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| 037 | _ | _ | |a FZJ-2014-07026 |
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| 100 | 1 | _ | |a Ungermann, J. |0 P:(DE-Juel1)129105 |b 0 |e Corresponding Author |u fzj |
| 245 | _ | _ | |a Level 2 processing for the imaging Fourier transform spectrometer GLORIA: derivation and validation of temperature and trace gas volume mixing ratios from calibrated dynamics mode spectra |
| 260 | _ | _ | |a Katlenburg-Lindau |c 2014 |b Copernicus |
| 336 | 7 | _ | |a article |2 DRIVER |
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| 520 | _ | _ | |a 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. |
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| 700 | 1 | _ | |a Blank, J. |0 P:(DE-Juel1)141861 |b 1 |
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| 700 | 1 | _ | |a Ebersoldt, A. |0 P:(DE-HGF)0 |b 3 |
| 700 | 1 | _ | |a Friedl-Vallon, F. |0 P:(DE-HGF)0 |b 4 |
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| 700 | 1 | _ | |a Latzko, T. |0 P:(DE-HGF)0 |b 13 |
| 700 | 1 | _ | |a Oelhaf, H. |0 P:(DE-HGF)0 |b 14 |
| 700 | 1 | _ | |a Olchewski, F. |0 P:(DE-HGF)0 |b 15 |
| 700 | 1 | _ | |a Preusse, P. |0 P:(DE-Juel1)129143 |b 16 |u fzj |
| 700 | 1 | _ | |a Rolf, C. |0 P:(DE-Juel1)139013 |b 17 |u fzj |
| 700 | 1 | _ | |a Schillings, J. |0 P:(DE-Juel1)133735 |b 18 |u fzj |
| 700 | 1 | _ | |a Suminska-Ebersoldt, O. |0 P:(DE-HGF)0 |b 19 |
| 700 | 1 | _ | |a Tan, V. |0 P:(DE-Juel1)129160 |b 20 |u fzj |
| 700 | 1 | _ | |a Thomas, N. |0 P:(DE-Juel1)129162 |b 21 |u fzj |
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