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Verfasst von:Herrmann, Maximilian [VerfasserIn]   i
 Sihler, Holger [VerfasserIn]   i
 Frieß, Udo [VerfasserIn]   i
 Wagner, Thomas [VerfasserIn]   i
 Platt, Ulrich [VerfasserIn]   i
 Gutheil, Eva [VerfasserIn]   i
Titel:Time-dependent 3D simulations of tropospheric ozone depletion events in the Arctic spring using the Weather Research and Forecasting model coupled with Chemistry (WRF-Chem)
Verf.angabe:Maximilian Herrmann, Holger Sihler, Udo Frieß, Thomas Wagner, Ulrich Platt, and Eva Gutheil
E-Jahr:2021
Jahr:20 May 2021
Umfang:8 S.
Teil:volume:21
 year:2021
 number:10
 pages:7611-7638
 extent:8
Fussnoten:Gesehen am 07.07.2021
Titel Quelle:Enthalten in: Atmospheric chemistry and physics
Ort Quelle:Katlenburg-Lindau : EGU, 2001
Jahr Quelle:2021
Band/Heft Quelle:21(2021), 10, Seite 7611-7638
ISSN Quelle:1680-7324
Abstract:<p><strong class="journal-contentHeaderColor">Abstract.</strong> Tropospheric bromine release and ozone depletion events (ODEs) as they commonly occur in the Arctic spring are studied using a regional model based on the open-source software package Weather Research and Forecasting model coupled with Chemistry (WRF-Chem). For this purpose, the MOZART (Model for Ozone and Related chemical Tracers)-MOSAIC (Model for Simulating Aerosol Interactions and Chemistry) chemical reaction mechanism is extended by bromine and chlorine reactions as well as an emission mechanism for reactive bromine via heterogeneous reactions on snow surfaces. The simulation domain covers an area of <span class="inline-formula">5040 km×4960 km</span>, centered north of Utqiaġvik (formerly Barrow), Alaska, and the time interval from February through May 2009. Several simulations for different strengths of the bromine emission are conducted and evaluated by comparison with in situ and ozone sonde measurements of ozone mixing ratios as well as by comparison with tropospheric BrO vertical column densities (VCDs) from the Global Ozone Monitoring Experiment-2 (GOME-2) satellite instrument. The base bromine emission scheme includes the direct emission of bromine due to bromide oxidation by ozone. Results of simulations with the base emission rate agree well with the observations; however, a simulation with 50 % faster emissions performs somewhat better. The bromine emission due to bromide oxidation by ozone is found to be important to provide an initial seed for the bromine explosion. Bromine release due to <span class="inline-formula">N<sub>2</sub>O<sub>5</sub></span> was found to be important from February to mid March but irrelevant thereafter. A comparison of modeled BrO with in situ and multi-axis differential optical absorption spectroscopy (MAX-DOAS) data hints at missing bromine release and recycling mechanisms on land or near coasts. A consideration of halogen chemistry substantially improves the prediction of the ozone mixing ratio with respect to the observations. Meteorological nudging is essential for a good prediction of ODEs over the 3-month period.</p>
DOI:doi:10.5194/acp-21-7611-2021
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Volltext ; Verlag: https://doi.org/10.5194/acp-21-7611-2021
 Volltext: https://acp.copernicus.org/articles/21/7611/2021/
 DOI: https://doi.org/10.5194/acp-21-7611-2021
Datenträger:Online-Ressource
Sprache:eng
K10plus-PPN:1762311445
Verknüpfungen:→ Zeitschrift

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