https://iopscience.iop.org/article/10.1088/2752-5295/ade61a/meta

*Authors*
Kwesi Twentwewa Quagraine, Travis Allen O'Brien, Kwesi A Quagraine, Ben
Kravitz and Simone Tilmes

Accepted Manuscript online *19 June 2025*

DOI 10.1088/2752-5295/ade61a

*Abstract*
In a warming climate, where climate adaptation and mitigation strategies
are
increasingly critical, understanding changes in major global atmospheric
moisture
transport mechanisms, such as atmospheric rivers (ARs), is essential for
assessing
shifts in the hydrological cycle. This study examines the frequency and
impacts of
ARs under the Shared Socioeconomic Pathway (SSP2-4.5) warming scenario and
the Stratospheric Aerosol Injection (SAI) scenario (ARISE-SAI-1.5). Our
findings indicate that under SAI-1.5, ARs retreat from inland regions, and
the occurrence of high-impact ARs (Category 3 and above) decreases,
although some uncertainty remains regarding the response time of ARs to
SAI. However, under future climate without SAI (SSP2-4.5), ARs penetrate
further inland and there are higher numbers of high-impact ARs (> Category
3 ARs). In the Northern Hemisphere oceans, SAI-1.5 leads to a gradual
increase in AR frequency compared to SSP2-4.5, whereas the Southern
Hemisphere oceans exhibit the opposite trend. Also, extreme AR-associated
precipitation is reduced under SAI-1.5 relative to SSP2-4.5, whereas
beneficial precipitation (Ralph et al., 2019) is projected to increase
under SAI-1.5. The contrasting responses associated with AR location and
intensity highlights the need for further research to better understand the
underlying drivers of AR changes before SAI can be considered in policy
decisions affecting global moisture transport mechanisms.

*Source: IOP Science*

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