Simulation of early 20th century global warming

Explore this paper's citation graph

Summary

Results from a set of six integrations of a coupled ocean-atmosphere climate model suggest that the warming of the early 20th century could have resulted from a combination of human-induced radiative forcing and an unusually large realization of internal multidecadal variability of the coupled Ocean-Atmosphere system.

Type
article
Published
2000-03-24
Cited by
298
References
29

Keywords

Radiative forcing, Climatology, Global warming, Environmental science, Forcing (mathematics)

References

Cited by

Related papers