Sammenlign metoder
Gjennomgå de valgte metodene side om side; rader som avviker, er uthevet.
| HYSPLIT× | Bulk Aerodynamic Flux× | |
|---|---|---|
| Fagfelt | Meteorologi | Meteorologi |
| Familie | Process / pipeline | Process / pipeline |
| Opprinnelsesår≠ | 1997 | 1981 |
| Opphavsperson≠ | Draxler and Hess | Large and Pond |
| Type≠ | Trajectory and dispersion model | Surface flux estimation method |
| Opprinnelig kilde≠ | Draxler, R. R., & Hess, G. D. (1997). Description of the HYSPLIT_4 modeling system. NOAA Technical Memorandum ERL ARL-224. link ↗ | 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 ↗ |
| Alias | HYSPLIT, Hybrid Single-Particle, Lagrangian trajectory model | Bulk aerodynamic approach, Bulk flux parametrization, Aerodynamic bulk method |
| Relaterte | 3 | 3 |
| Sammendrag≠ | 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. | 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. |
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