Impacts of hemispheric solar geoengineering on tropical cyclone frequency

This is the author accepted manuscript. The final version is available from Springer Nature via the DOI in this record. Solar geoengineering refers to a range of proposed methods for counteracting global warming by artificially reducing sunlight at Earth’s surface. The most widely known solar geoeng...

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Bibliographic Details
Published in:Nature Communications
Main Authors: Haywood, JM, Jones, AC, Dunstone, N, Hawcroft, M, Hodges, K, Jones, A, Emanuel, K
Format: Article in Journal/Newspaper
Language:English
Published: Springer Nature 2017
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Online Access:http://hdl.handle.net/10871/30094
https://doi.org/10.1038/s41467-017-01606-0
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Summary:This is the author accepted manuscript. The final version is available from Springer Nature via the DOI in this record. Solar geoengineering refers to a range of proposed methods for counteracting global warming by artificially reducing sunlight at Earth’s surface. The most widely known solar geoengineering proposal is stratospheric aerosol injection (SAI) which has impacts analogous to those from volcanic eruptions. Observations following major volcanic eruptions indicate that aerosol enhancements confined to a single hemisphere effectively modulate North Atlantic tropical cyclone (TC) activity in the following years. Here we investigate the effects of both single-hemisphere and global SAI scenarios on North Atlantic TC activity using the HadGEM2-ES general circulation model and various TC identification methods. We show that a robust result from all of the methods is that SAI applied to the southern hemisphere would enhance TC frequency relative to a global SAI application, and vice versa for SAI in the northern hemisphere. Our results reemphasize concerns regarding regional geoengineering and should motivate policymakers to regulate large-scale unilateral geoengineering deployments. A.C.J. was supported by a Met Office/NERC CASE (ref. 580009183) PhD studentship. M.K.H. and J.M.H. were supported by the Natural Environment Research Council/Department for International Development via the Future Climates for Africa (FCFA) funded project ‘Improving Model Processes for African Climate’ (IMPALA, NE/M017265/1).