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The polar stratospheric cloud event of January 24: Part 2. Photochemistry

Journal Article · · Geophysical Research Letters (American Geophysical Union); (United States)
;  [1]; ;  [2];  [3];  [4]; ;  [5]
  1. United Kingdom Meteorological Office, Bracknell (England)
  2. NOAA Environmental Research Laboratory, Boulder, CO (USA)
  3. NASA Langley Research Center, Hampton, VA (USA)
  4. Pennsylvania State Univ., Pittsburgh (USA)
  5. Harvard Univ., Cambridge, MA (USA)

During the 1988/89 Airborne Arctic Stratospheric Expedition (AASE), observations of the chemical composition, aerosol characteristics and atmospheric state were obtained from two aircraft, a NASA ER-2 and DC-8. In this paper the authors present a diagnosis of observations obtained using the ER-2 on January 24, 1989, using a Lagrangian coupled microphysical-photochemical model. They interpret the high chlorine monoxide mixing ratios observed from the ER-2 on the afternoon of January 24, 1989 as a result of in situ heterogeneous release of reactive chlorine from the reservoirs HCl and ClONO{sub 2} on Type 1 polar stratospheric cloud particles observed to be present at that time. This essential element in theories of polar ozone depletion has never before been observed directly in the stratosphere.

OSTI ID:
5332052
Journal Information:
Geophysical Research Letters (American Geophysical Union); (United States), Journal Name: Geophysical Research Letters (American Geophysical Union); (United States) Vol. 17:4; ISSN 0094-8276; ISSN GPRLA
Country of Publication:
United States
Language:
English