This is the fourth topic post in Unit I — Introduction to Environmental Law. It moves from the scale of biodiversity within ecosystems to atmosphere-level environmental problems — the ones that dominate international environmental law, covered fully in Unit V.
Students routinely use "global warming," "climate change," and "ozone depletion" as if they were interchangeable — but they are three distinct atmospheric phenomena, with different causes, different mechanisms, and different legal responses. Getting them mixed up is one of the most common exam mistakes in this unit. This post separates the three clearly, and then shows how they connect.
Ozone depletion is the thinning of the ozone layer in the Earth's stratosphere, caused by the breakdown of ozone (O₃) molecules. The ozone layer sits roughly 10 to 50 kilometres above the Earth's surface and absorbs nearly all of the Sun's harmful ultraviolet (UV-B and UV-C) radiation, shielding humans, wildlife, and ecosystems from it.
Causes of ozone depletion:
Effects of ozone depletion: increased UV exposure raises the risk of skin cancer, cataracts, and weakened immune systems in humans; disrupts marine ecosystems (particularly phytoplankton, a base of the ocean food chain); reduces crop yields in UV-sensitive crops like wheat, rice, and soybeans. Some ozone-depleting substances are also potent greenhouse gases, which is the first link between this topic and global warming.
The international legal response — the Montreal Protocol, 1987 — is covered in full in Unit V; for this unit, know that it exists and successfully reduced global CFC use.
Global warming is the long-term increase in the Earth's average surface temperature, caused by the excessive accumulation of greenhouse gases (GHGs) in the atmosphere.
Causes of global warming:
Climate change refers to long-term shifts in temperature, precipitation, and weather patterns — global warming is its primary driver, but climate change is the broader, downstream consequence. Where global warming describes the rise in temperature itself, climate change describes everything that rise sets off.
Effects of global warming and climate change together:
The full international legal framework — Kyoto Protocol, UNFCCC, and the Paris Agreement — is covered in Unit V; this unit only needs the underlying phenomena.
| Basis | Global Warming | Climate Change |
|---|---|---|
| Definition | Rise in Earth's average surface temperature | Long-term shift in temperature, precipitation, and weather patterns |
| Scope | Narrower — one specific measurable trend | Broader — includes temperature, rainfall, storm patterns, sea levels |
| Relationship | The primary cause | The resulting, wider-reaching effect |
| Example | Global average temperature crossed 1.5°C above pre-industrial levels for the first time in 2024 (WMO/Copernicus) | More frequent droughts in one region, more frequent floods in another, as a result |
How the three phenomena connect: Ozone Depletion (stratospheric ozone thins) → some ODS are also greenhouse gases → Global Warming (average surface temperature rises) → drives → Climate Change (broader, long-term shift in weather patterns).
An old refrigerant (a CFC) leaks from an outdated air-conditioning unit. As it drifts up into the stratosphere, it breaks down ozone molecules — that is ozone depletion. The same CFC molecule also happens to trap heat in the atmosphere — contributing, alongside CO₂ from power plants and vehicles, to global warming. Over decades, that warming shifts monsoon patterns, melts glaciers feeding Indian rivers, and increases the frequency of heatwaves — that broader, cascading shift is climate change. One molecule, three distinct but connected phenomena.