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Updated: Mar 26, 2026

Measurement of Aerosols Optical Thickness of the Atmosphere using the GLOBE Handheld Sun Photometer
Published on: May 29, 2019
New approaches to quantifying aerosol influence on the cloud radiative effect
Graham Feingold1, Allison McComiskey2, Takanobu Yamaguchi3
1Chemical Sciences Division, Earth System Research Laboratory, National Oceanic and Atmospheric Administration, Boulder, CO 80305; graham.feingold@noaa.gov.
Understanding aerosol-cloud interactions is crucial for climate science. This study proposes a new method using modeling and radiation measurements to better constrain aerosol radiative effects in clouds.
Area of Science:
- Atmospheric science
- Climate modeling
- Radiative transfer
Background:
- Aerosol-cloud interactions significantly impact Earth's radiative balance, but remain a major source of climate model uncertainty.
- Current atmospheric general circulation models lack the resolution to adequately represent complex aerosol-cloud processes.
- Observational constraints on aerosol-cloud interactions are scarce, hindering model validation.
Purpose of the Study:
- To develop a systematic approach for constraining aerosol radiative effects in shallow clouds.
- To bridge the gap between detailed microphysical understanding and large-scale emergent properties of aerosol-cloud systems.
- To improve the accuracy of climate projections by enhancing the representation of aerosol-cloud interactions.
Main Methods:
- A conceptual approach combining routine process modeling with satellite and surface-based shortwave radiation measurements.
- Integration of microphysical detail with scaling and emergent properties of the aerosol-cloud radiation system.
- Utilizing both Darwinian (detailed) and Newtonian (scaling) strategies for system analysis.
Main Results:
- A novel framework for constraining aerosol-cloud radiative effects in shallow clouds has been established.
- The study provides a pathway to merge detailed process understanding with observational data.
- The proposed method offers improved observational constraints for climate models.
Conclusions:
- Accurate representation of aerosol-cloud interactions is essential for reliable climate predictions.
- Combining process modeling with radiation measurements offers a robust strategy to constrain these interactions.
- This research contributes to reducing uncertainties in climate forcing estimates from aerosols.
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