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| Teoria della Similarità di Monin-Obukhov× | Modello WRF× | |
|---|---|---|
| Campo | Meteorologia | Meteorologia |
| Famiglia | Process / pipeline | Process / pipeline |
| Anno di origine≠ | 1954 | 2000 |
| Ideatore≠ | Monin and Obukhov | Skamarock and Klemp |
| Tipo≠ | Similarity scaling framework | Atmospheric simulation system |
| Fonte seminale≠ | 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 ↗ | 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. link ↗ |
| Alias≠ | Monin-Obukhov, Similarity theory, Monin-Obukhov length scale | Weather Research and Forecasting, WRF, ARW, NMM |
| Correlati≠ | 3 | 4 |
| Sintesi≠ | 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. | 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. |
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