مقایسهٔ روش‌ها

	باد حرارتی	مدل WRF
حوزه	هواشناسی	هواشناسی
خانواده	Process / pipeline	Process / pipeline
سال پیدایش	1920s	2000
پدیدآور	Jacobbian insights from geostrophic flow	Skamarock and Klemp
نوع	Wind-temperature relationship	Atmospheric simulation system
منبع بنیادین	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.
نام‌های دیگر	Thermal wind, Vertical wind shear, Barotropic	Weather Research and Forecasting, WRF, ARW, NMM
مرتبط	3	4
خلاصه	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.