R. Wanninkhof et al., GAS-EXCHANGE, DISPERSION, AND BIOLOGICAL PRODUCTIVITY ON THE WEST FLORIDA SHELF - RESULTS FROM A LAGRANGIAN TRACER STUDY, Geophysical research letters, 24(14), 1997, pp. 1767-1770
A Lagrangian tracer study was performed on the west Florida shelf in A
pril 1996 using deliberately injected trace gases. Although such studi
es have been performed previously, this work is the first where the de
liberate tracers, in conjunction with carbon system parameters, are us
ed to quantify changes in water column carbon inventories due to air-s
ea exchange and net community metabolism. The horizontal dispersion an
d the gas transfer velocity were determined over a period of 2 weeks f
rom the change in both the concentrations and the concentration ratio
of the two injected trace gases, sulfur hexafluoride (SF6) and helium-
3 (He-3). The second moment of the patch grew to 1.6 x 10(3) km(2) ove
r a period of 11 days. The gas transfer velocity, normalized to CO2 ex
change at 20 degrees C, was 8.4 cm hr(-1) at an average wind speed, U-
10, of 4.4 m s(-1) for the duration of the experiment, which is in goo
d agreement with empirical estimates. Remineralization rates exceeded
productivity, causing an increase in dissolved inorganic carbon of abo
ut 1 mu mol kg(-1) day(-1) in the water column. During this period of
senescence, 80% of the increase in inorganic carbon is attributed to c
ommunity remineralization and 20% due to invasion of atmospheric CO2.