The course begins with first principles: Earth’s temperature is determined by the balance between incoming shortwave solar radiation and outgoing longwave terrestrial radiation. Students learn to compute the effective radiating temperature of Earth (~255 K) and then explain why the surface temperature is ~288 K — the greenhouse effect. Key concepts include:
Future projections (IPCC AR6) are analyzed, comparing SSP scenarios from 1.5°C to 4.5°C warming by 2100. Students calculate expected sea level rise (thermal expansion + ice melt), ocean acidification (drop in pH ~0.3–0.4 units), and shifts in biome boundaries. esys 3362 upd
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