Table 1: Twenty seven GCM models used in this study to provide atmospheric forcing parameters to SEGMENT.
Model name |
Institution |
Horizontal resolution |
ACCESS1-0 |
Commonwealth scientific and Industrial research organisation (CSIRO)/Bureau of morology (BoM) |
192 × 145 |
ACCESS1-3 |
CSIRO/BoM |
192 × 145 |
CCSM 4 |
National center for Atmospheric research |
288 × 192 |
CanESM 2 |
Canadian centre for Climate modelling and Analysis |
128 × 64 |
CNRM-CM5 |
Centre national de recherches meteorologiques |
256 × 128 |
CESMI-BGC |
National center for Atmospheric research |
288 × 192 |
CESMI-CAM5 |
National center for Atmospheric research |
288 × 192 |
FGOALS-g2 |
Institute of Atmospheric physics, Chinese academy of sciences |
128 × 60 |
GFDL-CM3 |
Geophysical fluid dynamics laboratory |
144 × 90 |
GFDl-ESM-2G |
Geophysical fluid dynamics laboratory |
144 × 90 |
GFDl-ESM-2M |
Geophysical fluid dynamics laboratory |
144 × 90 |
GISS-E2-H |
NASA/Goddard institute for Space studies (GISS) |
144 × 90 |
GISS-E2-R |
NASA/GISS |
144 × 90 |
HadGEM2_AO |
National institute of Meteorological research, Korea meteorological administration (S. Korea) |
192 × 145 |
HadGEM2_CC |
Met office hadley centre |
192 × 145 |
HadGEM2_ES |
Met office hadley centre |
192 × 145 |
INM |
Institute of Numerical mathematics, Russian academy of Sciences |
180 × 120 |
IPSL-CM5A-LR |
Institute pierre simon laplace (France) |
96 × 96 |
IPSL-CM5A-MR |
Institute pierre simon laplace (France) |
144 × 143 |
IPSL-CM5B-LR |
Institute pierre simon laplace (France) |
96 × 96 |
MIROC5 |
Atmosphere and Ocean research institute, The tokyo university |
256 × 128 |
MIROC-ESM |
Japan agency for Marine-earth Science and Technology |
128 × 64 |
MRI-CGCM3 |
Meteorological research institute |
320 × 160 |
MPI-ESM-LR |
Max plank institute (MPI) for Meteorology |
128 × 64 |
MPI-ESM-MR |
Max plank institute (MPI) for Meteorology |
192 × 96 |
NorESMI-M |
Bjerknes center for Climate research, Norwegian meteorological institute |
144 × 96 |
NorESMI-ME |
|
144 × 96 Global grids |