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