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نظرية مونين-أوبوخوف للتشابه×تدفقات الديناميكا الهوائية بالجملة×
المجالعلم الأرصاد الجويةعلم الأرصاد الجوية
العائلةProcess / pipelineProcess / pipeline
سنة النشأة19541981
صاحب الطريقةMonin and ObukhovLarge and Pond
النوعSimilarity scaling frameworkSurface flux estimation method
المصدر التأسيسيMonin, 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 ↗Large, W. G., & Pond, S. (1981). Open ocean momentum flux measurements in moderate to strong winds. Journal of Physical Oceanography, 11(3), 324-336. DOI ↗
الأسماء البديلةMonin-Obukhov, Similarity theory, Monin-Obukhov length scaleBulk aerodynamic approach, Bulk flux parametrization, Aerodynamic bulk method
ذات صلة33
الملخصMonin-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 bulk aerodynamic method estimates surface energy and momentum fluxes from standard meteorological observations. Rather than measuring turbulent fluxes directly, it parameterizes them using measurements of wind speed, temperature, and moisture at a reference height (typically 10 m) and surface conditions, multiplied by empirically derived drag and transfer coefficients.
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ScholarGateقارن الطرق: Monin-Obukhov Similarity · Bulk Aerodynamic Flux. استُرجع بتاريخ 2026-06-20 من https://scholargate.app/ar/compare