Quantifying the regional and global exchange Of CO2 between the ocean and a
tmosphere requires knowledge of the factors that affect CO2 gas transfer (e
.g., wind speed) and the air-sea difference in partial pressure Of CO2 (PCO
2). A major uncertainty is the effect of short-term variability on airsea C
O2 flux. Using high sampling frequency wind speed and PCO2 data collected d
uring deployments of the autonomous CARbon Interface OCean Atmosphere (CARI
OCA) buoy, we compare CO2 fluxes at different sampling frequency of wind sp
eed (i.e., hourly versus daily averaged). Air-sea CO2 flux was up to three
times greater if high frequency wind data was used rather than daily averag
e values. This difference arises from the non-linear relationship between w
ind speed and CO2 gas transfer coefficient, and a better representation of
wind distribution at a higher frequency (i.e., hourly) of sampling. This fi
nding has significant implications for determining regional and global air-
sea CO2 fluxes, and understanding of the global carbon cycle.