During the fall 1997 North Atlantic Regional Experiment (NARE 97), two sepa
rate intercomparisons of aircraft-based carbon monoxide measurement instrum
entation were conducted. On September 2, CO measurements were simultaneousl
y made aboard the National Oceanic and Atmospheric Administration (NOAA) WP
-3 by vacuum ultraviolet (VUV) fluorescence and by tunable diode laser abso
rption spectroscopy (TDLAS), On September 18, an intercomparison flight was
conducted between two separate instruments, both employing the VUV fluores
cence method, on the NOAA WP-3 and the U,K. Meteorological Office C-130 Her
cules. The results indicate that both of the VUV fluorescence instruments a
nd the TDLAS system are capable of measuring ambient CO accurately and prec
isely with no apparent interferences in 5 s. The accuracy of the measuremen
ts, based upon three independent calibration systems, is indicated by the a
greement to within 11% with systematic offsets of less than 1 ppbv. In addi
tion, one of the groups participated in the Measurement of Air Pollution Fr
om Satellite (MAPS) intercomparison [Novelli ef at., 1998] with a different
measurement technique but very similar calibration system, and agreed with
the accepted analysis to within 5%. The precision of the measurements is i
ndicated by the variability of the ratio of simultaneous measurements from
the separate instruments, This variability is consistent with the estimated
precisions of 1.5 ppbv and 2.2 ppbv for the 5 s average results of the C-1
30 and the WP-3 instruments, respectively, and indicates a precision of app
roximately 3.6% for the TDLAS instrument. The excellent agreement of the in
struments in both intercomparisons demonstrates that significant interferen
ces in the measurements are absent in air masses that ranged from 7 km in t
he midtroposphere to boundary layer conditions including subtropical marine
air and continental outflow with embedded urban plumes. The intercompariso
n of the two VUV instruments that differed widely in their design indicates
that the VUV fluorescence technique for CO measurements is not particularl
y sensitive to the details of its implementation. These intercomparisons he
lp to establish the reliability of ambient CO measurements by the VUV fluor
escence technique.