Measurements of OH and RO2 radicals at Dome C, East Antarctica

Kukui, A.; Legrand, M.; Preunkert, S.; Frey, M. ORCID: https://orcid.org/0000-0003-0535-0416; Loisil, R.; Gil Roca, J.; Jourdain, B.; King, M.D.; France, J.L.; Ancellet, G.. 2014 Measurements of OH and RO2 radicals at Dome C, East Antarctica. Atmospheric Chemistry & Physics, 14. 12373-12392. 10.5194/acp-14-12373-2014

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Abstract/Summary

Concentrations of OH radicals and the sum of peroxy radicals, RO2, were measured in the boundary layer for the first time on the East Antarctic Plateau at the Concordia Station (Dome C, 75.10° S, 123.31° E) during the austral summer 2011/2012. The median concentrations of OH and RO2 radicals were 3.1 × 106 molecule cm−3 and 9.9 × 107 molecule cm−3, respectively. These values are comparable to those observed at the South Pole, confirming that the elevated oxidative capacity of the Antarctic atmospheric boundary layer found at the South Pole is not restricted to the South Pole but common over the high Antarctic plateau. At Concordia, the concentration of radicals showed distinct diurnal profiles with the median maximum of 5.2 × 106 molecule cm−3 at 11:00 and the median minimum of 1.1 × 106 molecule cm−3 at 01:00 for OH radicals and 1.7 × 108 molecule cm−3 and 2.5 × 107 molecule cm−3 for RO2 radicals at 13:00 and 23:00, respectively (all times are local times). Concurrent measurements of O3, HONO, NO, NO2, HCHO and H2O2 demonstrated that the major primary source of OH and RO2 radicals at Dome C was the photolysis of HONO, HCHO and H2O2, with the photolysis of HONO contributing ∼75% of total primary radical production. However, photochemical modelling with accounting for all these radical sources overestimates the concentrations of OH and RO2 radicals by a factor of 2 compared to field observations. Neglecting the OH production from HONO in the photochemical modelling results in an underestimation of the concentrations of OH and RO2 radicals by a factor of 2. To explain the observations of radicals in this case an additional source of OH equivalent to about 25% of measured photolysis of HONO is required. Even with a factor of 4 reduction in the concentrations of HONO, the photolysis of HONO represents the major primary radical source at Dome C. Another major factor leading to the large concentration of OH radicals measured at Dome C was large concentrations of NO molecules and fast recycling of peroxy radicals to OH radicals.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.5194/acp-14-12373-2014
Programmes:	BAS Programmes > Polar Science for Planet Earth (2009 - ) > Chemistry and Past Climate
Date made live:	17 Jun 2014 10:35 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/506988

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.5194/acp-14-12373-2014

Programmes:

BAS Programmes > Polar Science for Planet Earth (2009 - ) > Chemistry and Past Climate

Date made live:

17 Jun 2014 10:35 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/506988