000057451 001__ 57451
000057451 005__ 20240712100819.0
000057451 0247_ $$2WOS$$aWOS:000238675600010
000057451 0247_ $$2doi$$a10.5194/acp-6-2483-2006
000057451 0247_ $$2Handle$$a2128/8673
000057451 037__ $$aPreJuSER-57451
000057451 041__ $$aeng
000057451 082__ $$a550
000057451 084__ $$2WoS$$aMeteorology & Atmospheric Sciences
000057451 1001_ $$0P:(DE-HGF)0$$aDorf, M.$$b0
000057451 245__ $$aBalloon-borne stratospheric BrO measurements: comparison with Envisat/SCIAMACHY BrO limb profiles
000057451 260__ $$aKatlenburg-Lindau$$bEGU$$c2006
000057451 300__ $$a2483 - 2501
000057451 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article
000057451 3367_ $$2DataCite$$aOutput Types/Journal article
000057451 3367_ $$00$$2EndNote$$aJournal Article
000057451 3367_ $$2BibTeX$$aARTICLE
000057451 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000057451 3367_ $$2DRIVER$$aarticle
000057451 440_0 $$09601$$aAtmospheric Chemistry and Physics$$v6$$x1680-7316
000057451 500__ $$aRecord converted from VDB: 12.11.2012
000057451 520__ $$aFor the first time, results of four stratospheric BrO profiling instruments, are presented and compared with reference to the SLIMCAT 3-dimensional chemical transport model (3-D CTM). Model calculations are used to infer a BrO profile validation set, measured by 3 different balloon sensors, for the new Envisat/SCIAMACHY (ENVIronment SATellite/SCanning Imaging Absorption spectroMeter for Atmospheric CHartographY) satellite instrument. The balloon observations include ( a) balloon-borne in situ resonance fluorescence detection of BrO ( Triple), (b) balloon-borne solar occultation DOAS measurements ( Differential Optical Absorption Spectroscopy) of BrO in the UV, and ( c) BrO profiling from the solar occultation SAOZ ( Systeme d'Analyse par Observation Zenithale) balloon instrument. Since stratospheric BrO is subject to considerable diurnal variation and none of the measurements are performed close enough in time and space for a direct comparison, all balloon observations are considered with reference to outputs from the 3-D CTM. The referencing is performed by forward and backward air mass trajectory calculations to match the balloon with the satellite observations. The diurnal variation of BrO is considered by 1-D photochemical model calculation along the trajectories. The 1-D photochemical model is initialised with output data of the 3-D model with additional constraints on the vertical transport, the total amount and photochemistry of stratospheric bromine as given by the various balloon observations. Total [Br-y]=(20.1 +/- 2.5) pptv obtained from DOAS BrO observations at mid-latitudes in 2003, serves as an upper limit of the comparison. Most of the balloon observations agree with the photochemical model predictions within their given error estimates. First retrieval exercises of BrO limb profiling from the SCIAMACHY satellite instrument on average agree to around 20% with the photochemically-corrected balloon observations of the remote sensing instruments (SAOZ and DOAS). An exception is the in situ Triple profile, in which the balloon and satellite data mostly does not agree within the given errors. In general, the satellite measurements show systematically higher values below 25 km than the balloon data and a change in profile shape above about 25 km.
000057451 536__ $$0G:(DE-Juel1)FUEK406$$2G:(DE-HGF)$$aAtmosphäre und Klima$$cP22$$x0
000057451 588__ $$aDataset connected to Web of Science
000057451 650_7 $$2WoSType$$aJ
000057451 7001_ $$0P:(DE-HGF)0$$aBösch, H.$$b1
000057451 7001_ $$0P:(DE-HGF)0$$aButz, A.$$b2
000057451 7001_ $$0P:(DE-HGF)0$$aCamy-Peyret, C.$$b3
000057451 7001_ $$0P:(DE-HGF)0$$aChipperfield, M. P.$$b4
000057451 7001_ $$0P:(DE-HGF)0$$aEngel, A$$b5
000057451 7001_ $$0P:(DE-HGF)0$$aGoutail, F.$$b6
000057451 7001_ $$0P:(DE-HGF)0$$aGrunow, K.$$b7
000057451 7001_ $$0P:(DE-HGF)0$$aHendrick, F.$$b8
000057451 7001_ $$0P:(DE-Juel1)VDB61676$$aHrechanyy, S.$$b9$$uFZJ
000057451 7001_ $$0P:(DE-HGF)0$$aNaujokat, B.$$b10
000057451 7001_ $$0P:(DE-HGF)0$$aPommereau, J. P.$$b11
000057451 7001_ $$0P:(DE-HGF)0$$avan Roozendael, M.$$b12
000057451 7001_ $$0P:(DE-HGF)0$$aSioris, C.$$b13
000057451 7001_ $$0P:(DE-Juel1)129158$$aStroh, F.$$b14$$uFZJ
000057451 7001_ $$0P:(DE-HGF)0$$aWeidner, F.$$b15
000057451 7001_ $$0P:(DE-HGF)0$$aPfeilsticker, K.$$b16
000057451 773__ $$0PERI:(DE-600)2069847-1$$a10.5194/acp-6-2483-2006$$gVol. 6, p. 2483 - 2501$$p2483 - 2501$$q6<2483 - 2501$$tAtmospheric chemistry and physics$$v6$$x1680-7316$$y2006
000057451 8564_ $$uhttps://juser.fz-juelich.de/record/57451/files/acp-6-2483-2006.pdf$$yOpenAccess
000057451 8564_ $$uhttps://juser.fz-juelich.de/record/57451/files/acp-6-2483-2006.gif?subformat=icon$$xicon$$yOpenAccess
000057451 8564_ $$uhttps://juser.fz-juelich.de/record/57451/files/acp-6-2483-2006.jpg?subformat=icon-180$$xicon-180$$yOpenAccess
000057451 8564_ $$uhttps://juser.fz-juelich.de/record/57451/files/acp-6-2483-2006.jpg?subformat=icon-700$$xicon-700$$yOpenAccess
000057451 8564_ $$uhttps://juser.fz-juelich.de/record/57451/files/acp-6-2483-2006.pdf?subformat=pdfa$$xpdfa$$yOpenAccess
000057451 909CO $$ooai:juser.fz-juelich.de:57451$$pdnbdelivery$$pVDB$$pdriver$$popen_access$$popenaire
000057451 9141_ $$aNachtrag$$y2006
000057451 915__ $$0StatID:(DE-HGF)0010$$aJCR/ISI refereed
000057451 915__ $$0StatID:(DE-HGF)0510$$aOpenAccess
000057451 9131_ $$0G:(DE-Juel1)FUEK406$$bUmwelt$$kP22$$lAtmosphäre und Klima$$vAtmosphäre und Klima$$x0$$zfortgesetzt als P23
000057451 9201_ $$0I:(DE-Juel1)VDB47$$d31.12.2006$$gICG$$kICG-I$$lStratosphäre$$x1
000057451 970__ $$aVDB:(DE-Juel1)90366
000057451 9801_ $$aFullTexts
000057451 980__ $$aFullTexts
000057451 980__ $$aConvertedRecord
000057451 980__ $$aI:(DE-Juel1)IEK-7-20101013
000057451 980__ $$ajournal
000057451 980__ $$aVDB
000057451 980__ $$aUNRESTRICTED
000057451 981__ $$aI:(DE-Juel1)ICE-4-20101013
000057451 981__ $$aI:(DE-Juel1)IEK-7-20101013