© Crown copyright 2007 A fully resolved stratosphere: Impact on seasonal forecasting Alberto Arribas Monthly-to-Decadal area, Met Office Hadley Centre.

Slides:



Advertisements
Similar presentations
Scott's Winter Forecast ! How do I make a forecast?
Advertisements

Overview of KMA s Operational LRF Services Korea Meteorological Administration.
Recent & planned developments to the Met Office Global and Regional Ensemble Prediction System (MOGREPS) Richard Swinbank, Warren Tennant, Sarah Beare,
© Crown copyright 2007 Monthly-Seasonal forecasting Alberto Arribas Monthly to Decadal group, Met Office Hadley Centre Geneva, December 2011.
© Crown copyright Met Office Stratospheric Influences on the Troposphere Adam Scaife December 2010.
Page 1© Crown copyright 2004 Seasonal forecasting activities at the Met Office Long-range Forecasting Group, Hadley Centre Presenter: Richard Graham ECMWF.
Training Course 2013– NWP-PR: The Monthly Forecast System at ECMWF 1 Monthly Forecasting at ECMWF Frédéric Vitart European Centre for Medium-Range Weather.
© Crown copyright Met Office NEMOVAR status and plans Matt Martin, Dan Lea, Jennie Waters, James While, Isabelle Mirouze NEMOVAR SG, ECMWF, Jan 2012.
Monthly Forecasting at ECMWF
Sub-seasonal to seasonal prediction David Anderson.
Predictability of the Stratosphere and Associated Teleconnections
The role of the stratosphere in extended- range forecasting Thomas Jung Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research Germany.
Impact of EOS MLS ozone data on medium-extended range ensemble forecasts Jacob C. H. Cheung 1, Joanna D. Haigh 1, David R. Jackson 2 1 Imperial College.
1 NCAS SMA presentation 14/15 September 2004 The August 2002 European floods: atmospheric teleconnections and mechanisms Mike Blackburn (1), Brian Hoskins.
1 03/0045a © Crown copyright Evaluating water vapour in HadAM3 with 20 years of satellite data Richard P. Allan Mark A. Ringer Met Office, Hadley Centre.
Impacts of systematic model biases on intraseasonal variability of the Asian summer monsoon and the intraseasonal-interannual relationship A. G. Turner.
The effect of doubled CO 2 and model basic state biases on the monsoon- ENSO system Andrew Turner, Pete Inness, Julia Slingo Walker Institute / NCAS-Climate.
The effect of doubled CO 2 and model basic state biases on the monsoon- ENSO system: the mean response and interannual variability Andrew Turner, Pete.
Climate Prediction Division Japan Meteorological Agency Developments for Climate Services at Japan Meteorological Agency 1.
Slide 1 October 2011 Verification for polar regions  Scores computed for polewards of 65°  NB proposed for CBS is polewards of 60°  Verification at.
October Winter Forecast October 29, 2011 Pete Parsons, ODF Meteorologist Pete Parsons, ODF Meteorologist.
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
© Crown copyright Met Office The Met Office high resolution seasonal prediction system Anca Brookshaw – Monthly to Decadal Variability and Prediction,
Seasonal to decadal prediction of the Arctic Oscillation D. Smith, A. Scaife, A. Arribas, E. Blockley, A. Brookshaw, R.T. Clark, N. Dunstone, R. Eade,
© Crown copyright Met Office Decadal Climate Prediction Doug Smith, Nick Dunstone, Rosie Eade, Leon Hermanson, Adam Scaife.
© Crown copyright Met Office Improving seasonal forecasting: role of teleconnections Madrid. Febrero Alberto Arribas.
Enhanced seasonal forecast skill following SSWs DynVar/SNAP Workshop, Reading, UK, April 2013 Michael Sigmond (CCCma) John Scinocca, Slava Kharin.
Review of Northern Winter 2010/11
© Crown copyright Met Office GloSea4: the new Met Office Seasonal Forecasting System A. Arribas, M. Glover, D. Peterson, A. Maidens, M. Gordon, C. MacLachlan,
© Crown copyright Met Office Met Office seasonal forecasting for winter Jeff Knight (with thanks to many colleagues)
Exeter 1-3 December 2010 Monthly Forecasting with Ensembles Frédéric Vitart European Centre for Medium-Range Weather Forecasts.
© Crown copyright /0653 Met Office and the Met Office logo are registered trademarks Met Office Hadley Centre, FitzRoy Road, Exeter, Devon, EX1.
© Crown copyright Met Office CLIVAR Climate of the 20 th Century Project Adam Scaife, Chris Folland, Jim Kinter, David Fereday January 2009.
© Crown copyright Met Office An Introduction to Long-range Forecasting Emily Wallace Nov 2012.
Influence of the stratosphere on surface winter climate Adam Scaife, Jeff Knight, Anders Moberg, Lisa Alexander, Chris Folland and Sarah Ineson. CLIVAR.
High Resolution Climate Modelling in NERC (and the Met Office) Len Shaffrey, University of Reading Thanks to: Pier Luigi Vidale, Jane Strachan, Dave Stevens,
ECMWF Forecasts Laura Ferranti, Frederic Vitart and Fernando Prates.
CIMA CHFP Data Server.
EUROBRISA WORKSHOP, Paraty March 2008, ECMWF System 3 1 The ECMWF Seasonal Forecast System-3 Magdalena A. Balmaseda Franco Molteni,Tim Stockdale.
© Crown copyright Met Office Decadal predictions of the Atlantic ocean and hurricane numbers Doug Smith, Nick Dunstone, Rosie Eade, David Fereday, James.
© Crown copyright Met Office The stratosphere and Seasonal to Decadal Prediction Adam Scaife, Sarah Ineson, Jeff Knight and Andrew Marshall January 2009.
Page 1© Crown copyright 2004 A Review of UK Met Office Seasonal forecasts for Europe (1-8 months ahead) Andrew Colman, Richard Graham Met Office Hadley.
The Centre for Australian Weather and Climate Research A partnership between CSIRO and the Bureau of Meteorology Oscar Alves and the POAMA Team CAWCR (Centre.
Page 1© Crown copyright 2004 WP5.3 Assessment of Forecast Quality ENSEMBLES RT4/RT5 Kick Off Meeting, Paris, Feb 2005 Richard Graham.
Beyond CMIP5 Decadal Predictions and the role of aerosols in the warming slowdown Doug Smith, Martin Andrews, Ben Booth, Nick Dunstone, Rosie Eade, Leon.
Modes of variability and teleconnections: Part II Hai Lin Meteorological Research Division, Environment Canada Advanced School and Workshop on S2S ICTP,
© Crown copyright Met Office Strategy for Seasonal Prediction Development: UKMO and WGSIP activities Adam Scaife Head Monthly to Decadal Prediction Met.
© Crown copyright Met Office The impact of initial conditions on decadal climate predictions Doug Smith, Nick Dunstone, Rosie Eade, James Murphy, Holger.
© Crown copyright Met Office Stratospheric Extension to the CHFP “S-CHFP” and links to WCRP-SPARC Adam Scaife WGSIP July 2010.
Integrating Climate Science into Adaptation Actions Alberto Arribas Kuala Lumpur, November.
© Crown copyright Met Office Predictability and systematic error growth in Met Office MJO predictions Ann Shelly, Nick Savage & Sean Milton, UK Met Office.
1 An Assessment of the CFS real-time forecasts for Wanqiu Wang, Mingyue Chen, and Arun Kumar CPC/NCEP/NOAA.
© Crown copyright 2007 Forecasting weeks to months ahead Dr. Alberto Arribas Monthly-to-Decadal area, Met Office Hadley Centre Exeter, April 2014.
Page 1© Crown copyright 2007 Influence of ENSO on European Climate via the Stratosphere Sarah Ineson and Adam Scaife 2007.
The Met Office GloSea5 System
GPC-Montreal - Status Report - March 2014
Richard Graham on behalf of GPC Exeter Met Office Hadley Centre
Richard Graham on behalf of GPC Exeter Met Office Hadley Centre
GPC-Seoul: Status and future plans
Teleconnections in MINERVA experiments
Met Office GPC Adam Scaife Head of Monthly to Decadal Prediction Met Office © Crown copyright Met Office.
ENSO-NAO interactions via the stratosphere
Prospects for Wintertime European Seasonal Prediction
Predictability of the NAO? Adam Scaife
AGREPS – ACCESS Global and Regional Ensemble Prediction System
GloSea4 – the new Met Office Hadley Centre seasonal forecast system
Strat-trop interaction and Met Office seasonal forecasting
GloSea4: the Met Office Seasonal Forecasting System
MOGREPS developments and TIGGE
Presentation transcript:

© Crown copyright 2007 A fully resolved stratosphere: Impact on seasonal forecasting Alberto Arribas Monthly-to-Decadal area, Met Office Hadley Centre Reading, April 2013

-Ensemble forecast -Dealing with model drift obs. climatology Forecast simulations How do we make seasonal forecasts?

obs All Hindcast runs: ~ 12 members 14 years (96-09) Hindcast mean How do we make seasonal forecasts?

obs Hindcast mean Forecast members How do we make seasonal forecasts?

Bias corrected forecast obs How do we make seasonal forecasts?

Skill of seasonal forecasts Between 1990s and late 2000s, skill had barely improved, still minimal outside tropics

Change of strategy Hindcast length Frequency of system upgrades Centre's priorities JMA ~ 30 yr? ? NCEP ~ 40 yr8 yr Link to re-analysis ECWMF ~ 25 yr5 yr Med-range UK Met Office * 14 yr1 yr Link to model development * Arribas et al., 2011: GloSea4 ensemble prediction system for seasonal forecasting. MWR. 139,

GloSea history -Summer 2009: GloSea4 becomes operational -Nov. 2010: -Vertical high-res (L85 strat. / L75 ocean) -Sea-ice assimilation (concentrations) -Updated hcst ( ) -May 2011: -Monthly system -Nov. 2012: GloSea5! -Horizontal high-res (N216 atm. / 0.25 ocn) -NEMOVAR ODA

Improved GloSea5 Range: 7months Model: HadGEM3 Resolution: N216L85O(0.25)L75 Initialisation: daily, NWP state + NEMOVAR 0.25deg Method: Full field + hindcast bias correction Ensembles: SKEB2 stoch. physics, lagged initialisation Forecasts: Seasonal 2 day -1 : 42 members updated weekly Monthly 2 day -1 : 28 members updated daily Reference: MacLachlan et al., 2013, in prep.

Atmos & land surf: ERA-i Ocean: Seasonal ODA reanalysis Atmos & land surf: NWP anal Ocean/sea-ice : NEMOVAR A coupled system for med-range and ocean forecasting 60 days6 months 6 th Dec th Jan Forecasts Hindcasts 15 days - 24 members - IC perts. from MOGREPS-G - Coupled model as in GloSea5 - Run once a day - Comparison PS32 – PS34 - Operational end13 or 14? New suite:

GloSea5: Skillful NAO predictions! Scaife et al., 2013 Source: MetOffice.gov.uk R=0.60 NAO: November forecast for Dec-Jan-Feb observations forecast

PMSL anomalies from Nov for DJF 05/06 to 09/10 winters

Reasons for skilful NAO forecasts Gulf Stream Bias Wly wind bias => Blocking Deficit No Gulf Stream Bias No Wly wind bias => Good Blocking in N. Atl New Model Scaife et al., Geophys. Res. Lett., Low-res: 1 deg ocean High-res: 0.25 deg ocean

- Courtesy of Warwick Norton -

Not December! As found by Warwick Norton, there is very little skill in December Not a simple persistence of anomalies over the timescale of a few weeks Hints at a possible mechanism in late winter: ENSO/stratosphere => strongest NAO (Ineson and Scaife 2008) From Nick Dunstone

Looking at stratosphere: Data available L38 L85 GloSea4: N96 GloSea5: N

SSWs in L38 and L85 From David Fereday

Obs No Strat Moderate NinoStrong Nino From Anna Maidens

A quick diversion: How good are ENSO forecasts in GloSea5?

Improving ENSO forecasts Obs The westward extension of Nino is a common error in many climate models. It affects remote regions. High-res model has better ENSO pattern and teleconnections Low resolution High resolution

Nino 3.4 SST:ACC / RMSE&Spread ACC higher (good) RMSE reduced (also good) May JJANov DJF GloSea5 (red) GloSea4 (blue)

© Crown copyright Met Office ForecastObserved ENSO Teleconnection: Prec. Nino - Nina DJF JJA

Back to the stratosphere

Importance of stratosphere. Winter Strat. Winds Observations (winter 2012/2013) From Jeff Knight

Forecasts Easterly winds appear at high altitude first First signs in forecasts made on 21 December… Strat. Winds Observations Monthly Forecasts: January 2013 From Jeff Knight

© Crown copyright Met Office First significant Snow Fall ~18 th Jan Forecasters notified from late Dec => increased risk ACTIONABLE DfT notified on 4 th January: …there is now an increasing risk of cold conditions returning later in January and an increased chance of wintry conditions starting later this month… Wintry weather brings disruption to airports, road and rail networks across the UK, with more snow and ice on the way The Guardian 20 th Jan Metro 18 th Jan

Conclusions - GloSea5: High skill predicting winter NAO - Why? High horizontal res.; sea-ice; stratosphere - Skill highest in late winter, role of stratosphere? - Consistent with ENSO/Europe teleconnection through stratosphere and better SSW

Thanks Any questions?

Tropical storm tracks: impact of resolution 1990s ~240 km horizontal resolution 2000s ~120 km horizontal resolution Observations

Today: GloSea5 ~53 km horizontal resolution Observations Tropical storm tracks: impact of resolution