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Author: Cazzy Medley

A schematic diagram describing the impacts of cloud-surface-coupling on the aerosol-cloud-interaction. When a cloud is coupled with the surface, a cloud is formed near the top of the planetary boundary-layer (PBL) that interacts strongly with the well-mixed aerosol, whereas they have little interaction under decoupled conditions. As aerosol alters cloud microphysics (more aerosol leads to more cloud droplets of smaller particle size that makes cloud brighter), solar radiation reflected by cloud is more under coupled conditions than under decoupled conditions, or a stronger cooling effect as indicated by the orange arrows. As a result, lack of accounting for the cloud-surface coupling tends to result in an underestimation of aerosol indirect radiative forcing, which is likely a major contributing factor to the systematic discrepancies between observation-based and model-based estimate of the aerosol cooling effect. Adapted from Su et al. (2024, Sci. Adv.).

Aerosols Affect Climate More Than We Think

A key to improve climate prediction is to improve understanding of the impact of aerosol on clouds, or commonly known as the aerosol-cloud-interaction according to a new study led by Earth System Science Interdisciplinary Center (ESSIC) researchers published today in Science Advances.

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ESSIC at Maryland Day 2024

On Saturday, April 27, ESSIC faculty and staff gathered to celebrate Maryland Day, the University of Maryland’s largest community outreach event! This was the 26th year that the university held the event, and the 24th time that ESSIC has participated.

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Terrestrial Water Storage In 2023: A Review

Earlier this month, Nature Reviews Earth & Environment released their annual Climate Chronicles, a collection of their ‘Year in Review’ articles. In these pieces, leading experts outline the observed characteristics and changes to select climate metrics and policies over the course of the year, collectively documenting the state of the climate and its ongoing evolution.

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How Will Clouds Affect Climate Change?

One of the most critical questions in climate research today is how global clouds will change in a warmer environment. Physical mechanisms in the atmosphere have the potential to moderate or accelerate the warming from greenhouse gases. These mechanisms are called feedbacks. Even with today’s improved forecasts, feedback from clouds is uncertain – meaning scientists don’t know how much Earth’s average temperature will warm as the CO2 atmospheric concentrations continue to increase. A new University of Maryland and NASA study attempts to reduce this uncertainty by constructing a long-term trend in cloudiness using NASA and NOAA satellite observations going back to 1980.

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