विधियों की तुलना करें

	मोनिन-ओबुखोव समानता सिद्धांत	ऊष्मीय पवन
क्षेत्र	मौसम विज्ञान	मौसम विज्ञान
परिवार	Process / pipeline	Process / pipeline
उद्भव वर्ष	1954	1920s
प्रवर्तक	Monin and Obukhov	Jacobbian insights from geostrophic flow
प्रकार	Similarity scaling framework	Wind-temperature relationship
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.	Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press.
उपनाम	Monin-Obukhov, Similarity theory, Monin-Obukhov length scale	Thermal wind, Vertical wind shear, Barotropic
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 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.