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NCAR-GFDL Workshops on Model Development
3 meetings in 2002/2003 Latest this October at GFDL Focus has been on atmospheric models to date; Analogous oceanic effort beginning to form Will also be collaborating through atmospheric and oceanic CPTs
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Global climate sensitivity and cloud feedbacks
Regional climate responses Similarities and differences in model biases Comparing model development strategies, metrics Sharing diagnostics and data
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Currently running 4 100 year simulations with
SST Error Years 71-80 RMS=1.43 Currently running year simulations with 2 atmosphere and 2 ocean configurations; Freezing model by end of month T. Delworth
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GFDL AM2p5 vs NCAR CAM2 B. Soden
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GFDL AM2p12a vs NCAR CAM2x B. Soden
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Trade inversion height
AM2p10 AM2p12 meters S. Klein
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2 meter relative humidity
AM2p10 AM2p12 percent S. Klein
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J. Kiehl
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J. Norris, UCSD
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Compare sensitivities, cloud feedbacks, regional responses
in a hierarchy of model configurations Coupled scenarios 1% per year CO2 increase (CMIP) Equilibrium response with flux-adjusted slab-ocean Response to composite CMIP SST perturbation at time of CO2 doubling “Cess” uniform SST perturbation
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“Cess” Method Uniform ocean warming Measure change in TOA flux.
(-2 K to +2 K). Sea ice is fixed. CO2 is fixed. Measure change in TOA flux.
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A. Broccoli, B. Soden. T. Knutson, and others
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Cloud Feedback in AM2/Cess
(Negative FB) Radiative Damping (W/m2/K) (Positive FB) p12a B. Soden
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Composite CMIP2 SST change
at time of CO2 doubling
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Impact of Structured SST Change
Uniform Warming Structured Warming
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Change in Asian monsoon precipitation
JJA Change in global mean surface T CMIP SSTs ML CAM P. Kushner AM2
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Change in S. American precipitation
DJF Change in global mean surface T CMIP SSTs ML P. Kushner AM2 CAM
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Change in surface Temperature
Annual mean Change in global mean surface T Cess ML AM2 CAM
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Change in zonal mean zonal wind
Annual mean Change in global mean surface T Cess CMIP ML CAM AM2
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Model biases Upper tropospheric/lower stratospheric temperatures
Double ITCZ ENSO regressions (cloud forcing, flux into ocean) Arctic surface pressures
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Annual mean T AM2p12b CAMX
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AM2p12b CAMX
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AM2p12b CAMX
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DJF CAMX AM2p12b
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