O. Bujok et al., GHOST - A novel airborne gas chromatograph for in situ measurements of long-lived tracers in the lower stratosphere: Method and applications, J ATMOS CH, 39(1), 2001, pp. 37-64
A novel fully-automated airborne gas chromatograph for in situ measurements
of long-lived stratospheric tracers has been developed, combining the high
selectivity of a megabore PLOT capillary column with recently developed sa
mpling and separation techniques. The Gas cHromatograph for the Observation
of Stratospheric Tracers (GHOST) has been successfully operated during thr
ee STREAM campaigns (Stratosphere TRoposphere Experiment by Airborne Measur
ement) onboard a Cessna Citation II aircraft in two different modes: Either
N2O and CF2Cl2 (CFC-12) or CFC-12 and CFCl3 (CFC-11) have been measured si
multaneously, with a time resolution of 2 min for both modes. Under flight
conditions the instrument precision (1 sigma) for these species is better t
han 0.9%, and the accuracy (1 sigma) is better than 2.0% of the tropospheri
c values of all measured compounds. The detection limits (3 sigma) are belo
w 28 ppb for N2O, 14 ppt for CFC-12, and 8 ppt for CFC-11, respectively, i.
e., well below 10% of the tropospheric values of all measured compounds. Po
st-mission optimization of the chromatographic separation showed a possible
enhancement of the time resolution by up to a factor of 2, associated with
a comparable increase in precision and detection limit. As test of actual
performance of GHOST results from an in-flight N2O intercomparison with a t
unable diode laser absorption spectrometer (TDLAS) are presented. They yiel
d an excellent agreement between both instruments. Furthermore, on the basi
s of the hitherto most extensive set of upper tropospheric and lower strato
spheric data, the relative stratospheric N2O lifetime is re-assessed. When
referenced to the WMO reference CFC-11 lifetime of 45 +/- 7 years an N2O li
fetime of 91 +/- 15 years is derived, a value substantially smaller than th
e WMO reference lifetime of 120 years. Moreover, this value implies a strat
ospheric N2O sink strength of 16.3 +/- 2.7 Tg (N) yr(-1) which is 30% large
r than previous estimates.