| Title: |
The impacts of climate change on tropical-to-extratropical transitions in the North Atlantic Basin. |
| Authors: |
Garin, Aude; Pausata, Francesco S. R.; Boudreault, Mathieu; Ingrosso, Roberto |
| Source: |
Weather & Climate Dynamics; 2025, Vol. 6 Issue 4, p1379-1397, 19p |
| Subject Terms: |
Climate change; Tropical cyclones; Severe storms; Hurricanes; Cyclones; Seasons |
| Geographic Terms: |
North Atlantic Ocean; North America |
| Abstract: |
As tropical cyclones migrate toward mid-latitudes, they can transform into extratropical cyclones, a process known as extratropical transition. In the North Atlantic Basin, nearly half of hurricanes undergo this transition. After transitioning, these storms can reintensify, posing significant threats to populations and infrastructure along the eastern coast of North America. While the impacts of climate change on hurricanes have been extensively studied, there remain uncertainties about its effects on extratropical transitions. This study aims to assess how climate change affects the frequency, location, intensity, and duration of these transitions. To achieve this, high-resolution regional simulations from an atmospheric regional climate model, based on the Representative Concentration Pathways 8.5 (RCP8.5) emissions scenario, were used to compare two 30-year periods: the present (1990–2019) and the end of the century (2071–2100). The results indicate a projected decrease in the number of tropical hurricanes, with no significant change in extratropical transition rates. September and October continue to be the primary months for extratropical transitions. However, the season's peak appears to have shifted from September to October, suggesting that large-scale environmental conditions may become more favourable for extratropical transitions in October in the future. Although a poleward shift in the maximum intensity of tropical hurricanes is detected, the average latitude of the transitions does not change. Our findings suggest that transitioning storms will be more intense in the future, despite a less baroclinic atmosphere, due to a stronger contribution from latent heat transfer. However, the risk of reintensification after transition is not expected to increase. [ABSTRACT FROM AUTHOR] |
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| Database: |
Complementary Index |