Võrdle meetodeid

	Termiline tuul	WRF mudel
Valdkond	Meteoroloogia	Meteoroloogia
Perekond	Process / pipeline	Process / pipeline
Tekkeaasta	1920s	2000
Looja	Jacobbian insights from geostrophic flow	Skamarock and Klemp
Tüüp	Wind-temperature relationship	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	Thermal wind, Vertical wind shear, Barotropic	Weather Research and Forecasting, WRF, ARW, NMM
Seotud	3	4
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.	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.