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| Обемни аеродинамични потоци× | HYSPLIT× | Теория за подобие на Монин-Обухов× | |
|---|---|---|---|
| Област | Метеорология | Метеорология | Метеорология |
| Семейство | Process / pipeline | Process / pipeline | Process / pipeline |
| Година на възникване≠ | 1981 | 1997 | 1954 |
| Създател≠ | Large and Pond | Draxler and Hess | Monin and Obukhov |
| Тип≠ | Surface flux estimation method | Trajectory and dispersion model | Similarity scaling framework |
| Основополагащ източник≠ | 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 ↗ | Monin, A. S., & Obukhov, A. M. (1954). Basic laws of turbulent mixing in the ground layer of the atmosphere. Tr. Akad. Nauk SSSR, 24, 163-187. link ↗ |
| Други названия | Bulk aerodynamic approach, Bulk flux parametrization, Aerodynamic bulk method | HYSPLIT, Hybrid Single-Particle, Lagrangian trajectory model | Monin-Obukhov, Similarity theory, Monin-Obukhov length scale |
| Свързани | 3 | 3 | 3 |
| Резюме≠ | 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. | Monin-Obukhov similarity theory is a fundamental framework in boundary layer meteorology that describes how wind speed, temperature, and humidity vary with height near the surface. Published in 1954, it shows that normalized vertical profiles depend on a single dimensionless parameter—the Monin-Obukhov stability parameter—which quantifies the balance between mechanical turbulence and buoyant convection. |
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