Võrdle meetodeid

	Termiline tuul	Geostroofiline tuul
Valdkond	Meteoroloogia	Meteoroloogia
Perekond	Process / pipeline	Process / pipeline
Tekkeaasta	1920s	1857
Looja	Jacobbian insights from geostrophic flow	Buys Ballot, Coriolis
Tüüp	Wind-temperature relationship	Wind balance principle
Algallikas	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.
Rööpnimetused	Thermal wind, Vertical wind shear, Barotropic	Geostrophic wind, Geostrophic balance, Geostrophic approximation
Seotud	3	3
Kokkuvõte	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.	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.