เปรียบเทียบวิธี

	แบบจำลอง WRF	Eddy Covariance
สาขาวิชา	อุตุนิยมวิทยา	อุตุนิยมวิทยา
ตระกูล	Process / pipeline	Process / pipeline
ปีกำเนิด	2000	1951
ผู้ริเริ่ม	Skamarock and Klemp	Swinbank
ประเภท	Atmospheric simulation system	Micrometeorological flux measurement
แหล่งต้นตำรับ	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.	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.
ชื่อเรียกอื่น	Weather Research and Forecasting, WRF, ARW, NMM	Eddy covariance, EC flux, Eddy correlation, Direct flux measurement
ที่เกี่ยวข้อง	4	3
สรุป	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.	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.