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| Titel |
Eddy covariance fluxes and vertical concentration gradient measurements of NO and NO2 over a ponderosa pine ecosystem: observational evidence for within-canopy chemical removal of NOx |
| VerfasserIn |
K.-E. Min, S. E. Pusede, E. C. Browne, B. W. LaFranchi, R. C. Cohen |
| 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 ; 14, no. 11 ; Nr. 14, no. 11 (2014-06-04), S.5495-5512 |
| Datensatznummer |
250118770
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| Publikation (Nr.) |
 copernicus.org/acp-14-5495-2014.pdf |
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| Zusammenfassung |
| Exchange of NOx (NO+NO2) between the atmosphere and
biosphere is important for air quality, climate change, and ecosystem
nutrient dynamics. There are few direct ecosystem-scale measurements of the
direction and rate of atmosphere–biosphere exchange of NOx. As a
result, a complete description of the processes affecting NOx
following emission from soils and/or plants as they transit from within the
plant/forest canopy to the free atmosphere remains poorly constrained and
debated. Here, we describe measurements of NO and NO2 fluxes and
vertical concentration gradients made during the Biosphere Effects on
AeRosols and Photochemistry EXperiment 2009. In general, during daytime we
observe upward fluxes of NO and NO2 with counter-gradient fluxes of NO.
We find that NOx fluxes from the forest canopy are smaller than
calculated using observed flux–gradient relationships for conserved tracers
and also smaller than measured soil NO emissions. We interpret these
differences as primarily due to chemistry converting NOx to
higher nitrogen oxides within the forest canopy, which might be part of a
mechanistic explanation for the "canopy reduction factor" applied to soil
NOx emissions in large-scale models. |
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