विधियों की तुलना करें

	मोनिन-ओबुखोव समानता सिद्धांत	बल्क एयरोडायनामिक फ्लक्स
क्षेत्र	मौसम विज्ञान	मौसम विज्ञान
परिवार	Process / pipeline	Process / pipeline
उद्भव वर्ष	1954	1981
प्रवर्तक	Monin and Obukhov	Large and Pond
प्रकार	Similarity scaling framework	Surface flux estimation method
मौलिक स्रोत	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.
उपनाम	Monin-Obukhov, Similarity theory, Monin-Obukhov length scale	Bulk aerodynamic approach, Bulk flux parametrization, Aerodynamic bulk method
संबंधित	3	3
सारांश	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.