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@ARTICLE{Ern:1006441,
author = {Ern, Manfred and Diallo, Mohamadou A. and Khordakova, Dina
and Krisch, Isabell and Preusse, Peter and Reitebuch, Oliver
and Ungermann, Jörn and Riese, Martin},
title = {{T}he {QBO} and global-scale tropical waves in {A}eolus
wind observations, radiosonde data, and reanalyses},
reportid = {FZJ-2023-01675},
year = {2023},
abstract = {The quasi-biennial oscillation (QBO) of the stratospheric
tropical winds influences the global circulation over a wide
range of latitudes and altitudes. Although it has strong
effects on surface weather and climate, climate models have
large difficulties in simulating a realistic QBO, especially
in the lower stratosphere. Therefore, global wind
observations in the tropical upper troposphere and lower
stratosphere (UTLS) are of particular interest for
investigating the QBO and the tropical waves that contribute
significantly to its driving. In our work, we focus on the
years 2018–2022 and investigate the QBO and different
tropical wave modes in the UTLS region using global wind
observations by the Aeolus satellite instrument, and three
meteorological reanalyses (ERA-5, JRA-55, and MERRA-2).
Further, we compare these data with observations of selected
radiosonde stations. By comparison with Aeolus observations,
we find that on zonal average the QBO in the lower
stratosphere is well represented in all three reanalyses,
with ERA-5 performing best. Averaged over the years
2018–2022, agreement between Aeolus and the reanalyses is
better than 1 to 2 m s−1, with somewhat larger differences
during some periods. Different from zonal averages,
radiosonde stations provide only local observations and are
therefore biased by global-scale tropical waves, which
limits their use as a QBO standard. While reanalyses perform
well on zonal average, there can be considerable local
biases between reanalyses and radiosondes. We also find
that, in the tropical UTLS, zonal wind variances of
stationary waves and the most prominent global-scale
traveling equatorial wave modes, such as Kelvin waves,
Rossby-gravity waves, and equatorial Rossby waves, are in
good agreement between Aeolus and all three reanalyses (in
most cases better than 20 $\%$ of the peak values in the
UTLS). On zonal average, this supports the use of reanalyses
as a reference for comparison with free-running climate
models, while locally certain biases exist, particularly in
the QBO wind shear zones, and around the 2019–2020 QBO
disruption.},
cin = {IEK-7},
cid = {I:(DE-Juel1)IEK-7-20101013},
pnm = {2112 - Climate Feedbacks (POF4-211) / DFG project 429838442
- Wie wirken sich natürliche Variabilität und anthropogen
bedingte Änderungen auf die stratosphärische Brewer-Dobson
Zirkulation und den Ozonfluss in die Troposphäre aus?
(429838442)},
pid = {G:(DE-HGF)POF4-2112 / G:(GEPRIS)429838442},
typ = {PUB:(DE-HGF)25},
doi = {10.5194/egusphere-2023-408},
url = {https://juser.fz-juelich.de/record/1006441},
}