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PS10.1: Average O3 Concentration

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... solar radiation and the concentration of O2, both of ... The natural destruction of ozone, on the other hand, is dependent on the concentration of ozone. ... – PowerPoint PPT presentation

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Title: PS10.1: Average O3 Concentration


1
PS10.1 Average O3 Concentration

2
PS10.2 O3 Residence Time
  • The short residence time of O3 helps explain why
    O3 holes can develop and disappear so rapidly.
    Systems with short residence times respond very
    quickly to perturbationsin this case, O3 drops
    rapidly during the start of the Antarctic spring
    as free Cl destroys O3, and rises rapidly as
    these reactions drop off and O3 production picks
    up. If we could get rid of the Cl, the O3 layer
    would be fine. Unfortunately, Cl has a long
    residence time in the stratosphere, so even if we
    stop CFC emissions entirely, the destruction of
    ozone will continue for decades until the Cl is
    removed.

3
PS10.3 O3 Destruction by CFC-11
  • If production continues at a constant rate, then
    eventually production flow into stratosphere
    breakdown into free chlorine, and the
    steady-state rate of O3 destruction is

4
PS10.3 O3 Destruction by CFC-11
  • (0.86)(440,000) (0.9)(140,000)
  • (5.1)(2,600) (12.5)(2,600) (0.05)(81,200)
    (0.12)(500,000) (1.2)(70,000)
  • 700,000 t/yr CFC11 equivalent
  • So the total production of these compounds has
    the ozone-destroying potential equal to
    production of 300,000 700,000 1 MtCFC11.
  • Redoing the above calculation, this would lead
    to the destruction of about 4?1038
    molecules(O3)/y.

5
PS10.3 Reduction in O3 Stock
  • Before CFCs, the natural destruction of ozone
    equaled the rate of production, 2?1039 O3/y.
  • After CFCs, production remains unchanged. (As
    noted in class, that depends only on the flux of
    solar radiation and the concentration of O2, both
    of which are fairly constant.
  • The natural destruction of ozone, on the other
    hand, is dependent on the concentration of ozone.
    In other words, the residence time of O3 with
    respect to natural destruction remains constant.

6
PS10.3 Reduction in O3 Stock
  • P natural rate of O3 production (constant)
  • So natural O3 stock S S after CFCs
  • ? residence time for natural O3 destruction
  • D rate of O3 destruction due to CFCs
  • Before
  • After

20 reduction
7
PS10.3D Reduction in O3 Stock
  • Before
  • After

17 reduction
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