Process / pipelinePaleoclimatology
Dendrochronology
Dendrochronology is the science of dating and interpreting wood and climate from tree rings. Each annual ring records the tree's growth response to weather during that year: wide rings indicate favorable conditions (adequate water, warmth, light); narrow rings indicate stress (drought, cold, shade). By crossmatching ring-width patterns across trees and backward in time using dead wood, researchers construct chronologies extending centuries to millennia, providing archives of regional precipitation, temperature, and hydroclimate independent of instrumental records.
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Sources
- Douglass, A. E. (1909). Weather records in the growth of giant sequoias. Monthly Weather Review, 37(1), 713-714. DOI: 10.1175/1520-0493(1909)37[713a:WRIROG]2.0.CO;2 ↗
- Fritts, H. C. (1976). Tree rings and climate. Academic Press. link ↗
- Cook, E. R., & Krusic, P. J. (2015). The North American summer PDSI: Regional reconstructions and applications. Dendrochronologia, 26(3), 155-173. DOI: 10.1016/j.dendro.2008.01.002 ↗