000004663 001__ 4663
000004663 005__ 20240712101030.0
000004663 0247_ $$2DOI$$a10.1029/2008JD011679
000004663 0247_ $$2WOS$$aWOS:000266742600006
000004663 0247_ $$2ISSN$$a0141-8637
000004663 0247_ $$2Handle$$a2128/20433
000004663 037__ $$aPreJuSER-4663
000004663 041__ $$aeng
000004663 082__ $$a550
000004663 084__ $$2WoS$$aMeteorology & Atmospheric Sciences
000004663 1001_ $$0P:(DE-HGF)0$$aBrown, S.S.$$b0
000004663 245__ $$aReactive uptake coefficients for N2O5 determined from aircraft measuremnts during the Second Texas Air Quality Study: Comparison to current model parameterizations
000004663 260__ $$aWashington, DC$$bUnion$$c2009
000004663 300__ $$a1 - 16
000004663 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000004663 3367_ $$2DataCite$$aOutput Types/Journal article
000004663 3367_ $$00$$2EndNote$$aJournal Article
000004663 3367_ $$2BibTeX$$aARTICLE
000004663 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000004663 3367_ $$2DRIVER$$aarticle
000004663 440_0 $$06393$$aJournal of Geophysical Research D: Atmospheres$$v114$$x0148-0227$$yD00F10
000004663 500__ $$aThis work was supported by the NOAA Atmospheric Chemistry and Climate Program and the Texas Air Quality Study. The authors thank Prakash Bhave for useful discussions regarding uptake coefficient parameterizations. The authors also thank the crew of the NOAA P-3 for their dedication and professionalism.
000004663 520__ $$aThis paper presents determinations of reactive uptake coefficients for N2O5, gamma( N2O5), on aerosols from nighttime aircraft measurements of ozone, nitrogen oxides, and aerosol surface area on the NOAA P-3 during Second Texas Air Quality Study (TexAQS II). Determinations based on both the steady state approximation for NO3 and N2O5 and a plume modeling approach yielded gamma(N2O5) substantially smaller than current parameterizations used for atmospheric modeling and generally in the range 0.5-6 x 10(-3). Dependence of gamma(N2O5) on variables such as relative humidity and aerosol composition was not apparent in the determinations, although there was considerable scatter in the data. Determinations were also inconsistent with current parameterizations of the rate coefficient for homogenous hydrolysis of N2O5 by water vapor, which may be as much as a factor of 10 too large. Nocturnal halogen activation via conversion of N2O5 to ClNO2 on chloride aerosol was not determinable from these data, although limits based on laboratory parameterizations and maximum nonrefractory aerosol chloride content showed that this chemistry could have been comparable to direct production of HNO3 in some cases.
000004663 536__ $$0G:(DE-Juel1)FUEK406$$2G:(DE-HGF)$$aAtmosphäre und Klima$$cP22$$x0
000004663 588__ $$aDataset connected to Web of Science
000004663 650_7 $$2WoSType$$aJ
000004663 7001_ $$0P:(DE-HGF)0$$aDubé, W. P.$$b1
000004663 7001_ $$0P:(DE-Juel1)7363$$aFuchs, H.$$b2$$uFZJ
000004663 7001_ $$0P:(DE-HGF)0$$aRyerson, T.B.$$b3
000004663 7001_ $$0P:(DE-HGF)0$$aWollny, A.G.$$b4
000004663 7001_ $$0P:(DE-HGF)0$$aBrock, C.A.$$b5
000004663 7001_ $$0P:(DE-HGF)0$$aBahreini, R.$$b6
000004663 7001_ $$0P:(DE-HGF)0$$aMiddlebrook, A.M.$$b7
000004663 7001_ $$0P:(DE-HGF)0$$aNeuman, J.A.$$b8
000004663 7001_ $$0P:(DE-HGF)0$$aAtlas, E.$$b9
000004663 7001_ $$0P:(DE-HGF)0$$aRoberts, J.M.$$b10
000004663 7001_ $$0P:(DE-HGF)0$$aOsthoff, H.D.$$b11
000004663 7001_ $$0P:(DE-HGF)0$$aTrainer, M.$$b12
000004663 7001_ $$0P:(DE-HGF)0$$aFehsenfeld, F.C.$$b13
000004663 7001_ $$0P:(DE-HGF)0$$aRavishankara, A.R.$$b14
000004663 773__ $$0PERI:(DE-600)2016800-7 $$a10.1029/2008JD011679$$gVol. 114, p. 1 - 16$$p1 - 16$$q114<1 - 16$$tJournal of geophysical research / Atmospheres  $$tJournal of Geophysical Research$$v114$$x0148-0227$$y2009
000004663 8567_ $$uhttp://dx.doi.org/10.1029/2008JD011679
000004663 8564_ $$uhttps://juser.fz-juelich.de/record/4663/files/2008JD011679.pdf$$yOpenAccess
000004663 8564_ $$uhttps://juser.fz-juelich.de/record/4663/files/2008JD011679.pdf?subformat=pdfa$$xpdfa$$yOpenAccess
000004663 909CO $$ooai:juser.fz-juelich.de:4663$$pdnbdelivery$$pdriver$$pVDB$$popen_access$$popenaire
000004663 9131_ $$0G:(DE-Juel1)FUEK406$$bUmwelt$$kP22$$lAtmosphäre und Klima$$vAtmosphäre und Klima$$x0$$zfortgesetzt als P23
000004663 9141_ $$y2009
000004663 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection
000004663 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR
000004663 915__ $$0StatID:(DE-HGF)0111$$2StatID$$aWoS$$bScience Citation Index Expanded
000004663 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000004663 915__ $$0StatID:(DE-HGF)0010$$2StatID$$aJCR/ISI refereed
000004663 915__ $$0StatID:(DE-HGF)0030$$2StatID$$aPeer review
000004663 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bThomson Reuters Master Journal List
000004663 9201_ $$0I:(DE-Juel1)VDB791$$d30.09.2010$$gICG$$kICG-2$$lTroposphäre$$x1
000004663 970__ $$aVDB:(DE-Juel1)111843
000004663 9801_ $$aFullTexts
000004663 980__ $$aVDB
000004663 980__ $$aConvertedRecord
000004663 980__ $$ajournal
000004663 980__ $$aI:(DE-Juel1)IEK-8-20101013
000004663 980__ $$aUNRESTRICTED
000004663 981__ $$aI:(DE-Juel1)ICE-3-20101013
000004663 981__ $$aI:(DE-Juel1)IEK-8-20101013