Summertime NO<sub>x</sub> measurements during the CHABLIS campaign: can source and sink estimates unravel observed diurnal cycles?
NO<sub>x</sub> measurements were conducted at the Halley Research Station, coastal Antarctica, during the austral summer period 1 January–10 February 2005. A clear NO<sub>x</sub> diurnal cycle was observed with minimum concentrations close to instrumental detection limit (5 p...
| Main Authors: | , , , , , , , , , , |
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2012-01-01
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| Series: | Atmospheric Chemistry and Physics |
| Online Access: | http://www.atmos-chem-phys.net/12/989/2012/acp-12-989-2012.pdf |
| _version_ | 1818302710492954624 |
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| author | H. K. Roscoe E. W. Wolff A. Saiz-Lopez J. D. Lee A. E. Jones P. S. Anderson R. A. Salmon M. J. Evans W. J. Bloss S. J.-B. Bauguitte J. M. C. Plane |
| author_facet | H. K. Roscoe E. W. Wolff A. Saiz-Lopez J. D. Lee A. E. Jones P. S. Anderson R. A. Salmon M. J. Evans W. J. Bloss S. J.-B. Bauguitte J. M. C. Plane |
| author_sort | H. K. Roscoe |
| collection | DOAJ |
| description | NO<sub>x</sub> measurements were conducted at the Halley Research Station, coastal Antarctica, during the austral summer period 1 January–10 February 2005. A clear NO<sub>x</sub> diurnal cycle was observed with minimum concentrations close to instrumental detection limit (5 pptv) measured between 04:00–05:00 GMT. NO<sub>x</sub> concentrations peaked (24 pptv) between 19:00–20:00 GMT, approximately 5 h after local solar noon. An optimised box model of NO<sub>x</sub> concentrations based on production from in-snow nitrate photolysis and chemical loss derives a mean noon emission rate of 3.48 × 10<sup>8</sup> molec cm<sup>−2</sup> s<sup>−1</sup>, assuming a 100 m boundary layer mixing height, and a relatively short NO<sub>x</sub> lifetime of ~6.4 h. This emission rate compares to directly measured values ranging from 2.1 to 12.6 × 10<sup>8</sup> molec cm<sup>−2</sup> s<sup>−1</sup> made on 3 days at the end of the study period. Calculations of the maximum rate of NO<sub>2</sub> loss via a variety of conventional HO<sub>x</sub> and halogen oxidation processes show that the lifetime of NO<sub>x</sub> is predominantly controlled by halogen processing, namely BrNO<sub>3</sub> and INO<sub>3</sub> gas-phase formation and their subsequent heterogeneous uptake. Furthermore the presence of halogen oxides is shown to significantly perturb NO<sub>x</sub> concentrations by decreasing the NO/NO<sub>2</sub> ratio. We conclude that in coastal Antarctica, the potential ozone production efficiency of NO<sub>x</sub> emitted from the snowpack is mitigated by the more rapid NO<sub>x</sub> loss due to halogen nitrate hydrolysis. |
| first_indexed | 2024-12-13T05:43:14Z |
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| id | doaj.art-9010588279cc44a6aae9d736a35ad09f |
| institution | Directory Open Access Journal |
| issn | 1680-7316 1680-7324 |
| language | English |
| last_indexed | 2024-12-13T05:43:14Z |
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| publisher | Copernicus Publications |
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| series | Atmospheric Chemistry and Physics |
| spelling | doaj.art-9010588279cc44a6aae9d736a35ad09f2022-12-21T23:57:44ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242012-01-01122989100210.5194/acp-12-989-2012Summertime NO<sub>x</sub> measurements during the CHABLIS campaign: can source and sink estimates unravel observed diurnal cycles?H. K. RoscoeE. W. WolffA. Saiz-LopezJ. D. LeeA. E. JonesP. S. AndersonR. A. SalmonM. J. EvansW. J. BlossS. J.-B. BauguitteJ. M. C. PlaneNO<sub>x</sub> measurements were conducted at the Halley Research Station, coastal Antarctica, during the austral summer period 1 January–10 February 2005. A clear NO<sub>x</sub> diurnal cycle was observed with minimum concentrations close to instrumental detection limit (5 pptv) measured between 04:00–05:00 GMT. NO<sub>x</sub> concentrations peaked (24 pptv) between 19:00–20:00 GMT, approximately 5 h after local solar noon. An optimised box model of NO<sub>x</sub> concentrations based on production from in-snow nitrate photolysis and chemical loss derives a mean noon emission rate of 3.48 × 10<sup>8</sup> molec cm<sup>−2</sup> s<sup>−1</sup>, assuming a 100 m boundary layer mixing height, and a relatively short NO<sub>x</sub> lifetime of ~6.4 h. This emission rate compares to directly measured values ranging from 2.1 to 12.6 × 10<sup>8</sup> molec cm<sup>−2</sup> s<sup>−1</sup> made on 3 days at the end of the study period. Calculations of the maximum rate of NO<sub>2</sub> loss via a variety of conventional HO<sub>x</sub> and halogen oxidation processes show that the lifetime of NO<sub>x</sub> is predominantly controlled by halogen processing, namely BrNO<sub>3</sub> and INO<sub>3</sub> gas-phase formation and their subsequent heterogeneous uptake. Furthermore the presence of halogen oxides is shown to significantly perturb NO<sub>x</sub> concentrations by decreasing the NO/NO<sub>2</sub> ratio. We conclude that in coastal Antarctica, the potential ozone production efficiency of NO<sub>x</sub> emitted from the snowpack is mitigated by the more rapid NO<sub>x</sub> loss due to halogen nitrate hydrolysis.http://www.atmos-chem-phys.net/12/989/2012/acp-12-989-2012.pdf |
| spellingShingle | H. K. Roscoe E. W. Wolff A. Saiz-Lopez J. D. Lee A. E. Jones P. S. Anderson R. A. Salmon M. J. Evans W. J. Bloss S. J.-B. Bauguitte J. M. C. Plane Summertime NO<sub>x</sub> measurements during the CHABLIS campaign: can source and sink estimates unravel observed diurnal cycles? Atmospheric Chemistry and Physics |
| title | Summertime NO<sub>x</sub> measurements during the CHABLIS campaign: can source and sink estimates unravel observed diurnal cycles? |
| title_full | Summertime NO<sub>x</sub> measurements during the CHABLIS campaign: can source and sink estimates unravel observed diurnal cycles? |
| title_fullStr | Summertime NO<sub>x</sub> measurements during the CHABLIS campaign: can source and sink estimates unravel observed diurnal cycles? |
| title_full_unstemmed | Summertime NO<sub>x</sub> measurements during the CHABLIS campaign: can source and sink estimates unravel observed diurnal cycles? |
| title_short | Summertime NO<sub>x</sub> measurements during the CHABLIS campaign: can source and sink estimates unravel observed diurnal cycles? |
| title_sort | summertime no sub x sub measurements during the chablis campaign can source and sink estimates unravel observed diurnal cycles |
| url | http://www.atmos-chem-phys.net/12/989/2012/acp-12-989-2012.pdf |
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