مقایسهٔ روش‌ها

	باد ژئواستروفیک	مدل WRF
حوزه	هواشناسی	هواشناسی
خانواده	Process / pipeline	Process / pipeline
سال پیدایش	1857	2000
پدیدآور	Buys Ballot, Coriolis	Skamarock and Klemp
نوع	Wind balance principle	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	Geostrophic wind, Geostrophic balance, Geostrophic approximation	Weather Research and Forecasting, WRF, ARW, NMM
مرتبط	3	4
خلاصه	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.