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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 9, issue 18 | Copyright
Atmos. Chem. Phys., 9, 7131-7142, 2009
https://doi.org/10.5194/acp-9-7131-2009
© Author(s) 2009. This work is distributed under
the Creative Commons Attribution 3.0 License.

  24 Sep 2009

24 Sep 2009

Long-term tropospheric formaldehyde concentrations deduced from ground-based fourier transform solar infrared measurements

N. B. Jones1, K. Riedel2, W. Allan2, S. Wood2, P. I. Palmer3, K. Chance4, and J. Notholt5 N. B. Jones et al.
  • 1Department of Chemistry, University of Wollongong, NSW 2522, Australia
  • 2National Institute of Water and Atmospheric Research, Wellington, New Zealand
  • 3School of GeoSciences, University of Edinburgh, UK
  • 4Division of Engineering and Applied Sciences, Harvard University, Cambridge, Massachusetts, USA
  • 5Institute of Environmental Physics University of Bremen, Bremen, Germany

Abstract. We report a 13-year (1992–2005) dataset of total column measurements of formaldehyde (HCHO) over Lauder, New Zealand, inferred from solar infrared spectra measured using a high-resolution Fourier Transform Spectrometer (FTS). Ambient HCHO concentrations at this rural location are often close to levels typical of remote marine environments (<250 ppt), which are close to the detection limit using standard techniques. Consequently we develop a new method that successfully produces HCHO columns with sufficient sensitivity throughout the whole season. HCHO columns over Lauder have a strong seasonal cycle (±50%), with a mean column of 4.9×1015 molecules cm−2, peaking during summer months. A simple box model of CH4 oxidation reproduces the observed broad-scale seasonal cycle, but significantly underestimates the seasonal peak HCHO ground concentrations during summer. This suggests the existence of an additional significant source of HCHO, possibly isoprene that cannot be explained by oxidation of CH4 alone. The ground-based FTS column data compare well with collocated HCHO column measurements from the Global Ozone Monitoring Experiment (GOME) satellite instrument during the operational period of GOME (1996–2001, r2=0.65, mean bias=10%, n=48).

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