Krahasoni metodat

	Matodë e kovariancës së turbulencave	HYSPLIT	Teoria e Ngjashmërisë Monin-Obukhov
Fusha	Meteorologji	Meteorologji	Meteorologji
Familja	Process / pipeline	Process / pipeline	Process / pipeline
Viti i origjinës	1951	1997	1954
Krijuesi	Swinbank	Draxler and Hess	Monin and Obukhov
Lloji	Micrometeorological flux measurement	Trajectory and dispersion model	Similarity scaling framework
Burimi themelues	Baldocchi, D. (2003). Assessing the eddy covariance technique for evaluating carbon dioxide fluxes of ecosystems: past, present and future. Global Change Biology, 9(4), 479-492.	Draxler, R. R., & Hess, G. D. (1997). Description of the HYSPLIT_4 modeling system. NOAA Technical Memorandum ERL ARL-224.	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.
Emërtime të tjera	Eddy covariance, EC flux, Eddy correlation, Direct flux measurement	HYSPLIT, Hybrid Single-Particle, Lagrangian trajectory model	Monin-Obukhov, Similarity theory, Monin-Obukhov length scale
Të lidhura	3	3	3
Përmbledhja	The eddy covariance method is a direct, micrometeorological technique that measures turbulent fluxes of momentum, heat, water vapor, and CO2 by computing the covariance between high-frequency fluctuations of wind velocity and scalar properties (temperature, humidity, concentration). It is the gold standard for measuring ecosystem-atmosphere exchanges and validating model parameterizations.	HYSPLIT (Hybrid Single-Particle Lagrangian Integrated Trajectory Model) is a widely used atmospheric transport and dispersion model developed by NOAA's Air Resources Laboratory. It computes air parcel trajectories and pollutant dispersion using Lagrangian tracking to simulate how contaminants and particles move through the atmosphere over hours to weeks.	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.