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Théorie de la similarité de Monin-Obukhov×Modèle WRF×
DomaineMétéorologieMétéorologie
FamilleProcess / pipelineProcess / pipeline
Année d'origine19542000
Auteur d'origineMonin and ObukhovSkamarock and Klemp
TypeSimilarity scaling frameworkAtmospheric simulation system
Source fondatriceMonin, A. S., & Obukhov, A. M. (1954). Basic laws of turbulent mixing in the ground layer of the atmosphere. Tr. Akad. Nauk SSSR, 24, 163-187. 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 ↗
AliasMonin-Obukhov, Similarity theory, Monin-Obukhov length scaleWeather Research and Forecasting, WRF, ARW, NMM
Apparentées34
RésuméMonin-Obukhov similarity theory is a fundamental framework in boundary layer meteorology that describes how wind speed, temperature, and humidity vary with height near the surface. Published in 1954, it shows that normalized vertical profiles depend on a single dimensionless parameter—the Monin-Obukhov stability parameter—which quantifies the balance between mechanical turbulence and buoyant convection.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.
ScholarGateJeu de données
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ScholarGateComparer des méthodes: Monin-Obukhov Similarity · WRF Model. Consulté le 2026-06-20 sur https://scholargate.app/fr/compare