Table 1 List of CMIP6 models used in this study.

From: Patterns and frequency of projected future tropical cyclone genesis are governed by dynamic effects

Model name

Expanded model name

Horizontal resolution

TC detection criteria

Simulation used

[lat x lon]

ζ850 (m/s)

ta (K)

d (h)

SSP2-4.5

SSP5-8.5

CMCC-CM2-SR5

Euro-Mediterranean Centre on Climate Change coupled climate model

1.25 × 0.9

8.500 × 10−5

1.00

36

 

CNRM_CM6-1-HR

Centre National de Recherches Meteorologiques Coupled Global Climate Model, version 6

0.5 × 0.5

1.400 × 10−4

1.00

36

 

MIROC6

Model for Interdisciplinary Research on Climate, version 6

1.4 × 1.4

1.125 × 10−4

1.00

36

MPI-ESM1-2-HR

Max Planck Institute Earth System Model, medium resolution

0.9 × 0.9

1.0 × 10−5

0.60

36

MRI-ESM2-0

Meteorological Research Institute Earth System Model 2.0

1.1 × 1.1

8.000 × 10−5

1.00

36

NorESM2-MM

Norwegian Climate Center’s Earth System Model

1.25 × 0.9

5.250 × 10−5

1.00

36

  1. The model-dependent criteria for TC detection are the relative vorticity at 850 hPa, temperature anomaly, and duration. The last column indicates the future scenarios used in this study.