Projected Future Changes in Tropical Cyclones using the CMIP6 HighResMIP
Multi-model Ensemble
- Malcolm J Roberts,
- Alessio Bellucci,
- Benoit Vannière,
- Joanne Camp,
- Christopher David Roberts,
- Dian Putrashan,
- Jennifer Veronika Mecking,
- Kevin Hodges,
- Laurent Terray,
- Louis-Philippe Caron,
- Pier Luigi Vidale,
- Rein Haarsma,
- Retish Senan,
- Jon Seddon,
- Marie-Pierre Moine,
- Chihiro Kodama,
- Yohei Yamada,
- Colin M. Zarzycki,
- Paul Ullrich,
- Ryo Mizuta,
- Dan Fu,
- Gokhan Danabasoglu,
- Lixin Wu,
- Nan A. Rosenbloom,
- Qiuying Zhang,
- Enrico Scoccimarro,
- Fabrice Chauvin,
- Sophie Valcke,
- Hong Wang
Alessio Bellucci
Centro Euro-Mediterraneo sui Cambiamenti Climatici
Author ProfileJennifer Veronika Mecking
National Oceanography Centre Southampton
Author ProfileRetish Senan
European Centre for Medium Range Weather Forecasts (ECMWF)
Author ProfileMarie-Pierre Moine
CERFACS (Centre Européen de Recherche et de Formation Avancée en Calcul Scientifique)
Author ProfileChihiro Kodama
Japan Agency for Marine-Earth Science and Technology
Author ProfileYohei Yamada
Japan Agency for Marine-Earth Science and Technology
Author ProfileGokhan Danabasoglu
National Center for Atmospheric Research (NCAR)
Author ProfileNan A. Rosenbloom
National Center for Atmospheric Research (UCAR)
Author ProfileEnrico Scoccimarro
Fondazione Centro euro-Mediterraneo sui Cambiamenti Climatici - CMCC
Author ProfileAbstract
Future changes in tropical cyclone properties are an important component
of climate change impacts and risk for many tropical and mid-latitude
countries. In this study we assess the performance of a multi-model
ensemble of climate models, at resolutions ranging from 250km to 25km.
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 10m wind speeds
by 2050.