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Flux Aerodinàmic Global×HYSPLIT×
CampMeteorologiaMeteorologia
FamíliaProcess / pipelineProcess / pipeline
Any d'origen19811997
Autor originalLarge and PondDraxler and Hess
TipusSurface flux estimation methodTrajectory and dispersion model
Font seminalLarge, W. G., & Pond, S. (1981). Open ocean momentum flux measurements in moderate to strong winds. Journal of Physical Oceanography, 11(3), 324-336. DOI ↗Draxler, R. R., & Hess, G. D. (1997). Description of the HYSPLIT_4 modeling system. NOAA Technical Memorandum ERL ARL-224. link ↗
ÀliesBulk aerodynamic approach, Bulk flux parametrization, Aerodynamic bulk methodHYSPLIT, Hybrid Single-Particle, Lagrangian trajectory model
Relacionats33
ResumThe 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.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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ScholarGateCompara mètodes: Bulk Aerodynamic Flux · HYSPLIT. Recuperat el 2026-06-20 de https://scholargate.app/ca/compare