What Is Climate Change?

Climate change refers to long-term shifts in global temperatures and weather patterns. While natural factors have always influenced climate, human activities since the Industrial Revolution have been the primary driver of accelerated warming, mainly through the burning of fossil fuels like coal, oil, and natural gas.

The greenhouse effect is a natural process that warms the Earth. However, human activities have intensified this effect by increasing concentrations of greenhouse gases in the atmosphere, trapping more heat and raising global temperatures.

Key Greenhouse Gases

GasSourceGlobal Warming PotentialAtmospheric Lifetime
Carbon Dioxide (CO2)Fossil fuel combustion, deforestation1 (baseline)300-1000 years
Methane (CH4)Agriculture, landfills, natural gas80x (20-year)12 years
Nitrous Oxide (N2O)Agriculture, industrial processes273x (100-year)121 years
Fluorinated GasesIndustrial applications, refrigeration1000-23000xUp to 50,000 years

Observed Impacts

The Paris Agreement

Key Goals

The 2015 Paris Agreement aims to limit global warming to well below 2 degrees Celsius above pre-industrial levels, with efforts to limit the increase to 1.5 degrees. To achieve this, countries submit Nationally Determined Contributions (NDCs) outlining their emission reduction targets.

Despite commitments, current policies put the world on track for approximately 2.7 degrees of warming by 2100. Closing this gap requires rapid transformation of energy systems, transportation, agriculture, and industry.

Climate Tipping Points

Scientists have identified several tipping points that, once crossed, could trigger cascading and irreversible changes:

  1. Collapse of the Greenland and West Antarctic ice sheets
  2. Widespread permafrost thaw releasing stored carbon
  3. Dieback of the Amazon rainforest
  4. Shutdown of the Atlantic Meridional Overturning Circulation
  5. Loss of coral reef ecosystems
  6. Boreal forest shift and dieback