Climate change is a large-scale, long-term shift in the planet's weather patterns or average temperatures. Earth has had tropical climates and ice ages many times in its 4.5 billion years. So what's happening now?
Since the last ice age, which ended about 11,000 years ago, Earth's climate has been relatively stable, with an average global temperature of about 14 °C. However, in recent years, the average temperature has been increasing, and multiple indicators across the climate system show that climate is changing.
The information below details the seven main sources of evidence for climate change. You can find out more about the difference between weather and climate, what drives our climate and how our climate is changing in our What is climate change? or scroll to the foot of this page for our video - What is climate change?
Global average surface temperature has increased by about 1 °C since the 1850s. Each of the last three decades has been successively warmer than any other preceding decade in the instrumental record, and 16 of the 17 warmest years on record have occurred since the year 2001. Check out our interactive global temperature visualisation, here. You can also see how global average temperature has changed each year since 1850 in the video below:
Observations show that rainfall has increased in the mid-latitudes of the northern hemisphere since the beginning of the 20th century. There are also changes between seasons in different regions. For example, the UK's summer rainfall is decreasing on average, while winter rainfall is increasing. There is also evidence that heavy rainfall events have become more intensive, especially over North America. Longer-term records of rainfall are needed for some areas to resolve any trends from natural variability.
Changes in nature
Changes in the seasons (such as the UK spring starting earlier, autumn starting later) are bringing changes in the behaviour of species, for example, butterflies appearing earlier in the year and birds shifting their migration patterns.
Sea level rises
Since 1900, global mean sea level has risen by more than 20 cm. The rate of sea-level rise has increased in recent decades: from around 1.7 mm per year over the last century, to 3.3 mm per year since the early 1990s.
Glaciers all over the world - in the Alps, Rockies, Andes, Himalayas, Africa and Alaska - are melting and the rate of shrinkage has increased in recent decades.
Arctic sea-ice has been declining since the late 1970s, reducing in extent by about 4%, or 0.6 million square kilometres (an area about the size of Madagascar) per decade. The summer minimum Arctic sea ice extent has decreased by 13.3% per decade since 1979. At the same time Antarctic sea-ice has been more stable, though most areas have been at very low levels since autumn 2016. Read more in our sea ice briefings.
The Greenland and Antarctic ice sheets, which between them store the majority of the world's fresh water, are both shrinking at an accelerating rate.