Title: The Stratospheric Chemistry and The Ozone Layer
1The 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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3Temperature Structure of the Atmosphere
4Mesosphere
Stratopause
Height/km
Stratosphere
Tropopause
Troposphere
Latitude
5Black region is troposphere
Eruption of Mt Pinatubo, Phillipine Is, 5ON, June
1991
Satellite measurements of aerosol as a tracer for
stratospheric circulation
6Mesosphere
Stratosphere
Upper troposphere
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8MEAN (11yr) ATMOSPHERIC WINDS AT 20 km ALTITUDE
(NOAA Analysis)
9MEAN (11yr) ATMOSPHERIC TEMPERATURE AT 20 km
ALTITUDE (NOAA Analysis)
10Potential Vorticity At 20 km in the S.Polar
Vortex
1130 km Altitude 16 km
1950
The QBO In equatorial regions
1978
12Variations in mean O3 column(DU) due to QBO (from
satellite observations)
13Climatology of Global O3 column (after Dutsch,
1971) In Dobson units, i.e. mmHgx100 at STP
14Chemical Kinetics I
15Chemical Kinetics II
16Chemical Kinetics III
17O(3P)
O3
O2
O3
18Window region where UV radiation penetrates into
the lower stratosphere giving O2 hn ? O O
19Chemical lifetime of O3calculated daily averaged
photodissociation rate of molecular oxygen
20Release of catalysts by Photolysis in the
lower Stratosphere
21O2 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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27Interconversion of Cl ClO
Formation and release from reservoirs of Cl ClO
28STRATOSPERE
???? heterogeneous reactions on sulphate aerosol
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33OZONE 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.
34OZONE 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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