https://www.sciencedirect.com/science/article/pii/S1674927825001224

*Authors*
Yu FANG, Long CAO

*12 June 2025*

https://doi.org/10.1016/j.accre.2025.06.003

*Abstract*
Marine cloud brightening (MCB) has been proposed as a backup method to
mitigate some impacts of global warming. Cloud albedo can be increased over
ocean or land either intentionally or unintentionally. Our understanding of
how the climate response differs between cloud albedo enhancement over
ocean and land remains limited. In this study, we use the Community Earth
System Model (CESM) to explore the impact of cloud albedo enhancement over
either ocean or land on the terrestrial climate and carbon cycle. In our
simulation design, both MCB and land cloud brightening (LCB) are applied
over the latitude bands of 30ºS‒30ºN under atmospheric CO2 concentration of
800 × 10−6 to achieve a net negative radiative forcing of about −1 W/m2.
Over large parts of the low latitude land, MCB increases precipitation by
enhancing upward atmospheric motion, resulting in increased soil moisture.
In contrast, LCB decreases precipitation by inducing subsidence, resulting
in decreased soil moisture. Changes in climatic factors affect land gross
primary production (GPP). Relative to the high CO2 world, LCB reduces GPP
by 3.80 ± 0.09 GtC per year, which is about three times the reduction
caused by MCB (1.34 ± 0.10 GtC per year). These differences in GPP
responses are closely linked to changes in the hydrological cycle. In large
parts of low-latitude regions, MCB increases soil moisture, which acts to
enhance GPP. Conversely, LCB reduces soil moisture, which acts to suppress
GPP. MCB and LCB-induced changes in temperature, sunlight, and vapor
pressure deficit also play important roles in regulating GPP change. This
study would help us to better understand terrestrial climate and carbon
cycle consequences resulting from large-scale cloud albedo change over
either ocean or land, as well as large-scale albedo change over ocean and
land surface.

*Source: ScienceDirect*

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