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Thermische wind×WRF Model×
VakgebiedMeteorologieMeteorologie
FamilieProcess / pipelineProcess / pipeline
Jaar van ontstaan1920s2000
GrondleggerJacobbian insights from geostrophic flowSkamarock and Klemp
TypeWind-temperature relationshipAtmospheric simulation system
Oorspronkelijke bronHolton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press. link ↗Skamarock, W. C., Klemp, J. B., Dudhia, J., et al. (2008). A Description of the Advanced Research WRF Version 3. NCAR Technical Note NCAR/TN-475+STR. link ↗
AliassenThermal wind, Vertical wind shear, BarotropicWeather Research and Forecasting, WRF, ARW, NMM
Verwant34
SamenvattingThe thermal wind relationship is a fundamental meteorological principle that links vertical wind shear to horizontal temperature gradients. It states that wind speed increases with height in the direction of warming—a direct consequence of hydrostatic and geostrophic balance combined with the ideal gas law.The Weather Research and Forecasting (WRF) model is a mesoscale atmospheric simulation system used for weather forecasting, research, and climate applications. Developed cooperatively by NCAR, NOAA, and academic institutions, WRF became operational in 2004 and has become one of the most widely used atmospheric models worldwide.
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ScholarGateMethoden vergelijken: Thermal Wind · WRF Model. Geraadpleegd op 2026-06-20 via https://scholargate.app/nl/compare