https://iopscience.iop.org/article/10.1088/2752-5295/ad8df6/meta

*Authors*
Harpreet Kaur, Govindasamy Bala, Ashwin K Seshadri

*01 November 2024*

*Abstract*
Understanding the climate response to interhemispheric differences in
imposed radiative forcing is crucial for solar radiative modification (SRM)
investigations. While previous studies have shown that climate sensitivity
to solar insolation changes imposed in the northern versus the southern
hemisphere is different, the underlying mechanisms remain unclear. In this
study, we investigate the climate response to three different radiative
forcing scenarios: globally uniform radiative forcing, radiative forcing
imposed only in the northern hemisphere, and radiative forcing confined
only to the southern hemisphere. We find that the climate sensitivity is
larger when forcing is imposed only in the southern hemisphere. To explain
the mechanisms for this, we estimate climate feedbacks using the radiative
kernel approach. We find that albedo and Planck feedbacks are insensitive
to hemisphere of forcing, and the larger climate sensitivity to the
southern hemispheric radiative forcing is primarily due to differences in
shortwave cloud feedbacks. Additionally, we examine impacts of
interhemispheric differences in radiative forcing on tropical circulation,
planetary albedo, and land/sea warming contrast. Our results clearly
demonstrate how the Intertropical Convergence Zone (ITCZ) moves into the
hemisphere where the radiative forcing is larger without maintaining a
symmetric planetary albedo. Overall, our study provides insights into
climate system responses to interhemispheric differences in radiative
forcing caused by forcing agents such as aerosols from volcanic eruptions
and human activities, and land cover changes, in addition to solar
geoengineering.

*Source: IOP Science*

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