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Title: Chlorine chemistry on polar stratospheric cloud particles in the Arctic winter

Journal Article · · Science (Washington, D.C.); (United States)
;  [1];  [2]; ;  [3]; ; ;  [4];  [5];  [6]
  1. California Institute of Technology, Pasadena, CA (United States)
  2. Univ. of California, Irvine, CA (United States)
  3. Harvard Univ., Cambridge, MA (United States)
  4. National Aeronautics and Space Administration, Greenbelt, MD (United States)
  5. National Oceanographic and Atmospheric Agency, Boulder, CO (United States)
  6. NASA Ames Research Center, Moffett Field, CA (United States)

Simultaneous in situ measurements of hydrochloric acid (HCl) and chlorine monoxide (ClO) in the Arctic winter vortex showed large HCl losses, of up to 1 part per billion by volume (ppbv), which were correlated with high ClO levels of up to 1.4 ppbv. Air parcel trajectory analysis identified that this conversion of inorganic chlorine occurred at air temperatures of less than 196 [plus minus]4 kelvin. High ClO was always accompanied by loss of HCl mixing ratios equal to 1/2(ClO + 2Cl[sub 2]O[sub 2]). These data indicate that the heterogeneous reaction HCl + ClONO[sub 2] [yields] Cl[sub 2] + HNO[sub 3] on particles of polar stratospheric clouds establishes the chlorine partitioning, which, contrary to earlier notions, begins with an excess of ClONO[sub 2], not HCl.

OSTI ID:
5648933
Journal Information:
Science (Washington, D.C.); (United States), Vol. 261:5125; ISSN 0036-8075
Country of Publication:
United States
Language:
English