© Crown copyright Met Office Stratospheric Extension to the CHFP “S-CHFP” and links to WCRP-SPARC Adam Scaife WGSIP July 2010.

Slides:



Advertisements
Similar presentations
© Crown copyright Met Office WCRP Working Group on Seasonal to Interannual Prediction Adam Scaife & Francisco Doblas-Reyes (WGSIP co-chairs)
Advertisements

© Crown copyright Met Office Stratospheric Influences on the Troposphere Adam Scaife December 2010.
Sub-seasonal to seasonal prediction David Anderson.
Predictability of the Stratosphere and Associated Teleconnections
© Crown copyright 2007 A fully resolved stratosphere: Impact on seasonal forecasting Alberto Arribas Monthly-to-Decadal area, Met Office Hadley Centre.
The role of the stratosphere in extended- range forecasting Thomas Jung Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research Germany.
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
Dynamical responses to volcanic forcings in climate model simulations DynVar workshop Matthew Toohey with Kirstin Krüger, Claudia Timmreck, Hauke.
© Crown copyright Met Office The Met Office high resolution seasonal prediction system Anca Brookshaw – Monthly to Decadal Variability and Prediction,
Caio A. S. Coelho Centro de Previsão de Tempo e Estudos Climáticos (CPTEC) Instituto Nacional de Pesquisas Espaciais (INPE) 1 st EUROBRISA.
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,
The dynamical response to volcanic eruptions: sensitivity of model results to prescribed aerosol forcing Matthew Toohey 1 Kirstin Krüger 1,2, Claudia Timmreck.
© Crown copyright Met Office Improving seasonal forecasting: role of teleconnections Madrid. Febrero Alberto Arribas.
Understanding climate model biases in Southern Hemisphere mid-latitude variability Isla Simpson 1 Ted Shepherd 2, Peter Hitchcock 3, John Scinocca 4 (1)
Task: (ECSK06) Regional downscaling Regional modelling with HadGEM3-RA driven by HadGEM2-AO projections National Institute of Meteorological Research (NIMR)/KMA.
The Potential for Skill across the range of the Seamless-Weather Climate Prediction Problem Brian Hoskins Grantham Institute for Climate Change, Imperial.
Validation of the NCEP CFS forecasts Suranjana Saha Environmental Modeling Center NCEP/NWS/NOAA/DOC.
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 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.
Climate System Observations and Prediction Experiment (COPE) Task Force for Seasonal Prediction.
© 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.
Climate Forecasting Unit Prediction of climate extreme events at seasonal and decadal time scale Aida Pintó Biescas.
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,
International CLIVAR Working Group for Seasonal-to- Interannual Prediction (WGSIP) Ben Kirtman (Co-Chair WGSIP) George Mason University Center for Ocean-Land-Atmosphere.
Temperature trends in the upper troposphere/ lower stratosphere as revealed by CCMs and AOGCMs Eugene Cordero, Sium Tesfai Department of Meteorology San.
Hadley Centre © Crown copyright 2004 The CLIVAR International Climate of the Twentieth Century (C20C) Project 1. History and aims 2. Methodology and approach.
Stratospheric harbingers of anomalous weather regimes. M.P. Baldwin and T.J Dunkerton Science, 294:581. Propagation of the Arctic Oscillation from.
CIMA CHFP Data Server.
Decadal prediction  Scientific interest  Meetings and Workshops  Organizational aspects  WGSIP role and activities.
Page 1© Crown copyright 2006 Matt Huddleston With thanks to: Frederic Vitart (ECMWF), Ruth McDonald & Met Office Seasonal forecasting team 14 th March.
Only 1 major sudden stratospheric warming (SSW) observed in SH (2002) but minor warmings occurred in 2009 and 2012 NH events occur in 3 out of every 5.
13 March 20074th C20C Workshop1 Interannual Variability of Atmospheric Circulation in C20C models Simon Grainger 1, Carsten Frederiksen 1 and Xiagou Zheng.
© 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 The Hadley Centre The forcing of sea ice characteristics by the NAO in HadGEM1 UK Sea Ice Workshop, 9 September 2005 Chris.
© Crown copyright Met Office WCRP Working Group on Seasonal to Interannual Prediction Adam Scaife (Met Office) & Francisco Doblas-Reyes (IC3) (WGSIP co-chairs)
© Crown copyright Met Office WMO CBS operational collection/display of seasonal (and sub-seasonal) forecasts Richard Graham, Met Office Hadley Centre.
Stratosphere-Troposhere Coupling in Dynamical Seasonal Predictions Bo Christiansen Danish Meteorological Institute.
What is the Summer North Atlantic Oscillation (SNAO)?
Modes of variability and teleconnections: Part II Hai Lin Meteorological Research Division, Environment Canada Advanced School and Workshop on S2S ICTP,
Decadal Climate Prediction Project (DCPP) © Crown copyright 09/2015 | Met Office and the Met Office logo are registered trademarks Met Office FitzRoy Road,
Slide 1 Thorpex ICSC12 and WWRP SSC7 18 Nov The Sub-seasonal to Seasonal (S2S) Prediction Project 1 “Bridging the gap between weather and climate”
Kristina Fröhlich, (DWD), Daniela Domeisen (Univ. Hamburg), Amy Butler (NOAA), Matthias Bittner (MPI), Wolfgang Müller (MPI), Johanna Baehr (Univ. Hamburg)
Action Items and Recommendations WGSIP-12. Color Coding Items In Black Have Been Completed Items in Red Have No Progress to Date Items In Orange Have.
© 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 Long Range Forecasting and the Stratosphere a SPARC-WGSIP joint project? Adam Scaife October 2009.
The ENSO Signal in Stratospheric Temperatures from Radiosonde Observations Melissa Free NOAA Air Resources Lab Silver Spring 1.
Integrating Climate Science into Adaptation Actions Alberto Arribas Kuala Lumpur, November.
Teleconnection Patterns and Seasonal Climate Prediction over South America The Final Chapter??? Tércio Ambrizzi and Rosmeri P. da Rocha University of São.
Caio A. S. Coelho Centro de Previsão de Tempo e Estudos Climáticos (CPTEC) Instituto Nacional de Pesquisas Espaciais (INPE) 10 th International.
© 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.
Canadian Seasonal to Interannual Prediction System (CanSIPS)
WGSIP Francisco Doblas-Reyes (Barcelona Supercomputing Center BSC-CNS, Spain) William Merryfield (Canadian Centre for Climate Modelling and Analysis, Environment.
Teleconnections in MINERVA experiments
GPC CPTEC: Seasonal forecast activities update
Met Office GPC Adam Scaife Head of Monthly to Decadal Prediction Met Office © Crown copyright Met Office.
WCRP Working Group on Seasonal to Interannual Prediction
ENSO-NAO interactions via the stratosphere
Prospects for Wintertime European Seasonal Prediction
Predictability of the NAO? Adam Scaife
WGSIP16 Tuesday.
Strat-trop interaction and Met Office seasonal forecasting
GloSea4: the Met Office Seasonal Forecasting System
WCRP Working Group on Seasonal to Interannual Prediction
Beyond
Presentation transcript:

© Crown copyright Met Office Stratospheric Extension to the CHFP “S-CHFP” and links to WCRP-SPARC Adam Scaife WGSIP July 2010

© Crown copyright Met Office Climate-system Historical Forecast Project (i) Provide a baseline assessment of our seasonal prediction capabilities using the best available models of the climate system and data for initialisation. (ii) Provide a framework for assessing of current and planned observing systems, and a test bed for integrating process studies and field campaigns into model improvements (iii) Provide an experimental framework for focused research on how various components of the climate system interact and affect one another (iv) Provide a test bed for evaluating IPCC class models in seasonal prediction mode.

© Crown copyright Met Office Dynamical forecast Dynamical forecast + 70hPa stat fcast (Christiansen 2005) Why S-CHFP? (Baldwin and Dunkerton 2001) Surface wind at 60N (Ineson and Scaife, 2009) (Marshall and Scaife 2009) QBO teleconnection ENSO teleconnection

© Crown copyright Met Office Stratospheric extension of the CHFP Hi Top Hindcasts Parallel to WGSIP-CHFP Extended models Initialising extra atmosphere, better represented stratosphere Integrations 4 month lead times (1 st November and 1st May start dates) 2 seasons (DJF and JJA) Case study years: 1989 onwards At least 6 members per year, preferably more

© Crown copyright Met Office Stratospheric extension of the CHFP Basic Diagnostics Monthly means of: surface T, near surface T, precip, pmsl Monthly means of: t (10, 30, 50, 700, 850hPa) u, v (10, 30, 50, 200, 850hPa) Z (10, 30, 50, 500, 850, 1000hPa) Daily values: u, T (10, 30hPa), near surface T, sea level P Extensions Daily precip, Z500 and monthly means to match CMIP5 protocols 12 month forecasts 4 seasons, 10 members 1979 onwards

© Crown copyright Met Office Increased number of participants: InstituteModelResolutionModel top ReferenceContact Met Office HC HadGEM N96L85 N96L38 85km 40km Martin et al 2006, J. Clim., 19, Meteo France Arpege OPA L91 L hPa 10hPa Gueremy et al, 2005, Tellus, 57A, p ECMWF IFS L91 L hPa 5hPa CCCMA CMAM T63L71 T63L41 ~100km ~31km Scinocca et al 2008, ACP, 8, NCEP CFS v1 L64 ? ? Saha et al, J.Clim., vol.19, no.15, p CPTEC ?? IFM- GEOMAR ECHAM5 T63L31 T63L47 10hPa 0.01hPa Roeckner et al 2003, MPI report No. 349, 127pp Manzini et al 2006, J. Clim., 19,

© Crown copyright Met Office SPARC interaction General skill analysis Using standard probabilistic verification measures for different regions - WGSIP Predictions of annular modes? Sudden warmings and intraseasonal predictability Particularly in early part of forecasts ENSO teleconnections Strong evidence of an effect on Europe, perhaps SH too? Interannual predictability from the QBO? Not all models will simulate a QBO but all will initialise it Blocking frequency? Do the high-top models exhibit better blocking stats? Are they linked to SSWs? Attended the SPARC SSG in Oct 2009 on behalf of WGSIP Presented material on strat-trop coupling in S2D prediction Presented WGSIP CHFP and plan for Strat HFP Enthusiastic response - SPARC keen to take part in analysis

© Crown copyright Met Office Timeseries of winter NAO Forecast NAO from forecasts around 1 st Nov Observed NAO (EMSLP gridded, Ansell and Allan 2006) Observed NAO (station data, Jones et al 1997)

© Crown copyright Met Office Current Status Several groups are doing or have done hindcasts with vertically extended models: Meteo France – COMPLETE ECMWF – underway – complete by Dec 2010 UKMO Hadley Centre – underway – complete by Aug 2010 CCCMA – underway – complete by Dec 2010 CPTEC – complete by early 2011 IfM-GEOMAR – complete by Autumn 2010 DATA repository: CIMA (Carolina Vera) kindly agreed to host data parallel to CHFP First files to be uploaded in next few weeks

© Crown copyright Met Office SPARC - DynVar Workshop SPARC DynVar activity is part of the Stratospheric Process and their Role in Climate Project (SPARC). SPARC is a core project of the World Climate Research Program “To determine the dependence of the mean climate, climate variability, and climate change on stratospheric dynamics as represented in Climate Models” Plan to use CMIP5 and S-CHFP results The SPARC DynVar Activity will hold its 2nd Workshop in Boulder, Colorado, USA, 3-5 November 2010 Hosted by CIRES and NOAA in Boulder Colorado, will include a talk on seasonal and stratosphere and S-CHFP For further information and limited travel funds available to support attendance: