001     136133
005     20200610184609.0
024 7 _ |2 sirsi
|a (Sirsi) a292984
024 7 _ |2 ISSN
|a 0944-2952
024 7 _ |2 Handle
|a 2128/3609
037 _ _ |a PreJuSER-136133
041 _ _ |a German
084 _ 0 |a UMD - Atmospheric models
084 _ 0 |2 ZB
|a UMB - Atmospheric chemistry
088 1 _ |a Juel-2951
088 _ _ |a Juel-2951
|2 JUEL
100 1 _ |0 P:(DE-Juel1)16311
|a Poppe, Dirk
|b 0
|u fzj
245 _ _ |a A comparison of measured OH concentrations with model calculations
260 _ _ |a Jülich
|b Forschungszentrum Jülich GmbH Zentralbibliothek, Verlag
|c 1994
300 _ _ |a 44 S.
336 7 _ |0 PUB:(DE-HGF)29
|2 PUB:(DE-HGF)
|a Report
|m report
336 7 _ |2 DataCite
|a Output Types/Report
336 7 _ |2 BibTeX
|a TECHREPORT
336 7 _ |2 ORCID
|a REPORT
336 7 _ |0 10
|2 EndNote
|a Report
336 7 _ |2 DRIVER
|a report
490 0 _ |0 PERI:(DE-600)2414853-2
|a Berichte des Forschungszentrums Jülich
|v 2951
500 _ _ |a Record converted from JUWEL: 18.07.2013
520 _ _ |a The influence of chemical precursors and sunlight on the atmospheric OH abundance is investigated by a comparison of locally measured tropospheric OH concentration with model calculations. The latter are based on the gas phase reaction mechanism of the Regional Acid Deposition Model (RADM2) which incorporates an explicit inorganic and a comprehensive organic chemistry. The experimental data were obtained in the planetary boundary layer during two sets of campaigns. In Deuselbach (1983) and Schauinsland (1984) rural conditions were encountered with NO, concentrations on the average of 2.2 ppb and 0.9 ppb, respectively. This data set was already compared with model calculations based upon an older and less detailed chemical reaction scheme (Pemer et al., 1987). Since then the experimental data were reanalysed leading to modified measured OH concentrations and also to modified precursor concentrations. For a consistent comparison with the more recent campaigns in JOlich (1987 and 1988) we have redone the calculations. The modeled and measured OH-concentrations of the campaigns in 1983 and 1984 correlate well with a coefficient of correlation of r = 0.73. The model overpredicts OH by about 20%. Under more polluted conditions in JOlich with average NO, concentrations of 4 ppb the correlation coefficient between experimental and modeled data are significantly smaller (r = 0.61). Possible reasons are the influence of not measured precursors, for example isoprene, and the inapplicability of a quasi steady state model under the spatially inhomogeneous conditions in JOlich. Again the model overpredicts the OH concentration by about 15%, which is somewhat smaller than for the rural case. The precision of the comparison is limited by the uncertainties of the chemical reaction rate constants.
540 _ _ |a Neither this book nor any part of it may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, microfilming, and recording, or by any information storage and retrieval system, without permission in writing from the publisher.
650 _ 4 |a atmospheric calculation
650 _ 4 |a atmospheric chemistry
650 _ 4 |a atmospheric exchange process
650 _ 4 |a atmospheric gas
650 _ 4 |a atmospheric model
650 _ 4 |a atmospheric monitoring
653 _ _ |a chemical reaction scheme : atmospheric OH chemistry
700 1 _ |0 P:(DE-Juel1)VDB1843
|a Zimmermann, Joerg
|b 1
|u fzj
700 1 _ |0 P:(DE-Juel1)139077
|a Bauer, Reimar
|b 2
|u fzj
710 2 _ |a Institut für Atmosphärische Chemie (Jülich, 3) - ICG3
856 4 _ |u https://juser.fz-juelich.de/record/136133/files/Juel_2951_Poppe.pdf
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909 C O |o oai:juser.fz-juelich.de:136133
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