A global monthly-mean climatology of the air-sea oxygen flux is presented a
nd discussed. The climatology is based on the ocean oxygen climatology of N
ajjar and Keeling [1997] and wind speeds derived from a meteorological anal
ysis center. Seasonal variations are characterized by outgassing of oxygen
during spring and summer and ingassing of oxygen during fall and winter, a
pattern consistent with thermal and biological forcing of the air-sea oxyge
n flux. The annual mean flux pattern is characterized by ingassing at high
latitudes and the tropics and outgassing in middle latitudes. The air-sea o
xygen flux is shown to exhibit patterns that agree well with patterns seen
in a marine primary productivity climatology, in model generated air-sea O-
2 fluxes, in estimates of remineralization in the shallow aphotic zone base
d on seasonal oxygen variations, in observed seasonal nutrient-temperature
relationships, and in independent estimates of meridional oxygen transport
in the Atlantic ocean. We also find that extratropical mixed layer new prod
uction during the spring-summer period, computed from biological seasonal n
et outgassing of oxygen, is equivalent to the production of 4.5-5.6 Gt C, m
uch lower than previous estimates based on atmospheric O-2/N-2 measurements
.