is the analysis of tree rings, including the dating of annual rings and
study of patterns of ring characteristics, such as widths, density,
and isotopic composition. In mid- to upper latitudes, or areas where there
is seasonality in temperature and/or precipitation, many species of trees
form annual growth rings. Because the same set of environmental factors
influence tree growth throughout a region, the patterns of ring characteristics,
such as ring widths, are often common from tree to tree. These patterns
can be matched between trees in a process called crossdating,
which is used to assign exact calendar year dates to each individual ring.
Dated and measured rings from a number of trees in a region are combined
to form a tree-ring chronology. The chronology provides two main types of
- The chronology can be used as a tool for dating events that caused tree death or a marked change in the
appearance of a ring or set of rings. The death date can be used to date the tree cutting involved in the construction of wooden dwellings. Scars can record the timing of events such as fire, flood, avalanche, or other geomorphological events, while
sequences of suppressed or larger rings record events such as insect infestation, effects of pollution, or changes in forest dynamics.
- The chronology is an average of coherent variations in growth from a number of trees. It enhances the common
pattern of variation or "signal" -- usually related to climate -- while the non-common variance, or "noise" is dampened. Chronologies from trees that are sensitive to climate can be used to reconstruct past variations in seasonal temperature,
precipitation, drought, streamflow, and other climate-related variables.
Laboratory of Tree-Ring Research, The University of Arizona
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