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| Aerodynamiczny strumień masowy× | Model HYSPLIT× | |
|---|---|---|
| Dziedzina | Meteorologia | Meteorologia |
| Rodzina | Process / pipeline | Process / pipeline |
| Rok powstania≠ | 1981 | 1997 |
| Twórca≠ | Large and Pond | Draxler and Hess |
| Typ≠ | Surface flux estimation method | Trajectory and dispersion model |
| Źródło pierwotne≠ | Large, 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 ↗ |
| Inne nazwy | Bulk aerodynamic approach, Bulk flux parametrization, Aerodynamic bulk method | HYSPLIT, Hybrid Single-Particle, Lagrangian trajectory model |
| Pokrewne | 3 | 3 |
| Podsumowanie≠ | The 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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