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The exchange of trace gases between the Earth's surface and its atmosphere drives atmospheric composition. Airborne eddy covariance can provide observational constraints on surface fluxes at regional scales, helping to bridge the gap between top-down and bottom-up flux estimates and offering novel insights into biophysical and biogeochemical processes. The NASA Carbon Airborne Flux Experiment (CARAFE) utilizes the NASA C-23 Sherpa aircraft with a suite of commercial and custom instrumentationdoi:10.5194/amt-2017-398 fatcat:6qijt7iqtfelrhygwuwqxndtfi