Science Source

Forced and unforced ocean temperature changes in Atlantic and Pacific tropical cyclogenesis regions

Fingerprints the role of global warming in increased sea surface temperatures using climate models to study the possible causes of SST changes in Atlantic and Pacific tropical cyclogenesis regions
States the observed SST increases in these regions range from 0.32°C to 0.67°C over the 20th century
Finds 22 climate models examined here suggest that century-timescale SST changes of this magnitude cannot be explained solely by unforced variability of the climate system
Employs model simulations of natural internal variability to make probabilistic estimates of the contribution of external forcing to observed SST changes
Finds an 84% chance that external forcing explains at least 67% of observed SST increases in the two tropical cyclogenesis regions for the period 1906–2005
Finds that in experiments in which forcing factors are varied individually rather than jointly, human-caused changes in greenhouse gases are the main driver of the 20th-century SST increases in both tropical cyclogenesis regions