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@ARTICLE{Ern:280095,
author = {Ern, Manfred and Preusse, Peter and Riese, Martin},
title = {{D}riving of the {SAO} by gravity waves as observed from
satellite},
journal = {Annales geophysicae},
volume = {33},
number = {4},
issn = {0992-7689},
address = {Katlenburg, Lindau},
publisher = {Copernicus},
reportid = {FZJ-2015-07842},
pages = {483-504},
year = {2015},
abstract = {It is known that atmospheric dynamics in the tropical
stratosphere have an influence on higher altitudes and
latitudes as well as on surface weather and climate. In the
tropics, the dynamics are governed by an interplay of the
quasi-biennial oscillation (QBO) and semiannual oscillation
(SAO) of the zonal wind. The QBO is dominant in the lower
and middle stratosphere, and the SAO in the upper
stratosphere/lower mesosphere. For both QBO and SAO the
driving by atmospheric waves plays an important role. In
particular, the role of gravity waves is still not well
understood. In our study we use observations of the High
Resolution Dynamics Limb Sounder (HIRDLS) satellite
instrument to derive gravity wave momentum fluxes and
gravity wave drag in order to investigate the interaction of
gravity waves with the SAO. These observations are compared
with the ERA-Interim reanalysis. Usually, QBO westward winds
are much stronger than QBO eastward winds. Therefore, mainly
gravity waves with westward-directed phase speeds are
filtered out through critical-level filtering already below
the stratopause region. Accordingly, HIRDLS observations
show that gravity waves contribute to the SAO momentum
budget mainly during eastward wind shear, and not much
during westward wind shear. These findings confirm
theoretical expectations and are qualitatively in good
agreement with ERA-Interim and other modeling studies. In
ERA-Interim most of the westward SAO driving is due to
planetary waves, likely of extratropical origin. Still, we
find in both observations and ERA-Interim that sometimes
westward-propagating gravity waves may contribute to the
westward driving of the SAO. Four characteristic cases of
atmospheric background conditions are identified. The
forcings of the SAO in these cases are discussed in detail,
supported by gravity wave spectra observed by HIRDLS. In
particular, we find that the gravity wave forcing of the SAO
cannot be explained by critical-level filtering alone;
gravity wave saturation without critical levels being
reached is also important.},
cin = {IEK-7},
ddc = {550},
cid = {I:(DE-Juel1)IEK-7-20101013},
pnm = {244 - Composition and dynamics of the upper troposphere and
middle atmosphere (POF3-244)},
pid = {G:(DE-HGF)POF3-244},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000353840000007},
doi = {10.5194/angeo-33-483-2015},
url = {https://juser.fz-juelich.de/record/280095},
}