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رياح جيواستروفيك×نموذج WRF×
المجالعلم الأرصاد الجويةعلم الأرصاد الجوية
العائلةProcess / pipelineProcess / pipeline
سنة النشأة18572000
صاحب الطريقةBuys Ballot, CoriolisSkamarock and Klemp
النوعWind balance principleAtmospheric simulation system
المصدر التأسيسيHolton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press. link ↗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. link ↗
الأسماء البديلةGeostrophic wind, Geostrophic balance, Geostrophic approximationWeather Research and Forecasting, WRF, ARW, NMM
ذات صلة34
الملخصGeostrophic 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.
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ScholarGateقارن الطرق: Geostrophic Wind · WRF Model. استُرجع بتاريخ 2026-06-18 من https://scholargate.app/ar/compare