Climatic Change

, Volume 150, Issue 3–4, pp 211–225 | Cite as

Climatic drivers of tree growth at tree line in Southwest Yukon change over time and vary between landscapes

  • Katherine D. Dearborn
  • Ryan K. Danby


Growth of trees at their altitudinal and latitudinal range limits is expected to increase as climate warms, but trees often exhibit unexplained spatial and temporal variation in climate-growth responses, particularly in alpine regions. Until this variability is explained, predictions of future tree growth are unlikely to be accurate. We sampled Picea glauca (white spruce) growing at forest and tree line on north and south aspects in two mountain ranges of southwest Yukon to determine how and why ring-width patterns vary between topographic settings, and over time. We used multivariate statistical analysis to characterize variation in ring-width patterns between topographic factors and time periods, and calculated correlations between ring-width indices and climate variables to explain this variation. Ring-width patterns varied more between mountain ranges than elevations or aspects, particularly in recent decades when ring-widths increased in one mountain range but not the other. Growth responses to summer temperature were notably weaker during warmer time periods, but growth was not positively correlated to summer precipitation, suggesting trees may not be suffering from temperature-induced drought stress. Rather, ring-width indices began responding positively to spring snow depth after 1976. We conclude that tree growth is unlikely to increase in synchrony with rising air temperatures across subarctic tree lines in southwest Yukon. Instead, they may decline in areas that are prone to thin snowpacks or rapid spring runoff due to the negative influence warming springs will have on snow depth and, consequently, early growing season soil moisture.



We thank Allison Slater, Laura Kitchen, Courtenay Jacklin, Lucas Brehaut, and Daz Kambo for help with fieldwork; Sian Williams, Lance Goodwin, and staff at the Kluane Lake Research Station for their generosity and logistical support; the Kluane First Nation for kind permission to conduct research on their traditional territory; and Tom Kurkowski, Stephanie McAfee, Dan McKenney, and Pia Papadopol for assistance with and provision of climate data.

Funding information

Funding for this research was provided by the Natural Sciences and Engineering Research Council of Canada (NSERC), the W. Garfield Weston Foundation, Queen’s University, and the Northern Scientific Training Program (NSTP).

Supplementary material

10584_2018_2268_MOESM1_ESM.pdf (206 kb)
ESM 1 (PDF 205 kb)
10584_2018_2268_MOESM2_ESM.pdf (56 kb)
ESM 2 (PDF 55 kb)
10584_2018_2268_MOESM3_ESM.pdf (41 kb)
ESM 3 (PDF 40 kb)
10584_2018_2268_MOESM4_ESM.pdf (2.6 mb)
ESM 4 (PDF 2614 kb)


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Copyright information

© Springer Nature B.V. 2018

Authors and Affiliations

  1. 1.Department of Geography and PlanningQueen’s UniversityKingstonCanada
  2. 2.School of Environmental StudiesQueen’s UniversityKingstonCanada

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