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Ozone Type: Tropospheric
Lower atmosphere (0-10 miles)
Ozone Type: Stratospheric
10-30 miles above Earth
Tropospheric Ozone Location
Lower atmosphere (0-10 miles)
Stratospheric Ozone Location
10-30 miles above Earth
Tropospheric Ozone Formation
Secondary pollutant from Nitrogen oxides and VOCs (Volatile Organic Compounds) plus sunlight
Stratospheric Ozone Formation
Natural reaction where Oxygen gas and UV light form Ozone
Tropospheric Ozone Effect
Harmful to humans, causes smog
Stratospheric Ozone Effect
Protective barrier against UV radiation
"Good Ozone"
Stratospheric ozone
"Bad Ozone"
Tropospheric ozone
Stratospheric Ozone Nature
Natural and beneficial, shields life from harmful UV rays
Tropospheric Ozone Nature
Anthropogenic (human-made) and harmful
Stratospheric Ozone's Role
Absorbs 97-99% of UV-B and UV-C radiation
Importance of UV Absorption
Protects DNA from mutation and skin cancer
Importance of UV Absorption
Prevents cataracts and immune suppression in humans
CFCs (Chlorofluorocarbons)
Synthetic compounds used in refrigerants, aerosols, and foam
CFC Destruction Process Step 1
CFCs drift upward into the stratosphere (long-lived gases)
CFC Destruction Process Step 2
UV light breaks CFC molecules and releases chlorine atoms
CFC Destruction Process Step 3
A single chlorine atom reacts with and destroys ozone in a catalytic cycle, then is freed to destroy more
CFC Result
Significant ozone thinning over the poles, especially the Antarctic ozone hole
Montreal Protocol Year
Signed in 1987
Montreal Protocol Key Provision
Phase-out schedule for CFCs, halons, and other Ozone-Depleting Substances (ODS)
Montreal Protocol Key Provision
Created a Multilateral Fund to help developing countries transition
Montreal Protocol Key Provision
Implemented trade restrictions preventing non-signatories from selling ODS
Montreal Protocol Success Rate
97% of ozone-depleting substances phased out globally
Ozone Layer Recovery Projection
Projected to recover to pre-1980 levels by 2050-2075
Benefit of Montreal Protocol
Prevented millions of cases of skin cancer, cataracts, and crop loss
Challenge to Protocol Success
Illegal emissions from some factories (e.g., CFC-11 in China)
Challenge to Protocol Success
Slow natural breakdown of CFCs means full recovery will take decades