Goals of KT Theme
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Transcript of Goals of KT Theme
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CCSM AMWG MeetingNCAR, 12-14 Feb. 2008
CAM Diagnostics for the Super CAM
Bill Collins, UCB and LBL
Simulation: Marat Khairoutdinov and Dave RandallAnalysis: Rodger Ames, Mark Branson, Kelley Wittmeyer
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CCSM AMWG MeetingNCAR, 12-14 Feb. 2008
Goals of KT Theme
Improved toolsfor modeling cloudiness
Innovative toolsfor evaluating
simulations
Improved cloudparameterizations
Climate Centers
NWP Centers
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CCSM AMWG MeetingNCAR, 12-14 Feb. 2008
Recommendations & General Action Items(Previous STMs)
Near-term Action Items:• Develop student/post-doc interactions among CMMAP and
modeling centers.
• Subject MMF to same tests used by climate community.
• It is vitally important to analyze MMF in frameworks familiar to modeling centers:– NCAR diagnostic package– GFDL diagnostic package– NCEP diagnostic package
• This will help centers understand the implications of MMF using critical diagnostics for their applications.
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CCSM AMWG MeetingNCAR, 12-14 Feb. 2008
The AMIP Simulation with Super CAM• Simulation:
19-year long AMIP style simulation using the 1985-2004 sea surface temperature (SST) and sea ice distributions
• Manuscript:Evaluation of the simulated interannual and subseasonal variability in an AMIP-style simulation using the CSU Multi-scale Modeling Framework Marat Khairoutdinov, Charlotte DeMott, and David Randall
In press, J. Climate
• Websites for diagnostics:CMMAP -> Research -> Themes -> KT to Centers
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CCSM AMWG MeetingNCAR, 12-14 Feb. 2008
Mean and Variability Diagnostics
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CCSM AMWG MeetingNCAR, 12-14 Feb. 2008
MJO Daily Variability
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NCEP CAM3
Super CAM
As CMMAP has established:
• CAM’s MJO is weak in all measures.• Super CAM has much stronger MJO.
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CCSM AMWG MeetingNCAR, 12-14 Feb. 2008
CRE Cancellation over the Warm Pool?
• Super CAM reproduces correlation of SW and LW CRE found in observations.
• Super CAM tends to overestimate SW cloud forcing over the warm pool.
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CCSM AMWG MeetingNCAR, 12-14 Feb. 2008
Surface Temperature
• Super CAM has small mean errors in surface temperature (by design).
• Super CAM tends to overestimate tropical land surface temperatures.
• Fidelity of high-latitude land surface temperatures is much better than CAM.
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CCSM AMWG MeetingNCAR, 12-14 Feb. 2008
Surface Longwave Fluxes
• Downward longwave fluxes agree with observations.• Net longwave fluxes are affected by temperature biases.
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CCSM AMWG MeetingNCAR, 12-14 Feb. 2008
Surface Radiative Clear-Sky Fluxes
• Largest biases in clear-sky fluxes occur over tropical land.• Biases in longwave from temperature; shortwave from ?
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CCSM AMWG MeetingNCAR, 12-14 Feb. 2008
Next steps• How do MMF and standard physics differ
throughout the life cycle of MJO events?
• Methodology: run MMF and standard physicsside by side on the same model.
• Analysis:– Composite MJO events (in Lagrangian sense?)– Contrast tendencies from MMF and standard physics
• Experimental design to be done in near future.