Abstract
Climate change induces a myriad of effects which influences the global tropical cyclone (TC) genesis frequency. Here we explore how North Atlantic and Western Pacific TCs are affected under climate change using a present-day and a future (1% pCO2 scenario) ensemble of high resolution simulations. We find that the number of TCs decreases (-45%) in the North Atlantic but increases (+15%) in the Western Pacific. Part of these opposing variations are linked to differences in the ocean’s meridional overturning circulation, which gives rise to a different sea surface temperature response and air-sea fluxes between the two basins. The results show the important role of oceanic climate change on TC response.
Original language | English |
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Pages (from-to) | 2269-2284 |
Number of pages | 16 |
Journal | Climate Dynamics |
Volume | 61 |
Issue number | 5-6 |
Early online date | 22 Jan 2023 |
DOIs | |
Publication status | Published - Sept 2023 |
Bibliographical note
Funding Information:The authors thank Michael Kliphuis (IMAU, UU) for performing the CESM simulations. All computations and analysis were performed on the Dutch Supercomputers Cartesius and Snellius at SURFsara in Amsterdam.
Funding Information:
All CESM computations were performed within NWO-SURF project 17239. R.M.v.W and H.A.D. are funded by the European Union’s Horizon 2020 research and innovation program for the ITN TiPES under Grant Agreement Number 643073. N.B. is funded by a VICI grant from the NWO (Grant Number 453-13-006) and the ERC Advanced Grant COASTMOVE no. 884442.
Publisher Copyright:
© 2023, The Author(s).
Keywords
- AMOC weakening
- Climate change
- High-resolution modelling
- Tropical cyclones