Bandingkan kaedah

	Persamaan Omega Kuasi-Geostrofik	Model WRF
Bidang	Meteorologi	Meteorologi
Keluarga	Process / pipeline	Process / pipeline
Tahun asal	1970s	2000
Pengasas	Trenberth, Omaga	Skamarock and Klemp
Jenis	Diagnostic equation for vertical motion	Atmospheric simulation system
Sumber perintis	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.
Alias	QG omega equation, Quasi-geostrophic dynamics, Vertical motion prediction	Weather Research and Forecasting, WRF, ARW, NMM
Berkaitan	3	4
Ringkasan	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.