Predictions of Future Global Climate (2022)

Scientists from around the world with the Intergovernmental Panel on Climate Change (IPCC) tell us that during the past 100 years, the world's surface air temperature increased an average of 0.6° Celsius (1.1°F) due to burning fossil fuels that releases carbon dioxide and other greenhouse gases into the atmosphere. This may not sound like very much change, but even one degree can impact the Earth in many ways. Climate models predict that Earth's global average temperature will rise and additional 4° C (7.2° F) during the 21st Century if greenhouse gas levels continue to rise. But with swift action to reduce greenhouse gas emissions, models project that global average temperature will only rise an additional 1° Celsius (1.8° F).

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Predictions of Future Global Climate (1)

According to model projections, if we reduce greenhouse gas emissions, there will be about a degree of warming over this century (the purple line). If we do not reduce greenhouse gases as much, Earth will warm much more (orange line). The area around the lines indicates the range of model results from these two scenarios.
Credit: L.S. Gardiner/UCAR with IPCC (2013) data

Predicted Impacts of Climate Change

Climate change is predicted to impact regions differently. For example, temperature increases are expected to be greater on land than over oceans and greater at high latitudes than in the tropics and mid-latitudes. Warmer temperatures will cause (and are causing) changes to other aspects of climate - such as rain, snow, and clouds. They are also causing changes to the ocean, life, ice, and all other parts of the Earth system.

Changing Precipitation

A warmer average global temperature will cause the water cycle to “speed up” due to a higher rate of evaporation. More water vapor in the atmosphere will lead to more precipitation. Global average precipitation increases by 1% to 3% for each degree of warming, which means we are looking at a future with much more rain and snow, and a higher risk of flooding to some regions. By 2100, precipitation will increase by at least 1% with a possible increase of up to 12%. However, changes in precipitation will not be evenly distributed. Some locations will get more, and others will see less.

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Melting Snow and Ice

As the climate warms, snow and ice melt. It is predicted that the melting of glaciers, ice sheets, and other snow and ice on land in the summer will continue to be greater than the amount of precipitation that falls in the winter, which means a decrease in the total amount of snow and ice on the planet. Over the past 100 years, mountain glaciers in all areas of the world have decreased in size and so has the amount of permafrost in the Arctic. Greenland's ice sheet is melting faster, too. The amount of sea ice (frozen seawater) floating in the Arctic Ocean and around Antarctica is expected to decrease. Already the summer thickness of sea ice in the Arctic is about half of what it was in 1950.Arctic sea ice is melting more rapidly than the Antarctic sea ice. Melting ice may lead to changes in ocean circulation, too. Although there is some uncertainty about the amount of melt, summer in the Arctic Ocean will likely be ice-free by the end of the century.

Rising Sea Level

A warmer climate causes sea level to rise via two mechanisms: (1) melting glaciers and ice sheets (ice on land) add water to the oceans, raising the sea level, and (2) ocean water expands as it warms, increasing its volume and thus also raising sea level. During the 20th Century, sea levels rose about 10 to 20 cm (4 to 8 inches). Thermal expansion and melting ice each contributed about half of the rise, though there is some uncertainty in the exact magnitude of the contribution from each source. By the year 2100, models predict sea level will rise between 30 and 100 cm (12 to 39 inches), threatening coastal communities, wetlands, and coral reefs. The precise amount of sea level rise depends on how much we are able to reduce the amount of climate warming.

Acidic Ocean Water

Earth’s oceans are predicted to act as a buffer against climate change by taking up some of the excess heat and carbon dioxide from the atmosphere. This is good news in the short run, but more problematic in the long run. Carbon dioxide combined with seawater forms weak carbonic acid. Scientists believe this process has reduced the pH of the oceans by about 0.1 pH since pre-industrial times. Further acidification of 0.14 to 0.35 pH is expected by the year 2100. Higher acidity in the ocean causes problems for coral reefs and other marine organisms.

Changes to Ocean Currents

Large-scale ocean currents called thermohaline circulation, driven by differences in salinity and temperature, may also be disrupted as the climate warms. Changes in precipitation patterns and the influx of fresh water into the oceans from melting ice can alter salinity. Changing salinity, along with rising water temperature, may disrupt the currents. In an extreme case, thermohaline circulation could be disrupted or even shut down in some parts of the ocean, which could have large effects on climate.

Changing Severe Weather

Some climate scientists believe that hurricanes, typhoons, and other tropical cyclones will change as a result of global warming. Warm ocean surface waters provide the energy that drives these immense storms. Warmer oceans in the future are expected to cause the intensification of such storms. Although there may not be more tropical cyclones worldwide in the future, some scientists believe there will be a higher proportion of the most powerful and destructive storms. Some scientists believe we already see evidence for an upswing in the numbers of the most powerful storms. Others are less convinced.

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Changing Clouds

Clouds are a bit of a wild card in global climate models. Warmer global temperatures produce faster overall evaporation rates, resulting in more water vapor in the atmosphere...and more clouds. Different types of clouds at different locations have different effects on climate. Some shade the Earth, cooling the climate. Others enhance the greenhouse effect with their heat-trapping water vapor and droplets. Scientists expect a warmer world to be a cloudier one, but are not yet certain how the increased cloudiness will feed back into the climate system. Modeling the influence of clouds in the climate system is an area of active scientific research.

Risks to Marine Life

Ocean ecosystems will change as sea-surface temperatures continues to warm. Animals like fish are able to move to other ecosystems with cooler water at higher latitudes. But many marine organisms – like kelp and corals – that aren’t able to swim elsewhere are at high risk. Warmer waters in the shallow oceans have contributed to the death of about a quarter of the world's coral reefs in the last few decades. Many of the coral animals died after being weakened by bleaching, a process tied to warmed waters.

Risks to Life on Land

Changes in temperature, precipitation, and seasonal timing will alter the geographic ranges of many types of plants and animals. Since species can only survive if they are in a habitat that suits their needs, many species will face extinction if the geographic range where they can survive shrinks. If warming is kept to 2°C, 18% of insects, 16% of plants, and 8% of vertebrate animals are projected to lose over half of their geographic range. However, if we can keep the amount of warming to 1.5°C, the habitat loss to insects, plants, and vertebrates decreases by about a half. On the other hand, the range of some species, such as mosquitos which carry different types of diseases, may increase due to climate warming. Warming surface temperatures are also predicted to increase the frequency of heat waves and droughts, which can affect crop production, increase the risk of wildfires, and even impact human health.

Predictions of Future Global Climate (2)

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Climate change is causing many other aspects of Earth to change, including the examples noted in this graphic. Using models, scientists can project how these aspects of Earth are likely to change in the future as the climate continues to warm.

Abrupt changes are also possible as the climate warms

Some changes to the climate are gradual and predictable, while others are more sudden and difficult to foresee. The latter is often referred to as “tipping points.” A tipping point is a large, abrupt change that cannot readily be stopped at the last minute, even by employing drastic measures. Possible tipping points include:

The collapse of major ice sheets in Greenland and Antarctica

Melting of these ice sheets is an ongoing process. However, there are signs that moderate melting may accelerate into a runaway situation that leads to a relatively sudden loss of large amounts of ice. Such a collapse could lead to dramatic changes in sea level and could also impact ocean circulation.

Disruption of thermohaline circulation

If the ocean’s circulation changed dramatically or even shut down altogether, the transfer of heat in the climate system would be altered in a huge way.

A sudden release of methane

If the potent greenhouse gas methane were released rapidly from its stores in Arctic permafrost and special ices beneath the seafloor (called methane hydrates or clathrates), the rate of warming would increase. Methane releases would generate a feedback loop of increased greenhouse warming by methane, driving further methane emissions. Some scientists suspect that sudden increases in methane may have played a role in major extinction events in the past.

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Ocean uptake of carbon

Today, the ocean is absorbing CO2 that would otherwise stay in the atmosphere. At some point, seawater will become saturated with CO2 and unable to absorb any more. At that point, anthropogenic emissions of CO2 would all land in the atmosphere, increasing the rate of greenhouse warming. Acidification of the oceans could also disrupt marine life, causing photosynthesizing plankton to succumb, preventing them from removing CO2 from the air. Shells of many types of marine organisms might begin to dissolve in the presence of the acidic oceans, releasing the carbon stored within the shells back into the environment.

None of these tipping points are considered very likely to occur over the next several decades. Still, the consequences of any of them are so severe, and the fact that we cannot retreat from them once they’ve been set in motion is so problematic, that we must keep them in mind when evaluating the overall risks associated with climate change.


What will be the future of climate change? ›

Future changes are expected to include a warmer atmosphere, a warmer and more acidic ocean, higher sea levels, and larger changes in precipitation patterns. The extent of future climate change depends on what we do now to reduce greenhouse gas emissions. The more we emit, the larger future changes will be.

What is the prediction for global warming? ›

In the coming five years, the annual mean global temperature is likely to be at least 1°C warmer - within the range 0.9°C – 1.8°C - than preindustrial levels. The chance of temporarily reaching 1.5°C has roughly doubled compared to last year's predictions.

How is the climate predicted to change in the next 100 years? ›

Even if the atmospheric composition of greenhouse gases and other forcing agents was kept constant at levels from the year 2000, global warming would reach about 1.5℃ by the end of the century. Without changing our behaviour it could increase to 3-5℃ by the end of the century.

What is an important conclusion of climate prediction models? ›

1 Answer. An important conclusion of climate prediction models is Increase in global temperature will continue but can be reduced.

What is an important conclusion of climate prediction models Brainly? ›

Explanation: The conclusion is that human activity alters the climate system, raising the global average near-ground temperature.

How will climate change affect us? ›

Climate change can also impact human health by worsening air and water quality, increasing the spread of certain diseases, and altering the frequency or intensity of extreme weather events. Rising sea level threatens coastal communities and ecosystems.

When was the first prediction of climate change? ›

The first quantitative estimate of carbon dioxide-induced climate change was made by Svante Arrhenius, a Swedish scientist and Nobel laureate. In 1896, he calculated that “the temperature in the Arctic regions would rise 8 or 9 degrees Celsius if carbon dioxide increased to 2.5 or 3 times” its level at that time.

How will the climate be in 2050? ›

By 2050, without new policies...

As a result, global average temperature is projected to be 3 degrees celsius to 6 degrees celsius above pre-industrial levels by the end of the century, exceeding the internationally agreed goal of limiting it to 2 degrees celsius.

What will happen to the climate in 2025? ›

Climate Report. Emissions rates are still growing every year, though that growth has slowed. The world needs to reach negative growth soon to prevent a potential 3.2°C rise by the end of the century.

How hot will the Earth be in 2030? ›

AUnderstanding Global Warming of 1.5°C*

… warming above pre-industrial levels, with a likely range of 0.8°C to 1.2°C. Global warming is likely to reach 1.5°C between 2030 and 2052 if it continues to increase at the current rate.

How will the climate be in 2050? ›

By 2050, without new policies...

As a result, global average temperature is projected to be 3 degrees celsius to 6 degrees celsius above pre-industrial levels by the end of the century, exceeding the internationally agreed goal of limiting it to 2 degrees celsius.

How warm will the Earth be in 2050? ›

Global temperature is projected to warm by about 1.5 degrees Celsius (2.7° degrees Fahrenheit) by 2050 and 2-4 degrees Celsius (3.6-7.2 degrees Fahrenheit) by 2100.

How the world will be in 2050? ›

By 2050 , the world's population will exceed at least 9 billion and by 2050 the population of India will exceed that of China. By 2050, about 75% of the world population will be living in cities. Then there will be buildings touching the sky and cities will be settled from the ground up.

How many years do we have to save the Earth? ›

Scientists say eight years left to avoid worst effects.” : “IPCC climate report gives us 10 years to save the world.”

How long do we have before climate change becomes irreversible? ›

There is some indication the system has experienced a gradual weakening over the past few decades, and it may be critically unstable. Lenton's research suggests that if global temperatures continue to rise, the AMOC could collapse in 50 to 250 years.

What will happen in 2050 if climate change keeps going? ›

Climate shifts like heat waves could restrict the ability of people to work outdoor, and, in extreme cases, put their lives at risk. Under a 2050 climate scenario developed by NASA, continuing growth of the greenhouse emission at today's rate could lead to additional global warming of about 1.5 degrees Celsius by 2050.

How hot will it be in 2040? ›

Global Warming Will Hit 1.5 Degrees by 2040, UN IPCC Report Warns.

What will the environment be like in 2030? ›

By 2030, almost all countries will experience “extreme hot” weather every other year due mainly to greenhouse gas pollution by a handful of big emitters, according to a paper published Thursday by Communications Earth & Environment, reinforcing forecasts that the coming year will be one of the hottest on record.

What will happen if climate change doesn't stop? ›

The wildlife we love and their habitat will be destroyed, leading to mass species extinction. Superstorms, drought, and heat waves would become increasingly common and more extreme, leading to major health crises and illness. Agricultural production would plummet, likely leading to global food shortages and famine.

What will it be like in 2070? ›

2070 will be marked by increased acidification of oceans and slow but remorseless sea-level rise that will take hundreds if not thousands of years to reverse – a rise of more than half a metre this century will be the trajectory. “It's a very different world,” Thorne says.

What is the future of world? ›

Four billion years from now, the increase in Earth's surface temperature will cause a runaway greenhouse effect, creating conditions more extreme than present-day Venus and heating Earth's surface enough to melt it. By that point, all life on Earth will be extinct.

What things will we have in the future? ›

Life in the future: Tech that will change the way we live
  • Space Tourism. ...
  • Colonisation of other planets. ...
  • Robots in space and in the workplace. ...
  • Electric/self-driving cars. ...
  • Flying cars. ...
  • Robot butlers. ...
  • Roads over rivers. ...
  • Solar panel technology.
Jul 21, 2021

How the world will be in 3000? ›

By the year 3000, global warming would be more than a hot topic — the West Antarctic ice sheet could collapse, and global sea levels would rise by about 13 feet (4 meters), according to a new study.


1. See what three degrees of global warming looks like
(The Economist)
2. Global Climate Change; Explaining the Past, Predicting the Future
(Royal Geographical Society of South Australia)
3. 2050: what happens if we ignore the climate crisis
(Guardian News)
4. Europe’s climate in 2050
5. How Earth’s Geography Will Change With Climate Change
6. Failed climate predictions – what do they tell us?
(Mallen Baker)

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