Topic 1.10

Climate Change as a Hazard

Long-term shift in global temperatures and weather patterns - the defining challenge of our time

+1.2°C

Above pre-industrial

420+ ppm

CO₂ concentration

3mm/yr

Sea level rise

>95%

Scientific certainty

What is Climate Change?

Climate change is a long-term shift (decades to millennia) in global average temperatures and weather patterns. While climate has always changed naturally, the current warming is happening at an unprecedented rate - faster than any time in the last 10,000 years. Global temperature is now 1.2°C above pre-industrial levels (1850 baseline) and rising approximately 0.18°C per decade.

Evidence for Climate Change

Multiple independent lines of evidence all point to the same conclusion:

Temperature Records

  • • Rising 0.18°C per decade (last 100 years)
  • • Last 5 years = warmest on record
  • • Ocean temperatures also rising

Ice & Glaciers

  • • Mountain glaciers retreating worldwide
  • • Arctic sea ice declining (summer minimum shrinking)
  • • Greenland/Antarctic ice sheets losing mass

Sea Level

  • • Rising 3 mm/year (accelerating)
  • • Thermal expansion (water expands when heated)
  • • Glacial melt adding water to oceans

Ecological Changes

  • • Species migrating to cooler climates
  • • Breeding seasons shifting earlier
  • • Coral bleaching events increasing

Atmospheric CO₂

Currently 420+ ppm - the highest in 3 million years. Increasing at 2 ppm/year. Pre-industrial level was 280 ppm (stable for thousands of years).

Interactive: CO₂ & Climate Simulator

CO₂ & Climate Simulator
Year1990
1850195020242100
Industrial acceleration

393

CO₂ (ppm)

+1.0°C

Temperature

+16cm

Sea Level

Great acceleration: Post-war economic boom. CO₂ emissions accelerating rapidly. Global temperature starting measurable rise.

Causes of Climate Change

Natural Causes (Pre-industrial)

Solar variation: 11-year sunspot cycle affects energy output

Orbital cycles: Milankovitch cycles change Earth's position relative to sun (100,000+ year timescales)

Volcanic eruptions: SO₂ in stratosphere causes temporary cooling

Ocean circulation: El Niño/La Niña redistribute heat

Human Causes (Since 1850)

Fossil fuels: CO₂ from coal, oil, gas (~65% of emissions)

Agriculture: Methane from livestock + rice paddies

Fertilizers: N₂O from agricultural runoff

Deforestation: Removes CO₂-absorbing trees, releases stored carbon

Industry: Cement production is major CO₂ source

Why THIS Time is Different

  • • Rate of change is unprecedented in last 10,000 years
  • • Humans are the dominant cause (>95% scientific certainty, IPCC 2021)
  • • CO₂ concentration changing faster than natural cycles

Interactive: Emissions by Sector

Global Emissions by Sector

Click a sector to see mitigation options

The Greenhouse Effect

Natural Greenhouse Effect

Essential for life - without it Earth would be -18°C

  1. 1. Solar radiation enters atmosphere
  2. 2. Some absorbed by surface, warming it
  3. 3. Surface radiates heat (infrared)
  4. 4. GHGs (CO₂, CH₄, N₂O) absorb this heat
  5. 5. Heat radiates back to surface
  6. 6. Result: Surface stays warm enough for life
Enhanced Greenhouse Effect

The current problem - too much of a good thing

Human activities have increased GHG concentrations:

More GHGs in atmosphere
More heat trapped
Additional warming beyond natural level

This is the cause of current climate change

Global Impacts of Climate Change

Temperature & Weather

Heatwaves more frequent, intense, and longer. Heat-related illness/death increasing. Wet areas getting wetter (flooding risk ↑), dry areas getting drier (drought risk ↑). Weather patterns becoming more unpredictable.

Sea Level & Coasts

Rising 3 mm/year from thermal expansion + glacial melt. Threatening low-lying coastal areas and island nations. Saltwater intrusion into freshwater aquifers. Coastal erosion accelerating.

Ecosystems & Biodiversity

Species extinction (can't adapt/migrate fast enough). Habitat loss as climate zones shift. Food chains disrupted. Disease vectors expanding (e.g., malaria spreading poleward).

Food & Water Security

Crop yields declining from heat, drought, flooding. Livestock productivity reduced. Fishing stocks shifting location. 2 billion people depend on glacial water (Himalayas, Alps, Andes) - threatened by glacial melt.

Economic & Social

Rising insurance costs. Infrastructure damage from extreme weather. Agricultural losses. Climate migration (climate refugees). Potential conflict over scarce resources (water, arable land).

Climate Change as a Hazard Multiplier

Direct Hazards

  • • More intense tropical storms (more ocean energy)
  • • Longer, more severe droughts
  • • Extreme heat events
  • • Flooding from extreme rainfall

Indirect Hazards

  • • Famine from crop failure
  • • Disease outbreaks spreading
  • • Water scarcity conflicts
  • • Mass migration (climate refugees)
  • • Economic collapse in vulnerable regions

Interactive: Vulnerability Explorer

Vulnerability Explorer

Select Region Type

Select Climate Hazard

EXTREMEvulnerability

Key vulnerability factors:

  • Low-lying delta regions
  • Limited funds for sea defenses
  • High population density on coast
  • Agriculture dependent on coastal land

Who is Most Vulnerable?

  • LICs: Limited resources for adaptation, agriculture-dependent, food security precarious
  • Small island states: Rising sea levels are existential threat
  • Arid regions: Droughts intensifying existing water stress
  • Megacities in developing world: Overcrowded, informal settlements, poor drainage

Mitigation vs Adaptation

MITIGATION

Reduce GHG emissions - slow the warming

  • • Shift to renewable energy
  • • Improve energy efficiency
  • • Protect and restore forests
  • • Reduce meat consumption
  • • Carbon capture technology
ADAPTATION

Cope with impacts - live with the changes

  • • Build flood defenses
  • • Develop drought-resistant crops
  • • Heat-resistant buildings
  • • Improve healthcare systems
  • • Planned relocation from vulnerable areas

Key point: Both are needed. Mitigation alone won't stop all change because some warming is already "locked in" from past emissions. Adaptation alone won't work if warming continues unchecked.

Interactive: Adaptation Strategy Selector

Adaptation Strategy Selector

Select a climate threat:

Choose a response strategy:

Test Your Knowledge

Climate Change Quiz1/5

Current atmospheric CO₂ is approximately:

Exam Practice

Worked Example6 marks

Climate change is projected to increase tropical storm intensity by 10-20% over the next 50 years due to warmer ocean temperatures. Discuss how this will affect countries at different development levels differently.

Key Terms

Climate Change

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Long-term shift (decades+) in global average temperature and weather patterns

Greenhouse Effect

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Natural process where GHGs trap heat in atmosphere, keeping Earth warm enough for life

Enhanced Greenhouse Effect

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Increased heat trapping due to human-caused rise in GHG concentrations

Mitigation

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Actions to reduce GHG emissions and slow climate change (e.g., renewables, efficiency)

Adaptation

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Actions to cope with climate change impacts (e.g., flood defenses, drought-resistant crops)

Carbon Footprint

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Total GHG emissions caused by an individual, organization, or activity

Tipping Point

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Threshold beyond which changes become self-reinforcing and irreversible (e.g., ice sheet collapse)

IPCC

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Intergovernmental Panel on Climate Change - UN body assessing climate science

Grade 8/9 Focus

  • • Link climate change to increased natural hazard frequency and intensity
  • • Explain unequal vulnerability - why same hazard affects LICs/HICs differently
  • • Distinguish clearly between mitigation and adaptation with specific examples
  • • Use precise statistics: 420+ ppm CO₂, +1.2°C warming, 3mm/year sea level rise, >95% scientific certainty