Porovnat metody

	Geostrofický vítr	Kvazi-geostrofická rovnice pro omega
Obor	Meteorologie	Meteorologie
Rodina	Process / pipeline	Process / pipeline
Rok vzniku	1857	1970s
Tvůrce	Buys Ballot, Coriolis	Trenberth, Omaga
Typ	Wind balance principle	Diagnostic equation for vertical motion
Původní zdroj	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.
Další názvy	Geostrophic wind, Geostrophic balance, Geostrophic approximation	QG omega equation, Quasi-geostrophic dynamics, Vertical motion prediction
Příbuzné	3	3
Shrnutí	Geostrophic wind balance is a fundamental concept in meteorology that describes the balance between the pressure gradient force and the Coriolis force in large-scale atmospheric flow. When this balance is achieved, wind blows parallel to isobars without acceleration—a condition observed in the free atmosphere away from the equator and surface boundary layer.	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.