S.Alessandrini, S.Sperati, G.Decimi,

Slides:



Advertisements
Similar presentations
Medium-range Ensemble Streamflow forecast over France F. Rousset-Regimbeau (1), J. Noilhan (2), G. Thirel (2), E. Martin (2) and F. Habets (3) 1 : Direction.
Advertisements

ECMWF long range forecast systems
KMA will extend medium Range forecast from 7day to 10 day on Oct A post processing technique, Ensemble Model Output Statistics (EMOS), was developed.
Initialization Issues of Coupled Ocean-atmosphere Prediction System Climate and Environment System Research Center Seoul National University, Korea In-Sik.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Improving COSMO-LEPS forecasts of extreme events with.
CHOICES FOR HURRICANE REGIONAL ENSEMBLE FORECAST (HREF) SYSTEM Zoltan Toth and Isidora Jankov.
A 33 yr climatology of extreme wind power generation events in Great Britain EMS Annual Meeting & ECAM (2013) Dirk Cannon a, David Brayshaw a, John Methven.
Statistics, data, and deterministic models NRCSE.
1 Ensembles of Nearest Neighbor Forecasts Dragomir Yankov, Eamonn Keogh Dept. of Computer Science & Eng. University of California Riverside Dennis DeCoste.
Ensemble Post-Processing and it’s Potential Benefits for the Operational Forecaster Michael Erickson and Brian A. Colle School of Marine and Atmospheric.
A Regression Model for Ensemble Forecasts David Unger Climate Prediction Center.
ERCIM Environmental Modelling WG meeting Paris, 27 May 2009 Exploration of Wind Farm Power Output Using Meteorological Predictions Simon Lambert*, Maurice.
Comparison of hybrid ensemble/4D- Var and 4D-Var within the NAVDAS- AR data assimilation framework The 6th EnKF Workshop May 18th-22nd1 Presenter: David.
Multi-Model Ensembling for Seasonal-to-Interannual Prediction: From Simple to Complex Lisa Goddard and Simon Mason International Research Institute for.
Performance of the MOGREPS Regional Ensemble
SRNWP workshop - Bologne Short range ensemble forecasting at Météo-France status and plans J. Nicolau, Météo-France.
A Radar Data Assimilation Experiment for COPS IOP 10 with the WRF 3DVAR System in a Rapid Update Cycle Configuration. Thomas Schwitalla Institute of Physics.
Ensemble-variational sea ice data assimilation Anna Shlyaeva, Mark Buehner, Alain Caya, Data Assimilation and Satellite Meteorology Research Jean-Francois.
Application of a Multi-Scheme Ensemble Prediction System for Wind Power Forecasting in Ireland.
Observing Strategy and Observation Targeting for Tropical Cyclones Using Ensemble-Based Sensitivity Analysis and Data Assimilation Chen, Deng-Shun 3 Dec,
Improving WAsP predictions in (too) complex terrain
WWOSC 2014, Aug 16 – 21, Montreal 1 Impact of initial ensemble perturbations provided by convective-scale ensemble data assimilation in the COSMO-DE model.
ISDA 2014, Feb 24 – 28, Munich 1 Impact of ensemble perturbations provided by convective-scale ensemble data assimilation in the COSMO-DE model Florian.
Ensemble Predictions: Understanding Uncertainties Lars Landberg Wind Energy Department Risø National Laboratory DTU Denmark Gregor Giebel, Jake Badger,
© British Crown copyright 2014 Met Office A comparison between the Met Office ETKF (MOGREPS) and an ensemble of 4DEnVars Marek Wlasak, Stephen Pring, Mohamed.
Improving Ensemble QPF in NMC Dr. Dai Kan National Meteorological Center of China (NMC) International Training Course for Weather Forecasters 11/1, 2012,
MODEL OUTPUT STATISTICS (MOS) TEMPERATURE FORECAST VERIFICATION JJA 2011 Benjamin Campbell April 24,2012 EAS 4480.
1 An overview of the use of reforecasts for improving probabilistic weather forecasts Tom Hamill NOAA / ESRL, Physical Sciences Div.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss Cost Efficient Use of COSMO-LEPS Reforecasts Felix Fundel,
Verification of Global Ensemble Forecasts Fanglin Yang Yuejian Zhu, Glenn White, John Derber Environmental Modeling Center National Centers for Environmental.
Probabilistic Forecasting. pdfs and Histograms Probability density functions (pdfs) are unobservable. They can only be estimated. They tell us the density,
OWEMES 2006, Civitavecchia, Italy Accuracy of Short-Term Predictions for 25 GW Offshore Wind Power in Germany Jens Tambke, L. v. Bremen, N. Saleck, U.
Short-Range Ensemble Prediction System at INM José A. García-Moya SMNT – INM 27th EWGLAM & 12th SRNWP Meetings Ljubljana, October 2005.
Plans for Short-Range Ensemble Forecast at INM José A. García-Moya SMNT – INM Workshop on Short Range Ensemble Forecast Madrid, October,
WWRP_WSN05, Toulouse, 5-9 September 2005 / 1 Pertti Nurmi Juha Kilpinen Sigbritt Näsman Annakaisa Sarkanen ( Finnish Meteorological.
Stratosphere-Troposhere Coupling in Dynamical Seasonal Predictions Bo Christiansen Danish Meteorological Institute.
Application of an adaptive radiative transfer parameterisation in a mesoscale numerical weather prediction model DWD Extramural research Annika Schomburg.
An Examination Of Interesting Properties Regarding A Physics Ensemble 2012 WRF Users’ Workshop Nick P. Bassill June 28 th, 2012.
Preliminary results from assimilation of GPS radio occultation data in WRF using an ensemble filter H. Liu, J. Anderson, B. Kuo, C. Snyder, A. Caya IMAGe.
Kris Shrestha James Belanger Judith Curry Jake Mittelman Phillippe Beaucage Jeff Freedman John Zack Medium Range Wind Power Forecasts for Texas.
11th EMS & 10th ECAM Berlin, Deutschland The influence of the new ECMWF Ensemble Prediction System resolution on wind power forecast accuracy and uncertainty.
Nathalie Voisin 1, Florian Pappenberger 2, Dennis Lettenmaier 1, Roberto Buizza 2, and John Schaake 3 1 University of Washington 2 ECMWF 3 National Weather.
COSMO General Meeting Zurich, 2005 Institute of Meteorology and Water Management Warsaw, Poland- 1 - Simple Kalman filter – a “smoking gun” of shortages.
Short-Range Ensemble Prediction System at INM García-Moya, J.A., Santos, C., Escribà, P.A., Santos, D., Callado, A., Simarro, J. (NWPD, INM, SPAIN) 2nd.
Verification of ensemble precipitation forecasts using the TIGGE dataset Laurence J. Wilson Environment Canada Anna Ghelli ECMWF GIFS-TIGGE Meeting, Feb.
Kalman filtering at HNMS Petroula Louka Hellenic National Meteorological Service
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.
Judith Curry James Belanger Mark Jelinek Violeta Toma Peter Webster 1
DOWNSCALING GLOBAL MEDIUM RANGE METEOROLOGICAL PREDICTIONS FOR FLOOD PREDICTION Nathalie Voisin, Andy W. Wood, Dennis P. Lettenmaier University of Washington,
Munehiko Yamaguchi 12, Takuya Komori 1, Takemasa Miyoshi 13, Masashi Nagata 1 and Tetsuo Nakazawa 4 ( ) 1.Numerical Prediction.
Verification of wind gust forecasts Javier Calvo and Gema Morales HIRMAM /ALADIN ASM Utrecht May 11-15, 2009.
Improving Numerical Weather Prediction Using Analog Ensemble Presentation by: Mehdi Shahriari Advisor: Guido Cervone.
ECMWF/EUMETSAT NWP-SAF Satellite data assimilation Training Course Mar 2016.
of Temperature in the San Francisco Bay Area
Xuexing Qiu and Fuqing Dec. 2014
BACY = Basic Cycling A COSMO Data Assimilation Testbed for Research and Development Roland Potthast, Hendrik Reich, Christoph Schraff, Klaus.
Jean-Francois Geleyn, Jean-Francois Mahfouf
What is in our head…. Spatial Modeling Performance in Complex Terrain Scott Eichelberger, Vaisala.
of Temperature in the San Francisco Bay Area
Overall Statistics RMSE WRF-UA: 159 W m-2 WRF-UCSD: 171 W m-2 STDERR
MOS Developed by and Run at the NWS Meteorological Development Lab (MDL) Full range of products available at:
Improving forecasts through rapid updating of temperature trajectories and statistical post-processing Nina Schuhen, Thordis L. Thorarinsdottir and Alex.
Post Processing.
Observation uncertainty in verification
Comparison of different combinations of ensemble-based and variational data assimilation approaches for deterministic NWP Mark Buehner Data Assimilation.
Project Team: Mark Buehner Cecilien Charette Bin He Peter Houtekamer
The Met Office Ensemble of Regional Reanalyses
NWP activities in Austria in 2006/2007 Y. Wang
Wind Energy Potential in Europe: 2020 – 2030
Rapid Adjustment of Forecast Trajectories: Improving short-term forecast skill through statistical post-processing Nina Schuhen, Thordis L. Thorarinsdottir.
Presentation transcript:

S.Alessandrini, S.Sperati, G.Decimi, 11th EMS & 10th ECAM Berlin, Deutschland The influence of the new ECMWF Ensemble Prediction System resolution on wind power forecast accuracy and uncertainty estimation S.Alessandrini, S.Sperati, G.Decimi, P.Pinson2, (2DTU, Denmark ) 09/2011

Outline This work is a prosecution of the presentation of EMS 2010 A comparison of wind power deterministic forecast performances based on old and new version ECMWF GM during two periods (2008, 2011) is shown The new version of the EPS (ECMWF) is applied to understand if it is possible to increase the performances in the forecast of power prediction accuracy

ECMWF: ensemble model EPS run operationally until day 10 ahead, 51 members (perturbed), ctrl run (not perturbed) EPS resolutions increased from T399/T255 (60 km) to T639/T319 (32 km) on 26 January 2010 We have studied the different performances, between old and new version, using EPS member spread to predict the deterministic forecast error

Wind Power forecast system for EPS The NN is trained using ensemble mean and measured wind It is then applied to correct each member The theoretical power curve is verified against measured wind and power data to be representative of the wind farm ECMWF 51 members (0-72 hours wind forecast) NN Wind measurements 0-72 hours wind forecast (corrected) Power Curve (theoretical) Ensemble Power forecast 0-72 hours

Deterministic Wind Power forecast system used at RSE ECMWF deterministic forecast model 0-72 hours wind forecast Power measurements NN Power forecast 0-72 hours

Case Study: wind farm in Sicily The wind farm is made of 9 turbines with 850 kW of nominal power (50 m height) It’s located on a mountain region at around 700 m asl The wind (50 m agl) and power data of the year 2008-2011 are supplied by ENEL

Case Study: wind farm data, meteorological comparison Two time periods have been considered Old EPS and deterministic model version have been tested between 01-2008 and 11-2008 New EPS and deterministic model version have been tested between 11-2010 and 06-2011 2008 2011

Case Study: wind farm, deterministic power forecast Comparison of performances using the two versions of deterministic ECMWF meteorological model (2008->0.25°, 2011->0.15°) For each model the same forecast scheme is applied A training period for the NN and a test period to verify performances CONCLUSION: The increase of resolution doesn’t assure better performances also due to different meteorological conditions of the two periods

Case Study: wind farm, deterministic power forecast Comparison of performances using the new version of deterministic ECMWF meteorological model and EPS mean deterministic forecast CONCLUSION: the EPS ensemble mean leads to a better performances in power forecast with a gain of quite one day of predictability

Case study: EPS power forecast An horizontal bilinear interpolation is performed using the 4 nearest grid points A MOS technique (NN) is calibrated on the ensemble mean during the training data set to adjust the 51 members wind speed on the test period. Before MOS After MOS 2008 2011 2008 2011

Case study: EPS power forecast The PIT histograms for wind speed on the first 3 days show an overconfident model with both EPS version The wind speed ensemble spread is to small on the first 3 forecast days DAY 1 DAY 2 DAY 3 2008 2011

Case study: Recalibrated EPS A logit transform is applied to the members to approach a gaussian distribution A variance deficit (vd) is adaptively calculated for each forecast interval time (day 1, day 2, day 3) The average variance of (transformed) ensemble members is compared to the variance of the (transformed) errors over that period. The variance deficit is then calculated as vd = var(error)/mean(var(ensembles)). Ec(j) = <E> + vd *(E(j) - <E>)

Case study: Recalibrated EPS 2008 2011

Case study: Ensemble spread (wind) raw wind data (10m) after MOS after calibration

Case study: EPS DAY 1 DAY 2 DAY 3 2008 2011 The PIT histograms show a more calibrated model (wind) DAY 1 DAY 2 DAY 3 2008 2011

Case study: EPS recalibration (power) The theoretic power curve has been used to compute the ensemble power members because well fit the experimental data 2008 2011

Case study: EPS DAY 1 DAY 2 DAY 3 2008 2011 The PIT histograms show a calibrated model (power) DAY 1 DAY 2 DAY 3 2008 2011

Case study: Deterministic errors vs ensemble spread (power) Statistical comparison between average daily spread vs daily RMSE Of deterministic power forecast during the test period

Case study: Deterministic errors vs ensemble spread (power) DAY 1 DAY 2 DAY 3 2008 70% 2011 76%

Conclusions The EPS mean can be used to increase deterministic performances (2011 case) The new ECMWF deterministic model resolution doesn’t necessary guarantees better power forecast The EPS spread on the first 3 forecast days is too low in order to extract usable information from raw data (even after the MOS) even with the new EPS resolution After a statistical calibration the ensemble power spread seems to have enough correlation with the deterministic error in order to be used as a predictor of accuracy even after 72 hours The new EPS version seems to be slightly more accurate for the power error prediction