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• W2030129197 abstract "[1] Time-series of Pacific Decadal Oscillation (PDO) reconstructed from tree-rings in Western North America is found to have a statistically significant periodicity of 18.6-year period lunar nodal tidal cycle; negative (positive) PDO tends to occur in the period of strong (weak) diurnal tide. In the 3rd and 5th (10th, 11th and 13rd) year after the maximum diurnal tide, mean-PDO takes significant negative (positive) value, suggesting that the Aleutian Low is weak (strong), western-central North Pacific in 30–50°N is warm (cool) and equator-eastern rim of the Pacific is cool (warm). This contributes to climate predictability with a time-table from the astronomical tidal cycle." @default.
• W2030129197 created "2016-06-24" @default.
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• W2030129197 date "2009-03-12" @default.
• W2030129197 modified "2023-09-30" @default.
• W2030129197 title "The 18.6-year period moon-tidal cycle in Pacific Decadal Oscillation reconstructed from tree-rings in western North America" @default.
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• W2030129197 doi "https://doi.org/10.1029/2008gl036880" @default.
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