservation versus simulation

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2km Meso-NH simulation : 13:00 UTCSurface streamlines / CAPE / precipitation ( )

ECMWFECMWF ARPEGEARPEGE

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2km Meso-NH simulation : 14:00 UTCSurface streamlines / CAPE / precipitation ( )

ECMWFECMWF ARPEGEARPEGE

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Vertical cross sections of reflectivity along storm propagationVertical cross sections of reflectivity along storm propagation

Meso-NH (2km - Meso-NH (2km - ECMWF ECMWF driven)driven)

Meso-NH (2km - Meso-NH (2km - ARPEGEARPEGE driven) driven)

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Conlusion High sensitivity to initial conditions More convection with ARPEGE CI than with ECMWF CI (… with the truth in

between!) Earlier triggering with ARPEGE CI (too early) but a more realistic life cycle Major role of the low-level convergence

No significant improvement when : Resolution is increased from 2km to 500m(Triggering occurs too much upwind 3D turbulence is accounted for(very weak impact)

More on that topic : Trentmann (U. Mainz) and More on that topic : Trentmann (U. Mainz) and Cardwell (U. Manchester)Cardwell (U. Manchester)

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Méso-NH (500m – ECMWF driven)1dBz reflectivity contour

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12:15 – 13:0012:15 – 13:0013:15 – 14:0013:15 – 14:00

14:15 – 15:0014:15 – 15:0015:15 – 16:0015:15 – 16:00

Montancy Radar ObservationsMontancy Radar Observations

Meso-NH simulation (ECMWF)Meso-NH simulation (ECMWF) Meso-NH simulation (ARPEGE)Meso-NH simulation (ARPEGE)

15/07/0715/07/07

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12:15 – 13:0012:15 – 13:0013:15 – 14:0013:15 – 14:00

14:15 – 15:0014:15 – 15:0015:15 – 16:0015:15 – 16:00

Time evolution :Time evolution :Impact of the turbulence Impact of the turbulence scheme (1D/3D)scheme (1D/3D)

Meso-NH (2km – Meso-NH (2km – 1D turbulence1D turbulence))(0.1 mm precip contour)(0.1 mm precip contour)

Meso-NH (2km – Meso-NH (2km – 3D turbulence3D turbulence))(0.1 mm precip contour)(0.1 mm precip contour)

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12:15 – 13:0012:15 – 13:0013:15 – 14:0013:15 – 14:00

14:15 – 15:0014:15 – 15:0015:15 – 16:0015:15 – 16:00

Time evolution :Time evolution :Impact of the initial / forcing Impact of the initial / forcing conditions conditions

Meso-NH (2km - Meso-NH (2km - ARPEGEARPEGE driven) driven)(0.1 mm precip contour)(0.1 mm precip contour)

Meso-NH (2km - Meso-NH (2km - ECMWFECMWF driven) driven)(0.1 mm precip contour)(0.1 mm precip contour)

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Meso-NH (Meso-NH (500m500m – ECMWF driven) – ECMWF driven) (0.1 mm precip contour)(0.1 mm precip contour)

12:15 – 13:0012:15 – 13:0013:15 – 14:0013:15 – 14:00

14:15 – 15:0014:15 – 15:0015:15 – 16:0015:15 – 16:00

Time evolution : Time evolution : Impact of the resolution Impact of the resolution (2km/ 500m) (2km/ 500m)

Meso-NH (Meso-NH (2km 2km - ECMWF driven)- ECMWF driven)(0.1 mm precip contour)(0.1 mm precip contour)

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Meso-NH Forecasts http://mesonh.aero.obs-mip.fr/mesonh/cops/

• 3 domains (32, 8, and 2 km) with 2-way interaction. •Vertical grid with 50 levels up to 20 km with a grid length varying from 60 m to 600 m.• Initial and coupling fields with ECMWF operational forecasts• 30 h forecast starting at 00 UTC• Parameterization schemes: o 1.5-order turbulence scheme o ECMWF radiation package o ISBA surface scheme o Mixed-phase bulk microphysics: cloud, rain, ice, snow, graupel, and hail (hail is simulated for the inner model only) o Deep and shallow convection scheme for the 32 and 8 km models only

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Outline

Basic model evaluation Raingauges precipitation measurementsMeteosat IR observations

An example of an isolated thunderstorm forecast 15 July

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24h precipitation (P30h – P06h): 04 July 2007 (J185)24h precipitation (P30h – P06h): 04 July 2007 (J185)

Precip evaluation :Precip evaluation :

• BW stationsBW stations

• MF automatic MF automatic stationsstations

• Model fields Model fields interpolated at rain interpolated at rain gauge location gauge location

Thanks to M. Kunz Thanks to M. Kunz and P. Limnaios and P. Limnaios

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Time evolution of the spatially averaged 24h precip.

Julian day (July/August)Julian day (July/August)

P30

h-P

06h

(mm

)P

30h-

P06

h (m

m)

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Time evolution of the spatially averaged 24h precip.