000033290 001__ 33290
000033290 005__ 20240712101000.0
000033290 0247_ $$2DOI$$a10.1029/2001JD000557
000033290 0247_ $$2WOS$$aWOS:000180428300060
000033290 0247_ $$2ISSN$$a0141-8637
000033290 0247_ $$2Handle$$a2128/20639
000033290 037__ $$aPreJuSER-33290
000033290 041__ $$aeng
000033290 082__ $$a550
000033290 084__ $$2WoS$$aMeteorology & Atmospheric Sciences
000033290 1001_ $$0P:(DE-HGF)0$$aJohnson, B. J.$$b0
000033290 245__ $$aElectrochemical concentration cell (ECC) ozonesonde pump efficiency  measurements and tests on the sensitivity to ozone of buffered and unbuffered  ECC sensor cathode solutions
000033290 260__ $$aWashington, DC$$bUnion$$c2002
000033290 300__ $$a19
000033290 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000033290 3367_ $$2DataCite$$aOutput Types/Journal article
000033290 3367_ $$00$$2EndNote$$aJournal Article
000033290 3367_ $$2BibTeX$$aARTICLE
000033290 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000033290 3367_ $$2DRIVER$$aarticle
000033290 440_0 $$06393$$aJournal of Geophysical Research D: Atmospheres$$v107$$x0148-0227
000033290 500__ $$aRecord converted from VDB: 12.11.2012
000033290 520__ $$a[1] On the basis of extensive laboratory and field tests of electrochemical concentration cell (ECC) ozonesondes, a height-dependent artifact in ozone profile measurements was found that is primarily due to side reactions of the phosphate buffers used in the "standard'' 1% potassium iodide sensing solution. The influence of the buffers was revealed as a result of new, direct measurements of the ozonesonde pump flow rate efficiency made in an environmental chamber using an oil bubble flowmeter developed at National Oceanic and Atmospheric Administration/Climate Monitoring and Diagnostics Laboratory (NOAA/CMDL). The new flow rate measurements give pump efficiency correction factors that are 2 and 15% greater at 100 and 5 hPa, respectively, than those used in currently recommended procedures. Profile measurements using ozonesondes with differing ECC sensor solutions, on dual-sonde balloons and experiments in a simulation chamber, show that the impact of the buffers is most pronounced above the ozone partial pressure maximum. The effect is about a 10-15% overmeasurement of ozone at an altitude of 30 km. Careful consideration must be given to the combination of the sensing solution composition and pump efficiency correction if representative ozone profiles are to be obtained from ozonesonde measurements.
000033290 536__ $$0G:(DE-Juel1)FUEK257$$2G:(DE-HGF)$$aChemie und Dynamik der Geo-Biosphäre$$cU01$$x0
000033290 588__ $$aDataset connected to Web of Science
000033290 650_7 $$2WoSType$$aJ
000033290 65320 $$2Author$$aozonesonde
000033290 65320 $$2Author$$aiodometric method
000033290 65320 $$2Author$$aintercomparison
000033290 7001_ $$0P:(DE-HGF)0$$aOltmans, S.$$b1
000033290 7001_ $$0P:(DE-HGF)0$$aVömel, H.$$b2
000033290 7001_ $$0P:(DE-Juel1)16203$$aSmit, A. B.$$b3$$uFZJ
000033290 7001_ $$0P:(DE-HGF)0$$aDeshler, M. C.$$b4
000033290 7001_ $$0P:(DE-HGF)0$$aKröger, C.$$b5
000033290 773__ $$0PERI:(DE-600)2016800-7 $$a10.1029/2001JD000557$$gVol. 107, p. 19$$p19$$q107<19$$tJournal of geophysical research / Atmospheres  $$tJournal of Geophysical Research$$v107$$x0148-0227$$y2002
000033290 8567_ $$uhttp://dx.doi.org/10.1029/2001JD000557
000033290 8564_ $$uhttps://juser.fz-juelich.de/record/33290/files/2001JD000557.pdf$$yOpenAccess
000033290 8564_ $$uhttps://juser.fz-juelich.de/record/33290/files/2001JD000557.pdf?subformat=pdfa$$xpdfa$$yOpenAccess
000033290 909CO $$ooai:juser.fz-juelich.de:33290$$pdnbdelivery$$pdriver$$pVDB$$popen_access$$popenaire
000033290 9131_ $$0G:(DE-Juel1)FUEK257$$bEnvironment (Umwelt)$$kU01$$lChemie und Dynamik der Geo-Biosphäre$$vChemie und Dynamik der Geo-Biosphäre$$x0
000033290 9141_ $$y2001
000033290 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection
000033290 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR
000033290 915__ $$0StatID:(DE-HGF)0111$$2StatID$$aWoS$$bScience Citation Index Expanded
000033290 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000033290 915__ $$0StatID:(DE-HGF)0010$$2StatID$$aJCR/ISI refereed
000033290 915__ $$0StatID:(DE-HGF)0030$$2StatID$$aPeer review
000033290 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bThomson Reuters Master Journal List
000033290 9201_ $$0I:(DE-Juel1)VDB48$$d31.12.2006$$gICG$$kICG-II$$lTroposphäre$$x0
000033290 970__ $$aVDB:(DE-Juel1)3770
000033290 9801_ $$aFullTexts
000033290 980__ $$aVDB
000033290 980__ $$aConvertedRecord
000033290 980__ $$ajournal
000033290 980__ $$aI:(DE-Juel1)IEK-8-20101013
000033290 980__ $$aUNRESTRICTED
000033290 981__ $$aI:(DE-Juel1)ICE-3-20101013
000033290 981__ $$aI:(DE-Juel1)IEK-8-20101013