• 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.