Earth's Atmosphere and Climate Change
Ever wondered why Earth isn't a frozen wasteland like Mars? It's all down to our atmospheric composition and the greenhouse effect that keeps us cosy.
Today's atmosphere is 78% nitrogen and 21% oxygen, but 4.6 billion years ago, Earth was completely different. The early atmosphere was mainly carbon dioxide with no oxygen - just like Mars and Venus today. Intense volcanic activity released gases, and as water vapour cooled to form oceans, CO₂ dissolved and reacted with minerals.
Fossil fuels formed when ancient organic matter got buried and compressed. Coal came from ferns and trees, whilst oil and gas formed from compressed plankton. The greenhouse effect works because energy from the sun arrives as short wavelength radiation, gets absorbed by Earth's surface, then radiates back as long wavelength radiation that greenhouse gases trap.
Key Insight: Your carbon footprint measures all the CO₂ and greenhouse gases produced throughout a product's entire lifecycle - not just when you use it.
Climate change happens as we burn fossil fuels, releasing more CO₂ and methane. This increases temperatures, melts polar ice, raises sea levels, and creates more extreme weather patterns.































