Climate change evidence comes from many independent measurements of Earth, the atmosphere, the oceans, and living systems. Scientists do not rely on just one graph or one instrument. Instead, they compare records from satellites, weather stations, ice cores, tree rings, ocean buoys, and glaciers. When all of these lines of evidence point in the same direction, confidence in the conclusion becomes very strong.

The main pattern is that Earth is warming and the recent rate of change is unusual compared with much of recent natural history. Greenhouse gases such as carbon dioxide absorb outgoing infrared radiation, which changes Earth’s energy balance. As extra energy builds up, air and ocean temperatures rise, ice melts, sea level increases, and ecosystems shift. Evidence from the past also helps scientists separate natural climate variations from the stronger warming trend caused by human activities today.

Key Facts

  • CO2 + other greenhouse gases increase radiative forcing, which warms the climate system.
  • Global mean temperature has risen by about 1.1 degrees C since the late 1800s.
  • Sea level rises from both thermal expansion and added water from melting land ice.
  • Ice core records show that CO2 levels today are much higher than preindustrial levels.
  • Energy imbalance means incoming solar energy > outgoing infrared energy.
  • A simple climate relation is DeltaT = lambda x DeltaF, where temperature change depends on climate sensitivity and radiative forcing.

Vocabulary

Greenhouse gas
A greenhouse gas is a gas in the atmosphere that absorbs and re-emits infrared radiation, helping trap heat.
Radiative forcing
Radiative forcing is the change in Earth’s energy balance caused by factors such as greenhouse gases, aerosols, or solar changes.
Ice core
An ice core is a cylinder of ice drilled from glaciers or ice sheets that preserves past air bubbles and climate information.
Thermal expansion
Thermal expansion is the increase in volume that happens when seawater warms, which contributes to sea level rise.
Proxy record
A proxy record is an indirect source of climate information, such as tree rings or sediment layers, used to infer past conditions.

Common Mistakes to Avoid

  • Assuming weather and climate are the same, which is wrong because weather describes short-term local conditions while climate describes long-term patterns over decades or longer.
  • Using one cold winter or snowstorm to reject global warming, which is wrong because single events do not overturn long-term global temperature trends.
  • Thinking carbon dioxide is too small a part of the atmosphere to matter, which is wrong because even trace gases can strongly affect infrared absorption and Earth’s energy balance.
  • Believing sea level rise only comes from melting sea ice, which is wrong because floating sea ice adds little direct rise while warming oceans and melting land ice are the main contributors.

Practice Questions

  1. 1 A coastal tide gauge shows sea level rising at 3.4 mm per year. How much will sea level rise in 25 years if that rate stays constant? Give your answer in mm and cm.
  2. 2 A region had an average temperature of 14.2 degrees C in 1900 and 15.5 degrees C today. What is the temperature increase, and what is the percent increase relative to the 1900 value?
  3. 3 Scientists measure rising air temperature, warming oceans, shrinking glaciers, earlier spring events, and increasing atmospheric CO2. Explain why these multiple observations together provide stronger evidence for climate change than any one observation alone.