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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 13, issue 12
Atmos. Chem. Phys., 13, 6023–6029, 2013
https://doi.org/10.5194/acp-13-6023-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
Atmos. Chem. Phys., 13, 6023–6029, 2013
https://doi.org/10.5194/acp-13-6023-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 22 Jun 2013

Research article | 22 Jun 2013

Airborne lidar measurements of surface ozone depletion over Arctic sea ice

J. A. Seabrook1, J. A. Whiteway1, L. H. Gray1, R. Staebler2, and A. Herber3 J. A. Seabrook et al.
  • 1Centre for Research in Earth and Space Science (CRESS), York University, 4700 Keele Street, Toronto, Ontario, M3J 1P3, Canada
  • 2Environment Canada, 4905 Dufferin Street, Toronto, Ontario, M3H 5T4, Canada
  • 3Alfred Wegener Institute, Bussestrasse 24, 27570 Bremerhaven, Germany

Abstract. A differential absorption lidar (DIAL) for measurement of atmospheric ozone concentration was operated aboard the Polar 5 research aircraft in order to study the depletion of ozone over Arctic sea ice. The lidar measurements during a flight over the sea ice north of Barrow, Alaska, on 3 April 2011 found a surface boundary layer depletion of ozone over a range of 300 km. The photochemical destruction of surface level ozone was strongest at the most northern point of the flight, and steadily decreased towards land. All the observed ozone-depleted air throughout the flight occurred within 300 m of the sea ice surface. A back-trajectory analysis of the air measured throughout the flight indicated that the ozone-depleted air originated from over the ice. Air at the surface that was not depleted in ozone had originated from over land. An investigation into the altitude history of the ozone-depleted air suggests a strong inverse correlation between measured ozone concentration and the amount of time the air directly interacted with the sea ice.

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