Global distributions of methanol and formic acid retrieved for the first time from the IASI/MetOp thermal infrared sounder

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Abstract

Methanol (CH3OH) and formic acid (HCOOH) are among the most abundant volatile organic compounds present in the atmosphere. In this work, we derive the global distributions of these two organic species using for the first time the Infrared Atmospheric Sounding Interferometer (IASI) launched onboard the MetOp-A satellite in 2006. This paper describes the method used and provides a first critical analysis of the retrieved products. The retrieval process follows a two-step approach in which global distributions are first obtained on the basis of a simple radiance indexing (transformed into brightness temperatures), and then mapped onto column abundances using suitable conversion factors. For methanol, the factors were calculated using a complete retrieval approach in selected regions. In the case of formic acid, a different approach, which uses a set of forward simulations for representative atmospheres, has been used. In both cases, the main error sources are carefully determined: the average relative error on the column for both species is estimated to be about 50%, increasing to about 100% for the least favorable conditions. The distributions for the year 2009 are discussed in terms of seasonality and source identification. Time series comparing methanol, formic acid and carbon monoxide in different regions are also presented. © 2011 Author(s).

Figures

  • Fig. 1. Top panel: IASI normalized radiance spectrum in the spectral region between 950 and 1200 cm−1 containing methanol and formic acid absorption bands. Bottom panels: Contribution to the IASI spectrum of different atmospheric species plotted in transmittance. The vertical lines indicate the target channels (in red) and the baseline channels (in blue) which are used for the 1Tb determination (nine channels are used for CH3OH, and three for HCOOH). See Sect. 2.2 for details.
  • Fig. 2. Top panel: Illustration of the two CH3OH a priori profiles (continental and oceanic) derived from the IMAGESv2 CTM model for the year 2007. Open circles represent the a priori on the 4 layers retrieval grid. Bottom panels: Plot (expressed in %) of the associated covariance matrices (left: for land, right: for ocean).
  • Table 1. Selected regions and periods for the retrieval of methanol using the Optimal Estimation Method.
  • Fig. 4. Illustration of the influence of water vapor and ozone concentrations on the methanol 1Tb. Simulations were performed for the midlatitude summer model with varying concentrations of H2O (black squares) and O3 (red squares) while the CH3OH amount was fixed. In both cases, a linear dependence is found.
  • Fig. 3. Top panel: Example of a methanol retrieval from an IASI spectrum recorded over Namibia (20.16◦ S–21.50◦ E) on 20 October 2008. The observed (blue curve) spectrum is shown together with the fit residue (in cyan) and the dashed horizontal lines delimit this residue by its RMS value. The dark green curve is the fit residue when CH3OH is not taken into account in the retrieval, the red curve represents the calculated CH3OH contribution to the spectrum and the dashed vertical line indicates the detectable CH3OH absorption band. Bottom panel: Mean total column averaging kernels presented for retrievals performed over land (green curve) and over ocean (blue curve).
  • Fig. 5. Correlation between the retrieved total columns of methanol and the corresponding 1Tb for various regions (corrected for O3 and H2O dependency, see text for details). The conversion factors are given by the slopes of the linear fit (gray curve) separated for retrievals above land (Top panel) and above ocean (Bottom panel). More details about the selected regions for the retrievals can be found in Table 1.
  • Fig. 6. Seasonal distributions of methanol total columns for the year 2009. The white areas correspond to a filter for sandy scenes where emissivity is uncertain.
  • Fig. 7. Histogram of the relative differences between the simulated CH3OH total columns and the total columns derived from the 1Tb calculation.

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APA

Razavi, A., Karagulian, F., Clarisse, L., Hurtmans, D., Coheur, P. F., Clerbaux, C., … Stavrakou, T. (2011). Global distributions of methanol and formic acid retrieved for the first time from the IASI/MetOp thermal infrared sounder. Atmospheric Chemistry and Physics, 11(2), 857–872. https://doi.org/10.5194/acp-11-857-2011

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