Uporedite metode

	Квазигеострофичка Омега једначина	WRF Модел
Oblast	Meteorologija	Meteorologija
Porodica	Process / pipeline	Process / pipeline
Godina nastanka	1970s	2000
Tvorac	Trenberth, Omaga	Skamarock and Klemp
Tip	Diagnostic equation for vertical motion	Atmospheric simulation system
Temeljni izvor	Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press.	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.
Drugi nazivi	QG omega equation, Quasi-geostrophic dynamics, Vertical motion prediction	Weather Research and Forecasting, WRF, ARW, NMM
Srodne	3	4
Sažetak	The 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.