Carbon Dioxide and Climate: A Scientific Assessment | |
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Created | 1979 |
Commissioned by | National Academy of Sciences |
Author(s) |
The Charney Report, formally titled Carbon Dioxide and Climate: A Scientific Assessment, is an American scientific report published in 1979 that predicts global warming due to greenhouse gas emissions from human use of fossil fuels.
When early climate models predicted a rise in average surface temperatures, the White House asked the president of the National Academy of Sciences to assess their scientific robustness. Meteorologist Jule Charney was charged with this task and assembled eight renowned climate researchers.
They concluded that the model projections, particularly those of Syukuro Manabe and James E. Hansen, were consistent with scientific knowledge of the physical processes governing the climate system and indicated that humanity was changing the climate through the greenhouse effect. Despite advances in scientific knowledge, their estimated equilibrium climate sensitivity of 3 °C (±1.5 °C) has remained largely unchallenged - with only minor refinements - over the ensuing forty years.
The publication of the Charney Report is considered a milestone in the history of understanding climate change.
The mechanism of the greenhouse effect and the role of carbon dioxide (CO2) as a greenhouse gas, particularly as emitted by humans by burning fossil fuels, have been known since the 19th century. By the mid-20th century, an increasing number of researchers predicted that anthropogenic greenhouse gas emissions would cause an increase in the average surface temperature of the atmosphere. In the 1950s, the work of Roger Revelle and Hans Suess established that the ocean was a smaller carbon sink than previously thought. In the following decade, the first results of Charles Keeling's measurements showed an increase in the atmospheric concentration of CO2 (the Keeling curve). [1] [2] [3]
In 1975, Wallace Broecker popularized the term "global warming" in a Science article predicting unprecedented temperatures in the 21st century, based on the first digital climate models that appeared in the 1960s. [4] [1] [2] Two years later, the National Academy of Sciences issued a widely publicized report, Energy and Climate, warning of warming in the 21st century that could reach an average of 6 °C by the end of the 22nd century due to fossil fuel use, and calling for more scientific research to reduce uncertainties. [5] [6] [7] [8]
In the 1970s, the scientific consensus recognized humanity's ability to affect the climate, and the scientific community increasingly focused on the possibility of global warming. However, there was no clear consensus on the warming, which was then imperceptible. The hypothesis of global cooling due to anthropogenic aerosol emissions was also circulating, including in the media, where Reid Bryson popularized it for the public. [3] [9] [5]
Meanwhile, scientific climate research coincided with the rise of environmentalism - societal concern about human impact on the environment, especially in the United States. [2] [10] The 1970s also saw global droughts that led to famine and skyrocketing food prices, underscoring the importance of climate to agriculture. The decade was marked by the first oil shock, which led U.S. President Jimmy Carter to consider increasing domestic production of fossil fuels and to create the Department of Energy. [2] [5] [11]
In 1977, the United States Department of Energy prepared a CO2 research program and requested a report from the JASON Committee, a group of scientists advising the Department of Defense. Although the JASON members were not climatologists, they studied the effect of CO2 emissions on climate using a model they had developed to estimate equilibrium climate sensitivity or the amount of warming caused by a doubling of atmospheric CO2 concentrations relative to pre-industrial levels. They concluded that climate sensitivity is 2.4 °C, which could lead to negative economic and social consequences. This result was consistent with earlier estimates from general circulation models, and as science historians Naomi Oreskes and Erik M. Conway note, the political connections of the JASON committee members gave the report considerable authority. [2] [11] [12]
One of the report's authors, Gordon MacDonald, along with environmental activist Rafe Pomerance, met with Jimmy Carter's science advisor and director of the Office of Science and Technology Policy, Frank Press, to present their findings. [13] [14] On May 22, 1979, Press wrote to National Academy of Sciences President Philip Handler requesting a study to determine the scientific reliability of climate models. [13] [11]
Handler asked Jule Charney, a renowned meteorologist and modeler at the Massachusetts Institute of Technology (MIT), to chair a working group on the issue. Charney brought together eight distinguished scientists to form the Ad Hoc Study Group on Carbon Dioxide and Climate: Akio Arakawa, D. James Baker, Bert Bolin, Robert E. Dickinson, Richard M. Goody, Cecil Leith , Henry Stommel, and Carl Wunsch. [2] [11] [15]
On July 23, 1979, the nine scientists, accompanied by their families, met in Woods Hole on the Massachusetts coast, where the National Academy of Sciences has a conference center. Also present as observers were members of various federal agencies and staff of the National Research Council, who oversaw the report development. [13] After working together in Woods Hole from July 23 to July 27, and continuing to exchange ideas in the following weeks, [16] the group produced a 22-page report entitled Carbon Dioxide and Climate: A Scientific Assessment.
Jule Charney decided to evaluate not only the JASON committee's model but also the more advanced three-dimensional general circulation models of Syukuro Manabe (from NOAA's Geophysical Fluid Dynamics Laboratory) and James E. Hansen (from NASA's Goddard Institute for Space Studies ). The first model estimated equilibrium climate sensitivity between 2 °C and 3 °C, while the second model estimated values close to 4 °C. Both researchers were invited to present how their models worked, and the difference in their estimates was largely due to different approaches to modeling certain physical processes, such as the positive feedback loop triggered by melting ice (decreasing albedo). [5] [11] [13] [17]
All models, by definition, simplify the complex physics of climate, and uncertainties remain, for example, about the dominant feedback effect of clouds (depending on their altitude) or the interactions between the ocean surface layer and the thermocline. The researchers, led by Jule Charney, therefore examined all possible negative feedback loops that could counteract the greenhouse warming predicted by the models in the presence of increased atmospheric CO2 concentrations. As they wrote in the report: "[We] have concluded that the oversimplifications and inaccuracies in the models are not likely to have vitiated the principal conclusion that there will be appreciable warming." [18] The document thus concludes with an estimated equilibrium climate sensitivity of 3 °C, with a margin of error of ±1.5 °C (i.e., from 1.5 °C to 4.5 °C). [11] [13] [19] The authors also point out - and this prediction later proved accurate - that the ocean's heat absorption capacity could delay noticeable atmospheric warming by several decades for a given level of CO2 emissions: [20] [21] "We may not be given a warning until the CO2 loading is such that an appreciable climate change is inevitable." [18]
The conclusions of the Charney Report have since been confirmed by new instrumental data sets, comparisons with past climates, and more sophisticated computer models. [20] [21] [22] In particular, the range of error estimated in the report for equilibrium climate sensitivity (1.5 °C to 4.5 °C) is consistent with that evaluated in the IPCC Fifth Assessment Report, with the central value (3 °C) consistent with the IPCC Sixth Assessment Report (2021), which concluded with a narrower range of error. [22] [23]
The Charney Report did not introduce new scientific knowledge about climate change, but it did reaffirm the scientific robustness of climate models, based on a solid understanding of physical processes, and demonstrated a growing scientific consensus about future warming. [10] [13] [20] [21] [24] However, knowledge about climate change remained theoretical, and not all researchers were convinced by the computer models. The first tangible evidence of warming came a decade later, with Jean Jouzel and Claude Lorius' reconstructions of past climates using Antarctic ice cores. [5] [3] [25]
The Charney Report, published in 1979, was covered by Science under the headline CO2 in Climate: Doomsday Predictions Have No Faults. [14] [26] The report circulated in scientific and business circles but did not lead to political action to reduce greenhouse gas emissions. [9] [13] [20]
The year 1979 is considered a landmark in the history of knowledge about human-caused climate change because of the publication of the report and the simultaneous organization of the first World Climate Conference by the World Meteorological Organization (WMO). It preceded by nine years the creation of the Intergovernmental Panel on Climate Change (IPCC), an initiative led by Bert Bolin, one of the authors of the Charney Report. [9] [27] [28] [29] [30]
The scientific community has been investigating the causes of climate change for decades. After thousands of studies, it came to a consensus, where it is "unequivocal that human influence has warmed the atmosphere, ocean and land since pre-industrial times." This consensus is supported by around 200 scientific organizations worldwide, The dominant role in this climate change has been played by the direct emissions of carbon dioxide from the burning of fossil fuels. Indirect CO2 emissions from land use change, and the emissions of methane, nitrous oxide and other greenhouse gases play major supporting roles.
Global warming potential (GWP) is an index to measure how much infrared thermal radiation a greenhouse gas would absorb over a given time frame after it has been added to the atmosphere. The GWP makes different greenhouse gases comparable with regard to their "effectiveness in causing radiative forcing". It is expressed as a multiple of the radiation that would be absorbed by the same mass of added carbon dioxide, which is taken as a reference gas. Therefore, the GWP has a value of 1 for CO2. For other gases it depends on how strongly the gas absorbs infrared thermal radiation, how quickly the gas leaves the atmosphere, and the time frame being considered.
Global cooling was a conjecture, especially during the 1970s, of imminent cooling of the Earth culminating in a period of extensive glaciation, due to the cooling effects of aerosols or orbital forcing. Some press reports in the 1970s speculated about continued cooling; these did not accurately reflect the scientific literature of the time, which was generally more concerned with warming from an enhanced greenhouse effect.
There is a nearly unanimous scientific consensus that the Earth has been consistently warming since the start of the Industrial Revolution, that the rate of recent warming is largely unprecedented, and that this warming is mainly the result of a rapid increase in atmospheric carbon dioxide (CO2) caused by human activities. The human activities causing this warming include fossil fuel combustion, cement production, and land use changes such as deforestation, with a significant supporting role from the other greenhouse gases such as methane and nitrous oxide. This human role in climate change is considered "unequivocal" and "incontrovertible".
Radiative forcing is a concept used to quantify a change to the balance of energy flowing through a planetary atmosphere. Various factors contribute to this change in energy balance, such as concentrations of greenhouse gases and aerosols, and changes in surface albedo and solar irradiance. In more technical terms, it is defined as "the change in the net, downward minus upward, radiative flux due to a change in an external driver of climate change." These external drivers are distinguished from feedbacks and variability that are internal to the climate system, and that further influence the direction and magnitude of imbalance. Radiative forcing on Earth is meaningfully evaluated at the tropopause and at the top of the stratosphere. It is quantified in units of watts per square meter, and often summarized as an average over the total surface area of the globe.
World Climate Report, a newsletter edited by Patrick Michaels, was produced by the Greening Earth Society, a non-profit organization created by the Western Fuels Association.
Climate sensitivity is a key measure in climate science and describes how much Earth's surface will warm for a doubling in the atmospheric carbon dioxide (CO2) concentration. Its formal definition is: "The change in the surface temperature in response to a change in the atmospheric carbon dioxide (CO2) concentration or other radiative forcing." This concept helps scientists understand the extent and magnitude of the effects of climate change.
Greenhouse gas (GHG) emissions from human activities intensify the greenhouse effect. This contributes to climate change. Carbon dioxide, from burning fossil fuels such as coal, oil, and natural gas, is one of the most important factors in causing climate change. The largest emitters are China followed by the United States. The United States has higher emissions per capita. The main producers fueling the emissions globally are large oil and gas companies. Emissions from human activities have increased atmospheric carbon dioxide by about 50% over pre-industrial levels. The growing levels of emissions have varied, but have been consistent among all greenhouse gases. Emissions in the 2010s averaged 56 billion tons a year, higher than any decade before. Total cumulative emissions from 1870 to 2022 were 703 GtC, of which 484±20 GtC from fossil fuels and industry, and 219±60 GtC from land use change. Land-use change, such as deforestation, caused about 31% of cumulative emissions over 1870–2022, coal 32%, oil 24%, and gas 10%.
Greenhouse gases (GHGs) are the gases in the atmosphere that raise the surface temperature of planets such as the Earth. What distinguishes them from other gases is that they absorb the wavelengths of radiation that a planet emits, resulting in the greenhouse effect. The Earth is warmed by sunlight, causing its surface to radiate heat, which is then mostly absorbed by greenhouse gases. Without greenhouse gases in the atmosphere, the average temperature of Earth's surface would be about −18 °C (0 °F), rather than the present average of 15 °C (59 °F).
The history of the scientific discovery of climate change began in the early 19th century when ice ages and other natural changes in paleoclimate were first suspected and the natural greenhouse effect was first identified. In the late 19th century, scientists first argued that human emissions of greenhouse gases could change Earth's energy balance and climate. The existence of the greenhouse effect, while not named as such, was proposed as early as 1824 by Joseph Fourier. The argument and the evidence were further strengthened by Claude Pouillet in 1827 and 1838. In 1856 Eunice Newton Foote demonstrated that the warming effect of the sun is greater for air with water vapour than for dry air, and the effect is even greater with carbon dioxide.
Climate change feedbacks are natural processes that impact how much global temperatures will increase for a given amount of greenhouse gas emissions. Positive feedbacks amplify global warming while negative feedbacks diminish it. Feedbacks influence both the amount of greenhouse gases in the atmosphere and the amount of temperature change that happens in response. While emissions are the forcing that causes climate change, feedbacks combine to control climate sensitivity to that forcing.
A climate change scenario is a hypothetical future based on a "set of key driving forces". Scenarios explore the long-term effectiveness of mitigation and adaptation. Scenarios help to understand what the future may hold. They can show which decisions will have the most meaningful effects on mitigation and adaptation.
Representative Concentration Pathways (RCP) are climate change scenarios to project future greenhouse gas concentrations. These pathways describe future greenhouse gas concentrations and have been formally adopted by the IPCC. The pathways describe different climate change scenarios, all of which were considered possible depending on the amount of greenhouse gases (GHG) emitted in the years to come. The four RCPs – originally RCP2.6, RCP4.5, RCP6, and RCP8.5 – are labelled after the expected changes in radiative forcing from the year 1750 to the year 2100. The IPCC Fifth Assessment Report (AR5) began to use these four pathways for climate modeling and research in 2014. The higher values mean higher greenhouse gas emissions and therefore higher global surface temperatures and more pronounced effects of climate change. The lower RCP values, on the other hand, are more desirable for humans but would require more stringent climate change mitigation efforts to achieve them.
Climate inertia or climate change inertia is the phenomenon by which a planet's climate system shows a resistance or slowness to deviate away from a given dynamic state. It can accompany stability and other effects of feedback within complex systems, and includes the inertia exhibited by physical movements of matter and exchanges of energy. The term is a colloquialism used to encompass and loosely describe a set of interactions that extend the timescales around climate sensitivity. Inertia has been associated with the drivers of, and the responses to, climate change.
The Special Report on Global Warming of 1.5 °C (SR15) was published by the Intergovernmental Panel on Climate Change (IPCC) on 8 October 2018. The report, approved in Incheon, South Korea, includes over 6,000 scientific references, and was prepared by 91 authors from 40 countries. In December 2015, the 2015 United Nations Climate Change Conference called for the report. The report was delivered at the United Nations' 48th session of the IPCC to "deliver the authoritative, scientific guide for governments" to deal with climate change. Its key finding is that meeting a 1.5 °C (2.7 °F) target is possible but would require "deep emissions reductions" and "rapid, far-reaching and unprecedented changes in all aspects of society". Furthermore, the report finds that "limiting global warming to 1.5 °C compared with 2 °C would reduce challenging impacts on ecosystems, human health and well-being" and that a 2 °C temperature increase would exacerbate extreme weather, rising sea levels and diminishing Arctic sea ice, coral bleaching, and loss of ecosystems, among other impacts.
The Sixth Assessment Report (AR6) of the United Nations (UN) Intergovernmental Panel on Climate Change (IPCC) is the sixth in a series of reports which assess the available scientific information on climate change. Three Working Groups covered the following topics: The Physical Science Basis (WGI); Impacts, Adaptation and Vulnerability (WGII); Mitigation of Climate Change (WGIII). Of these, the first study was published in 2021, the second report February 2022, and the third in April 2022. The final synthesis report was finished in March 2023. It includes a summary for policymakers and was the basis for the 2023 United Nations Climate Change Conference (COP28) in Dubai.