What is it about?
According to a prior study, 46% of North Atlantic hurricanes transition into mid-latitude cyclones as they move poleward, potentially bringing hazardous weather to locations that rarely experience hurricane impacts. Previous studies also indicate that projected climate change will worsen the impacts of hurricanes and tropical storms, especially with increased rainfall. These factors motivated us to investigate how climate change could affect the characteristics of transitioning hurricanes. We utilized computer-based experiments to simulate hurricane Irene, which affected the eastern U.S. in 2011. In one simulation, we reproduced the observed storm. In an experimental simulation, we examined how the storm would change in a warmer climate. The future transitioning storm featured substantially heavier precipitation and stronger winds. In addition, the amount of time it took the storm to complete its transitioning was about 60% longer in the warmer simulations.
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Why is it important?
While many hurricanes moving out of the tropics weaken, a subset of these systems intensify and increase in size. We studied one of these storms, Irene from 2011, which was a very high impact event in the present climate. Our experimental simulations show that in a warmer climate, the impacts of Irene would have been even greater, with heavier rainfall and stronger winds. Also, because the transition process took longer, this suggests that in the future, hurricane conditions could potentially reach higher latitudes. While this is only a single case study, it provides a useful perspective and informs other experiments we are doing now with “generic” or “idealized” simulations of this type of weather system.
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This page is a summary of: Extratropical Transition of Hurricane Irene (2011) in a Changing Climate, Journal of Climate, May 2019, American Meteorological Society,
DOI: 10.1175/jcli-d-18-0558.1.
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