Módszerek összehasonlítása

	WRF Modell	Tömeg-aerodinamikai áramlás	HYSPLIT
Tudományterület	Meteorológia	Meteorológia	Meteorológia
Módszercsalád	Process / pipeline	Process / pipeline	Process / pipeline
Keletkezés éve	2000	1981	1997
Megalkotó	Skamarock and Klemp	Large and Pond	Draxler and Hess
Típus	Atmospheric simulation system	Surface flux estimation method	Trajectory and dispersion model
Alapmű	Skamarock, W. C., Klemp, J. B., Dudhia, J., et al. (2008). A Description of the Advanced Research WRF Version 3. NCAR Technical Note NCAR/TN-475+STR.	Large, W. G., & Pond, S. (1981). Open ocean momentum flux measurements in moderate to strong winds. Journal of Physical Oceanography, 11(3), 324-336.	Draxler, R. R., & Hess, G. D. (1997). Description of the HYSPLIT_4 modeling system. NOAA Technical Memorandum ERL ARL-224.
Alternatív nevek	Weather Research and Forecasting, WRF, ARW, NMM	Bulk aerodynamic approach, Bulk flux parametrization, Aerodynamic bulk method	HYSPLIT, Hybrid Single-Particle, Lagrangian trajectory model
Kapcsolódó	4	3	3
Összefoglaló	The Weather Research and Forecasting (WRF) model is a mesoscale atmospheric simulation system used for weather forecasting, research, and climate applications. Developed cooperatively by NCAR, NOAA, and academic institutions, WRF became operational in 2004 and has become one of the most widely used atmospheric models worldwide.	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.