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CH3041
ANTARCTIC OZONE HOLE III
• A heterogeneously catalysed reaction
  occurs on the surface of PSC ice crystals.
     ClONO2(g)+ HCl(g)® Cl2(g)+ HNO3(aq)
  This happens all through winter.
• Polar spring, sunlight returns & with it O3 
  formation but:          1Cl2(g)+ hn ®2Cl.(g)
• The net result is rapid generation of Cl. 
   followed by massive loss of O3.
• This is a transient phenomenon by mid-
  spring  the ice crystals melt and release
   NOx. The catalytic reaction stops, the NOx 
   traps OCl. and normal O3 levels return.