Comparer des méthodes

	Théorie de la similarité de Monin-Obukhov	Flux aérodynamique global	Vent thermique
Domaine	Météorologie	Météorologie	Météorologie
Famille	Process / pipeline	Process / pipeline	Process / pipeline
Année d'origine	1954	1981	1920s
Auteur d'origine	Monin and Obukhov	Large and Pond	Jacobbian insights from geostrophic flow
Type	Similarity scaling framework	Surface flux estimation method	Wind-temperature relationship
Source fondatrice	Monin, 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.	Large, W. G., & Pond, S. (1981). Open ocean momentum flux measurements in moderate to strong winds. Journal of Physical Oceanography, 11(3), 324-336.	Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press.
Alias	Monin-Obukhov, Similarity theory, Monin-Obukhov length scale	Bulk aerodynamic approach, Bulk flux parametrization, Aerodynamic bulk method	Thermal wind, Vertical wind shear, Barotropic
Apparentées	3	3	3
Résumé	Monin-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.	The thermal wind relationship is a fundamental meteorological principle that links vertical wind shear to horizontal temperature gradients. It states that wind speed increases with height in the direction of warming—a direct consequence of hydrostatic and geostrophic balance combined with the ideal gas law.