Compara mètodes

	Vent tèrmic	L'equació omega quasi-geotròfica
Camp	Meteorologia	Meteorologia
Família	Process / pipeline	Process / pipeline
Any d'origen	1920s	1970s
Autor original	Jacobbian insights from geostrophic flow	Trenberth, Omaga
Tipus	Wind-temperature relationship	Diagnostic equation for vertical motion
Font seminal	Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press.	Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press.
Àlies	Thermal wind, Vertical wind shear, Barotropic	QG omega equation, Quasi-geostrophic dynamics, Vertical motion prediction
Relacionats	3	3
Resum	The 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 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.