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지균풍×WRF 모델×
분야기상학기상학
계열Process / pipelineProcess / pipeline
기원 연도18572000
창시자Buys Ballot, CoriolisSkamarock and Klemp
유형Wind balance principleAtmospheric simulation system
원전Holton, 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 ↗
별칭Geostrophic wind, Geostrophic balance, Geostrophic approximationWeather Research and Forecasting, WRF, ARW, NMM
관련34
요약Geostrophic 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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