Eddy covariance fluxes and vertical concentration gradient measurements of NO and NO<sub>2</sub> over a ponderosa pine ecosystem: observational evidence for within-canopy chemical removal of NO<sub>x</sub>
Exchange of NO<sub>x</sub> (NO+NO<sub>2</sub>) 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 N...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2014-06-01
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| Series: | Atmospheric Chemistry and Physics |
| Online Access: | http://www.atmos-chem-phys.net/14/5495/2014/acp-14-5495-2014.pdf |
| _version_ | 1828391782350585856 |
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| author | K.-E. Min S. E. Pusede E. C. Browne B. W. LaFranchi R. C. Cohen |
| author_facet | K.-E. Min S. E. Pusede E. C. Browne B. W. LaFranchi R. C. Cohen |
| author_sort | K.-E. Min |
| collection | DOAJ |
| description | Exchange of NO<sub>x</sub> (NO+NO<sub>2</sub>) 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 NO<sub>x</sub>. As a
result, a complete description of the processes affecting NO<sub>x</sub>
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 NO<sub>2</sub> 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 NO<sub>2</sub> with counter-gradient fluxes of NO.
We find that NO<sub>x</sub> 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 NO<sub>x</sub> to
higher nitrogen oxides within the forest canopy, which might be part of a
mechanistic explanation for the "canopy reduction factor" applied to soil
NO<sub>x</sub> emissions in large-scale models. |
| first_indexed | 2024-12-10T07:08:20Z |
| format | Article |
| id | doaj.art-32ef02ab3a2845a6af7f30d6ce4c8649 |
| institution | Directory Open Access Journal |
| issn | 1680-7316 1680-7324 |
| language | English |
| last_indexed | 2024-12-10T07:08:20Z |
| publishDate | 2014-06-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Atmospheric Chemistry and Physics |
| spelling | doaj.art-32ef02ab3a2845a6af7f30d6ce4c86492022-12-22T01:58:08ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242014-06-0114115495551210.5194/acp-14-5495-2014Eddy covariance fluxes and vertical concentration gradient measurements of NO and NO<sub>2</sub> over a ponderosa pine ecosystem: observational evidence for within-canopy chemical removal of NO<sub>x</sub>K.-E. Min0S. E. Pusede1E. C. Browne2B. W. LaFranchi3R. C. Cohen4University of California at Berkeley, Department of Earth and Planetary Science, Berkeley, USAUniversity of California at Berkeley, Department of Chemistry, Berkeley, USAUniversity of California at Berkeley, Department of Chemistry, Berkeley, USAUniversity of California at Berkeley, Department of Chemistry, Berkeley, USAUniversity of California at Berkeley, Department of Earth and Planetary Science, Berkeley, USAExchange of NO<sub>x</sub> (NO+NO<sub>2</sub>) 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 NO<sub>x</sub>. As a result, a complete description of the processes affecting NO<sub>x</sub> 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 NO<sub>2</sub> 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 NO<sub>2</sub> with counter-gradient fluxes of NO. We find that NO<sub>x</sub> 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 NO<sub>x</sub> to higher nitrogen oxides within the forest canopy, which might be part of a mechanistic explanation for the "canopy reduction factor" applied to soil NO<sub>x</sub> emissions in large-scale models.http://www.atmos-chem-phys.net/14/5495/2014/acp-14-5495-2014.pdf |
| spellingShingle | K.-E. Min S. E. Pusede E. C. Browne B. W. LaFranchi R. C. Cohen Eddy covariance fluxes and vertical concentration gradient measurements of NO and NO<sub>2</sub> over a ponderosa pine ecosystem: observational evidence for within-canopy chemical removal of NO<sub>x</sub> Atmospheric Chemistry and Physics |
| title | Eddy covariance fluxes and vertical concentration gradient measurements of NO and NO<sub>2</sub> over a ponderosa pine ecosystem: observational evidence for within-canopy chemical removal of NO<sub>x</sub> |
| title_full | Eddy covariance fluxes and vertical concentration gradient measurements of NO and NO<sub>2</sub> over a ponderosa pine ecosystem: observational evidence for within-canopy chemical removal of NO<sub>x</sub> |
| title_fullStr | Eddy covariance fluxes and vertical concentration gradient measurements of NO and NO<sub>2</sub> over a ponderosa pine ecosystem: observational evidence for within-canopy chemical removal of NO<sub>x</sub> |
| title_full_unstemmed | Eddy covariance fluxes and vertical concentration gradient measurements of NO and NO<sub>2</sub> over a ponderosa pine ecosystem: observational evidence for within-canopy chemical removal of NO<sub>x</sub> |
| title_short | Eddy covariance fluxes and vertical concentration gradient measurements of NO and NO<sub>2</sub> over a ponderosa pine ecosystem: observational evidence for within-canopy chemical removal of NO<sub>x</sub> |
| title_sort | eddy covariance fluxes and vertical concentration gradient measurements of no and no sub 2 sub over a ponderosa pine ecosystem observational evidence for within canopy chemical removal of no sub x sub |
| url | http://www.atmos-chem-phys.net/14/5495/2014/acp-14-5495-2014.pdf |
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