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Global warming is the mainly human-caused rise of the average temperature of the Earth's climate system and has been demonstrated by direct temperature measurements and by measurements of various effects of the warming. It is a major aspect of climate change which, in addition to rising global surface temperatures, also includes its effects, such as changes in precipitation. While there have been prehistoric periods of global warming, observed changes since the mid-20th century have been unprecedented in rate and scale.

The Intergovernmental Panel on Climate Change (IPCC) concluded that, "human influence on climate has been the dominant cause of observed warming since the mid-20th century". These findings have been recognized by the national science academies of major nations and are not disputed by any scientific body of national or international standing. The largest human influence has been the emission of greenhouse gases such as carbon dioxide, methane, and nitrous oxide. Fossil fuel burning is the principal source of these gases, with agricultural emissions and deforestation also playing significant roles.

The effects of global warming include rising sea levels, regional changes in precipitation, more frequent extreme weather events such as heat waves, and expansion of deserts. Surface temperature increases are greatest in the Arctic, which have contributed to the retreat of glaciers, permafrost, and sea ice. Overall, higher temperatures bring more rain and snowfall, but for some regions droughts and wildfires increase instead. Climate change threatens to diminish crop yields, harming food security, and rising sea levels may flood coastal infrastructure. Environmental impacts include the extinction or relocation of many species as their ecosystems change, most immediately in coral reefs, mountains, and the Arctic. Some impacts, such as loss of snow cover, increased water vapour, and melting permafrost, cause feedback effects that further increase the rate of global warming. Ocean acidification caused by increased CO₂ levels is commonly grouped with these effects even though it is not driven by temperature.

Mitigation efforts to address global warming include the development and deployment of low carbon energy technologies, policies to reduce fossil fuel emissions, reforestation, forest preservation, as well as the development of potential climate engineering technologies. Societies and governments are also working to adapt to current and future global warming impacts, including improved coastline protection, better disaster management, and the development of more resistant crops.

Countries work together on climate change under the umbrella of the United Nations Framework Convention on Climate Change (UNFCCC), which has near-universal membership. The ultimate goal of the convention is to "prevent dangerous anthropogenic interference with the climate system". Although the parties to the UNFCCC have agreed that deep cuts in emissions are required and that global warming should be limited to well below 2 °C (3.6 °F) in the Paris Agreement of 2016, the Earth's average surface temperature has already increased by about half this threshold. With current policies and pledges, global warming by the end of the century is expected to reach just over 2 °C to 4 °C, depending on how sensitive the climate is to emissions. The IPCC has stressed the need to keep global warming below 1.5 °C (2.7 °F) compared to pre-industrial levels in order to avoid irreversible impacts. At the current greenhouse gas (GHG) emission rate, the carbon budget for staying below 1.5 °C (2.7 °F) would be exhausted by 2028.

Observed temperature rise

Multiple independently produced instrumental datasets confirm that the 2009–2018 decade was 0.93 ± 0.07 °C (1.67 ± 0.13 °F) warmer than the pre-industrial baseline (1850–1900). Currently, surface temperatures are rising by about 0.2 °C (0.36 °F) per decade. Since 1950, the number of cold days and nights have decreased, and the number of warm days and nights have increased. Historical patterns of warming and cooling, like the Medieval Climate Anomaly and the Little Ice Age, were not as synchronous as current warming, but may have reached temperatures as high as those of the late-20th century in a limited set of regions. The observed rise in temperature and CO₂ concentrations have been so rapid that even abrupt geophysical events that took place in Earth's history do not approach current rates.

Climate proxy records show that natural variations offset the early effects of the Industrial Revolution, so there was little net warming between the 18th century and the mid-19th century, when thermometer records began to provide global coverage. The Intergovernmental Panel on Climate Change (IPCC) has adopted the baseline reference period 1850–1900 as an approximation of pre-industrial global mean surface temperature.

The warming evident in the instrumental temperature record is consistent with a wide range of observations, documented by many independent scientific groups. Although the most common measure of global warming is the increase in the near-surface atmospheric temperature, over 90% of the additional energy in the climate system over the last 50 years has been stored in the ocean, warming it. The remainder of the additional energy has melted ice and warmed the continents and the atmosphere. The ocean heat uptake drives thermal expansion which has contributed to observed sea level rise. Further indicators of climate change include an increase in the frequency and intensity of heavy precipitation, melting of snow and land ice and increased atmospheric humidity. Flora and fauna also portray behaviour consistent with warming, such as the earlier timing of spring events, such as the flowering of plants.

Regional trends

Global warming refers to global averages, with the amount of warming varying by region. Since the pre-industrial period, global average land temperatures have increased almost twice as fast as global average temperatures. This is due to the larger heat capacity of oceans and because oceans lose more heat by evaporation. Patterns of warming are independent of the locations of greenhouse gas emissions because the gases persist long enough to diffuse across the planet; however, localized black carbon deposits on snow and ice do contribute to Arctic warming.

The Northern Hemisphere and North Pole have warmed much faster than the South Pole and Southern Hemisphere. The Northern Hemisphere not only has much more land, but also more snow area and sea ice, because of how the land masses are arranged around the Arctic Ocean. As these surfaces flip from being reflective to dark after the ice has melted, they start absorbing more heat. The Southern Hemisphere already had little sea ice in summer before it started warming. Arctic temperatures have increased and are predicted to continue to increase during this century at over twice the rate of the rest of the world. As the temperature difference between the Arctic and the equator decreases, ocean currents that are driven by that temperature difference, like the Gulf Stream, weaken.

Warmer and colder years

Although record-breaking years attract considerable media attention, individual years are less significant than the overall global surface temperature which are subject to short-term fluctuations that overlie long-term trends. An example of such an episode is the slower rate of surface temperature increase from 1998 to 2012, which was described as the global warming hiatus. Throughout this period, ocean heat storage continued to progress steadily upwards, and in subsequent years, surface temperatures have spiked upwards. The slower pace of warming can be attributed to a combination of natural fluctuations, reduced solar activity, and increased reflection sunlight of by particles from volcanic eruptions.

Physical drivers of recent climate change

By itself, the climate system experiences various cycles which can last for years (such as the El Niño–Southern Oscillation) to decades or centuries. Other changes are caused by an imbalance of energy at the top of the atmosphere: external forcings. These forcings are "external" to the climate system, but not always external to the Earth. Examples of external forcings include changes in the composition of the atmosphere (e.g. increased concentrations of greenhouse gases), solar luminosity, volcanic eruptions, and variations in the Earth's orbit around the Sun.

Attribution of climate change is the effort to scientifically show which mechanisms are responsible for observed changes in Earth's climate. First, known internal climate variability and natural external forcings need to be ruled out. Therefore, a key approach is to use computer modelling of the climate system to determine unique "fingerprints" for all potential causes. By comparing these fingerprints with observed patterns and evolution of climate change, and the observed history of the forcings, the causes of the observed changes can be determined. For example, solar forcing can be ruled out as major cause because its fingerprint is warming in the entire atmosphere, and only the lower atmosphere has warmed as expected for greenhouse gases. The major causes of current climate change are primarily greenhouse gases, and secondarily land use changes, and aerosols and soot.

Greenhouse gases

Greenhouse gases trap heat radiating from the Earth to space. This heat, in the form of infrared radiation, gets absorbed and emitted by these gases in the atmosphere, thus warming the lower atmosphere and the surface. Before the Industrial Revolution, naturally occurring amounts of greenhouse gases caused the air near the surface to be warmer by about 33 °C (59 °F) than it would be in their absence. Without the Earth's atmosphere, the Earth's average temperature would be well below the freezing temperature of water. While water vapour (~50%) and clouds (~25%) are the biggest contributors to the greenhouse effect, they increase as a function of temperature and are therefore considered feedbacks. Increased concentrations of gases such as CO₂ (~20%), ozone and N₂O are external forcing on the other hand. Ozone acts as a greenhouse gas in the lowest layer of the atmosphere, the troposphere. Furthermore, it is highly reactive and interacts with other greenhouse gases and aerosols.

Human activity since the Industrial Revolution, mainly extracting and burning fossil fuels, has increased the amount of greenhouse gases in the atmosphere. This CO₂, methane, tropospheric ozone, CFCs, and nitrous oxide has increased radiative forcing. In 2018, the concentrations of CO₂ and methane had increased by about 45% and 160%, respectively, since pre-industrial times. In 2013, CO₂ readings taken at the world's primary benchmark site in Mauna Loa surpassing 400 ppm for the first time. These levels are much higher than at any time during the last 800,000 years, the period for which reliable data have been collected from ice cores. Less direct geological evidence indicates that CO₂ values have not been this high for millions of years.

Global anthropogenic greenhouse gas emissions in 2018 excluding land use change were equivalent to 52 billion tonnes of carbon dioxide. Of these emissions, 72% was carbon dioxide from fossil fuel burning and industry, 19% was from methane, 6% was from nitrous oxide, and 3% was from fluorinated gases. A further 4 billion tonnes of CO₂ was released as a consequence of land use change, which is primarily due to deforestation. Using life-cycle assessment to estimate emissions relating to final consumption, the dominant sources of 2010 emissions were: food (26–30% of emissions); washing, heating, and lighting (26%); personal transport and freight (20%); and building construction (15%).

The land surface plays a double role in determining GHG concentrations. Agriculture and forestry are both major sources of greenhouse gases, with agricultural emissions being dominated by livestock. Natural responses to human-induced environmental changes, such as nitrogen deposition and climate change, have increased carbon fixation in the soil and photosynthesis, and therefore act as a significant carbon sink for CO₂, more than offsetting these GHG sources. The net result is an estimated removal (sink) of about 6 billion tonnes annually, or about 15% of total CO₂ emissions. The ocean also serves as a significant carbon sink via a two-step process. First, CO₂ dissolves in the surface water. Afterwards, the ocean's overturning circulation distributes it deep into the ocean's interior, where it accumulates over time. Over the last two decades, the wold's oceans have removed between 20 and 30% of emitted CO₂. The strength of both the land and ocean sinks increase as CO₂ levels in the atmosphere rise. In this respect they act as negative feedbacks in global warming.

Land surface change

Humans change the Earth's surface mainly to create more agricultural land. Today agriculture takes up 50% of the world's habitable land, while 37% is forests, and that latter figure continues to decrease, largely due to continued forest loss in the tropics. This deforestation is the most significant aspect of land use change affecting global warming. The main causes are: deforestation through permanent land use change for agricultural products such as beef and palm oil (27%), forestry/forest products (26%), short term agricultural cultivation (24%), and wildfires (23%).

In addition to impacting greenhouse gas concentrations, land use changes affect global warming through a variety of other chemical and physical dynamics as well. Changing the type of vegetation in a region impacts the local temperature by changing how much sunlight gets reflected back into space, called albedo, and how much heat is lost by evaporation. For instance, the change from a dark forest to grassland makes the surface lighter, causing it to reflect more sunlight. Deforestation can also contribute to changing temperatures by affecting the release of aerosols and other chemical compounds that affect clouds; and by changing wind patterns when the land surface has different obstacles. Globally, these effects are estimated to have led to a slight cooling, dominated by an increase in surface albedo. But there is significant geographic variation in how this works. In the tropics the net effect is to produce a significant warming, while at latitudes closer to the poles a loss of albedo leads to an overall cooling effect.

Aerosols and clouds

Solid and liquid particles known as aerosols – from volcanoes, plankton, and human-made pollutants – reflect incoming sunlight, cooling the climate. From 1961 to 1990, a gradual reduction in the amount of sunlight reaching the Earth's surface was observed, a phenomenon popularly known as global dimming, typically attributed to aerosols from biofuel and fossil fuel burning. Aerosol removal by precipitation gives tropospheric aerosols an atmospheric lifetime of only about a week, while stratospheric aerosols can remain in the atmosphere for a few years. Globally, aerosols have been declining since 1990, removing some of the masking of global warming that they had been providing.

In addition to their direct effect by scattering and absorbing solar radiation, aerosols have indirect effects on the Earth's radiation budget. Sulfate aerosols act as cloud condensation nuclei and thus lead to clouds that have more and smaller cloud droplets. These clouds reflect solar radiation more efficiently than clouds with fewer and larger droplets. This effect also causes droplets to be of more uniform size, which reduces the growth of raindrops and makes clouds more reflective to incoming sunlight. Indirect effects of aerosols are the largest uncertainty in radiative forcing.

While aerosols typically limit global warming by reflecting sunlight, black carbon in soot that falls on snow or ice can contribute to global warming. Not only does this increase the absorption of sunlight, it also increases melting and sea level rise. Limiting new black carbon deposits in the Arctic could reduce global warming by 0.2 °C by 2050.

Natural forcings

As the Sun is the Earth's primary energy source, changes in incoming sunlight directly affect the climate system. Solar irradiance has been measured directly by satellites, and indirect measurements are available beginning in the early 1600s. There has been no upward trend in the amount of the Sun's energy reaching the Earth, so it cannot be responsible for the current warming. Physical climate models are also unable to reproduce the rapid warming observed in recent decades when taking into account only variations in solar output and volcanic activity. Another line of evidence for the warming not being due to the Sun is how temperature changes differ at different levels in the Earth's atmosphere. According to basic physical principles, the greenhouse effect produces warming of the lower atmosphere (the troposphere), but cooling of the upper atmosphere (the stratosphere). If solar variations were responsible for the observed warming, warming of both the troposphere and the stratosphere would be expected, but that has not been the case.

Climate change feedback

The response of the climate system to an initial forcing is increased by self-reinforcing feedbacks and reduced by balancing feedbacks. The main balancing feedback to global temperature change is radiative cooling to space as infrared radiation, which increases strongly with increasing temperature. The main reinforcing feedbacks are the water vapour feedback, the ice–albedo feedback, and probably the net effect of clouds. Uncertainty over feedbacks is the major reason why different climate models project different magnitudes of warming for a given amount of emissions.

As air gets warmer, it can hold more moisture. After an initial warming due to emissions of greenhouse gases, the atmosphere will hold more water. As water is a potent greenhouse gas, this further heats the climate: the water vapour feedback. The reduction of snow cover and sea ice in the Arctic reduces the albedo of the Earth's surface. More of the Sun's energy is now absorbed in these regions, contributing to Arctic amplification, which has caused Arctic temperatures to increase at more than twice the rate of the rest of the world. Arctic amplification also causes methane to be released as permafrost melts, which is expected to surpass land use changes as the second strongest anthropogenic source of greenhouse gases by the end of the century.

Cloud cover may change in the future. If cloud cover increases, more sunlight will be reflected back into space, cooling the planet. Simultaneously, the clouds enhance the greenhouse effect, warming the planet. The opposite is true if cloud cover decreases. It depends on the cloud type and location which process is more important. Overall, the net feedback over the industrial era has probably been self-reinforcing.

Roughly half of each year's CO₂ emissions have been absorbed by plants on land and in oceans. Carbon dioxide and an extended growing season have stimulated plant growth making the land carbon cycle a balancing feedback. Climate change also increases droughts and heat waves that inhibit plant growth, which makes it uncertain whether this balancing feedback will persist in the future. Soils contain large quantities of carbon and may release some when they heat up. As more CO₂ and heat are absorbed by the ocean, it is acidifying and ocean circulation can change, changing the rate at which the ocean can absorb atmospheric carbon.

Models, projections and carbon budget

A climate model is a representation of the physical, chemical, and biological processes that affect the climate system. Computer models attempt to reproduce and predict the circulation of the oceans, the annual cycle of the seasons, and the flows of carbon between the land surface and the atmosphere. There are more than two dozen scientific institutions that develop climate models. Models not only project different future temperature with different emissions of greenhouse gases, but also do not fully agree on the strength of different feedbacks on climate sensitivity and the amount of inertia of the system.

Climate models incorporate different external forcings. For different greenhouse gas inputs four RCPs (Representative Concentration Pathways) are used: "a stringent mitigation scenario (RCP2.6), two intermediate scenarios (RCP4.5 and RCP6.0) and one scenario with very high GHG emissions (RCP8.5)". Models also include changes in the Earth's orbit, historical changes in the Sun's activity, and volcanic forcing. RCPs only look at concentrations of greenhouse gases, factoring out uncertainty as to whether the carbon cycle will continue to remove about half of the carbon dioxide from the atmosphere each year. Climate model projections summarized in the report indicated that, during the 21st century, the global surface temperature is likely to rise a further 0.3 to 1.7 °C (0.5 to 3.1 °F) in a moderate scenario, or as much as 2.6 to 4.8 °C (4.7 to 8.6 °F) in an extreme scenario, depending on the rate of future greenhouse gas emissions and on climate feedback effects.

These models are also used to estimate the remaining carbon emissions budget. According to the IPCC, global warming can be kept below 1.5 °C with a two-thirds chance if emissions after 2018 do not exceed 420 or 570 GtCO₂ depending on the choice of the measure of global temperature. This amount corresponds to 10 to 13 years of current emissions. There are high uncertainties about the budget in either direction.

The physical realism of models is tested by examining their ability to simulate contemporary or past climates. Past models have underestimated the rate of Arctic shrinkage and underestimated the rate of precipitation increase. Sea level rise since 1990 was underestimated in older models, but now agrees well with observations. The 2017 United States-published National Climate Assessment notes that "climate models may still be underestimating or missing relevant feedback processes".

A subset of climate models add societal factors to a simple physical climate model. These models simulate how population, economic growth, and energy use affect – and interact with – the physical climate. With this information, these models can produce scenarios of how greenhouse gas emissions may vary in the future. This output is then used as input for physical climate models to generate climate change projections. Emissions scenarios, estimates of changes in future emission levels of greenhouse gases, depend upon uncertain economic, sociological, technological, and natural developments. In some scenarios emissions continue to rise over the century, while others have reduced emissions. Fossil fuel reserves are abundant, and will not limit carbon emissions in the 21st century.

Emission scenarios can be combined with modelling of the carbon cycle to predict how atmospheric concentrations of greenhouse gases might change in the future. According to these combined models, by 2100 the atmospheric concentration of CO₂ could be as low as 380 or as high as 1400 ppm, depending on the Shared Socioeconomic Pathway (SSP) the world takes and the mitigation scenario. The 10th Emissions Gap Report issued by the United Nations Environment Programme (UNEP) predicts that if emissions continue to increase at the same rate as they have in 2010–2020, global temperatures would rise by as much as 4 °C by 2100.

Effects

Physical environment

The environmental effects of global warming are broad and far-reaching. They include effects on the oceans, ice, and weather and may occur gradually or rapidly. Evidence for these effects come from studying climate change in the past, modelling and modern observations. Since the 1950s, droughts and heat waves have appeared simultaneously with increasing frequency. Extremely wet or dry events within the monsoon period have increased in India and East Asia. Various mechanisms have been identified that might explain extreme weather in mid-latitudes from the rapidly warming Arctic, such as the jet stream becoming more erratic. The maximum rainfall and wind speed from hurricanes and typhoons are likely increasing.

Between 1993 and 2017, the global mean sea level rose on average by 3.1 ± 0.3 mm per year, with an acceleration detected as well. Over the 21st century, the IPCC projects that in a very high emissions scenario the sea level could rise by 61–110 cm. The rate of ice loss from glaciers and ice sheets in the Antarctic is a key area of uncertainty since this source could account for 90% of the potential sea level rise: increased ocean warmth is undermining and threatening to unplug Antarctic glacier outlets, potentially resulting in more rapid sea level rise. The retreat of non-polar glaciers also contributes to sea level rise.

Global warming has led to decades of shrinking and thinning of the Arctic sea ice, making it vulnerable to atmospheric anomalies. Projections of declines in Arctic sea ice vary. While ice-free summers are expected to be rare at 1.5 °C (2.7 °F) degrees of warming, they are set to occur once every three to ten years at a warming level of 2.0 °C (3.6 °F), increasing the ice–albedo feedback. Higher atmospheric CO₂ concentrations have led to an increase in dissolved CO₂, which causes ocean acidification. Furthermore, oxygen levels decrease because oxygen is less soluble in warmer water, an effect known as ocean deoxygenation.

Abrupt and long-term impacts

The long-term effects of global warming include further ice melt, ocean warming, sea level rise, and ocean acidification. On the timescale of centuries to millennia, the magnitude of global warming will be determined primarily by anthropogenic CO₂ emissions. This is due to carbon dioxide's very long lifetime in the atmosphere. Carbon dioxide is slowly taking up by the ocean, such that ocean acidification will continue for hundreds to thousands of years. The emissions are estimated to have prolonged the current interglacial period by at least 100,000 years. Because the great mass of glaciers and ice caps depressed the Earth's crust, another long-term effect of ice melt and deglaciation is the gradual rising of landmasses, a process called post-glacial rebound. Sea level rise will continue over many centuries, with an estimated rise of 2.3 metres per degree Celsius (4.2 ft/°F) after 2000 years.

If global warming exceeds 1.5 °C, there is a greater risk of passing through ‘tipping points’, thresholds beyond which certain impacts can no longer be avoided even if temperatures are reduced. Some large-scale changes could occur abruptly, i.e. over a short time period. One potential source of abrupt tipping would be the rapid release of methane and carbon dioxide from permafrost, which would amplify global warming. Another example is the possibility for the Atlantic Meridional Overturning Circulation to slow or shut down, which could trigger cooling in the North Atlantic, Europe, and North America. If multiple temperature and carbon cycle tipping points re-inforce each other, or if there were to be strong threshold behaviour in cloud cover, there could be a global tipping into a hothouse Earth. A 2018 study tried to identify such a planetary threshold for self-reinforcing feedbacks and found that even a 2 °C (3.6 °F) increase in temperature over pre-industrial levels may be enough to trigger such a hothouse Earth scenario.

Biosphere

In terrestrial ecosystems, the earlier arrival of spring, as well as poleward and upward shifts in plant and animal ranges, have been linked with high confidence to recent warming. It is expected that most ecosystems will be affected by higher atmospheric CO₂ levels and higher global temperatures. Global warming has contributed to the expansion of drier climatic zones, such as, probably, the expansion of deserts in the subtropics. Without substantial actions to reduce the rate of global warming, land-based ecosystems risk major shifts in their composition and structure. Overall, it is expected that climate change will result in the extinction of many species and reduced diversity of ecosystems. Rising temperatures push bees to their physiological limits, and could cause the extinction of their populations.

The ocean has heated more slowly than the land, but plants and animals in the ocean have migrated towards the colder poles as fast as or faster than species on land. Just as on land, heat waves in the ocean occur more due to climate change, with harmful effects found on a wide range of organisms such as corals, kelp, and seabirds. Ocean acidification threatens damage to coral reefs, fisheries, protected species, and other natural resources of value to society. Higher oceanic CO₂ may affect the brain and central nervous system of certain fish species, which reduces their ability to hear, smell, and evade predators.

• Some biosphere impacts attributed to climate change
• Repeated coral bleaching has been damaging the Great Barrier Reef and threatens reefs worldwide.
• Unusual drought and higher temperatures produced the historically large 2020 bushfires in Australia.
• Permafrost thaws as the Arctic warms, undermining infrastructure and releasing methane in a positive feedback loop.
• The habitat of the Arctic ecosystem is sea ice, and as it disappears polar bears, walruses, and other residents are dying off.
• In Colorado a greater number of mountain pine beetles survive winters, killing large swaths of forest.

Humans

The effects of climate change on human systems, mostly due to warming and shifts in precipitation, have been detected worldwide. The social impacts of climate change will be uneven across the world. All regions are at risk of experiencing negative impacts, with low-latitude, less developed areas facing the greatest risk. Global warming has likely already increased global economic inequality, and is projected to do so in the future. Regional impacts of climate change are now observable on all continents and across ocean regions. The Arctic, Africa, small islands, and Asian megadeltas are regions that are likely to be especially affected by future climate change. Many risks increase with higher magnitudes of global warming.

Food and water

Crop production will probably be negatively affected in low-latitude countries, while effects at northern latitudes may be positive or negative. Global warming of around 4 °C relative to late 20th century levels could pose a large risk to global and regional food security. The impact of climate change on crop productivity for the four major crops was negative for wheat and maize, and neutral for soy and rice, in the years 1960–2013. Up to an additional 183 million people worldwide, particularly those with lower incomes, are at risk of hunger as a consequence of warming. While increased CO₂ levels help crop growth at lower temperature increases, those crops do become less nutritious. Based on local and indigenous knowledge, climate change is already affecting food security in mountain regions in South America and Asia, and in various drylands, particularly in Africa. Regions dependent on glacier water, regions that are already dry, and small islands are also at increased risk of water stress due to climate change.

Livelihoods, industry, and infrastructure

In small islands and mega deltas, inundation from sea level rise is expected to threaten vital infrastructure and human settlements. This could lead to homelessness in countries with low-lying areas such as Bangladesh, as well as statelessness for populations in island nations, such as the Maldives and Tuvalu. Climate change can be an important driver of migration, both within and between countries.

The majority of severe impacts of climate change are expected in sub-Saharan Africa and South-East Asia, where existing poverty is exacerbated. Current inequalities between men and women, between rich and poor and between people of different ethnicity have been observed to worsen as a consequence of climate variability and climate change. Existing stresses include poverty, political conflicts, and ecosystem degradation. Regions may even become uninhabitable, with humidity and temperatures reaching levels too high for humans to survive. In June 2019, U.N. special rapporteur Philip Alston indicated that global warming could "push more than 120 million more people into poverty by 2030 and will have the most severe impact in poor countries, regions, and the places poor people live and work".

Health and security

Generally, impacts on public health will be more negative than positive. Impacts include the direct effects of extreme weather, leading to injury and loss of life; and indirect effects, such as undernutrition brought on by crop failures. Various infectious diseases are more easily transmitted in a warming climate, such as dengue fever, which affects children most severely, and malaria. Young children are further the most vulnerable to food shortages, and together with older people to extreme heat. Temperature rise has been connected to increased numbers of suicides. Climate change has been linked to an increase in violent conflict by amplifying poverty and economic shocks, which are well-documented drivers of these conflicts. Links have been made between a wide range of violent behaviour including fist fights, violent crimes, civil unrest, and wars.

• Some human impacts attributed to climate change
• Desertification in the Sahel region of Mali threatens to displace populations in areas where rainfall is already sparse.
• Agriculture is being impacted by droughts, rising temperatures, loss of glacial-fed rivers, and extreme weather.
• Tidal flooding in Venice, Miami, and other coastal cities increases as sea levels rise.
• Southern Bangladesh after the passage of Cyclone Sidr. Increased rainfall from storms and rising sea levels can lead to catastrophic flooding.
• Heat waves like the one in Europe in 2019 are becoming more common and extreme.

Responses

Mitigation of and adaptation to climate change are two complementary responses to global warming. Successful adaptation is easier if there are substantial emission reductions. Many of the countries that have contributed least to global greenhouse gas emissions are among the most vulnerable to climate change, which raises questions about justice and fairness with regard to mitigation and adaptation.

Mitigation

Climate change can be mitigated through the reduction of greenhouse gas emissions or the enhancement of the capacity of carbon sinks to absorb greenhouse gases from the atmosphere. Near- and long-term trends in the global energy system are inconsistent with limiting global warming to below 1.5 or 2 °C relative to pre-industrial levels. Pledges made as part of the Paris Agreement would lead to about 3 °C of warming at the end of the 21st century, relative to pre-industrial levels. To keep warming under 1.5 °C, a far-reaching system change on an unprecedented scale is necessary in energy, land, cities, transport, buildings, and industry: but globally the benefits of keeping warming under 2 °C exceed the costs.

Technology

Low-carbon energy technologies such as solar energy, wind energy have seen substantial progress over the last few years, but nuclear energy, and carbon capture and storage have not improved similarly. Renewables are currently the cheapest source of new power generation but require energy storage for a continuous supply. Another approach is the installation of wide-area super grids in order to minimize local fluctuations of wind and solar energy. In addition to the expansion of renewable energy, decarbonisation in the energy sector also requires electrification and building a smarter and more flexible energy grid. The use of bioenergy may bring negative consequences for food security. Further measures in the energy sector include energy conservation and increased energy efficiency and decarbonizing buildings and transport.

On land, emissions reductions can be achieved by preventing deforestation and preventing food waste. Furthermore, certain carbon sink can be enhanced, for example, reforestation. Soils can sequester large quantities of CO₂ and as such better soil management in croplands and grassland is an effective mitigation technology. Many 1.5 °C and 2 °C mitigation scenarios depend heavily on negative emission technologies. However, these technologies are typically not yet mature and may be too expensive for large scale deployment.

Policies and measures

It has been suggested that the most effective and comprehensive policy to reduce carbon emissions is a carbon tax or the closely related emissions trading. Alternative effective policies include a moratorium on burning coal and a phase-out of energy subsidies which promote fossil fuel use, redirecting some to support the transition to clean energy. The development and scaling-up of clean technology, such as cement that produces less CO₂, is critical to achieve sufficient emission reductions for the Paris agreement goals. Individual action on climate change to reduce a person's carbon footprint include: limiting overconsumption, living car-free, forgoing air travel and adopting a plant-based diet. Co-benefits of climate change mitigation may help society and individuals more quickly. For example, policies to reduce greenhouse gas emissions often also limit air pollution, improving public health.

Adaptation

Climate change adaptation is "the adjustment in natural or human systems in response to actual or expected climatic stimuli or their effects, which moderates harm or exploits beneficial opportunities". While some adaptation responses call for trade-offs, others bring synergies and co-benefits. Examples of adaptation are improved coastline protection, better disaster management, and the development of more resistant crops. Increased use of air conditioning allows people to better cope with heat, but also increases energy demand. The adaptation may be planned, either in reaction to or anticipation of global warming, or spontaneous, i.e. without government intervention. Adaptation is especially important in developing countries since they are predicted to bear the brunt of the effects of global warming. The capacity and potential for humans to adapt, called adaptive capacity, is unevenly distributed across different regions and populations, and developing countries generally have less capacity to adapt. The public sector, private sector, and communities are all gaining experience with adaptation, and adaptation is becoming embedded within certain planning processes.

Climate engineering

Geoengineering or climate engineering is the deliberate large-scale modification of the climate to counteract climate change. Techniques fall generally into the categories of solar radiation management and carbon dioxide removal, although various other schemes have been suggested. A study from 2014 investigated the most common climate engineering methods and concluded that they are either ineffective or have potentially severe side effects and cannot be stopped without causing rapid climate change.

Society and culture

Political response

The geopolitics of climate change is complex and was often framed as a prisoners' dilemma, in which all countries benefit from mitigation done by other countries, but individual countries would lose from investing in a transition to a low-carbon economy themselves. Net importers of fossil fuels win economically from transitioning, and net exporters face stranded assets: fossil fuels they cannot sell. Furthermore, the benefits to individual countries in terms of public health and local environmental improvents of coal phase out exceed the costs, potentially eliminating the free-rider problem. The geopolitics may be further complicated by the supply chain of rare earth metals, which are necessary to produce clean technology.

UN Framework Convention

As of 2020 nearly all countries in the world are parties to the United Nations Framework Convention on Climate Change (UNFCCC). The objective of the Convention is to prevent dangerous human interference with the climate system. As stated in the Convention, this requires that greenhouse gas concentrations are stabilized in the atmosphere at a level where ecosystems can adapt naturally to climate change, food production is not threatened, and economic development can be sustained. The Framework Convention was agreed on in 1992, but global emissions have risen since then. Its yearly conferences are the stage of global negotiations.

This mandate was sustained in the 1997 Kyoto Protocol to the Framework Convention. In ratifying the Kyoto Protocol, most developed countries accepted legally binding commitments to limit their emissions. These first-round commitments expired in 2012. United States President George W. Bush rejected the treaty on the basis that "it exempts 80% of the world, including major population centres such as China and India, from compliance, and would cause serious harm to the US economy". During these negotiations, the G77 (a lobbying group in the United Nations representing developing countries) pushed for a mandate requiring developed countries to " the lead" in reducing their emissions. This was justified on the basis that the developed countries' emissions had contributed most to the accumulation of greenhouse gases in the atmosphere, per-capita emissions were still relatively low in developing countries, and the emissions of developing countries would grow to meet their development needs.

In 2009 several UNFCCC Parties produced the Copenhagen Accord, which has been widely portrayed as disappointing because of its low goals, leading poorer nations to reject it. Nations associated with the Accord aimed to limit the future increase in global mean temperature to below 2 °C. In 2015 all UN countries negotiated the Paris Agreement, which aims to keep climate change well below 2 °C. The agreement replaced the Kyoto Protocol. Unlike Kyoto, no binding emission targets are set in the Paris Agreement. Instead, the procedure of regularly setting ever more ambitious goals and reevaluating these goals every five years has been made binding. The Paris Agreement reiterated that developing countries must be financially supported. As of November 2019, 194 states and the European Union have signed the treaty and 186 states and the EU have ratified or acceded to the agreement. In November 2019 the Trump administration notified the UN that it would withdraw the United States from the Paris Agreement in 2020.

Other policy

In 2019, the British Parliament became the first national government in the world to officially declare a climate emergency. Other countries and jurisdictions followed. In November 2019 the European Parliament declared a "climate and environmental emergency", and the European Commission presented its European Green Deal with which they hope to make the EU carbon-neutral in 2050.

While the ozone layer and climate change are considered separate problems, the solution to the former has significantly mitigated global warming. The estimated mitigation of the Montreal Protocol, an international agreement to stop emitting ozone-depleting gases, is estimated to have been more effective than the Kyoto Protocol, which was specifically designed to curb greenhouse gas emissions. It has been argued that the Montreal Protocol, may have done more than any other measure, as of 2017, to mitigate climate change as those substances were also powerful greenhouse gases.

Scientific consensus

In the scientific literature, there is an overwhelming consensus that global surface temperatures have increased in recent decades and that the trend is caused mainly by human-induced emissions of greenhouse gases. No scientific body of national or international standing disagrees with this view. Scientific discussion takes place in journal articles that are peer-reviewed, which scientists subject to assessment every couple of years in the Intergovernmental Panel on Climate Change reports. In 2013, the IPCC Fifth Assessment Report stated that "is extremely likely that human influence has been the dominant cause of the observed warming since the mid-20th century". Their 2018 report expressed the scientific consensus as: "human influence on climate has been the dominant cause of observed warming since the mid-20th century".

Consensus has further developed that some form of action should be taken to protect people against the impacts of climate change, and national science academies have called on world leaders to cut global emissions. In November 2017, in the second warning to humanity, 15,364 scientists from 184 countries stated that "the current trajectory of potentially catastrophic climate change due to rising greenhouse gases from burning fossil fuels, deforestation, and agricultural production – particularly from farming ruminants for meat consumption" is "especially troubling". In 2019, a group of more than 11,000 scientists from 153 countries named climate change an "emergency" that would lead to "untold human suffering" if no big shifts in action takes place. The emergency declaration emphasized that economic growth and population growth "are among the most important drivers of increases in CO₂ emissions from fossil fuel combustion" and that "we need bold and drastic transformations regarding economic and population policies".

Public opinion and disputes

The global warming problem came to international public attention in the late 1980s. Significant regional differences exist in how concerned people are about climate change and how much they understand the issue. In 2010, just a little over half the US population viewed it as a serious concern for either themselves or their families, while 73% of people in Latin America and 74% in developed Asia felt this way. Similarly, in 2015 a median of 54% of respondents considered it "a very serious problem", but Americans and Chinese (whose economies are responsible for the greatest annual CO₂ emissions) were among the least concerned. Worldwide in 2011, people were more likely to attribute global warming to human activities than to natural causes, except in the US where nearly half of the population attributed global warming to natural causes. Public reactions to global warming and concern about its effects have been increasing, with many perceiving it as the worst global threat. In a 2019 CBS poll, 64% of the US population said that climate change is a "crisis" or a "serious problem", with 44% saying human activity was a significant contributor.

Due to confusing media coverage in the early 1990s, issues such as ozone depletion and climate change were often mixed up, affecting public understanding of these issues. Although there are a few areas of linkage, the relationship between the two is weak.

Controversy

From about 1990 onward, American conservative think tanks had begun challenging the legitimacy of global warming as a social problem. They challenged the scientific evidence, argued that global warming would have benefits, warned that concern for global warming was some kind of socialist plot to undermine American capitalism, and asserted that proposed solutions would do more harm than good. Organizations such as the libertarian Competitive Enterprise Institute, as well as conservative commentators, have challenged IPCC climate change scenarios, funded scientists who disagree with the scientific consensus, and provided their own projections of the economic cost of stricter controls.

Global warming has been the subject of controversy, substantially more pronounced in the popular media than in the scientific literature, with disputes regarding the nature, causes, and consequences of global warming. The disputed issues include the causes of increased global average air temperature, especially since the mid-20th century, whether this warming trend is unprecedented or within normal climatic variations, whether humankind has contributed significantly to it, and whether the increase is completely or partially an artifact of poor measurements. Additional disputes concern estimates of climate sensitivity, predictions of additional warming, what the consequences of global warming will be, and what to do about it. One suggestion is that the best individual actions include having fewer children but some disagree with encouraging people to stop having children, saying that children "embody a profound hope for the future", and that more emphasis should be placed on lifestyle choices of the world's wealthy, fossil fuel companies, and government inaction.

In the 20th century and early 2000s some companies, such as ExxonMobil, challenged IPCC climate change scenarios, funded scientists who disagreed with the scientific consensus, and provided their own projections of the economic cost of stricter controls. In general, since the 2010s, global oil companies do not dispute that climate change exists and is caused by the burning of fossil fuels. As of 2019, however, some are lobbying against a carbon tax and plan to increase production of oil and gas, but others are in favour of a carbon tax in exchange for immunity from lawsuits which seek climate change compensation.

Protest and litigation

Protests seeking more ambitious climate action have increased in the 2010s in the form of fossil fuel divestment, worldwide demonstrations, and a school strike for climate. Mass civil disobedience actions by Extinction Rebellion and Ende Gelände have ended in police intervention and large-scale arrests. Litigation is increasingly used as a tool to strengthen climate action, with governments being the biggest target of lawsuits demanding that they become ambitious on climate action or enforce existing laws. Cases against fossil-fuel companies, from activists, shareholders and investors, generally seek compensation for loss and damage.

History of the science

In the seventeenth century it was demonstrated that glass, though transparent to sunlight, obstructs radiant heat, followed by the discovery in the eigtheenth century that non-luminous warm objects emit "obscure" (infrared) heat. In a 1824 memoir summarising research into heat transfer, Joseph Fourier assessed sources heating the globe, and the balancing emission of infrared radiation. He proposed a simple formulation of what was later called the greenhouse effect; transparent atmosphere lets through visible light, which warms the surface. The warmed surface emits infrared radiation, but the atmosphere is relatively opaque to infrared and slows the emission of energy, warming the planet.

Starting in 1859, John Tyndall established that nitrogen and oxygen (99% of dry air) are transparent to infrared, but water vapour and traces of some molecules (significantly methane and carbon dioxide) both absorb infrared and, when warmed, emit infrared radiation. His 1861 paper proposed changing concentrations of these gases could have caused "all the mutations of climate which the researches of geologists reveal" and would explain ice age changes.

Svante Arrhenius noted that water vapour in air continuously varied, but carbon dioxide (CO₂) was determined by long term geological processes. At the end of an ice age, warming from increased CO₂ would increase the amount of water vapour, amplifying its effect in a feedback process. In 1896, he published the first climate model of its kind, showing that halving of CO₂ could have produced the drop in temperature initiating the ice age. Arrhenius calculated the temperature increase expected from doubling CO₂ to be around 5–6 °C (9.0–10.8 °F). Other scientists were initially sceptical and believed the greenhouse effect to be saturated so that adding more CO₂ would make no difference. Experts thought climate would be self-regulating. From 1938 Guy Stewart Callendar published evidence that climate was warming and CO₂ levels increasing, but his calculations met the same objections.

1950s military research found less saturation of the greenhouse effect at high altitudes. Earlier calculations treated the atmosphere as a single layer and used digital computers to model the different layers and found added CO₂ would cause warming. Hans Suess found evidence CO₂ levels had been rising, Roger Revelle showed the oceans would not absorb the increase, and together they helped Charles Keeling to begin a record of continued increase, the Keeling Curve. Revelle, Plass and other scientists alerted media to press for government attention, the dangers of global warming came to the fore at James Hansen's 1988 Congressional testimony. Scientific research on climate change expanded, and the Intergovernmental Panel on Climate Change, set up in 1988 to provide formal advice to the world's governments, has spurred unprecedented levels of exchange between different scientific disciplines.

Terminology

Research in the 1950s suggested that temperatures were increasing, and a 1952 newspaper used the term "climate change". This phrase next appeared in a November 1957 report in The Hammond Times which described Roger Revelle's research into the effects of increasing human-caused CO₂ emissions on the greenhouse effect: "a large scale global warming, with radical climate changes may result". A 1971 MIT report referred to the human impact as "inadvertent climate modification", identifying many possible causes. Both the terms global warming and climate change were used only occasionally until 1975, when Wallace Smith Broecker published a scientific paper on the topic, "Climatic Change: Are We on the Brink of a Pronounced Global Warming?". The phrase began to come into common use, and in 1976 Mikhail Budyko's statement that "a global warming up has started" was widely reported. An influential 1979 National Academy of Sciences study headed by Jule Charney followed Broecker in using global warming to refer to rising surface temperatures, while describing the wider effects of increased CO₂ as climate change.

There were increasing heatwaves and drought problems in the summer of 1988, and NASA climate scientist James Hansen's testimony in the U.S. Senate sparked worldwide interest. He said, "Global warming has reached a level such that we can ascribe with a high degree of confidence a cause and effect relationship between the greenhouse effect and the observed warming." Public attention increased over the summer, and global warming became the dominant popular term, commonly used both by the press and in public discourse. In the 2000s, the term climate change increased in popularity. The term climate change is also used to refer to past and future climate changes that persist for an extended period of time, and includes regional changes as well as global change. The two terms are often used interchangeably.

Various scientists, politicians and news media have adopted the terms climate crisis or a climate emergency to talk about climate change, while using global heating instead of global warming. The policy editor-in-chief of The Guardian explained why they included this language in their editorial guidelines: "We want to ensure that we are being scientifically precise, while also communicating clearly with readers on this very important issue". Oxford Dictionary chose climate emergency as the word of the year 2019 and defines the term as "a situation in which urgent action is required to reduce or halt climate change and avoid potentially irreversible environmental damage resulting from it".

See also

Template:Misplaced Pages books

• Anthropocene – proposed geological time interval for a new period where humans are having significant geological impact
• Global cooling – minority view held by scientists in the 1970s that imminent cooling of the Earth would take place

Notes

1. IPCC AR5 WG1 Summary for Policymakers 2013, p. 4: Warming of the climate system is unequivocal, and since the 1950s, many of the observed changes are unprecedented over decades to millennia. The atmosphere and ocean have warmed, the amounts of snow and ice have diminished, sea level has risen, and the concentrations of greenhouse gases have increased; EPA 2016: The U.S. Global Change Research Program, the National Academy of Sciences, and the Intergovernmental Panel on Climate Change (IPCC) have each independently concluded that warming of the climate system in recent decades is "unequivocal". This conclusion is not drawn from any one source of data but is based on multiple lines of evidence, including three worldwide temperature datasets showing nearly identical warming trends as well as numerous other independent indicators of global warming (e.g. rising sea levels, shrinking Arctic sea ice).
2. IPCC AR5 SYR Glossary 2014, p. 124: Global warming refers to the gradual increase, observed or projected, in global surface temperature, as one of the consequences of radiative forcing caused by anthropogenic emissions.; IPCC SR15 Ch1 2018, p. 51: "Global warming is defined in this report as an increase in combined surface air and sea surface temperatures averaged over the globe and over a 30-year period. Unless otherwise specified, warming is expressed relative to the period 1850–1900, used as an approximation of pre-industrial temperatures in AR5.".
3. Shaftel 2016; Associated Press, 22 September 2015: "The terms global warming and climate change can be used interchangeably. Climate change is more accurate scientifically to describe the various effects of greenhouse gases on the world because it includes extreme weather, storms and changes in rainfall patterns, ocean acidification and sea level.".
4. IPCC AR5 WG1 Ch5 2013, pp. 389, 399–400: "5: Information from Paleoclimate Archives: The PETM was marked by ... global warming of 4 °C to 7 °C ..... Deglacial global warming occurred in two main steps from 17.5 to 14.5 ka and 13.0 to 10.0 ka.
5. IPCC AR5 WG1 Summary for Policymakers 2013, p. 4: Warming of the climate system is unequivocal, and since the 1950s, many of the observed changes are unprecedented over decades to millennia. The atmosphere and ocean have warmed, the amounts of snow and ice have diminished, sea level has risen, and the concentrations of greenhouse gases have increased; IPCC SR15 Ch1 2018, p. 54: The abundant empirical evidence of the unprecedented rate and global scale of impact of human influence on the Earth System (Steffen et al., 2016; Waters et al., 2016) has led many scientists to call for an acknowledgement that the Earth has entered a new geological epoch: the Anthropocene.
6. ^ "Global Annual Mean Surface Air Temperature Change". NASA. Retrieved 23 February 2020..
7. ^ IPCC AR5 SYR Glossary 2014, p. 124.
8. USGCRP Chapter 3 2017 Figure 3.1 panel 2, Figure 3.3 panel 5.
9. ^ IPCC SR15 Ch1 2018, p. 53.
10. Gleick, 7 January 2017; "Scientific Consensus: Earth's Climate is Warming". Climate Change: Vital Signs of the Planet. NASA JPL. Archived from the original on 28 March 2020. Retrieved 29 March 2020. {{cite web}}: Invalid |ref=harv (help)
11. ^ US EPA 2019.
12. Kevin E. Trenberth and John T. Fasullo (5 October 2016). "Insights into Earth's Energy Imbalance from Multiple Sources". Journal of Climate. 29 (20): 7495–7505. Bibcode:2016JCli...29.7495T. doi:10.1175/JCLI-D-16-0339.1. {{cite journal}}: Invalid |ref=harv (help)
13. IPCC AR5 WG2 Technical Summary 2014, pp. 44–46; D'Odorico et al. 2013.
14. National Geographic 2019; NPR 2010.
15. Campbella et al. 2016; National Research Council 2012, pp. 26–27.
16. EPA (19 January 2017). "Climate Impacts on Ecosystems". Archived from the original on 27 January 2018. Retrieved 5 February 2019. {{cite web}}: Invalid |ref=harv (help)
17. ^ Met Office 2016.
18. UNFCCC 1992, Article 2, "Objective".
19. Decision 1/CP.16, paragraph 4, in UNFCCC: Cancun 2010: "deep cuts in global greenhouse gas emissions are required according to science, and as documented in the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, with a view to reducing global greenhouse gas emissions so as to hold the increase in global average temperature below 2 °C above preindustrial levels"; The Guardian, 12 December 2015; Paris Agreement 2015, Article 2, Section 1(a).
20. IPCC SR15 Ch1 2018, p. 51.
21. Climate Action Tracker 2019, p. 1; United Nations Environment Programme 2019, p. 27.
22. IPCC SR15 Summary for Policymakers 2018, p. 7:Future climate-related risks (...) are larger if global warming exceeds 1.5 °C (2.7 °F) before returning to that level by 2100 than if global warming gradually stabilizes at 1.5°C. (...) Some impacts may be long-lasting or irreversible, such as the loss of some ecosystems (high confidence).
23. Mercator Institute 2020; IPCC SR15 Ch2 2018, p. 96: This assessment suggests a remaining budget of about 420 GtCO₂ for a twothirds chance of limiting warming to 1.5°C, and of about 580 GtCO₂ for an even chance (medium confidence).
24. Neukom et al. 2019.
25. "The Oceans Are Heating Up Faster Than Expected". scientific american. Retrieved 3 March 2020.
26. IPCC SR15 Summary for Policymakers 2018, p. 4; WMO 2019, p. 6.
27. IPCC SR15 Ch1 2018, p. 81.
28. IPCC AR5 WG1 Ch2 2013, p. 162.
29. IPCC AR5 WG1 Ch5 2013, p. 386; Neukom et al. 2019.
30. IPCC SR15 Ch1 2018, p. 54.
31. ^ IPCC SR15 Ch1 2018, p. 57: This report adopts the 51-year reference period, 1850–1900 inclusive, assessed as an approximation of pre-industrial levels in AR5 .... Temperatures rose by 0.0 °C–0.2 °C from 1720–1800 to 1850–1900 (Hawkins et al., 2017); Hawkins et al. 2017, p. 1844: "The period after 1800 is influenced by the Dalton Minimum in solar activity and the large eruptions of an unlocated volcano in 1808/09, Tambora (1815; Raible et al. 2016), and several others in the 1820s and 1830s. In addition, greenhouse gas concentrations had already increased slightly by this time .... The 1720–1800 period is most suitable to be defined as preindustrial in physical terms ... The 1850–1900 period is a reasonable pragmatic surrogate for preindustrial global mean temperature."
32. IPCC AR5 WG1 Summary for Policymakers 2013, pp. 4–5: "Global-scale observations from the instrumental era began in the mid-19th century for temperature and other variables ... the period 1880 to 2012 ... multiple independently produced datasets exist."
33. Kennedy et al. 2010, p. S26. Figure 2.5 shows various graphs.
34. "Climate Change: Ocean Heat Content". NOAA. 2018. Archived from the original on 12 February 2019. Retrieved 20 February 2019. {{cite web}}: Invalid |ref=harv (help)
35. IPCC AR5 WG1 Ch3 2013, p. 257: "Ocean warming dominates the global energy change inventory. Warming of the ocean accounts for about 93% of the increase in the Earth's energy inventory between 1971 and 2010 (high confidence), with warming of the upper (0 to 700 m) ocean accounting for about 64% of the total.
36. Cazenave et al. 2014.
37. Kennedy et al. 2010, pp. S26, S59–S60; USGCRP Chapter 1 2017, p. 35.
38. IPCC AR4 WG2 Summary for Policymakers 2007, Part B: "Current knowledge about observed impacts of climate change on the natural and human environment".
39. IPCC AR4 WG2 Ch1 2007, Sec. 1.3.5.1: "Changes in phenology", p. 99.
40. IPCC SRCCL Summary for Policymakers 2019, p. 7.
41. Sutton, Dong & Gregory 2007.
42. United States Environmental Protection Agency 2016, p. 5: "Black carbon that is deposited on snow and ice darkens those surfaces and decreases their reflectivity (albedo). This is known as the snow/ice albedo effect. This effect results in the increased absorption of radiation that accelerates melting."
43. NOAA, 10 July 2011.
44. IPCC AR5 WG1 Ch12 2013, p. 1062; Cohen et al. 2014.
45. NASA, 12 September 2018: "We are seeing a major shift in the circulation in the North Atlantic, likely related to a weakening Atlantic Meridional Overturning Circulation (AMOC)", said Pershing. "One of the side effects of a weaker AMOC is that the Gulf Stream shifts northward and the cold current flowing into the Gulf of Maine gets weaker. This means we get more warmer water pushing into the Gulf."
46. Sévellec & Drijfhout 2018; Mooney 2018.
47. England et al. 2014; Knight et al. 2009.
48. Lindsey 2018.
49. Delworth & Zeng 2012, p. 5; Franzke et al. 2020.
50. National Research Council 2012, p. 9.
51. IPCC AR5 WG1 Ch10 2013, p. 916.
52. Knutson 2017, p. 443; IPCC AR5 WG1 Ch10 2013, pp. 875–876.
53. ^ USGCRP 2009, p. 20.
54. IPCC AR5 WG1 Summary for Policymakers 2013, pp. 13–14.
55. NASA. "The Causes of Climate Change". Climate Change: Vital Signs of the Planet. Archived from the original on 8 May 2019. Retrieved 8 May 2019. {{cite web}}: Invalid |ref=harv (help)
56. IPCC AR4 WG1 Ch1 2007, FAQ1.1: "To emit 240 W m, a surface would have to have a temperature of around −19 °C (−2 °F). This is much colder than the conditions that actually exist at the Earth's surface (the global mean surface temperature is about 14 °C).
57. ACS. "What Is the Greenhouse Effect?". Archived from the original on 26 May 2019. Retrieved 26 May 2019. {{cite web}}: Invalid |ref=harv (help)
58. Schmidt et al. 2010; USGCRP Climate Science Supplement 2014, p. 742.
59. Wang, Shugart & Lerdau 2017.
60. The Guardian, 19 February 2020.
61. WMO 2020, p. 5.
62. BBC, 10 May 2013; Schiermeier 2015.
63. Siegenthaler et al. 2005; Lüthi et al. 2008.
64. BBC, 10 May 2013.
65. Olivier & Peters 2019, p. 14, 16-17.
66. Olivier & Peters 2019, p. 17.
67. Poore & Nemecek 2018.
68. Bajzelj, Allwood & Cullen 2013.
69. ^ IPCC SRCCL Summary for Policymakers 2019, pp. 10–11.
70. Reisinger & Clark 2018.
71. IPCC SROCC Ch5 2019, p. 450
72. Ritchie & Roser 2018.
73. TSC Webmaster 2018.
74. UN FAO 2016, p. 18.
75. Curtis et al. 2018.
76. ^ Seymour & Gibbs 2019.
77. IPCC SRCCL Ch2 2019, p. 172: "The global biophysical cooling alone has been estimated by a larger range of climate models and is −0.10 ± 0.14°C; it ranges from – 0.57°C to +0.06°C ... This cooling is essentially dominated by increases in surface albedo: historical land cover changes have generally led to a dominant brightening of land as discussed in AR5".
78. Haywood 2016; Samset et al. 2018.
79. IPCC AR5 WG1 Ch2 2013, p. 183.
80. He et al. 2018; Storelvmo et al. 2016.
81. Ramanathan & Carmichael 2008.
82. Wild et al. 2005; Storelvmo et al. 2016; Samset et al. 2018.
83. Twomey 1977.
84. Albrecht 1989.
85. USGCRP Chapter 2 2017, p. 78.
86. Ramanathan & Carmichael 2008; RIVM 2016.
87. Sand et al. 2015.
88. ^ USGCRP Chapter 2 2017, p. 78.
89. National Research Council 2008, p. 6.
90. "Is the Sun causing global warming?". Climate Change: Vital Signs of the Planet. Archived from the original on 5 May 2019. Retrieved 10 May 2019. {{cite web}}: Invalid |ref=harv (help)
91. Schmidt, Shindell & Tsigaridis 2014; Fyfe et al. 2016.
92. IPCC AR4 WG1 Ch9 2007, pp. 702–703.
93. IPCC AR4 WG1 Ch9 2007, pp. 702–703; Randel et al. 2009.
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97. Wolff et al. 2015: "the nature and magnitude of these feedbacks are the principal cause of uncertainty in the response of Earth's climate (over multi-decadal and longer periods) to a particular emissions scenario or greenhouse gas concentration pathway."
98. NASA, 28 May 2013.
99. Cohen et al. 2014.
100. Farquharson et al. 2019; NASA, 20 August 2018; The Guardian, 18 June 2019.
101. USGCRP Chapter 2 2017, p. 90.
102. NASA, 16 June 2011: "So far, land plants and the ocean have taken up about 55 percent of the extra carbon people have put into the atmosphere while about 45 percent has stayed in the atmosphere. Eventually, the land and oceans will take up most of the extra carbon dioxide, but as much as 20 percent may remain in the atmosphere for many thousands of years."
103. Scientific American, 23 January 2018: "Climate change's negative effects on plants will likely outweigh any gains from elevated atmospheric carbon dioxide levels"; IPCC SRCCL Ch2 2019, p. 133.
104. Melillo et al. 2017: Our first-order estimate of a warming-induced loss of 190 Pg of soil carbon over the 21st century is equivalent to the past two decades of carbon emissions from fossil fuel burning.
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106. IPCC AR5 SYR Glossary 2014, p. 120.
107. Carbon Brief, 15 January 2018, "What is a climate model?".
108. Carbon Brief, 15 January 2018, "Who does climate modelling around the world?".
109. Stott & Kettleborough 2002.
110. Séférian et al. 2019.
111. IPCC AR5 SYR Summary for Policymakers 2014, Sec. 2.1..
112. Carbon Brief, 15 January 2018, "What are the different types of climate models?".
113. IPCC AR5 WG1 Technical Summary 2013.
114. IPCC AR5 WG1 Technical Summary 2013, p. 57.
115. IPCC SR15 Summary for Policymakers 2018, p. 12.
116. IPCC AR4 WG1 Ch8 2007, Sec. FAQ 8.1.
117. Stroeve et al. 2007; National Geographic, 13 August 2019.
118. Liepert & Previdi 2009.
119. Rahmstorf et al. 2007; Mitchum et al. 2018.
120. USGCRP Chapter 15 2017.
121. Carbon Brief, 15 January 2018, "What are the inputs and outputs for a climate model?"; Carbon Brief, 21 March 2019.
122. IPCC AR4 WG3 Ch3 2007, Section 3.1: Emissions scenarios: Issues related to mitigation in the long term context Archived 23 December 2018 at the Wayback Machine.
123. Riahi et al. 2017; Carbon Brief, 19 April 2018.
124. IPCC TAR WG3 Summary for Policymakers 2001, Introduction, paragraph 6 Archived 11 March 2006 at the Wayback Machine.
125. Matthews et al. 2009; Congressional Research Service 2009, p. 9.
126. Carbon Brief, 19 April 2018; Meinshausen 2019, p. 462.
127. Science Magazine, 26 November 2019.
128. NOAA 2017.
129. Hansen et al. 2016; Smithsonian, 26 June 2016.
130. USGCRP Chapter 15 2017, p. 415.
131. Scientific American, 29 April 2014; Burke & Stott 2017.
132. Francis & Vavrus 2012; Sun, Perlwitz & Hoerling 2016; Carbon Brief, 31 January 2019.
133. USGCRP Chapter 9 2017, p. 260.
134. WCRP Global Sea Level Budget Group 2018.
135. IPCC SROCC Ch4 2019, p. 324: GMSL (global mean sea level, red) will rise between 0.43 m (0.29–0.59 m, likely range) (RCP2.6) and 0.84 m (0.61–1.10 m, likely range) (RCP8.5) by 2100 (medium confidence) relative to 1986–2005.
136. U.S. Geological Survey, 18 June 2018.
137. DeConto & Pollard 2016; NOAA, 1 August 2018.
138. NOAA, 1 August 2018.
139. Zhang et al. 2008.
140. IPCC AR5 WG1 Ch11 2013, p. 995; Wang & Overland 2009.
141. IPCC SROCC Summary for Policymakers 2019, p. 18.
142. Pistone, Eisenman & Ramanathan 2019.
143. Doney et al. 2009.
144. Deutsch et al. 2011.
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146. IPCC AR5 WG1 Ch12 2013, p. 1112.
147. Crucifix 2016
148. McGuire 2010.
149. Smith et al. 2009; Levermann et al. 2013.
150. IPCC SR15 Ch3 2018, p. 283.
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152. Clark et al. 2008; BBC, 22 February 2013.
153. ScienceDaily, 20 December 2004; Liu et al. 2017.
154. Lenton et al. 2019.
155. Phys.org, 6 August 2018; Steffen et al. 2018; The Guardian, 7 August 2018.
156. IPCC AR4 SYR 2007, Section 1: Observed changes in climate and their effects Archived 23 December 2018 at the Wayback Machine.
157. IPCC AR4 WG2 Ch4 2007, Executive Summary Archived 27 June 2019 at the Wayback Machine, p. 213.
158. IPCC SRCCL Summary for Policymakers 2019, p. 7; Zeng & Yoon 2009.
159. The Washington Post, 30 August 2018.
160. Urban 2015.
161. ScienceDaily, 28 June 2018.
162. Poloczanska et al. 2013.
163. Smale et al. 2019.
164. UNEP 2010, pp. 4–8.
165. ScienceDaily, 21 January 2012.
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Special Report: Climate change and Land

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Books, reports and legal documents

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• Climate Action Tracker (2019). Warming projections global update, December 2019 (PDF) (Report). {{cite report}}: Invalid |ref=harv (help)
• Douglas, David C.; Atwood, Todd C. (2017), Butterworth, Andy (ed.), "Uncertainties in Forecasting the Response of Polar Bears to Global Climate Change", Marine Mammal Welfare: Human Induced Change in the Marine Environment and its Impacts on Marine Mammal Welfare, Animal Welfare, Springer International Publishing, pp. 463–473, doi:10.1007/978-3-319-46994-2_25, ISBN 978-3-319-46994-2, retrieved 12 April 2020</ref>
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• Academia Brasileira de Ciéncias (Brazil); Royal Society of Canada; Chinese Academy of Sciences; Académie des Sciences (France); Deutsche Akademie der Naturforscher Leopoldina (Germany); Indian National Science Academy; Accademia Nazionale dei Lincei (Italy); Science Council of Japan, Academia Mexicana de Ciencias; Russian Academy of Sciences; Royal Society (United Kingdom); National Academy of Sciences (United States of America) (2005). "Joint science academies' statement: Global response to climate change" (PDF). Archived from the original (PDF) on 9 September 2013. Retrieved 6 January 2014.
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• Müller, Benito (February 2010). Copenhagen 2009: Failure or final wake-up call for our leaders? EV 49 (PDF). Oxford Institute for Energy Studies. p. i. ISBN 978-1-907555-04-6. Archived (PDF) from the original on 10 July 2017. Retrieved 18 May 2010. {{cite book}}: Invalid |ref=harv (help)
• National Academies Of Sciences, Engineering (2019). Negative Emissions Technologies and Reliable Sequestration: A Research Agenda. Washington, D.C.: National Academies of Sciences, Engineering, and Medicine. doi:10.17226/25259. ISBN 978-0-309-48452-7. PMID 31120708.
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• National Research Council (2012). Climate Change: Evidence, Impacts, and Choices (PDF) (Report). Archived (PDF) from the original on 20 February 2013. Retrieved 9 September 2017. {{cite report}}: Invalid |ref=harv (help)
• Newell, Peter (14 December 2006). Climate for Change: Non-State Actors and the Global Politics of the Greenhouse. Vol. 109. Cambridge University Press. pp. 75–76. Bibcode:2001AgFM..109...75B. doi:10.1016/S0168-1923(01)00246-5. ISBN 978-0-521-02123-4. Retrieved 30 July 2018. {{cite book}}: |journal= ignored (help); Invalid |ref=harv (help)
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• Oreskes, Naomi (2007). "The scientific consensus on climate change: How do we know we're not wrong?". In DiMento, Joseph F. C.; Doughman, Pamela M. (eds.). Climate Change: What It Means for Us, Our Children, and Our Grandchildren. The MIT Press. ISBN 978-0-262-54193-0. {{cite book}}: Invalid |ref=harv (help)
• Oreskes, Naomi; Conway, Erik (25 May 2010). Merchants of Doubt: How a Handful of Scientists Obscured the Truth on Issues from Tobacco Smoke to Global Warming (first ed.). Bloomsbury Press. ISBN 978-1-59691-610-4. {{cite book}}: Invalid |ref=harv (help)
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Non-technical sources

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External links

• Resources in your library
• Resources in other libraries

• Official list of United Nations Framework Convention on Climate Change members

Research

• NASA Goddard Institute for Space Studies – Global change research
• Climate Change at the National Academies – repository for reports
• Met Office: Climate Guide – UK National Weather Service
• Educational Global Climate Modelling (EdGCM) – research-quality climate change simulator

Educational

• NRDC Guide: Global Warming 101
• NASA: Climate change: How do we know?
• Global Climate Change Indicators – NOAA
• Result of total melting of Polar regions on World – (National Geographic Society; 2013)

• Global warming
• Climate change
• Climate history
• Climate forcing
• Future problems
• Global environmental issues
• Words coined in the 1950s