Related Experiment Video
Updated: May 27, 2026

06:27
Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer
Published on: May 29, 2019
Aerosol indirect effect on biogeochemical cycles and climate
1Department of Earth and Atmospheric Sciences, Atkinson Center for the Sustainable Future, Cornell University, Ithaca, NY 14850, USA.
Summary
Anthropogenic aerosols impact climate through direct and indirect effects. A newly identified indirect effect via biogeochemical feedbacks, driven by CO(2) changes, has a significant cooling impact, potentially increasing climate mitigation costs.
Area of Science:
- Climate Science
- Atmospheric Chemistry
- Biogeochemistry
Background:
- The climate impact of anthropogenic aerosols is typically assessed by direct radiative and indirect aerosol-cloud interaction effects.
- A longer-term aerosol impact through biogeochemical feedbacks, primarily altering atmospheric CO(2) concentrations, has been less explored.
Purpose of the Study:
- To quantify the net biogeochemical effect of anthropogenic aerosols on climate.
- To assess the implications of this effect for climate mitigation strategies and carbon targets.
Main Methods:
- Analysis of aerosol impacts on land and ocean biogeochemical cycles.
- Estimation of the radiative forcing equivalent of the net biogeochemical effect.
Main Results:
- Aerosols influence biogeochemical cycles through physical forcing, nutrient addition, and pollutant effects.
- The net biogeochemical effect of aerosols is estimated to cause a radiative forcing of -0.5 ± 0.4 watts per square meter.
Conclusions:
- The indirect climate effect of aerosols via biogeochemical feedbacks is substantial.
- Achieving lower carbon targets may be more economically challenging than previously projected due to these aerosol effects.
Related Concept Videos
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...
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.
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 are Biogeochemical Cycles?
The most common elements in organic molecules, carbon, hydrogen, oxygen, nitrogen, sulfur, and phosphorus, are only available in the ecosystem in limited amounts. Therefore, these nutrients must be recycled through both biotic and abiotic components of the ecosystem, in processes generally called biogeochemical cycles.
The Sulfur Cycle
Sulfur, an important element in the chemical makeup of proteins, is recycled through the atmosphere and aquatic and terrestrial environments. Found in the atmosphere as sulfur dioxide (SO2), sulfur is released by decaying organisms, weathered rocks, geothermal vents, volcanos, and burning fossil fuels. It is deposited into the ecosystem, cycled through the biotic community, and either released back into the atmosphere as gas or deposited in marine sediment for long-term storage and eventual...
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.

