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Ozone Layer Depletion




🌑️ Chapter 06 · Topic 03 · 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.

πŸ›‘οΈ Stratospheric Ozone β€” The Protective Shield

The ozone layer is a region of Earth’s stratosphere containing high concentrations of ozone (O₃). It is our planet’s natural sunscreen, absorbing most of the Sun’s harmful ultraviolet radiation.

  • Located in the stratosphere, approximately 15–35 km above Earth’s surface (peak concentration at ~25 km)
  • Absorbs UV-B (280–315 nm) and UV-C (100–280 nm) radiation β€” both harmful to life
  • UV-A (315–400 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
πŸ“Œ Tropospheric vs Stratospheric Ozone: Stratospheric ozone (15–35 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.

βš—οΈ 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†’ O₃ (ozone)
  • Natural destruction: O₃ + UV β†’ Oβ‚‚ + O; O + O₃ 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
⭐ 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.

☠️ Ozone-Depleting Substances (ODS)

SubstanceFull NameMain UsesODPStatus
CFCsChlorofluorocarbons (e.g., CFC-11, CFC-12)Refrigerants, aerosol propellants, foam blowing agents0.6–1.0Phased out under Montreal Protocol
HCFCsHydrochlorofluorocarbons (e.g., HCFC-22)Refrigerants (transitional replacement for CFCs)0.02–0.11Being phased out (transitional)
HalonsBromofluorocarbons (e.g., Halon-1301)Fire extinguishers3–10Phased out; highest ODP per molecule
Methyl BromideCH₃BrAgricultural fumigant (soil sterilisation)0.6Phased out in developed countries
Carbon TetrachlorideCClβ‚„Solvent, fire extinguishers (historical)1.1Phased out
Methyl ChloroformCH₃CCl₃Industrial solvent0.12Phased out
πŸ“Œ 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 (3–10). 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.

πŸ”¬ Mechanism of Ozone Depletion by CFCs

  1. CFCs are released at ground level (from refrigerators, aerosols, etc.) β€” they are very stable and do not react in the troposphere
  2. CFCs slowly drift up to the stratosphere over 6–10 years
  3. In the stratosphere, intense UV radiation breaks the CFC molecule: CFC β†’ Cl (chlorine radical) + other fragments
  4. The chlorine radical attacks ozone: Cl + O₃ β†’ ClO + Oβ‚‚
  5. ClO reacts with atomic oxygen: ClO + O β†’ Cl + Oβ‚‚
  6. The chlorine radical is regenerated β€” it is a catalyst (not consumed in the reaction)
  7. One Cl atom can destroy 100,000 ozone molecules before being deactivated
  8. Bromine (from halons) is even more effective at destroying ozone than chlorine
⭐ 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.

πŸ•³οΈ 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 (September–November)
  • 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 (<βˆ’78Β°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)
πŸ“Œ 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).

β˜€οΈ Effects of Ozone Depletion

EffectDetails
Skin cancerUV-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
CataractsUV-B damages the lens of the eye β†’ cataracts (clouding of lens) β†’ blindness. Leading cause of blindness globally
Immune suppressionUV-B suppresses the human immune system β†’ increased susceptibility to infections and reduced vaccine effectiveness
Crop damageUV-B damages plant DNA, reduces photosynthesis, stunts growth; affects soybean, wheat, rice yields
Marine ecosystem damageUV-B penetrates ocean surface β†’ damages phytoplankton (base of marine food chain) β†’ disrupts entire marine ecosystem
Material degradationUV-B degrades plastics, paints, rubber, and building materials faster

πŸ“œ 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
⭐ 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 2011–2013)
  • 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

🌱 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 (2018–2019) β€” traced to eastern China; subsequently reduced
πŸ“Œ 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.

βœ… Revision Checklist β€” Ozone Layer Depletion

βœ… Ozone layer = stratosphere = 15–35 km altitude = absorbs UV-B and UV-C
βœ… Dobson Units (DU) = measure of ozone column; normal ~300 DU; ozone hole <220 DU
βœ… Chapman cycle = natural ozone formation and destruction = in balance without ODS
βœ… CFCs = most important ODS = stable in troposphere = drift to stratosphere over 6–10 years
βœ… 1 Cl atom from CFC = destroys 100,000 ozone molecules (catalytic)
βœ… Halons = highest ODP per molecule (3–10) = used in fire extinguishers
βœ… ODP = Ozone Depletion Potential = relative to CFC-11 (ODP=1)
βœ… Antarctic ozone hole = discovered 1985 = forms in spring (Sep–Nov)
βœ… Polar vortex + Polar Stratospheric Clouds = conditions for Antarctic ozone hole
βœ… Effects: skin cancer, cataracts, immune suppression, crop damage, marine ecosystem damage
βœ… 1% ozone decrease β†’ 2% UV-B increase β†’ 3% skin cancer increase
βœ… Vienna Convention (1985) = framework; Montreal Protocol (1987) = binding phase-out
βœ… Montreal Protocol = only UN treaty with universal ratification (197 parties)
βœ… Most successful environmental treaty = prevented 2 million skin cancer cases/year
βœ… Kigali Amendment (2016) = phase-down of HFCs = could prevent 0.5Β°C warming
βœ… HFCs = zero ODP but high GWP = replaced CFCs = now being phased down
βœ… India ratified Kigali Amendment in 2021; HFC phase-down by 85% by 2047
βœ… Ozone recovery: mid-latitudes ~2040; Arctic ~2045; Antarctica ~2066
βœ… Nobel Prize Chemistry 1995 = Molina, Rowland, Crutzen = CFC-ozone link