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Geophysical Fluid Dynamics Laboratory Review

Geophysical Fluid Dynamics Laboratory Review. June 30 - July 2, 2009. Seasonal-Decadal Predictability, Prediction and Ensemble Coupled Data Assimilation. Presented by Tony Rosati. Key Questions.

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Geophysical Fluid Dynamics Laboratory Review

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  1. Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009

  2. Seasonal-Decadal Predictability, Prediction and Ensemble Coupled Data Assimilation Presented by Tony Rosati

  3. Key Questions • What seasonal-decadal predictability exists in the climate system, and what are the mechanisms responsible for that predictability? • To what degree is the identified predictability (and associated climatic impacts) dependent on model formulation? • Are current and planned initialization and observing systems adequate to initialize models for decadal prediction? • Is the identified decadal predictability of societal relevance? 3

  4. Ensemble Coupled Data Assimilation (ECDA) is at the heart of prediction efforts • Provides initial conditions for Seasonal-Decadal Prediction • Provides validation for predictions and model development • Ocean Analysis kept current and available on GFDL website • Active participation in CLIVAR/GSOP intercomparisons

  5. GHGNA forcings Atmosphere model obs PDF Prior PDF u, v, t, q, ps Land model uo, vo, to τx,τy (Qt,Qq) Data Assim (Filtering) Analysis PDF Sea-Ice model Ocean model T,S,U,V Tobs,Sobs Pioneering development of coupled data assimilation system • Ensemble CoupledData Assimilation estimates the temporally-evolving probability distribution of climate states under observational data constraint: • Multi-variate analysis maintains physical balances between state variables such as T-S relationship – primarily geostrophic balance • Ensemble filter maintains the nonlinearity of climate evolution • All coupled components adjusted by observed data through instantaneously-exchanged fluxes • Optimal ensemble initialization of coupled model with minimum initialization shocks OAR 2008 Outstanding Paper Award: S. Zhang, M. J. Harrison, A. Rosati, and A. Wittenberg

  6. New coupled assimilation system dramaticallyimproves ENSO prediction skill J F M A M J J A S O N D Forecast Start Month ECDA Forecast Lead Time (months)‏ 1 3 5 7 9 11 J F M A M J J A S O N D Forecast Start Month NINO3 ACC 0.6 Forecast Lead Time (months)‏ 1 3 5 7 9 11 3D-variational assimilation system GFDL participating CTB/NCEP/National MME, IRI and APCC

  7. ECDA research activities to improve initialization • Multi-model ECDA to help mitigate bias • Fully coupled model parameter estimation within ECDA • ECDA in high resolution CGCM • Assess additional predictability from full depth ARGO profilers

  8. Decadal Potential Predictabilitywith a focus on the Atlantic • How well does the ECDA system constrain the AMOC? • Given that the ocean observing system is non-stationary, what impact does that have on the AMOC predictability? • What are the sources of AMOC predictability and how dependent are they to the various observing networks ? We use a “perfect model” framework to address these questions Results: The ARGO network outperforms the XBT network in both assimilation and forecast skill in idealized experiments

  9. Key goal: assess whether climate projections for the next several decades can be enhanced when the models are initialized from observed state of the climate system. Use ECDA for initial conditions from “observed state” Produce ocean reanalysis 1970-2009 Use “workhorse” CM2.1 model from IPCC AR4 [2009] Decadal hindcasts from 1980 onwards (10 member ensembles) Decadal predictions starting from 2001 onwards (10 member ensembles) Use experimental high resolution model (if scientifically warranted) [2010] Decadal predictions starting from 2001 onwards (10 member ensembles) Use CM3 model for IPCC AR5 [2010, tentative] Decadal predictions starting from 2001 onwards (10 member ensemble) GFDL Decadal Prediction Research in support of IPCC AR5 9

  10. Summary • Development of new advanced assimilation techniques using coupled climate models • Apply these techniques to detecting climate change while providing estimates of their uncertainty • Improve our understanding of predictability at decadal time scales • Provide a foundation for the development of a NOAA capability for decadal predictions

  11. Geophysical Fluid Dynamics Laboratory Review June 30 - July 2, 2009

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