TY - JOUR
T1 - Projected Future Changes in Tropical Cyclones Using the CMIP6 HighResMIP Multimodel Ensemble
AU - Roberts, Malcolm John
AU - Camp, Joanne
AU - Seddon, Jon
AU - Vidale, Pier Luigi
AU - Hodges, Kevin
AU - Vannière, Benoît
AU - Mecking, Jenny
AU - Haarsma, Rein
AU - Bellucci, Alessio
AU - Scoccimarro, Enrico
AU - Caron, Louis Philippe
AU - Chauvin, Fabrice
AU - Terray, Laurent
AU - Valcke, Sophie
AU - Moine, Marie Pierre
AU - Putrasahan, Dian
AU - Roberts, Christopher D.
AU - Senan, Retish
AU - Zarzycki, Colin
AU - Ullrich, Paul
AU - Yamada, Yohei
AU - Mizuta, Ryo
AU - Kodama, Chihiro
AU - Fu, Dan
AU - Zhang, Qiuying
AU - Danabasoglu, Gokhan
AU - Rosenbloom, Nan
AU - Wang, Hong
AU - Wu, Lixin
N1 - Publisher Copyright:
©2020. Crown copyright.
PY - 2020/7/28
Y1 - 2020/7/28
N2 - Future changes in tropical cyclone properties are an important component of climate change impacts and risk for many tropical and midlatitude countries. In this study we assess the performance of a multimodel ensemble of climate models, at resolutions ranging from 250 to 25 km. We use a common experimental design including both atmosphere-only and coupled simulations run over the period 1950–2050, with two tracking algorithms applied uniformly across the models. There are overall improvements in tropical cyclone frequency, spatial distribution, and intensity in models at 25 km resolution, with several of them able to represent very intense storms. Projected tropical cyclone activity by 2050 generally declines in the South Indian Ocean, while changes in other ocean basins are more uncertain and sensitive to both tracking algorithm and imposed forcings. Coupled models with smaller biases suggest a slight increase in average TC 10 m wind speeds by 2050.
AB - Future changes in tropical cyclone properties are an important component of climate change impacts and risk for many tropical and midlatitude countries. In this study we assess the performance of a multimodel ensemble of climate models, at resolutions ranging from 250 to 25 km. We use a common experimental design including both atmosphere-only and coupled simulations run over the period 1950–2050, with two tracking algorithms applied uniformly across the models. There are overall improvements in tropical cyclone frequency, spatial distribution, and intensity in models at 25 km resolution, with several of them able to represent very intense storms. Projected tropical cyclone activity by 2050 generally declines in the South Indian Ocean, while changes in other ocean basins are more uncertain and sensitive to both tracking algorithm and imposed forcings. Coupled models with smaller biases suggest a slight increase in average TC 10 m wind speeds by 2050.
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U2 - 10.1029/2020GL088662
DO - 10.1029/2020GL088662
M3 - Article
C2 - 32999514
AN - SCOPUS:85088592460
SN - 0094-8276
VL - 47
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 14
M1 - e2020GL088662
ER -