So sánh phương pháp

	Eddy Covariance	Mô hình WRF
Lĩnh vực	Khí tượng học	Khí tượng học
Họ	Process / pipeline	Process / pipeline
Năm ra đời	1951	2000
Người khởi xướng	Swinbank	Skamarock and Klemp
Loại	Micrometeorological flux measurement	Atmospheric simulation system
Công trình gốc	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.	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.
Tên gọi khác	Eddy covariance, EC flux, Eddy correlation, Direct flux measurement	Weather Research and Forecasting, WRF, ARW, NMM
Liên quan	3	4
Tóm tắt	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.	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.