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dc.date.accessioned2016-05-20T09:09:22Z
dc.date.available2016-05-20T09:09:22Z
dc.date.created2011-09-01T14:41:17Z
dc.date.issued2011
dc.identifier.citationSodemann, Harald Pommier, M Arnold, SR Monks, SA Stebel, Kerstin Burkhart, John Faulkner Hair, JW Diskin, GS Clerbaux, C Coheur, PF Hurtmans, D Schlager, H Blechschmidt, Anne-Marlene Kristjansson, Jon Egill Stohl, Andreas . Episodes of cross-polar transport in the Arctic troposphere during July 2008 as seen from models, satellite, and aircraft observations. Atmospheric Chemistry and Physics. 2011, 11(8), 3631-3651
dc.identifier.urihttp://hdl.handle.net/10852/50319
dc.description.abstractDuring the POLARCAT summer campaign in 2008, two episodes (2–5 July and 7–10 July 2008) occurred where low-pressure systems traveled from Siberia across the Arctic Ocean towards the North Pole. The two cyclones had extensive smoke plumes from Siberian forest fires and anthropogenic sources in East Asia embedded in their associated air masses, creating an excellent opportunity to use satellite and aircraft observations to validate the performance of atmospheric transport models in the Arctic, which is a challenging model domain due to numerical and other complications. Here we compare transport simulations of carbon monoxide (CO) from the Lagrangian transport model FLEXPART and the Eulerian chemical transport model TOMCAT with retrievals of total column CO from the IASI passive infrared sensor onboard the MetOp-A satellite. The main aspect of the comparison is how realistic horizontal and vertical structures are represented in the model simulations. Analysis of CALIPSO lidar curtains and in situ aircraft measurements provide further independent reference points to assess how reliable the model simulations are and what the main limitations are. The horizontal structure of mid-latitude pollution plumes agrees well between the IASI total column CO and the model simulations. However, finer-scale structures are too quickly diffused in the Eulerian model. Applying the IASI averaging kernels to the model data is essential for a meaningful comparison. Using aircraft data as a reference suggests that the satellite data are biased high, while TOMCAT is biased low. FLEXPART fits the aircraft data rather well, but due to added background concentrations the simulation is not independent from observations. The multi-data, multi-model approach allows separating the influences of meteorological fields, model realisation, and grid type on the plume structure. In addition to the very good agreement between simulated and observed total column CO fields, the results also highlight the difficulty to identify a data set that most realistically represents the actual pollution state of the Arctic atmosphere.en_US
dc.languageEN
dc.language.isoenen_US
dc.publisherCopernicus
dc.rightsAttribution 3.0 Unported
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/
dc.titleEpisodes of cross-polar transport in the Arctic troposphere during July 2008 as seen from models, satellite, and aircraft observationsen_US
dc.typeJournal articleen_US
dc.creator.authorSodemann, Harald
dc.creator.authorPommier, M
dc.creator.authorArnold, SR
dc.creator.authorMonks, SA
dc.creator.authorStebel, Kerstin
dc.creator.authorBurkhart, John Faulkner
dc.creator.authorHair, JW
dc.creator.authorDiskin, GS
dc.creator.authorClerbaux, C
dc.creator.authorCoheur, PF
dc.creator.authorHurtmans, D
dc.creator.authorSchlager, H
dc.creator.authorBlechschmidt, Anne-Marlene
dc.creator.authorKristjansson, Jon Egill
dc.creator.authorStohl, Andreas
cristin.unitcode185,15,22,0
cristin.unitnameInstitutt for geofag
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1
dc.identifier.cristin836312
dc.identifier.bibliographiccitationinfo:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Atmospheric Chemistry and Physics&rft.volume=11&rft.spage=3631&rft.date=2011
dc.identifier.jtitleAtmospheric Chemistry and Physics
dc.identifier.volume11
dc.identifier.issue8
dc.identifier.startpage3631
dc.identifier.endpage3651
dc.identifier.doihttp://dx.doi.org/10.5194/acp-11-3631-2011
dc.identifier.urnURN:NBN:no-53950
dc.type.documentTidsskriftartikkelen_US
dc.type.peerreviewedPeer reviewed
dc.source.issn1680-7316
dc.identifier.fulltextFulltext https://www.duo.uio.no/bitstream/handle/10852/50319/1/acp-11-3631-2011.pdf
dc.type.versionPublishedVersion


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