Kunashir (Kuriles) Oak 400-year reconstruction of temperature and relation to the Pacific Decadal Oscillation

• Published in: Palaeogeography, palaeoclimatology, palaeoecology palaeoclimatology, palaeoecology, 2004-07, Vol.209 (1), p.303-311
• Main Authors: Jacoby, G, Solomina, O, Frank, D, Eremenko, N, D'Arrigo, R
• Format: Article
• Language: English
• Subjects: North Pacific; Paleoclimate; PDO; Tree rings
• ISSN: 0031-0182; 1872-616X
• DOI: 10.1016/j.palaeo.2004.02.015

Paleoclimatic records of northwest Pacific variations are scarce but can be extended by proxy records from old-aged trees around the North Pacific Rim. In July of 2001 on Kunashir Island at the southern extent of the Kuriles, tree cores were extracted from century-old oaks ( Quercus crispula) and developed into a 400-year tree-ring width index series. Analyses showed the ring-width indices to correlate strongly with summer (June–September) temperatures as recorded at Ugno-Kurilsky on the Island. The summer temperatures were reconstructed using the tree-ring data and 52% of the variance was explained by the tree-ring indices. The recorded temperature data and the tree-ring data show similar correlation patterns with sea-surface temperatures (SSTs) of the North Pacific. Studies of North Pacific variations, as quantified by the Pacific Decadal Oscillation (PDO), show the PDO to be an important index of large-scale climate variation. The tree-ring series explains more than 33% of the variance of the July–September Pacific Decadal Oscillation and has similar spectral properties, further supporting the concept of multidecadal variation or shifts in North Pacific climate, for four centuries.