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Long-term climate impact of large stratospheric water vapor perturbations
  • Martin Jucker,
  • Chris Lucas,
  • Deepashree Dutta
Martin Jucker
Climate Change Research Centre and Centre of Excellence for Climate Extremes, University of New South Wales

Corresponding Author:[email protected]

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Chris Lucas
Bureau of Meteorology
Deepashree Dutta
Climate Change Research Centre and Centre of Excellence for Climate Extremes, University of New South Wales

Abstract

The amount of water vapor injected into the stratosphere after the eruption of Hunga Tonga-Hunga Ha'apai (HTHH) was unprecedented, and it is therefore unclear what it might mean for surface climate. We use chemistry climate model simulations to assess the long-term surface impacts of stratospheric water vapor (SWV) anomalies similar to those caused by HTHH, but neglect the relatively minor aerosol loading from the eruption. The simulations show that the SWV anomalies lead to strong and persistent warming of Northern Hemisphere landmasses in boreal winter, and austral winter cooling over Australia, years after eruption, demonstrating that large SWV forcing  can have surface impacts on a decadal timescale. We also emphasize that the surface response to SWV anomalies is more complex than simple warming due to greenhouse forcing and is influenced by factors such as regional circulation patterns and cloud feedbacks. Further research is needed to fully understand the multi-year effects of SWV anomalies and their relationship with climate phenomena like El Niño Southern Oscillation.
01 Dec 2023Submitted to ESS Open Archive
03 Dec 2023Published in ESS Open Archive
27 May 2024Published in Journal of Climate. https://doi.org/10.1175/JCLI-D-23-0437.1