Halogen Oxides in the Troposphere (ClO/BrO)


 

Instrument:Halogen Oxides in the Troposphere (ClO/BrO) 
Principal Investigators:Darin TooheyWilliam Brune
Organization:Program in Atmospheric Sciences Campus Box 311
University of Colorado
Boulder, CO 80309-0311
Department of Meteorology
504 Walker Building
The Pennsylvania State University
University Park, PA 16802

Measurement Description: Halogen oxides (ClO and BrO in this configuration) are rapidly converted to halogen atoms by addition of nitric oxide. The atoms are then detected sensitively and selectively by resonance fluorescence in the vacuum ultraviolet (Cl at 118.9 nm and Br at 131.7 nm). For measurements of BrO in the troposphere the pressure of the air sample must be reduced to less than 100 hPa, else oxygen in the flow absorbs all the radiation at 131.7 nm. On the DC-8 this pressure reduction will be accomplished by incorporating our detection system into the ATHOS (Brune and colleagues, Penn State) sampling system, which uses Laser-Induced Fluorescence at low pressure to detect OH and HO2.

Accuracy:ClO 25% (2 sigma)
 BrO 35% (2 sigma)
Precision:ClO < 5%
 BrO < 20% (at 5 ppt)
Response time: ClO 30 s
BrO 2 min

 

References:
McKinney, K. A., J. M. Pierson, and D.W. Toohey,A wintertime in situ profile of BrO between 17 and 27 km in the Arctic vortex, Geophys. Res. Lett., 24, 853-856, 1997.
Pierson, J. M., K. A. McKinney, D. W. Toohey, J. J. Margitan, U. Schmidt, A. Engel, and P. A. Newman,An investigation of ClO photochemistry in the chemically perturbed arctic vortex, J. Atmos. Chem., 32, 61-81, 1999.
More information can be found at http://paos.colorado.edu/~toohey/strato2c.html