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| 001 | 185599 | ||
| 005 | 20240712100906.0 | ||
| 024 | 7 | _ | |a 10.5194/amtd-7-4229-2014 |2 doi |
| 024 | 7 | _ | |a 2128/8187 |2 Handle |
| 037 | _ | _ | |a FZJ-2014-07025 |
| 082 | _ | _ | |a 550 |
| 100 | 1 | _ | |a Kaufmann, M. |0 P:(DE-Juel1)129128 |b 0 |e Corresponding Author |u fzj |
| 245 | _ | _ | |a Retrieval of three-dimensional small scale structures in upper tropospheric/lower stratospheric composition as measured by GLORIA |
| 260 | _ | _ | |a Katlenburg-Lindau |c 2014 |b Copernicus |
| 336 | 7 | _ | |a Journal Article |b journal |m journal |0 PUB:(DE-HGF)16 |s 185599 |2 PUB:(DE-HGF) |
| 336 | 7 | _ | |a Output Types/Journal article |2 DataCite |
| 336 | 7 | _ | |a Journal Article |0 0 |2 EndNote |
| 336 | 7 | _ | |a ARTICLE |2 BibTeX |
| 336 | 7 | _ | |a JOURNAL_ARTICLE |2 ORCID |
| 336 | 7 | _ | |a article |2 DRIVER |
| 520 | _ | _ | |a The three-dimensional quantification of small scale processes in the upper troposphere and lower stratosphere is one of the challenges of current atmospheric research and requires the development of new measurement strategies. This work presents first results from the newly developed Gimballed Limb Observer for Radiance Imaging of the Atmosphere (GLORIA) obtained during the ESSenCe and TACTS/ESMVal aircraft campaigns. The focus of this work is on the so-called dynamics mode data characterized by a medium spectral and a very high spatial resolution. The retrieval strategy for the derivation of two- and three-dimensional constituent fields in the upper troposphere and lower stratosphere is presented. Uncertainties of the main retrieval targets (temperature, O3, HNO3 and CFC-12) and their spatial resolution are discussed. During ESSenCe, high resolution two-dimensional cross-sections have been obtained. Comparisons to collocated remote-sensing and in-situ data indicate a good agreement between the data sets. During TACTS/ESMVal a tomographic flight pattern to sense an intrusion of stratospheric air deep into the troposphere has been performed. This filament could be reconstructed with an unprecedented spatial resolution of better than 500 m vertically and 20 km × 20 km horizontally. |
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| 700 | 1 | _ | |a Blank, J. |0 P:(DE-Juel1)141861 |b 1 |
| 700 | 1 | _ | |a Guggenmoser, T. |0 P:(DE-Juel1)143753 |b 2 |u fzj |
| 700 | 1 | _ | |a Ungermann, J. |0 P:(DE-Juel1)129105 |b 3 |u fzj |
| 700 | 1 | _ | |a Engel, A. |0 P:(DE-HGF)0 |b 4 |
| 700 | 1 | _ | |a Ern, M. |0 P:(DE-Juel1)129117 |b 5 |u fzj |
| 700 | 1 | _ | |a Friedl-Vallon, F. |0 P:(DE-HGF)0 |b 6 |
| 700 | 1 | _ | |a Gerber, D. |0 P:(DE-HGF)0 |b 7 |
| 700 | 1 | _ | |a Grooss, J. U. |0 P:(DE-Juel1)129122 |b 8 |u fzj |
| 700 | 1 | _ | |a Guenther, G. |0 P:(DE-HGF)0 |b 9 |
| 700 | 1 | _ | |a Höpfner, M. |0 P:(DE-HGF)0 |b 10 |
| 700 | 1 | _ | |a Kleinert, A. |0 P:(DE-HGF)0 |b 11 |
| 700 | 1 | _ | |a Latzko, Th. |0 P:(DE-HGF)0 |b 12 |
| 700 | 1 | _ | |a Maucher, G. |0 P:(DE-HGF)0 |b 13 |
| 700 | 1 | _ | |a Neubert, T. |0 P:(DE-Juel1)133921 |b 14 |u fzj |
| 700 | 1 | _ | |a Nordmeyer, H. |0 P:(DE-HGF)0 |b 15 |
| 700 | 1 | _ | |a Oelhaf, H. |0 P:(DE-HGF)0 |b 16 |
| 700 | 1 | _ | |a Olschewski, F. |0 P:(DE-HGF)0 |b 17 |
| 700 | 1 | _ | |a Orphal, J. |0 P:(DE-HGF)0 |b 18 |
| 700 | 1 | _ | |a Preusse, P. |0 P:(DE-Juel1)129143 |b 19 |u fzj |
| 700 | 1 | _ | |a Schlager, H. |0 P:(DE-HGF)0 |b 20 |
| 700 | 1 | _ | |a Schneider, Herbert |0 P:(DE-Juel1)133743 |b 21 |u fzj |
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| 700 | 1 | _ | |a Vogel, B. |0 P:(DE-Juel1)129164 |b 25 |u fzj |
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| 700 | 1 | _ | |a Riese, M. |0 P:(DE-Juel1)129145 |b 28 |u fzj |
| 773 | _ | _ | |a 10.5194/amtd-7-4229-2014 |g Vol. 7, no. 4, p. 4229 - 4274 |0 PERI:(DE-600)2507817-3 |n 4 |p 4229 - 4274 |t Atmospheric measurement techniques discussions |v 7 |y 2014 |x 1867-8610 |
| 856 | 4 | _ | |u www.atmos-meas-tech-discuss.net/7/4229/2014 |
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