Observations of hydroxyl and peroxy radicals and the impact of Br0 at Summit, Greenland in 2007 and 2008
Liao, J.; Huey, L.G.; Tanner, D.J.; Brough, Neil; Brooks, S.; Dibb, J.E.; Stutz, J.; Thomas, J.L.; Lefer, B.; Haman, C.; Gorham, K.. 2011 Observations of hydroxyl and peroxy radicals and the impact of Br0 at Summit, Greenland in 2007 and 2008. Atmospheric Chemistry and Physics, 11 (16). 8577-8591. 10.5194/acp-11-8577-2011Before downloading, please read NORA policies.
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The Greenland Summit Halogen-HO(x) (GSHOX) Campaign was performed in spring 2007 and summer 2008 to investigate the impact of halogens on HO(x) (= OH+HO(2)) cycling above the Greenland Ice Sheet. Chemical species including hydroxyl and peroxy radicals (OH and HO(2) + RO(2)), ozone (O(3)), nitrogen oxide (NO), nitric acid (HNO(3)), nitrous acid (HONO), reactive gaseous mercury (RGM), and bromine oxide (BrO) were measured during the campaign. The median midday values of HO(2) + RO(2) and OH concentrations observed by chemical ionization mass spectrometry (CIMS) were 2.7x10(8) molec cm(-3) and 3.0x10(6) molec cm(-3) in spring 2007, and 4.2x10(8) molec cm(-3) and 4.1x10(6) molec cm(-3) in summer 2008. A basic photochemical 0-D box model highly constrained by observations of H(2)O, O(3), CO, CH(4), NO, and J values predicted HO(2) + RO(2) (R = 0.90, slope = 0.87 in 2007; R = 0.79, slope = 0.96 in 2008) reasonably well and under predicted OH (R = 0.83, slope = 0.72 in 2007; R = 0.76, slope = 0.54 in 2008). Constraining the model to HONO observations did not significantly improve the ratio of OH to HO(2) + RO(2) and the correlation between predictions and observations. Including bromine chemistry in the model constrained by observations of BrO improved the correlation between observed and predicted HO(2) + RO(2) and OH, and brought the average hourly OH and HO(2) + RO(2) predictions closer to the observations. These model comparisons confirmed our understanding of the dominant HO(x) sources and sinks in this environment and indicated that BrO impacted the OH levels at Summit. Although, significant discrepancies between observed and predicted OH could not be explained by the measured BrO. Finally, observations of enhanced RGM were found to be coincident with under prediction of OH.
|Item Type:||Publication - Article|
|Digital Object Identifier (DOI):||10.5194/acp-11-8577-2011|
|Programmes:||BAS Programmes > Polar Science for Planet Earth (2009 - ) > Chemistry and Past Climate|
|Additional Information. Not used in RCUK Gateway to Research.:||Open access article made available under a CC-BY Creative Commons Attribution license.|
|NORA Subject Terms:||Atmospheric Sciences|
|Date made live:||10 Oct 2011 16:47|
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