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| 莫宁-奥布霍夫相似理论× | 热成风× | |
|---|---|---|
| 领域 | 气象学 | 气象学 |
| 方法族 | Process / pipeline | Process / pipeline |
| 起源年份≠ | 1954 | 1920s |
| 提出者≠ | Monin and Obukhov | Jacobbian insights from geostrophic flow |
| 类型≠ | Similarity scaling framework | Wind-temperature relationship |
| 开创性文献≠ | 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 ↗ | Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press. link ↗ |
| 别名 | Monin-Obukhov, Similarity theory, Monin-Obukhov length scale | Thermal wind, Vertical wind shear, Barotropic |
| 相关 | 3 | 3 |
| 摘要≠ | 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 thermal wind relationship is a fundamental meteorological principle that links vertical wind shear to horizontal temperature gradients. It states that wind speed increases with height in the direction of warming—a direct consequence of hydrostatic and geostrophic balance combined with the ideal gas law. |
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