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Bill Scheftic Atmo 558 May 6th 2008
The (attempted) development of a cloud model from Fovell’s warm bubble exercise Bill Scheftic Atmo 558 May 6th 2008
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Outline Introduction to model Model Dynamical Core in 3-d
Example of Discretization Kessler Microphysics Basic State No Shear Case Shear Case 00Z May 5, 2007 Case
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Introduction to Model Pseud0-anelastic (flux form equations)
Boussinesq No Coriolis force Time resolution = 2 or 2.5 second Horizontal grid: 500 m 750 m Vertical grid: 500 m to 700 m
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3d - Dynamic Core – flux form
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Discretization – Arakawa-C
Horizontal Vertical j=3 v v k=3 w w j=2 u s u s u k=2 u s u s u j=2 v v k=2 w w j=1 u s u s u k=1 u s u s u j=1 k=1 v v w w i=1 i=1 i=2 i=2 i=3 i=1 i=1 i=2 i=2 i=3
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Example for w-equation
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Kessler Microphysics Modified from WRF code (Kessler 1969, Klemp and Wilhelmson 1978, Wicker and Wilhelmson 1995) Kessler scheme takes in prs, density, temp, Qv, Qc, and Qr Returns a modified value of temp, Qv, Qc, and Qr over a given timestep. Computes, fall velocity of rain drops autoconversion and collection. condensation evaporation of rain Did not implement as tendency, rather updated at every timestep.
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Basic State and Initial Cond.
Initialized sounding has about 1200 J/kg of Cape Tropopause at 12000m Lowest layer approx. 16 g/kg Initial condition 0.7 K temp perturbation 8000 m diameter Hydrostatically balanced at start
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No-Shear
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No-Shear
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No-Shear
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No-Shear
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Shear
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Shear
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Shear
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Shear
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00Z May 5, 2007 Case
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00Z May 5, 2007 Case
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00Z May 5, 2007 Case
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00Z May 5, 2007 Case
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00Z May 5, 2007 Case
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