Slide 1 Bilateral meeting 2011Slide 1, ©ECMWF Status and plans for the ECMWF forecasting System.

Slides:



Advertisements
Similar presentations
Slide 1ECMWF forecast User Meeting -- Reading, June 2006 Verification of weather parameters Anna Ghelli, ECMWF.
Advertisements

Slide 1ECMWF forecast products users meeting – Reading, June 2005 Verification of weather parameters Anna Ghelli, ECMWF.
R. Forbes, 17 Nov 09 ECMWF Clouds and Radiation University of Reading ECMWF Cloud and Radiation Parametrization: Recent Activities Richard Forbes, Maike.
© European Centre for Medium-Range Weather Forecasts Operational and research activities at ECMWF now and in the future Sarah Keeley Education Officer.
ECMWF long range forecast systems
Introduction to parametrization Introduction to Parametrization of Sub-grid Processes Anton Beljaars room 114) What is parametrization?
© Crown copyright Met Office Impact experiments using the Met Office global and regional model Presented by Richard Dumelow to the WMO workshop, Geneva,
C ontacts: Marit Helene Jensen, Norwegian Meteorological Institute, P.O.Box 43 Blindern, N-0313 OSLO, NORWAY. HIRLAM at met.no.
Slide 1 IPWG, Beijing, October 2008 Slide 1 Assimilation of rain and cloud-affected microwave radiances at ECMWF Alan Geer, Peter Bauer, Philippe.
Data assimilation schemes in numerical weather forecasting and their link with ensemble forecasting Gérald Desroziers Météo-France, Toulouse, France.
6 th SMOS Workshop, Lyngby, DK Using TMI derived soil moisture to initialize numerical weather prediction models: Impact studies with ECMWF’s.
Performance Characteristics of a Pseudo-operational Ensemble Kalman Filter April 2006, EnKF Wildflower Meeting Greg Hakim & Ryan Torn University of Washington.
Verification of Numerical Weather Prediction systems employed by the Australian Bureau of Meteorology over East Antarctica during the summer season.
Global Forecast System (GFS) Model Previous called the Aviation (AVN) and Medium Range Forecast (MRF) models. Global model and 64 levels Relatively primitive.
Numerical weather prediction: current state and perspectives M.A.Tolstykh Institute of Numerical Mathematics RAS, and Hydrometcentre of Russia.
Francesca Marcucci, Lucio Torrisi with the contribution of Valeria Montesarchio, ISMAR-CNR CNMCA, National Meteorological Center,Italy First experiments.
UKmet February Hybrid Ensemble-Variational Data Assimilation Development A partnership to develop and implement a hybrid 3D-VAR system –Joint venture.
Slide 1 GIFS-TIGGE 31 August - 2 September 2011 TIGGE at ECMWF David Richardson, Head, Meteorological Operations Section Slide.
WWOSC 2014, Aug 16 – 21, Montreal 1 Impact of initial ensemble perturbations provided by convective-scale ensemble data assimilation in the COSMO-DE model.
On Improving GFS Forecast Skills in the Southern Hemisphere: Ideas and Preliminary Results Fanglin Yang Andrew Collard, Russ Treadon, John Derber NCEP-EMC.
Data assimilation and observing systems strategies Pierre Gauthier Data Assimilation and Satellite Meteorology Division Meteorological Service of Canada.
COSMO General Meeting, Offenbach, 7 – 11 Sept Dependance of bias on initial time of forecasts 1 WG1 Overview
GEWEX GRP10/2011Ⓒ ECMWF Role of products:Imperatives 1, 2, 5 Coherent, consistent, data products (closure) Long time series Order: reprocessed / recalibrated.
Simulation of Intense Convective Precipitation Observed during ARMEX Someshwar Das, R. Ashrit, M. Dasgupta, Someshwar Das 1, R. Ashrit 1, M. Dasgupta 1,
14 th Annual WRF Users’ Workshop. June 24-28, 2013 Improved Initialization and Prediction of Clouds with Satellite Observations Tom Auligné Gael Descombes,
The 2nd International Workshop on GPM Ground Validation TAIPEI, Taiwan, September 2005 GV for ECMWF's Data Assimilation Research Peter
Soil moisture generation at ECMWF Gisela Seuffert and Pedro Viterbo European Centre for Medium Range Weather Forecasts ELDAS Interim Data Co-ordination.
HIRLAM 3/4D-Var developments Nils Gustafsson, SMHI.
Sensitivity Analysis of Mesoscale Forecasts from Large Ensembles of Randomly and Non-Randomly Perturbed Model Runs William Martin November 10, 2005.
Modern Era Retrospective-analysis for Research and Applications: Introduction to NASA’s Modern Era Retrospective-analysis for Research and Applications:
26 th EWGLAM & 11 th SRNWP meetings, Oslo, Norway, 4 th - 7 th October 2004 Stjepan Ivatek-Šahdan RC LACE Data Manager Croatian Meteorological and Hydrological.
Data assimilation, short-term forecast, and forecasting error
MINERVA workshop, GMU, Sep MINERVA and the ECMWF coupled ensemble systems Franco Molteni, Frederic Vitart European Centre for Medium-Range.
Ensemble data assimilation in an operational context: the experience at the Italian Weather Service Massimo Bonavita and Lucio Torrisi CNMCA-UGM, Rome.
EWGLAM Oct Some recent developments in the ECMWF model Mariano Hortal ECMWF Thanks to: A. Beljars (physics), E. Holm (humidity analysis)
Page 1© Crown copyright 2004 SRNWP Lead Centre Report on Data Assimilation 2005 for EWGLAM/SRNWP Annual Meeting October 2005, Ljubljana, Slovenia.
Progress Update of Numerical Simulation for OSSE Project Yongzuo Li 11/18/2008.
DRAFT – Page 1 – January 14, 2016 Development of a Convective Scale Ensemble Kalman Filter at Environment Canada Luc Fillion 1, Kao-Shen Chung 1, Monique.
Page 1 Developments in regional DA Oct 2007 © Crown copyright 2007 Mark Naylor, Bruce Macpherson, Richard Renshaw, Gareth Dow Data Assimilation and Ensembles,
Active/Passive Microwave Observations Provide Essential Climate Variables for Studying Hydrologic Cycle Probably the Greatest Consequences of Our Warming.
Page 1© Crown copyright 2005 DEVELOPMENT OF 1- 4KM RESOLUTION DATA ASSIMILATION FOR NOWCASTING AT THE MET OFFICE Sue Ballard, September 2005 Z. Li, M.
MPO 674 Lecture 2 1/20/15. Timeline (continued from Class 1) 1960s: Lorenz papers: finite limit of predictability? 1966: First primitive equations model.
Vincent N. Sakwa RSMC, Nairobi
A study on the spread/error relationship of the COSMO-LEPS ensemble Purpose of the work  The spread-error spatial relationship is good, especially after.
Simulations of MAP IOPs with Lokal Modell: impact of nudging on forecast precipitation Francesco Boccanera, Andrea Montani ARPA – Servizio Idro-Meteorologico.
Cloudnet Workshop April 2003 A.Tompkins 1 Changes to the ECMWF cloud scheme  Recent package of changes for 25r3:  COMPLETE REWRITE OF NUMERICS FOR CLOUD.
Incrementing moisture fields with satellite observations
COSMO General Meeting 2008, Krakow Modifications to the COSMO-Model Cumulus Parameterisation Scheme (Tiedtke 1989): Implementation and Testing Dimitrii.
1)Consideration of fractional cloud coverage Ferrier microphysics scheme is designed for use in high- resolution mesoscale model and do not consider partial.
© Crown copyright Met Office Predictability and systematic error growth in Met Office MJO predictions Ann Shelly, Nick Savage & Sean Milton, UK Met Office.
Status of the NWP-System & based on COSMO managed by ARPA-SIM COSMO I77 kmBCs from IFSNudgingCINECA COSMO I22.8 kmBCs from COSMO I7 Interpolated from COSMO.
Land-Surface evolution forced by predicted precipitation corrected by high-frequency radar/satellite assimilation – the RUC Coupled Data Assimilation System.
Global vs mesoscale ATOVS assimilation at the Met Office Global Large obs error (4 K) NESDIS 1B radiances NOAA-15 & 16 HIRS and AMSU thinned to 154 km.
OSEs with HIRLAM and HARMONIE for EUCOS Nils Gustafsson, SMHI Sigurdur Thorsteinsson, IMO John de Vries, KNMI Roger Randriamampianina, met.no.
Regional Re-analyses of Observations, Ensembles and Uncertainties of Climate information Per Undén Coordinator UERRA SMHI.
Mesoscale Assimilation of Rain-Affected Observations Clark Amerault National Research Council Postdoctoral Associate - Naval Research Laboratory, Monterey,
Overview of ECMWF, KMA, March 2013 © ECMWF Slide 1 Overview of research and developments at ECMWF Niels Bormann with contributions from Erland Källén,
Implementation of Terrain Resolving Capability for The Variational Doppler Radar Analysis System (VDRAS) Tai, Sheng-Lun 1, Yu-Chieng Liou 1,3, Juanzhen.
The GSI Capability to Assimilate TRMM and GPM Hydrometeor Retrievals in HWRF Ting-Chi Wu a, Milija Zupanski a, Louie Grasso a, Paula Brown b, Chris Kummerow.
ECMWF/EUMETSAT NWP-SAF Satellite data assimilation Training Course Mar 2016.
Indirect impact of ozone assimilation using Gridpoint Statistical Interpolation (GSI) data assimilation system for regional applications Kathryn Newman1,2,
Hybrid Data Assimilation
Recent changes in the ALADIN operational suite
Impact of hyperspectral IR radiances on wind analyses
Sub-seasonal prediction at ECMWF
Global Forecast System (GFS) Model
ECMWF activities: Seasonal and sub-seasonal time scales
NWP Strategy of DWD after 2006 GF XY DWD Feb-19.
Development of an advanced ensemble-based ocean data assimilation approach for ocean and coupled reanalyses Eric de Boisséson, Hao Zuo, Magdalena Balmaseda.
Global Forecast System (GFS) Model
Presentation transcript:

Slide 1 Bilateral meeting 2011Slide 1, ©ECMWF Status and plans for the ECMWF forecasting System

Slide 2 Bilateral meeting 2011Slide 2, ©ECMWF Overview  Performance of the forecasting system  Research highlights:  CY36R2 (22 June 2010): GRIB API and Ensemble Data Assimilation (to initiate the EPS)  CY36R4 (9 November 2010): New physics package, surface EKF, snow analysis,…  CY37R2 (in the pipeline): Ensemble Data Assimilation to provide flow-dependent variances to 4D-Var, reduction of observation error for AMSU-A, GRIB-2 for model level fields

Slide 3 Bilateral meeting 2011Slide 3, ©ECMWF Overview  Performance of the forecasting system  Research highlights:  CY36R2 (22 June 2010): GRIB API and Ensemble Data Assimilation (to initiate the EPS)  CY36R4 (9 November 2010): New physics package, surface EKF, snow analysis,…  CY37R2 (in the pipeline): Ensemble Data Assimilation to provide flow-dependent variances to 4D-Var, reduction of observation error for AMSU-A, GRIB-2 for model level fields

Slide 4 Deterministic forecast headline score Bilateral meeting 2011Slide 4, ©ECMWF

Slide 5 Comparison with other centres: autumn, NH Bilateral meeting 2011Slide 5, ©ECMWF

Slide 6 Bilateral meeting 2011 Precipitation skill Europe D+2 D+4 Slide 6, ©ECMWF

Slide 7 Comparison of TC forecasts from HKO, , western North Pacific Bilateral meeting 2011Slide 7, ©ECMWF

Slide 8 Russian heat wave Bilateral meeting 2011Slide 8, ©ECMWF

Slide 9 Bilateral meeting 2011Slide 9, ©ECMWF Overview  Performance of the forecasting system  Research highlights:  CY36R2 (22 June 2010): GRIB API and Ensemble Data Assimilation (to initiate the EPS)  CY36R4 (9 November 2010): New physics package, surface EKF, snow analysis…  CY37R2 (in the pipeline): Ensemble Data Assimilation to provide flow-dependent variances to 4D-Var, reduction of observation error for AMSU-A, GRIB-2 for model level fields  others

November 2010 IFS cycle 36r4  Selected contents Prognostic rain and snow with more comprehensive cloud microphysics EKF for soil moisture analysis New snow analysis (O-I) Enhancement of all-sky radiance assimilation

Slide 11 New prognostic cloud microphysics scheme WATER VAPOUR CLOUD Liquid/Ice PRECIP Rain/Snow Evaporation Autoconversion Evaporation Condensation CLOUD FRACTION Current Cloud Scheme New Cloud Scheme 2 prognostic cloud variables + w.v. Ice/water diagnostic Fn(T) Diagnostic precipitation 5 prognostic cloud variables + water vapour Ice and water now independent More physically based, greater realism Significant change to degrees of freedom Change to water cycle balances in the model More than double the lines of “cloud” code!

Slide 12 New prognostic cloud microphysics Representation of mixed phase The most significant change in the new scheme is the improved physical representation of the mixed phase. Current scheme: diagnostic fn(T) split between ice and liquid cloud (a crude approximation of the wide range of values observed in reality). New scheme: wide range of supercooled liquid water for a given T. PDF of liquid water fraction of cloud for the diagnostic mixed phase scheme (dashed line) and the prognostic ice/liquid scheme (shading)

Slide 13 A new snow analysis (I) For snow SYNOP reports an satellite based snow cover are assimilated A new 4 km IMS snow cover is assimilated into a new OI analysis replacing Cressman interpolation Here shown is the analysed snow cover Cressman and IMS_24km OI and IMS 4km

Slide 14 Impact of Cycle 36r4 Bilateral meeting 2011Slide 14, ©ECMWF

Slide 15 SEEPS: impact of 36r4 Bilateral meeting 2011Slide 15, ©ECMWF

Slide 16 Bilateral meeting 2011Slide 16, ©ECMWF Overview  Performance of the forecasting system  Research highlights:  CY36R2 (22 June 2010): GRIB API and Ensemble Data Assimilation (to initiate the EPS)  CY36R4 (9 November 2010): New physics package, surface EKF, snow analysis…  CY37R2 (in the pipeline): Ensemble Data Assimilation to provide flow-dependent variances to 4D-Var, reduction of observation error for AMSU-A, GRIB-2 for model level fields  others

In the pipeline: IFS cycle 37R2  Selected contents Increased weight to AMSU-A data Direct use of EDA in 4D-Var Retuning of new physics GRIB-2 for model level fields

Slide 18 Ensemble of Data Assimilations (EDA)  Perturbed observations  Perturbed SSTs  Stochastic physics X0X0 X +12h 4DVAR Δx2Δx2 Δx1Δx1 Δx3Δx3 Δx4Δx4 Ensemble initial perturbations →

Slide 19 EDA – flow dependent variances Standard deviation of zonal wind component at ~850hPa and p msl ms -1 9h forecasts 23/ UTC 24/ UTC

Slide 20 Impact of Cycle 37R2 Bilateral meeting 2011Slide 20, ©ECMWF NH SH ZVW

Slide 21 Bilateral meeting 2011Slide 21, ©ECMWF Overview  Performance of the forecasting system  Research highlights:  CY36R2 (22 June 2010): GRIB API and Ensemble Data Assimilation (to initiate the EPS)  CY36R4 (9 November 2010): New physics package, surface EKF, snow analysis…  CY37R2 (in the pipeline): Ensemble Data Assimilation to provide flow-dependent variances to 4D-Var, reduction of observation error for AMSU-A, GRIB-2 for model level fields  Others (small selection)

Slide 22 Research Department Annual Plan 2011Slide 22 Main research/development topics 2011:  Ensemble data assimilation methods (EDA, EKF)  Weak constraint, long window 4D-Var  Vertical resolution increase  Numerical experimentation into the “grey zone”  Improved physical parameterizations  Implement NEMO ocean model and NEMOVAR in EPS  Seasonal forecasting system 4  ERA-CLIM  MACC in Near-Real-Time  IFS maintenance and optimisation (cycles, code, scripts)  Object Oriented Prediction System

Slide 23 One concern: Speed-up of 4D-Var Nodes

Slide 24 Ensemble Kalman filter development Bilateral meeting 2011Slide 24, ©ECMWF