- Page 1 and 2: ATMOSPHERIC MODELINGNUMERICAL WEATH
- Page 3 and 4: MTO477Brief History of Meteorology
- Page 5: Excerpts from Aristotle’sMeteorol
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Molecular scale (10,000 km)Global w
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Part 1: An Overview ofNumerical Wea
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Highlights1991 (August) - Regional
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Highlights 2000 (January) - Resolut
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Barotropic AtmosphereSurfaces ofcon
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Baroclinic Atmosphere No assumption
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Basic Principles of NWP(Fred Carr)
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Seek equations between variables yo
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Physical ProcessEssential component
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Model FundamentalsModel Components
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Model ComponentsCentralized Guidanc
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Physical Processes in NatureNWP mod
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Parameterizing Physical Processes P
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Parameterizing Sub Grid-Scale Proce
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Impacts of Parameterizing Problems
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IMPACT OF MODEL STRUCTURES&DYNAMICS
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1- NWP EquationsCertain physical la
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2-The Primitive Equations For forec
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Wind Forecast EquationsWest-to-East
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South-to-North ComponentThis equati
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Additional Information: Coriolis Fo
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Continuity Equation In this example
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Moisture Forecast EquationTime chan
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Prognostic/Diagnostic EquationsEqua
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Physical ProcessesThe diabatic heat
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How Models Solve the ForecastEquati
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3-Grid Point: Data Representation I
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4-Grid Point Models As discussed ea
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Additional Information: SimplifiedF
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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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6- Spectral Model : Truncation Effe
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Non-Hydrostatic ModelsNon-hydrostat
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SummaryGRID POINT MODELSCharacteris
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NON-HYDROSTATIC MODELSCharacteristi
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Primitive equations of motion: Set
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6 primitive equations are considere
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Once three conditions are “suitab
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5 Major Steps in the Production of
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Courant-Friederichs-Lewy criteria c
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Hydrostatic vs. Non-Hydrostatic Hyd
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Vertical Resolution Can be set arbi
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ParameterizationThe representation
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3 reasons processes need to be para