- Page 1: ATMOSPHERIC MODELINGNUMERICAL WEATH
- Page 5: Excerpts from Aristotle’sMeteorol
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The Forces of a Parcel of Air
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Atmospheric Model Aerosol processes
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Highlights 1955 - First Operational
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Highlights 1996 - AVN/MRF changed t
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Highlights2001 (November) - Major c
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Equivalent-Barotropic Atmosphere Co
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Thermal Wind (Remember?)The thermal
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Written in general form:tAiA i = de
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Example of a diagnostic equation:Co
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NUMERICAL WEATHER PREDICTIONLECTURE
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Model ComponentsForecast:This repre
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Model ComponentsDynamics:In NWP, dy
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Parameterized Processes and Paramet
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Parameterizing Sub Grid-Scale Proce
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Accounting for the Effects of Physi
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Outlook As computer power increases
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DiscussionThe correct choices are (
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1- NWP EquationsIn NWP, future valu
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2-The Primitive Equations
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Horizontal advection of west-to-eas
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Additional Information: Coriolis Fo
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Additional Information: Coriolis Fo
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Temperature Forecast EquationTime c
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Hydrostatic or Vertical MomentumEqu
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Physical ProcessesAll of the foreca
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How Models Solve the ForecastEquati
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Representing the Forecast Variables
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3-Grid Point: Data RepresentationGr
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4-Grid Point ModelsIn the real atmo
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5- SPECTRAL MODELHow Data are Repre
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Use of Grid Point Methods in Spectr
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Impacts of Grid Point Physics Calcu
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7- Hydrostatic Models Most grid poi
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Non-Hydrostatic Models In addition,
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HYDROSTATIC MODELS Characteristics
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References Carr, F.H., 1988: Introd
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The dependent variables in this set
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Problems in finding suitable latera
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Conditions whichOnemakeBIGthe primi
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Courant-Friederichs-Lewy criteria C
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Setting up a Numerical Model Grid p
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Horizontal resolution Horizontal re
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Sigma Coordinate System (σ)p• De
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Convective ParameterizationSchemes
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«Computations indicate that a perf