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Global Climate Change

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Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
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Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
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There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...
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Related Experiment Video

Updated: Apr 25, 2026

Monitoring Pedogenic Inorganic Carbon Accumulation Due to Weathering of Amended Silicate Minerals in Agricultural Soils.
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Clouds moderate Amazon deforestation's climate effect.

Gunnar Myhre1

  • 1CICERO Center for International Climate Research, Oslo, Norway.

Science (New York, N.Y.)
|April 23, 2026
PubMed
Summary

Increased cloud cover offers a partial cooling effect, counteracting some of the warming from carbon dioxide emissions. This finding highlights the complex interplay between greenhouse gases and atmospheric conditions.

Area of Science:

  • Climate Science
  • Atmospheric Physics
  • Earth System Science

Background:

  • Carbon dioxide (CO2) emissions are a primary driver of global warming.
  • Cloud cover dynamics are a significant factor in Earth's energy balance.
  • The precise impact of clouds on anthropogenic warming remains an active area of research.

Purpose of the Study:

  • To investigate the influence of increased cloud cover on global temperatures.
  • To quantify the extent to which clouds mitigate CO2-induced warming.
  • To improve climate models by incorporating observed cloud feedback mechanisms.

Main Methods:

  • Analysis of satellite-derived cloud data.
  • Utilizing climate model simulations with varying CO2 concentrations.

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  • Comparing temperature anomalies under different cloud cover scenarios.
  • Main Results:

    • An observed increase in cloud cover was found to partially offset global warming.
    • The cooling effect of enhanced cloudiness was quantified.
    • Model simulations corroborated the observational findings regarding cloud feedback.

    Conclusions:

    • Cloud cover plays a crucial, albeit complex, role in regulating global temperatures.
    • The study provides evidence for a negative feedback loop involving clouds that can dampen warming.
    • Further research is needed to fully understand cloud-aerosol interactions and their impact on climate sensitivity.