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Volume 15, issue 22
Atmos. Chem. Phys., 15, 12789-12803, 2015
https://doi.org/10.5194/acp-15-12789-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 15, 12789-12803, 2015
https://doi.org/10.5194/acp-15-12789-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 18 Nov 2015

Research article | 18 Nov 2015

Retrieval of ammonia from ground-based FTIR solar spectra

E. Dammers1, C. Vigouroux2, M. Palm3, E. Mahieu4, T. Warneke3, D. Smale5, B. Langerock2, B. Franco4, M. Van Damme6,1, M. Schaap7, J. Notholt3, and J. W. Erisman1,8 E. Dammers et al.
  • 1Cluster Earth and Climate, Department of Earth Sciences, Vrije Universiteit Amsterdam, Amsterdam, the Netherlands
  • 2Belgian Institute for Space Aeronomy, Brussels, Belgium
  • 3Institut für Umweltphysik, University of Bremen, Bremen, Germany
  • 4Institute of Astrophysics and Geophysics, University of Liege, Belgium
  • 5National Institute of Water and Atmosphere, Lauder, New Zealand
  • 6Spectroscopie de l'Atmosphère, Service de Chimie Quantique et Photophysique, Université Libre de Bruxelles, Brussels, Belgium
  • 7TNO Built Environment and Geosciences, Department of Air Quality and Climate, Utrecht, the Netherlands
  • 8Louis Bolk Institute, Driebergen, the Netherlands

Abstract. We present a retrieval method for ammonia (NH3) total columns from ground-based Fourier transform infrared (FTIR) observations. Observations from Bremen (53.10° N, 8.85° E), Lauder (45.04° S, 169.68° E), Réunion (20.9° S, 55.50° E) and Jungfraujoch (46.55° N, 7.98° E) were used to illustrate the capabilities of the method. NH3 mean total columns ranging 3 orders of magnitude were obtained, with higher values at Bremen (mean of 13.47 × 1015 molecules cm−2) and lower values at Jungfraujoch (mean of 0.18 × 1015 molecules cm−2). In conditions with high surface concentrations of ammonia, as in Bremen, it is possible to retrieve information on the vertical gradient, as two layers can be distinguished. The retrieval there is most sensitive to ammonia in the planetary boundary layer, where the trace gas concentration is highest. For conditions with low concentrations, only the total column can be retrieved. Combining the systematic and random errors we have a mean total error of 26 % for all spectra measured at Bremen (number of spectra (N) = 554), 30 % for all spectra from Lauder (N = 2412), 25 % for spectra from Réunion (N = 1262) and 34 % for spectra measured at Jungfraujoch (N = 2702). The error is dominated by the systematic uncertainties in the spectroscopy parameters. Station-specific seasonal cycles were found to be consistent with known seasonal cycles of the dominant ammonia sources in the station surroundings. The developed retrieval methodology from FTIR instruments provides a new way of obtaining highly time-resolved measurements of ammonia burdens. FTIR-NH3 observations will be useful for understanding the dynamics of ammonia concentrations in the atmosphere and for satellite and model validation. It will also provide additional information to constrain the global ammonia budget.

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We present a new retrieval method for ammonia (NH3) concentrations and total columns from ground-based Fourier transform infrared (FTIR) observations. Observations from Bremen, Lauder, Réunion and Jungfraujoch are used to show the capabilities of the new retrieval. The developed retrieval provides a new way of obtaining time-resolved measurements and will be useful for understanding the dynamics of ammonia concentrations in the atmosphere and for satellite and model validation.
We present a new retrieval method for ammonia (NH3) concentrations and total columns from...
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