Mechanisms of tropical cyclone response under climate change in the community earth system model

René van Westen*, Henk Dijkstra, Nadia Bloemendaal

*Corresponding author for this work

Research output: Contribution to journalArticleAcademicpeer-review

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 languageEnglish
Pages (from-to)2269-2284
Number of pages16
JournalClimate Dynamics
Volume61
Issue number5-6
Early online date22 Jan 2023
DOIs
Publication statusPublished - 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

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