000012594 001__ 12594
000012594 005__ 20240712100914.0
000012594 0247_ $$2DOI$$a10.1029/2009JD012731
000012594 0247_ $$2WOS$$aWOS:000280328800001
000012594 0247_ $$2ISSN$$a0022-1406
000012594 0247_ $$2ISSN$$a0148-0227
000012594 0247_ $$2Handle$$a2128/20498
000012594 037__ $$aPreJuSER-12594
000012594 041__ $$aeng
000012594 082__ $$a550
000012594 082__ $$a550
000012594 084__ $$2WoS$$aMeteorology & Atmospheric Sciences
000012594 1001_ $$0P:(DE-HGF)0$$aTilmes, S.$$b0
000012594 245__ $$aAn Aircraft-based Upper Troposphere Lower Stratosphere O3, CO and H2O Climatology for the Northern Hemisphere
000012594 260__ $$aWashington, DC$$aWashington, DC$$bUnion$$bUnion$$c2010
000012594 300__ $$aD14303
000012594 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000012594 3367_ $$2DataCite$$aOutput Types/Journal article
000012594 3367_ $$00$$2EndNote$$aJournal Article
000012594 3367_ $$2BibTeX$$aARTICLE
000012594 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000012594 3367_ $$2DRIVER$$aarticle
000012594 440_0 $$03369$$aJournal of Geophysical Research$$v115$$x0022-1406
000012594 500__ $$aThis work is supported in part by the National Center for Atmospheric Research (NCAR) in support by the National Science Foundation and by the NASA Upper Atmosphere Program. Research at the Jet Propulsion Laboratory was performed under contract with NASA. Thanks are also due to NCEP Environmental Modeling Center (EMC) for providing meteorological analysis. The authors thank Louisa Emmons and Rolando Garcia for helpful comments and suggestions.
000012594 520__ $$aWe present a climatology of O-3, CO, and H2O for the upper troposphere and lower stratosphere (UTLS), based on a large collection of high-resolution research aircraft data taken between 1995 and 2008. To group aircraft observations with sparse horizontal coverage, the UTLS is divided into three regimes: the tropics, subtropics, and the polar region. These regimes are defined using a set of simple criteria based on tropopause height and multiple tropopause conditions. Tropopause-referenced tracer profiles and tracer-tracer correlations show distinct characteristics for each regime, which reflect the underlying transport processes. The UTLS climatology derived here shows many features of earlier climatologies. In addition, mixed air masses in the subtropics, identified by O-3-CO correlations, show two characteristic modes in the tracer-tracer space that are a result of mixed air masses in layers above and below the tropopause (TP). A thin layer of mixed air (1-2 km around the tropopause) is identified for all regions and seasons, where tracer gradients across the TP are largest. The most pronounced influence of mixing between the tropical transition layer and the subtropics was found in spring and summer in the region above 380 K potential temperature. The vertical extent of mixed air masses between UT and LS reaches up to 5 km above the TP. The tracer correlations and distributions in the UTLS derived here can serve as a reference for model and satellite data evaluation.
000012594 536__ $$0G:(DE-Juel1)FUEK491$$2G:(DE-HGF)$$aAtmosphäre und Klima$$cP23$$x0
000012594 588__ $$aDataset connected to Web of Science
000012594 650_7 $$2WoSType$$aJ
000012594 7001_ $$0P:(DE-HGF)0$$aPan, L.L.$$b1
000012594 7001_ $$0P:(DE-HGF)0$$aHoor, P.$$b2
000012594 7001_ $$0P:(DE-HGF)0$$aAtlas, E.$$b3
000012594 7001_ $$0P:(DE-HGF)0$$aAvery, M.A.$$b4
000012594 7001_ $$0P:(DE-HGF)0$$aCampos, T.$$b5
000012594 7001_ $$0P:(DE-HGF)0$$aCristensen, L.E.$$b6
000012594 7001_ $$0P:(DE-HGF)0$$aDiskin, G.S.$$b7
000012594 7001_ $$0P:(DE-HGF)0$$aGao, R.-S.$$b8
000012594 7001_ $$0P:(DE-HGF)0$$aHerman, R.L.$$b9
000012594 7001_ $$0P:(DE-HGF)0$$aHintsa, E.J.$$b10
000012594 7001_ $$0P:(DE-HGF)0$$aLoewenstein, M.$$b11
000012594 7001_ $$0P:(DE-HGF)0$$aLopez, J.$$b12
000012594 7001_ $$0P:(DE-HGF)0$$aPaige, M.E.$$b13
000012594 7001_ $$0P:(DE-HGF)0$$aPittman, J.V.$$b14
000012594 7001_ $$0P:(DE-HGF)0$$aPodolske, J.r.$$b15
000012594 7001_ $$0P:(DE-HGF)0$$aProffitt, J.R.$$b16
000012594 7001_ $$0P:(DE-HGF)0$$aSachse, G.W.$$b17
000012594 7001_ $$0P:(DE-Juel1)VDB1410$$aSchiller, C.$$b18$$uFZJ
000012594 7001_ $$0P:(DE-HGF)0$$aSchlager, H.$$b19
000012594 7001_ $$0P:(DE-HGF)0$$aSmith, J.$$b20
000012594 7001_ $$0P:(DE-Juel1)129155$$aSpelten, N.$$b21$$uFZJ
000012594 7001_ $$0P:(DE-HGF)0$$aWebster, C.$$b22
000012594 7001_ $$0P:(DE-HGF)0$$aWeinheimer, A.$$b23
000012594 7001_ $$0P:(DE-HGF)0$$aZondlo, M.A.$$b24
000012594 773__ $$0PERI:(DE-600)2016800-7$$a10.1029/2009JD012731$$gVol. 115, p. D14303$$pD14303$$q115<D14303$$tJournal of geophysical research / Atmospheres$$v115$$x0022-1406$$y2010
000012594 8567_ $$uhttp://dx.doi.org/10.1029/2009JD012731
000012594 8564_ $$uhttps://juser.fz-juelich.de/record/12594/files/2009JD012731.pdf$$yOpenAccess
000012594 8564_ $$uhttps://juser.fz-juelich.de/record/12594/files/2009JD012731.pdf?subformat=pdfa$$xpdfa$$yOpenAccess
000012594 909CO $$ooai:juser.fz-juelich.de:12594$$pdnbdelivery$$pdriver$$pVDB$$popen_access$$popenaire
000012594 9131_ $$0G:(DE-Juel1)FUEK491$$bErde und Umwelt$$kP23$$lAtmosphäre und Klima$$vAtmosphäre und Klima$$x0$$zvormals P22
000012594 9141_ $$y2010
000012594 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000012594 915__ $$0StatID:(DE-HGF)0010$$aJCR/ISI refereed
000012594 9201_ $$0I:(DE-Juel1)IEK-7-20101013$$gIEK$$kIEK-7$$lStratosphäre$$x0
000012594 970__ $$aVDB:(DE-Juel1)124280
000012594 9801_ $$aFullTexts
000012594 980__ $$aVDB
000012594 980__ $$aConvertedRecord
000012594 980__ $$ajournal
000012594 980__ $$aI:(DE-Juel1)IEK-7-20101013
000012594 980__ $$aUNRESTRICTED
000012594 981__ $$aI:(DE-Juel1)ICE-4-20101013