Global Warming 101

Everything you wanted to know about our changing climate but were too afraid to ask.

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Temperatures in Beijing rose above 104 degrees Fahrenheit on July 6, 2023.

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What is global warming?

What causes global warming, how is global warming linked to extreme weather, what are the other effects of global warming, where does the united states stand in terms of global-warming contributors, is the united states doing anything to prevent global warming, is global warming too big a problem for me to help tackle.

A: Since the Industrial Revolution, the global annual temperature has increased in total by a little more than 1 degree Celsius, or about 2 degrees Fahrenheit. Between 1880—the year that accurate recordkeeping began—and 1980, it rose on average by 0.07 degrees Celsius (0.13 degrees Fahrenheit) every 10 years. Since 1981, however, the rate of increase has more than doubled: For the last 40 years, we’ve seen the global annual temperature rise by 0.18 degrees Celsius, or 0.32 degrees Fahrenheit, per decade.

The result? A planet that has never been hotter . Nine of the 10 warmest years since 1880 have occurred since 2005—and the 5 warmest years on record have all occurred since 2015. Climate change deniers have argued that there has been a “pause” or a “slowdown” in rising global temperatures, but numerous studies, including a 2018 paper published in the journal Environmental Research Letters , have disproved this claim. The impacts of global warming are already harming people around the world.

Now climate scientists have concluded that we must limit global warming to 1.5 degrees Celsius by 2040 if we are to avoid a future in which everyday life around the world is marked by its worst, most devastating effects: the extreme droughts, wildfires, floods, tropical storms, and other disasters that we refer to collectively as climate change . These effects are felt by all people in one way or another but are experienced most acutely by the underprivileged, the economically marginalized, and people of color, for whom climate change is often a key driver of poverty, displacement, hunger, and social unrest.

A: Global warming occurs when carbon dioxide (CO 2 ) and other air pollutants collect in the atmosphere and absorb sunlight and solar radiation that have bounced off the earth’s surface. Normally this radiation would escape into space, but these pollutants, which can last for years to centuries in the atmosphere, trap the heat and cause the planet to get hotter. These heat-trapping pollutants—specifically carbon dioxide, methane, nitrous oxide, water vapor, and synthetic fluorinated gases—are known as greenhouse gases, and their impact is called the greenhouse effect .

Though natural cycles and fluctuations have caused the earth’s climate to change several times over the last 800,000 years, our current era of global warming is directly attributable to human activity—specifically to our burning of fossil fuels such as coal, oil, gasoline, and natural gas, which results in the greenhouse effect. In the United States, the largest source of greenhouse gases is transportation (29 percent), followed closely by electricity production (28 percent) and industrial activity (22 percent). Learn about the natural and human causes of climate change .

Curbing dangerous climate change requires very deep cuts in emissions, as well as the use of alternatives to fossil fuels worldwide. The good news is that countries around the globe have formally committed—as part of the 2015 Paris Climate Agreement —to lower their emissions by setting new standards and crafting new policies to meet or even exceed those standards. The not-so-good news is that we’re not working fast enough. To avoid the worst impacts of climate change, scientists tell us that we need to reduce global carbon emissions by as much as 40 percent by 2030. For that to happen, the global community must take immediate, concrete steps: to decarbonize electricity generation by equitably transitioning from fossil fuel–based production to renewable energy sources like wind and solar; to electrify our cars and trucks; and to maximize energy efficiency in our buildings, appliances, and industries.

A: Scientists agree that the earth’s rising temperatures are fueling longer and hotter heat waves, more frequent droughts, heavier rainfall, and more powerful hurricanes .

In 2015, for example, scientists concluded that a lengthy drought in California—the state’s worst water shortage in 1,200 years —had been intensified by 15 to 20 percent by global warming. They also said the odds of similar droughts happening in the future had roughly doubled over the past century. And in 2016, the National Academies of Science, Engineering, and Medicine announced that we can now confidently attribute some extreme weather events, like heat waves, droughts, and heavy precipitation, directly to climate change.

The earth’s ocean temperatures are getting warmer, too—which means that tropical storms can pick up more energy. In other words, global warming has the ability to turn a category 3 storm into a more dangerous category 4 storm. In fact, scientists have found that the frequency of North Atlantic hurricanes has increased since the early 1980s, as has the number of storms that reach categories 4 and 5. The 2020 Atlantic hurricane season included a record-breaking 30 tropical storms, 6 major hurricanes, and 13 hurricanes altogether. With increased intensity come increased damage and death. The United States saw an unprecedented 22 weather and climate disasters that caused at least a billion dollars’ worth of damage in 2020, but 2017 was the costliest on record and among the deadliest as well: Taken together, that year's tropical storms (including Hurricanes Harvey, Irma, and Maria) caused nearly $300 billion in damage and led to more than 3,300 fatalities.

The impacts of global warming are being felt everywhere. Extreme heat waves have caused tens of thousands of deaths around the world in recent years. And in an alarming sign of events to come, Antarctica has lost nearly four trillion metric tons of ice since the 1990s. The rate of loss could speed up if we keep burning fossil fuels at our current pace, some experts say, causing sea levels to rise several meters in the next 50 to 150 years and wreaking havoc on coastal communities worldwide.

A: Each year scientists learn more about the consequences of global warming , and each year we also gain new evidence of its devastating impact on people and the planet. As the heat waves, droughts, and floods associated with climate change become more frequent and more intense, communities suffer and death tolls rise. If we’re unable to reduce our emissions, scientists believe that climate change could lead to the deaths of more than 250,000 people around the globe every year and force 100 million people into poverty by 2030.

Global warming is already taking a toll on the United States. And if we aren’t able to get a handle on our emissions, here’s just a smattering of what we can look forward to:

  • Disappearing glaciers , early snowmelt, and severe droughts will cause more dramatic water shortages and continue to increase the risk of wildfires in the American West.
  • Rising sea levels will lead to even more coastal flooding on the Eastern Seaboard, especially in Florida, and in other areas such as the Gulf of Mexico.
  • Forests, farms, and cities will face troublesome new pests , heat waves, heavy downpours, and increased flooding . All of these can damage or destroy agriculture and fisheries.
  • Disruption of habitats such as coral reefs and alpine meadows could drive many plant and animal species to extinction.
  • Allergies, asthma, and infectious disease outbreaks will become more common due to increased growth of pollen-producing ragweed , higher levels of air pollution , and the spread of conditions favorable to pathogens and mosquitoes.

Though everyone is affected by climate change, not everyone is affected equally. Indigenous people, people of color, and the economically marginalized are typically hit the hardest . Inequities built into our housing , health care , and labor systems make these communities more vulnerable to the worst impacts of climate change—even though these same communities have done the least to contribute to it.

A: In recent years, China has taken the lead in global-warming pollution , producing about 26 percent of all CO2 emissions. The United States comes in second. Despite making up just 4 percent of the world’s population, our nation produces a sobering 13 percent of all global CO2 emissions—nearly as much as the European Union and India (third and fourth place) combined. And America is still number one, by far, in cumulative emissions over the past 150 years. As a top contributor to global warming, the United States has an obligation to help propel the world to a cleaner, safer, and more equitable future. Our responsibility matters to other countries, and it should matter to us, too.

A: We’ve started. But in order to avoid the worsening effects of climate change, we need to do a lot more—together with other countries—to reduce our dependence on fossil fuels and transition to clean energy sources.

Under the administration of President Donald Trump (a man who falsely referred to global warming as a “hoax”), the United States withdrew from the Paris Climate Agreement, rolled back or eliminated dozens of clean-air protections, and opened up federally managed lands, including culturally sacred national monuments , to fossil fuel development. Although President Biden has pledged to get the country back on track, years of inaction during and before the Trump administration—and our increased understanding of global warming’s serious impacts—mean we must accelerate our efforts to reduce greenhouse gas emissions.

Despite the lack of cooperation from the Trump administration, local and state governments made great strides during this period through efforts like the American Cities Climate Challenge and ongoing collaborations like the Regional Greenhouse Gas Initiative . Meanwhile, industry and business leaders have been working with the public sector, creating and adopting new clean-energy technologies and increasing energy efficiency in buildings, appliances, and industrial processes. Today the American automotive industry is finding new ways to produce cars and trucks that are more fuel efficient and is committing itself to putting more and more zero-emission electric vehicles on the road. Developers, cities, and community advocates are coming together to make sure that new affordable housing is built with efficiency in mind , reducing energy consumption and lowering electric and heating bills for residents. And renewable energy continues to surge as the costs associated with its production and distribution keep falling. In 2020 renewable energy sources such as wind and solar provided more electricity than coal for the very first time in U.S. history.

President Biden has made action on global warming a high priority. On his first day in office, he recommitted the United States to the Paris Climate Agreement, sending the world community a strong signal that we were determined to join other nations in cutting our carbon pollution to support the shared goal of preventing the average global temperature from rising more than 1.5 degrees Celsius above preindustrial levels. (Scientists say we must stay below a 2-degree increase to avoid catastrophic climate impacts.) And significantly, the president has assembled a climate team of experts and advocates who have been tasked with pursuing action both abroad and at home while furthering the cause of environmental justice and investing in nature-based solutions.

A: No! While we can’t win the fight without large-scale government action at the national level , we also can’t do it without the help of individuals who are willing to use their voices, hold government and industry leaders to account, and make changes in their daily habits.

Wondering how you can be a part of the fight against global warming? Reduce your own carbon footprint by taking a few easy steps: Make conserving energy a part of your daily routine and your decisions as a consumer. When you shop for new appliances like refrigerators, washers, and dryers, look for products with the government’s ENERGY STAR ® label; they meet a higher standard for energy efficiency than the minimum federal requirements. When you buy a car, look for one with the highest gas mileage and lowest emissions. You can also reduce your emissions by taking public transportation or carpooling when possible.

And while new federal and state standards are a step in the right direction, much more needs to be done. Voice your support of climate-friendly and climate change preparedness policies, and tell your representatives that equitably transitioning from dirty fossil fuels to clean power should be a top priority—because it’s vital to building healthy, more secure communities.

You don’t have to go it alone, either. Movements across the country are showing how climate action can build community , be led by those on the front lines of its impacts, and create a future that’s equitable and just for all .

This story was originally published on March 11, 2016 and has been updated with new information and links.

This NRDC.org story is available for online republication by news media outlets or nonprofits under these conditions: The writer(s) must be credited with a byline; you must note prominently that the story was originally published by NRDC.org and link to the original; the story cannot be edited (beyond simple things such as grammar); you can’t resell the story in any form or grant republishing rights to other outlets; you can’t republish our material wholesale or automatically—you need to select stories individually; you can’t republish the photos or graphics on our site without specific permission; you should drop us a note to let us know when you’ve used one of our stories.

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What is Climate Change? PowerPoint Presentation

Publication Date Wed, 06/01/2022 - 12:00 Authors Morgan Lawrence PDF Document What is Climate Change? PowerPoint Presentation (1.6 MB)

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Climate Matters • November 25, 2020

New Presentation: Our Changing Climate

Key concepts:.

Climate Central unveils Our Changing Climate —an informative and customizable climate change presentation that meteorologists, journalists, and others can use for educational outreach and/or a personal Climate 101 tool.

The presentation follows a ”Simple, Serious, Solvable” framework, inspired by climate scientist Scott Denning. This allows the presenter to comfortably explain, and the viewers to easily understand, the causes (Simple), impacts (Serious), and solutions (Solvable) of climate change. 

Our Changing Climate is a revamped version of our 2016 climate presentation, and includes the following updates and features:

Up-to-date graphics and topics

Local data and graphics

Fully editable slides (add, remove, customize)

Presenter notes, background information, and references for each slide

Supplementary and bonus slides

Download Outline (PDF, 110KB)

Download Full Presentation (PPT, 148MB)

Updated: April 2021

Climate Central is presenting a new outreach and education resource for meteorologists, journalists, and others—a climate change presentation, Our Changing Climate . This 55-slide presentation is a guide through the basics of climate change, outlining its causes, impacts, and solutions. This climate change overview is unique because it includes an array of local graphics from our ever-expanding media library. By providing these local angles, the presenter can demonstrate that climate change is not only happening at a global-scale, but in our backyards.

This presentation was designed to support your climate change storytelling, but can also double as a great Climate 101 tool for journalists or educators who want to understand climate change better. Every slide contains main points along with background information, so people that are interested can learn at their own pace or utilize graphics for their own content. 

In addition to those features, it follows the “Simple, Serious, Solvable” framework inspired by Scott Denning, a climate scientist and professor of atmospheric science at Colorado State University (and a good friend of the program). These three S’s help create the presentation storyline and outline the causes (Simple), impacts (Serious), and solutions (Solvable) of climate change. 

Simple. It is simple—burning fossil fuels is heating up the Earth. This section outlines the well-understood science that goes back to the 1800s, presenting local and global evidence that our climate is warming due to human activities.

Serious. More extreme weather, rising sea levels, and increased health and economic risks—the consequences of climate change. In this section, well, we get serious. Climate change impacts are already being felt around the world, and they will continue to intensify until we cut greenhouse gas emissions. 

Solvable. With such a daunting crisis like climate change, it is easy to get wrapped up in the negative impacts. This section explains how we can curb climate change and lists the main pathways and solutions to achieving this goal. 

With the rollout of our new climate change presentation, we at Climate Central would value any feedback on this presentation. Feel free to reach out to us about how the presentation worked for you, how your audience reacted, or any ideas or topics you would like to see included. 

ACKNOWLEDGMENTS & SPECIAL THANKS

Climate Central would like to acknowledge Paul Gross at WDIV-TV in Detroit and the AMS Station Science Committee for the original version of the climate presentation, Climate Change Outreach Presentation , that was created in 2016. We would also like to give special thanks to Scott Denning, professor of atmospheric science at Colorado State University and a member of our NSF advisory board, for allowing us to use this “Simple, Serious, Solvable” framework in this presentation resource.

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Simpler Presentations of Climate Change

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Figure showing modeled atmospheric carbon dioxide concentrations over an image of Earth’s surface, with warmer colors representing higher concentrations

Science Leads the Future

Cover of the November-December 2022 issue of Eos

Are We Entering The Golden Age Of Climate Modeling?

Alumni push universities forward on climate, indoor air pollution in the time of coronavirus, how an unlikely friendship upended permafrost myths, the alarming rise of predatory conferences, science leads the future, and the future is now.

Has this happened to you? You are presenting the latest research about climate change to a general audience, maybe at the town library, to a local journalist, or even in an introductory science class. After presenting the solid science about greenhouse gases, how they work, and how we are changing them, you conclude with “and this is what the models predict about our climate future…”

At that point, your audience may feel they are being asked to make a leap of faith. Having no idea how the models work or what they contain and leave out, this final and crucial step becomes to them a “trust me” moment. Trust me moments can be easy to deny.

This problem has not been made easier by a recent expansion in the number of models and the range of predictions presented in the literature. One recent study making this point is that of Hausfather et al. [2022], which presents the “hot model” problem: the fact that some of the newer models in the Coupled Model Intercomparison Project Phase 6 (CMIP6) model comparison yield predictions of global temperatures that are above the range presented in the Intergovernmental Panel on Climate Change’s (IPCC) Sixth Assessment Report (AR6). The authors present a number of reasons for, and solutions to, the hot model problem.

Models are crucial in advancing any field of science. They represent a state-of-the-art summary of what the community understands about its subject. Differences among models highlight unknowns on which new research can be focused.

But Hausfather and colleagues make another point: As questions are answered and models evolve, they should also converge. That is, they should not only reproduce past measurements, but they should also begin to produce similar projections into the future. When that does not happen, it can make trust me moments even less convincing.

Are there simpler ways to make the major points about climate change, especially to general audiences, without relying on complex models?

We think there are.

Old Predictions That Still Hold True

In a recent article in Eos , Andrei Lapenis retells the story of Mikhail Budyko ’s 1972 predictions about global temperature and sea ice extent [ Budyko , 1972]. Lapenis notes that those predictions have proven to be remarkably accurate. This is a good example of effective, long-term predictions of climate change that are based on simple physical mechanisms that are relatively easy to explain.

There are many other examples that go back more than a century. These simpler formulations don’t attempt to capture the spatial or temporal detail of the full models, but their success at predicting the overall influence of rising carbon dioxide (CO 2 ) on global temperatures makes them a still-relevant, albeit mostly overlooked, resource in climate communication and even climate prediction.

One way to make use of this historical record is to present the relative consistency over time in estimates of equilibrium carbon sensitivity (ECS), the predicted change in mean global temperature expected from a doubling of atmospheric CO 2 . ECS can be presented in straightforward language, maybe even without the name and acronym, and is an understandable concept.

Estimates of ECS can be traced back for more than a century (Table 1), showing that the relationship between CO 2 in the atmosphere and Earth’s radiation and heat balance, as an expression of a simple and straightforward physical process, has been understood for a very long time. We can now measure that balance with precision [e.g., Loeb et al. , 2021], and measurements and modeling using improved technological expertise have all affirmed this scientific consistency.

Table 1. Selected Historical Estimates of Equilibrium Carbon Sensitivity (ECS)

Settled Science

Another approach for communicating with general audiences is to present an abbreviated history demonstrating that we have known the essentials of climate change for a very long time—that the basics are settled science.

The following list is a vastly oversimplified set of four milestones in the history of climate science that we have found to be effective. In a presentation setting, this four-step outline also provides a platform for a more detailed discussion if an audience wants to go there.

  • 1850s: Eunice Foote observes that, when warmed by sunlight, a cylinder filled with CO 2 attained higher temperatures and cooled more slowly than one filled with ambient air, leading her to conclude that higher concentrations of CO 2 in the atmosphere should increase Earth’s surface temperature [ Foote , 1856]. While not identifying the greenhouse effect mechanism, this may be the first statement in the scientific literature linking CO 2 to global temperature. Three years later, John Tyndall separately develops a method for measuring the absorbance of infrared radiation and demonstrates that CO 2 is an effective absorber (acts as a greenhouse gas) [ Tyndall , 1859 ; 1861 ]. 
  • 1908: Svante Arrhenius describes a nonlinear response to increased CO 2 based on a year of excruciating hand calculations actually performed in 1896 [ Arrhenius , 1896]. His value for ECS is 4°C (Table 1), and the nonlinear response has been summarized in a simple one-parameter model .
  • 1958: Charles Keeling establishes an observatory on Mauna Loa in Hawaii. He begins to construct the “ Keeling curve ” based on measurements of atmospheric CO 2 concentration over time. It is amazing how few people in any audience will have seen this curve.
  • Current: The GISS data set of global mean temperature from NASA’s Goddard Institute for Space Studies records the trajectory of change going back decades to centuries using both direct measurements and environmental proxies.

The last three of these steps can be combined graphically to show how well the simple relationship derived from Arrhenius ’s [1908] projections, driven by CO 2 data from the Keeling curve, predicts the modern trend in global average temperature (Figure 1). The average error in this prediction is only 0.081°C, or 8.1 hundredths of a degree.

Black-and-white data plot showing measured changes in global mean temperature (open circles) compared with predictions (solid circles) from a simple model between about 1960 and 2020

A surprise to us was that this relationship can be made even more precise by adding the El Niño index (November–January (NDJ) from the previous year) as a second predictor. The status of the El Niño–Southern Oscillation ( ENSO ) system has been known to affect global mean temperature as well as regional weather patterns. With this second term added , the average error in the prediction drops to just over 0.06°C, or 6 one hundredths of a degree.

It is also possible to extend this simple analysis into the future using the same relationship and IPCC AR6 projections for CO 2 and “assessed warming” (results from four scenarios combined; Figure 2).

Although CO 2 is certainly not the only cause of increased warming, it provides a powerful index of the cumulative changes we are making to Earth’s climate system.

A presentation built around the consistency of equilibrium carbon sensitivity estimates does not deliver a complete understanding of the changes we are causing in the climate system, but the relatively simple, long-term historical perspective can be an effective way to tell the story.

In this regard, it is interesting that the “Summary for Policy Makers” [ Intergovernmental Panel on Climate Change , 2021] from the most recent IPCC science report also includes a figure (Figure SPM.10, p. 28) that captures both measured past and predicted future global temperature change as a function of cumulative CO 2 emissions alone. Given that the fraction of emissions remaining in the atmosphere over time has been relatively constant, this is equivalent to the relationship with concentration presented here. That figure also presents the variation among the models in predicted future temperatures, which is much greater than the measurement errors in the GISS and Keeling data sets that underlie the relationship in Figure 1.

A presentation built around the consistency of ECS estimates and the four steps clearly does not deliver a complete understanding of the changes we are causing in the climate system, but the relatively simple, long-term historical perspective can be an effective way to tell the story of those changes.

Past Performance and Future Results

Black-and-white data plot showing values of assessed global mean warming through the year 2100 compared with predictions from a simple model

Projecting the simple model used in Figure 1 into the future (Figure 2) assumes that the same factors that have made CO 2 alone such a good index to climate change to date will remain in place. But we know there are processes at work in the world that could break this relationship.

For example, some sources now see the electrification of the economic system, including transportation, production, and space heating and cooling, as part of the path to a zero-carbon economy [e.g., Gates , 2021]. But there is one major economic sector in which energy production is not the dominant process for greenhouse gas emissions and carbon dioxide is not the major greenhouse gas. That sector is agriculture.

The U.S. Department of Agriculture has estimated that agriculture currently accounts for about 10% of total U.S. greenhouse gas emissions, with nitrous oxide (N 2 O) and methane (CH 4 ) being major contributors to that total. According to the EPA (Figure 3), agriculture contributes 79% of N 2 O emissions in the United States, largely from the production and application of fertilizers (agricultural soil management) as well as from manure management, and 36% of CH 4 emissions (enteric fermentation and manure management—one might add some of the landfill emissions to that total as well).

If we succeed in moving nonagricultural sectors of the economy toward a zero-carbon state, the relationship in Figures 1 and 2 will be broken. The rate of overall climate warming would be reduced significantly, but N 2 O and CH 4 would begin to play a more dominant role in driving continued greenhouse gas warming of the planet, and we will then need more complex models than the one used for Figures 1 and 2. But just how complex?

Three pie charts showing EPA-reported total U.S. greenhouse gas emissions in 2020 (left) as well as sources of N2O (center) and CH4 (right) emissions.

In his recent book Life Is Simple , biologist Johnjoe McFadden traces the influence across the centuries of William of Occam (~1287–1347) and Occam’s razor as a concept in the development of our physical understanding of everything from the cosmos to the subatomic structure of matter [ McFadden , 2021]. One simple statement of Occam’s razor is, Entities should not be multiplied without necessity.

This is a simple and powerful statement: Explain a set of measurements with as few parameters, or entities, as possible. But the definition of necessity can change when the goals of a model or presentation change. The simple model used in Figures 1 and 2 tells us nothing about tomorrow’s weather or the rate of sea level rise or the rate of glacial melt. But for as long as the relationship serves to capture the role of CO 2 as an accurate index of changes in mean global temperature, it can serve the goal of making plain to general audiences that there are solid, undeniable scientific reasons why climate change is happening.

Getting the Message Across

When and if the simple relationship derived from Arrhenius’s calculations does fail as an accurate index of changes in mean global temperature, it will still provide a useful platform for explaining what has happened and why.

If we move toward an electrified economy and toward zero-carbon sources of electricity, the simple relationship derived from Arrhenius’s calculations will no longer serve that function. But when and if it does fail, it will still provide a useful platform for explaining what has happened and why. Perhaps there will be another, slightly more complex model for predicting and explaining climate change that involves three gases.

No matter how our climate future evolves, simpler and more accessible presentations of climate change science will always rely on and begin with our current understanding of the climate system. Complex, detailed models will be central to predicting our climate future (Figure 2 here would not be possible without them), but we will be more effective communicators if we can discern how best to simplify that complexity when presenting the essentials of climate science to general audiences.

Arrhenius, S. (1896), On the influence of carbonic acid in the air upon temperature of the ground, Philos. Mag. J. Sci. , Ser. 5 , 41 , 237–276, https://doi.org/10.1080/14786449608620846 .

Arrhenius, S. (1908), Worlds in the Making: The Evolution of the Universe , translated by H. Borns, 228 pp., Harper, New York.

Budyko, M. I. (1972), Man’s Impact on Climate [in Russian], Gidrometeoizdat, St. Petersburg, Russia.

Foote, E. (1856), Circumstances affecting the heat of the Sun’s rays,  Am. J. Sci. Arts ,  22 (66), 382–383,  ia800802.us.archive.org/4/items/mobot31753002152491/mobot31753002152491.pdf .

Gates, B. (2021), How to Avoid a Climate Disaster , 257 pp., Alfred A. Knopf, New York.

Hausfather, Z., et al. (2022), Climate simulations: Recognize the ‘hot model’ problem, Nature , 605 , 26–29, https://doi.org/10.1038/d41586-022-01192-2 .

Intergovernmental Panel on Climate Change (2021), Summary for policymakers, in Climate Change 2021: The Physical Science Basis—Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change , edited by V. Masson-Delmotte et al., pp. 3–32, Cambridge Univ. Press, Cambridge, U.K., and New York, https://www.ipcc.ch/report/ar6/wg1/downloads/report/IPCC_AR6_WGI_SPM.pdf .

Loeb, N. G., et al. (2021), Satellite and ocean data reveal marked increase in Earth’s heating rate, Geophys. Res. Lett. , 48 (13), e2021GL093047, https://doi.org/10.1029/2021GL093047 .

McFadden, J. (2021), Life Is Simple: How Occam’s Razor Set Science Free and Shapes the Universe , 376 pp., Basic Books, New York.

Tyndall, J. (1859), Note on the transmission of radiant heat through gaseous bodies,  Proc. R. Soc. London ,  10 , 37–39,  https://www.jstor.org/stable/111604 . 

Tyndall, J. (1861), I. The Bakerian Lecture.—On the absorption and radiation of heat by gases and vapours, and on the physical connexion of radiation, absorption, and conduction, Philos. Trans. R. Soc. London , 151 , https://doi.org/10.1098/rstl.1861.0001 .

Author Information

John Aber ( [email protected] ) and Scott V. Ollinger, Department of Natural Resources and the Environment and the Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, Durham

Update, 26 September 2022: This article has been updated to include the early contribution of Eunice Foote in the study of CO 2 and its effects on Earth’s climate.

Citation:  Aber, J., and S. V. Ollinger (2022), Simpler presentations of climate change,  Eos, 103, https://doi.org/10.1029/2022EO220444 . Published on 13 September 2022.

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  • Environment

How global warming is disrupting life on Earth

The signs of global warming are everywhere, and are more complex than just climbing temperatures.

Our planet is getting hotter. Since the Industrial Revolution—an event that spurred the use of fossil fuels in everything from power plants to transportation—Earth has warmed by 1 degree Celsius, about 2 degrees Fahrenheit. 

That may sound insignificant, but 2023 was the hottest year on record , and all 10 of the hottest years on record have occurred in the past decade. 

Global warming and climate change are often used interchangeably as synonyms, but scientists prefer to use “climate change” when describing the complex shifts now affecting our planet’s weather and climate systems. 

Climate change encompasses not only rising average temperatures but also natural disasters, shifting wildlife habitats, rising seas , and a range of other impacts. All of these changes are emerging as humans continue to add heat-trapping greenhouse gases , like carbon dioxide and methane, to the atmosphere.

What causes global warming?

When fossil fuel emissions are pumped into the atmosphere, they change the chemistry of our atmosphere, allowing sunlight to reach the Earth but preventing heat from being released into space. This keeps Earth warm, like a greenhouse, and this warming is known as the greenhouse effect . 

Carbon dioxide is the most commonly found greenhouse gas and about 75 percent of all the climate warming pollution in the atmosphere. This gas is a product of producing and burning oil, gas, and coal. About a quarter of Carbon dioxide also results from land cleared for timber or agriculture. 

Methane is another common greenhouse gas. Although it makes up only about 16 percent of emissions, it's roughly 25 times more potent than carbon dioxide and dissipates more quickly. That means methane can cause a large spark in warming, but ending methane pollution can also quickly limit the amount of atmospheric warming. Sources of this gas include agriculture (mostly livestock), leaks from oil and gas production, and waste from landfills. 

What are the effects of global warming? 

One of the most concerning impacts of global warming is the effect warmer temperatures will have on Earth's polar regions and mountain glaciers. The Arctic is warming four times faster than the rest of the planet. This warming reduces critical ice habitat and it disrupts the flow of the jet stream, creating more unpredictable weather patterns around the globe. 

( Learn more about the jet stream. )

A warmer planet doesn't just raise temperatures. Precipitation is becoming more extreme as the planet heats. For every degree your thermometer rises, the air holds about seven percent more moisture. This increase in moisture in the atmosphere can produce flash floods, more destructive hurricanes, and even paradoxically, stronger snow storms. 

The world's leading scientists regularly gather to review the latest research on how the planet is changing. The results of this review is synthesized in regularly published reports known as the Intergovernmental Panel on Climate Change (IPCC) reports. 

A recent report outlines how disruptive a global rise in temperature can be:

  • Coral reefs are now a highly endangered ecosystem. When corals face environmental stress, such as high heat, they expel their colorful algae and turn a ghostly white, an effect known as coral bleaching . In this weakened state, they more easily die. 
  • Trees are increasingly dying from drought , and this mass mortality is reshaping forest ecosystems.
  • Rising temperatures and changing precipitation patterns are making wildfires more common and more widespread. Research shows they're even moving into the eastern U.S. where fires have historically been less common.
  • Hurricanes are growing more destructive and dumping more rain, an effect that will result in more damage. Some scientists say we even need to be preparing for Cat 6 storms . (The current ranking system ends at Cat 5.)

How can we limit global warming? 

Limiting the rising in global warming is theoretically achievable, but politically, socially, and economically difficult. 

Those same sources of greenhouse gas emissions must be limited to reduce warming. For example, oil and gas used to generate electricity or power industrial manufacturing will need to be replaced by net zero emission technology like wind and solar power. Transportation, another major source of emissions, will need to integrate more electric vehicles, public transportation, and innovative urban design, such as safe bike lanes and walkable cities. 

( Learn more about solutions to limit global warming. )

One global warming solution that was once considered far fetched is now being taken more seriously: geoengineering. This type of technology relies on manipulating the Earth's atmosphere to physically block the warming rays of the sun or by sucking carbon dioxide straight out of the sky.

Restoring nature may also help limit warming. Trees, oceans, wetlands, and other ecosystems help absorb excess carbon—but when they're lost, so too is their potential to fight climate change. 

Ultimately, we'll need to adapt to warming temperatures, building homes to withstand sea level rise for example, or more efficiently cooling homes during heat waves. 

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Greenhouse Effect

Global warming describes the current rise in the average temperature of Earth’s air and oceans. Global warming is often described as the most recent example of climate change.

Earth Science, Meteorology, Geography

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Global warming describes the current rise in the average temperature of Earth’s air and oceans. Global warming is often described as the most recent example of climate change . Earth’s climate has changed many times. Our planet has gone through multiple ice ages , in which ice sheets and glaciers covered large portions of Earth. It has also gone through warm periods when temperatures were higher than they are today. Past changes in Earth’s temperature happened very slowly, over hundreds of thousands of years. However, the recent warming trend is happening much faster than it ever has. Natural cycles of warming and cooling are not enough to explain the amount of warming we have experienced in such a short time—only human activities can account for it. Scientists worry that the climate is changing faster than some living things can adapt to it. In 1988, the World Meteorological Organization and the United Nations Environment Programme established a committee of climatologists , meteorologists , geographers , and other scientists from around the world. This Intergovernmental Panel on Climate Change (IPCC) includes thousands of scientists who review the most up-to-date research available related to global warming and climate change. The IPCC evaluates the risk of climate change caused by human activities. According to the IPCC’s most recent report (in 2007), Earth’s average surface temperatures have risen about 0.74 degrees Celsius (1.33 degrees Fahrenheit) during the past 100 years. The increase is greater in northern latitudes . The IPCC also found that land regions are warming faster than oceans. The IPCC states that most of the temperature increase since the mid-20th century is likely due to human activities. The Greenhouse Effect Human activities contribute to global warming by increasing the greenhouse effect. The greenhouse effect happens when certain gases—known as greenhouse gases —collect in Earth’s atmosphere . These gases, which occur naturally in the atmosphere, include carbon dioxide , methane , nitrogen oxide, and fluorinated gases sometimes known as chlorofluorocarbons (CFCs). Greenhouse gases let the sun’s light shine onto Earth’s surface, but they trap the heat that reflects back up into the atmosphere. In this way, they act like the insulating glass walls of a greenhouse. The greenhouse effect keeps Earth’s climate comfortable. Without it, surface temperatures would be cooler by about 33 degrees Celsius (60 degrees Fahrenheit), and many life forms would freeze . Since the Industrial Revolution in the late 1700s and early 1800s, people have been releasing large quantities of greenhouse gases into the atmosphere. That amount has skyrocketed in the past century. Greenhouse gas emissions increased 70 percent between 1970 and 2004. Emissions of carbon dioxide, the most important greenhouse gas, rose by about 80 percent during that time. The amount of carbon dioxide in the atmosphere today far exceeds the natural range seen over the last 650,000 years. Most of the carbon dioxide that people put into the atmosphere comes from burning fossil fuels such as oil , coal , and natural gas . Cars, trucks, trains, and planes all burn fossil fuels. Many electric power plants also burn fossil fuels. Another way people release carbon dioxide into the atmosphere is by cutting down forests . This happens for two reasons. Decaying plant material, including trees, releases tons of carbon dioxide into the atmosphere. Living trees absorb carbon dioxide. By diminishing the number of trees to absorb carbon dioxide, the gas remains in the atmosphere. Most methane in the atmosphere comes from livestock farming , landfills , and fossil fuel production such as coal mining and natural gas processing. Nitrous oxide comes from agricultural technology and fossil fuel burning. Fluorinated gases include chlorofluorocarbons, hydrochlorofluorocarbons , and hydrofluorocarbons. These greenhouse gases are used in aerosol cans and refrigeration. All of these human activities add greenhouse gases to the atmosphere, trapping more heat than usual and contributing to global warming. Effects of Global Warming Even slight rises in average global temperatures can have huge effects. Perhaps the biggest, most obvious effect is that glaciers and ice caps melt faster than usual. The meltwater drains into the oceans, causing sea levels to rise and oceans to become less salty. Ice sheets and glaciers advance and retreat naturally. As Earth’s temperature has changed, the ice sheets have grown and shrunk, and sea levels have fallen and risen. Ancient corals found on land in Florida, Bermuda, and the Bahamas show that the sea level must have been five to six meters (16-20 feet) higher 130,000 years ago than it is today. Earth doesn’t need to become oven-hot to melt the glaciers. Northern summers were just three to five degrees Celsius (five to nine degrees Fahrenheit) warmer during the time of those ancient fossils than they are today. However, the speed at which global warming is taking place is unprecedented . The effects are unknown. Glaciers and ice caps cover about 10 percent of the world’s landmass today. They hold about 75 percent of the world’s fresh water. If all of this ice melted, sea levels would rise by about 70 meters (230 feet). The IPCC reported that the global sea level rose about 1.8 millimeters (0.07 inches) per year from 1961 to 1993, and 3.1 millimeters (0.12 inches) per year since 1993. Rising sea levels could flood coastal communities, displacing millions of people in areas such as Bangladesh, the Netherlands, and the U.S. state of Florida. Forced migration would impact not only those areas, but the regions to which the “ climate refugees ” flee . Millions more people in countries like Bolivia, Peru, and India depend on glacial meltwater for drinking, irrigation , and hydroelectric power . Rapid loss of these glaciers would devastate those countries. Glacial melt has already raised the global sea level slightly. However, scientists are discovering ways the sea level could increase even faster. For example, the melting of the Chacaltaya Glacier in Bolivia has exposed dark rocks beneath it. The rocks absorb heat from the sun, speeding up the melting process. Many scientists use the term “climate change” instead of “global warming.” This is because greenhouse gas emissions affect more than just temperature. Another effect involves changes in precipitation like rain and snow . Patterns in precipitation may change or become more extreme. Over the course of the 20th century, precipitation increased in eastern parts of North and South America, northern Europe, and northern and central Asia. However, it has decreased in parts of Africa, the Mediterranean, and parts of southern Asia. Future Changes Nobody can look into a crystal ball and predict the future with certainty. However, scientists can make estimates about future population growth, greenhouse gas emissions, and other factors that affect climate. They can enter those estimates into computer models to find out the most likely effects of global warming. The IPCC predicts that greenhouse gas emissions will continue to increase over the next few decades . As a result, they predict the average global temperature will increase by about 0.2 degrees Celsius (0.36 degrees Fahrenheit) per decade. Even if we reduce greenhouse gas and aerosol emissions to their 2000 levels, we can still expect a warming of about 0.1 degree Celsius (0.18 degrees Fahrenheit) per decade. The panel also predicts global warming will contribute to some serious changes in water supplies around the world. By the middle of the 21st century, the IPCC predicts, river runoff and water availability will most likely increase at high latitudes and in some tropical areas. However, many dry regions in the mid-latitudes and tropics will experience a decrease in water resources. As a result, millions of people may be exposed to water shortages . Water shortages decrease the amount of water available for drinking, electricity , and hygiene . Shortages also reduce water used for irrigation. Agricultural output would slow and food prices would climb. Consistent years of drought in the Great Plains of the United States and Canada would have this effect. IPCC data also suggest that the frequency of heat waves and extreme precipitation will increase. Weather patterns such as storms and tropical cyclones will become more intense. Storms themselves may be stronger, more frequent, and longer-lasting. They would be followed by stronger storm surges , the immediate rise in sea level following storms. Storm surges are particularly damaging to coastal areas because their effects (flooding, erosion , damage to buildings and crops) are lasting. What We Can Do Reducing our greenhouse gas emissions is a critical step in slowing the global warming trend. Many governments around the world are working toward this goal. The biggest effort so far has been the Kyoto Protocol , which was adopted in 1997 and went into effect in 2005. By the end of 2009, 187 countries had signed and ratified the agreement. Under the protocol , 37 industrialized countries and the European Union have committed to reducing their greenhouse gas emissions. There are several ways that governments, industries, and individuals can reduce greenhouse gases. We can improve energy efficiency in homes and businesses. We can improve the fuel efficiency of cars and other vehicles. We can also support development of alternative energy sources, such as solar power and biofuels , that don’t involve burning fossil fuels. Some scientists are working to capture carbon dioxide and store it underground, rather than let it go into the atmosphere. This process is called carbon sequestration . Trees and other plants absorb carbon dioxide as they grow. Protecting existing forests and planting new ones can help balance greenhouse gases in the atmosphere. Changes in farming practices could also reduce greenhouse gas emissions. For example, farms use large amounts of nitrogen-based fertilizers , which increase nitrogen oxide emissions from the soil. Reducing the use of these fertilizers would reduce the amount of this greenhouse gas in the atmosphere. The way farmers handle animal manure can also have an effect on global warming. When manure is stored as liquid or slurry in ponds or tanks, it releases methane. When it dries as a solid, however, it does not. Reducing greenhouse gas emissions is vitally important. However, the global temperature has already changed and will most likely continue to change for years to come. The IPCC suggests that people explore ways to adapt to global warming as well as try to slow or stop it. Some of the suggestions for adapting include:

  • Expanding water supplies through rain catchment , conservation , reuse, and desalination .
  • Adjusting crop locations, variety, and planting dates.
  • Building seawalls and storm surge barriers and creating marshes and wetlands as buffers against rising sea levels .
  • Creating heat-health action plans , boosting emergency medical services, and improving disease surveillance and control.
  • Diversifying tourism attractions, because existing attractions like ski resorts and coral reefs may disappear.
  • Planning for roads and rail lines to cope with warming and/or flooding.
  • Strengthening energy infrastructure , improving energy efficiency, and reducing dependence on single sources of energy.

Barking up the Wrong Tree Spruce bark beetles in the U.S. state of Alaska have had a population boom thanks to 20 years of warmer-than-average summers. The insects have managed to chew their way through 1.6 million hectares (four million acres) of spruce trees.

Disappearing Penguins Emperor penguins ( Aptenodytes forsteri ) made a showbiz splash in the 2005 film March of the Penguins . Sadly, their encore might include a disappearing act. In the 1970s, an abnormally long warm spell caused these Antarctic birds' population to drop by 50 percent. Some scientists worry that continued global warming will push the creatures to extinction by changing their habitat and food supply.

Shell Shock A sudden increase in the amount of carbon dioxide in the atmosphere does more than change Earth's temperature. A lot of the carbon dioxide in the air dissolves into seawater. There, it forms carbonic acid in a process called ocean acidification. Ocean acidification is making it hard for some sea creatures to build shells and skeletal structures. This could alter the ecological balance in the oceans and cause problems for fishing and tourism industries.

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Video: Global Warming from 1880 to 2022

January 12, 2023

Earth's average surface temperature in 2022 tied with 2015 as the fifth warmest on record, according to an analysis by NASA. Continuing the planet's long-term warming trend, global temperatures in 2022 were 1.6 degrees Fahrenheit (0.89 degrees Celsius) above the average for NASA's baseline period (1951-1980), scientists from NASA's Goddard Institute for Space Studies (GISS) in New York reported.

The past nine years have been the warmest years since modern recordkeeping began in 1880. This means Earth in 2022 was about 2 degrees Fahrenheit (or about 1.11 degrees Celsius) warmer than the late 19th century average.

Full story: https://climate.nasa.gov/news/3246/nasa-says-2022-fifth-warmest-year-on-record-warming-trend-continues/

NASA's Scientific Visualization Studio. Data provided by Robert B. Schmunk (NASA/GSFC GISS).

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Global Warming

Miss Parson – Allerton Grange School

Aims and objectives

  • To be able to define and understand the process of Global Warming.
  • Be able to describe the effects of Global Warming on a global and local scale.
  • Be able to recognise how the effects of Global Warming can be reduced.

What is�Global Warming ?

Global warming is the increase in the world’s average temperature, believed to be the result from the release of carbon dioxide and other gases into the atmosphere by burning fossil fuels.

This increase in greenhouse gases is causing an increase in the rate of the greenhouse effect .

The Greenhouse�Effect

The earth is warming rather like the inside of a greenhouse. On a basic level the sun’s rays enter the earths atmosphere and are prevented from escaping by the greenhouse gases. This results in higher world temperatures.

In more detail………

Energy from the sun drives the earth's weather and climate, and heats the earth's surface; in turn, the earth radiates energy back into space. Atmospheric greenhouse gases (water vapor, carbon dioxide, and other gases) trap some of the outgoing energy, retaining heat somewhat like the glass panels of a greenhouse.�

Without this natural "greenhouse effect," temperatures would be much lower than they are now, and life as known today would not be possible. Instead, thanks to greenhouse gases, the earth's average temperature is a more hospitable 60°F. However, problems may arise when the atmospheric concentration of greenhouse gases increases. �

What are the�greenhouse gases?

Since the beginning of the industrial revolution, atmospheric concentrations of carbon dioxide have increased nearly 30%, methane concentrations have more than doubled, and nitrous oxide concentrations have risen by about 15%. Why are greenhouse gas concentrations increasing?

Burning of fossil fuels and other human activities are the primary reason for the increased concentration of carbon dioxide.

CFC’s from aerosols, air conditioners, foam packaging and refrigerators most damaging (approx 6%).

Methane is released from decaying organic matter, waste dumps, animal dung, swamps and peat bogs (approx 19%).

Nitrous Oxide is emitted from car exhausts, power stations and agricultural fertiliser (approx 6%).

The major contributor is Carbon Dioxide (approx 64%).

Task 1:The �Greenhouse Effect

Complete your worksheet by cutting and labeling the diagram and answering the questions

Task 2 : Effects of global warming

You are about to see a series of pictures which show some of the effects of global warming.

Draw a rough sketch then write down the effects or titles for the pictures you've drawn

I’m thinking !

What are the consequences of Global Warming?

What are the pictures showing, what are the effects of global warming?

How did�you do?

Hurricanes –extreme weather

Flooding of coastal areas

Desertification

Ice caps melt

Rise in temperatures

Loss of wildlife habitats and species

Sea level rise

Extreme storms

There are also some positive effects of global warming

  • Decrease in death and disease
  • Healthier, faster growing forests due to excess CO2
  • Longer growing seasons
  • Warmer temperatures (UK Mediterranean climate!!)
  • Plants and shrubs will be able to grow further north and in present desert conditions
  • Heavier rainfall in certain locations will give higher agricultural production (Rice in India, Wheat in Africa).

How can Global Warming be reduced?

  • Reduce the use of fossil fuels. A major impact would be to find alternatives to coal, oil and gas power stations.
  • Afforest areas, trees use up the CO2, reduce deforestation.
  • Reduce the reliance on the car (promote shared public transport).
  • Try to use energy efficiently (turn off lights and not use as much!).
  • Reduce, Reuse, Recycle.
  • Careful long term planning to reduce the impact of global warming.
  • Global Warming is the increase in global temperatures due to the increased rate of the Greenhouse Effect.
  • Greenhouse gases trap the incoming solar radiation, these gases include Carbon Dioxide, CFCs, Methane, Nitrous Oxides and other Halocarbons. These are released by human activity.
  • We need the Greenhouse effect to maintain life on earth as we know it…however if we keep adding to the Greenhouse gases there will be many changes.
  • Consequences can be negative ( ice caps melt, sea level rise, extreme weather conditions) or positive (more rain in drought areas, longer growing season).

Re do diagram slide 7

http://www.flickr.com/photos/wwworks/2222523486/ - slide 1

http://www.flickr.com/photos/dzwjedziak/375723120/ - slide 8 and 1

http://www.flickr.com/photos/bratan/452189020/ - slide 4

http://www.flickr.com/photos/hogbard/412932972/- slide 6

http://www.flickr.com/photos/tiger_empress/467671978/ - slide 8

http://www.flickr.com/photos/48135670@N00/97951579/ - slide 9,12

http://www.flickr.com/photos/60158441@N00/177929708/ - slide 9,12

http://www.flickr.com/photos/andzer/1480068258/ - slide 9,12

http://www.flickr.com/photos/nickrussill/146743082/ - slide 9,12

http://www.flickr.com/photos/dasha/443747644/ - slide 10,13

http://www.flickr.com/photos/11371618@N00/469788104/ - slide 10,13

http://www.flickr.com/photos/mikebaird/2087879492/ - slide 10,13

http://www.flickr.com/photos/7471118@N02/432453250/ - slide 10,13

http://www.flickr.com/photos/madron/2595909135/ - slide 11

http://www.flickr.com/photos/chi-liu/491412087/ - slide 12,13

http://www.flickr.com/photos/fabbriciuse/2073789872/ - slide 16

http://www.flickr.com/photos/algo/92463787/ - slide 16

http://www.flickr.com/photos/nickwheeleroz/2295584401/ - slide 16

http://www.flickr.com/photos/andidfl/229169559/ - slide 16

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What’s Going On in This Graph?

Teach About Climate Change With 30 Graphs From The New York Times

A new collection to explore our planet’s warming oceans, intensifying storms and rising air temperatures, as well as its greenhouse gas emissions and climate solutions.

Source: Berkeley Earth Land/Ocean Temperature Record

By Michael Gonchar

How can we help students really see climate change when it is a planet-wide process gradually unfolding over decades? Any given hurricane, prolonged drought or scorching hot day (or summer ) might be more likely to occur because of the changing climate. But there will always be weather anomalies; just like in sports, records will be set.

Images can be very powerful (like a video of a starving polar bear ), and they can be an important resource in helping young people to see the effects of a warming planet. But perhaps no visual can tell the story of climate change more succinctly, and more effectively, than graphs. Because a single graph can show change over time.

In this teaching resource, we have gathered 30 graphs previously published in The New York Times that relate to climate change. We organize them by topic: rising air temperature, intensifying storms and changing precipitation, warming oceans, greenhouse gas emissions, and climate solutions. Above each graph you’ll find the link to the original Times article. Scroll down to the bottom of this post to find teaching strategies for using one or more of these graphs in your classroom.

Note: For more climate-related graphs, visit this post from 2019.

Rising Air Temperature

Graph 1: From “ It’s Not Your Imagination. Summers Are Getting Hotter. ”

Graph 2: From “ Here’s Where Global Heat Records Stand So Far in July ”

A graph showing daily global surface air temperatures for every year since 1979.

Graph 3: From “ Why We’re Experiencing So Many Unusually Hot Summer Nights ”

Graph 4: From “ Earth Was Due for Another Year of Record Warmth. But This Warm? ”

Graph 5: From “ A New Era in Global Heat ”

Graph 6: From “ The Last 8 Years Were the Hottest on Record ”

Graph 7: From “ Opinion | I Study Climate Change. The Data Is Telling Us Something New. ”

Global warming may have accelerated in the past 15 years

Annual average temperatures since 1850

Graph 8: From “ See How 2023 Shattered Records to Become the Hottest Year ”

Intensifying Storms and Changing Precipitation

Graph 9: From “ Every Country Has Its Own Climate Risks. What’s Yours ? ”

Graph 10: From “ Every Place Has Its Own Climate Risk. What Is It Where You Live? ”

presentation on global warming

Risk level (low to very high)

Extreme heat

Water stress

Sea level rise

presentation on global warming

Extreme rainfall

Graph 11: From “ These Maps Tell the Story of Two Americas: One Parched, One Soaked ”

Graph 12: From “ These Maps Tell the Story of Two Americas: One Parched, One Soaked ”

Warming Oceans

Graph 13: From “ What This Year’s ‘Astonishing’ Ocean Heat Means for the Planet ”

Graph 14: From “ What This Year’s ‘Astonishing’ Ocean Heat Means for the Planet ”

Graph 15: From “ What This Year’s ‘Astonishing’ Ocean Heat Means for the Planet ”

Graph 16: From “ Where’s All the Antarctic Sea Ice? Annual Peak Is the Lowest Ever Recorded. ”

Graph 17: From “ Antarctic Sea Ice Is at a ‘Very Concerning’ Record Low ”

Greenhouse Gas Emissions

Graph 18: From “ Who Has the Most Historical Responsibility for Climate Change? ”

Graph 19: From “ Who Has the Most Historical Responsibility for Climate Change? ”

Graph 20: From “ Who Has the Most Historical Responsibility for Climate Change? ”

Graph 21: From “ How Electricity Is Changing, Country by Country ”

Graph 22: From “ How Electricity Is Changing, Country by Country ”

Graph 23: From “ U.S. Carbon Emissions Fell in 2023 as Coal Use Tumbled to New Lows ”

Climate Solutions

Graph 24: From “ Yes, There Has Been Progress on Climate. No, It’s Not Nearly Enough. ”

Graph 25: From “ How Electricity Is Changing, Country by Country ”

Graph 26: From “ The Clean Energy Future Is Arriving Faster Than You Think ”

Graph 27: From “ The Clean Energy Future Is Arriving Faster Than You Think ”

Graph 28: From “ U.S. Carbon Emissions Fell in 2023 as Coal Use Tumbled to New Lows ”

Graph 29: From “ Where Wind and Solar Power Need to Grow for America to Meet Its Goals ”

Graph 30: From “ Which Elected Leaders Should Do More on Climate? What Americans Say, in Four Maps. ”

Strategies for Teaching With This Collection

1. Notice and wonder.

For more than seven years we have been collaborating with the American Statistical Association to bring New York Times graphs into classrooms via our What’s Going On in This Graph? activity. Each week we post a new graph and then invite students to respond to four open-ended prompts:

What do you notice?

What do you wonder?

How does this relate to you and your community?

Create a catchy headline that captures the graph’s main idea.

Teachers can use this same activity with one or more graphs from this collection. Students can journal individually or share their observations with a partner before moving into a class discussion. Or, you can host the conversations online (similar to our comments section ), where students post their ideas in an online classroom forum and the teacher and other students submit replies with the goal of helping one another deepen their analysis.

For more detailed information about how to use this approach, visit our previous climate change graph collection , or watch our three-minute tutorial or 45-minute webinar .

2. Read and react.

Invite students to pick any graph from the collection and click on the article link above it. Then they should read the piece and answer these questions:

How does the article contribute to your understanding of climate change?

What role do the graphs embedded in the article serve? Do they make it better? If you were the article’s editor, would you have made the decision to include the graphs? Why, or why not?

What other questions do you have after reading the article?

3. Investigate.

To create each of the graphs in this collection, the Times graphics team used data from one or more sources. Ask students to find the source of the data, which is labeled on the graph itself or in the article, and then investigate using the following prompts:

Who collected this data? Why did they collect it?

How did they collect it? What was their methodology?

When was this data collected? Is it still current?

Is this data accurate and reliable? How do you know?

What do you think about the way Times editors decided to present the data visually in a graph? Do you think they made the right choices? Why, or why not?

How else could this data be presented?

There are 30 graphs in this collection. Assign students to work in pairs or small groups, and then have them discuss which graph they think is most effective for teaching the general public about Earth’s changing climate. Or, have students choose a few. Then they should explain why they selected that graph — or those graphs.

Got any suggestions?

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Global Warming vs. Climate Change

Global warming vs. climate change presentation, free google slides theme and powerpoint template.

We only have one planet, and we must take care of it. It is our home, and it will be the home of future generations (we are not yet certain of the existence of the typical spaceship from the movies that will take us beyond the Solar System). Concepts such as global warming and climate change are on the agenda given the imperative need to take care of the Earth. However, are they the same, where do they differ, and is one the result of the other one? Slidesgo has designed this template to talk about these concepts, their differences and all that they imply in our lives. In addition, you can easily modify the presentation and adapt it to the content you need. It would also be a very good idea to use it to raise awareness about the climate events that can happen on our planet if we don't start making changes now.

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  • Includes information about fonts, colors, and credits of the free resources used

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    global warming, the phenomenon of increasing average air temperatures near the surface of Earth over the past one to two centuries.

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    Article Vocabulary Global warming is the long-term warming of the planet's overall temperature. Though this warming trend has been going on for a long time, its pace has significantly increased in the last hundred years due to the burning of fossil fuels. As the human population has increased, so has the volume of fossil fuels burned.

  3. PPTX World Wide Fund for Nature

    The presentation consists of 12 slides that introduces the topic of climate change. By learning more about the science and geography that affects our world, young people can understand what needs to be done, recognise what matters most to them, and take action to help protect people, places, wildlife and things they love.

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    Global Warming Presentation Free Google Slides theme and PowerPoint template Global warming has been a hot topic for decades (no pun intended) and will in all probability continue to be one for years to come. So how do you explain the phenomenon, its causes and consequences to your elementary students?

  5. Global Warming 101

    A: Global warming occurs when carbon dioxide (CO 2) and other air pollutants collect in the atmosphere and absorb sunlight and solar radiation that have bounced off the earth's surface.Normally ...

  6. PDF Introduction to Climate Change

    Climate change (sometimes called global warming) is the process of our planet heating up. Our planet has already warmed by an average of 1°C in the last 100 years and if things don't change, it could increase by a lot more than that.

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    What is global warming, explained The planet is heating up—and fast. 2:49 Causes and Effects of Climate Change By Christina Nunez Published January 22, 2019 • 7 min read Glaciers are melting, sea...

  8. What is Climate Change? PowerPoint Presentation

    Publication Date. Wed, 06/01/2022 - 12:00. Authors. Morgan Lawrence. PDF Document. What is Climate Change? PowerPoint Presentation (1.6 MB) Return to top.

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    This 55-slide presentation is a guide through the basics of climate change, outlining its causes, impacts, and solutions. This climate change overview is unique because it includes an array of...

  10. PDF Climate change and the sustainable development agenda

    Global Warming of 1.5 °C, an IPCC special report on the impacts of global warming of 1.5°C above pre-industrial levels and related global greenhouse gas emission pathways, in the context of ...

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    Video: Global Warming Broken Down by Latitude Zone (1880-2022) Video: Southern Hemisphere ozone between July 1 and December 31 for selected years between 1979 and 2018. ... Karen St. Germain, NASA's director of Earth science, gave a presentation at the 2021 United Nations Climate Change Conference. Video: What NASA Knows from Decades of Earth ...

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    The basics of climate change science have been known for a long time, and the predicted impact of a doubling of atmospheric carbon dioxide on global temperature hasn't changed much in 100 years.

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    Other effects could take place later this century, if warming continues. These include: Sea levels are expected to rise between 10 and 32 inches (26 and 82 centimeters) or higher by the end of the ...

  14. Free templates about Global Warming for Google Slides & PPT

    16:9 Causes of Global Warming Lesson for Elementary You don't need to keep looking, you've already found the perfect presentation for your elementary lesson about global warming. Here's what you're going to find in this template: lots of cute stickers of the Earth, tables, graphs, charts, maps… Do you need more?

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  16. Free Google Slides and PPT Templates on Climate Change

    Global Warming vs. Climate Change We only have one planet, and we must take care of it. It is our home, and it will be the home of future generations (we are not yet certain of the existence of the typical spaceship from the movies that will take us beyond the Solar System). Concepts such... Multi-purpose 16:9

  17. Video: Global Warming from 1880 to 2022

    Earth's average surface temperature in 2022 tied with 2015 as the fifth warmest on record, according to an analysis by NASA. Continuing the planet's long-term warming trend, global temperatures in 2022 were 1.6 degrees Fahrenheit (0.89 degrees Celsius) above the average for NASA's baseline period (1951-1980), scientists from NASA's Goddard ...

  18. Global Warming Powerpoint Templates and Google Slides Themes

    Take your presentations on global warming to the next level with a global warming PowerPoint template. Whether you're an environmental scientist, educator, or climate activist, these templates will help you deliver your message with impact and professionalism. With a range of customizable slides, you can easily present data, explain concepts ...

  19. Global Warming

    Global warming is the increase in the world's average temperature, believed to be the result from the release of carbon dioxide and other gases into the atmosphere by burning fossil fuels. This...

  20. Global Warming Consequences and Effects

    Education Ads Global Warming Consequences and Effects Presentation Free Google Slides theme and PowerPoint template We must take action now: this world is facing a big problem right now called global warming. It's causing respiratory diseases and a rise in sea levels, among other things.

  21. 30 Climate Change Graphs

    Global warming may have accelerated in the past 15 years. Annual average temperatures since 1850. 1850 . 1900 . 1950 . 2000 . 0 . 0.5 . 1 . 1.5°C above preindustrial levels . 2023 to date.

  22. Climate change: The world just marked a year above a critical limit of

    Global warming surpassed 1.5 degrees Celsius over the past 12 months for the first time on record, new data shows, breaching a critical threshold that, if it continues, will push the limits of ...

  23. How to know when the world has passed 1.5°C of global warming

    Temperatures have been exceeding the 1.5°C threshold over single days for roughly a decade (see chart 2) and their seasonal fluctuations make single days a poor indicator of long-term warming.

  24. Climate Change

    Are you preparing a presentation on climate change for class? Surprise your teacher with this professional template. It has green colors, connected to the environment, and includes pedagogical illustrations related to ecology. It has a guide index to help you focus your presentation.

  25. World breaches critical global warming limit over a year for first time

    Global warming surpassed 1.5 degrees Celsius over the past 12 months for the first time on record, new data shows, breaching a critical threshold that, if it continues, will push the limits of ...

  26. Municipal Vulnerability Index Tool Climate Council Presentation

    Global Warming Solutions Act. About; Read the Plan; Vermont Climate Council; Measuring & Assessing Progress. Greenhouse Gas Inventory; Measuring & Assessing Progress Tool; Resilience Strategy; Get Involved. Get Involved; Calendar; Resources; Search Submit Disclaimer. Municipal Vulnerability Index Tool Climate Council Presentation. Date ...

  27. Global Warming Facts

    Global warming is a real problem that is already causing catastrophes in the world. In order to convince everyone to collaborate in stopping this threat to our planet, there is nothing better than scientific facts.

  28. Global Warming vs. Climate Change

    Global Warming vs. Climate Change Presentation Free Google Slides theme and PowerPoint template We only have one planet, and we must take care of it. It is our home, and it will be the home of future generations (we are not yet certain of the existence of the typical spaceship from the movies that will take us beyond the Solar System).