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@ARTICLE{Ungermann:185600,
author = {Ungermann, J. and Blank, J. and Dick, M. and Ebersoldt, A.
and Friedl-Vallon, F. and Giez, A. and Guggenmoser, T. and
Höpfner, M. and Jurkat, T. and Kaufmann, M. and Kaufmann,
S. and Kleinert, A. and Krämer, M. and Latzko, T. and
Oelhaf, H. and Olchewski, F. and Preusse, P. and Rolf, C.
and Schillings, J. and Suminska-Ebersoldt, O. and Tan, V.
and Thomas, N. and Voigt, C. and Zahn, A. and Zöger, M. and
Riese, M.},
title = {{L}evel 2 processing for the imaging {F}ourier transform
spectrometer {GLORIA}: derivation and validation of
temperature and trace gas volume mixing ratios from
calibrated dynamics mode spectra},
journal = {Atmospheric measurement techniques discussions},
volume = {7},
number = {12},
issn = {1867-8610},
address = {Katlenburg-Lindau},
publisher = {Copernicus},
reportid = {FZJ-2014-07026},
pages = {12037 - 12080},
year = {2014},
abstract = {he Gimballed Limb Observer for Radiance Imaging of the
Atmosphere (GLORIA) is an airborne infrared limb-imager
combining a two-dimensional infrared detector with a Fourier
transform spectrometer. It was operated aboard the new
German Gulfstream G550 research aircraft HALO during the
Transport And Composition in the upper Troposphere/lowermost
Stratosphere (TACTS) and Earth System Model Validation
(ESMVAL) campaigns in summer 2012.This paper describes the
retrieval of temperature and trace gas (H2O, O3, HNO3)
volume mixing ratios from GLORIA dynamics mode spectra. 26
integrated spectral windows are employed in a joint fit to
retrieve seven targets using consecutively a fast and an
accurate tabulated radiative transfer model. Typical
diagnostic quantities are provided including effects of
uncertainties in the calibration and horizontal resolution
along the line-of-sight. Simultaneous in-situ observations
by the BAsic HALO Measurement And Sensor System (BAHAMAS),
the Fast In-Situ Stratospheric Hygrometer (FISH), FAIRO, and
the Atmospheric chemical Ionization Mass Spectrometer (AIMS)
allow a validation of retrieved values for three flights in
the upper troposphere/lowermost stratosphere region spanning
polar and sub-tropical latitudes. A high correlation is
achieved between the remote sensing and the in-situ trace
gas data, and discrepancies can to a large fraction be
attributed to differences in the probed air masses caused by
different sampling characteristics of the instruments.This
1-D processing of GLORIA dynamics mode spectra provides the
basis for future tomographic inversions from circular and
linear flight paths to better understand selected dynamical
processes of the upper troposphere and lowermost
stratosphere.},
cin = {IEK-7 / ZEA-2},
ddc = {550},
cid = {I:(DE-Juel1)IEK-7-20101013 / I:(DE-Juel1)ZEA-2-20090406},
pnm = {234 - Composition and Dynamics of the Upper Troposphere and
Stratosphere (POF2-234)},
pid = {G:(DE-HGF)POF2-234},
typ = {PUB:(DE-HGF)16},
doi = {10.5194/amtd-7-12037-2014},
url = {https://juser.fz-juelich.de/record/185600},
}