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	Równanie quasi-geostroficznej prędkości opadania	Wiatr geostroficzny	Inwersja potencjalnej cyrkulacji
Dziedzina	Meteorologia	Meteorologia	Meteorologia
Rodzina	Process / pipeline	Process / pipeline	Process / pipeline
Rok powstania	1970s	1857	1985
Twórca	Trenberth, Omaga	Buys Ballot, Coriolis	Haynes, McIntyre, Hoskins
Typ	Diagnostic equation for vertical motion	Wind balance principle	Diagnostic inversion method
Źródło pierwotne	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.	Haynes, P., & McIntyre, M. E. (1987). On the evolution of vorticity and potential vorticity in the atmosphere. Journal of the Atmospheric Sciences, 44(5), 828-841.
Inne nazwy	QG omega equation, Quasi-geostrophic dynamics, Vertical motion prediction	Geostrophic wind, Geostrophic balance, Geostrophic approximation	PV inversion, Potential vorticity, PV thinking
Pokrewne	3	3	3
Podsumowanie	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.	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.	Potential vorticity (PV) inversion is a diagnostic technique that reconstructs atmospheric wind and pressure fields from the spatial distribution of potential vorticity. This method assumes that, in a geostrophically balanced atmosphere, the PV field uniquely determines the balanced circulation around anomalies.