The greenhouse effect and global warming (spec 4.17, 4.21P, 4.22P)
COβ + methane trap infrared β warming β climate change.
The natural greenhouse effect keeps Earth's average surface temperature at about +15 Β°C (without it, Earth would be ~-18 Β°C β frozen). It is GOOD β life depends on it.
How it works (mechanism):
- Short-wavelength SOLAR radiation (mostly visible light + UV) passes through the atmosphere and warms the Earth's surface.
- The Earth re-radiates this heat as long-wavelength INFRARED radiation back towards space.
- Greenhouse gases (COβ, methane, water vapour, NβO) in the atmosphere ABSORB this outgoing infrared.
- The gas molecules then re-emit infrared in ALL directions, including BACK towards the Earth's surface.
- This 'traps' heat in the lower atmosphere, warming the planet.
The ENHANCED greenhouse effect is the EXTRA warming caused by HIGHER concentrations of greenhouse gases from human activities.
Main greenhouse gases and their sources:
| Gas | Source | Notes |
|---|---|---|
| COβ | Burning fossil fuels (coal, oil, gas), deforestation by burning | Most abundant; COβ has risen from 280 ppm (pre-industrial) to >420 ppm today |
| Methane (CHβ) | Cattle (flatulence), rice paddies (anaerobic bacteria), landfill, natural gas leaks | ~25Γ more potent than COβ per molecule, but in lower concentration |
| Nitrous oxide (NβO) | Fertilisers, vehicle exhausts | Very potent but small amounts |
| Water vapour | Naturally present; increased by warming (positive feedback) | Most abundant greenhouse gas overall |
| CFCs | Refrigerants (older), aerosol sprays (older) | Also damage ozone layer; banned by Montreal Protocol |
Biological consequences of global warming:
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Melting of polar ice and glaciers β sea-level rise β coastal flooding β loss of coastal habitats (mangroves, estuaries).
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Shifting climate zones β species ranges change. Tropical species expand poleward; cold-adapted species (polar bears, snow leopards) lose habitat. Spring arrives earlier β disrupts pollinator-flower synchrony.
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Ocean acidification β COβ + HβO β carbonic acid (HβCOβ). Lower ocean pH dissolves carbonate shells β corals BLEACH and die; shellfish, plankton suffer.
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Extreme weather β heatwaves, droughts, storms, floods. Crop failure β famine. Wildfires destroy ecosystems.
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Spread of disease β warmer climates allow tropical disease vectors (mosquitoes carrying malaria, dengue, Zika) to expand into previously cool regions.
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Mass extinction β many species cannot adapt fast enough. Estimates: 5-50 % of species at risk by 2100 depending on warming scenario.
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Food production β wheat / rice yields fall in heat-stressed regions; some boreal regions become more productive. Net effect is likely negative.
Don't confuse with OZONE DEPLETION. The OZONE LAYER (in the stratosphere) absorbs harmful UV. CFCs destroy ozone β more UV reaches surface β skin cancer, eye damage, harm to plants. This is a SEPARATE problem from the greenhouse effect β different gases, different layers of atmosphere, different consequences. Both can be caused by CFCs, but the mechanisms differ.
- Greenhouse gases absorb INFRARED and re-emit it β trap heat.
- Main gases: COβ (fossil fuels, deforestation), CHβ (cattle, rice paddies, landfill).
- Consequences: melting ice, sea-level rise, climate shifts, extreme weather, ocean acidification, spread of disease, mass extinction.
- Don't confuse greenhouse effect with OZONE depletion (different problem).
See the full worked example for human influences on the environment β