Tree-ring growth varies with climate and stand density in a red pine plantation forest in the Great Lakes region of North America

Abstract

Red pine (Pinus resinosa Ait.) was widely planted across the Great Lakes region of North America in the early 20th century to restore tree cover to degraded forest and agricultural lands. In this study, a dendrochronological assessment of radial growth response to climate was conducted in an 82-year-old, previously thinned red pine plantation forest in southern Ontario, Canada. Climate-growth relationships were analyzed at multi-monthly and annual time scales using a 72-year residual growth chronology (1942–2013). Warmer temperatures and periodic drought during the current and previous growing seasons were associated with decreased growth, while higher precipitation during the early part of the current growing season was associated with increased growth. Moving interval correlation analysis of long-term trends indicated that climate-growth relations were temporally unstable due to thinning and variation in climate over the length of the chronology. The correlation between climate and growth was stronger when stand density was relatively high and diminished in the two decades following thinning. These results indicate that growth of red pine plantations near the species’ southern range limit may be much reduced if exposed to a warmer, drier future climate and that periodic thinning can help mitigate the impacts of future climate change on these plantations.