The Stratospheric Chemistry and The Ozone Layer - PowerPoint PPT Presentation

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The Stratospheric Chemistry and The Ozone Layer

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O2 hn(l 243nm) O O oxygen photolysis. O O2 M O3 M ozone formation ... Concentration of O atoms fall off in lower stratosphere as photolysis of O2 and O3 ... – PowerPoint PPT presentation

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Title: The Stratospheric Chemistry and The Ozone Layer


1
The Stratospheric Chemistry and The Ozone Layer
  • Stratospheric circulation
  • Stratospheric photochemistry
  • Gas phase reactions
  • Ozone and Catalytic cycles

Dr Tony Cox ERCA 2004 -Lecture 2
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Temperature Structure of the Atmosphere
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Mesosphere
Stratopause
Height/km
Stratosphere
Tropopause
Troposphere
Latitude
5
Black region is troposphere
Eruption of Mt Pinatubo, Phillipine Is, 5ON, June
1991
Satellite measurements of aerosol as a tracer for
stratospheric circulation
6
Mesosphere
Stratosphere
Upper troposphere
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MEAN (11yr) ATMOSPHERIC WINDS AT 20 km ALTITUDE
(NOAA Analysis)
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MEAN (11yr) ATMOSPHERIC TEMPERATURE AT 20 km
ALTITUDE (NOAA Analysis)
10
Potential Vorticity At 20 km in the S.Polar
Vortex
11
30 km Altitude 16 km
1950
The QBO In equatorial regions
1978
12
Variations in mean O3 column(DU) due to QBO (from
satellite observations)
13
Climatology of Global O3 column (after Dutsch,
1971) In Dobson units, i.e. mmHgx100 at STP
14
Chemical Kinetics I
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Chemical Kinetics II
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Chemical Kinetics III
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O(3P)
O3
O2
O3
18
Window region where UV radiation penetrates into
the lower stratosphere giving O2 hn ? O O
19
Chemical lifetime of O3calculated daily averaged
photodissociation rate of molecular oxygen
20
Release of catalysts by Photolysis in the
lower Stratosphere
21
O2 hn(llt243nm) ? O O oxygen
photolysis O O2 M ? O3 M
ozone formation O O3 ? O2 O2
ozone destruction O3 hn(llt310nm) ? O(1D)
O2 O3 hn(llt1180nm) ? O O2 oxygen
photolysis
NO2 hn(llt243nm) ? NO O NO2 photolysis O
O2 M ? O3 M ozone formation
X O3 ? XO O2 XO O ? X O2 Net O O3
? O2 O2 ozone destruction X H, OH, NO,
Cl, Br, etc
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Interconversion of Cl ClO
Formation and release from reservoirs of Cl ClO
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STRATOSPERE
???? heterogeneous reactions on sulphate aerosol
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OZONE DEPLETION CYCLES IN THE LOWER STRATOSPHERE
Concentration of O atoms fall off in lower
stratosphere as photolysis of O2 and O3 reduces.
Catalytic destruction through cycles involving
participation of atomic O is less important.
Other cycles not involving O(3P) can occur.
34
OZONE DEPLETION CYCLES INVOLVING HALOGENS THE
LOWER STRATOSPHERE
Involving ClOx/NOx coupling ClO NO2
ClONO2 ClONO2 hn Cl NO3 NO3 hn
NO O2 NO O3 NO2 O2 Cl O3
ClO O2 net O3 O3 3O2 Involving
NOx/Halogen (X Br or I) coupling XO HO2
HOX O2 HOX hn X HO OH O3 HO2
O2 X O3 XO O2 net O3 O3 3O2
35
???? heterogeneous reactions on sulphate aerosol
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