About climate change

This page explains what climate change is, how we know it is happening, and what this might mean for the future.

What is climate change?

Earth’s atmosphere is made up of oxygen, a large amount of nitrogen and a small percentage of greenhouse gases.

Greenhouse gases act like a blanket around the Earth. They trap warmth from the sun and make life on Earth possible. Without them, too much heat would escape and the surface of the planet would freeze. However, increasing the concentration of greenhouse gases in the atmosphere causes the Earth to heat more and the climate to change.

This process is often called global warming but it is better to think of it as climate change because it is likely to change other aspects of climate as well as temperature, and also bring about more extreme climate events such as floods, storms, cyclones and droughts.

Multiple lines of evidence show climate change is happening

There is lots of evidence that tells us the average temperatures of the world's atmosphere and oceans have increased over the last 150 years.

Evidence includes:

  • direct temperature measurements on land
  • changes in the dates when lakes and rivers freeze and their ice melts
  • a reduction in the extent of snow cover in the Northern Hemisphere
  • a reduction in glaciers
  • extended growing seasons of plants
  • changes in the heat stored in the ocean
  • changes in rainfall patterns resulting in more floods, droughts and intense rain.

A number of biological changes have also been observed.

These include:

  • shifts in the ranges of some plant and animal species
  • earlier timing of spring events such as leaf-unfolding, bird migration and egg-laying for some species.

Together these indicators provide clear evidence that the climate is changing.

It is extremely likely that humans are the cause of recent warming

It is true that climate change has been driven by natural causes in the past. Our climate has undergone many changes over millions of years — from ice ages to tropical heat and back again. Natural changes over the past 10,000 years have generally been gradual which has enabled people, plants and animals to adapt or migrate, although some prehistoric climate changes may have been abrupt and are likely to have led to mass extinction of species.

However, over the past 150 years there has been a marked and growing increase in greenhouse gas producing activities such as industry, agriculture and transportation. These human-induced activities are increasing the level of greenhouse gases in our atmosphere and causing the Earth not only to heat up, but to heat up at an unprecedented rate. This recent warming can only be explained by the influence of humans.

The levels of carbon dioxide and methane in the atmosphere are increasing

The levels of carbon dioxide and methane in the atmosphere have increased as the result of human activities and are now higher than they have been in at least 800,000 years.

We know this from a number of ice core studies. Snow traps tiny bubbles of air as it falls and is compressed into ice. Over the years, more and more ice layers stack up on top of each other. Drilling into ice sheets in Antarctica and Greenland provides a record of what the atmosphere was like back in time.

Direct measurements of atmospheric concentrations of greenhouse gases show how our global greenhouse gas emissions have grown in past decades.

These analyses provide very clear and consistent results that today's greenhouse gas concentrations are far higher than they were at any time during the past 800,000 years

The Earth’s temperature is changing at a rate unprecedented in recent history

Globally, our climate has been relatively stable for the past 10,000 years.  If the world does not take action to reduce greenhouse gas emissions, the global average temperature is very likely to change more rapidly during the 21st century than during any natural variations over the past 10,000 years. This will make it difficult for plants and animals to adapt to climate change.

Limiting climate change will require substantial reductions of greenhouse gas emissions

Future climate change will largely depend on the total sum of greenhouse gases emitted since the start of the industrial revolution. Greenhouse gas emissions have continued to increase over past decades and limiting climate change will mean reversing this trend.

The effects of climate change will continue even after emissions are reduced

The climate system takes time to change, and human activities have already released large amounts of greenhouse gases into the atmosphere. As a result, the effects of climate change will continue even if we reduce emissions now. For example, the deep oceans take centuries to heat up when the atmosphere above them warms. This means that oceans will continue to heat up, and therefore expand causing sea-levels to rise, even if greenhouse gas concentrations in the atmosphere are no longer increasing. Although we cannot avoid climate change entirely, reducing our emissions can limit its impact.

The climate system is very complex and there are still uncertainties about future climate changes

How the climate will change in the future depends on the amount of greenhouse gases we release into the atmosphere. It also depends on how the Earth responds to the increased heating. So we cannot be precise about future climate change. But we are generally sure of the direction of change (eg, the world will become warmer and global average sea-levels will rise). We can also give plausible ranges for those changes. For example, scenarios of future climate change looked at by the Intergovernmental Panel on Climate Change (IPCC) show the world’s average temperature is expected to increase by between 0.9 and 5.4 degrees Celsius at the end of the 21st century, relative to the average temperature from 1850-1900.

Climate change will affect New Zealand

Climate change is already affecting our climate. It is likely to impact our agriculture and other climate-sensitive industries, our native ecosystems, infrastructure, health and biosecurity, as well as having broader social and economic impacts.

New Zealand can expect to see changes in wind patterns, storm tracks, the occurrence of droughts and frosts and the frequency of heavy rainfall events as well as rising temperatures. The impacts of climate change in New Zealand will become more pronounced as time goes on.

In 2013, the Office of the Prime Minister’s Chief Science Advisor published a report on ‘New Zealand’s Changing Climate and Oceans’. This report is available at: Publications Office [Prime Minister’s Chief Science Advisor website].

Watch a video on the science of climate change

The Intergovernmental Panel on Climate Change (IPCC) provides comprehensive assessments of climate change science covering the physical science basis, impacts, adaptation and vulnerability, and mitigation.

The following video funded by the UN Foundation summarises information from IPCC’s 2013 report on the physical science of climate change.

Climate Change — The state of the science [Vimeo website]