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Dendrochronology (dendron
= tree, chronos = time, logos = the
science of) is defined as the science that uses
tree rings dated to their exact year of formation
to analyze temporal and spatial patterns in the
physical and cultural sciences. Analysis of tree
ring widths can be used to reconstruct both gradual
and abrupt changes in the climate of the past as
well as historical occurrences of major
disturbances such as fire, drought, and insect
outbreaks.
Diameter growth of trees in the
North Temperate Zone is typically characterized by
a single annual ring. In addition to variation
caused by species, age, and soil conditions, the
width of the growth ring depends upon the weather
conditions and disturbance patterns of the current
year. Temperature and soil water appear to be most
highly correlated to changes in ring
widths.
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