方法对比
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| 涡动相关法× | 莫宁-奥布霍夫相似理论× | |
|---|---|---|
| 领域 | 气象学 | 气象学 |
| 方法族 | Process / pipeline | Process / pipeline |
| 起源年份≠ | 1951 | 1954 |
| 提出者≠ | Swinbank | Monin and Obukhov |
| 类型≠ | Micrometeorological flux measurement | Similarity scaling framework |
| 开创性文献≠ | Baldocchi, D. (2003). Assessing the eddy covariance technique for evaluating carbon dioxide fluxes of ecosystems: past, present and future. Global Change Biology, 9(4), 479-492. DOI ↗ | 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 ↗ |
| 别名≠ | Eddy covariance, EC flux, Eddy correlation, Direct flux measurement | Monin-Obukhov, Similarity theory, Monin-Obukhov length scale |
| 相关 | 3 | 3 |
| 摘要≠ | The eddy covariance method is a direct, micrometeorological technique that measures turbulent fluxes of momentum, heat, water vapor, and CO2 by computing the covariance between high-frequency fluctuations of wind velocity and scalar properties (temperature, humidity, concentration). It is the gold standard for measuring ecosystem-atmosphere exchanges and validating model parameterizations. | 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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