Evolution of Climate Change Science

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Create a presentation about climate change

This presentation traces the history of climate change science from 19th-century pioneers like Fourier and Foote to modern insights, highlighting key milestones, the greenhouse effect, paleoclimate ev

November 19, 202511 slides
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Slide 1 - The History of Climate Change Science

The slide features the title "The History of Climate Change Science," which serves as an introduction to the topic. Its subtitle, "From Early Suspicions to Modern Evidence," outlines the progression from initial theories to contemporary scientific proof.

The History of Climate Change Science

From Early Suspicions to Modern Evidence

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Slide 2 - Presentation Agenda

The presentation agenda outlines the historical progression of climate science, starting with early 19th-century discoveries, observations, and scientific theories. It continues through key mathematical models and predictions of that era, 20th-century technological advancements and empirical evidence confirming climate change, and concludes with the environmental, economic, and social impacts plus future implications.

Presentation Agenda

  1. Early Discoveries in Climate Science

Initial observations and scientific theories from the 19th century.

  1. 19th-Century Calculations and Predictions

Key mathematical models and early forecasts of global warming.

  1. 20th-Century Advancements and Evidence

Technological progress and empirical data confirming climate change.

  1. Key Impacts and Future Implications

Environmental, economic, and social consequences of ongoing changes.

Source: Climate Change Presentation

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Slide 3 - Early Suspicions of Climate Change

This section header slide, titled "Early Suspicions of Climate Change," introduces section 02 of the presentation. It highlights that suspicions of ice ages and paleoclimate changes first emerged in the early 19th century.

Early Suspicions of Climate Change

02

Early Suspicions of Climate Change

Ice ages and paleoclimate changes first suspected in the early 19th century.

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Slide 4 - 19th Century Foundations

In the 19th century, Joseph Fourier first proposed the greenhouse effect in 1824, laying early groundwork for understanding atmospheric warming. This was followed by Claude Pouillet strengthening the evidence between 1827 and 1838, and Eunice Newton Foote demonstrating CO2's warming potential in 1856.

19th Century Foundations

  • Joseph Fourier proposes greenhouse effect (1824)
  • Claude Pouillet strengthens evidence (1827-1838)
  • Eunice Newton Foote demonstrates CO2 warming (1856)
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Slide 5 - Key Milestones Timeline

The timeline slide outlines key milestones in the early scientific understanding of the greenhouse effect and human-induced climate change. Starting with Joseph Fourier's 1824 proposal that Earth's atmosphere traps heat like a greenhouse, it progresses through Eunice Newton Foote's 1856 experiments demonstrating CO2's heat absorption, Svante Arrhenius's 1896 calculations of CO2 doubling causing 5-6°C warming, and accumulating 20th-century evidence confirming global warming.

Key Milestones Timeline

1824: Fourier Proposes Greenhouse Effect Joseph Fourier suggests Earth's atmosphere traps heat like a greenhouse. 1856: Foote Demonstrates CO2 Heating Eunice Newton Foote experiments show CO2 absorbs heat from sunlight. 1896: Arrhenius Quantifies Human CO2 Impact Svante Arrhenius calculates that doubling CO2 could warm Earth by 5-6°C. 20th Century: Accumulating Evidence of Climate Change Throughout the 20th century, scientists gather data confirming human-induced global warming.

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Slide 6 - Eunice Newton Foote's Insight

In 1856, pioneering American scientist Eunice Newton Foote conducted an experiment demonstrating that carbonic acid gas (CO2) absorbs and retains solar heat more effectively than other substances. Her quote, "'The highest effect of the sun's rays I have found to be in the case of carbonic acid gas,'" laid the groundwork for understanding the greenhouse effect.

Eunice Newton Foote's Insight

> 'The highest effect of the sun's rays I have found to be in the case of carbonic acid gas.' This 1856 experiment by Eunice Newton Foote revealed CO2's ability to absorb and retain solar heat, laying the foundation for understanding the greenhouse effect.

— Eunice Newton Foote, pioneering American scientist

Source: Demonstrating CO2's heat-trapping properties in 1856

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Slide 7 - Visualizing the Greenhouse Effect

The slide illustrates the greenhouse effect through a visual diagram, showing how sunlight freely enters Earth's atmosphere and is absorbed by the planet, which then radiates heat back out. Greenhouse gases trap this outgoing infrared radiation, leading to natural warming that is enhanced by human activities.

Visualizing the Greenhouse Effect

!Image

  • Sunlight enters Earth's atmosphere freely
  • Earth absorbs heat and radiates it back
  • Greenhouse gases trap outgoing infrared radiation
  • Resulting in natural and enhanced warming

Source: Image from Wikipedia article "Greenhouse effect"

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Slide 8 - Impactful Calculations

The slide "Impactful Calculations" highlights key climate science milestones, including the prediction of a 5-6°C global temperature rise from doubling atmospheric CO2 levels. It also notes Svante Arrhenius's 1896 calculation as the first climate model demonstrating human impact on emissions and an early forecast of CO2's critical role in warming.

Impactful Calculations

  • 5-6°C: CO2 Doubling Warming

Predicted global temperature rise

  • 1896: First Climate Model

Arrhenius calculated human impact

  • Doubling: Atmospheric CO2 Threshold

Early prediction of emissions role

Source: Svante Arrhenius (1896)

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Slide 9 - Paleoclimate vs. Modern Science

Paleoclimate science highlights natural fluctuations in Earth's climate over millennia, driven by factors like orbital changes, volcanic activity, and solar variations, resulting in long-term cycles such as ice ages and warmer interglacials. In contrast, modern science attributes rapid, unprecedented warming since the late 19th century to human activities, including fossil fuel use, deforestation, and industry, which have elevated greenhouse gas levels and disrupted the planet's energy balance.

Paleoclimate vs. Modern Science

Paleoclimate: Natural VariationsModern Science: Human Influence
Earth's climate has naturally fluctuated over millennia due to orbital changes, volcanic activity, and solar variations, leading to ice ages and warmer interglacials. These cycles occur over tens of thousands of years, driven by non-human factors.Since the late 19th century, human activities have rapidly increased greenhouse gas emissions from fossil fuels, deforestation, and industry, disrupting Earth's energy balance and causing unprecedented warming at a pace far exceeding natural changes.
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Slide 10 - 20th Century and Beyond

This section header slide is titled "20th Century and Beyond," marking a key phase in the history of climate science. Its subtitle highlights the growing scientific consensus supported by evidence of human-induced climate change.

20th Century and Beyond

20th Century and Beyond

Scientific consensus grows with evidence of anthropogenic climate change.

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Slide 11 - Conclusion: Lessons from History

The conclusion slide, titled "Lessons from History," highlights how scientific insights from Fourier to the present day underscore the urgent need for action on emissions to combat climate change. It features a subtitle urging immediate steps to protect our planet.

Conclusion: Lessons from History

From Fourier to today, science shows urgent need for action on emissions to mitigate climate change.

Act now to protect our planet.

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