000047472 001__ 47472
000047472 005__ 20240712100829.0
000047472 0247_ $$2DOI$$a10.1029/2005JD006639
000047472 0247_ $$2WOS$$aWOS:000240945800001
000047472 0247_ $$2ISSN$$a0141-8637
000047472 0247_ $$2Handle$$a2128/20488
000047472 037__ $$aPreJuSER-47472
000047472 041__ $$aeng
000047472 082__ $$a550
000047472 084__ $$2WoS$$aMeteorology & Atmospheric Sciences
000047472 1001_ $$0P:(DE-HGF)0$$aMacKenzie, A. R.$$b0
000047472 245__ $$aTropopause and hygropause vairability over the equatorial Indian Ocean during February and March 1999
000047472 260__ $$aWashington, DC$$bUnion$$c2006
000047472 300__ $$aD18112
000047472 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000047472 3367_ $$2DataCite$$aOutput Types/Journal article
000047472 3367_ $$00$$2EndNote$$aJournal Article
000047472 3367_ $$2BibTeX$$aARTICLE
000047472 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000047472 3367_ $$2DRIVER$$aarticle
000047472 440_0 $$06393$$aJournal of Geophysical Research D: Atmospheres$$v111$$x0148-0227$$yD18
000047472 500__ $$aRecord converted from VDB: 12.11.2012
000047472 520__ $$aMeasurements of temperature, water vapor, total water, ozone, and cloud properties were made above the western equatorial Indian Ocean in February and March 1999. The cold- point tropopause was at a mean pressure- altitude of 17 km, equivalent to a potential temperature of 380 K, and had a mean temperature of 190 K. Total water mixing ratios at the hygropause varied between 1.4 and 4.1 ppmv. The mean saturation water vapor mixing ratio at the cold point was 3.0 ppmv. This does not accurately represent the mean of the measured total water mixing ratios because the air was unsaturated at the cold point for about 40% of the measurements. As well as unsaturation at the cold point, saturation was observed above the cold point on almost 30% of the profiles. In such profiles the air was saturated with respect to water ice but was free of clouds ( i. e., backscatter ratio < 2) at potential temperatures more than 5 K above the tropopause and hygropause. Individual profiles show a great deal of variability in the potential temperatures of the cold point and hygropause. We attribute this to short timescale and space- scale perturbations superimposed on the seasonal cycle. There is neither a clear and consistent " setting'' of the tropopause and hygropause to the same altitude by dehydration processes nor a clear and consistent separation of tropopause and hygropause by the Brewer- Dobson circulation. Similarly, neither the tropopause nor the hygropause provides a location where conditions consistently approach those implied by a simple " tropopause freeze drying'' or " stratospheric fountain'' hypothesis.
000047472 536__ $$0G:(DE-Juel1)FUEK406$$2G:(DE-HGF)$$aAtmosphäre und Klima$$cP22$$x0
000047472 588__ $$aDataset connected to Web of Science
000047472 650_7 $$2WoSType$$aJ
000047472 7001_ $$0P:(DE-Juel1)VDB1410$$aSchiller, C.$$b1$$uFZJ
000047472 7001_ $$0P:(DE-HGF)0$$aPeter, Th.$$b2
000047472 7001_ $$0P:(DE-HGF)0$$aAdriani, A.$$b3
000047472 7001_ $$0P:(DE-HGF)0$$aBeuermann, J.$$b4
000047472 7001_ $$0P:(DE-HGF)0$$aBujok, A. A.$$b5
000047472 7001_ $$0P:(DE-HGF)0$$aCairo, F.$$b6
000047472 7001_ $$0P:(DE-HGF)0$$aCorti, T.$$b7
000047472 7001_ $$0P:(DE-HGF)0$$aDiDonfrancesco, G.$$b8
000047472 7001_ $$0P:(DE-Juel1)6110$$aGensch, I.$$b9$$uFZJ
000047472 7001_ $$0P:(DE-HGF)0$$aKiemle, C.$$b10
000047472 7001_ $$0P:(DE-Juel1)129131$$aKrämer, M.$$b11$$uFZJ
000047472 7001_ $$0P:(DE-HGF)0$$aKröger, C.$$b12
000047472 7001_ $$0P:(DE-HGF)0$$aMerkulov, S.$$b13
000047472 7001_ $$0P:(DE-HGF)0$$aOulanovsky, A.$$b14
000047472 7001_ $$0P:(DE-HGF)0$$aRavegnani, F.$$b15
000047472 7001_ $$0P:(DE-Juel1)129146$$aRohs, S.$$b16$$uFZJ
000047472 7001_ $$0P:(DE-HGF)0$$aRudakov, V.$$b17
000047472 7001_ $$0P:(DE-HGF)0$$aSalter, P.$$b18
000047472 7001_ $$0P:(DE-HGF)0$$aSantacesaria, V.$$b19
000047472 7001_ $$0P:(DE-HGF)0$$aStefanutti, L.$$b20
000047472 7001_ $$0P:(DE-HGF)0$$aYushkov, V.$$b21
000047472 773__ $$0PERI:(DE-600)2016800-7 $$a10.1029/2005JD006639$$gVol. 111, p. D18112$$pD18112$$q111<D18112$$tJournal of geophysical research / Atmospheres  $$tJournal of Geophysical Research$$v111$$x0148-0227$$y2006
000047472 8567_ $$uhttp://dx.doi.org/10.1029/2005JD006639
000047472 8564_ $$uhttps://juser.fz-juelich.de/record/47472/files/2005JD006639.pdf$$yOpenAccess
000047472 8564_ $$uhttps://juser.fz-juelich.de/record/47472/files/2005JD006639.pdf?subformat=pdfa$$xpdfa$$yOpenAccess
000047472 909CO $$ooai:juser.fz-juelich.de:47472$$pdnbdelivery$$pdriver$$pVDB$$popen_access$$popenaire
000047472 9131_ $$0G:(DE-Juel1)FUEK406$$bUmwelt$$kP22$$lAtmosphäre und Klima$$vAtmosphäre und Klima$$x0$$zfortgesetzt als P23
000047472 9141_ $$y2006
000047472 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection
000047472 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR
000047472 915__ $$0StatID:(DE-HGF)0111$$2StatID$$aWoS$$bScience Citation Index Expanded
000047472 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000047472 915__ $$0StatID:(DE-HGF)0010$$2StatID$$aJCR/ISI refereed
000047472 915__ $$0StatID:(DE-HGF)0030$$2StatID$$aPeer review
000047472 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bThomson Reuters Master Journal List
000047472 9201_ $$0I:(DE-Juel1)VDB47$$d31.12.2006$$gICG$$kICG-I$$lStratosphäre$$x0
000047472 970__ $$aVDB:(DE-Juel1)74893
000047472 9801_ $$aFullTexts
000047472 980__ $$aVDB
000047472 980__ $$aConvertedRecord
000047472 980__ $$ajournal
000047472 980__ $$aI:(DE-Juel1)IEK-7-20101013
000047472 980__ $$aUNRESTRICTED
000047472 981__ $$aI:(DE-Juel1)ICE-4-20101013
000047472 981__ $$aI:(DE-Juel1)IEK-7-20101013