A tropopause-related climatology of ozone profiles (TpO3 climatology)
A new ozone climatology (TpO3
climatology), based on ozonesonde (1980-2006) and SAGE-II satellite measurements(1984-2005) covers altitudes from the Earth’s surface up to ~60 km. This climatology is novel in that the
ozone profiles are categorized according to calendar month, latitude, and local
tropopause heights. It presents ozone
mixing ratio profiles in 10° latitude zones on a 1 km pressure
altitude grid (z=16 log10(1013/P), P is pressure in hPa), according to the tropopause (or double
tropopause) heights. The
probability distribution of tropopause heights is also provided.
The TpO3 climatology has several benefits
compared a sea-level- or tropopause-referenced climatology. In particular:
(i) The dependence of the ozone abundance and its
variability on tropopause height is preserved. This allows a more accurate
characterization of ozone profiles and a partial characterization of
longitudinal variability.
(ii)
Variability in the upper troposphere and the lower stratosphere is reduced when
compared to sea-level-referenced climatologies.
(iii)
Ozone profiles in the presence of double tropopauses are somewhat better
characterized.
(iv)
The availability of the tropopause height statistics makes it
possible to reduce the TpO3 climatology to a more traditional
sea-level-referenced or tropopause-referenced climatology.
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the TpO3 climatology
For more details:
In publications using the TpO3
climatology please include the reference to the paper above.
Contact: Viktoria Sofieva(firstname.lastname(at) fmi.fi)
Last updated: 9
January 2014