Update on seasonal forecast system based on SL-AV model at Hydrometcentre of Russia. Decadal prediction plans. M.A. Tolstykh (2,1) and D.B.Kiktev (1),

Slides:



Advertisements
Similar presentations
Verification Activity in Sub-seasonal Forecasting at JMA 1 Climate Prediction Division / JMA Yuhei Takaya WWRP/THORPEX/WCRP Sub-seasonal to Seasonal Implementation.
Advertisements

© European Centre for Medium-Range Weather Forecasts Operational and research activities at ECMWF now and in the future Sarah Keeley Education Officer.
V. Shashkin et al. Mass-conservative SL, WWOSC-2104, P&P August 21, 2014 Inherently mass-conservative semi-Lagrangian transport scheme and global hydrostatic.
LRF Training, Belgrade 13 th - 16 th November 2013 © ECMWF Sources of predictability and error in ECMWF long range forecasts Tim Stockdale European Centre.
ECMWF long range forecast systems
WCRP OSC 2011: Strategies for improving seasonal prediction © ECMWF Strategies for improving seasonal prediction Tim Stockdale, Franco Molteni, Magdalena.
Contents 1. Data assimilation in Russian Hydrometcentre at the end of Tsyroulnikov M.D., Zaripov R.B., Tolstykh M.A., Bagrov A.N. 2. Development.
Extended range prediction during 2013 season Using Ensemble Prediction System based in CFSv2 And GFSv2 forced with Bias corrected CFSv2 forecasted SST.
INPE Activities on Seasonal Climate Predictions Paulo Nobre INPE-CCST-CPTEC WGSIP-12, Miami, January 2009.
Verification of NCEP SFM seasonal climate prediction during Jae-Kyung E. Schemm Climate Prediction Center NCEP/NWS/NOAA.
Overview Northern hemisphere extra-tropics El Niño Seasonal Climate – Winter Mike Blackburn Seasonal Climate Discussion, 14 April 2010.
Exeter 1-3 December 2010 Monthly Forecasting with Ensembles Frédéric Vitart European Centre for Medium-Range Weather Forecasts.
Climate Forecasting Unit Second Ph’d training talk Prediction of climate extreme events at seasonal and decadal time scale Aida Pintó Biescas.
India summer monsoon rainfall in ECMWF Sys3 – ICTP, August Indian summer monsoon rainfall in the ECMWF seasonal fc. System-3: predictability and.
Climate Forecasting Unit Prediction of climate extreme events at seasonal and decadal time scale Aida Pintó Biescas.
Barcelona, 2015 Ocean prediction activites at BSC-IC3 Virginie Guemas and the Climate Forecasting Unit 9 February 2015.
Available products for Seasonal forecasting J.P. Céron – Direction de la Climatologie.
Intraseasonal TC prediction in the southern hemisphere Matthew Wheeler and John McBride Centre for Australia Weather and Climate Research A partnership.
Alan Robock Department of Environmental Sciences Rutgers University, New Brunswick, New Jersey USA
The Centre for Australian Weather and Climate Research A partnership between CSIRO and the Bureau of Meteorology Summary/Future Re-anal.
Research Needs for Decadal to Centennial Climate Prediction: From observations to modelling Julia Slingo, Met Office, Exeter, UK & V. Ramaswamy. GFDL,
3. Products of the EPS for three-month outlook 1) Outline of the EPS 2) Examples of products 3) Performance of the system.
The Centre for Australian Weather and Climate Research A partnership between CSIRO and the Bureau of Meteorology Sub-Seasonal Prediction Activities and.
One-year re-forecast ensembles with CCSM3.0 using initial states for 1 January and 1 July in Model: CCSM3 is a coupled climate model with state-of-the-art.
ECMWF Training course 26/4/2006 DRD meeting, 2 July 2004 Frederic Vitart 1 Predictability on the Monthly Timescale Frederic Vitart ECMWF, Reading, UK.
WGSIP12 – Miami - January 2009 – Impacts verification - Andy Morse Preliminary report on verification scores for malaria and the climate drivers DEMETER.
VERIFICATION OF A DOWNSCALING SEQUENCE APPLIED TO MEDIUM RANGE METEOROLOGICAL PREDICTIONS FOR GLOBAL FLOOD PREDICTION Nathalie Voisin, Andy W. Wood and.
Verification of operational seasonal forecasts at RA-VI Regional Climate Center South East European Virtual Climate Change Centre Goran Pejanović Marija.
Description of the IRI Experimental Seasonal Typhoon Activity Forecasts Suzana J. Camargo, Anthony G. Barnston and Stephen E.Zebiak.
September 14, 2013SEASONAL AND EXTENDED RANGE PREDICTION GROUPSlide 1 INITIAL CONDITION 13 th September 2013 Extended range prediction during 2013 season.
Fifth Session of the South Asian Climate Outlook Forum (SASCOF-5) JMA Seasonal Prediction of South Asian Climate for Summer 2014 Hitoshi Sato Climate Prediction.
Seasonal Outlook for 2010 Southwest Monsoon Rainfall D. S. Pai Director, Long Range Forecasting South Asian Climate Outlook Forum (SASCOF -1) April.
1 Summary of CFS ENSO Forecast December 2010 update Mingyue Chen, Wanqiu Wang and Arun Kumar Climate Prediction Center 1.Latest forecast of Nino3.4 index.
Indian Institute of Tropical Meteorology (IITM) Suryachandra A. Rao Colloborators: Hemant, Subodh, Samir, Ashish & Kiran Dynamical Seasonal Prediction.
and Decadal Prediction Systems
GPC-Montreal - Status Report - March 2014
Richard Graham on behalf of GPC Exeter Met Office Hadley Centre
Северо-Евразийский Климатический Центр
Predictability: How can we predict the climate decades into the future when we can’t even predict the weather for next week? Predictability of the first.
JMA Seasonal Prediction of South Asian Climate for OND 2017
JMA Seasonal Prediction of South Asian Climate for OND 2017
GPC-Seoul: Status and future plans
Challenges of Seasonal Forecasting: El Niño, La Niña, and La Nada
ENSO Frequency Cascade and Implications for Predictability
STATUS of Global Producing Center - Beijing
Recent changes in the ALADIN operational suite
GPC CPTEC: Seasonal forecast activities update
El Nino and La Nina An important atmospheric variation that has an average period of three to seven years. Goes between El Nino, Neutral, and La Nina (ENSO.
Multi-model seasonal forecast Operational systems
Shuhua Li and Andrew W. Robertson
David Salstein, Edward Lorenz, Alan Robock, and John Roads
A coupled ensemble data assimilation system for seasonal prediction
Sub-seasonal prediction at ECMWF
Seasonal Predictions for South Asia
Long Range Forecast Transient Intercomparison Project (LRFTIP-A)
WP4.1 : Exploiting CCI products in CMIP like experiments
The Importance of Reforecasts at CPC
University of Washington Center for Science in the Earth System
Caio Coelho (Joint CBS/CCl IPET-OPSLS Co-chair) CPTEC/INPE, Brazil
Predictability assessment of climate predictions within the context
ECMWF activities: Seasonal and sub-seasonal time scales
Precipitation variability over Arizona and
Earth Climate System Model of INM RAS
Barcelona, 23 September 2015 Impact of resolution and initialisation in climate seasonal predictions F.J. Doblas Reyes.
WP3.10 : Cross-assessment of CCI-ECVs over the Mediterranean domain
GloSea4: the Met Office Seasonal Forecasting System
Environment Canada Monthly and Seasonal Forecasting Systems
Decadal Climate Prediction at BSC
Multiscale global atmosphere model SL-AV: applications for numerical weather prediction, climate change modelling using massively parallel computers Tolstykh.
Ryan Kang, Wee Leng Tan, Thea Turkington, Raizan Rahmat
Presentation transcript:

Update on seasonal forecast system based on SL-AV model at Hydrometcentre of Russia. Decadal prediction plans. M.A. Tolstykh (2,1) and D.B.Kiktev (1), R.B. Zaripov (1), E.N.Kruglova (1), I.A.Kulikova (1) Hydrometcentre of Russia (1); Institute of Numerical Matematics Russian Academy of Sciences (2) 2015

Plan Seasonal forecast system at HMCR Plans for running decadal forecasts at INM RAS

Seasonal version of SL-AV model Semi-implicit semi-Lagrangian vorticity-divergence dynamical core of own development (Tolstykh 2010), mostly ALADIN/LACE parameterizations. Current version: Resolution 1.4x1.125 degrees lon/lat, 28 levels. Described in (Tolstykh et al, Izvestia RAN, Ser. PhA&O, 2010) with updates in (Tolstykh et al Izvestia RAN, 2014) Verification of seasonal forecasts (also for MGO (St.Petersbourg) forecasts) http://neacc.meteoinfo.ru/verificationforecast

Running forecasts d0-63: 1.1x1.4 L28 once a week, 20 member ensemble initialized on 00Z every Wednesday forced py persisted SST anomalies (mean for 2 weeks) from NCEP (Reynolds SST OI v2). Perturbation from a breeding cycle. Re-forecast suite with 10 members spanning 30 years (1981-2010) run in real-time. m0-4: Forecast suite is the same as d0-63, but forecast lead time is 4 months. Runs on the last Wednesday of a month. Re-forecast suite with 10 members spanning 30 years (1981-2010) 00Z and 12Z 26-30 of each month (24-28 for February). Input to APCC, WMO LC LRF multi-model ensemble. Forecasts are also available at North Eurasia Climate Centre site (neacc.meteoinfo.ru)

Scores and forecasts at NEACC site Skill scores: ROC_A - ROC Score Above Normal ROC_N - ROC Score Near Normal ROC_B - ROC Score Below Normal RO - sign consistency coefficient ACC - anomaly correlation coefficient RMSE - root mean square error Some plots from WMO LC are also available

Activities since 16th session NEACC site (forecasts, diagnostics – scores, indices,…) Implementing CHFP and S2S output standards. New snow albedo parameterization in SL-AV, cloudiness retuning. Moving from NCEP2 to ERA Interim data for hindcasts. Too fast transition to new technology -> serious bug in operational seasonal forecasts in January Corrected by the end of February

Comparison of hindcasts errors for 2011 and 2014 versions Comparison of hindcasts errors for 2011 and 2014 versions. RMSE averaged over 4 seasons and 28 years (1983-2010), for H500(dam) , MSLP (hPa), T850, Т2м, H200 (dam) with respect to reanalysis . S20 - (90 - 20 S), N20 – (20-90 N), TR – (20S-20N). Изменения за все 4 сезона. Изменения для зимнего периода в Т2м – положительны

New version of the model More accurate SW and LW radiation parameterization(CLIRAD SW + RRTM LW). ALARO-0 microphysics Increased horizontal resolution (0.72°x0.9° lat-lon) Promising preliminary results (especially in dynamics), poor precip so far, tuning is underway

Plans for decadal forecasts at INM RAS INMCM5 with improvements - higher model top, better stratosphere resolution, - new cloudiness and condensation parameterizations, - aerosols description. Two resolutions considered: `Optimistic’: Atm. 2˚x1.5˚L73, Oc. 0.5˚x0.25˚L40 (twice higher ocean horizontal resolution than in CMIP5) Atm. 2˚x1.5˚L21, Oc. 1˚x0.5˚L40 Depends on computer resources availability

Thank you for attention!