Articles | Volume 9, issue 12
https://doi.org/10.5194/amt-9-5781-2016
https://doi.org/10.5194/amt-9-5781-2016
Research article
 | 
05 Dec 2016
Research article |  | 05 Dec 2016

Validation of ACE-FTS version 3.5 NOy species profiles using correlative satellite measurements

Patrick E. Sheese, Kaley A. Walker, Chris D. Boone, Chris A. McLinden, Peter F. Bernath, Adam E. Bourassa, John P. Burrows, Doug A. Degenstein, Bernd Funke, Didier Fussen, Gloria L. Manney, C. Thomas McElroy, Donal Murtagh, Cora E. Randall, Piera Raspollini, Alexei Rozanov, James M. Russell III, Makoto Suzuki, Masato Shiotani, Joachim Urban, Thomas von Clarmann, and Joseph M. Zawodny

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Cited articles

ACE-FTS: ACE-FTS Level 2 data, available at: http://www.ace.uwaterloo.ca, last access: November 2016.
Bauer, R., Rozanov, A., McLinden, C. A., Gordley, L. L., Lotz, W., Russell III, J. M., Walker, K. A., Zawodny, J. M., Ladstätter-Weißenmayer, A., Bovensmann, H., and Burrows, J. P.: Validation of SCIAMACHY limb NO2 profiles using solar occultation measurements, Atmos. Meas. Tech., 5, 1059–1084, https://doi.org/10.5194/amt-5-1059-2012, 2012.
Bogumil, K., Orphal, J., Voigt, S., Bovensmann, H., Fleischmann, O. C., Hartmann, M., Homann, T., Spietz, P., Vogel, A., and Burrows, J. P.: Reference spectra of atmospheric trace gases measured with the SCIAMACHY PFM satellite spectrometer, Proc. 1st Europ. Sympos. Atmos. Meas. from Space (ESAMS-99), 2, 443–447, ESA-ESTEC, Noordwijk, 18–22 January 1999.
Boone, C. D., Nassar, R., Walker, K. A., Rochon, Y., McLeod, S. D., Rinsland, C. P., and Bernath, P. F.: Retrievals for the Atmospheric Chemistry Experiment Fourier-Transform Spectrometer, Appl. Opt., 44, 7218–7231, https://doi.org/10.1364/AO.44.007218, 2005.
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This study validates version 3.5 of the ACE-FTS NOy species data sets by comparing diurnally scaled ACE-FTS data to correlative data from 11 other satellite limb sounders. For all five species examined (NO, NO2, HNO3, N2O5, and ClONO2), there is good agreement between ACE-FTS and the other data sets in various regions of the atmosphere. In these validated regions, these NOy data products can be used for further investigation into the composition, dynamics, and climate of the stratosphere.