Võrdle meetodeid

	Geostroofiline tuul	WRF mudel
Valdkond	Meteoroloogia	Meteoroloogia
Perekond	Process / pipeline	Process / pipeline
Tekkeaasta	1857	2000
Looja	Buys Ballot, Coriolis	Skamarock and Klemp
Tüüp	Wind balance principle	Atmospheric simulation system
Algallikas	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.
Rööpnimetused	Geostrophic wind, Geostrophic balance, Geostrophic approximation	Weather Research and Forecasting, WRF, ARW, NMM
Seotud	3	4
Kokkuvõte	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 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.