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Global Climate Change01:50

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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The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
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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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Using Generative Art to Convey Past and Future Climate Transitions
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A real-time Global Warming Index.

K Haustein1, M R Allen2,3, P M Forster4

  • 1Environmental Change Institute, University of Oxford, Oxford, UK. karsten.haustein@ouce.ox.ac.uk.

Scientific Reports
|November 15, 2017
PubMed
Summary
This summary is machine-generated.

We developed a real-time index for global human-induced warming, assessing its reliability against climate uncertainties. This tool offers better context for temperature targets and can stabilize climate policy.

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Area of Science:

  • Climate science
  • Earth system science
  • Environmental science

Background:

  • Global warming is a significant concern, necessitating accurate measurement and policy.
  • Existing methods for assessing human impact on climate can be complex and subject to uncertainty.

Purpose of the Study:

  • To introduce a straightforward, real-time index for global human-induced warming.
  • To evaluate the index's resilience against uncertainties in climate forcing and natural climate variations.
  • To provide enhanced scientific context for global temperature stabilization goals and potentially reduce climate policy volatility.

Main Methods:

  • Developing a novel real-time index for global warming.
  • Quantifying uncertainties from temperature observations, radiative forcings, internal climate variability, and model responses.
  • Comparing the proposed index with established methods for estimating human contribution to global temperature change.

Main Results:

  • The proposed index offers a simple, real-time measure of global human-induced warming.
  • The index's robustness was successfully assessed against various sources of uncertainty.
  • The index aligns with more complex methodologies for attributing global temperature changes to human activities.

Conclusions:

  • The developed index provides a reliable and accessible tool for monitoring human-induced warming.
  • This index can improve the scientific basis for climate policy and potentially reduce its fluctuations.
  • The findings support the use of this index for better understanding and managing climate change impacts.