The tables below contain all of the items in the timeline above, organized by category: greenhouse gases, modeling, past climate, impacts of climate change, and climate reports. If you have suggestions for additions to this timeline of the History of Climate Science Research, please contact us.

Greenhouse Gases and the Greenhouse Effect
DateEvent
1640

Carbon Dioxide Discovered

Johann Baptista van Helmolt, Flemish alchemist, determined that air is a mixture of gases. He studied carbon dioxide, which he called the “spirit of wood” because it was given off when wood was burned. In an experiment, he burned coal to see how much carbon dioxide it added to the air.

1754

First Carbon Dioxide Detector

Joseph Black, a medical student in Edinburgh, figured out that limewater can be used as a carbon dioxide (CO2) detector. He observed that the normally clear liquid turned milky when exposed to "fixed air," which is what he called CO2. He started measuring the gas everywhere with his limewater, and found that it was released from mineral water, fermenting yeast, burning coal and oil, cremating corpses, and human exhalation. The limewater instrument was later improved by Lord Cavendish, and became known as the Cavendish Apparatus.

Learn more: The Discovery of the Greenhouse Effect

1760

Industrial Revolution Begins

Since the start of the Industrial Revolution, the way people live and work has changed dramatically as manufacturing expanded. Over time, the amount of fossil fuels burned increased, which has increased the amount of carbon dioxide (CO2 ) in the atmosphere . Before the Industrial Revolution, there was approximately 280 parts per million (ppm) of CO2 in the air. Today, that amount is over 400 ppm.

1824

Describing Earth's Atmosphere as a Greenhouse

Jean-Baptiste-Joseph Fourier, a mathematician working for Napoleon, was the first to describe how Earth's atmosphere retains warmth on what would otherwise be a very cold planet.. To help explain the concept, he compared the atmosphere to the glass walls of a greenhouse.

Learn more: The Discovery of the Greenhouse Effect

1856

Discovering Gases That Trap Heat

Eunice Foote, American scientist, discovered that carbon dioxide and water vapor cause air to warm in sunlight. In 1856, she presented her findings at the meeting of the American Association for the Advancement of Science (AAAS).

“A paper was read before the late meeting of the Scientific Association, by Prof. Henry for Mrs. Eunice Foot, detailing her experiments to determine the effects of the sun’s rays on different gases,” noted an 1856 article in Scientific American.

1859

Testing the Heat-Trapping Ability of Gases

John Tyndall, British physicist, tested the gases in the atmosphere to find out which are responsible for the greenhouse effect. He found that nitrogen and oxygen, which make up almost all of the atmosphere, have no ability to trap heat, but that three gases present in smaller quantities do: carbon dioxide, ozone, and water vapor. Tyndall speculated that if the amounts of these gases dropped, it would chill the Earth.

1896

Evaporating Coal Mines Into the Air

Svante Arrhenius, Swedish chemist, wrote in a scientific article that "We are evaporating our coal mines into the air". He added that this would eventually have an impact on the atmosphere that could lead to a warmer planet.

Learn more: Svante Arrhenius and the Greenhouse Effect [.pdf]

1938

Increasing Carbon Dioxide and Increasing Temperatures

British coal engineer George Callendar compiled all carbon dioxide measurements made over the previous 100 years and found that the amount of CO2 was increasing. He also found that temperatures were rising. His conclusion was that this was a good thing, that "the return of the deadly glaciers should be delayed indefinitely."

Read his 1949 article: Can Carbon Dioxide Influence Climate?

1957

Our Unintended Experiment

Roger Revelle, U.S. oceanographer, and Hans Suess, Austrian-born U.S. chemist, realizing that carbon dioxide from industrial sources must be building up in the atmosphere, wrote in 1957: "Thus human beings are now carrying out a large scale geophysical experiment of a kind that could not have happened in the past nor be reproduced in the future."

1958

Climate Science on Television

The Bell Telephone Science Hour addressed how our actions could be changing Earth's climate. "Even now, [we] may be unwittingly changing the world's climate through the waste products of [our] civilization," said the narrator. "Due to our release from factories and automobiles every year of more than six billion tons of carbon dioxide, which helps the air absorb heat from the Sun, our atmosphere seems to be getting warmer."

1958

Daily Measurements of Carbon Dioxide

Charles Keeling started making daily measurements of the amount of carbon dioxide in the air atop Mauna Loa in Hawaii. That first March day, he found 313 parts per million (ppm) of carbon dioxide in the air. The measurements, which are still make each day, reached 400 ppm on May 9, 2013, and continue to climb.

1988

Climate in Congress

NASA climate scientist James Hansen testified before the Senate Energy and Natural Resources Committee stating that climate was warming, greenhouse gases are responsible for the warming, and we are responsible for the growth in these gases.

1992

An Increasingly Acidic Ocean

U.S. scientists Stephen V. Smith and R.W. Buddemeier pointed out that more carbon dioxide (CO2) in the ocean could be a problem for coral reefs. Later experiments confirmed their hypothesis that CO2 makes seawater slightly acidic, which makes it difficult for corals and other animals to build reefs. Today at NCAR, scientist Joanie Kleypas builds on their work, researching the impacts of acidic oceans on marine life.

2016

CO2 Stays Above 400 ppm Year-round

September is typically when carbon dioxide is at a minimum in its annual cycle. September 2016 was the first time that minimum level was over 400 parts per million. Before large-scale burning of fossil fuels, CO2 levels were about 280 ppm.

Learn more: The World Passes 400 PPM Threshold. Permanently

 

Modeling the Earth and Future Climate
DateEvent
1960s

Simple Models to Study the Atmosphere

Syukuro Manabe and Richard Wetherald developed a basic model of the atmosphere at NOAA. With the model, they found that more carbon dioxide in the atmosphere causes higher temperatures at Earth's surface. This simple model was the first step toward development of complex Earth system models.

Read their 1967 paper: Thermal Equilibrium of the Atmosphere with a Given Distribution of Relative Humidity

“Greenhouse gases are the second most important factor for climate, after the Sun.” -Syukuro Manabe

1960s

Modeling the Whole Atmosphere

At the National Center for Atmospheric Research, scientists Akira Kasahara and Warren Washington developed a model of the whole atmosphere called a general circulation model. At first, they ran the model on a CDC 3600, a computer that filled a room yet only had a single processor. “We pretty much beat the thing up because we were running a general circulation model on it 24 hours a day, seven days a week,” said Washington. “They didn’t anticipate for people to use computers in that way.”

Learn more: NCAR's CDC 3600

1975-1985

Better Models and Faster Computers

More powerful supercomputers like the Cray 1A allowed researchers to develop more complex models that included the dynamics of both the atmosphere and ocean. Their results confirmed those from earlier models: climate is warming because of the greenhouse gases added to the atmosphere.

Learn more: NCAR's Cray 1A

1990s

Climate System Models

New models were developed to include how the ocean, land, sea ice, and atmosphere interact to affect the climate. At the end of the decade, the National Center for Atmospheric Research ran a new model, the Community Climate System Model (CCSM), on its latest supercomputer to learn more about interactions in Earth's climate system.

Learn more: 1998 special issue on CCSM results in the Journal of Climate

1990

Regional Climate Modeling

Robert Dickinson led a team to create a regional climate model for the western United States in 1989 and, in 1990, Filippo Giorgi simulated regional climate using a model nested in a general circulation model (GCM). Regional climate modeling has allowed predictions of how global climate change impacts local areas.

Learn more: Thirty years of regional climate modeling

2010

Earth System Models

Models that can include dynamics of the Earth system, including feedbacks and biogeochemical cycling, gave a more detailed view of climate change and its impacts. Advancements in modeling at NCAR, NOAA, and other research centers around the world have ushered in a new era in understanding of our complex planet.

Learn more:

 

Studying Past Climate
DateEvent
1891

Climate Recorded in Dust

Self-taught geologist John Hardcastle realized that large deposits of wind-blown dust (known as loess) in New Zealand record changes in climate from Ice Ages to warm periods in between.
"This growing dust heap played the part of an observant bystander, taking notes of certain climatic phenomena as they successively arose." —John Hardcastle

Learn more: John Hardcastle on Glacier Motion and Glacial Loess

1966

Ice Core Uncovers 8,200 Years of Climate

At Camp Century, Greenland, an ice core was extracted that showed 8,200 years of annual snow accumulation as thin layers in the ice. The thin layers of ice allowed scientists to reconstruct ancient climate using an ice core for the first time.

Learn more: Core of climate history

1966

Climate History from the Ocean Floor

In 1966, a shipbuilding company began making a ship with a drill rig on top for the Deep Sea Drilling Project, a project based at the Scripps Institute of Oceanography in San Diego, California. The drill rig would allow scientists to collect cores from the ocean floor around the world that contain layers of sediments – a record of ancient changes in climate over millions of years. Today the Integrated Ocean Drilling Program continues to collect these deepsea records.

Learn more: Integrated Ocean Drilling Program

1985

Drilling 150,000 Years Deeper into the Ice

Ice cores extracted from Antarctic ice in 1985 showed carbon dioxide and temperature had gone up and down together in wide swings over the past 150,000 years, the same relationship that computer models suggested.

Learn more: Core of climate history

2005

Finding Really Old Ice and its Climate History

A deep ice core from East Antarctica helped us understand how climate has changed over the past 650,000 years. Studying ancient air bubbles in the ice, scientists have learned details about the ancient atmosphere, including that levels of carbon dioxide are unusually high today compared to past interglacial periods.

Learn more: Core of climate history

2012

Indigenous Climate Knowledge

Since 2012, the Rising Voices program has brought indigenous knowledge and western science together to improve understanding of climate change and other types of science and to develop strategies for resilient and sustainable communities.

"We need to appreciate the experience and knowledge that has been transferred from generation to generation to generation in Native American communities." - Bob Gough

Learn more: Rising Voices at NCAR

 

The Science of Climate Impacts
DateEvent
1950s

Shrinking Arctic Sea Ice

Measurements since the 1950s indicate that the amount of sea ice in the Arctic has been declining. The Arctic is projected to have no summer ice cover by the middle of this century.

Check on sea ice at the National Snow and Ice Data Center.

1950s-1970s

Air Pollution Dampens Warming

Aerosols, emitted into the atmosphere from smokestacks and tailpipes, caused a slight cooling of climate, which fueled speculation that we could enter an Ice Age. As countries passed clean air legislation, aerosol pollution decreased and climate warming continued.

2003

Heat Wave Linked to Climate Change

Researchers determined that climate change played a large role in the 2003 heatwave in Europe, which resulted in more than 30,000 deaths.

Learn more: European Summer Heat Wave of 2003

2006

Economic Impacts of Climate Change

The Stern Review described the economic impacts of climate change, finding that mitigating (reducing the amount of greenhouse gas emissions) and adapting (making changes to the way we live) would be much less expensive than the cost of trying to recover from the disastrous impacts of climate change in the future.

Read the report: The Stern Review on the Economics of Climate Change

2007-2008

Studying Impacts in the Polar Regions

During International Polar Year which was actually two years' long (2007-2008), scientists documented numerous impacts of climate change on the polar regions, which are warming more rapidly than other areas of Earth. Impacts included melting ice, thawing permafrost, and changes in ecosystems. They found that changes were especially pronounced in the Arctic.

2011

The Effect of Climate Change on Extreme Weather

A new branch of climate science, called attribution research, formed to study how global climate change affects extreme weather events such as heat waves, hurricanes, floods, and droughts. Each year since 2011, the Bulletin of the American Meteorological Society has issued a special report about extreme weather events during the past year and how the risk of severe weather has been altered by climate change.

Read the report: Explaining Extreme Events from a Climate Perspective

2019

Dwindling Biodiversity

With Earth system models, scientists are now able to study how species and ecosystems around the world are likely to be affected by climate change and other human impacts. According to a 2019 United Nations report, climate change and other human impacts such as pollution and land use are threatening species worldwide. "Around 1 million species already face extinction, many within decades, unless action is taken," according to the report.

Read the report: United Nations 2019 Report
Learn how NCAR is modeling Western Pacific coral reefs

 

Climate Reports by the Intergovernmental Panel on Climate Change (IPCC)
DateEvent
1988

The Intergovernmental Panel on Climate Change (IPCC) Formed

The IPCC was formed by the World Meteorological Organization and the United Nations to review the latest climate science every few years and help governments around the world understand what we know about climate change, its impacts, and efforts to adapt and mitigate.

Learn more: About the IPCC

1990

First Climate Assessment Report by the IPCC

Published in 1990, the IPCC's First Assessment Report stated that it was certain that "human activities are substantially increasing the atmospheric concentrations of greenhouse gases."According to the report, greenhouse gas increases had caused temperature to increase by 0.3° to 0.6° Celsius (0.5 - 1.1° Fahrenheit) over the past century and would cause global average temperature to warm about 1°C (1.8°F) by 2025 and 3°C (5.4°F) by 2100. Projections for regional temperature and precipitation changes were highly uncertain.

Learn more: Read the Overview of the IPCC First Assessment Report [.pdf]

1995

Evidence Suggests Human Influence on Climate

The Second Assessment Report of the IPCC provided key information that led to the development of the Kyoto Protocol in 1997."Considerable progress has been made in the understanding of climate change science since 1990," wrote the authors.
Acknowledging that global climate had changed over the past century, the authors noted that regional climate change was also evident and that "global sea level has risen by 10 - 25 centimeters (4-10 inches) over the past 100 years."

Learn more: About the Kyoto Protocol

2001

New and Stronger Evidence That We Are Causing Climate Change

According to the Third Assessment Report of the Intergovernmental Panel on Climate Change (IPCC), "there is new and stronger evidence that most of the warming observed over the last 50 years is attributable to human activities."

Climate models projected that, between 1990 and 2100, Earth's atmosphere would warm by 1.4 to 5.8°C (2.5 to 10.4°F), depending on how much greenhouse gas humans emitted during that time. "The projected rate of warming is very likely to be without precedent during at least the last 10,000 years," noted the authors. The report outlined the impacts of warming, such as changing precipitation patterns, melting glaciers, and rising sea levels, as well as changes to biodiversity, economic systems, and human health.

2007

Climate Change Indisputable

The IPCC Fourth Assessment Report noted that human-caused greenhouse gas emissions had increased 70% between 1970 and 2004 and the effects of climate change were becoming apparent. "Warming of the climate system is unequivocal," wrote the authors of the 2007 report, "as is now evident from observations of increases in global average air and ocean temperatures, widespread melting of snow and ice and rising global average sea level."

"Anthropogenic [human-caused] warming could lead to some impacts that are abrupt or irreversible," they warned. "More extensive adaptation than is currently occurring is required to reduce vulnerability to climate change."

2014

Emissions Are the Highest in History

The IPCC 5th Assessment Report noted that our influence on climate is clear and "recent anthropogenic emissions of greenhouse gases are the highest in history."

The report's findings led to the Paris Climate Accord, in which nearly all of the world's countries (174 countries in total) committed to actions limiting warming to below 2° Celsius (3.6° Fahrenheit) in an effort to avoid the most catastrophic impacts. (The United States announced in 2017 that it would back out of the agreement.)

Learn more: Paris Climate Accord