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Temperature rise

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Atmospheric Science

Definition

Temperature rise refers to the increase in Earth's average surface temperature due to various factors, including greenhouse gas emissions and changes in land use. This phenomenon is closely linked to climate change, as rising temperatures can alter weather patterns, affect ecosystems, and influence global climate systems. Understanding temperature rise is essential for assessing the impacts of climate change and for making projections about future climate scenarios.

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5 Must Know Facts For Your Next Test

  1. Global average temperatures have risen by approximately 1.2°C since the late 19th century, primarily due to human activities such as burning fossil fuels.
  2. Temperature rise can lead to severe weather events, including increased frequency and intensity of heatwaves, storms, and heavy precipitation.
  3. Melting polar ice caps and glaciers contribute to rising sea levels, which can exacerbate coastal flooding and threaten ecosystems and communities.
  4. Rising temperatures affect biodiversity by altering habitats and species distributions, leading to shifts in ecosystems and increased extinction rates.
  5. The rate of temperature rise is projected to accelerate if current trends in greenhouse gas emissions continue, with potential increases of 1.5°C or more by the end of the century.

Review Questions

  • How does temperature rise relate to the concept of radiative forcing, and what role do greenhouse gases play in this relationship?
    • Temperature rise is directly influenced by radiative forcing, which measures how much energy from the sun is absorbed or reflected by Earth’s atmosphere. Greenhouse gases, such as carbon dioxide and methane, enhance the greenhouse effect by trapping heat within the atmosphere. As concentrations of these gases increase due to human activities, the energy balance shifts, resulting in a net positive radiative forcing that leads to an increase in Earth's average surface temperature.
  • What are some climate feedback mechanisms that could be triggered by temperature rise, and how might they impact future climate scenarios?
    • Temperature rise can initiate several climate feedback mechanisms that may either amplify or mitigate further warming. For instance, melting ice reduces the Earth's albedo effect, causing more sunlight to be absorbed and leading to additional warming. Similarly, increased temperatures can result in greater evaporation rates, which contribute to more water vapor in the atmosphere—a potent greenhouse gas—thus intensifying warming. These feedback loops make predicting future climate scenarios increasingly complex as they can accelerate the effects of initial temperature increases.
  • Evaluate the implications of projected temperature rises on global ecosystems and human societies, considering both immediate and long-term effects.
    • Projected temperature rises pose significant challenges for both global ecosystems and human societies. Immediate effects include disruptions to weather patterns that can lead to food insecurity due to crop failures or water scarcity from altered precipitation patterns. Long-term implications involve habitat loss and species extinction as ecosystems struggle to adapt to rapid changes. Additionally, communities may face increased risks from extreme weather events, health issues related to heat exposure, and economic strains due to infrastructure damage. The interconnectedness of these impacts highlights the urgent need for effective mitigation strategies.
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