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|The Discovery of Global Warming January 2017|
It is an epic story: the struggle of thousands of men and women over the course of a century for very high stakes. For some, the work required actual physical courage, a risk to life and limb in icy wastes or on the high seas. The rest needed more subtle forms of courage. They gambled decades of arduous effort on the chance of a useful discovery, and staked their reputations on what they claimed to have found. Even as they stretched their minds to the limit on intellectual problems that often proved insoluble, their attention was diverted into grueling administrative struggles to win minimal support for the great work. A few took the battle into the public arena, often getting more blame than praise; most labored to the end of their lives in obscurity. In the end they did win their goal, which was simply knowledge.
The scientists who labored to understand Earth's climate discovered that many factors influence it. Everything from volcanoes to factories shape our winds and rains. The scientific research itself was shaped by many influences, from popular misconceptions to government funding, all happening at once. A traditional history would try to squeeze the story into a linear text, one event following another like beads on a string. Inevitably some parts are left out. Yet for this sort of subject we need total history, including all the players — mathematicians and biologists, lab technicians and government bureaucrats, industrialists and politicians, newspaper reporters and the ordinary citizen. This Web site is an experiment in a new way to tell a historical story. Think of the site as an object like a sculpture or a building. You walk around, looking from this angle and that. In your head you are putting together a rounded representation, even if you don't take the time to inspect every cranny. That is the way we usually learn about anything complex.
You can start with the following 10-minute overview. Or skip down to advice on using this site. This and all other files are available in a printable format (but you'll miss the hyperlinks and the most recent updates).
The story in a nutshell: Like most histories, this one begins far back. People had long suspected that human activity could change the local climate. For example, ancient Greeks and 19th-century Americans debated how cutting down forests might bring more rainfall to a region, or perhaps less. But greater shifts of climate happened all by themselves. The discovery in the mid 19th century that there had been ice ages in the distant past proved that climate could change radically over much of the globe, a change vastly beyond anything mere humans seemed able to cause. So what did cause global climate change — was it variations in the heat of the Sun? Volcanoes erupting clouds of smoke? The raising and lowering of mountain ranges, which diverted wind patterns and ocean currents? Or could it be changes in the composition of the air itself? In 1824 a French scientist had explained that Earth's temperature would be much lower if the planet lacked an atmosphere, and in 1859 an English scientist discovered that the chief gases that trapped heat were water vapor and carbon dioxide (CO2).
In 1896 the Swedish scientist Svante Arrhenius published a new idea. By burning fossil fuels such as coal, thus adding CO2 to Earth's atmosphere, humanity would raise the planet's average temperature. This "greenhouse effect," as it later came to be called, was only one of many speculations about climate change, and not the most plausible. The few scientists who paid attention to Arrhenius used clumsy experiments and rough approximations to argue that our emissions could not change the planet. Most people thought it was already obvious that puny humanity could never affect the vast global climate cycles, which were governed by a benign "balance of nature."
In the 1930s, measurements showed that the United States and North Atlantic region had warmed significantly during the previous half-century. Scientists supposed this was just a phase of some mild natural cycle, probably regional, with unknown causes. Only one lone voice, the English steam engineer and amateur scientist Guy Stewart Callendar, published arguments that greenhouse warming was underway. If so, he and most others thought it would be beneficial.
In the 1950s, Callendar's claims provoked a few scientists to look into the question with far better techniques and calculations than earlier generations could have deployed. This research was made possible by a sharp increase of government funding, especially from military agencies that wanted to know more about the weather and geophysics in general. Not only might such knowledge be crucial in future battles, but scientific progress could bring a nation prestige in the Cold War competition. The new studies showed that, contrary to earlier crude assumptions, CO2 might indeed build up in the atmosphere and bring warming. In 1960 painstaking measurements of the level of the gas in the atmosphere by Charles Keeling, a young scientist with an obsession for accuracy, drove home the point. The level was in fact rising year by year.
During the next decade a few scientists worked up simple mathematical models of the planet's climate system and turned up feedbacks that could make the system surprisingly sensitive. Others figured out ingenious ways to retrieve past temperatures by studying ancient pollen and fossil shells. It appeared that grave climate change could happen, and in the past had happened, within as little as a century or two. This finding was reinforced by more elaborate models of the general circulation of the atmosphere, an offshoot of a government-funded effort to use the new digital computers to predict (and perhaps even deliberately change) the weather. Calculations made in the late 1960s suggested that in the next century, as CO2 built up in the atmosphere, average temperatures would rise a few degrees. But the models were preliminary, and the 21st century seemed far away.
In the early 1970s, the rise of environmentalism raised public doubts about the benefits of any human activity for the planet. Curiosity about climate change turned into anxious concern. A few degrees of warming no longer sounded benign, and as scientists looked into possible impacts they noticed alarming possibilities of rising sea levels and possible damage to agriculture.
Meanwhile a few scientists pointed out that human activity was putting not only CO2 but ever more dust and smog particles into the atmosphere, where they could block sunlight and cool the world. Analysis of Northern Hemisphere weather statistics showed that a cooling trend had begun in the 1940s; was pollution the cause? (Decades later, scientists would confirm that soaring industrial pollution had in fact contributed to temporary Northern Hemisphere cooling.) The public media were confused, sometimes predicting a balmy globe with coastal areas flooded as the ice caps melted, sometimes foreboding a catastrophic new ice age, sometimes quoting expert assurances that nothing much would change. Study panels of scientists, first in the U.S. and then internationally, began to warn that one or another kind of future climate change might pose a severe threat. The main thing scientists agreed on was that they scarcely understood the climate system. They only policy action they recommended was to fund more research to find out what might really happen. Research activity did accelerate using state-of-the-art computers, international programs to assemble weather data, and adventurous expeditions across oceans and ice caps to gather information on past climates.
Most scientists thought a disastrous cooling was unlikely, if only because dust and smog fall out of the atmosphere in weeks, whereas CO2 would linger for centuries. Computer models, improving at the breakneck pace of computing in general, consistently showed warming. With worries about climate change rising, in 1979 the U.S. National Academy of Sciences convened a committee of experts to hash out what could reliably be said. They reached a consensus that when CO2 reached double the pre-industrial level, sometime in the following century, the planet would probably warm up by about 3°C (5.4°F), plus or minus a degree or two.
Earlier scientists had sought a single master-key to climate, but now they were coming to understand that climate is an intricate system responding to a great many influences. Volcanic eruptions and solar variations were still plausible causes of change, and some argued these would swamp any effects of human activities. Even subtle changes in the Earth's orbit could make a difference. To the surprise of many, studies of ancient climates showed that astronomical cycles had partly set the timing of the ice ages. Apparently the climate was so delicately balanced that almost any small perturbation might set off a large shift. According to the new "chaos" theories, in a complex system a shift might happen suddenly. Support for the idea came from ice cores arduously drilled from the Greenland ice sheet. They showed large and disconcertingly abrupt temperature jumps in the past, on a scale not of centuries but decades.
The improved computer models also began to suggest how such jumps could happen, for example through a change in the circulation of ocean currents. Experts now predicted that global warming could bring not only rising sea levels but unprecedented droughts, storm floods, and other disasters. A few politicians began to suspect there might be a public issue here. However, the modelers had to make many arbitrary assumptions about clouds and the like, and reputable scientists disputed the reliability of the results. Others pointed out how little was known about the way living ecosystems interact with climate and the atmosphere. They argued, for example, over how much CO2 humanity might be adding to the atmosphere through deforestation. One thing the scientists agreed on was the need for still larger and more coherent research programs. But the research remained disorganized, and funding grew only in irregular surges.
One unexpected discovery was that the levels of other "greenhouse gases" such as methane and chlorofluorocarbons were rising explosively. Suddenly scientists found that global warming could come twice as fast as expected — in their children's lifetimes or even their own. Gathering at a 1985 conference in Austria, climate experts from 29 nations agreed to call on the world's governments to consider forging international agreements to restrict greenhouse gas emissions. Policy makers ignored the advice, and the public scarcely noticed.
By the late 1970s global temperatures had begun to rise again. Some climate scientists predicted that an unprecedented global warming would become apparent around the year 2000. Their worries finally caught wide public attention in the summer of 1988, the hottest on record till then. Computer modeler James Hansen made headlines when he told a Congressional hearing and journalists that greenhouse warming was almost certainly underway. And a major international meeting of scientists in Toronto called on governments to undertake active steps to cut greenhouse gas emissions.
The response was vehement. Corporations and individuals who opposed all government regulation began to spend millions of dollars on lobbying, advertising, and "reports" that mimicked scientific publications, striving to convince the public that there was no problem at all. Environmental groups, less wealthy but more enthusiastic, helped politicize the issue with urgent cries of alarm. The many scientific uncertainties, and the sheer complexity of climate, made room for limitless debate over what actions, if any, governments should take.
In a field opened up by a handful of individuals who had taken a year or so off from their other work, now hundreds of scientists dedicated their careers, backed up by thousands of assistants and technicians. Some programs were huge, mobilizing cooperation among a dozen or more nations to provide data from weather stations, research ships, and (by far the most expensive) satellites to monitor temperatures, clouds, ocean currents, ice sheets and more. Their conclusions became increasingly reliable.
Was the global temperature rise due to an increase in the Sun's activity? That had seemed plausible to some, since for decades solar activity had been increasing in parallel with temperature. However, nobody could come up with a good explanation for how the slight changes in solar energy output could change climate so much. In the 1990s solar activity plunged while Earth's temperature climbed higher than ever, and most scientists concluded that solar activity could only be a minor influence. The issue was settled for good by a massive analysis of millions of measurements made in all the world's oceans. The observed long-term pattern of warming closely matched computer predictions of a greenhouse warming "signature," entirely different from changes that might be due to solar activity, volcanoes, or other possible influences on climate.
Some skeptics warned that the computer models were unreliable. If the models could reproduce the actual climate, that was only because the modelers had tweaked their parameters (for example, the numbers that described how clouds formed) until the models matched current climate data. Didn't that make them useless in calculating a different climate? But modelers gradually replaced their arbitrary tweaks with laboratory and observational numbers. And they began to match in detail not only the present climate but changes observed over the past century, and even the wholly different ice-age climate. Particularly convincing was a prediction that Hansen's team made shortly after a huge volcanic explosion polluted the stratosphere in 1991. They calculated a temporary global pattern of cooling over the next couple of years — and such a pattern in fact appeared.
The physics of clouds and pollution remained too complicated to work out completely. Modeling teams that fed different plausible assumptions into their computers got somewhat different results for particular regions, although always overall global warming. Rapid improvements in understanding of the many factors that affected the climate system did not help, for as new complexities were added to the models, they brought in new uncertainties. The prediction remained the same as the Academy panel had found in 1979 (and as computer modelers continued to find into the 21st century): if the CO2 level doubled, mean global temperature would rise 3°C, give or take a degree or two. If greenhouse gas emissions continued without restraint, that would come before the end of the 21st century. After that the temperature would rise still higher, to levels that everyone now realized would be catastrophic.
Meanwhile important news came from studies of ancient climates recorded in Antarctic ice cores, retrieved by a French and Russian team from one of the most inhospitable places on Earth.
A study of tree rings in ancient logs and other data meanwhile indicated that since the 1860s, Northern Hemisphere temperatures had soared to a level higher than anything in at least the past thousand years, and at a more rapid rate. Skeptics passionately attacked the "hockey-stick" shaped curve as fallacious or even fraudulent. However, independent projects by many other researchers using independent data confirmed that recent global temperatures had abruptly shot up above anything experienced in the past several thousand years.
In 1988 when scientists had first begun to call for restrictions on greenhouse gases, the world's governments created a panel to give advice on the issue. Although managed under the auspices of the United Nations, this Intergovernmental Panel on Climate Change (IPCC) was comprised of representatives appointed independently by each government. Hundreds, and later thousands, of experts donated their time to study groups that worked out what could or could not be reliably said. By 2001 the IPCC managed to establish a consensus, phrased so cautiously that none of the government representatives ventured to dissent. It was much more likely than not, the panel announced, that our civilization was headed for severe global warming. At that point the discovery of global warming was essentially completed. Scientists knew the most important things about how the climate could change during the 21st century, and what impacts might follow. How the climate would actually change now depended chiefly on what policies governments would choose to enact.
Back in 1992 the world's leaders had met in Rio de Janeiro to discuss environmental problems. In a Framework Convention on Climate Change, signed by more than 150 nations, they solemnly promised to work toward preventing "dangerous anthropogenic interference with the climate system." The parties to the Convention agreed to meet periodically, and a 1997 Conference of the Parties in Kyoto set targets for industrialized nations to reduce greenhouse gas emissions. But the developing nations refused to consider such reductions, and the U.S. Senate, spurred by a propaganda campaign led by right-wing and industrial interests, rejected the Kyoto treaty in advance.
In the early 21st century the IPCC's conclusions were reviewed and endorsed by the national science academies of every major nation, along with virtually every other organization that could speak for a scientific consensus. Specialists meanwhile improved their understanding of some less probable but more severe possible impacts. For example, there were signs that disintegrating ice sheets could raise sea levels faster than the IPCC had suggested. Worse, new evidence suggested that the warming itself was causing changes in forests and tundra that would generate still more warming.
By 2010 impacts long predicted were turning up, sooner than many had expected — acidification of the oceans, unprecedented deadly heat waves, record-breaking floods and droughts, heat-related changes in the survival of sensitive species. Most impressive, as scientists ever since Arrhenius had predicted, were changes in the Arctic. The summer Arctic ice pack was dwindling with unprecedented speed and Greenland was melting. In Antarctica, the disintegration of some ice sheets into the ocean might be irreversible. Meanwhile it became clear that even if all emissions could be instantly halted, the gases already in the air would bring some additional warming for millennia. Computer studies found that problems would get truly serious if global temperatures rose more than 1.5°C or so above the pre-industrial level, which was now almost unavoidable.
The scientists who had been predicting for decades that the world would become significantly warmer were now obviously correct. Most science journalists, business leaders, and the general public had accepted the consensus. Only in the U.S., and to a lesser extent Canada, Australia, and Russia — nations with powerful fossil fuel industries — did important political figures continue to scoff at the evidence. An ever larger number of individuals, corporate entities, and government bodies at every level decided that something had to be done.
Some developed nations made strenuous efforts to meet their Kyoto targets. As wind and solar power expanded their costs fell with remarkable speed, and Western Europe's emissions plunged. World-wide, however, emissions climbed more rapidly than ever, with China and other developing nations in the lead. The Kyoto agreement had failed. Meanwhile groups who denied that emissions should be restricted pointed to a supposed "hiatus" in the temperature rise. Most experts saw only a normal random fluctuation, and the argument ended in 2015 as warming leaped to 1.0° above pre-industrial.
Hopes for a new legally binding treaty collapsed when a 2009 meeting in Copenhagen dissolved in acrimony. Taking a less ambitious approach, in the Paris Agreement of 2015 nearly all the world's governments volunteered individual targets for reducing emissions. If every nation met its target, global temperature would probably still climb another two degrees or more, well into the dangerous zone. But utter catastrophe might be avoided, and future meetings would press for ever stronger pledges. Studies found that effective steps could be taken at surprisingly little cost, and many people and organizations began to take them.
See the summary of expected Impacts of Climate Change
Getting around: There are two sorts of essays here. Lengthy ones tell the history of some major development, such as computer modeling or international negotiations. Shorter ones delve more deeply into a particular topic — partly because it had an important impact, and partly to show some typical details of what was going on behind the scenes. At the end of most essays you will find links suggesting related supplementary essays (as enrichment) and major essays (as a path to continue through the main story).
In each essay, on the right of the text you will see links to essays about other topics. Follow forward an arrow to see how the events you are reading about gave something => TO the other topic. Follow back an arrow to track influence <= FROM the other topic (that is where you'll find the more complete account of a development). A double arrow <=> shows MUTUAL interaction.
Numbered notes, like this, (12) give references. Notes with an asterisk, like this, (12*) have some informative text in addition. You can click on the note to go to its text and references, and once there you can click on a reference to reach the item in the bibliography. To return from the bibliography, use your browser's Back button.
To start in, for the scientific story, a good starting-point is the keystone essay on the basic discoveries about The Carbon Dioxide Greenhouse Effect, followed perhaps by attempts to explain changes with Simple Models of Climate. If you are interested especially in the social connections of climate studies you could start, for example, with the facts of The Modern Temperature Trend and proceed to the long essay on U.S. Government: The View from Washington, followed by International Cooperation. For basic information and recent developments, see the page of links and bibliography.
Utilities: There is a Table of Contents (site map)... Milestones are listed in a timeline... Historians and climate scientists should read the introduction on methods and sources and are urged to contribute your thoughts including comments and corrections... References are listed in the bibliography. The site search function is only partially implemented; you can use Google by preceding your search term with "site:history.aip.org/climate/".
The statements on this site represent the views of the author and are not endorsed by the American Institute of Physics. Two of the Institute's Member Societies have taken positions on climate change, see the American Physical Society's statement and the American Geophysical Union's statement.
1. Schindler (1999). BACK