Сравнение методов
Просматривайте выбранные методы рядом; строки с различиями подсвечены.
| HYSPLIT× | Массовый аэродинамический поток× | |
|---|---|---|
| Область | Метеорология | Метеорология |
| Семейство | Process / pipeline | Process / pipeline |
| Год появления≠ | 1997 | 1981 |
| Автор метода≠ | Draxler and Hess | Large and Pond |
| Тип≠ | Trajectory and dispersion model | Surface flux estimation method |
| Основополагающий источник≠ | 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 ↗ |
| Другие названия | HYSPLIT, Hybrid Single-Particle, Lagrangian trajectory model | Bulk aerodynamic approach, Bulk flux parametrization, Aerodynamic bulk method |
| Связанные | 3 | 3 |
| Сводка≠ | 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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