natural centennial tropical pacific variability in coupled...
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![Page 1: Natural Centennial Tropical Pacific Variability in Coupled ...ocp.ldeo.columbia.edu/res/div/ocp/glodech/PDFs/... · J. Fidel Gonzalez-Rouco3 1LDEO, 2WHOI and 3UCM. Millennial Climate](https://reader034.vdocuments.net/reader034/viewer/2022050323/5f7c82059a0d1f3f5c674453/html5/thumbnails/1.jpg)
Natural CentennialTropical Pacific Variability
in Coupled GCMsJason E. Smerdon1
Kris Karnauskas2
Richard Seager1
J. Fidel Gonzalez-Rouco3
1LDEO, 2WHOI and 3UCM
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Millennial Climate Model SimulationsNCAR CCSM 1.4 Paleo Run (2007)
21 Modeling Groups Performing “Long-Term Experiments”
10 Groups Performing (multiple) Last Millennium Experiments
GKSS ECHO-g FOR2 Paleo Run (2003, 2006)
Coupled Model Intercomparison Project Phase 5(CMIP5)
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CurrentCollection of
Forced TransientMillennial Runs
Gonzalez-Rouco et al., Medieval Climate Anomalyto Little Ice Age transition as simulated by currentclimate models, PAGES news, 19(1), 2011
CSM1.4 and CCSM3ECHO-G: ERIK1 and 2
IPSLMPI-ESM E1 and E2
CNRM
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Model Forcings Since 850GHG Concentrations
Global Cropland/Pasture Area
Schmidt, G. A., et al., 2011: Climate forcing reconstructions for usein PMIP simulations of the last millennium (v1.0), Geosci. ModelDev., 4, 33-45, doi:10.5194/gmd-4-33-2011.
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Model ForcingsSince 850
Volcanic Stratospheric Aerosols
Total Solar Irradiance
Schmidt, G. A., et al., 2011: Climate forcing reconstructions for use inPMIP simulations of the last millennium (v1.0), Geosci. Model Dev., 4,33-45, doi:10.5194/gmd-4-33-2011.
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Observational SST and SLPGradients
Karnauskas, K. B., R. Seager, A. Kaplan, Y. Kushnir, M. A. Cane, 2009: Observed Strengthening of the ZonalSea Surface Temperature Gradient across the Equatorial Pacific Ocean. J. Climate, 22, 4316–4321.
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Observed Trends in the SST Gradient
Karnauskas, K. B., R. Seager, A. Kaplan, Y. Kushnir, M. A. Cane, 2009: Observed Strengthening of the ZonalSea Surface Temperature Gradient across the Equatorial Pacific Ocean. J. Climate, 22, 4316–4321.
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Observed Trends in SST andSLP Gradients
Karnauskas, K. B., R. Seager, A. Kaplan, Y. Kushnir, M. A. Cane, 2009: Observed Strengthening of the ZonalSea Surface Temperature Gradient across the Equatorial Pacific Ocean. J. Climate, 22, 4316–4321.
SST
SLP
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Modeled SST and SLP Climatology
Karnauskas, K. B., R. Seager, A. Kaplan, Y. Kushnir, M. A. Cane, 2009: Observed Strengthening of the ZonalSea Surface Temperature Gradient across the Equatorial Pacific Ocean. J. Climate, 22, 4316–4321.
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Simulated Zonal SST and SLPGradients (Control Runs)
Karnauskas, K. B., J. E. Smerdon, R. Seager and J. F. Gonzalez-Rouco, Patterns of Unforced Centennial–Scale ClimateVariability in the Tropical Pacific, in preparation.
ECHO–G Coupled Climate ModelECHAM4 atmospheric & HOPE–G ocean models
Atm. Resolution: T30 (~3.75°) by 19 levels
Ocean Resolution: T42 (~2.8°; meridional resolutionincreasing to ~0.5° near the equator) by 20 levels
The ECHO–G applies a time-invariant fluxadjustment (heat and freshwater fluxes) to avoidclimate drift
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Trends in Simulated SST Gradients
Karnauskas, K. B., J. E. Smerdon, R. Seager and J. F. Gonzalez-Rouco, Patterns of Unforced Centennial–Scale ClimateVariability in the Tropical Pacific, in preparation.
0.10 - 0.68 °C 0.11 - 0.66 °C -0.4 - 0.64 °C
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Are Low-Frequency OscillationsJust ENSO Modulation?
Karnauskas, K. B., J. E. Smerdon, R. Seager and J. F. Gonzalez-Rouco, Patterns of Unforced Centennial–Scale ClimateVariability in the Tropical Pacific, in preparation.
ObservationsGFDLECHO-G
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Amplitude Modulations in theZebiak-Cane Model
Clement, A. and M. A. Cane, 1999: A role for the tropical Pacificcoupled ocean-atmosphere system on Milankovitch and millenialtimescales. Part I: A modeling study of tropical Pacific variability. In:P.U. Clark and R.S. Webb (Editors), Mechanisms of Millennial-ScaleGlobal Climate Change. 29 Am. Geophys. Union, pp. 363.
NINO3 SSTA
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Are Low-Frequency OscillationsJust ENSO Modulation?
Karnauskas, K. B., J. E. Smerdon, R. Seager and J. F. Gonzalez-Rouco, Patterns of Unforced Centennial–Scale ClimateVariability in the Tropical Pacific, in preparation.
GFDL
ECHO-G
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Are Low-Frequency OscillationsJust ENSO Modulation?
Karnauskas, K. B., J. E. Smerdon, R. Seager and J. F. Gonzalez-Rouco, Patterns of Unforced Centennial–Scale ClimateVariability in the Tropical Pacific, in preparation.
ECHO-G LF Composite ENSO Variability
X X
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Global Patterns
Karnauskas, K. B., J. E. Smerdon, R. Seager and J. F. Gonzalez-Rouco, Patterns of Unforced Centennial–Scale ClimateVariability in the Tropical Pacific, in preparation.
GFDL Low-pass FilteredWP SST Correlations GFDL Composite Pattern
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Composite PatternsGFDL ECHO-G
Karnauskas, K. B., J. E. Smerdon, R. Seager and J. F. Gonzalez-Rouco, Patterns of Unforced Centennial–Scale ClimateVariability in the Tropical Pacific, in preparation.
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Conclusions• If nature exhibits strong natural variability in tropical Pacific SSTs on
centennial time scales, then the assumption that the observed centennialtrend in the SST gradient is a response to radiative forcing is difficult todefend. Nevertheless, the natural variability could strengthen or weaken inthe future as the natural variability evolves and combines (interacts?) withany forced response, clearly having implications for tropical Pacific andglobal climate.
• If the centennial variability in the models is spurious, it is nevertheless acomponent of the models and will continue to influence coupled GCMprojections of future climate, as well as initialized decadal hindcasts andforecasts that are being conducted with these models. In both cases, thenatural centennial variability must be properly phased at the beginning ofthe forecast or projection to isolate the forced change from the spuriousmodeled natural variability.
• Increasing numbers of millennial-length forced transient runs from fullycoupled GCMs will become available over the next several years andshould be an important resources for understanding these simulatedperiods of variability. These simulated periods of variability must also bevalidated against proxy evidence.