Initialized decadal prediction for transition to positive phase of the Interdecadal Pacific Oscillation
The negative phase of the Interdecadal Pacific Oscillation (IPO), a dominant mode of multi-decadal variability of sea surface temperatures (SSTs) in the Pacific, contributed to the reduced rate of global surface temperature warming in the early 2000s. A proposed mechanism for IPO multidecadal variability indicates that the presence of decadal timescale upper ocean heat content in the off-equatorial western tropical Pacific can provide conditions for an interannual El Niño/Southern Oscillation event to trigger a transition of tropical Pacific SSTs to the opposite IPO phase. Here we show that a decadal prediction initialized in 2013 simulates predicted Niño3.4 SSTs that have qualitatively tracked the observations through 2015. The year three to seven average prediction (2015-2019) from the 2013 initial state shows a transition to the positive phase of the IPO from the previous negative phase and a resumption of larger rates of global warming over the 2013-2022 period consistent with a positive IPO phase.
document
https://n2t.org/ark:/85065/d7gx4d5h
eng
geoscientificInformation
Text
publication
2016-01-01T00:00:00Z
publication
2016-01-02T00:00:00Z
Copyright 2016 Authors. This work is distributed under the Creative Commons Attribution 3.0 License.
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