Atmospheric Chemistry and Physics (Jun 2009)

Equatorial total column of nitrous oxide as measured by IASI on MetOp-A: implications for transport processes

  • P. Ricaud,
  • J.-L. Attié,
  • H. Teyssèdre,
  • L. El Amraoui,
  • V.-H. Peuch,
  • M. Matricardi,
  • P. Schluessel

Journal volume & issue
Vol. 9, no. 12
pp. 3947 – 3956

Abstract

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In this paper we use the total columns of nitrous oxide (N<sub>2</sub>O) as retrieved from the radiance spectra as measured by the Infrared Atmospheric Sounding Interferometer (IASI) instrument aboard the MetOp-A platform and distributed by the European Organisation for the Exploitation of Meteorological Satellites (EUMETSAT) during the March–May (MAM) 2008 period. Since the total column of N<sub>2</sub>O reflects concentrations in the middle troposphere, cloud-free columnar N<sub>2</sub>O measurements are used to assess transport processes in the equatorial band (10&deg; S–10&deg; N). We compare the measured data set with the outputs produced by the 3-D chemical-transport model MOCAGE during the period MAM 2002–2004. To reflect MAM 2008 concentrations, MOCAGE results have been scaled by a factor 1.0125 in order to represent the change in concentration of N<sub>2</sub>O since 2004. IASI N<sub>2</sub>O equatorial measurements show a maximum over Africa (4.96&times;10<sup>&minus;3</sup> kg m<sup>&minus;2</sup>) and a minimum over South America (4.86&times;10<sup>&minus;3</sup> kg m<sup>&minus;2</sup>) in reasonable agreement with the outputs from MOCAGE despite the fact that emissions of N<sub>2</sub>O are more intense over America than over Africa. The amplitude of the longitudinal variation of total column N<sub>2</sub>O along the equatorial band is twice as intense in the measurements (~1.6%) than as in the model calculations (~0.8%), and much greater than the IASI mean random error (0.16–0.33%). A difference between the two data sets is observed above the Western Pacific (110&deg; E–150&deg; E) with a marked minimum in IASI compared to MOCAGE. Recent theoretical studies (Ricaud et al., 2007 and 2009) have shown the potentially important effect of the Walker and the Hadley cells on the tropospheric distribution of N<sub>2</sub>O in producing a local maximum in N<sub>2</sub>O above Africa. Based on equatorial total columns of N<sub>2</sub>O retrieved from IASI, our results are consistent with the fact that Africa is a zone of convergence of airmasses coming from different convective regions whilst Western Pacific behaves more like a divergence zone.