A. Kortzinger et al., The international at-sea intercomparison of fCO(2) systems during the R/V Meteor Cruise 36/1 in the North Atlantic Ocean, MAR CHEM, 72(2-4), 2000, pp. 171-192
The 'International Intercomparison Exercise of fCO(2) Systems' was carried
out in 1996 during the R/V Meteor Cruise 36/1 from Bermuda/UK to Gran Canar
ia/Spain. Nine groups from six countries (Australia, Denmark, France, Germa
ny, Japan, USA) participated in this exercise, bringing together 15 partici
pants with seven underway fugacity of carbon dioxide (fCO(2)) systems, one
discrete fCO(2) system, and two underway pH systems, as well as systems for
discrete measurement of total alkalinity and total dissolved inorganic car
bon. Here, we compare surface seawater fCO(2) measured synchronously by all
participating instruments. A common infrastructure (seawater and calibrati
on gas supply), different quality checks (performance of calibration proced
ures for CO2, temperature measurements) and a common procedure for calculat
ion of final fCO(2) were provided to reduce the largest possible amount of
controllable sources of error. The results show that under such conditions
underway measurements of the fCO(2) in surface seawater and overlying air c
an be made to a high degree of agreement(+/-1 mu atm) with a variety of pos
sible equilibrator and system designs. Also, discrete fCO(2) measurements c
an be made in good agreement (+/-3 mu atm) with underway fCO(2) data sets.
However, even well-designed systems, which are operated without any obvious
sign of malfunction, can show significant differences of the order of 10 m
u atm. Based on our results, no "best choice" for the type of the equilibra
tor nor specifics on its dimensions and flow rates of seawater and air can
be made in regard to the achievable accuracy of the fCO(2) system. Measurem
ents of equilibrator temperature do not seem to be made with the required a
ccuracy resulting in significant errors in fCO(2) results. Calculation of f
CO(2) from high-quality total dissolved inorganic carbon (C-T) and total al
kalinity (A(T)) measurements does not yield results comparable in accuracy
and precision to fCO(2) measurements. (C) 2000 Elsevier Science B.V. All ri
ghts reserved.