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Related Concept Videos

Microbes and Climate Change01:27

Microbes and Climate Change

Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...
Global Climate Change01:50

Global Climate Change

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.
What is Climate?01:16

What is Climate?

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.
What is Weather?01:07

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The Carbon Cycle01:14

The Carbon Cycle

Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
Radiation: Applications01:17

Radiation: Applications

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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Related Experiment Video

Updated: Jul 3, 2026

Using Generative Art to Convey Past and Future Climate Transitions
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Using Generative Art to Convey Past and Future Climate Transitions

Published on: March 31, 2023

Meteorologically Driven Changes in Future Global Air Quality: Physical and Monetized Impacts.

Erin E McDuffie1, Lee T Murray2, Sebastian D Eastham3

  • 1EPA Office of Atmospheric Protection, Washington, D.C. 20460, United States.

Environmental Science & Technology
|July 2, 2026
PubMed
Summary

Future air pollution changes may reduce deaths by 180,000 annually by 2100 due to fewer fine particulate matter (PM2.5) deaths, despite increased ozone impacts. This offers significant global health and economic benefits.

Keywords:
air pollutionbenefitcostmeteorological projectionsmortality

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Split Point Analysis and Uncertainty Quantification of Thermal-Optical Organic/Elemental Carbon Measurements
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Split Point Analysis and Uncertainty Quantification of Thermal-Optical Organic/Elemental Carbon Measurements

Published on: September 7, 2019

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Last Updated: Jul 3, 2026

Using Generative Art to Convey Past and Future Climate Transitions
06:10

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Split Point Analysis and Uncertainty Quantification of Thermal-Optical Organic/Elemental Carbon Measurements
10:22

Split Point Analysis and Uncertainty Quantification of Thermal-Optical Organic/Elemental Carbon Measurements

Published on: September 7, 2019

Area of Science:

  • Environmental Health Science
  • Atmospheric Chemistry and Physics
  • Climate Change Impact Assessment

Background:

  • Ambient air pollution, including ozone and fine particulate matter (PM2.5), is a major global environmental health risk.
  • Future air pollution impacts depend on population dynamics and climate-driven meteorological changes affecting pollutant levels.
  • Previous global-scale assessments of combined meteorological and population impacts on air pollution mortality are limited.

Purpose of the Study:

  • To quantify the impact of future meteorological and population changes on global air pollution-attributable mortality by 2100.
  • To estimate the monetized health impacts associated with projected changes in air pollution.
  • To analyze regional variations in air pollution impacts under different global warming scenarios.

Main Methods:

  • Utilized output from general circulation, atmospheric chemistry, and health impact models.
  • Isolated the effects of meteorological changes and population projections on air pollution mortality.
  • Assessed sensitivities to meteorological projections, health impact functions, and warming scenarios.

Main Results:

  • Estimated 180,000 fewer annual deaths by 2100 due to meteorologically driven air pollution changes (excluding emission changes).
  • Projected an annual monetized benefit of $7.3 trillion from reduced PM2.5-attributable mortality, offset by increased ozone mortality.
  • Identified regional disparities: Northern Hemisphere shows net pollution decrease (nitrate aerosol), Southern Hemisphere shows net increase (ozone, organic aerosol).

Conclusions:

  • Meteorological changes alone, without emission reductions, are projected to decrease global air pollution mortality by 2100.
  • Significant regional differences exist, with the Southern Hemisphere facing increased mortality risks from ozone and organic aerosols.
  • Future air quality and associated health outcomes are highly sensitive to climate change and population trends.