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001     30239
005     20240709074302.0
024 7 _ |2 DOI
|a 10.1016/S0273-1177(03)00588-X
024 7 _ |2 WOS
|a WOS:000222000000007
037 _ _ |a PreJuSER-30239
041 _ _ |a eng
082 _ _ |a 520
084 _ _ |2 WoS
|a Engineering, Aerospace
084 _ _ |2 WoS
|a Astronomy & Astrophysics
084 _ _ |2 WoS
|a Geosciences, Multidisciplinary
084 _ _ |2 WoS
|a Meteorology & Atmospheric Sciences
100 1 _ |a Schaeler, B.
|b 0
|0 P:(DE-HGF)0
245 _ _ |a A case study of trace gas transports near the tropopause
260 _ _ |a Amsterdam [u.a.]
|b Elsevier Science
|c 2004
300 _ _ |a 1053 - 1057
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 Advances in Space Research
|x 0273-1177
|0 9884
|y 7
|v 33
500 _ _ |a Record converted from VDB: 12.11.2012
520 _ _ |a The CRISTA experiment provided global measurements of atmospheric trace gases in the stratosphere and upper troposphere during its second mission in August 1997. A new data product has recently been developed, yielding water vapor mixing ratios around the tropopause. The high data density of CRISTA makes an efficient assimilation of the water vapor field (by means of the NCAR ROSE CTM) possible. From these data turbulent trace gas fluxes upsilon'chi' are derived. The global distribution of the H2O fluxes is found to be highly structured at a given pressure level. Zonal means of fluxes indicate transport barriers at the equator and near the tropopause. This is compared to effective diffusivities of P. Haynes and E. Shuckburgh [J. Geophys. Res. 105 (2000) 22795] and general agreement is obtained. There is one important discrepancy, though: the effective diffusivities show a transequatorial "bridge" at about 350 K potential temperature (about 12 km), a "bridge" which is also seen in the CRISTA water vapor data, but at a considerably higher altitude. This finding is confirmed by ozone data from CRISTA and from UARS. (C) 2003 COSPAR. Published by Elsevier Ltd. All rights reserved.
536 _ _ |a Chemie und Dynamik der Geo-Biosphäre
|c U01
|2 G:(DE-HGF)
|0 G:(DE-Juel1)FUEK257
|x 0
588 _ _ |a Dataset connected to Web of Science
650 _ 7 |a S
|2 WoSType
653 2 0 |2 Author
|a water vapor
653 2 0 |2 Author
|a tropopause
653 2 0 |2 Author
|a turbulent flux
653 2 0 |2 Author
|a transport barriers
653 2 0 |2 Author
|a middle atmosphere dynamics
653 2 0 |2 Author
|a ozone
653 2 0 |2 Author
|a CRISTA
700 1 _ |a Offermann, D.
|b 1
|0 P:(DE-HGF)0
700 1 _ |a Hoffmann, L.
|b 2
|0 P:(DE-HGF)0
700 1 _ |a Riese, M.
|b 3
|u FZJ
|0 P:(DE-Juel1)129145
773 _ _ |a 10.1016/S0273-1177(03)00588-X
|g Vol. 33, p. 1053 - 1057
|p 1053 - 1057
|q 33<1053 - 1057
|0 PERI:(DE-600)2023311-5
|t Advances in space research
|v 33
|y 2004
|x 0273-1177
856 7 _ |u http://dx.doi.org/10.1016/S0273-1177(03)00588-X
909 C O |o oai:juser.fz-juelich.de:30239
|p VDB
913 1 _ |k U01
|v Chemie und Dynamik der Geo-Biosphäre
|l Chemie und Dynamik der Geo-Biosphäre
|b Environment (Umwelt)
|0 G:(DE-Juel1)FUEK257
|x 0
914 1 _ |y 2004
915 _ _ |0 StatID:(DE-HGF)0010
|a JCR/ISI refereed
920 1 _ |k ICG-I
|l Stratosphäre
|d 31.12.2006
|g ICG
|0 I:(DE-Juel1)VDB47
|x 0
970 _ _ |a VDB:(DE-Juel1)27788
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
981 _ _ |a I:(DE-Juel1)IEK-7-20101013

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