π‘οΈ Chapter 06 Β· Topic 03 Β· Climate Change
Ozone Layer Depletion
Stratospheric ozone, ozone-depleting substances (CFCs, HCFCs, halons), ozone hole over Antarctica, Vienna Convention, Montreal Protocol, Kigali Amendment, and ozone recovery β complete UPSC & PSC notes.
π‘οΈ Stratospheric Ozone β The Protective Shield
The ozone layer is a region of Earth’s stratosphere containing high concentrations of ozone (Oβ). It is our planet’s natural sunscreen, absorbing most of the Sun’s harmful ultraviolet radiation.
- Located in the stratosphere, approximately 15β35 km above Earth’s surface (peak concentration at ~25 km)
- Absorbs UV-B (280β315 nm) and UV-C (100β280 nm) radiation β both harmful to life
- UV-A (315β400 nm) is not absorbed by ozone β reaches Earth’s surface
- Ozone concentration is measured in Dobson Units (DU) β 1 DU = 0.01 mm thickness of pure ozone at standard conditions
- Normal ozone column: 300 DU; ozone hole defined as <220 DU
- Despite being called a “layer,” ozone is spread thinly β if compressed to sea-level pressure, it would be only ~3 mm thick
π Tropospheric vs Stratospheric Ozone: Stratospheric ozone (15β35 km) = beneficial β protects from UV radiation. Tropospheric (ground-level) ozone = harmful β a secondary air pollutant formed from NOβ + VOCs + sunlight; causes respiratory problems and crop damage. “Good ozone up high, bad ozone nearby” β a common exam distinction.
βοΈ Ozone Formation and Destruction β Chapman Cycle
The Chapman cycle (1930) describes the natural formation and destruction of stratospheric ozone:
- Formation: Oβ + UV radiation β 2O (atomic oxygen); O + Oβ β Oβ (ozone)
- Natural destruction: Oβ + UV β Oβ + O; O + Oβ β 2Oβ
- In the natural cycle, ozone formation and destruction are in balance
- Human-made chemicals (CFCs etc.) disrupt this balance by accelerating ozone destruction
β Key Point: The Chapman cycle shows that ozone is constantly being formed and destroyed naturally. The problem is that ozone-depleting substances (ODS) dramatically accelerate the destruction side, breaking the natural equilibrium. One chlorine atom from a CFC molecule can destroy 100,000 ozone molecules through a catalytic chain reaction.
β οΈ Ozone-Depleting Substances (ODS)
| Substance | Full Name | Main Uses | ODP | Status |
|---|---|---|---|---|
| CFCs | Chlorofluorocarbons (e.g., CFC-11, CFC-12) | Refrigerants, aerosol propellants, foam blowing agents | 0.6β1.0 | Phased out under Montreal Protocol |
| HCFCs | Hydrochlorofluorocarbons (e.g., HCFC-22) | Refrigerants (transitional replacement for CFCs) | 0.02β0.11 | Being phased out (transitional) |
| Halons | Bromofluorocarbons (e.g., Halon-1301) | Fire extinguishers | 3β10 | Phased out; highest ODP per molecule |
| Methyl Bromide | CHβBr | Agricultural fumigant (soil sterilisation) | 0.6 | Phased out in developed countries |
| Carbon Tetrachloride | CClβ | Solvent, fire extinguishers (historical) | 1.1 | Phased out |
| Methyl Chloroform | CHβCClβ | Industrial solvent | 0.12 | Phased out |
π ODP (Ozone Depletion Potential): A measure of how much a substance depletes the ozone layer relative to CFC-11 (ODP = 1). Halons have the highest ODP per molecule (3β10). CFCs are the most important ODS due to their large quantities released. HFCs (used as CFC replacements) have zero ODP but high GWP β addressed by the Kigali Amendment.
π¬ Mechanism of Ozone Depletion by CFCs
- CFCs are released at ground level (from refrigerators, aerosols, etc.) β they are very stable and do not react in the troposphere
- CFCs slowly drift up to the stratosphere over 6β10 years
- In the stratosphere, intense UV radiation breaks the CFC molecule: CFC β Cl (chlorine radical) + other fragments
- The chlorine radical attacks ozone: Cl + Oβ β ClO + Oβ
- ClO reacts with atomic oxygen: ClO + O β Cl + Oβ
- The chlorine radical is regenerated β it is a catalyst (not consumed in the reaction)
- One Cl atom can destroy 100,000 ozone molecules before being deactivated
- Bromine (from halons) is even more effective at destroying ozone than chlorine
β Nobel Prize: Mario Molina, F. Sherwood Rowland, and Paul Crutzen won the Nobel Prize in Chemistry (1995) for their work on the formation and decomposition of stratospheric ozone, including the discovery of the CFC-ozone depletion mechanism. Molina and Rowland first proposed the CFC-ozone link in 1974.
π³οΈ Ozone Hole over Antarctica
- The Antarctic ozone hole was discovered in 1985 by British scientists (Farman, Gardiner, Shanklin) from the British Antarctic Survey
- It forms every year during the Antarctic spring (SeptemberβNovember)
- Why Antarctica? Two special conditions:
- Polar Vortex β a strong circular wind pattern that isolates Antarctic air during winter, preventing mixing with ozone-rich air from lower latitudes
- Polar Stratospheric Clouds (PSCs) β form at very low temperatures (<β78Β°C) during Antarctic winter; provide surfaces for chemical reactions that activate chlorine from CFCs
- In spring, sunlight returns β UV activates the chlorine β rapid ozone destruction β ozone hole forms
- The hole has reached up to 29 million kmΒ² in size (larger than North America)
- Ozone levels inside the hole can drop to <100 DU (normal ~300 DU)
π Arctic Ozone Hole: The Arctic also experiences ozone depletion, but less severe than Antarctica because the Arctic polar vortex is weaker and less stable. However, record Arctic ozone depletion occurred in 2020 β a 40% reduction over the Arctic. Climate change may actually worsen Arctic ozone depletion by cooling the stratosphere (even as the troposphere warms).
βοΈ Effects of Ozone Depletion
| Effect | Details |
|---|---|
| Skin cancer | UV-B causes DNA damage in skin cells β melanoma (most deadly) and non-melanoma skin cancers. 1% decrease in ozone β 2% increase in UV-B β 3% increase in skin cancer |
| Cataracts | UV-B damages the lens of the eye β cataracts (clouding of lens) β blindness. Leading cause of blindness globally |
| Immune suppression | UV-B suppresses the human immune system β increased susceptibility to infections and reduced vaccine effectiveness |
| Crop damage | UV-B damages plant DNA, reduces photosynthesis, stunts growth; affects soybean, wheat, rice yields |
| Marine ecosystem damage | UV-B penetrates ocean surface β damages phytoplankton (base of marine food chain) β disrupts entire marine ecosystem |
| Material degradation | UV-B degrades plastics, paints, rubber, and building materials faster |
π International Treaties β Vienna Convention & Montreal Protocol
Vienna Convention (1985)
- First international agreement to address ozone depletion
- A framework convention β set the stage for action but did not mandate specific reductions
- Established the principle of international cooperation on ozone protection
- Entered into force: 1988; 197 parties (universal ratification)
Montreal Protocol (1987)
- The most successful environmental treaty in history β often cited as the gold standard for international environmental cooperation
- Mandated the phase-out of ozone-depleting substances (CFCs, halons, HCFCs, etc.)
- 197 parties β the only UN treaty to achieve universal ratification
- Differentiated timelines: developed countries phased out CFCs by 1996; developing countries by 2010
- Has prevented an estimated 2 million cases of skin cancer per year and protected 1.5 million lives annually
- Also has significant climate co-benefits β ODS are also potent GHGs; Montreal Protocol has done more to slow climate change than the Kyoto Protocol
- Secretariat: UNEP, Nairobi
β Key Amendments to Montreal Protocol:
- London Amendment (1990) β added more substances; accelerated phase-out
- Copenhagen Amendment (1992) β accelerated CFC phase-out; added HCFCs and HBFCs
- Beijing Amendment (1999) β added bromochloromethane
- Kigali Amendment (2016) β phase-down of HFCs (see below)
Kigali Amendment (2016)
- Adopted in Kigali, Rwanda in October 2016; entered into force January 2019
- Targets HFCs (Hydrofluorocarbons) β used as replacements for CFCs; have zero ODP but very high GWP (hundreds to thousands)
- HFCs are powerful greenhouse gases β their phase-down could prevent 0.5Β°C of warming by 2100
- Developed countries: reduce HFCs by 85% by 2036 (baseline 2011β2013)
- Developing countries (Group 1, including China): reduce by 80% by 2045
- Developing countries (Group 2, including India, Pakistan, Gulf states): reduce by 85% by 2047
- India ratified the Kigali Amendment in 2021
π± Ozone Layer Recovery
- Thanks to the Montreal Protocol, atmospheric concentrations of most ODS are declining
- The ozone layer is slowly recovering β but it takes decades because ODS persist in the atmosphere for many years
- UNEP/WMO Scientific Assessment (2022): ozone layer expected to recover to 1980 levels by:
- Mid-latitudes: ~2040
- Arctic: ~2045
- Antarctica: ~2066
- The Antarctic ozone hole is showing signs of recovery β but year-to-year variability is large
- Concern: illegal CFC-11 emissions detected (2018β2019) β traced to eastern China; subsequently reduced
π India’s Commitments: India is a party to the Montreal Protocol and its amendments. India has successfully phased out CFCs and halons. India is phasing out HCFCs (HCFC-22 used in air conditioners). Under the Kigali Amendment, India will phase down HFCs by 85% by 2047. India’s HCFC Phase-out Management Plan (HPMP) is supported by the Multilateral Fund of the Montreal Protocol.
β Revision Checklist β Ozone Layer Depletion
β
Ozone layer = stratosphere = 15β35 km altitude = absorbs UV-B and UV-C
β Dobson Units (DU) = measure of ozone column; normal ~300 DU; ozone hole <220 DU
β Chapman cycle = natural ozone formation and destruction = in balance without ODS
β CFCs = most important ODS = stable in troposphere = drift to stratosphere over 6β10 years
β 1 Cl atom from CFC = destroys 100,000 ozone molecules (catalytic)
β Halons = highest ODP per molecule (3β10) = used in fire extinguishers
β ODP = Ozone Depletion Potential = relative to CFC-11 (ODP=1)
β Antarctic ozone hole = discovered 1985 = forms in spring (SepβNov)
β Polar vortex + Polar Stratospheric Clouds = conditions for Antarctic ozone hole
β Effects: skin cancer, cataracts, immune suppression, crop damage, marine ecosystem damage
β 1% ozone decrease β 2% UV-B increase β 3% skin cancer increase
β Vienna Convention (1985) = framework; Montreal Protocol (1987) = binding phase-out
β Montreal Protocol = only UN treaty with universal ratification (197 parties)
β Most successful environmental treaty = prevented 2 million skin cancer cases/year
β Kigali Amendment (2016) = phase-down of HFCs = could prevent 0.5Β°C warming
β HFCs = zero ODP but high GWP = replaced CFCs = now being phased down
β India ratified Kigali Amendment in 2021; HFC phase-down by 85% by 2047
β Ozone recovery: mid-latitudes ~2040; Arctic ~2045; Antarctica ~2066
β Nobel Prize Chemistry 1995 = Molina, Rowland, Crutzen = CFC-ozone link
β Dobson Units (DU) = measure of ozone column; normal ~300 DU; ozone hole <220 DU
β Chapman cycle = natural ozone formation and destruction = in balance without ODS
β CFCs = most important ODS = stable in troposphere = drift to stratosphere over 6β10 years
β 1 Cl atom from CFC = destroys 100,000 ozone molecules (catalytic)
β Halons = highest ODP per molecule (3β10) = used in fire extinguishers
β ODP = Ozone Depletion Potential = relative to CFC-11 (ODP=1)
β Antarctic ozone hole = discovered 1985 = forms in spring (SepβNov)
β Polar vortex + Polar Stratospheric Clouds = conditions for Antarctic ozone hole
β Effects: skin cancer, cataracts, immune suppression, crop damage, marine ecosystem damage
β 1% ozone decrease β 2% UV-B increase β 3% skin cancer increase
β Vienna Convention (1985) = framework; Montreal Protocol (1987) = binding phase-out
β Montreal Protocol = only UN treaty with universal ratification (197 parties)
β Most successful environmental treaty = prevented 2 million skin cancer cases/year
β Kigali Amendment (2016) = phase-down of HFCs = could prevent 0.5Β°C warming
β HFCs = zero ODP but high GWP = replaced CFCs = now being phased down
β India ratified Kigali Amendment in 2021; HFC phase-down by 85% by 2047
β Ozone recovery: mid-latitudes ~2040; Arctic ~2045; Antarctica ~2066
β Nobel Prize Chemistry 1995 = Molina, Rowland, Crutzen = CFC-ozone link