https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2020GL086954

Storm Track Changes in the Middle East and North Africa Under Stratospheric
Aerosol Geoengineering
K. Karami  S. Tilmes  H. Muri  S. V. Mousavi
First published: 15 June 2020
https://doi.org/10.1029/2020GL086954
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Abstract
As a potential approach to prevent dangerous climate change, stratospheric
aerosol geoengineering (SAG) aims to reflect some incoming solar radiation
into space and reduce temperatures. Previous modeling studies suggest that
storm tracks will shift poleward due to the increases in the greenhouse gas
concentrations. As a consequence of this, the Middle East, North Africa,
and Mediterranean regions will most likely experience a strong
precipitation decrease, increasing the pressure on the region's vulnerable
environment. Our results from an Earth system model indicate that SAG can
partially offset the poleward shift of the storm tracks, thus potentially
soothing the environmental and water stresses of the region. However, other
climatic side effects may occur, hence still motivating ambitious
mitigation action to reduce emissions and impacts of global warming. The
results presented may have practical implications for ongoing climate
policy debates in the region.

Plain Language Summary
As a potential approach to prevent dangerous climate change, stratospheric
aerosol geoengineering aims to reflect a small percentage of incoming solar
radiation into space to reduce the global mean temperature. However,
regional impacts are not clear, especially in the global south. This
article provides the first analysis of changes in the storm‐tracks from
stratospheric aerosol geoengineering in the Middle East and North Africa
(MENA) region. The results of our study indicate that the poleward shift of
the storm‐tracks due to increases in the greenhouse gas concentration could
be partially offset, and thus potentially sooth some of the environmental,
in particular water, stresses. However, other side effects may occur,
motivating for an ambitious mitigation pathway still.

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