HSC Geography · Human–Environment Interactions

13.2 Environmental & Human Causes of Climate Change

Chapter 13 · Climate Change · NESA Stage 6 (2022) · Revision deck
By the end you can…

Learning goals

Section 1

Two kinds of cause

Natural vs human

Natural

Orbital cycles, solar output, volcanoes, ocean circulation. Slow — millennia.

Human

Carbon-cycle disruption, fossil fuels, deforestation, enhanced greenhouse. Fast — ~250 yrs.

The recent change is far too rapid to be natural — and lines up with industrialisation.

Section 2 · Natural

Ice-age cycles

Milankovitch cycles

To blame humans, you must first rule out the natural drivers.

Section 3 · Natural

Volcanic activity

Case study: Mount Pinatubo (1991)

~20 million tonnes of SO₂ → cooled Earth ~0.5°C for 1–2 years

Volcanoes cause short-term cooling, not warming — and all volcanoes' annual CO₂ is far less than human emissions.

EnvironmentChange

So volcanoes can't explain sustained warming either.

Section 4 · Human

Disrupting the carbon cycle

The carbon cycle, broken

ATMOSPHERE (CO₂) Plants (sink)photosynthesis Oceans (sink)absorb CO₂ HUMANS: fossil fuels+ deforestation (removes sinks)

Fossil fuels add carbon and deforestation removes sinks → a net rise in CO₂.

Section 5 · Human

The enhanced greenhouse effect

Natural vs enhanced

Natural

Keeps Earth ~33°C warmer — essential for life.

Enhanced (human)

Extra CO₂, methane, N₂O trap more heat → warming.

It's not the effect that's the problem — it's the human increase.

Section 6

The clincher: 800,000 years

CO₂ is off the chart

300 ppm — never exceeded in 800,000 yrs 300420pastnow >420

Today's CO₂ is outside the entire natural range — and spikes with industrialisation. Nature can't do this.

Recap

13.2 in one screen

Pull it together

Next: 13.3 — Impacts of climate change.

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