Atmospheric Chemistry and Physics (Dec 2008)

Contribution of very short-lived organic substances to stratospheric chlorine and bromine in the tropics – a case study

  • J. C. Laube,
  • A. Engel,
  • H. Bönisch,
  • T. Möbius,
  • D. R. Worton,
  • W. T. Sturges,
  • K. Grunow,
  • U. Schmidt

Journal volume & issue
Vol. 8, no. 23
pp. 7325 – 7334

Abstract

Read online

The total stratospheric organic chlorine and bromine burden was derived from balloon-borne measurements in the tropics (Teresina, Brazil, 5&deg;04´ S, 42&deg;52´ W) in 2005. Whole air samples were collected cryogenically at altitudes between 15 and 34 km. For the first time, we report measurements of a set of 28 chlorinated and brominated substances in the tropical upper troposphere and stratosphere including ten substances with an atmospheric lifetime of less than half a year. The substances were quantified using pre-concentration techniques followed by Gas Chromatography with Mass Spectrometric detection. In the tropical tropopause layer at altitudes between 15 and 17 km we found 1.1–1.4% of the chlorine and 6–8% of the bromine to be present in the form of very short-lived organic compounds. By combining the data with tropospheric reference data and age of air observations the abundances of inorganic chlorine and bromine (Cl<sub>y</sub> and Br<sub>y</sub>) were derived. At an altitude of 34 km we calculated 3062 ppt of Cl<sub>y</sub> and 17.5 ppt of Br<sub>y</sub> from the decomposition of both long- and short-lived organic source gases. Furthermore we present indications for the presence of additional organic brominated substances in the tropical upper troposphere and stratosphere.