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Future tropical cyclone intensities in the Caribbean: high-resolution regional climate model for better understanding

The Caribbean region is prone to the strong winds and low air pressures of tropical cyclones and their corresponding storm surge that driving coastal flooding. To protect coastal communities from the impacts of tropical cyclones, it is important to understand how this impact of tropical cyclones might change towards the future. This study applies the storyline approach to show what tropical cyclones Maria (2017) and Dorian (2019) could look like in a 2 °C and 3.4 °C warmer future climate. These two possible future climates are simulated with a high-resolution regional climate model using the pseudo global warming approach. Using the climate response from these simulations we apply a Delta-quantile mapping technique to derive future changes in wind speed and mean sea level pressure. We apply this Delta technique to tropical cyclones Maria and Dorian’s observed wind and pressure fields to force a hydrodynamic model for simulating storm surge levels under historical and future climate conditions. Results show that the maximum storm surge heights of Maria and Dorian could increase by up to 0.31 m and 0.56 m, respectively.

(a) maximum surge height of Hurricane Maria using the observed TC track as forcing; (b) difference in maximum surge height using ΔPGW, calculated as ΔPGW minus IBTrACS; (c) same as (b) but for ΔTP2; (d–f) same as (a–c) but for Hurricane Dorian.

These results clearly show that future changes in storm surge heights are not negligible compared to end-of-the-century sea level rise projections, something that is sometimes overlooked in large-scale assessments of future coastal flood risk.

Dullaart, J.C.M., de Vries, H., Bloemendaal, N. et al. Improving our understanding of future tropical cyclone intensities in the Caribbean using a high-resolution regional climate model. Sci Rep 14, 6108 (2024). https://doi.org/10.1038/s41598-023-49685-y

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