Finding Evidence of Past Climates
Scientists are basically climate detectives, digging up clues about Earth's weather history from some pretty clever places. Sediment cores from lake bottoms contain pollen that reveals what plants were growing thousands of years ago - tropical pollen means the climate was much warmer back then.
Ice cores are like nature's time capsules. Scientists drill deep into ancient ice and extract air bubbles that contain CO₂ from thousands of years ago. Low CO₂ levels usually mean the climate was colder, whilst high levels suggest warmer periods.
Dendrochronology (tree ring dating) shows annual growth patterns in trees. Thick rings mean good growing conditions with warm, wet weather, whilst thin rings suggest harsh years with cold or dry conditions.
Cool Fact: Fossils of animals that now live in warm climates tell us those areas used to be much hotter - imagine finding crocodile fossils in Scotland!
Milankovitch cycles explain the natural climate swings over thousands of years. Earth's orbit changes shape every 100,000 years, its tilt shifts every 41,000 years, and it wobbles like a spinning top every 26,000 years. When these cycles align, they can trigger ice ages or super-warm periods.
Sunspot cycles also affect our climate. The sun goes through 11-year cycles from minimum to maximum sunspot activity, with maximum periods creating solar flares that pump out more heat.