This Will Be My Most Disliked Video On YouTube | Climate Change

Astrum
31 Aug 202322:14

Summary

TLDRThis video explores the history of Earth's global temperature changes and how they relate to modern climate change. It delves into how scientists track past temperatures using ice cores and microscopic organisms, revealing patterns of warming and cooling over millions of years. The video highlights that while Earth's temperatures have fluctuated naturally, the recent rapid rise over the past 100 years is unprecedented and driven by human activity. The discussion emphasizes the urgency of addressing climate change to mitigate its long-term effects, supported by data and historical context.

Takeaways

  • 🌍 Global warming is a hot topic today, with discussions about rising temperatures, fossil fuels, and environmental dangers.
  • đŸŒĄïž Accurate global temperature records have been kept since 1850, but scientists can estimate ancient temperatures using ice cores and air bubbles trapped in glaciers.
  • ❄ Ice cores can help scientists understand past atmospheric composition and temperature by measuring gas levels trapped in ancient ice.
  • 🐚 Tiny marine organisms called foraminifera also help scientists calculate ancient global temperatures by analyzing oxygen isotopes in their shells.
  • 📉 Earth’s temperature has fluctuated over millions of years, with periods much hotter and colder than today, driven by factors like CO2 levels, volcanic activity, and meteor impacts.
  • 🌀 Milankovitch Cycles, which affect Earth’s orbital movement, help explain recurring ice ages and temperature fluctuations over thousands to millions of years.
  • ❗ The recent rise in global temperatures, unlike past patterns, is happening at an unprecedented speed, primarily driven by human activity since the Industrial Revolution.
  • đŸŒ± Similar to how early plants altered Earth's atmosphere, human industrialization is now significantly increasing CO2 and methane levels, warming the planet.
  • ⚠ Rapid climate changes pose a threat to ecosystems, as species may not have enough time to adapt, leading to extinctions or forced migrations.
  • 🛑 While global temperature change has momentum, halting CO2 emissions and using technologies like carbon capture could slow or reverse some effects of climate change.

Q & A

  • What is the primary focus of the video?

    -The video focuses on understanding global warming in the context of Earth's temperature history and exploring how human activity has impacted the recent rapid rise in global temperatures.

  • How do scientists determine the global temperature before modern thermometers?

    -Scientists use methods like ice coring and analyzing the shells of foraminifera. Ice cores trap air bubbles, which can reveal atmospheric composition, while foraminifera shells trap oxygen isotopes, helping scientists estimate past temperatures.

  • What is the significance of foraminifera in studying Earth's temperature history?

    -Foraminifera are tiny organisms whose shells trap oxygen isotopes. Since they have existed for 500 million years, scientists use their shells to estimate global temperatures from much earlier periods, beyond what ice cores can provide.

  • What are the Milankovitch cycles, and how do they impact Earth's climate?

    -Milankovitch cycles refer to periodic changes in Earth's orbital movements that affect its climate. These cycles operate over thousands to millions of years and include changes in Earth's axial tilt and orbital eccentricity, which influence temperature fluctuations and ice ages.

  • Why is the recent uptick in global temperatures considered unusual?

    -The recent rise in global temperatures is unusual because it has occurred in just 100 years, much faster than the natural fluctuations caused by Milankovitch cycles, which typically take thousands to millions of years.

  • How does human activity contribute to global warming?

    -Human activities, especially since the Industrial Revolution, have increased the levels of greenhouse gases like CO2 and methane in the atmosphere, leading to a rapid rise in global temperatures, faster than natural cycles.

  • What are some natural factors that have influenced Earth's temperature in the past?

    -Natural factors include the emergence of life forms like plants that absorb CO2, volcanic activity releasing greenhouse gases, and major events like meteor impacts, which have contributed to significant temperature changes in Earth's history.

  • What are the potential consequences of the current rapid rise in global temperatures?

    -Rapid temperature rise can lead to habitat loss, species extinction, rising sea levels, and more extreme weather patterns. Many ecosystems may struggle to adapt to these fast changes, leading to widespread disruption.

  • What does the IPCC recommend to mitigate the effects of climate change?

    -The IPCC recommends reducing CO2 emissions toward net zero, developing carbon capture and storage technologies, and implementing global policies to slow down or reverse the harmful effects of climate change.

  • Why is context important in discussions about climate change?

    -Context helps differentiate between natural temperature fluctuations that occur over millennia and the recent, rapid rise caused by human activities. Without this broader understanding, it is easy to misunderstand or downplay the urgency of the issue.

Outlines

00:00

đŸ”„ Introduction to Global Warming Concerns

The video opens with a discussion on how global warming has become a frequent topic in media, often sparking heated debates. The presenter, Alex McColgan, explains his hesitation to engage in the conversation earlier but feels there is now valuable information to add. He emphasizes the importance of understanding historical temperature patterns to contextualize the current global temperature rise and addresses the question: 'Are we really the hottest we've ever been?'

05:00

❄ How Scientists Measure Ancient Temperatures

This paragraph explores how scientists determine past temperatures. It starts with a discussion on thermometer-based measurements dating back to 1850, followed by a detailed explanation of ice core sampling, which helps measure ancient atmospheric gas ratios. This allows scientists to estimate historical global temperatures. It concludes by noting that for time periods older than a million years, scientists use tiny organisms like foraminifera to infer temperatures through their shells, similar to ice cores.

10:01

📉 Earth's Temperature Trends Over Millions of Years

The focus shifts to analyzing temperature patterns from 500 million years ago using data from foraminifera. The Earth has experienced significant fluctuations, sometimes 14°C hotter or 5°C colder than today. These changes are partially attributed to factors such as the emergence of plants or volcanic activity. When zooming in on more recent data (last 65 million years), distinct smaller cycles of rapid temperature rises followed by gradual drops—like the occurrence of ice ages—become evident.

15:06

🌍 Milankovitch Cycles and Their Impact on Earth's Climate

The paragraph explains Milankovitch Cycles, long-term orbital movements of the Earth affecting its climate. These cycles occur over tens of thousands to millions of years and influence the Earth's temperature by changing how much sunlight the planet reflects. Earth's axis tilt and orbital eccentricity play roles in periodic ice ages and warmer interglacial periods. Currently, we're in an interglacial phase, but the ongoing rise in global temperature doesn’t align with these long-term cycles.

20:07

⏳ Human Influence and Rapid Temperature Rise

The rapid temperature increase over the last 100 years is highlighted, noting that this change is unprecedented in such a short time frame compared to historical fluctuations. The rise is not linked to Milankovitch Cycles or catastrophic events like meteor strikes. Instead, human activities, especially industrialization and the release of greenhouse gases like CO2, are identified as the primary causes of this swift global temperature rise.

đŸžïž CO2 Levels, Surface Ice, and Extinction Risks

This section delves deeper into how human-induced CO2 levels, now at unprecedented highs, have led to surface ice loss and further heating of the planet. The melting ice diminishes Earth's ability to reflect heat, leading to a feedback loop of rising temperatures. Rapid environmental changes could trigger mass extinctions, as species may struggle to adapt quickly enough to new conditions, forcing them to migrate or die out.

💡 Mitigating Climate Change: Solutions and Challenges

The paragraph discusses the potential solutions to climate change, including reducing CO2 emissions and developing carbon capture technologies like Project Longship in Norway. Although some scientists are skeptical about the efficacy of these methods, large-scale efforts could eventually stabilize or reverse some effects of climate change. The IPCC’s 2021 report is referenced, highlighting the urgency of action to avoid more severe impacts.

🔄 Earth's Climate in Historical Context: What Can Be Done?

The final paragraphs wrap up by emphasizing the delicate balance of Earth's climate, demonstrating how even small changes can have massive long-term impacts. Human activities have sped up natural processes, and while some climate change consequences are irreversible, there is still time to mitigate others. The presenter stresses the importance of consensus on facts to enable global cooperation and underscores that the rapid pace of current climate change is the true concern.

🧠 Mental Health and Climate Overwhelm: BetterHelp Sponsorship

In a sponsored segment, the video shifts focus to mental health, introducing BetterHelp as a solution for those feeling overwhelmed by daily crises like climate change. The presenter highlights the importance of mental health support, explaining how BetterHelp's online therapy services can connect individuals with licensed professionals. The partnership aims to promote mental well-being while supporting the video’s broader climate-related content.

Mindmap

Keywords

💡Global Warming

Global warming refers to the long-term increase in Earth's average surface temperature due to human activities, especially the emission of greenhouse gases. In the video, global warming is the central theme, discussed in relation to rising temperatures, the Industrial Revolution, and its rapid acceleration over the past 100 years compared to historical climate cycles.

💡Milankovitch Cycles

Milankovitch Cycles are long-term changes in Earth's orbit and axial tilt, influencing the planet's climate patterns over tens of thousands to millions of years. The video explains that these cycles are responsible for the periodic ice ages and warmer interglacial periods and contrasts them with the current rapid temperature changes, which cannot be explained by these natural cycles.

💡Ice Cores

Ice cores are cylindrical samples taken from glaciers or ice sheets that contain trapped air bubbles from different historical periods. In the video, they are described as a method scientists use to estimate past global temperatures by analyzing the gases trapped in these air bubbles. This technique provides crucial insights into Earth's historical climate data.

💡Foraminifera

Foraminifera are microscopic, single-celled marine organisms with shells that trap oxygen isotopes, which scientists analyze to estimate global temperatures from millions of years ago. The video highlights the importance of these organisms in understanding Earth's ancient climate patterns, allowing scientists to reconstruct temperatures far beyond the reach of ice core data.

💡Industrial Revolution

The Industrial Revolution refers to the period starting in the late 18th century when human activities significantly increased the use of fossil fuels, leading to mass emissions of greenhouse gases like CO2. The video explains how this event marks a turning point in the acceleration of global warming, contrasting it with the slower, natural climatic changes over millennia.

💡Greenhouse Gases

Greenhouse gases, such as CO2 and methane, trap heat in Earth's atmosphere, leading to global temperature increases. The video explains that rising levels of these gases, particularly from human activities like industrialization and agriculture, are the primary cause of the recent rapid uptick in global temperatures.

💡IPCC (Intergovernmental Panel on Climate Change)

The IPCC is a global organization that compiles scientific data on climate change and provides reports on its effects and possible mitigation strategies. The video refers to the IPCC's reports, which confirm human influence as the dominant cause of recent global warming and emphasize the importance of reducing CO2 emissions to mitigate further climate change.

💡Carbon Capture

Carbon capture refers to technologies designed to remove CO2 from the atmosphere and store it underground or in other secure locations. In the video, projects like Norway's Project Longship are mentioned as potential solutions to help reverse the warming trend, although the speaker expresses skepticism about their effectiveness on a large scale.

💡Interglacial Period

An interglacial period is a warmer phase between ice ages, where polar ice caps retreat, and global temperatures are relatively stable. The video explains that we are currently in an interglacial period within the larger context of an ongoing ice age, but recent human-induced temperature increases are unusual compared to past interglacial phases.

💡Great Oxidation Event

The Great Oxidation Event occurred around 2.4 billion years ago when cyanobacteria began photosynthesizing, releasing oxygen into the atmosphere and significantly cooling Earth's climate. The video uses this event as an example of how even small organisms can drastically alter Earth's atmospheric composition and climate, paralleling the impact of humans on the current climate.

Highlights

Global warming has become a frequent topic in news headlines, and the discussion has become as heated as the climate itself.

The video focuses on contextualizing modern temperature changes by looking at historical climate patterns.

Scientists have been recording global temperatures since 1850 using thermometers, but methods like ice coring allow us to estimate temperatures from before that time.

Ice cores contain air bubbles trapped in snow, allowing scientists to measure past atmospheric compositions and estimate global temperatures from thousands of years ago.

Foraminifera, tiny single-celled organisms with porous shells, provide data on global temperatures from over 500 million years ago using oxygen isotope analysis.

The Earth's temperature has fluctuated dramatically over the past 500 million years, with periods both 14 degrees Celsius hotter and -5 degrees Celsius colder than today.

Temperature changes over the last 65 million years reveal smaller, cyclical fluctuations related to ice ages and interglacial periods.

Milankovitch Cycles, driven by Earth's orbital movements, cause periodic temperature fluctuations over thousands of years.

Human activity, especially since the Industrial Revolution, is the primary driver of the rapid rise in global temperatures seen over the last 100 years.

CO2 levels are now higher than at any point in the last 800,000 years, contributing significantly to climate change.

Melankovic Cycles and human-induced changes in the atmosphere are causing a feedback loop, accelerating the melting of polar ice caps and global warming.

Rapid global temperature changes threaten ecosystems and species, as life cannot easily adapt to fast-changing environments.

The IPCC report confirms human activity is the main cause of global warming and calls for immediate action to reduce CO2 emissions and limit further damage.

Carbon capture projects, such as Norway's Project Longship, aim to reduce CO2 in the atmosphere by storing it underground.

The current rise in temperature is an unprecedented event within Earth's historical patterns, directly linked to human industrialization and activity.

Transcripts

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[Music]

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foreign it's getting hot outside

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nowadays it's difficult to turn on the

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news without hearing someone talking

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about global warming

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headlines are filled with references to

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Rising temperature levels fossil fuels

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and encroaching danger and the

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discussion around the subject has gotten

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as heated as the weather

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this has been a topic I've been wary

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about weighing in on simply because of

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how sensitive a subject it has become in

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recent times

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I've sat on this particular video for

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three years occasionally updating it but

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not quite feeling it was the right time

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to release it I didn't want to Simply

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create more noise

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however I do now think there is

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something worth adding to the discussion

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after all there is plenty we hear about

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the current temperature of the planet

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what is often not talked about is the

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patterns of temperature change that

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existed in the past that contextualize

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that modern temperature

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are we really the hottest we've ever

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been scientists believe that in the last

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100 years the global temperature has

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been increasing but how does this fit

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into wider patterns and Trends and how

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did they find any of this out

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I'm Alex mccolgan and you're watching

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astrum and today we will be taking a

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closer look at the data recording the

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temperature history of our own Planet

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it's only by understanding the ancient

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past that we can contextualize the

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current discussion on global warming and

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answer what exactly are scientists so

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worried about

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so to begin how do we know what the

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temperature used to be

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it's easy to find the current Global

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temperature today all you need is a

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thermometer and you can go outside and

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take a reading

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with enough readings taken at different

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locations around the globe you can find

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an average temperature for the whole

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planet

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scientists have actually been doing this

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since 1850 meaning that our records on

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average global temperatures are fairly

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accurate since this date

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however mercury thermometers were only

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invented in 1714 so how do we know what

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the temperature was before these Global

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readings started being taken how do we

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know the temperature a thousand years

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ago or even a million years ago before

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humans were on the scene

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some of you may already know the answer

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or at least a partial answer

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scientists can approximate global

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temperatures in the past through ice

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Coring

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essentially when snow falls because it

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is powdery it traps little bubbles of

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air where it lands if this snow doesn't

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melt but has more snowfall on it later

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such as in a very cold place like a

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glacier you can end up with layers of

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snow and ice-trapped air bubbles going

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back for many many years it creates

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something similar to the rings on a tree

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by collecting ice form this way

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scientists can take sections to a lab

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and melt it releasing the air relating

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to specific years

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they then can measure the different

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ratios of gases released from the air

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bubbles which tells them the atmospheric

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composition at that time

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and because we can test how much heat is

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retained by a gas when exposed to a

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constant temperature like the sun for

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instance CO2 retains more heat while

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oxygen retains less with enough samples

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scientists can calculate roughly what

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the global temperature was during that

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year

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however the oldest Glaciers are only a

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million or so years old

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to get a good idea of the trends that

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govern global temperatures we're gonna

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have to go back much earlier than that

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how do we know what the global

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temperature was over a million years ago

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the answer might surprise you

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clams

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actually not clams but something similar

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a tiny single cellular organism no

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larger than a full stop called for a

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mini fairer

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like clams these organisms produce

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shells around themselves and these

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shells are slightly porous oxygen in

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particular is taken into the shell and

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trapped there remaining in place even

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when the foreign minifera dies

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so using a similar process to the ice

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cores if scientists can find shells of

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dead foraminifera from a particular year

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they can release that air and work out

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from it the global temperature

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this process is slightly different as

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instead of air composition scientists

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are looking at different oxygen Isotopes

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but basically it's a very similar

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process

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foreign minifera are still around today

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and first came onto the scene 500

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million years ago so they are

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instrumental in helping us get a clear

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picture of global temperatures during

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this much longer time period

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but what is that picture

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Based on data collected from foreign

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minifera it looks something like this

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[Music]

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there is a certain degree of uncertainty

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to this findings get more reliable the

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closer we get to the present day

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but as you can see from General Trends

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the Earth's temperature has undergone

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significant changes over the last 500

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million years

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at times it is Phase temperature

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averages 14 degrees Celsius hotter than

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we have today and at other times about

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-5 degrees Celsius lower

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so we are not the hottest we have ever

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been then again that's not surprising to

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anyone who knew that the surface of the

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Earth when it was just formed was mostly

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magma

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but you may not have expected these

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fluctuations

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why are they happening

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scientists are not entirely sure as

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there doesn't seem to be much of a

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pattern to them on this Grand scale but

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they believe that some of these

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fluctuations are from the emergence of

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new life forms for instance the arrival

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of plants at around 450 million years

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before the present might explain why the

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temperature dropped then

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they started absorbing atmospheric CO2

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and turned it into oxygen which retains

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less heat other changes could have been

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caused by plate tectonics and volcanic

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activity putting more CO2 into the air

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and still other changes could have been

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caused by possible meteor impacts like

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the one that wiped out the dinosaurs

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however this is not the full picture by

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increasing the resolution and zooming in

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slightly we begin to see another

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interesting Trend let's look at the 65

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million year picture

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[Music]

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within the large sweeping changes it

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turns out that there are many smaller

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fluctuations these become more obvious

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when we zoom in again

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and again

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and again

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by this point we can see a distinct

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smaller pattern occurring rapid rises in

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global temperatures followed by gradual

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dips

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it's hard to get your head around the

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sheer scope of the Earth's history but

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each one of these dips represents entire

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ice ages

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ice ages are technically defined as any

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point in Earth's history where there is

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ice on the polar caps something that is

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not always the case so technically as

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I've mentioned in a previous video we

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are in an ice age right now

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however although the general trend of

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the Earth's temperature at the moment is

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towards ice ages we are in something

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known as an interglacial period a span

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of many thousands of years where the

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Earth is temporarily warmer in between

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fall ice ages in the last full Ice Age

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the polar caps reach the UK and parts of

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the US

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but what is causing these dips and Rises

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on our graph

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well I go into more detail about this in

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my video on milankovic Cycles which you

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can watch here but just to brush up on

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them very quickly milankovic Cycles are

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the periodic changes that take place

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within our planet's climate due to

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fluctuations in its orbital movement

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around the Sun

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usually over the course of thousands of

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years

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surface ice affects the temperature of a

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planet the more surface ice a planet has

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the colder the planet tends to be as

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more heat is reflected back into space

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but equally important is the direction

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that surface ice is facing

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consider ice to be like a shield that

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will reflect the sun's Rays if that ice

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is not pointed in the direction of the

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sunlight it cannot reflect it so anytime

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the planet points its surface eyes

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towards the Sun the Earth tends to get

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cooler creating something of a feedback

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loop

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this matters because the Earth's axis

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isn't stable of the span of thousands of

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years it moves back and forth sometimes

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pointing the polar ice caps more towards

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the Sun and sometimes pulling them

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further away

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although this change is only a couple of

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degrees at most it is enough that over

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time it has an impact on the global

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temperature

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the temperature drops as the ice Shield

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faces the Sun and rises again as it

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points away this fluctuation is one

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example of a melanchovic cycle

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there are other melanchovic Cycles which

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are consistent Cycles in the Earth's

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orbit that affect its temperature acting

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on time scales of twenty three thousand

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forty one thousand one hundred thousand

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four hundred and five thousand and 2.4

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million years

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whenever these coincide with each other

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they create even greater changes to the

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global temperature

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you can see the gaps between the ice

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ages in this graph tend to be about 100

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000 years apart perfectly in line with

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one of the milankovic Cycles

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specifically the change in the earth's

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orbital eccentricity but all of the

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Cycles have an impact

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so where are we in relation to one of

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these language Cycles let's zoom in some

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more

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as you can see we have risen out of an

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ice age and have ended a fairly stable

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plateau of global temperature this is

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consistent with the rapid rise in

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temperature slash slow drop in

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temperature that characterizes ice ages

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and the periods between them

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all of human history from the pyramids

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to the present day can be found on this

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plateau

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although humans existed before this

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point they hadn't really got the hang of

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building any civilizations

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scientists have named this Plateau where

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human history began the Hollow Scene

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period

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however the uptick right at the end is

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not so usual

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this uptick represents a rise in the

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global temperature by one degree which

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technically is still roughly on par with

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the interglacial period before our

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current one over 100 000 years ago

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however it is not the temperature change

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that is concerning about this uptick it

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is how quickly it is rising

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unlike all the other changes on all

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these graphs which have taken place over

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hundreds of millions of years at the

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longest and thousands of years at the

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shortest this rise took place in 100

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years this could have a big impact on

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the ecosystems on the planet

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so what could have caused this uptick

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the answer cannot be milankovic Cycles

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as you have seen these Cycles take place

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on the scale of thousands of years at

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least and millions at most even when we

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zoom in on sections of our graph where

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there appear to be sharp upticks we

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realize that these Rises take place over

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a couple of Thousand-Year periods

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Milankovitch cycles are described as a

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weak but consistent forces like the

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trickle of a stream that eventually

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erodes around him they do not create

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effects over such a small time frame as

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100 years

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similarly there has been no cataclysmic

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events such as the one that wiped out

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the dinosaurs which might be our other

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explanation

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that meteor was thought to be 10

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kilometers wide and struck with the

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force of 21 to 921 billion Hiroshima a

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bombs

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about 75 percent of species died in the

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climate change that happened in its

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aftermath if something like that had hit

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Earth since 1850 we would have noticed

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it

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however there is one factor that does

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explain this change in global

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temperatures the activity of humans

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it is not the first time that living

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organisms have had an impact on the

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global temperature remember it is

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believed that some of the changes we see

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here are caused by the introduction of

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plant life absorbing CO2 and releasing

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oxygen

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similarly back when life was still all

play13:28

single-celled organisms about 2.4

play13:31

billion years ago the arrival for the

play13:34

first time of cyanobacteria that could

play13:37

photosynthesize had a massive impact on

play13:40

the atmosphere for the first time an

play13:43

organism started putting oxygen into the

play13:45

atmosphere this occurred at such a rate

play13:48

there was an event known as the great

play13:50

oxidation event which coincided with a

play13:53

significant drop in the global

play13:55

temperature

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some scientists believed the entire

play13:58

world almost froze entirely over as

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there is evidence of glacial activity at

play14:04

the equator a snowball Earth as it came

play14:07

to be known

play14:09

what we learn from this is that the

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balance of global temperatures is very

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delicate a single species that starts to

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change the atmospheric ratio of gases

play14:19

can have a massive impact overloading

play14:22

the subtler effects of melanchovic

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Cycles

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and since 1850 humans have definitely

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changed the way we have been interacting

play14:31

with the atmosphere

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unlike the previous roughly 10 000 years

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of human history since 1760 and the

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Industrial Revolution human activity has

play14:42

produced vast amounts of greenhouse

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gases as a waste product of

play14:46

industrialization and farming

play14:48

in the last four decades Each decade has

play14:52

been the hottest decade on record since

play14:54

we started tracking global temperatures

play14:56

in 1850

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CO2 levels are now at a global average

play15:01

of 410 parts per million and methane at

play15:06

1866 parts per billion Which is higher

play15:09

than we have seen in the last 800 000

play15:11

years which means since before about

play15:14

eight ice ages and interglacial periods

play15:17

between them

play15:19

and importantly the global cover of

play15:21

surface ice has been retreating

play15:23

consistently since 1950. something

play15:27

scientists do not believe to have

play15:29

happened for the last two thousand years

play15:32

as you will recall this has a knock on

play15:35

effect on milankovic Cycles as a planet

play15:37

with less surface ice does not reflect

play15:40

as much heat from the Sun so it tends to

play15:42

get even hotter

play15:44

like pushing a cart down a hill these

play15:47

changes have a certain amount of

play15:48

momentum to them

play15:50

and sadly rapid changes in global

play15:53

temperature tends to lead to species

play15:55

going extinct

play15:57

it normally takes thousands of years for

play16:00

life to adapt to the conditions you

play16:02

might find during an Ice Age woolly

play16:04

mammoths to conditions today elephants

play16:08

natural selection takes time to develop

play16:10

in a species the traits they need to

play16:13

thrive in a new environment

play16:15

if species are not given this time they

play16:18

either have to move to a new environment

play16:20

better suited to them or they will die

play16:23

out

play16:24

as the habitable zones begin to migrate

play16:26

towards the poles some zones will vanish

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completely while new hot desert

play16:32

environments will be created that life

play16:34

in general is poorly adapted to

play16:38

it's important to note that these events

play16:41

are not Unstoppable Global temperature

play16:43

change does have some momentum but if we

play16:47

as humans find ways to stop changing the

play16:49

atmosphere's ratio then in time

play16:52

melanchovic Cycles will take over again

play16:54

and the rise will stop that's why it's

play16:57

so important for governments to listen

play16:59

to reports by institutions like the ipcc

play17:01

an international group of scientists

play17:04

funded by multiple governments tasked

play17:07

with finding out the realities of

play17:09

climate change who in 2021 released

play17:12

their sixth assessment report explaining

play17:14

the physical science basis

play17:17

in it they stated that it is unequivocal

play17:20

that human influence has warmed the

play17:23

atmosphere ocean and land

play17:26

however they also offer suggestions

play17:28

namely the importance of halting or

play17:31

rapidly reducing CO2 emissions towards

play17:34

net zero as CO2 is the largest

play17:37

contributor towards climate change

play17:38

followed by methane

play17:40

they also recommended the development of

play17:43

carbon dioxide removal facilities to be

play17:45

established worldwide

play17:47

some of these are already in operation

play17:49

such as project longship in Norway their

play17:52

aim is to take CO2 out of the atmosphere

play17:55

and bury it beneath the ground

play17:57

interpleted fossil fuel reservoirs

play18:00

the ipcc says that actions like this if

play18:03

widespread enough will reduce Global

play18:06

surface temperature and even reverse

play18:08

certain other processes like

play18:10

acidification of the oceans

play18:12

personally I'm not super convinced by

play18:15

current carbon capture projects but they

play18:18

do exist

play18:19

but these efforts need to be done on a

play18:23

large-scale government level

play18:25

ultimately my aim for this video was to

play18:28

examine what global warming meant within

play18:30

the context of Earth's wider history

play18:33

from it we can see that it's not

play18:35

actually accurate to say that we are the

play18:38

hottest we've ever been and I find that

play18:40

a really fascinating insight

play18:42

however that fact alone is not the

play18:45

reason some people think it is to not

play18:47

worry about the problem climate change

play18:50

is a process that usually takes

play18:52

Millennia I've realized the worrying

play18:55

part is not necessarily the change

play18:57

itself but rather the speed at which it

play19:00

is happening

play19:01

some life forms might get left behind

play19:03

and how will Humanity cope we don't know

play19:07

as we haven't been around long enough to

play19:09

deal with the extremes of the past

play19:11

while human activity has sped up certain

play19:14

elements and while we can undo some of

play19:17

what has been done through our actions

play19:19

now some things like higher sea levels

play19:22

will be with us for up to 1 000 years

play19:25

according to the latest ipcc report we

play19:28

are past the point of no return for 1.5

play19:30

degrees Celsius and will need to make

play19:33

rapid fundamental changes to our society

play19:36

this decade to stop it going any further

play19:39

than that

play19:40

this will be hard

play19:42

there's no way we as a species will be

play19:45

able to achieve this hard path unless we

play19:48

can agree on the facts that underpin it

play19:50

though

play19:51

without the broader context of agreed

play19:53

upon data it will forever be perfectly

play19:55

possible to arrive at a wide range of

play19:57

conclusions and different paths we

play20:00

should take that is why when it comes to

play20:02

any discussion context is so important

play20:06

by looking at the pattern of our

play20:08

planet's history we see that the current

play20:10

uptick in global temperatures is an

play20:13

induced event that doesn't match already

play20:15

existing patterns and it perfectly

play20:18

coincides with human activity debate

play20:21

what you want to do with that

play20:23

information and the best path to take in

play20:25

light of it but these are the facts set

play20:28

in ice and the bones of organisms long

play20:30

dead they will Brook no argument

play20:36

dealing with all the crises that the

play20:38

world seems to throw at you daily can

play20:40

get a little overwhelming sometimes it's

play20:43

important to take care of yourself

play20:44

that's why today's video is in Pay

play20:46

partnership with betterhelp

play20:49

mental health is a cause that is deeply

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important to me and I've seen that when

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someone is struggling it can be hard to

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seek help sometimes but having someone

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to talk to even if it's just to get

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things off your chest can be hugely

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beneficial

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betterhelp is the world's largest

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therapy service and they've made it

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their mission to increase accessibility

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to that vital service for everyone

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their online platform can get you

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registered with a credentialed therapist

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giving you access to a wealth of

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experience as well as that vital

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listening ear

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it's 100 online and remote meaning you

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can call your therapist or send messages

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switch at no additional cost

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I think therapy is something everyone

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can benefit from and there are countless

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stories of people who have seen Better

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Health Service improve their mental

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well-being if better help is something

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that you feel could help you why not

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support the channel and click my link in

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the description below betterhelp.com

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forward slash astrum for a 10 discount

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off your first month I highly recommend

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it

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thanks for watching

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want to learn more about some of the

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Cycles earth goes through check out this

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playlist here a big thanks to my patrons

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and members if you want to support what

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I'm doing and have your name added to

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this list check the links below all the

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best and see you next time

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Étiquettes Connexes
Climate ChangeGlobal WarmingTemperature HistoryEarth ScienceMilankovitch CyclesHuman ImpactIce AgesGreenhouse GasesEnvironmental ScienceSustainability
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