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Bulk Aerodynamic Flux×Monin-Obukhov-Ähnlichkeitstheorie×
FachgebietMeteorologieMeteorologie
FamilieProcess / pipelineProcess / pipeline
Entstehungsjahr19811954
UrheberLarge and PondMonin and Obukhov
TypSurface flux estimation methodSimilarity scaling framework
Wegweisende QuelleLarge, W. G., & Pond, S. (1981). Open ocean momentum flux measurements in moderate to strong winds. Journal of Physical Oceanography, 11(3), 324-336. DOI ↗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. link ↗
AliasnamenBulk aerodynamic approach, Bulk flux parametrization, Aerodynamic bulk methodMonin-Obukhov, Similarity theory, Monin-Obukhov length scale
Verwandt33
ZusammenfassungThe 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.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.
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ScholarGateMethoden vergleichen: Bulk Aerodynamic Flux · Monin-Obukhov Similarity. Abgerufen am 2026-06-20 von https://scholargate.app/de/compare