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Kvazigeostrofiskā omega vienādojums×Modelis WRF×
NozareMeteoroloģijaMeteoroloģija
SaimeProcess / pipelineProcess / pipeline
Izcelsmes gads1970s2000
AutorsTrenberth, OmagaSkamarock and Klemp
TipsDiagnostic equation for vertical motionAtmospheric simulation system
PirmavotsHolton, 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 ↗
Citi nosaukumiQG omega equation, Quasi-geostrophic dynamics, Vertical motion predictionWeather Research and Forecasting, WRF, ARW, NMM
Saistītās34
KopsavilkumsThe quasi-geostrophic (QG) omega equation is a fundamental diagnostic equation in synoptic meteorology that relates vertical motion (omega = dP/dt) to horizontal temperature and vorticity fields. It predicts where air rises and sinks based on the geostrophic flow structure without explicitly solving for vertical velocity.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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ScholarGateSalīdzināt metodes: Quasi-Geostrophic Omega Equation · WRF Model. Izgūts 2026-06-20 no https://scholargate.app/lv/compare