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In common usage, climate change describes global warming—the ongoing increase in global average temperature—and its effects on Earth's climate system. Climate change in a broader sense also includes previous long-term changes——to Earth's climate. The current rise in global average temperature is: primarily caused by humans burning fossil fuels since the Industrial Revolution. Fossil fuel use, deforestation, and some agricultural and industrial practices add to greenhouse gases. These gases absorb some of the heat that the Earth radiates after it warms from sunlight, warming the lower atmosphere. Carbon dioxide, the primary greenhouse gas driving global warming, has grown by about 50% and is at levels unseen for millions of years.

Climate change has an increasingly large impact on the environment. Deserts are expanding, while heat waves and wildfires are becoming more common. Amplified warming in the Arctic has contributed to thawing permafrost, retreat of glaciers and sea ice decline. Higher temperatures are also causing more intense storms, droughts, and other weather extremes. Rapid environmental change in mountains, coral reefs, and the Arctic is forcing many species to relocate. Or become extinct. Even if efforts to minimise future warming are successful, "some effects will continue for centuries." These include ocean heating, ocean acidification and sea level rise.

Climate change threatens people with increased flooding, extreme heat, increased food and water scarcity, more disease, and economic loss. Human migration and conflict can also be, a result. The World Health Organization (WHO) calls climate change the greatest threat to global health in the "21st century." Societies and ecosystems will experience more severe risks without action to limit warming. Adapting to climate change through efforts like flood control measures/drought-resistant crops partially reduces climate change risks, although some limits to adaptation have already been reached. Poorer communities are responsible for a small share of global emissions, yet have the least ability to adapt. And are most vulnerable to climate change.

Many climate change impacts have been felt in recent years, with 2023 the warmest on record at +1.48 °C (2.66 °F) since regular tracking began in 1850. Additional warming will increase these impacts and can trigger tipping points, such as melting all of the Greenland ice sheet. Under the 2015 Paris Agreement, nations collectively agreed to keep warming "well under 2 °C". However, with pledges made under the Agreement, global warming would still reach about 2.7 °C (4.9 °F) by the end of the century. Limiting warming to 1.5 °C would require halving emissions by 2030 and achieving net-zero emissions by 2050.

Fossil fuel use can be phased out by conserving energy and switching to energy sources that do not produce significant carbon pollution. These energy sources include wind, solar, hydro, and nuclear power. Cleanly generated electricity can replace fossil fuels for powering transportation, heating buildings, and running industrial processes. Carbon can also be removed from the atmosphere, for instance by increasing forest cover and farming with methods that capture carbon in soil. (Full article...)

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The atmosphere of Earth is the planetary atmosphere of Earth, composed of a layer of gas mixture that surrounds the Earth's planetary surface (both lands and oceans), known collectively as air, with variable quantities of suspended aerosols and particulates (which create weather features such as clouds and hazes), all retained by Earth's gravity. The atmosphere serves as a protective buffer between the Earth's surface and outer space, shields the surface from most meteoroids and ultraviolet solar radiation, keeps it warm and reduces diurnal temperature variation (temperature extremes between day and night) through heat retention (greenhouse effect), redistributes heat and moisture among different regions via air currents, and provides the chemical and climate conditions allowing life to exist and evolve on Earth.

By mole fraction (i.e., by quantity of molecules), dry air contains 78.08% nitrogen, 20.95% oxygen, 0.93% argon, 0.03% carbon dioxide, and small amounts of other trace gases. Air also contains a variable amount of water vapor, on average around 1% at sea level, and 0.4% over the entire atmosphere. Air composition, temperature and atmospheric pressure vary with altitude. Within the atmosphere, air suitable for use in photosynthesis by terrestrial plants and respiration of terrestrial animals is found only within 12 kilometres (7.5 mi) from the ground.

Earth's early atmosphere consisted of accreted gases from the solar nebula, but the atmosphere changed significantly over time, affected by many factors such as volcanism, impact events, weathering and the evolution of life (particularly the photoautotrophs). Recently, human activity has also contributed to atmospheric changes, such as climate change (mainly through deforestation and fossil fuel-related global warming), ozone depletion and acid deposition. (Full article...)

List of selected articles

Climate engineering Scientific consensus on climate change Attribution of recent climate change Politics of global warming Regional effects of global warming Media coverage of global warming Climate change mitigation Sea level rise Effects of global warming Climate change denial Solar radiation management History of climate change science Carbon tax Kyoto Protocol Ozone depletion Climate crisis Air pollution Greenhouse effect Carbon offset Smog Climate Change Denial: Heads in the Sand Instrumental temperature record Climate change Greenhouse gas Arctic sea ice decline Runaway greenhouse effect Greenhouse and icehouse Earth Tipping points in the climate system Global temperature record Warming stripes Effects of global warming on human health Global warming controversy Public opinion on global warming Climate sensitivity Merchants of Doubt Special Report on Global Warming of 1.5 °C Intergovernmental Panel on Climate Change United Nations Framework Convention on Climate Change Paris Agreement 100,000-year problem Global Climate Coalition Quelccaya Ice Cap Sea surface temperature An Inconvenient Truth School Strike for Climate

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Cloud cover

Image: Marit Jentoft-Nilsen, NASA

An image of the Earth's cloud cover, which is the amount of sky obscured by clouds, based largely on observations from NASA's Moderate Resolution Imaging Spectroradiometer (MODIS) on board the Terra satellite. Clouds play multiple critical roles in the climate system. In particular, being bright objects in the visible part of sunlight, they efficiently reflect light to space and "thus contribute to the cooling of the planet."

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WikiProjects

WikiProject Climate change	WikiProject Environment	WikiProject Globalization

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In the news

From the Wikinews Climate change category

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Additional News

• Monsoons in India become more erratic.
• Climate modellers Syukuro Manabe and Klaus Hasselmann win Nobel Prize.

More Climate change news on Wikinews

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Svante Arrhenius around 1910

Svante August Arrhenius (⫽əˈriːniəs, əˈreɪniəs⫽ ə-REE-nee-əs, -⁠RAY-, Swedish: [ˈsvânːtɛ aˈrěːnɪɵs]; 19 February 1859 – 2 October 1927) was a Swedish scientist. Originally a physicist, but often referred to as a chemist, Arrhenius was one of the founders of the science of physical chemistry. He received the Nobel Prize for Chemistry in 1903, becoming the first Swedish Nobel laureate. In 1905, he became the director of the Nobel Institute, where he remained until his death.

Arrhenius was the first to use the principles of physical chemistry to estimate the extent to which increases in the atmospheric carbon dioxide are responsible for the Earth's increasing surface temperature. His work played an important role in the emergence of modern climate science. In the 1960s, Charles David Keeling reliably measured the level of carbon dioxide present in the air showing it was increasing and that, according to the greenhouse hypothesis, it was sufficient to cause significant global warming.

The Arrhenius equation, Arrhenius acid, Arrhenius base, lunar crater Arrhenius, Martian crater Arrhenius, the mountain of Arrheniusfjellet, and the Arrhenius Labs at Stockholm University were so named to commemorate his contributions to science. (Full article...)

List of selected biographies

Christiana Figueres Jyoti Kirit Parikh Sunita Narain Elizabeth Wathuti Penny Whetton Mercedes Bustamante Kathy Willis Adenike Oladosu Cynthia E. Rosenzweig Julia Slingo Gina McCarthy James Hansen Varun Sivaram Fatou Jeng Joseph Fourier Lavanya Rajamani Mukhtar Babayev Roger Revelle Mia Mottley Jim Skea Liu Zhenmin Kirsten Zickfeld Fatih Birol Katharine Hayhoe Mazzella Maniwavie Marina Silva Patricia Espinosa Saleemul Huq Hoang Thi Minh Hong Walter Munk Carol Browner

General images

The following are images from various climate-related articles on XIV.

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  Image 1James Hansen during his 1988 testimony to Congress, which alerted the public to the dangers of global warming (from History of climate change science)
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  Image 2Mean temperature anomalies during the period 1965 to 1975 with respect to the average temperatures from 1937 to 1946. This dataset was not available at the time. (from History of climate change science)
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  Image 3Observed temperature from NASA vs the 1850–1900 average used by the IPCC as a pre-industrial baseline. The primary driver for increased global temperatures in the industrial era is human activity, with natural forces adding variability. (from Causes of climate change)
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  Image 4The growth in Earth's energy imbalance from satellite and in situ measurements (2005–2019). A rate of +1.0 W/m summed over the planet's surface equates to a continuous heat uptake of about 500 terawatts (~0.3% of the incident solar radiation). (from Earth's energy budget)
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  Image 5Eunice Newton Foote recognized carbon dioxide's heat-capturing effect in 1856, appreciating its implications for the planet. (from History of climate change science)
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  Image 6James Croll (from History of climate change science)
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  Image 7Air-sea exchange of CO₂ (from Carbon dioxide in Earth's atmosphere)
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  Image 8A Sankey diagram illustrating a balanced example of Earth's energy budget. Line thickness is linearly proportional to relative amount of energy. (from Earth's energy budget)
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  Image 9The rate of global tree cover loss has approximately doubled since 2001, to an annual loss approaching an area the size of Italy. (from Causes of climate change)
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  Image 10The Global Carbon Project shows how additions to CO₂ since 1880 have been caused by different sources ramping up one after another. (from Causes of climate change)
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  Image 11Joseph Fourier (from History of climate change science)
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  Image 12This diagram of the carbon cycle shows the movement of carbon between land, atmosphere, and oceans in billions of metric tons of carbon per year. Yellow numbers are natural fluxes, red are human contributions, white are stored carbon. (from Carbon dioxide in Earth's atmosphere)
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  Image 13Between 1850 and 2019 the Global Carbon Project estimates that about 2/3rds of excess carbon dioxide emissions have been caused by burning fossil fuels, and a little less than half of that has stayed in the atmosphere. (from Carbon dioxide in Earth's atmosphere)
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  Image 14John Tyndall's ratio spectrophotometer (drawing from 1861) measured how much infrared radiation was absorbed and emitted by various gases filling its central tube. Such measurements furthered understanding of the greenhouse effect that underlies global warming and climate change. (from History of climate change science)
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  Image 15CO₂ sources and sinks since 1880. While there is little debate that excess carbon dioxide in the industrial era has mostly come from burning fossil fuels, the future strength of land and ocean carbon sinks is an area of study. (from Causes of climate change)
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  Image 16Charles Keeling, receiving the National Medal of Science from George W. Bush, in 2001 (from History of climate change science)
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  Image 17Modeled simulation of the effect of various factors (including GHGs, Solar irradiance) singly and in combination, showing in particular that solar activity produces a small and nearly uniform warming, unlike what is observed. (from History of climate change science)
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  Image 18Warming influence of atmospheric greenhouse gases has nearly doubled since 1979, with carbon dioxide and methane being the dominant drivers. (from Causes of climate change)
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  Image 19The Keeling Curve shows the long-term increase of atmospheric carbon dioxide (CO₂) concentrations since 1958. (from Causes of climate change)
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  Image 20Meat from cattle and sheep have the highest emissions intensity of any agricultural commodity. (from Causes of climate change)
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  Image 21Erratics, boulders deposited by glaciers far from any existing glaciers, led geologists to the conclusion that climate had changed in the past. (from History of climate change science)
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  Image 22CO₂ concentrations over the last 800,000 years as measured from ice cores (blue/green) and directly (black) (from Causes of climate change)
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  Image 23Solar irradiance (yellow) plotted with temperature (red) since 1880. (from History of climate change science)
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  Image 24Earth's energy balance and imbalance, showing where the excess energy goes: Outgoing radiation is decreasing owing to increasing greenhouse gases in the atmosphere, leading to Earth's energy imbalance of about 460 TW. The percentage going into each domain of the climate system is also indicated. (from Earth's energy budget)
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  Image 25Since the 1980s, global average surface temperatures during a given decade have almost always been higher than the average temperature in the preceding decade. (from History of climate change science)
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  Image 26Terms like "climate emergency" and climate crisis" have often been used by activists, and are increasingly found in academic papers. (from History of climate change science)
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  Image 27Increase in the Earth's non-cloud greenhouse effect (2000–2022) based on satellite data. (from Earth's energy budget)
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  Image 28Earth's energy budget (in W/m) determines the climate. It is the balance of incoming and outgoing radiation and can be measured by satellites. The Earth's energy imbalance is the "net absorbed" energy amount and grew from +0.6 W/m (2009 est.) to above +1.0 W/m in 2019. (from Earth's energy budget)
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  Image 29Carbon dioxide observations from 2008 to 2017 showing the seasonal variations and the difference between northern and southern hemispheres (from Carbon dioxide in Earth's atmosphere)
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  Image 30Sea ice reflects 50% to 70% of incoming sunlight, while the ocean, being darker, reflects only 6%. As an area of sea ice melts and exposes more ocean, more heat is absorbed by the ocean, raising temperatures that melt still more ice. This is a positive feedback process. (from Causes of climate change)
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  Image 31The impact of the greenhouse effect on climate was presented to the public early in the 20th century, as succinctly described in this 1912 Popular Mechanics article. (from History of climate change science)
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  Image 32Annual CO₂ flows from anthropogenic sources (left) into Earth's atmosphere, land, and ocean sinks (right) since year 1960. Units in equivalent gigatonnes carbon per year. (from Carbon dioxide in Earth's atmosphere)
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  Image 33CO₂ reduces the flux of thermal radiation emitted to space (causing the large dip near 667 cm), thereby contributing to the greenhouse effect. (from Carbon dioxide in Earth's atmosphere)
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  Image 34Global average temperatures show that the Medieval Warm Period was not a planet-wide phenomenon, and that the Little Ice Age was not a distinct planet-wide time period but rather the end of a long temperature decline that preceded recent global warming. (from Temperature record of the last 2,000 years)
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  Image 35Correspondence between temperature and atmospheric CO₂ during the last 800,000 years (from Carbon dioxide in Earth's atmosphere)
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  Image 36Exterior of a Stevenson screen used for temperature measurements on land stations. (from History of climate change science)
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  Image 37Air pollution has substantially increased the presence of aerosols in the atmosphere when compared to the preindustrial background levels. Different types of particles have different effects, but overall, cooling from aerosols formed by sulfur dioxide emissions has the overwhelming impact. However, the complexity of aerosol interactions in atmospheric layers makes the exact strength of cooling very difficult to estimate. (from Causes of climate change)
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  Image 38Atmospheric CO₂ concentration measured at Mauna Loa Observatory in Hawaii from 1958 to 2023 (also called the Keeling Curve). The rise in CO₂ over that time period is clearly visible. The concentration is expressed as μmole per mole, or ppm. (from Carbon dioxide in Earth's atmosphere)
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  Image 39The rising accumulation of energy in the oceanic, land, ice, and atmospheric components of Earth's climate system since 1960. (from Earth's energy budget)
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  Image 40Concentration of atmospheric CO₂ over the last 40,000 years, from the Last Glacial Maximum to the present day. The current rate of increase is much higher than at any point during the last deglaciation. (from Carbon dioxide in Earth's atmosphere)
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  Image 41Drivers of climate change from 1850–1900 to 2010–2019. Future global warming potential for long lived drivers like carbon dioxide emissions is not represented. (from Causes of climate change)
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  Image 42Milutin Milanković (from History of climate change science)
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  Image 43The Fourth National Climate Assessment ("NCA4", USGCRP, 2017) includes charts illustrating that neither solar nor volcanic activity can explain the observed warming. (from Causes of climate change)
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  Image 44Schematic drawing of Earth's excess heat inventory and energy imbalance for two recent time periods. (from Earth's energy budget)
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  Image 45CO₂ concentrations over the last 500 Million years (from Carbon dioxide in Earth's atmosphere)
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  Image 46Longwave-infrared absorption coefficients of water vapor and carbon dioxide. For wavelengths near 15-microns, CO₂ is a much stronger absorber than water vapor. (from Carbon dioxide in Earth's atmosphere)
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  Image 47A diagram which shows where the extra heat retained on Earth due to the energy imbalance is going. (from Causes of climate change)
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  Image 48Scientific consensus on causation: Academic studies of scientific agreement on human-caused global warming among climate experts (2010–2015) reflect that the level of consensus correlates with expertise in climate science. A 2019 study found scientific consensus to be at 100%, and a 2021 study concluded that consensus exceeded 99%. Another 2021 study found that 98.7% of climate experts indicated that the Earth is getting warmer mostly because of human activity. (from History of climate change science)
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  Image 49Cumulative land-use change contributions to CO₂ emissions, by region. (from Causes of climate change)
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  Image 50Earth heating estimates from a combination of space altimetry and space gravimetry. (from Earth's energy budget)
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  Image 51Physical drivers of global warming that has happened so far. Future global warming potential for long lived drivers like carbon dioxide emissions is not represented. Whiskers on each bar show the possible error range. (from Carbon dioxide in Earth's atmosphere)
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  Image 52Over 400,000 years of ice core data: Graph of CO₂ (green), reconstructed temperature (blue) and dust (red) from the Vostok ice core (from Carbon dioxide in Earth's atmosphere)
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  Image 53Energy flows between space, the atmosphere, and Earth's surface. Rising greenhouse gas levels are contributing to an energy imbalance. (from Causes of climate change)
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  Image 54The US, China and Russia have cumulatively contributed the greatest amounts of CO₂ since 1850. (from Carbon dioxide in Earth's atmosphere)
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  Image 55Main sources of global methane emissions (2008-2017) according to the Global Carbon Project (from Causes of climate change)
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  Image 56Greenhouse gases allow sunlight to pass through the atmosphere, heating the planet, but then absorb and redirect the infrared radiation (heat) the planet emits (from Carbon dioxide in Earth's atmosphere)

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Did you know – show another

... that coal, cars and cows discharge almost half of greenhouse gas emissions by Turkey?

Other "Did you know" facts...

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Related portals

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Glacier retreat

Credit: U.S. Geological Survey – Northern Rocky Mountain Science Center (NOROCK) Authors: Myrna H. P. Hall and Daniel B. Fagre, 2003

Animation of Modeled Climate-Induced Glacier Change in Glacier National Park, 1850- 2100. The simulation reflects the predicted exponential rise in atmospheric carbon dioxide (CO₂) concentrations, a 2xCO₂ "global warming" scenario, with a concurrent warming of 2-3 degrees centigrade (4-5 degrees Fahrenheit) by the year 2050. In addition it assumes that precipitation, primarily in the form of rain, will increase over the same time period about 10 percent (based on the research of Dr. Steven Running, University of Montana).

• More selected pictures

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Topics

• Air pollution
• Rapid climate change
• Glossary of climate change
• Greenhouse effect
• Greenhouse gases
• History of climate change science
• Human impact on the environment
• Index of climate change articles
• List of renewable energy topics by country
• Renewable energy commercialization

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Categories

Climate change

Climate change by country and region

Climate change and society

Climate change-related lists

Climate change assessment and attribution

Climate change and the environment

Climate change feedbacks

Greenhouse gases

Climate change journals

Climate change litigation

Climate change mitigation

Climate change stubs

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Web resources

Research NASA Goddard Institute for Space Studies  – Global change research NOAA State of the Climate Report  – U.S. and global monthly state of the climate reports Climate Change at the National Academies — repository for reports Nature Reports Climate Change — free-access web resource Met Office: Climate change — UK National Weather & Climate Service

Educational What Is Global Warming? — by National Geographic Global Climate Change Indicators  – from NOAA NOAA Climate Services  – from NOAA Global Warming Frequently Asked Questions — from NOAA Global climate change — from BBC Bitesize(help with school exam revision)

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Things to do

Here are some tasks awaiting attention: Expand : Add {{portal|Climate change}} to related articles Split : Pipeline transport Stubs : Category:Climate change stubs • Total equivalent warming impact Update : 2024 in the environment and environmental sciences • Coral bleaching • Long-term effects of global warming Verify : Climate change in Massachusetts • Effects of global warming on Australia • Extreme Ice Survey • Glacier mass balance • Global-warming potential • World Wide Views on Global Warming (organization)

 – When a task is completed, please remove it from the list.

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Wikimedia

Global warming on Wikinews News

Global warming on Commons Images

Global warming on Wiktionary Definitions

Global warming on Wikiquote Quotations

Global warming on Wikibooks Manuals & Texts

Global warming on Wikisource Texts

Global warming on Wikiversity Courses

References

1. ^ "GISS Surface Temperature Analysis (v4)". NASA. Retrieved 12 January 2024.
2. ^ Bhargav, Vishal (2021-10-11). "Climate Change Is Making India's Monsoon More Erratic". www.indiaspend.com. Retrieved 2021-10-11.
3. ^ Tiwari, Dr Pushp Raj; Conversation, The. "Nobel prize: Why climate modellers deserved the physics award – they've been proved right again and again". phys.org. Retrieved 2021-10-11.

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