000062611 001__ 62611
000062611 005__ 20240712100855.0
000062611 0247_ $$2DOI$$a10.1029/2008GL033641
000062611 0247_ $$2WOS$$aWOS:000256137900004
000062611 0247_ $$2Handle$$a2128/20682
000062611 037__ $$aPreJuSER-62611
000062611 041__ $$aeng
000062611 082__ $$a550
000062611 084__ $$2WoS$$aGeosciences, Multidisciplinary
000062611 1001_ $$0P:(DE-HGF)0$$aCorti, T.$$b0
000062611 245__ $$aUnprecedented evidence for deep convection hydrating the tropical stratosphere
000062611 260__ $$aWashington, DC$$bAmerican Geophysical Union$$c2008
000062611 300__ $$aL10810
000062611 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000062611 3367_ $$2DataCite$$aOutput Types/Journal article
000062611 3367_ $$00$$2EndNote$$aJournal Article
000062611 3367_ $$2BibTeX$$aARTICLE
000062611 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000062611 3367_ $$2DRIVER$$aarticle
000062611 440_0 $$02249$$aGeophysical Research Letters$$v35$$x0094-8276
000062611 500__ $$aRecord converted from VDB: 12.11.2012
000062611 520__ $$aWe report on in situ and remote sensing measurements of ice particles in the tropical stratosphere found during the Geophysica campaigns TROCCINOX and SCOUT-O3. We show that the deep convective systems penetrated the stratosphere and deposited ice particles at altitudes reaching 420 K potential temperature. These convective events had a hydrating effect on the lower tropical stratosphere due to evaporation of the ice particles. In contrast, there were no signs of convectively induced dehydration in the stratosphere.
000062611 536__ $$0G:(DE-Juel1)FUEK406$$2G:(DE-HGF)$$aAtmosphäre und Klima$$cP22$$x0
000062611 588__ $$aDataset connected to Web of Science
000062611 650_7 $$2WoSType$$aJ
000062611 7001_ $$0P:(DE-HGF)0$$aLuo, B. P.$$b1
000062611 7001_ $$0P:(DE-HGF)0$$ade Reus, M.$$b2
000062611 7001_ $$0P:(DE-HGF)0$$aBrunner, D.$$b3
000062611 7001_ $$0P:(DE-HGF)0$$aCairo, F.$$b4
000062611 7001_ $$0P:(DE-HGF)0$$aMahoney, M.J.$$b5
000062611 7001_ $$0P:(DE-HGF)0$$aMartucci, G.$$b6
000062611 7001_ $$0P:(DE-HGF)0$$aMatthey, R.$$b7
000062611 7001_ $$0P:(DE-HGF)0$$aMitev, V.$$b8
000062611 7001_ $$0P:(DE-Juel1)VDB65027$$ados Santos, F. H.$$b9$$uFZJ
000062611 7001_ $$0P:(DE-Juel1)VDB1410$$aSchiller, C.$$b10$$uFZJ
000062611 7001_ $$0P:(DE-HGF)0$$aShur, G.$$b11
000062611 7001_ $$0P:(DE-HGF)0$$aSitnikov, N.M.$$b12
000062611 7001_ $$0P:(DE-Juel1)129155$$aSpelten, N.$$b13$$uFZJ
000062611 7001_ $$0P:(DE-HGF)0$$aVössing, H.J.$$b14
000062611 7001_ $$0P:(DE-HGF)0$$aBorrmann, S.$$b15
000062611 7001_ $$0P:(DE-HGF)0$$aPeter, T.$$b16
000062611 773__ $$0PERI:(DE-600)2021599-X$$a10.1029/2008GL033641$$gVol. 35, p. L10810$$pL10810$$q35<L10810$$tGeophysical research letters$$v35$$x0094-8276$$y2008
000062611 8567_ $$uhttp://dx.doi.org/10.1029/2008GL033641
000062611 8564_ $$uhttps://juser.fz-juelich.de/record/62611/files/2008GL033641.pdf$$yOpenAccess
000062611 8564_ $$uhttps://juser.fz-juelich.de/record/62611/files/2008GL033641.pdf?subformat=pdfa$$xpdfa$$yOpenAccess
000062611 909CO $$ooai:juser.fz-juelich.de:62611$$pdnbdelivery$$pdriver$$pVDB$$popen_access$$popenaire
000062611 9131_ $$0G:(DE-Juel1)FUEK406$$bUmwelt$$kP22$$lAtmosphäre und Klima$$vAtmosphäre und Klima$$x0$$zfortgesetzt als P23
000062611 9141_ $$y2008
000062611 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000062611 915__ $$0StatID:(DE-HGF)0010$$aJCR/ISI refereed
000062611 9201_ $$0I:(DE-Juel1)VDB790$$d30.09.2010$$gICG$$kICG-1$$lStratosphäre$$x1
000062611 970__ $$aVDB:(DE-Juel1)99135
000062611 9801_ $$aFullTexts
000062611 980__ $$aVDB
000062611 980__ $$aConvertedRecord
000062611 980__ $$ajournal
000062611 980__ $$aI:(DE-Juel1)IEK-7-20101013
000062611 980__ $$aUNRESTRICTED
000062611 981__ $$aI:(DE-Juel1)ICE-4-20101013
000062611 981__ $$aI:(DE-Juel1)IEK-7-20101013