https://journals.ametsoc.org/view/journals/clim/aop/JCLI-D-23-0225.1/JCLI-D-23-0225.1.xml

*Authors*
Hui Li, Jadwiga H. Richter, Aixue Hu, Gerald A. Meehl, and Douglas MacMartin

*Online Publication*: *16 Aug 2023*
DOI: https://doi.org/10.1175/JCLI-D-23-0225.1

*Abstract*
The subpolar North Atlantic (SPNA) shows contrasting responses in two
sensitivity experiments with increased stratospheric aerosols, offering
insight into the physical processes that may impact the Atlantic meridional
overturning circulation (AMOC) in a warmer climate. In one, the upper ocean
becomes warm and salty, but in the other it becomes cold and fresh. The
changes are accompanied by diverging AMOC responses. The first experiment
strengthens the AMOC, opposing the weakening trend in the reference
simulation. The second experiment shows a much smaller impact. Both
simulations use the Community Earth System Model with the Whole Atmosphere
Community Climate Model component (CESM-WACCM)) but differ in model
versions and stratospheric aerosol specifications. Despite both experiments
using similar approaches to increase stratospheric aerosols to counteract
the rising global temperature, the contrasting SPNA and AMOC responses
indicate a considerable dependency on model physics, climate states, and
model responses to forcings. This study focuses on examining the physical
processes involved with the impact of stratospheric aerosols on the SPNA
salinity changes and their potential connections with the AMOC and the
Arctic. We find that in both cases, increased stratospheric aerosols act to
enhance the SPNA upper ocean salinity by reducing freshwater export from
the Arctic, which is closely tied to the Arctic sea ice changes. The impact
on AMOC is primarily through the thermal component of the surface buoyancy
fluxes, with negligible contributions from the freshwater component. These
experiments shed light on the physical processes that dictate the important
connections between the SPNA, the Arctic, the AMOC, and their subsequent
feedbacks on the climate system.

*Source: AMS*

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