EGU2020-13736
https://doi.org/10.5194/egusphere-egu2020-13736
EGU General Assembly 2020
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Time dependent 3D tomography of a mountain wave over the Andes with GLORIA IR limb imager

Lukas Krasauskas1, Markus Geldenhuys1, Peter Preusse1, jörn Ungermann1, Michael Höpfner2, Felix Friedl-Vallon2, Bernd Kaifler3, Markus Rapp3, and Riese Martin1
Lukas Krasauskas et al.
  • 1Forschungszentrum Jülich, IEK-7, Jülich, Germany (l.krasauskas@fz-juelich.de)
  • 2Karlsruher Institut für Technologie, Karlsruhe, Germany
  • 3Deutsches Zentrum für Luft- und Raumfahrt, Cologne, Germany

The Gimballed Limb Observer for Radiance Imaging of the Atmosphere (GLORIA) is an aircraft-
based Fourier transform spectrometer with a 2D detector array jointly developed by Forschungszentrum
Jülich and Karlsruhe Institute of Technology. Air temperature and volume mixing ratios of various
trace gases are retrieved from the measured IR spectra. GLORIA's viewing direction can be panned between 45 and 135
w. r. t. the flight direction. Combining this capability with flight paths that encircle the observed
atmospheric region, multiple measurements of the same air mass can be performed, allowing for 3D
tomography of the atmosphere with a vertical resolution down to 250 m and horizontal resolution of
around 25 km.
GLORIA flew on the German HALO research aircraft during the SouthTRAC measurement cam-
paign held in southern Argentina in September-November 2019. One of the main goals of the campaign
was gravity wave study using GLORIA, as well as an upward looking ALIMA lidar instrument devel-
oped by Deutsches Zentrum für Luft- und Raumfahrt (DLR), and in situ instruments. During one of
the research flights, a large amplitude mountain wave was observed over the Andes. The air volume
near the mountains was encircled twice, providing a unique opportunity to study the time evolution
of an orographic gravity wave with a help of 3D time dependent temperature retrieval. We present
the initial analysis of this dataset, showing complex temperature structure with several overlapping
gravity wave families at altitudes of 9 to 14 km. GLORIA data is complemented by the ALIMA lidar
temperature retrieval at altitudes between about 20 and 60 km, providing insight into further upward
propagation and breaking of the observed mountain wave. We also compare our results with ECMWF model data.

How to cite: Krasauskas, L., Geldenhuys, M., Preusse, P., Ungermann, J., Höpfner, M., Friedl-Vallon, F., Kaifler, B., Rapp, M., and Martin, R.: Time dependent 3D tomography of a mountain wave over the Andes with GLORIA IR limb imager, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13736, https://doi.org/10.5194/egusphere-egu2020-13736, 2020.