https://www.sciencedirect.com/science/article/pii/S1674283422000526

Effects of solar radiation modification on the ocean carbon cycle: An Earth
system modeling study

Xiaoyu Jin, Long Cao, Jingyu Zhang

ABSTRACT

Solar radiation modification (SRM, also termed as geoengineering) has been
proposed as a potential option to counteract anthropogenic warming. The
underlying idea of SRM is to reduce the amount of sunlight reaching the
atmosphere and surface, thus offsetting some amount of global warming.
Here, we use an Earth system model to investigate the impact of SRM on the
global carbon cycle and ocean biogeochemistry. We simulate the temporal
evolution of global climate and the carbon cycle from the pre-industrial
period to the end of this century under three scenarios: the RCP4.5
CO2 emission
pathway, the RCP8.5 CO2 emission pathway, and the RCP8.5 CO2 emission
pathway with the implementation of SRM to maintain the global mean surface
temperature at the level of RCP4.5. Our simulations show that SRM, by
altering global climate, also affects the global carbon cycle. Compared to
the RCP8.5 simulation without SRM, by the year 2100, SRM reduces
atmospheric CO2 by 65 ppm mainly as a result of increased CO2 uptake by the
terrestrial biosphere. However, SRM-induced change in atmospheric CO2 and
climate has a small effect in mitigating ocean acidification. By the year
2100, relative to RCP8.5, SRM causes a decrease in surface ocean hydrogen
ion concentration ([H+]) by 6% and attenuates the seasonal amplitude of [H+]
by about 10%. Our simulations also show that SRM has a small effect on
globally integrated ocean net primary productivity relative to the
high-CO2 simulation
without SRM. Our study contributes to a comprehensive assessment of the
effects of SRM on both the physical climate and the global carbon cycle.

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