North Pacific decadal climate variability since 1661
Climate in the North Pacific and North American sectors has experienced interdecadal shifts during the twentieth century. A network of recently developed tree-ring chronologies for Southern and Baja California extends the instrumental record and reveals decadal-scale variability back to 1661. The Pacific decadal oscillation (PDO) is closely matched by the dominant mode of tree-ring variability that provides a preliminary view of multiannual climate fluctuations spanning the past four centuries. The reconstructed PDO index features a prominent bidecadal oscillation, whose amplitude weakened in the late l700s to mid-1800s. A comparison with proxy records of ENSO suggests that the greatest decadal-scale oscillations in Pacific climate between 1706 and 1977 occurred around 1750, 1905, and 1947.
Citation Information
Publication Year | 2001 |
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Title | North Pacific decadal climate variability since 1661 |
DOI | 10.1175/1520-0442(2001)014%3C0005:NPDCVS%3E2.0.CO;2 |
Authors | Franco Biondi, Alexander Gershunov, Daniel R. Cayan |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Journal of Climate |
Index ID | 70185082 |
Record Source | USGS Publications Warehouse |