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| Mô hình WRF× | Lý thuyết Tương tự Monin-Obukhov× | |
|---|---|---|
| Lĩnh vực | Khí tượng học | Khí tượng học |
| Họ | Process / pipeline | Process / pipeline |
| Năm ra đời≠ | 2000 | 1954 |
| Người khởi xướng≠ | Skamarock and Klemp | Monin and Obukhov |
| Loại≠ | Atmospheric simulation system | Similarity scaling framework |
| Công trình gốc≠ | 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 ↗ | 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 ↗ |
| Tên gọi khác≠ | Weather Research and Forecasting, WRF, ARW, NMM | Monin-Obukhov, Similarity theory, Monin-Obukhov length scale |
| Liên quan≠ | 4 | 3 |
| Tóm tắt≠ | 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. | 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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