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Decrease of stratospheric NO[sub 2] at 44[degrees]N caused by Pinatubo volcanic aerosols

Journal Article · · Geophysical Research Letters (American Geophysical Union); (United States)
DOI:https://doi.org/10.1029/93GL01800· OSTI ID:5733124
;  [1]; ;  [2];  [3]
  1. Nagoya Univ., Aichi (Japan)
  2. National Inst. of Water and Atmospheric Research, Central Otago (New Zealand)
  3. Meteorological Research Inst., Ibaraki (Japan)

This paper presents measurements of stratospheric NO[sub 2] made over northern Japan since April 1991. Other work has shown that in the southern hemisphere, following the arival of the SO[sub 2] cloud from the eruption of Mt Pinatubo, there has been a marked decrease in the stratospheric NO[sub 2]levels. Laboratory studies have suggested that heterogeneous reactions on the surfaces of sulfuric acid aerosols can convert NO[sub x] to HNO[sub 3]. This data also shows marked decreases in stratospheric NO[sub 2]. Lidar measurements, and satellite observations show that volcanic aerosols were moving into the stratosphere at 25 km altitudes just prior to the onset of these observed decreases.

OSTI ID:
5733124
Journal Information:
Geophysical Research Letters (American Geophysical Union); (United States), Journal Name: Geophysical Research Letters (American Geophysical Union); (United States) Vol. 20:18; ISSN GPRLAJ; ISSN 0094-8276
Country of Publication:
United States
Language:
English