Slayt 1 - RTC, Regional Training Centre - Turkey

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Atmospheric Model Aerosol processes (Microphysics) Nucleation/condensation Phase changes Cloud processes Conden./evap./deposition/sublim. Precipitation Stability (Vertical/Slantwise Ascent) Convection Entrainment Radiative transfer UV/visible/near-IR/thermal-IR Scattering/absorption Snow, ice, water albedosMeteorological processes Velocity Geopotential Pressure Water vapor Temperature Density TurbulenceSurface processes Temperatures and water content of Soil Water Snow Sea ice Vegetation Roads Roofs Surface energy/moisture fluxes Ocean-atmosphere exchange Ocean dynamics, chemistry
Part 1: An Overview ofNumerical WeatherPrediction
Page 1 and 2:
ATMOSPHERIC MODELINGNUMERICAL WEATH
Page 3 and 4:
MTO477Brief History of Meteorology
Page 5:
Excerpts from Aristotle’sMeteorol
Page 72: The Forces of a Parcel of Air
Page 86 and 87: Highlights 1955 - First Operational
Page 88 and 89: Highlights 1996 - AVN/MRF changed t
Page 90 and 91: Highlights2001 (November) - Major c
Page 92 and 93: Equivalent-Barotropic Atmosphere Co
Page 94 and 95: Thermal Wind (Remember?)The thermal
Page 96 and 97: Written in general form:tAiA i = de
Page 98 and 99: Example of a diagnostic equation:Co
Page 100 and 101: NUMERICAL WEATHER PREDICTIONLECTURE
Page 102 and 103: Model ComponentsForecast:This repre
Page 104 and 105: Model ComponentsDynamics:In NWP, dy
Page 106 and 107: Parameterized Processes and Paramet
Page 108 and 109: Parameterizing Sub Grid-Scale Proce
Page 110 and 111: Accounting for the Effects of Physi
Page 112 and 113: Outlook As computer power increases
Page 114 and 115: DiscussionThe correct choices are (
Page 116 and 117: 1- NWP EquationsIn NWP, future valu
Page 118 and 119: 2-The Primitive Equations
Page 120 and 121: Horizontal advection of west-to-eas
Page 122 and 123: Additional Information: Coriolis Fo
Page 124 and 125: Additional Information: Coriolis Fo
Page 126 and 127: Temperature Forecast EquationTime c
Page 128 and 129: Hydrostatic or Vertical MomentumEqu
Page 130 and 131: Physical ProcessesAll of the foreca
Page 132 and 133: How Models Solve the ForecastEquati
Page 134 and 135:
Representing the Forecast Variables
Page 136 and 137:
3-Grid Point: Data RepresentationGr
Page 138 and 139:
4-Grid Point ModelsIn the real atmo
Page 140 and 141:
5- SPECTRAL MODELHow Data are Repre
Page 142 and 143:
Use of Grid Point Methods in Spectr
Page 144 and 145:
Impacts of Grid Point Physics Calcu
Page 146 and 147:
7- Hydrostatic Models Most grid poi
Page 148 and 149:
Non-Hydrostatic Models In addition,
Page 151 and 152:
HYDROSTATIC MODELS Characteristics
Page 153 and 154:
References Carr, F.H., 1988: Introd
Page 155 and 156:
The dependent variables in this set
Page 157 and 158:
Problems in finding suitable latera
Page 159 and 160:
Conditions whichOnemakeBIGthe primi
Page 161 and 162:
Courant-Friederichs-Lewy criteria C
Page 163 and 164:
Setting up a Numerical Model Grid p
Page 165 and 166:
Horizontal resolution Horizontal re
Page 167 and 168:
Sigma Coordinate System (σ)p• De
Page 169 and 170:
Convective ParameterizationSchemes
Page 171:
«Computations indicate that a perf
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Slayt 1 - RTC, Regional Training Centre - Turkey

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