Eddy covariance (also known as eddy correlation, eddy flux, and aerodynamic) is a key micrometeorological technique to measure and calculate vertical turbulent fluxes within atmospheric boundary layers. The method directly measures the turbulent exchange of properties such as heat, water vapor, and momentum between the Earth's surface and the atmosphere. It's widely used in environmental science, agriculture, and meteorology to understand ecosystem processes and climate change impacts.
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