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Abstract. While the hydroxyl radical (•OH) in the snowpack is likely a dominant oxidant for organic species and bromide, little is known about the kinetics or steady-state concentrations of •OH on/in snow and ice. Here we measure the formation rate, lifetime, and concentration of •OH for illuminated polar snow samples studied in the laboratory and in the field. Laboratory studies show that •OH kinetics and steady-state concentrations are essentially the same for a given sample studied as ice and liquid; this is in contrast to other photooxidants, which show a concentration enhancement in ice relative to solution as a result of kinetic differences in the two phases. The average production rate of •OH in samples studied at Summit, Greenland, is 5 times lower than the average measured in the laboratory, while the average •OH lifetime determined in the field is 5 times higher than in the laboratory. These differences indicate that the polar snows we studied in the laboratory are affected by contamination, despite significant efforts to prevent this; our results suggest similar contamination may be a widespread problem in laboratory studies of ice chemistry. Steady-state concentrations of •OH in clean snow studied in the field at Summit, Greenland, range from (0.8 to 3) × 10−15 M, comparable to values reported for midlatitude cloud and fog drops, rain, and deliquesced marine particles, even though impurity concentrations in the snow samples are much lower. Partitioning of firn air •OH to the snow grains will approximately double the steady-state concentration of snow-grain hydroxyl radical, leading to an average [•OH] in near-surface, summer Summit snow of approximately 4 × 10−15 M. At this concentration, the •OH-mediated lifetimes of organics and bromide in Summit snow grains are approximately 3 days and 7 h, respectively, suggesting that hydroxyl radical is a major oxidant for both species.

<p><strong>Abstract.</strong> While hydroxyl radical (·OH) in the snowpack is likely a dominant oxidant for organic species and bromide, little is known about the kinetics or steady-state concentrations of ·OH on/in snow and ice. Here we measure the formation rate, lifetime, and concentration of ·OH for illuminated polar snow samples studied in the laboratory and in the field. Laboratory studies show that ·OH kinetics and steady-state concentrations are essentially the same for a given sample studied as ice and liquid, in contrast to other oxidants, which show a concentration enhancement in ice relative to solution. The average production rate of ·OH in samples studied at Summit, Greenland is 5 times lower than the average measured in the laboratory, while the average ·OH lifetime determined in the field is 5 times higher than in the laboratory. These differences indicate the polar snows studied in the laboratory are affected by contamination, despite efforts to prevent this. Steady-state concentrations of ·OH in snow studied in the field at Summit, Greenland range from (0.8 to 3) × 10<sup>−15</sup> M, comparable to values reported for mid-latitude cloud and fog drops, rain, and deliquesced marine particles, even though impurity concentrations in the snow samples are much lower. Partitioning of firn-air ·OH to the snow grains will approximately double the steady-state concentration of snow-grain hydroxyl radical, leading to an average [·OH] in near-surface, summer Summit snow of approximately 4 × 10<sup>−15</sup> M. At this concentration, the ·OH-mediated lifetimes of organics and bromide in Summit snow grains are approximately 3 days and 7 hours, respectively, suggesting that hydroxyl radical is a major oxidant for both species.</p>

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