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Global Warming

Also known as:global temperature riseanthropogenic warmingclimate warming

Global warming refers to the long-term increase in Earth's average surface temperature, primarily caused by the enhanced greenhouse effect resulting from human-induced emissions of greenhouse gases such as carbon dioxide, methane, and nitrous oxide. Since the pre-industrial era (before 1850), global average temperatures have risen by approximately 1.2°C, with the rate of warming accelerating significantly since the mid-20th century. This warming drives profound changes in climate patterns, sea levels, ice cover, and biodiversity worldwide.

Global Temperature Anomalies and Key Milestones

Period / YearTemperature AnomalyCO₂ ConcentrationKey Event
Pre-industrial (1850)Baseline (0°C)280 ppmReference period
1950+0.1°C311 ppmPost-WWII industrial expansion
1988+0.4°C351 ppmIPCC established
2016+1.0°C403 ppmHottest year at that time
2023+1.4°C419 ppmHottest year on record
Paris Agreement target+1.5°C limitStabilisation goalThreshold to limit severe impacts

Interactive Tools

PhET Greenhouse Effect Simulation

Simulate how increasing CO₂ levels raise Earth's surface temperature

Open Tool

Khan Academy – Global Warming

Lessons on causes, evidence, and consequences of global warming

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WolframAlpha Climate

Query global temperature records, CO₂ data, and climate projections

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Graph of global surface temperature anomalies from 1880 to present showing an upward trend

Wikimedia Commons, CC BY-SA

Related Terms

Earth Science

Greenhouse Effect

The greenhouse effect is the process by which certain gases in Earth's atmosphere — primarily water vapour, carbon dioxide, methane, and nitrous oxide — absorb and re-emit infrared radiation from the planet's surface, trapping heat and warming the lower atmosphere. This natural phenomenon is essential for life on Earth, raising the average surface temperature from a frigid −18°C (without greenhouse gases) to the current mean of approximately 15°C. Human activities that increase greenhouse gas concentrations enhance this effect, driving global warming and climate change.

Earth Science

Climate Change

Climate change refers to long-term shifts in global and regional climate patterns, including changes in temperature, precipitation, wind patterns, and the frequency of extreme weather events, driven largely by human activities since the mid-20th century. While Earth's climate has always varied naturally due to orbital cycles, volcanic eruptions, and solar variability, the current rate and magnitude of change are unprecedented in the geological record of the past 800,000 years. The primary driver is the increased atmospheric concentration of greenhouse gases from burning fossil fuels, deforestation, and agricultural practices.

Earth Science

El Niño

El Niño is the warm phase of the El Niño–Southern Oscillation (ENSO), a periodic climate pattern involving anomalously warm sea surface temperatures in the central and eastern tropical Pacific Ocean that typically occurs every 2 to 7 years and lasts 9 to 12 months. This ocean–atmosphere interaction disrupts normal trade wind patterns, suppresses the cold upwelling of the Peruvian coast, and triggers widespread alterations in global precipitation and temperature distributions. El Niño events are associated with droughts in Australia and South Asia, flooding in South America and East Africa, and unusually warm global mean temperatures.

The phrase "global warming" was popularised in the 1970s and 1980s to describe the rising mean surface temperature of the Earth. Wallace Broecker is often credited with bringing the term to wider scientific attention in his 1975 paper "Climatic Change: Are We on the Brink of a Pronounced Global Warming?" The words derive from Latin globus (sphere) and Old English wearmian (to become warm).

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