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| Titel |
Ozone production and transport over the Amazon Basin during the dry-to-wet and wet-to-dry transition seasons |
| VerfasserIn |
M. M. Bela, K. M. Longo, S. R. Freitas, D. S. Moreira, V. Beck, S. C. Wofsy, C. Gerbig, K. Wiedemann, M. O. Andreae, P. Artaxo |
| Medientyp |
Artikel
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| Sprache |
Englisch
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| ISSN |
1680-7316
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| Digitales Dokument |
URL |
| Erschienen |
In: Atmospheric Chemistry and Physics ; 15, no. 2 ; Nr. 15, no. 2 (2015-01-21), S.757-782 |
| Datensatznummer |
250119338
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| Publikation (Nr.) |
 copernicus.org/acp-15-757-2015.pdf |
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| Zusammenfassung |
| The Regional Carbon Balance in Amazonia (BARCA) campaign provided the first
Amazon Basin-wide aircraft measurements of ozone (O3) during both the
dry-to-wet (November and December 2008) and wet-to-dry (May 2009) transition
seasons. Extremely low background values (< 20 ppb) were observed
to the west and north of Manaus in both seasons and in all regions during the
wet-to-dry transition. On the other hand, elevated O3 levels
(40–60 ppb) were seen during the dry-to-wet transition to the east and
south of Manaus, where biomass burning emissions of O3 precursors were
present. Chemistry simulations with the CCATT-BRAMS and WRF-Chem models are
within the error bars of the observed O3 profiles in the boundary layer
(0–3 km a.s.l.) in polluted conditions. However, the models overestimate
O3 in the boundary layer in clean conditions, despite lacking the
predominant NO source from soil. In addition, O3 simulated by the models
was either within the error bars or lower than BARCA observations in
mid-levels (3–5 km a.s.l.), and lower than total tropospheric O3
retrieved from the OMI/MLS instruments, which is primarily comprised of
middle troposphere O3 and thus reflects long-range transport processes.
Therefore, the models do a relatively poor job of representing the free
troposphere-boundary layer gradient in O3 compared with aircraft and
satellite observations, which could be due to missing long-range and
convective transport of O3 at mid-levels. Additional simulations with
WRF-Chem showed that the model O3 production is very sensitive to both
the O3 deposition velocities and the NOx emissions, which
were both about one-half of observed values. These results indicate the
necessity of more realistic model representations of emissions, deposition,
and convective processes for accurate monitoring and prediction of increases
in O3 production in the Amazon Basin as the regional population grows. |
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