Airborne lidar measurements of surface ozone depletion over Arctic sea ice

• Published in: Atmospheric Chemistry and Physics
• Main Authors: Seabrook, J. A., Whiteway, J. A., Gray, L. H., Staebler, R., Herber, A.
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2013
• Subjects: article; Verlagsveröffentlichung; Arctic; Barrow; Sea ice; Alaska
• Online Access: https://doi.org/10.5194/acp-13-6023-2013; https://noa.gwlb.de/receive/cop_mods_00045528; https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00045148/acp-13-6023-2013.pdf; https://acp.copernicus.org/articles/13/6023/2013/acp-13-6023-2013.pdf

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.