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Facts about Ozone
absorbs most UV (all UV-C)
allow life to proliferate
can be degraded by CFCs
3 O2 → 6 O → 2 O3 (ozone)
sunlight catalyzes this reaction
O3 ←→ O2
happens naturally and in equilibrium w/o pollution + human interference
UV Absorption by Ozone
UV-A → all passes
UV-B → some passes
sunblock
cause sunburn, cancer, reduce PS/crop production/productivity
UV-C → none passes
lethal
disinfection purposes
Measuring Ozone
Dobson Units (DU)
the depth ozone molecules would occupy at STP
1 DU → 0.01 mm of ozone
normal = 300-500 DU (3-5 mm thick)
ozone thinning = O3 breaks apart → molecules scattered
SUN INCREASES PRODUCTION OF OZONE
more made at tropics
Ozone Depleting Substances (ODS)
ODS = Cl, Br, F
CFCs + HCFCs = (hydro)chlorofluorocarbons used to replace CFCs
used as refrigerants
discovered in 1930s
many types
stable, long life
dissipate into air, not soluble (gases, can’t be removed)
MEDCs phased out first → LEDCs
CFCs migrate up to the stratosphere
UV breaks the Cl off the CFC ‘cule
Cl reacts with O3, breaking it apart
1 Cl can destroy ~300,000 O3
Cl can form HCl (hydrochloric acid) → drop to troposphere → precipitates down
Other ODS’s
Methyl Bromide
soil fumigator to rid pests + soil pathogens
naturally formed in the ocean + burning biomass
2 yr lifespan
Br IS 50X STRONGER THAN Cl IN DESTROYING O3
Halons
fire suppressant
Hydrobromofluorocarbons
solvents, cleaning agents, fire suppressants
Carbon tetrachloride
solvent, dry cleaning agent, refrigerant, propellant
Methyl chloroform
industrial solvent, degreasing agent, correction fluid
Volcanic emissions (natty occuring)
Changes in Stratospheric Ozone Layers
Ozone varies over time + szn
measurement didn’t begin until the 70s
1980s → 5-15% reduction measured (NOT seasonal variation)
Ozone Hole
Seasonal Loss at Poles
@ antarctic + arctic
ozone = lowest spring to summer at the poles
no new O3 being made in winter, takes months for sunlight to help re-establish the layer
Polar Stratospheric Clouds
winter → CFCs build up in clouds
Cl isn’t breaking off yet (sun catalyzes Cl break off)
when sun returns in spring, the reaction breaking off Cl happens → ozone decreases
sun breaks the polar vortex which allows air movement + O3 can move in (helps reestablish layer)
ozone depleted air pushes toward the tropics
ozone made in summer and fall in polar regions (strongest sunlight)
International Agreements to Manage the Ozone Layer
UN legislation
Vienna Convention
protects ozone
support research + exchange info
Montreal Protocol (MOST SUCCESSFUL INTL AGREEMENT TO PROTECT ENVIRONMENT)
Targets to reduce emissions of ODS’s
targets on ODS are legally binding
assistance to LEDCs
More Agreements
Montreal Protocol
timetable reduce CFCs by 50%, freeze halon production
ALLOW each country to set own law + compliance
London Amendment
target to phase out main ODS
deadline 2000, LEDCS = 2010
Copenhagen
moved deadline up
Beijing
more stringent (strict) controls on HCFCs
added more ODSs to be phased out by 2004
Montreal Protocol
amendments hv been made due to new knowledge of ozone + ODSs
ratified by all 197 nations in 2015
is MOST SUCCESSFUL INTL AGREEMENT that has used SCIENCE to direct CHANGE + POLICIES
an exemplar of intl cooperation
Challenges
CFC lifespan (+ other ODSs)
long lived, even when eliminated, they’re still up in the atm
ODSs in discarded equipment
they can release into the atm
lack of alternatives to replace the ODSs that aren’t ODSs (some do hv shorter lifespan tho)
many alternatives are also GHGs
HCFCs are to be phased out by 2030
Illegal trade of ODSs
Lack of policing + enforcement
Progress on Ozone Protection
Production of the main ODSs is banned (except for some med + research applications)
Overall emission reduced
Atm lvls of ODSs are leveling/declining (will take a bit of time due to lifespan)
Long life of CFCs will make ozone recovery a long road