เปรียบเทียบวิธี

	Eddy Covariance	HYSPLIT
สาขาวิชา	อุตุนิยมวิทยา	อุตุนิยมวิทยา
ตระกูล	Process / pipeline	Process / pipeline
ปีกำเนิด	1951	1997
ผู้ริเริ่ม	Swinbank	Draxler and Hess
ประเภท	Micrometeorological flux measurement	Trajectory and dispersion model
แหล่งต้นตำรับ	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.
ชื่อเรียกอื่น	Eddy covariance, EC flux, Eddy correlation, Direct flux measurement	HYSPLIT, Hybrid Single-Particle, Lagrangian trajectory model
ที่เกี่ยวข้อง	3	3
สรุป	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.