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LACE Data Assimilation Working Days 14-16 June 2011, Budapest HARMONIE DA suite at KNMI Jan Barkmeijer With contributions from: Cisco de Bruijn, Siebren de Haan, Gert-Jan Marseille, Emiel van der Plas, and Wim de Rooy. Content. Description KNMI DA suite Monitoring tools
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LACE Data Assimilation Working Days 14-16 June 2011, Budapest HARMONIE DA suite at KNMI Jan Barkmeijer With contributions from: Cisco de Bruijn, Siebren de Haan, Gert-Jan Marseille, Emiel van der Plas, and Wim de Rooy.
Content • Description KNMI DA suite • Monitoring tools • Problems encountered • Future developments
The KNMI Data assimilation suite • Initial run at 15 November 2010, but many changes (experimental status) • since then. • Runs at ECMWF, using hourly boundaries and observation set from a H7.2 • Hirlam suite at KNMI (ectrans is used to tranfer data vice-versa) • Cycling time is 6h and a 24h forecast is produced at 00 and 12 UTC. • Integration area (300x300 gp at 2.5km grid resolution) covers the Netherlands and vertical resolution is 60 levels (Meteo-France definition). Lowest model level around 9m • Harmonie model cycle H36h1.2 with some modifications • Data is processed e.g. at DMI/KNMI for monitoring purposes.
Area definition 200x200 300x300 400x400 500x500
LBC data from Hirlam forecast for both runs RADAR 300x300 400x400
Computation of background error statistics - Used the recipe as described on the Hirlam wiki page for Harmonie Data-assimilation - Central here is the creation of a series of downscaled Harmonie 6h forecasts for 20060920-20061031 at 00 UTC, using 4 members of the ECMWF EPS
Confusion w.r.t. virtual and real temperature (LSPRT) DMI Harmonie suite KNMI old Courtesy Nils Gustafsson
After correction DMI KNMI new
Content • Description KNMI DA suite • Monitoring tools • Problems encountered • Future developments
What data sets are being used (2)? Mode-S drops out
o-a/o-b statistics for April negative bias
Monitoring with KNMI Parametrization Testbed (KPT) 1D column at Cabauw from 3D run
Content • Description KNMI DA suite • Monitoring tools • Problems encountered • Future developments
EDMFM and cloud scheme changes Increase variance computation in the cloud scheme to alleviate the on-off character in the generation of cloud Modis VIS satellite image 13th of May 2008 1315 UTC Cloud cover Cloud cover
Occurrence of negative q in the analysis Also other hydrometeors are affected (e.g. cloud-ice and cloud-water) First-guess Analysis
Impact on 24-h accumulated precipitation original analysis modified
Vertical nesting strategy 1.3hPa 10hPa 0.01hPa
Vertical nesting strategy 1.3hPa 10hPa 0.01hPa Since 1 June 2011 a parallel 3dvar suite runs at ECMWF (cy36h1.3) and with ECMWF boundaries
T+12h forecast for T2m valid 5 June 2011 at 12 UTC HIRLAM LBC ECMWF LBC
RADAR 3DVAR + HIRLAM LBC 400x400 500x500
RADAR 3DVAR + ECMWF LBC 400x400 500x500
FUTURE PLANS - Get radar data-assimilation running - Implementation of a 800x800xL60 Harmonie suite at KNMI, 3dvar with cycling time of 3 hour (or less) - Add more q observations: GPS, Cloud data (e.g. cover) - Develop more tools for monitoring (MetEvaluation) - Coupling with other applications: surge model, LOTOS (air pollution model) - Increase research effort on DA+EPS: + timing/location of convection + 4dvar without nonlinear updates