Articles | Volume 8, issue 10
https://doi.org/10.5194/amt-8-4369-2015
https://doi.org/10.5194/amt-8-4369-2015
Research article
 | 
16 Oct 2015
Research article |  | 16 Oct 2015

Relative drifts and biases between six ozone limb satellite measurements from the last decade

N. Rahpoe, M. Weber, A. V. Rozanov, K. Weigel, H. Bovensmann, J. P. Burrows, A. Laeng, G. Stiller, T. von Clarmann, E. Kyrölä, V. F. Sofieva, J. Tamminen, K. Walker, D. Degenstein, A. E. Bourassa, R. Hargreaves, P. Bernath, J. Urban, and D. P. Murtagh

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Cited articles

Adams, C., Bourassa, A. E., Sofieva, V., Froidevaux, L., McLinden, C. A., Hubert, D., Lambert, J. -C., Sioris, C. E., and Degenstein, D. A.: Assessment of Odin-OSIRIS ozone measurements from 2001 to the present using MLS, GOMOS, and ozone sondes, Atmos. Meas. Tech. Discuss., 6, 3819–3857, https://doi.org/10.5194/amtd-6-3819-2013, 2013.
Bertaux, J. L., Kyrölä, E., Fussen, D., Hauchecorne, A., Dalaudier, F., Sofieva, V., Tamminen, J., Vanhellemont, F., Fanton d'Andon, O., Barrot, G., Mangin, A., Blanot, L., Lebrun, J. C., Pérot, K., Fehr, T., Saavedra, L., Leppelmeier, G. W., and Fraisse, R.: Global ozone monitoring by occultation of stars: an overview of GOMOS measurements on ENVISAT, Atmos. Chem. Phys., 10, 12091–12148, https://doi.org/10.5194/acp-10-12091-2010, 2010.
Bhartia, P. K., Harris, N., Van Roozendael, M., Weber, M., Eckman, R., Loyola, D., Urban, J., von Savigny, C., Dameris, M., and Godin-Beekmann, S. (Eds.): Changes in the vertical distribution of ozone – SI2N report, Special Issue, Atmos. Chem. Phys., http://www.atmos-chem-phys.net/special_issue284.html, 2012.
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. Optics, 44, 7218–7231, 2005.
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Short summary
The analyses among six satellite instruments measuring ozone reveals that the relative drift between the sensors is not significant in the stratosphere and we conclude that merging of data from these instruments is possible. The merged ozone profiles can then be ingested in global climate models for long-term forecasts of ozone and climate change in the atmosphere. The added drift uncertainty is estimated at about 3% per decade (1 sigma) and should be applied in the calculation of ozone trends.