H. Schlager et al., IN-SITU OBSERVATIONS OF AIR-TRAFFIC EMISSION SIGNATURES IN THE NORTH-ATLANTIC FLIGHT CORRIDOR, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 102(D9), 1997, pp. 10739-10750
Focussed aircraft measurements have been carried out over the eastern
North Atlantic to search for signals of air traffic emissions in the f
light corridor region. Observations include NO, NO2, HNO3, SO2, O-3, H
2O, total condensation nuclei (CN), and meteorological parameters. A f
light pattern with constant-altitude north-south legs across the major
North Atlantic air traffic tracks was flown. Signatures of air traffi
c emissions were clearly detected for NOx, SO2, and CN with peak conce
ntrations of 2 ppbv, 0.25 ppbv, and 500 cm(-3), respectively, exceedin
g background values by factors of 30 (NOx), 5 (SO2), and 3 (CN). The o
bserved NOx, SO2, and CN peaks were attributed to aircraft plumes base
d on radar observations of the source air traffic and wind measurement
s. Major aircraft exhaust signatures are due to relatively fresh emiss
ions, i.e., superpositions of 2 to 5 plumes with ages of about 15 min
to 3 hs. The observed plume peak concentrations of NOx compare fairly
well with concentrations computed with a Gaussian plume model using ho
rizontal and vertical diffusivities as obtained by recent large-eddy s
imulations, measured vertical wind shear, and the corridor air traffic
information. For the major emission signatures a mean CN/NOx abundanc
e ratio of 300 cm(-3) ppbv(-1) was measured corresponding to an emissi
on index (EI) of about 10(16) particles per 1 kg fuel burnt. This is h
igher than the expected soot particle EI of modern wide-bodied aircraf
t. For the most prominent plumes no increase of HNO3 concentrations ex
ceeding variations of background values was observed. This indicates t
hat only a small fraction of the emitted NOx is oxidized in the plumes
within a timescale of about 3 hs for the conditions of the measuremen
ts.