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Published byChloe Todd Modified over 8 years ago
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Understanding Forecast Skill What is the Overall Limit of Predictability? What Limits Predictability? –Uncertainty in Initial Conditions: Chaos within Non-Linear Dynamics of the Coupled System –Uncertainty as the System Evolves: External Stochastic Effects Model Dependence? –Model Error
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CFSIE - Reduce Noise Version (interactive ensemble) of CFS
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RMS(Obs)*1.4 CFSIE RMSE CFS Spread CFS RMSE CFSIE Spread
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Western Pacific Problem Hypothesis: Atmospheric Internal Dynamics (Stochastic Forcing) is Occurring on Space and Time Scales that are Too Coherent Too Coherent Oceanic Response Excessive Ocean Forcing Atmosphere Test: Add White Noise to Latent Heat Flux
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Contemporaneous Latent Heat Flux - SST Correlation Control Coupled Model Increased “Randomness” Coupled Model Add White Noise in Space and Time to Latent Heat Flux in the Western Pacific (Ad-Hoc) Observational Estimates Based on NASA GFSST2 Data
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SST OGCM rand (1, …, N) Sfc Fluxes 1 AGCM 1 Sfc Fluxes 2 AGCM 2 Sfc Fluxes N AGCM N Selected Member’s Sfc Fluxes Random Interactive Ensemble Approach Ensemble of N AGCMs all receive same OGCM-output SST each day OGCM receives output of single, randomly-selected AGCM each day Randomly select 1 member’s surface fluxes each day
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Standard IERandom IE Nino34 Regression on Equatorial Pacific SSTA
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Nino3.4 Power Spectra Period (months) Increasing Stochastic Atmospheric Forcing Increase the ENSO Period Reduced Stochastic Atmospheric Forcing Moderate Stochastic Atmospheric Forcing Increased Stochastic Atmospheric Forcing
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