Ice sheets are made up of layers of ice, one layer formed each year, scientists can analyse the gases trapped in the layers to determine past temperatures
Remains of organisms found in ocean sediment cores can also be analysed to extend the temperature record back at least 5 million years
Pollen from plants gets preserved in sediment, scientists can identify and date the pollen to show which species were living at that time, and infer past climate conditions
As a tree grows it forms a new ring each year, the thickness of the rings shows what the climate was like, providing a reliable source of evidence of climate change for the past 10 000 years
Since the 1850s, global temperatures have been measured accurately using thermometers, providing a reliable but short-term record of temperature change, historical records can extend the record further back
Variations in the Earth's orbit around the Sun, including eccentricity, tilt, and wobble, may have caused the glacial and interglacial cycles of the Quaternary period
Major volcanic eruptions eject large quantities of material into the atmosphere, some of which reflects the Sun's rays back out to space, causing short-term cooling
The Sun's energy output isn't constant, changes in short cycles of about 11 years and possibly longer cycles, reduced solar output may cause cooling in some areas, but is not thought to have a major effect on global climate change
Greenhouse gases, such as carbon dioxide (CO2) and methane, absorb outgoing heat from the Earth, so less is lost to space, keeping the planet warm, but increased levels trap more energy and cause the planet to warm up even more
Plants remove CO2 from the atmosphere through photosynthesis, when trees are cut down they stop taking in CO2 and CO2 is also released when the trees are burnt or decompose