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Convectively Forced Gravity Wave Drag GWD C in the CFS and GFS. Åke Johansson. ACKNOWLEDGEMENTS. Hye-Yeong Chun Jong-Jin Baik In-Sun Song Suranjana Saha Shrinivas Moorthi Hua-Lu Pan Jordan Alpert Huug van den Dool Mark Iredell. OUTLINE. Theory by Chun and Baik 1998
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Convectively ForcedGravity Wave DragGWDCin the CFS and GFS Åke Johansson
ACKNOWLEDGEMENTS Hye-Yeong Chun Jong-Jin Baik In-Sun Song Suranjana Saha Shrinivas Moorthi Hua-Lu Pan Jordan Alpert Huug van den Dool Mark Iredell
OUTLINE • Theory by Chun and Baik 1998 • Parameterization proposed by Chun and Baik 1998 • Climate runs with CFS • Data Assimilation and Week-1 runs with GFS • Conclusions • Suggestions
2-Dimensional x-z Steady-state Non-rotating Hydrostatic Inviscid Boussinesq Linearized – Small perturbations U, N Constant with x and z 0 ; Orographic Forcing Convective Forcing
U = 15 m/s N = 0.007 s-1 Zb = 1.5 km Zt = 11 km a1 = 10 km a2 = 5 a1 To = 273 K Qo = 1 J/kg/s w u
F = -U M Fz = -Uz M
F = -U M M F
F = -U M M F H L
c1 c2 a1 = αΔx c1 = 1.41 c2 = - 0.38 α = 0.1
V Vct Essentially 1-dimensional in the horizontal plane
Wave breaking Reduction of Momentum Flux M F
Lindzen’s Saturation Hypothesis If Reduce wave amplitude so that Ri = ¼ Gives new reduced
Main Reasons for Wave braking Stress Reduction Momentum deposition • Critical levels • Low wind speeds • Low density
Climate runs with CFS SET22 T126L64
Yonsei Univ GCM 2001 4° x 5° ( lat x lon ) Δx ~ 445 Km 15 Layers Top a 1 hPa Perpetual July AMIP integrations for 360 days Last 90 day averages are considered With vs Without GWDC α = 0.4 Encouraging Results NCAR CCM3 2004 T42 Δx ~ 315 Km 18 Layers Top a 2.5 hPa Perpetual January and July AMIP integrations for 3 yrs Last 2 yrs averages are considered With vs Without GWDC α < 0.16 Encouraging Results
CFS Experiments T126L64 Δx ~ 106 Km Top at 0.2 hPa SET22 = Operational CFS + Several updates New Shortwave radiation: Hourly + RRTM1 Longwave Radiation: Hourly + RRTM Realistic CO2 Maximum-random cloud overlap ESMF 3.0.1 Enthalpy equation
Two GWDC Experiments Two different ways in which the momentum compensation within the cloud is distributed
Extreme Negative and Positive Anomalies Stratospheric Polar Night Jet 1971-2000
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DJF GWDC1 1/10 Contour interval