Carbon dioxide cools the upper atmosphere. Satellite measurements suggest that concentrations of this greenhouse gas have risen in the thermosphere over the past decade, with implications for the energy balance of the upper atmosphere.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 12 print issues and online access
$259.00 per year
only $21.58 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
References
Emmert, J. T., Stevens, M. H., Bernath, P. F., Drob, D. P. & Boone, C. D. Nature Geosci. 5, http://dx.doi.org/10.1038/ngeo1626 (2012).
Qian, L., Laštovička, J., Roble, R. G. & Solomon, S. C. J. Geophys. Res. 116, A00H03 (2011).
Emmert, J. T., Lean, J. L. & Picone, J. M. Geophys. Res. Lett. 37, L12102 (2010).
Lewis, H. G., Saunders, A., Swinerd, G. & Newland, R. J. J. Geophys. Res. 116, A00H08 (2011).
Bernath, P. F. et al., Geophys. Res. Lett. 32, L15S01 (2005).
Beagley, S. R. et al. Atmos. Chem. Phys. 10, 1133–1153 (2010).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Noël, S. Rise in upper-atmospheric carbon. Nature Geosci 5, 848–849 (2012). https://doi.org/10.1038/ngeo1648
Published:
Issue Date:
DOI: https://doi.org/10.1038/ngeo1648