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@ARTICLE{Hoffmann:155275,
author = {Hoffmann, L. and Alexander, M. J. and Clerbaux, C. and
Grimsdell, A. W. and Meyer, Catrin and Rößler, T. and
Tournier, B.},
title = {{I}ntercomparison of stratospheric gravity wave
observations with {AIRS} and {IASI}},
journal = {Atmospheric measurement techniques discussions},
volume = {7},
number = {8},
issn = {1867-8610},
address = {Katlenburg-Lindau},
publisher = {Copernicus},
reportid = {FZJ-2014-04449},
pages = {8415 - 8464},
year = {2014},
abstract = {Gravity waves are an important driver for the atmospheric
circulation and have substantial impact on weather and
climate. Satellite instruments offer excellent opportunities
to study gravity waves on a global scale. This study focuses
on observations from the Atmospheric Infrared Sounder (AIRS)
onboard the National Aeronautics and Space Administration's
Aqua satellite and the Infrared Atmospheric Sounding
Interferometer (IASI) onboard the European MetOp satellites.
The main aim of this study is an intercomparison of
stratospheric gravity wave observations of both instruments.
In particular, we analyzed AIRS and IASI 4.3 μm brightness
temperature measurements, which directly relate to
stratospheric temperature. Three case studies showed that
AIRS and IASI provide a clear and consistent picture of the
temporal development of individual gravity wave events.
Statistical comparisons based on a five-year period of
measurements (2008–2012) showed similar spatial and
temporal patterns of gravity wave activity. However, the
statistical comparisons also revealed systematic differences
of variances between AIRS and IASI (about $45\%)$ that we
attribute to the different spatial measurement
characteristics of both instruments. We also found
differences between day- and nighttime data (about $30\%)$
that are partly due to the local time variations of the
gravity wave sources. While AIRS has been used successfully
in many previous gravity wave studies, IASI data are applied
here for the first time for that purpose. Our study shows
that gravity wave observations from different hyperspectral
infrared sounders such as AIRS and IASI can be directly
related to each other, if instrument-specific
characteristics such as different noise levels and spatial
resolution and sampling are carefully considered. The
ability to combine observations from different satellites
provides an opportunity to create a long-term record, which
is an exciting prospect for future climatological studies of
stratospheric gravity wave activity.},
cin = {JSC},
ddc = {550},
cid = {I:(DE-Juel1)JSC-20090406},
pnm = {411 - Computational Science and Mathematical Methods
(POF2-411)},
pid = {G:(DE-HGF)POF2-411},
typ = {PUB:(DE-HGF)16},
doi = {10.5194/amtd-7-8415-2014},
url = {https://juser.fz-juelich.de/record/155275},
}