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Volume 9, issue 12
Atmos. Meas. Tech., 9, 6081–6100, 2016
https://doi.org/10.5194/amt-9-6081-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Meas. Tech., 9, 6081–6100, 2016
https://doi.org/10.5194/amt-9-6081-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 20 Dec 2016

Research article | 20 Dec 2016

Global distributions of CO2 volume mixing ratio in the middle and upper atmosphere from daytime MIPAS high-resolution spectra

Á. Aythami Jurado-Navarro et al.

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Beagley, S. R., Boone, C. D., Fomichev, V. I., Jin, J. J., Semeniuk, K., McConnell, J. C., and Bernath, P. F.: First multi-year occultation observations of CO2 in the MLT by ACE satellite: observations and analysis using the extended CMAM, Atmos. Chem. Phys., 10, 1133–1153, https://doi.org/10.5194/acp-10-1133-2010, 2010.
Bermejo-Pantaleón, D., Funke, B., Lopez-Puertas, M., García-Comas, M., Stiller, G. P., von Clarmann, T., Linden, A., Grabowski, U., Höpfner, M., Kiefer, M., Glatthor, N., Kellmann, S., and Lu, G.: Global Observations of Thermospheric Temperature and Nitric Oxide from MIPAS spectra at 5.3 µm, J. Geophys. Res., 116, A10313, https://doi.org/10.1029/2011JA016752, 2011.
De Laurentis, M.: Planning of MIPAS new special modes January 2005 Campaign, Tech. rep., ESA Technical Note, ENVI-SPPA-EOPG-TN-05-0002, 2005.
Feofilov, A. G., Kutepov, A. A., She, C.-Y., Smith, A. K., Pesnell, W. D., and Goldberg, R. A.: CO2(v2)-O quenching rate coefficient derived from coincidental SABER/TIMED and Fort Collins lidar observations of the mesosphere and lower thermosphere, Atmos. Chem. Phys., 12, 9013–9023, https://doi.org/10.5194/acp-12-9013-2012, 2012.
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We present global distributions of CO2 concentrations in the upper atmosphere (70–140 km) derived from high-resolution 4.3 µm MIPAS spectra from 2005 to 2012. CO2 relative abundances have been measured at 120–140 km for the first time. The data have an unprecedented accuracy. CO2 shows a strong seasonal behaviour. CO2 largely controls the temperature of the upper atmosphere and its measurement is very important for understanding the impact of climate change in this region.
We present global distributions of CO2 concentrations in the upper atmosphere (70–140 km)...
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