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Published byΖώσιμος Δάβης Modified over 6 years ago
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CAM3.5 Model and Intraseasonal Variability Changes
Rich Neale and Jadwiga (Yaga) Richter MJO Workshop November 2007
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Modifications CCSM3->CCSM3.5
Provide the best model for biogeochemistry spin-up CCMS4 will be very different Deep Convection Convective momentum transports (Richter) Dilute instead of undilute plume calculation (Neale) Cloud Fraction Polar cloud freeze-drying (Vavrus) Calculation update (Park) Other Model Changes LAND -New hydrology, surface datasets, canopy integration ICE – CSIM to CICE OCEAN – ocean advection scheme Other Changes New chemistry modules (GHGs, aerosols)
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Deep Convection Changes Zhang-McFarlane Scheme (1995)
1. Change from an Undilute to a Dilute Reference Parcel (DIL, Raymond and Blythe, 1986) Improve diurnal cycle over land Sensitivity to tropospheric drying 2. Introduction of Convective Momentum Transports (CMT, Gregory et al. 1997) Include a missing process Decrease excessive surface trades Couple convection and dynamics du/dt = …+d[u’w’]/dz (dq/dt = …+d[q’w’]/dz)
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CAM3 + Convection Changes
Annual Rainfall Error CAM3 CAM3 + Convection Changes
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Annual Surface Stress Error CAM3 + Convection Changes
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Taylor Diagram of Key Metrics
- Improved mean RMSE by 15% Annual Cycle of Monthly Means
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Intra-Seasonal Variance Madden Julian Oscillation (MJO) and Kelvin Waves Deficient OLR (15N-15S)
Observed (NOAA) CAM3
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Intra-Seasonal Variance Improvements
CAM3+CONV CAM3 CAM3+CMT CAM3 CAM3+DIL CAM3
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MJO Variance Winter (November-April)
OLR filtered for MJO wavenumbers (1-5) and periods (30-90days) Winter (November-April) Contour interval 20 (W/m2)2
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MJO Variance Summer (May-October)
OLR filtered for MJO wavenumbers (1-5) and periods (30-90days) Summer (May-October) Contour interval 20 (W/m2)2
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U 850mb Lag Correlation N. Winter N. Summer
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Intra-Seasonal Variance CCSM3
CAM3+CONV CAM3 CCSM3+CONV CCSM3
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MJO Variance Winter (November-April)
OLR filtered for MJO wavenumbers (1-5) and periods (30-90 days) Winter (November-April) Contour interval 20 (W/m2)2
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OLR filtered for MJO wavenumbers (1-5) and periods (30-90days)
MJO Variance OLR filtered for MJO wavenumbers (1-5) and periods (30-90days) Summer (May-October)
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U 850mb Lag Correlation N. Winter N. Summer
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CCSM3 ENSO nino3
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Lag 0 Nino 3 SST Correlation
CCSM3 CCSM3 + Convection Changes
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Lag Regression Lag Correlation w/ Jan Nino3.4 SST’
Obs. CCSM3 Hendon et al. (2007) CCSM3 + CONV
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Taylor Diagram of Key Metrics
- Improved mean RMSE by 10% Annual Cycle of Monthly Means
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Summary CCSM3.5 for biogeochemistry experiments
CMT + Dilution changes dominate in the tropics Reduced excessive trades, improved precip. and mean vertical structure CAM - improved eastward propagation into Pacific, strong westward propagation remains CCSM – MJO power closer to observed, increased propagation coherence MJO disturbances have a significant role to play in improving ENSO, Neale et al. (2007)
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