Process / pipelineDendrochronology and paleoclimatology
Dendrochronology Method
Dendrochronology is the science of dating and analyzing tree rings to reconstruct past climatic conditions, chronologies, and tree growth patterns. Pioneered by Andrew Ellicott Douglass in the early twentieth century and formalized by Fritts and colleagues, dendrochronology enables precise dating of historical wood samples and generates millennial-length climate records, becoming indispensable for paleoclimatology, archaeology, and forest ecology.
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Sources
- Fritts, H. C. (1976). Tree Rings and Climate. Academic Press. link ↗
- Stokes, D. L., & Smiley, T. L. (1996). An Introduction to Tree-Ring Dating. University of Arizona Press. link ↗
- Douglass, A. E. (1929). The Secret of the Southwest Solved by Talkless Rings. National Geographic Magazine, 56(6), 736–770. link ↗
- Briffa, K. R. (2000). Annual Climate Variability in the Holocene: Interpreting the Message of Ancient Trees. The Quaternary Review, 9(2), 87–105. DOI: 10.1016/S1040-6182(99)00090-1 ↗