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Examine os métodos selecionados lado a lado; as linhas que diferem ficam destacadas.

Fluxo Aerodinâmico Global×Teoria de Similaridade de Monin-Obukhov×
ÁreaMeteorologiaMeteorologia
FamíliaProcess / pipelineProcess / pipeline
Ano de origem19811954
Autor originalLarge and PondMonin and Obukhov
TipoSurface flux estimation methodSimilarity scaling framework
Fonte seminalLarge, 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 ↗
Outros nomesBulk aerodynamic approach, Bulk flux parametrization, Aerodynamic bulk methodMonin-Obukhov, Similarity theory, Monin-Obukhov length scale
Relacionados33
ResumoThe 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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ScholarGateComparar métodos: Bulk Aerodynamic Flux · Monin-Obukhov Similarity. Recuperado em 2026-06-20 de https://scholargate.app/pt/compare