000033263 001__ 33263
000033263 005__ 20240712100959.0
000033263 0247_ $$2DOI$$a10.1029/2001JD000793
000033263 0247_ $$2WOS$$aWOS:000178896500003
000033263 0247_ $$2ISSN$$a0141-8637
000033263 0247_ $$2Handle$$a2128/20859
000033263 037__ $$aPreJuSER-33263
000033263 041__ $$aeng
000033263 082__ $$a550
000033263 084__ $$2WoS$$aMeteorology & Atmospheric Sciences
000033263 1001_ $$0P:(DE-HGF)0$$aNedoluha, G. E.$$b0
000033263 245__ $$aPolar Ozone and Aerosol Measurement III measurements of water vapor in the  upper troposphere and lowermost stratosphere
000033263 260__ $$aWashington, DC$$bUnion$$c2002
000033263 300__ $$a10
000033263 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000033263 3367_ $$2DataCite$$aOutput Types/Journal article
000033263 3367_ $$00$$2EndNote$$aJournal Article
000033263 3367_ $$2BibTeX$$aARTICLE
000033263 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000033263 3367_ $$2DRIVER$$aarticle
000033263 440_0 $$06393$$aJournal of Geophysical Research D: Atmospheres$$v107$$x0148-0227
000033263 500__ $$aRecord converted from VDB: 12.11.2012
000033263 520__ $$a[1] We present water vapor measurements made by the Polar Ozone and Aerosol Measurement (POAM) III instrument since May 1998 in the upper troposphere and lowermost stratosphere. While POAM III is primarily a stratospheric instrument, many of the POAM III occultation measurements allow for the retrieval of water vapor in the upper troposphere. The Measurements of Ozone and Water Vapor by Airbus In-Service Aircraft (MOZAIC) instruments provide a large number of coincident measurements and thus offer the best opportunity to validate POAM measurements in the highly spatially variable regions of the upper troposphere-lowermost stratosphere, where the mixing ratios are much larger than those found throughout most of the stratosphere. The comparison shows that there is no statistically significant difference in the response of the two instruments to changes in water vapor and that in the regime where the MOZAIC measurements are thought to be most accurate, the water vapor mixing ratios measured by POAM are 10% higher. The POAM III Northern Hemisphere measurements are taken from 55 to 71 and show a qualitatively reasonable seasonal variation, with high mixing ratios in the upper troposphere in the summer and low mixing ratios in the winter. Comparisons of the seasonal variations of the POAM measurements with those from the upper tropospheric Microwave Limb Sounder (MLS) measurements from the early 1990s show qualitative similarities. The similar to1 km vertical resolution of POAM measurements allows us to study in greater detail than other satellite instruments the complex variations in water vapor that occur in the upper troposphere and lowermost stratosphere. Among the interesting features observed is a rise in the level of the high-latitude hygropause from April through September.
000033263 536__ $$0G:(DE-Juel1)FUEK257$$2G:(DE-HGF)$$aChemie und Dynamik der Geo-Biosphäre$$cU01$$x0
000033263 588__ $$aDataset connected to Web of Science
000033263 650_7 $$2WoSType$$aJ
000033263 65320 $$2Author$$awater vapor
000033263 65320 $$2Author$$alowermost stratosphere
000033263 65320 $$2Author$$aupper troposphere
000033263 7001_ $$0P:(DE-HGF)0$$aBevilacqua, R.$$b1
000033263 7001_ $$0P:(DE-HGF)0$$aHoppel, K. W.$$b2
000033263 7001_ $$0P:(DE-HGF)0$$aLumpe, J. D.$$b3
000033263 7001_ $$0P:(DE-Juel1)16203$$aSmit, H. G. J.$$b4$$uFZJ
000033263 773__ $$0PERI:(DE-600)2016800-7 $$a10.1029/2001JD000793$$gVol. 107, p. 10$$p10$$q107<10$$tJournal of geophysical research / Atmospheres  $$tJournal of Geophysical Research$$v107$$x0148-0227$$y2002
000033263 8567_ $$uhttp://dx.doi.org/10.1029/2001JD000793
000033263 8564_ $$uhttps://juser.fz-juelich.de/record/33263/files/2001JD000793.pdf$$yOpenAccess
000033263 8564_ $$uhttps://juser.fz-juelich.de/record/33263/files/2001JD000793.pdf?subformat=pdfa$$xpdfa$$yOpenAccess
000033263 909CO $$ooai:juser.fz-juelich.de:33263$$pdnbdelivery$$pdriver$$pVDB$$popen_access$$popenaire
000033263 9131_ $$0G:(DE-Juel1)FUEK257$$bEnvironment (Umwelt)$$kU01$$lChemie und Dynamik der Geo-Biosphäre$$vChemie und Dynamik der Geo-Biosphäre$$x0
000033263 9141_ $$aNachtrag 2002$$y2001
000033263 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection
000033263 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR
000033263 915__ $$0StatID:(DE-HGF)0111$$2StatID$$aWoS$$bScience Citation Index Expanded
000033263 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000033263 915__ $$0StatID:(DE-HGF)0010$$2StatID$$aJCR/ISI refereed
000033263 915__ $$0StatID:(DE-HGF)0030$$2StatID$$aPeer review
000033263 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bThomson Reuters Master Journal List
000033263 9201_ $$0I:(DE-Juel1)VDB48$$d31.12.2006$$gICG$$kICG-II$$lTroposphäre$$x0
000033263 970__ $$aVDB:(DE-Juel1)3745
000033263 9801_ $$aFullTexts
000033263 980__ $$aVDB
000033263 980__ $$aConvertedRecord
000033263 980__ $$ajournal
000033263 980__ $$aI:(DE-Juel1)IEK-8-20101013
000033263 980__ $$aUNRESTRICTED
000033263 981__ $$aI:(DE-Juel1)ICE-3-20101013
000033263 981__ $$aI:(DE-Juel1)IEK-8-20101013