000052885 001__ 52885
000052885 005__ 20240712101053.0
000052885 0247_ $$2DOI$$a10.1029/2006JD007442
000052885 0247_ $$2WOS$$aWOS:000245017000002
000052885 0247_ $$2ISSN$$a0141-8637
000052885 0247_ $$2Handle$$a2128/20426
000052885 037__ $$aPreJuSER-52885
000052885 041__ $$aeng
000052885 082__ $$a550
000052885 084__ $$2WoS$$aMeteorology & Atmospheric Sciences
000052885 1001_ $$0P:(DE-HGF)0$$aDinar, E.$$b0
000052885 245__ $$aHygroscopic growth of atmospheric and model humic-like substances
000052885 260__ $$aWashington, DC$$bUnion$$c2007
000052885 300__ $$aD05211
000052885 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000052885 3367_ $$2DataCite$$aOutput Types/Journal article
000052885 3367_ $$00$$2EndNote$$aJournal Article
000052885 3367_ $$2BibTeX$$aARTICLE
000052885 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000052885 3367_ $$2DRIVER$$aarticle
000052885 440_0 $$06393$$aJournal of Geophysical Research D: Atmospheres$$v112$$x0148-0227
000052885 500__ $$aRecord converted from VDB: 12.11.2012
000052885 520__ $$aThe hygroscopic growth (HG) of humic-like substances (HULIS) extracted from smoke and pollution aerosol particles and of Suwannee River fulvic acid (SRFA, bulk and fractions of different molecular weight) was measured by humidity tandem differential mobility analyzer (H-TDMA). By characterizing physical and chemical parameters such as molecular weight, elemental composition, and surface tension, we test the effect of these parameters on particle interactions with water vapor. For molecular weight-fractionated SRFA fractions, the growth factor at 90% relative humidity was generally inversely proportional to the molecular weight. HULIS extracts from ambient particles are more hygroscopic than all the SRFA fractions and exhibit different hygroscopic properties depending on their origin and residence time in the atmosphere. The results point out some dissimilarities between SRFA and aerosol- derived HULIS. The cloud condensation nuclei (CCN) behavior of the studied materials was predicted on the basis of hygroscopic growth using a recently introduced approach of Kreidenweis et al. (2005) and compared to CCN activity measurements on the same samples (Dinar et al., 2006). It is found that the computational approach (Kreidenweis et al., 2005) works reasonably well for SRFA fractions but is limited in use for the HULIS extracts from aerosol particles. The difficulties arise from uncertainties associated with HG measurements at high relative humidity, which leads to large errors in the predicted CCN activity.
000052885 536__ $$0G:(DE-Juel1)FUEK406$$2G:(DE-HGF)$$aAtmosphäre und Klima$$cP22$$x0
000052885 588__ $$aDataset connected to Web of Science
000052885 650_7 $$2WoSType$$aJ
000052885 7001_ $$0P:(DE-HGF)0$$aTaraniuk, I.$$b1
000052885 7001_ $$0P:(DE-HGF)0$$aGraber, E. R.$$b2
000052885 7001_ $$0P:(DE-Juel1)VDB45939$$aAnttila, T.$$b3$$uFZJ
000052885 7001_ $$0P:(DE-Juel1)16346$$aMentel, T. F.$$b4$$uFZJ
000052885 7001_ $$0P:(DE-HGF)0$$aRudich, Y.$$b5
000052885 773__ $$0PERI:(DE-600)2016800-7 $$a10.1029/2006JD007442$$gVol. 112, p. D05211$$pD05211$$q112<D05211$$tJournal of geophysical research / Atmospheres $$tJournal of Geophysical Research$$v112$$x0148-0227$$y2007
000052885 8567_ $$uhttp://dx.doi.org/10.1029/2006JD007442
000052885 8564_ $$uhttps://juser.fz-juelich.de/record/52885/files/2006JD007442.pdf$$yOpenAccess
000052885 8564_ $$uhttps://juser.fz-juelich.de/record/52885/files/2006JD007442.pdf?subformat=pdfa$$xpdfa$$yOpenAccess
000052885 909CO $$ooai:juser.fz-juelich.de:52885$$pdnbdelivery$$pdriver$$pVDB$$popen_access$$popenaire
000052885 9131_ $$0G:(DE-Juel1)FUEK406$$bUmwelt$$kP22$$lAtmosphäre und Klima$$vAtmosphäre und Klima$$x0$$zfortgesetzt als P23
000052885 9141_ $$y2007
000052885 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection
000052885 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR
000052885 915__ $$0StatID:(DE-HGF)0111$$2StatID$$aWoS$$bScience Citation Index Expanded
000052885 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000052885 915__ $$0StatID:(DE-HGF)0010$$2StatID$$aJCR/ISI refereed
000052885 915__ $$0StatID:(DE-HGF)0030$$2StatID$$aPeer review
000052885 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bThomson Reuters Master Journal List
000052885 9201_ $$0I:(DE-Juel1)VDB791$$d30.09.2010$$gICG$$kICG-2$$lTroposphäre$$x1
000052885 970__ $$aVDB:(DE-Juel1)83217
000052885 9801_ $$aFullTexts
000052885 980__ $$aVDB
000052885 980__ $$aConvertedRecord
000052885 980__ $$ajournal
000052885 980__ $$aI:(DE-Juel1)IEK-8-20101013
000052885 980__ $$aUNRESTRICTED
000052885 981__ $$aI:(DE-Juel1)ICE-3-20101013
000052885 981__ $$aI:(DE-Juel1)IEK-8-20101013