English - Cornell Tree-Ring Laboratory - Cornell University 2025

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Our key long-range goal is to build long multi-millennial scale tree-ring chronologies in the Aegean and Near East that will extend from the present to the early Holocene to cover, broadly speaking, the last 10,000 years of human and environmental history.
Dendrochronology is the precise and reliable assignment of the tree rings year of formation. It is defined as the study of the chronological sequence of annual growth rings in trees (Ferguson, 1970).
The greatest weaknesses are that: tree-ring chronologies only capture a fraction of climate variability; their response may be limited to specific seasonal windows some do not respond directly to a single monthly or even seasonal climate variable; they may not record the climate variables of interest to
Even given this amount of material, and a suitable local master curve, the method is not always successful, but where it is it yields a very precise date, giving not only the exact year, but even the season of growth of the outermost ring present.
The Cornell Lab of Ornithology is a member-supported unit of Cornell University in Ithaca, New York, which studies birds and other wildlife.
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Dendrochronology can show us more than just the age of trees. It can also give us a glimpse into past climatic conditions. In temperate zones, one year of growth will equal one tree ring. A wet growing season makes a wider ring, while a dry growing season makes a narrower ring.

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