guest ::
| Home > Publications database > Backtrajectory reconstruction of water vapour and ozone in-situ observations in the TTL > print |
| Home > Publications database > Backtrajectory reconstruction of water vapour and ozone in-situ observations in the TTL > print |
| 001 | 22110 | ||
| 005 | 20240709074306.0 | ||
| 024 | 7 | _ | |2 DOI |a 10.1127/0941-2948/2012/0314 |
| 024 | 7 | _ | |2 WOS |a WOS:000306436800004 |
| 037 | _ | _ | |a PreJuSER-22110 |
| 041 | _ | _ | |a eng |
| 082 | _ | _ | |a 550 |
| 084 | _ | _ | |2 WoS |a Meteorology & Atmospheric Sciences |
| 100 | 1 | _ | |a Plöger, F. |0 P:(DE-Juel1)129141 |b 0 |u FZJ |
| 245 | _ | _ | |a Backtrajectory reconstruction of water vapour and ozone in-situ observations in the TTL |
| 260 | _ | _ | |a Stuttgart |b E. Schweizerbart Science Publishers |c 2012 |
| 300 | _ | _ | |a 239 - 244 |
| 336 | 7 | _ | |a Journal Article |0 PUB:(DE-HGF)16 |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 |
| 440 | _ | 0 | |a Meteorologische Zeitschrift |x 0941-2948 |0 14161 |y 3 |v 21 |
| 500 | _ | _ | |3 POF3_Assignment on 2016-02-29 |
| 500 | _ | _ | |a We thank the ECMWF for providing the reanalysis data, COST for funding a Short Term Scientific Mission for F. PLOEGER, and in particular N. THOMAS for programming support. |
| 520 | _ | _ | |a Water vapour and ozone in-situ observations in the tropical tropopause layer (TTL) during the three tropical campaigns SCOUT-O3, AMMA and TroCCiNOx are reconstructed from diabatic and kinematic backtrajectories, with the reconstruction method for the tracer fields based on freeze-drying and photochemichal ozone production. The results using diabatic trajectories show that both water vapour and ozone in-situ observations can be well reconstructed from trajectories. Consequentially, in-situ observations agree with the assumption of freeze-drying due to the large-scale temperature field as the main control mechanism for water vapour and photochemical production and transport as main control mechanisms for tropical ozone. The kinematic ozone reconstruction, however, shows a large high-bias during SCOUT-O3 and a too strong variability during all campaigns, due to excessive transport of stratospheric ozone into the TTL. We conclude that kinematic reconstructions of in-situ observations are less reliable than diabatic, due to unrealistic inhomogeneities in the velocity field. |
| 536 | _ | _ | |a Atmosphäre und Klima |c P23 |2 G:(DE-HGF) |0 G:(DE-Juel1)FUEK491 |x 0 |
| 588 | _ | _ | |a Dataset connected to Web of Science |
| 650 | _ | 7 | |a J |2 WoSType |
| 700 | 1 | _ | |a Konopka, P. |0 P:(DE-Juel1)129130 |b 1 |u FZJ |
| 700 | 1 | _ | |a Müller, R. |0 P:(DE-Juel1)129138 |b 2 |u FZJ |
| 700 | 1 | _ | |a Günther, G. |0 P:(DE-Juel1)129123 |b 3 |u FZJ |
| 700 | 1 | _ | |a Grooss, J.-U. |0 P:(DE-Juel1)129122 |b 4 |u FZJ |
| 700 | 1 | _ | |a Schiller, C. |0 P:(DE-Juel1)VDB1410 |b 5 |u FZJ |
| 700 | 1 | _ | |a Ravegnani, F. |0 P:(DE-HGF)0 |b 6 |
| 700 | 1 | _ | |a Ulanovski, A. |0 P:(DE-HGF)0 |b 7 |
| 700 | 1 | _ | |a Riese, M. |0 P:(DE-Juel1)129145 |b 8 |u FZJ |
| 773 | _ | _ | |a 10.1127/0941-2948/2012/0314 |g Vol. 21, p. 239 - 244 |p 239 - 244 |q 21<239 - 244 |0 PERI:(DE-600)2045168-4 |t Meteorologische Zeitschrift |v 21 |y 2012 |x 0941-2948 |
| 856 | 7 | _ | |u http://dx.doi.org/10.1127/0941-2948/2012/0314 |
| 909 | C | O | |o oai:juser.fz-juelich.de:22110 |p VDB |p VDB:Earth_Environment |
| 913 | 1 | _ | |b Erde und Umwelt |k P23 |l Atmosphäre und Klima |1 G:(DE-HGF)POF2-230 |0 G:(DE-Juel1)FUEK491 |2 G:(DE-HGF)POF2-200 |v Atmosphäre und Klima |x 0 |z vormals P22 |
| 913 | 2 | _ | |a DE-HGF |b Marine, Küsten- und Polare Systeme |l Atmosphäre und Klima |1 G:(DE-HGF)POF3-240 |0 G:(DE-HGF)POF3-249H |2 G:(DE-HGF)POF3-200 |v Addenda |x 0 |
| 914 | 1 | _ | |y 2012 |
| 915 | _ | _ | |a JCR/ISI refereed |0 StatID:(DE-HGF)0010 |2 StatID |
| 915 | _ | _ | |a JCR |0 StatID:(DE-HGF)0100 |2 StatID |
| 915 | _ | _ | |a WoS |0 StatID:(DE-HGF)0111 |2 StatID |b Science Citation Index Expanded |
| 915 | _ | _ | |a DBCoverage |0 StatID:(DE-HGF)0150 |2 StatID |b Web of Science Core Collection |
| 915 | _ | _ | |a DBCoverage |0 StatID:(DE-HGF)0199 |2 StatID |b Thomson Reuters Master Journal List |
| 915 | _ | _ | |a DBCoverage |0 StatID:(DE-HGF)0200 |2 StatID |b SCOPUS |
| 915 | _ | _ | |a DBCoverage |0 StatID:(DE-HGF)1040 |2 StatID |b Zoological Record |
| 920 | 1 | _ | |k IEK-7 |l Stratosphäre |g IEK |0 I:(DE-Juel1)IEK-7-20101013 |x 0 |
| 970 | _ | _ | |a VDB:(DE-Juel1)138377 |
| 980 | _ | _ | |a VDB |
| 980 | _ | _ | |a ConvertedRecord |
| 980 | _ | _ | |a journal |
| 980 | _ | _ | |a I:(DE-Juel1)IEK-7-20101013 |
| 980 | _ | _ | |a UNRESTRICTED |
| 981 | _ | _ | |a I:(DE-Juel1)ICE-4-20101013 |
| Library | Collection | CLSMajor | CLSMinor | Language | Author |
|---|