Using recent laboratory and field results we explore the possibility of a c
ubic relationship between gas exchange and instantaneous (or short-term) wi
nd speed, and its impact on global air-sea fluxes. The theoretical foundati
on for such a dependency is based on retardation of gas transfer at low to
intermediate winds by surfactants, which are ubiquitous in the world's ocea
ns, and bubble-enhanced transfer at higher winds. The proposed cubic relati
onship shows a weaker dependence of gas transfer at low wind speed and a si
gnificantly stronger dependence at high wind speed than previous relationsh
ips. A long-term relationship derived from such a dependence, combined with
the monthly CO2 climatology of Takahashi [1997], leads to an increase in t
he global annual oceanic CO2 uptake from 1.4 Gigaton C yr(-1) to 2.2 Gigato
n C yr(-1). Although a cubic relationship fits within global bomb-C-14 ocea
nic uptake constraints, additional checks are warranted, particularly at hi
gh wind speeds where the enhancement is most pronounced.