The Met Office Ensemble of Regional Reanalyses

Slides:



Advertisements
Similar presentations
© Crown Copyright Source: Met Office Dale Barker, Tomas Landelius, Eric Bazile, Francesco Isotta, Phil Jones 17 April 2013 EURO4M – WP2: Regional.
Advertisements

Recent & planned developments to the Met Office Global and Regional Ensemble Prediction System (MOGREPS) Richard Swinbank, Warren Tennant, Sarah Beare,
Atmospheric Reanalyses Update Mike Bosilovich. ReanalysisHoriz.ResDatesVintageStatus NCEP/NCAR R1T present1995ongoing NCEP-DOE R2T present2001ongoing.
Dale Barker, Richard Renshaw, Peter Jermey WWOSC, Montreal, Canada, 20 August 2014 Regional Reanalysis At The Met Office © Crown Copyright 2012 Source:
Data assimilation of trace gases in a regional chemical transport model: the impact on model forecasts E. Emili 1, O. Pannekoucke 1,2, E. Jaumouillé 2,
Toward a Real Time Mesoscale Ensemble Kalman Filter Gregory J. Hakim Dept. of Atmospheric Sciences, University of Washington Collaborators: Ryan Torn (UW)
Background In deriving basic understanding of atmospheric phenomena, the analysis often revolves around discovering and exploiting relationships between.
Models for model error –Additive noise. What is Q(x 1, x 2, t 1, t 2 )? –Covariance inflation –Multiplicative noise? –Parameter uncertainty –“Structural”
A comparison of hybrid ensemble transform Kalman filter(ETKF)-3DVAR and ensemble square root filter (EnSRF) analysis schemes Xuguang Wang NOAA/ESRL/PSD,
Slide 1 Evaluation of observation impact and observation error covariance retuning Cristina Lupu, Carla Cardinali, Tony McNally ECMWF, Reading, UK WWOSC.
Lili Lei1,2, David R. Stauffer1 and Aijun Deng1
Francesca Marcucci, Lucio Torrisi with the contribution of Valeria Montesarchio, ISMAR-CNR CNMCA, National Meteorological Center,Italy First experiments.
Performance of the MOGREPS Regional Ensemble
Ensemble-variational sea ice data assimilation Anna Shlyaeva, Mark Buehner, Alain Caya, Data Assimilation and Satellite Meteorology Research Jean-Francois.
ESA DA Projects Progress Meeting 2University of Reading Advanced Data Assimilation Methods WP2.1 Perform (ensemble) experiments to quantify model errors.
Observing Strategy and Observation Targeting for Tropical Cyclones Using Ensemble-Based Sensitivity Analysis and Data Assimilation Chen, Deng-Shun 3 Dec,
Advances in the use of observations in the ALADIN/HU 3D-Var system Roger RANDRIAMAMPIANINA, Regina SZOTÁK and Gabriella Csima Hungarian Meteorological.
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.
Federal Department of Home Affairs FDHA Federal Office of Meteorology and Climatology MeteoSwiss High-resolution data assimilation in COSMO: Status and.
A Comparison of the Northern American Regional Reanalysis (NARR) to an Ensemble of Analyses Including CFSR Wesley Ebisuzaki 1, Fedor Mesinger 2, Li Zhang.
The Australian Community Climate Earth-System Simulator The Australian Community Climate and Earth System Simulator Kamal Puri (ACCESS Group Leader)
© British Crown copyright 2014 Met Office A comparison between the Met Office ETKF (MOGREPS) and an ensemble of 4DEnVars Marek Wlasak, Stephen Pring, Mohamed.
Interoperability at INM Experience with the SREPS system J. A. García-Moya NWP – Spanish Met Service INM SRNWP Interoperability Workshop ECMWF –
Using satellite data to understand uncertainties in reanalyses: UERRA Richard Renshaw, Peter Jermey with thanks to Jörg Trentmann, Jennifer Lenhardt, Andrea.
Covariance Modeling “Where America’s Climate, Weather, Ocean and Space Weather Services Begin” JCSDA Summer Colloquium July 27, 2015 Presented by John.
Ensemble data assimilation in an operational context: the experience at the Italian Weather Service Massimo Bonavita and Lucio Torrisi CNMCA-UGM, Rome.
Deutscher Wetterdienst Vertical localization issues in LETKF Breogan Gomez, Andreas Rhodin, Hendrik Reich.
Ensemble Kalman Filter in a boundary layer 1D numerical model Samuel Rémy and Thierry Bergot (Météo-France) Workshop on ensemble methods in meteorology.
Ensemble assimilation & prediction at Météo-France Loïk Berre & Laurent Descamps.
Page 1© Crown copyright 2004 SRNWP Lead Centre Report on Data Assimilation 2005 for EWGLAM/SRNWP Annual Meeting October 2005, Ljubljana, Slovenia.
Use ensemble error covariance information in GRAPES 3DVAR Jiandong GONG, Ruichun WANG NWP center of CMA Oct 27, 2015.
Implementation and Testing of 3DEnVAR and 4DEnVAR Algorithms within the ARPS Data Assimilation Framework Chengsi Liu, Ming Xue, and Rong Kong Center for.
11th EMS & 10th ECAM Berlin, Deutschland The influence of the new ECMWF Ensemble Prediction System resolution on wind power forecast accuracy and uncertainty.
Langen, September 2003 COSMO-LEPS objective verification Chiara Marsigli, Francesco Boccanera, Andrea Montani, Fabrizio Nerozzi, Tiziana Paccagnella.
Page 1 Developments in regional DA Oct 2007 © Crown copyright 2007 Mark Naylor, Bruce Macpherson, Richard Renshaw, Gareth Dow Data Assimilation and Ensembles,
Performance of COSMO-LEPS over the Alpine region Chiara Marsigli, Andrea Montani, Fabrizio Nerozzi, Tiziana Paccagnella ARPA-SMR, Bologna, Italy ICAM/MAP.
Page 1 Andrew Lorenc WOAP 2006 © Crown copyright 2006 Andrew Lorenc Head of Data Assimilation & Ensembles Numerical Weather Prediction Met Office, UK Data.
The operational Meteo-France ensemble 4D-Var (L. Berre, G. Desroziers, and co-authors) Ensemble assimilation (operational with 6 members…) :
Hybrid (3D-VAR /ETKF) Data Assimilation System
Ensemble prediction review for WGNE, 2010 Tom Hamill 1 and Pedro de Silva-Dias 2 1 NOAA/ESRL 2 Laboratório Nacional de Computação Científica
© Crown copyright Met Office Recent [Global DA] Developments at the Met Office Dale Barker, Weather Science, Met Office THORPEX/DAOS Meeting, 28 June 2011.
The application of ensemble Kalman filter in adaptive observation and information content estimation studies Junjie Liu and Eugenia Kalnay July 13th, 2007.
ALADIN 3DVAR at the Hungarian Meteorological Service 1 _____________________________________________________________________________________ 27th EWGLAM.
Regional Re-analyses of Observations, Ensembles and Uncertainties of Climate information Per Undén Coordinator UERRA SMHI.
E. Bazile, C. Soci, F. Besson & ?? UERRA meeting Exeter, March 2014 Surface Re-Analysis and Uncertainties for.
Station lists and bias corrections Jemma Davie, Colin Parrett, Richard Renshaw, Peter Jermey © Crown Copyright 2012 Source: Met Office© Crown copyright.
Exploring and Validating LM Performances at Very High Resolution M. Didone, D. Lüthi, H.C Davies Institute for Atmospheric and Climate Science, ETH Zürich.
1 MODIS winds assimilation experiments and impact studies to date at the Met Office Howard Berger, Mary Forsythe, Met Office, Bracknell/Exeter, UK UW-CIMSS.
© Crown copyright Met Office Mismatching Perturbations at the Lateral Boundaries in Limited-Area Ensemble Forecasting Jean-François Caron … or why limited-area.
ECMWF/EUMETSAT NWP-SAF Satellite data assimilation Training Course Mar 2016.
Hybrid Data Assimilation
Xuexing Qiu and Fuqing Dec. 2014
Met Office Ensemble System Current Status and Plans
GPC-Seoul: Status and future plans
BACY = Basic Cycling A COSMO Data Assimilation Testbed for Research and Development Roland Potthast, Hendrik Reich, Christoph Schraff, Klaus.
MO – Design & Plans UERRA GA 2016 Peter Jermey
UERRA WP3 Assessing uncertainties by evaluation against independent observational datasets DWD, KNMI, MI, EDI, UEA, NMA-RO, MO Task 3.1 Coordinated uncertainty.
Implementation of Ensemble Data Assimilation in Global NWP
S.Alessandrini, S.Sperati, G.Decimi,
Vertical localization issues in LETKF
FSOI adapted for used with 4D-EnVar
Developing 4D-En-Var: thoughts and progress
Initial trials of 4DEnVAR
AGREPS – ACCESS Global and Regional Ensemble Prediction System
Real-time WRF EnKF 36km outer domain/4km nested domain D1 (36km)
Ramble: What is the purpose of an ensemble forecast? The dominant philosophy at the moment is that ensemble forecasts provide uncertainty information.
Development of an advanced ensemble-based ocean data assimilation approach for ocean and coupled reanalyses Eric de Boisséson, Hao Zuo, Magdalena Balmaseda.
MOGREPS developments and TIGGE
Fabien Carminati, Stefano Migliorini, & Bruce Ingleby
Presentation transcript:

The Met Office Ensemble of Regional Reanalyses EMS 2015 The Met Office Ensemble of Regional Reanalyses Peter Jermey Dale Barker, Jemma Davie, Amy Doherty, Sana Mahmood, Adam Maycock, Richard Renshaw

Reanalysis at the Met Office 2008 & 2009 European Reanalysis 12km Deterministic Reanalysis 40 year European Reanalysis 12km Deterministic Reanalysis 20 member Ensemble Reanalysis

Uncertainties in Ensembles of Regional Reanalyses Ensemble using static 4DVAR Provides lower resolution fields with uncertainty estimation i.e. mean and spread at 24km Production start: Dec 2015 Deterministic reanalysis using hybrid 4DVAR Uses ensemble reanalysis uncertainty to improve assimilation (B) Provides higher resolution deterministic fields at 12km Production start: late 2016

Uncertainties in Ensembles of Regional Reanalyses Ensemble & Deterministic systems coupled 4DVAR minimises weighted sum of differences with background & obs Weights are dependent on background error covariance matrix (B) Ensemble uses fixed bg error cov (B=Bc) Ensemble provides EOTD to ensemble EDA - "hybrid" 4DVAR - weighted sum of bg error covs (B=bcBc+beBe) Bc + Be H 4 Y D B V R A I R D 4 D V A R 4 D V A R 4 D V A R UM UM UM UM

Ensemble System Represent every uncertainty in the system via perturbations Uncertainty in Observations Model Boundary Conditions Each ensemble member has a different realisation of these Set of (input) realisations represent the span of all possible realisations Therefore (output) spread should estimate uncertainty in the system

Observations For every observation we have a measurement and an uncertainty estimate... To obtain several realisations randomly perturb the measurement within the uncertainty estimate...

Model To perturb the model we need an estimate of model error... Assuming the analyses are drawn from the same distribution as the truth.

Boundary Conditions * * 80km *planned

RMS v Spread T2 & 500H (10 members) Germany Temperature 1.5m Geopotential Height 500hPa

Examples of Product 18Z on 18/02/10 mean uncertainty

Probability Maps Probability 50m wind 3ms-1 < speed < 15ms-1 >0.9 <0.1 Probability 50m wind 3ms-1 < speed < 15ms-1 18Z on 18/02/10 Probability of 1mm/6h 12Z to 18Z 18/02/10

Improve quality of ensemble What’s Next ..? Improve quality of ensemble Port to ECMWF Regional SURF Ensemble production aim to start December 2015 Regional hybrid Deterministic production aim to start late 2016

Thank you for listening

Initial Test Run (no inflation) T2 & 500H 1. Each member equally likely 2. Mean Error < Ctrl Error 3. En Spread = Mean RMSE 4. Model Freq. = Obs. Freq. 500H T2