E. Corazza et G. Tesi, TROPOSPHERIC HYDROGEN AND CARBON OXIDES IN ANTARCTICA AND IN GREENLAND, Science of the total environment, 161, 1995, pp. 803-809
Tropospheric trace gases (H-2, CO, and CO2) were measured in polar are
as for two seasons in Antarctica (Italian base Terra Nova Bay) and two
in Greenland (European base Summit, Greenland Icecore Program [GRIP])
, yielding the following average concentrations: Antarctica (1989-1990
): H-2, 528 ppbv; CO, 51 ppbv; CO2, 354 ppmv; Antarctica (1990-1991):
H-2, 522; CO, 51; Greenland (1991): H-2, 548; CO, 114; Greenland (1999
): CO, 107 (hydrogen discarded). Computer automated gas chromatographi
c analyses were done in situ using a reduction gas detector (RGD) and
a complete set of standards each day, for periods of 2 h in Greenland
and 3 h in Antarctica. Approximately 200 analyses were conducted durin
g each campaign. Peak areas and standard calibrations in the laborator
y were obtained using programs written especially for the purpose. For
both Antarctica and Greenland, some differences were found between th
e two subsequent seasons; the greatest differences, however, were foun
d in Antarctica within the same season (different origins of air masse
s). The inter-hemispheric asymmetry is clear and significant. It most
likely occurs because pollution from the northern hemisphere reaches t
he northernmost regions through the polar vortex, whereas Antarctica i
s more isolated by the Southern Ocean.