As part of the CarbonWatch-NZ research programme, air samples were collected at 28 sites around Auckland, New Zealand, to determine the atmospheric ratio (
R
CO
) of excess (local enhancement over background) carbon monoxide to fossil CO
2
(CO
2
ff). Sites were categorized into seven types (background, forest, industrial, suburban, urban, downwind and motorway) to observe
R
CO
around Auckland. Motorway flasks observed
R
CO
of 14 ± 1 ppb ppm
−1
and were used to evaluate traffic
R
CO
. The similarity between suburban (14 ± 1 ppb ppm
−1
) and traffic
R
CO
suggests that traffic dominates suburban CO
2
ff emissions during daytime hours, the period of flask collection. The lower urban
R
CO
(11 ± 1 ppb ppm
−1
) suggests that urban CO
2
ff emissions are comprised of more than just traffic, with contributions from residential, commercial and industrial sources, all with a lower
R
CO
than traffic. Finally, the downwind sites were believed to best represent
R
CO
for Auckland City overall (11 ± 1 ppb ppm
−1
). We demonstrate that the initial discrepancy between the downwind
R
CO
and Auckland's estimated daytime inventory
R
CO
(15 ppb ppm
−1
) can be attributed to an overestimation in inventory traffic CO emissions. After revision based on our observed motorway
R
CO
, the revised inventory
R
CO
(12 ppb ppm
−1
) is consistent with our observations.
This article is part of the Theo Murphy meeting issue 'Radiocarbon in the Anthropocene'.