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Based at Oregon State University since its inception in 1995, the Northwest Alliance for Computational Science and Engineering (NACSE) is an interdisciplinary research coalition that works to make large scientific databases accessible to different user audiences.


The data served in the Pacific Northwest Tree Ring Database were collected and analyzed by David L. Peterson (University of Washington and USDA Forest Service) and David W. Peterson.

Pacific Northwest Tree Ring Database

Mountain Hemlock
Mountain Hemlock
(Tsuga mertensiana)
[Photograph: Susan McDougall @ USDA-NRCS PLANTS Database]

The Pacific Northwest Tree Ring Database contains time series of radial growth from tree ring research conducted in Oregon and Washington. Users can query the database for particular sites, species, elevation, or start and end years. Data can be viewed on screen or downloaded.

Tree-ring data were gathered on 11 sites for mountain hemlock and 9 sites for subalpine fir. Sampling locations were chosen to represent the range of climatic conditions under which subalpine fir and mountain hemlock occur in this area. At most locations, three sites were selected for tree-ring chronology development that spanned the local elevational range. Increment cores were collected from 9-30 trees at each site, and two cores were taken from each tree. In the lab, tree-rings were dated and measured to produce a ring-width time series for each ring.

Subalpine Fir
Subalpine Fir (Abies lasiocarpa)
[Photograph: Susan McDougall @ USDA-NRCS PLANTS Database]

What is a Tree Ring?

Tree Ring of Douglas Fir
Douglas-fir (Pseudotsuga menziesii) cross section obtained from the Zuni Mountains of New Mexico
[Photograph: Copyright H.D. Grissino-Mayer]
Each year a tree's trunk grows wider from the continual division of cells beneath the bark during the growth season. Some cells (called phloem) develop into new bark, while others (called xylem) contribute to the layers of wood. During the growth season, the xylem cells grow at different rates depending on the climatic conditions. At the end of the season, growth ceases and there is an obvious boundary at the edge of the ring. It is then possible to determine the age of a tree by counting its number of rings. Dead trees can be sampled by taking a cross section of the trunk. Rather than cut down a living tree to count its rings, scientists use an increment borer to bore into a tree's trunk and then extract a core of the wood. The resulting sample preserves the tree ring structure without harming the tree. Climate scientists study tree rings to learn about past climate patterns.

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