Abstract
This article contains measurements of raw radial growth, distance to pith, and calculated basal area increments (BAI) from 444 5-mm increment cores (237 trees) collected in July 2016 from the Beaverhead-Deerlodge National Forest, MT. These data were used for the study presented in “Mountain pine beetle attack faster growing lodgepole pine at low elevations in western Montana, USA” [1]. Plot locations where increment cores were taken as well as code to calculate BAI are also included. Cores were collected from lodgepole pine (Pinus contorta) trees that were killed during a recent bark beetle outbreak (220 cores; 117 trees) as well as trees that survived the outbreak (210 cores; 113 trees) in twelve stands spanning north and south aspects and three elevational bands along a 600-m gradient. 14 additional cores were collected from 7 strip-attacked trees. Increment cores were prepared and measured using standard dendrochronological techniques, “An Introduction to Tree-Ring Dating” [2]. Master chronologies for each aspect-elevation combination were created using approximately ten cores from surviving trees at each location. Cores were cross-dated, then scanned at 2400 dpi. Annual ring widths were measured using CooRecorder 7.7, “Cybis Electronic, CDendro and CooRecorder V.7.7” [3], and final chronologies were quantitatively validated in COFECHA, “Computer-assisted quality control in tree-ring dating and measurement, Tree-Ring Society” [4].
Highlights
Data on beetle-killed and surviving lodgepole pine (Pinus contorta) radial growth from the Beaverhead-Deerlodge National Forest, MT prior to a severe mountain pine beetle outbreak
Raw; analyzed Two cores were collected per tree
Data were collected from north/south aspects and three elevational bands, and from both beetle-killed and surviving trees
Summary
Our study sites are located within the Boulder Mountains of the Beaverhead-Deerlodge National Forest, where elevation ranges from $ 1400 m to $ 3100 m. Study sites are located between $ 1800 m and $ 2500 m elevation. Primary tree species in the area are lodgepole pine (Pinus contorta), Douglas-fir Was the warmest month with an average maximum air temperature of 28.2 °C [5]. Within this period, annual precipitation averaged 279 mm, with most precipitation falling in June. The actual study site air temperature is likely lower and precipitation higher as Boulder, MT is located just outside the forested area at a lower elevation (1521 m)
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