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Climate Modelling for Ireland   Ray McGrath, Met Éireann  EPA Climate Change Conference, 30 June 2010, Aviva Stadium, Dublin
Outline ,[object Object],[object Object],[object Object]
History ,[object Object],[object Object],[object Object],[object Object]
History ,[object Object],[object Object],[object Object],[object Object]
History ,[object Object],[object Object],[object Object],[object Object]
Average number of days per month with ground frost (1961-1990) ‏ EU ENSEMBLES Project – European Climate (2004 – 2009) ‏ ENSEMBLES : EU FP6-funded project involving 66 institutes (including Met Éireann) from 20 countries.  Goal: Run  ensembles  of different climate models to sample  uncertainties Assess  reliability  of models for historical periods Working towards a  probabilistic  framework for  projections  of climate change Focus: season, decadal, centennial; global, regional and local.  Applications of societal relevance ENSEMBLES has produced ~25 regional climate simulation datasets for Europe; also 7 global simulations.
EU ENSEMBLES Project – European Climate (Sep 2004 – Dec 2009) ‏ C4I contribution: 2 centennial simulations over Europe
EU ENSEMBLES Project – European Climate (Sep 2004 – Dec 2009) ‏ Source: van der Linden P., and J.F.B. Mitchell (eds.) 2009: ENEMBLES: Climate Change and its Impacts: Summary of research and results from the ENSEMBLES project.
Flood or drought? Change in river Suck discharge: 2021-2060 relative to 1961-2000. Based on 13 ENSEMBLES simulations. EU ENSEMBLES Project: local applications
ENSEMBLES/C4I: expected change (%) in seasonal rainfall 2021-2050 compared with 1961-1990  (mean of 20 climate model simulations) Winter Spring Summer Autumn But large spread between the simulations…  too much uncertainty
ENSEMBLES/C4I RCM simulations have highlighted the uncertainty in precipitation forecasts. Example: expected winter change (%)  2021-2050  compared with 1961-1990 20 member ensemble 12 member ensemble Spread reflects model differences. GHG emission uncertainty is not included (same in all simulations) .
ENSEMBLES: expected change (%) in seasonal rainfall  2071-2100  compared with 1961-1990 (mean of 12 climate model simulations) Winter Spring Summer Autumn
Lessons learned from C4I/ENSEMBLES ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
In 2007 Met Éireann /ICHEC / UCD became partners in  EC-Earth , a consortium of European Weather Services and Institutes (~23 in total) established to develop and use a common global Earth System Model: atmosphere, ocean/sea-ice, land, atmospheric chemistry, Carbon cycle – unified within a single package.  EC-Earth modelling work will feed into the next IPCC Assessment Report Climate modelling in Met Éireann: moving to the global scale
[object Object],[object Object],[object Object],Background to EC-Earth
Joint EC-Earth and ECMWF seasonal forecast components Planned EC-Earth components For CMIP5: T159L62, 1 deg Ocean On 6 platforms OASIS Atmosphere GCM: IFS Ocean GCM: NEMO Sea-ice:LIM2/3 Land: IFS H-tessel Atmospheric Chemistry  and aerosols: TM5 Vegetation: LPJ Marine ecosystem: PISCES New EC-Earth components
Timeline Testing/tuning –> Spin-up runs –> CMIP5 runs An  ensemble  of simulations planned  –  distributed among partners Test phase Historical run + Initialized Decadal hindcasts ~900 yrs 1850 2005 Pre-industrial Spin-up 2 independent simulations by Met  É ireann / ICHEC and DMI/KNMI. RCP runs 2100
CMIP5 - Coupled Model Intercomparison Project Phase 5 ,[object Object],[object Object],[object Object]
CMIP5 - Coupled Model Intercomparison Project Phase 5 ,[object Object],[object Object],[object Object],[object Object],“ Long-Term” (century & longer, 2100/2300) TIER 1 TIER 2 CORE “ realistic” diagnostic “ Near-Term” (decadal) (initialized ocean state) prediction & predictability CORE TIER 1
CMIP5 - Coupled Model Intercomparison Project Phase 5 ,[object Object],[object Object],[object Object],[object Object],[object Object]
Irish partner ICHEC: Designated Earth System Grid ‘Data Node’ through  e-INIS   (the Irish National e-Infrastructure) PCMDI - Program for Climate Model Diagnosis and Intercomparison  BADC -  British Atmospheric Data Centre ICHEC – Irish Centre for High-End Computing ICHEC
Met  É ireann / ICHEC schedule of EC-Earth simulations: CMIP5 Commitment ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Met  É ireann / ICHEC schedule of EC-Earth  simulations for local use ,[object Object],[object Object],[object Object],[object Object],How Ireland/UK elevations “appear” on the 25km global EC-Earth grid
 
EC-Earth spin-up event: change in the meridional overturning circulation (MOC) after ~500 years and recovery SST Anomaly during MOC decrease Cold spell lasted ~50 years, lagged MOC decline by ~20 years…  An unforced event simulated by the model (no influx of fresh water into the N. Atlantic, etc.)
EC-Earth spin-up event: changes in the average SST (anomalies) over the Atlantic SST oscillations ~40 year cycle – similar to observed Atlantic Multidecadal Oscillation. Cold dip an echo of 8.2kyr event in Holocene? Relative year
Data source: http://www.ncdc.noaa.gov/paleo/pubs/alley2000/alley2000.htm 8.2kyr cold event   Central Greenland reconstructed temperature   8.2kyr event linked with drainage of glacial lake into N. Atlantic… but may be simply ‘natural variability’ as seen in EC-Earth simulation
Regional models not neglected: coupled atmosphere-ocean regional climate model (RCA_NEMO) developed System evaluated by simulating climate over the above area 1961-1990 and comparing against ERA-40 reanalysis data.
[object Object],[object Object],[object Object],[object Object],[object Object],Coupled atmosphere-ocean  regional  climate model
Greenland 5 km DEM, Ice Thickness, and Bedrock Elevation Grids ,[object Object],[object Object],[object Object],[object Object]
Future Plans EC-Earth outputs (particularly the decadal simulations) will be used to investigate changes in weather extremes e.g. rainfall. Selected outputs downscaled to 2-5km grid. Outputs will be freely available to drive applications to study local impacts of climate change (flooding, storm surge, coastal erosion, renewable energy – wind/wave, agriculture, forestry,… Empirical Orthogonal Function (EOF) analysis of annual Irish rainfall (1941-2009). The time evolution of the Principle Component for the first mode is shown with a 5-year running trend line. Where is the climate heading?
Acknowledgements ,[object Object],[object Object],[object Object],[object Object],[object Object]

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Climate Modelling for Ireland -Dr Ray McGrath, Met Eireann

  • 1. Climate Modelling for Ireland Ray McGrath, Met Éireann EPA Climate Change Conference, 30 June 2010, Aviva Stadium, Dublin
  • 2.
  • 3.
  • 4.
  • 5.
  • 6. Average number of days per month with ground frost (1961-1990) ‏ EU ENSEMBLES Project – European Climate (2004 – 2009) ‏ ENSEMBLES : EU FP6-funded project involving 66 institutes (including Met Éireann) from 20 countries. Goal: Run ensembles of different climate models to sample uncertainties Assess reliability of models for historical periods Working towards a probabilistic framework for projections of climate change Focus: season, decadal, centennial; global, regional and local. Applications of societal relevance ENSEMBLES has produced ~25 regional climate simulation datasets for Europe; also 7 global simulations.
  • 7. EU ENSEMBLES Project – European Climate (Sep 2004 – Dec 2009) ‏ C4I contribution: 2 centennial simulations over Europe
  • 8. EU ENSEMBLES Project – European Climate (Sep 2004 – Dec 2009) ‏ Source: van der Linden P., and J.F.B. Mitchell (eds.) 2009: ENEMBLES: Climate Change and its Impacts: Summary of research and results from the ENSEMBLES project.
  • 9. Flood or drought? Change in river Suck discharge: 2021-2060 relative to 1961-2000. Based on 13 ENSEMBLES simulations. EU ENSEMBLES Project: local applications
  • 10. ENSEMBLES/C4I: expected change (%) in seasonal rainfall 2021-2050 compared with 1961-1990 (mean of 20 climate model simulations) Winter Spring Summer Autumn But large spread between the simulations… too much uncertainty
  • 11. ENSEMBLES/C4I RCM simulations have highlighted the uncertainty in precipitation forecasts. Example: expected winter change (%) 2021-2050 compared with 1961-1990 20 member ensemble 12 member ensemble Spread reflects model differences. GHG emission uncertainty is not included (same in all simulations) .
  • 12. ENSEMBLES: expected change (%) in seasonal rainfall 2071-2100 compared with 1961-1990 (mean of 12 climate model simulations) Winter Spring Summer Autumn
  • 13.
  • 14. In 2007 Met Éireann /ICHEC / UCD became partners in EC-Earth , a consortium of European Weather Services and Institutes (~23 in total) established to develop and use a common global Earth System Model: atmosphere, ocean/sea-ice, land, atmospheric chemistry, Carbon cycle – unified within a single package. EC-Earth modelling work will feed into the next IPCC Assessment Report Climate modelling in Met Éireann: moving to the global scale
  • 15.
  • 16. Joint EC-Earth and ECMWF seasonal forecast components Planned EC-Earth components For CMIP5: T159L62, 1 deg Ocean On 6 platforms OASIS Atmosphere GCM: IFS Ocean GCM: NEMO Sea-ice:LIM2/3 Land: IFS H-tessel Atmospheric Chemistry and aerosols: TM5 Vegetation: LPJ Marine ecosystem: PISCES New EC-Earth components
  • 17. Timeline Testing/tuning –> Spin-up runs –> CMIP5 runs An ensemble of simulations planned – distributed among partners Test phase Historical run + Initialized Decadal hindcasts ~900 yrs 1850 2005 Pre-industrial Spin-up 2 independent simulations by Met É ireann / ICHEC and DMI/KNMI. RCP runs 2100
  • 18.
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  • 20.
  • 21. Irish partner ICHEC: Designated Earth System Grid ‘Data Node’ through e-INIS (the Irish National e-Infrastructure) PCMDI - Program for Climate Model Diagnosis and Intercomparison BADC - British Atmospheric Data Centre ICHEC – Irish Centre for High-End Computing ICHEC
  • 22.
  • 23.
  • 24.  
  • 25. EC-Earth spin-up event: change in the meridional overturning circulation (MOC) after ~500 years and recovery SST Anomaly during MOC decrease Cold spell lasted ~50 years, lagged MOC decline by ~20 years… An unforced event simulated by the model (no influx of fresh water into the N. Atlantic, etc.)
  • 26. EC-Earth spin-up event: changes in the average SST (anomalies) over the Atlantic SST oscillations ~40 year cycle – similar to observed Atlantic Multidecadal Oscillation. Cold dip an echo of 8.2kyr event in Holocene? Relative year
  • 27. Data source: http://www.ncdc.noaa.gov/paleo/pubs/alley2000/alley2000.htm 8.2kyr cold event Central Greenland reconstructed temperature 8.2kyr event linked with drainage of glacial lake into N. Atlantic… but may be simply ‘natural variability’ as seen in EC-Earth simulation
  • 28. Regional models not neglected: coupled atmosphere-ocean regional climate model (RCA_NEMO) developed System evaluated by simulating climate over the above area 1961-1990 and comparing against ERA-40 reanalysis data.
  • 29.
  • 30.
  • 31. Future Plans EC-Earth outputs (particularly the decadal simulations) will be used to investigate changes in weather extremes e.g. rainfall. Selected outputs downscaled to 2-5km grid. Outputs will be freely available to drive applications to study local impacts of climate change (flooding, storm surge, coastal erosion, renewable energy – wind/wave, agriculture, forestry,… Empirical Orthogonal Function (EOF) analysis of annual Irish rainfall (1941-2009). The time evolution of the Principle Component for the first mode is shown with a 5-year running trend line. Where is the climate heading?
  • 32.

Hinweis der Redaktion

  1. Rep. Con. Pathways: 2.6, 4.5, 8.5 W/m2.
  2. CMIP5 is meant to provide a framework for coordinated climate change experiments for the next five years and thus includes simulations for assessment in the AR5 as well as others that extend beyond the AR5. CMIP5 is not, however, meant to be comprehensive; it cannot possibly include all the different model intercomparison activities
  3. 0.25 degree atmosphere/ocean; 3-hour coupling; heat and momentum fluxes to the ocean; NEMO returns SST.