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Pacific Decadal Oscillation: Tropical Pacific Forcing versus Internal Variability
2018
Journal of Climate
The Pacific decadal oscillation (PDO) is the leading mode of sea surface temperature (SST) variability over the North Pacific (north of 208N). Its South Pacific counterpart (south of 208S) is the South Pacific decadal oscillation (SPDO). The effects of tropical eastern Pacific (TEP) SST forcing and internal atmospheric variability are investigated for both the PDO and SPDO using a 10-member ensemble tropical Pacific pacemaker experiment. Each member is forced by the historical radiative forcing
doi:10.1175/jcli-d-18-0164.1
fatcat:6vwyrvcwuzbsrbrz6cx7sprvru