The characterization of inter-decadal climate variability in the Southern Hemisphere is severely constrained by the shortness of the instrumental climate records. To help relieve this constraint, we have developed and analyzed a reconstruction of warm-season (November-April) temperatures from Tasmanian tree rings that now extends back to 800 B.C.
CITATION STYLE
Cook, E. R., Buckley, B. M., & D’Arrigo, R. D. (1996). Inter-decadal climate oscillations in the Tasmanian sector of the Southern Hemisphere: Evidence from tree rings over the past three millennia. In Climatic Variations and Forcing Mechanisms of the Last 2000 Years (pp. 141–160). Springer Berlin Heidelberg. https://doi.org/10.1007/978-3-642-61113-1_8
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