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IB DP Biology Study Notes

4.12.1 Anthropogenic Causes

Human activities have markedly influenced the Earth's climate. This section delves deep into the anthropogenic reasons for the upsurge in atmospheric concentrations of carbon dioxide and methane, and how we discern correlation from causation, particularly using data from Antarctic ice cores.

Atmospheric Concentrations: Carbon Dioxide (CO₂) and Methane (CH₄)

Carbon Dioxide (CO₂)

  • Origins:
    • Carbon dioxide is naturally present in Earth's atmosphere.
    • Primary sources encompass respiration in living organisms, decomposition of organic matter, emissions from the ocean, and output from volcanic eruptions.
  • Anthropogenic Emission:
    • Burning of Fossil Fuels: Coal, oil, and natural gas, when combusted for energy and transportation, emit significant amounts of CO₂. As the world's dependence on fossil fuels has increased, so have CO₂ levels.
    • Deforestation: Trees absorb CO₂ and provide oxygen. However, large-scale deforestation, mainly for agriculture or urbanisation, reduces the Earth's capacity to absorb CO₂.
    • Industrial Processes: Activities such as cement production release large quantities of CO₂ as a by-product.
  • Effects on the Atmosphere:
    • CO₂ is a major greenhouse gas. It absorbs and emits infrared radiation, causing the Earth's temperature to rise.
    • This enhanced greenhouse effect has been central to global warming and climatic changes.

Methane (CH₄)

  • Origins:
    • Produced both naturally and through human activities.
    • Natural processes like wetland microbial activity, digestive processes of herbivores, and termite metabolism contribute to its production.
  • Anthropogenic Emission:
    • Agriculture: Rice paddies produce methane during the decomposition of organic matter in flooded fields. Livestock, especially cattle, produce methane during digestion.
    • Waste Management: Landfills emit methane as organic waste breaks down anaerobically.
    • Energy Sector: Coal mining releases methane trapped within coal seams. Also, during the extraction and transportation of natural gas, methane can leak into the atmosphere.
  • Effects on the Atmosphere:
    • Although present in smaller concentrations compared to CO₂, methane's capability to trap heat in the atmosphere is far superior.
    • Its concentration, due to anthropogenic activities, has been increasing at a concerning rate, intensifying its greenhouse effect.
A pie chart showing global greenhouse gas emissions by sector.

Image courtesy of Our World in Data

Correlation vs Causation: Antarctic Ice Core Data

Understanding Correlation

  • Definition: A statistical measure that expresses the extent to which two variables change in relation to each other.
  • Implication: A strong correlation does not mean one variable caused changes in another, merely that they tend to vary together.

Understanding Causation

  • Definition: An established cause-and-effect relationship, implying direct influence and change.
  • Implication: To establish causation, researchers often conduct controlled experiments, but in cases like climate change, this is impractical, so multiple lines of evidence are used.

Antarctic Ice Cores: Deciphering Climate's Past

  • Formation:
    • Layers of snow compact over centuries to form ice sheets.
    • Each layer, encapsulating tiny air bubbles, gives a glimpse into the atmosphere of that time.
  • Ice Core Analysis:
    • By extracting and studying these air bubbles, scientists deduce past concentrations of greenhouse gases.
    • Ice cores from Antarctica have offered invaluable data, encompassing over 800,000 years.
Antarctic Ice Cores analysis

Image courtesy of NASA Climate Change

Correlation in Ice Core Records

  • Historical Record:
    • The data from ice cores displays a distinct correlation between CO₂ and CH₄ concentrations and Earth's temperature.
    • Times with elevated levels of these gases align with warmer global conditions, whereas reduced levels correspond to cooler periods or ice ages.

Making Sense of Correlation and Causation

  • Questioning the Data: It's crucial to ask whether CO₂ and CH₄ changes drove temperature alterations or were a result of them.
  • Other Climate Drivers:
    • Factors like Earth's orbital changes, volcanic activity, and variations in solar radiation have historically impacted climate.
    • However, the swift and significant recent uptick in greenhouse gases and temperatures, especially in the past century, hints at a dominant anthropogenic influence.
  • Weighing the Evidence:
    • While correlation does not prove causation, the overwhelming consistency across multiple data sources underscores a likely causal relationship between human-induced greenhouse gas emissions and the current trend of global warming.

FAQ

While carbon dioxide (CO₂) is naturally released into the atmosphere from sources like respiration, ocean emissions, and volcanic eruptions, anthropogenic emissions have introduced an imbalance. Natural sources are generally offset by natural sinks, like forests and oceans absorbing CO₂. However, human activities, particularly the burning of fossil fuels, deforestation, and certain industrial processes, have significantly amplified CO₂ emissions without a corresponding increase in natural sinks. Consequently, a larger proportion of CO₂ remains in the atmosphere, intensifying the greenhouse effect. Over recent decades, anthropogenic emissions have been responsible for the majority of the increase in atmospheric CO₂ concentrations, overshadowing the contributions from natural sources.

Distinguishing between correlation and causation is crucial in climate change research because establishing a mere correlation between two variables does not mean that one directly causes changes in the other. For instance, while there's a correlation between increasing greenhouse gas concentrations and rising global temperatures, it's essential to determine whether the gases drive temperature changes or if there's another underlying cause. Establishing causation requires rigorous scientific evidence and often multiple lines of inquiry. In the realm of climate change, proving causation helps policymakers and the public understand the direct implications of human actions on global warming, ensuring more informed decisions about mitigation and adaptation.

Human activities have significantly disrupted the carbon cycle, which naturally balances the input and removal of carbon dioxide (CO₂) from the atmosphere. Deforestation reduces the number of trees that act as carbon sinks, absorbing CO₂ and storing carbon. Large-scale burning of fossil fuels releases vast amounts of CO₂ that had been sequestered underground for millions of years. Moreover, changes in land use, such as the conversion of forests to agricultural lands, release the stored carbon in trees and soil back into the atmosphere. Urbanisation and industrialisation also contribute to higher energy consumption and subsequent CO₂ emissions. These anthropogenic disturbances in the carbon cycle have led to an imbalance, resulting in steadily increasing atmospheric CO₂ concentrations.

Elevated concentrations of greenhouse gases, particularly carbon dioxide and methane, intensify the greenhouse effect, leading to global warming. As the Earth's average temperature rises, it disrupts and alters global climate patterns. This disruption manifests as more frequent and severe extreme weather events. For instance, warmer temperatures enhance the rate of evaporation, leading to more intense rainfall and flooding in certain regions, while simultaneously causing prolonged droughts in others. The warmer atmosphere holds more moisture, making storms like hurricanes more intense. Melting ice and expanding seawater due to warming further contribute to rising sea levels, escalating the risk of coastal flooding. In essence, the heightened greenhouse effect due to anthropogenic emissions is a significant driver behind the increased incidence and severity of extreme weather events.

Methane emissions from human activities predominantly stem from the agricultural sector, waste management, and the energy sector. In agriculture, rice paddies produce methane during the anaerobic decomposition of organic matter in the waterlogged fields. Livestock, particularly cattle, produce methane during their digestive processes. In waste management, landfills are a major source of methane as organic waste breaks down in the absence of oxygen. Furthermore, the energy sector emits methane during coal mining and the extraction and transportation of natural gas. Despite its lower concentration in the atmosphere compared to carbon dioxide, methane is over 20 times more effective at trapping heat, making its greenhouse effect substantially more potent on a per molecule basis.

Practice Questions

Explain the anthropogenic sources of carbon dioxide and methane, and describe their impact on the greenhouse effect and global warming.

Carbon dioxide (CO₂) has several anthropogenic sources. The burning of fossil fuels such as coal, oil, and natural gas for energy and transport is the primary contributor. Industrial processes, especially cement production, also emit significant CO₂. Deforestation further exacerbates the problem by reducing the number of trees that can absorb CO₂. Methane (CH₄), on the other hand, has its primary anthropogenic origins from agriculture, particularly from rice cultivation and cattle breeding. Landfills and the energy sector, especially coal mining and natural gas extraction, are also notable contributors. Both CO₂ and CH₄ are potent greenhouse gases. While CO₂ is more prevalent, methane is considerably more effective at trapping heat on a per molecule basis. Their increasing concentrations amplify the greenhouse effect, leading to global warming, thereby altering the Earth's climate.

Antarctic ice cores have provided valuable insights into past atmospheric conditions. Elaborate on how they help in distinguishing between correlation and causation in the context of greenhouse gas concentrations and global temperatures.

Antarctic ice cores are formed from compacted layers of snow, each encapsulating air bubbles that offer a snapshot of past atmospheric compositions. By analysing these bubbles, scientists have discerned historical concentrations of greenhouse gases. These data sets have consistently shown correlations between atmospheric concentrations of CO₂ and CH₄ and global temperatures. During periods with elevated levels of these gases, the Earth experienced warmer conditions, and conversely, lower levels matched cooler periods or ice ages. However, mere correlation does not establish causation. While factors like Earth's orbital changes and solar radiation variations have historically impacted the climate, the recent rapid increase in greenhouse gases and temperatures hints at a dominant human influence. The consistency across multiple data sources and the unprecedented speed of current changes suggest a causal relationship between anthropogenic greenhouse gas emissions and contemporary global warming.

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