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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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Updated: May 26, 2025

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A long-term decline in downward surface solar radiation.

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|February 24, 2025
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Summary

Downward surface solar radiation (DSSR) declined globally from 1959-2014 due to greenhouse gases and aerosols. Future DSSR depends on climate scenarios, with reduced aerosols and moderate warming suggesting a brighter outlook.

Keywords:
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Area of Science:

  • Earth System Science
  • Climate Science
  • Atmospheric Science

Background:

  • Downward surface solar radiation (DSSR) is crucial for Earth's climate system.
  • Past decadal fluctuations in land-based DSSR are documented.
  • Understanding DSSR trends is vital for climate change assessment.

Purpose of the Study:

  • To analyze global DSSR trends from 1959 to 2014.
  • To quantify the contributions of greenhouse gases (GHGs) and aerosols to DSSR changes.
  • To project future DSSR variations based on climate change scenarios.

Main Methods:

  • Utilized station observations and Coupled Model Intercomparison Project Phase 6 (CMIP6) simulations.
  • Analyzed decadal trends in DSSR.
  • Differentiated the impacts of GHGs and anthropogenic aerosols.

Main Results:

  • A consistent global decline in DSSR was observed between 1959 and 2014.
  • Greenhouse gases (GHGs) and anthropogenic aerosols had comparable contributions to this decline.
  • GHG influence, primarily through temperature-driven water vapor increases, became more dominant in the satellite era.
  • Future DSSR changes are predictable using global mean surface temperature (GMST) and aerosol concentrations.

Conclusions:

  • Future DSSR trends are sensitive to climate change scenarios (e.g., SSP245/SSP126).
  • Reduced aerosol concentrations and moderate warming in certain scenarios may halt or reverse the DSSR decline.
  • These findings suggest a potentially brighter future regarding surface solar radiation.