Articles | Volume 15, issue 22
https://doi.org/10.5194/acp-15-13161-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-15-13161-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Reassessment of MIPAS age of air trends and variability
F. J. Haenel
CORRESPONDING AUTHOR
Karlsruhe Institute of Technology, Institute for Meteorology and Climate Research, Karlsruhe, Germany
G. P. Stiller
Karlsruhe Institute of Technology, Institute for Meteorology and Climate Research, Karlsruhe, Germany
T. von Clarmann
Karlsruhe Institute of Technology, Institute for Meteorology and Climate Research, Karlsruhe, Germany
Instituto de Astrofísica de Andalucía (CSIC), 18008 Granada, Spain
E. Eckert
Karlsruhe Institute of Technology, Institute for Meteorology and Climate Research, Karlsruhe, Germany
N. Glatthor
Karlsruhe Institute of Technology, Institute for Meteorology and Climate Research, Karlsruhe, Germany
U. Grabowski
Karlsruhe Institute of Technology, Institute for Meteorology and Climate Research, Karlsruhe, Germany
S. Kellmann
Karlsruhe Institute of Technology, Institute for Meteorology and Climate Research, Karlsruhe, Germany
M. Kiefer
Karlsruhe Institute of Technology, Institute for Meteorology and Climate Research, Karlsruhe, Germany
A. Linden
Karlsruhe Institute of Technology, Institute for Meteorology and Climate Research, Karlsruhe, Germany
T. Reddmann
Karlsruhe Institute of Technology, Institute for Meteorology and Climate Research, Karlsruhe, Germany
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Saved (final revised paper)
Latest update: 23 Nov 2024
Short summary
Stratospheric circulation is thought to change as a consequence of climate change. Empirical evidence, however, is sparse. In this paper we present latitude- and altitude-resolved trends of the mean age of stratospheric air as derived from SF6 measurements performed by the MIPAS satellite instrument. The mean of the age of stratospheric air is a measure of the intensity of the Brewer-Dobson circulation. In this paper we discuss differences with respect to a preceding analysis by Stiller et al.
Stratospheric circulation is thought to change as a consequence of climate change. Empirical...
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