000023764 001__ 23764
000023764 005__ 20240712100842.0
000023764 0247_ $$2DOI$$a10.1029/2001JD000577
000023764 0247_ $$2WOS$$aWOS:000180490000004
000023764 0247_ $$2ISSN$$a0141-8637
000023764 0247_ $$2Handle$$a2128/20886
000023764 037__ $$aPreJuSER-23764
000023764 041__ $$aeng
000023764 082__ $$a550
000023764 084__ $$2WoS$$aMeteorology & Atmospheric Sciences
000023764 1001_ $$0P:(DE-HGF)0$$aSmith, A. K.$$b0
000023764 245__ $$aMiddle atmosphere Kelvin waves observed in CRISTA 1 and 2 temperature and trace species
000023764 260__ $$aWashington, DC$$bUnion$$c2002
000023764 300__ $$aD23
000023764 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000023764 3367_ $$2DataCite$$aOutput Types/Journal article
000023764 3367_ $$00$$2EndNote$$aJournal Article
000023764 3367_ $$2BibTeX$$aARTICLE
000023764 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000023764 3367_ $$2DRIVER$$aarticle
000023764 440_0 $$06393$$aJournal of Geophysical Research D: Atmospheres$$v107$$x0148-0227
000023764 500__ $$aRecord converted from VDB: 12.11.2012
000023764 520__ $$a[1] A number of tropical perturbations that have all the characteristics of Kelvin waves are identified in temperature measurements from the two flights of the Cryogenic Infrared Spectrometers and Telescopes for the Atmosphere (CRISTA) instrument. The background wind conditions during the two flights were quite different due to the different phases of the quasi-biennial oscillation (QBO), and there were differences in the Kelvin waves observed. During each flight, there were several different zonal wave numbers and/or frequencies present simultaneously. The observed waves conform well to theory. In particular, lower-frequency waves are confined to the lower stratosphere, while higher-frequency waves appear in the upper stratosphere and mesosphere; the waves are centered on the equator; and the frequency and structure satisfy the dispersion relation. Wave signals also appear in several stratospheric trace species: O-3, CFC-11 (CFCl3), HNO3, N2O, and CH4. The sense of the correlation of these trace species perturbations with temperature (negative for CFC-11, N2O, and CH4; positive for lower stratospheric HNO3 and O3) confirms that vertical velocity is responsible for the perturbations. There is a shift in the relative phases as photochemical processes become more important with increasing altitude. Upper stratospheric ozone correlates negatively with temperature due to temperature-dependent reaction rates that destroy ozone.
000023764 536__ $$0G:(DE-Juel1)FUEK257$$2G:(DE-HGF)$$aChemie und Dynamik der Geo-Biosphäre$$cU01$$x0
000023764 588__ $$aDataset connected to Web of Science
000023764 650_7 $$2WoSType$$aJ
000023764 7001_ $$0P:(DE-Juel1)VDB12001$$aPreusse, P.$$b1$$uFZJ
000023764 7001_ $$0P:(DE-HGF)0$$aOberheide, J.$$b2
000023764 773__ $$0PERI:(DE-600)2016800-7 $$a10.1029/2001JD000577$$gVol. 107, p. D23$$pD23$$q107<D23$$tJournal of geophysical research / Atmospheres  $$tJournal of Geophysical Research$$v107$$x0148-0227$$y2002
000023764 8567_ $$uhttp://dx.doi.org/10.1029/2001JD000577
000023764 8564_ $$uhttps://juser.fz-juelich.de/record/23764/files/2001JD000577.pdf$$yOpenAccess
000023764 8564_ $$uhttps://juser.fz-juelich.de/record/23764/files/2001JD000577.pdf?subformat=pdfa$$xpdfa$$yOpenAccess
000023764 909CO $$ooai:juser.fz-juelich.de:23764$$pdnbdelivery$$pdriver$$pVDB$$popen_access$$popenaire
000023764 9131_ $$0G:(DE-Juel1)FUEK257$$bEnvironment (Umwelt)$$kU01$$lChemie und Dynamik der Geo-Biosphäre$$vChemie und Dynamik der Geo-Biosphäre$$x0
000023764 9141_ $$y2002
000023764 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection
000023764 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR
000023764 915__ $$0StatID:(DE-HGF)0111$$2StatID$$aWoS$$bScience Citation Index Expanded
000023764 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000023764 915__ $$0StatID:(DE-HGF)0010$$2StatID$$aJCR/ISI refereed
000023764 915__ $$0StatID:(DE-HGF)0030$$2StatID$$aPeer review
000023764 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bThomson Reuters Master Journal List
000023764 9201_ $$0I:(DE-Juel1)VDB47$$d31.12.2006$$gICG$$kICG-I$$lStratosphäre$$x0
000023764 970__ $$aVDB:(DE-Juel1)14719
000023764 9801_ $$aFullTexts
000023764 980__ $$aVDB
000023764 980__ $$aConvertedRecord
000023764 980__ $$ajournal
000023764 980__ $$aI:(DE-Juel1)IEK-7-20101013
000023764 980__ $$aUNRESTRICTED
000023764 981__ $$aI:(DE-Juel1)ICE-4-20101013
000023764 981__ $$aI:(DE-Juel1)IEK-7-20101013