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Pöörisvoogude meetod (Eddy Covariance)×HYSPLIT×
ValdkondMeteoroloogiaMeteoroloogia
PerekondProcess / pipelineProcess / pipeline
Tekkeaasta19511997
LoojaSwinbankDraxler and Hess
TüüpMicrometeorological flux measurementTrajectory and dispersion model
AlgallikasBaldocchi, 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. DOI ↗Draxler, R. R., & Hess, G. D. (1997). Description of the HYSPLIT_4 modeling system. NOAA Technical Memorandum ERL ARL-224. link ↗
RööpnimetusedEddy covariance, EC flux, Eddy correlation, Direct flux measurementHYSPLIT, Hybrid Single-Particle, Lagrangian trajectory model
Seotud33
KokkuvõteThe 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.
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ScholarGateVõrdle meetodeid: Eddy Covariance · HYSPLIT. Loetud 2026-06-20 aadressilt https://scholargate.app/et/compare