GFDL-CM3salinity biasesThe variability of the Atlantic Meridional Overturning Circulation (AMOC) and the Meridional Freshwater Transport (Mov) at 24°N, 11°S, and 30°S, simulated with the GFDL-CM3 model under the historical (1860–2005) and RCP 4.5 and 8.5 scenarios (2006–2100) are ...
GFDL-CM3salinity biasesThe variability of the Atlantic Meridional Overturning Circulation (AMOC) and the Meridional Freshwater Transport (Mov) at 24°N, 11°S, and 30°S, simulated with the GFDL-CM3 model under the historical (1860–2005) and RCP 4.5 and 8.5 scenarios (2006–2100) are ...
China 128×108 Chinese Academy of science GFDL-CM3 Geophysical Fluid Dynamics USA 144×90 GFDL-ESM2G Laboratory 144×90 GFDL-ESM2M 144×90 HadGEM2-CC Met Office Hadley Centre UK 192×145 HadGEM2-ES 192×145 INM-CM4 Russian Academy of Sciences, Russia 180×120 Institute of Numerical Mathema...
Response of the Tropical Indian Ocean to Greenhouse Gases and Aerosol Forcing in the GFDL CM3 Coupled Climate ModelIndian Ocean Dipolegreenhouse gasesaerosolsIOD skewnessSST residualThe Indian Ocean Dipole (IOD) is one of the leading modes of interannual sea surface temperature (SST) variability in ...
Simulations of three natural decadal climate variability phenomena in CMIP5 experiments with the UKMO HadCM3, GFDL-CM2.1, NCAR-CCSM4, and MIROC5 global earth system modelsDecadal climate variabilityPacific decadal oscillationWest Pacific warm pool...