Canadian Forest Service Publications
Continental-scale tree-ring-based projection of Douglas-fir growth: Testing the limits of space-for-time substitution. 2020. Klesse, S.; DeRose, R.J.; Babst, F.; Black, B.A.; Anderegg, L.D.L.; Axelson, J.; Ettinger, A.; Griesbauer, H.; Guiterman, C.H.; Harley, G.; Harvey, J.E.; Lo, Y.-H.; Lynch, A.M.; O'Connor, C.; Restaino, C.; Sauchyn, D.; Shaw, J.D.; Smith, D.J.; Wood, L.; Villanueva-Diaz, J.; Evans, M.E.K. Global Change Biology 26(9):5146-5163.
Issued by: Northern Forestry Centre
Catalog ID: 40982
Availability: PDF (download)
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A central challenge in global change research is the projection of the future behavior of a system based upon past observations. Tree-ring data have been used increasingly over the last decade to project tree growth and forest ecosystem vulnerability under future climate conditions. But how can the response of tree growth to past climate variation predict the future, when the future does not look like the past? Space-for-time substi tution (SFTS) is one way to overcome the problem of extrapolation: the response at a given location in a warmer future is assumed to follow the response at a warmer location today. Here we evaluated an SFTS approach to projecting future growth of Douglas-fir (Pseudotsuga menziesii), a species that occupies an exceptionally large environmental space in North America. We fit a hierarchical mixed-effects model to capture ring-width variability in response to spatial and temporal variation in climate. We found opposing gradients for productivity and climate sensitivity with highest growth rates and weakest response to interannual climate variation in the mesic coastal part of Douglas-fir's range; narrower rings and stronger climate sensitivity occurred across the semi-arid interior. Ring-width response to spatial versus temporal temperature variation was opposite in sign, suggesting that spatial variation in productivity, caused by local adaptation and other slow processes, cannot be used to anticipate changes in productivity caused by rapid climate change. We thus substituted only climate sensitivities when projecting future tree growth. Growth declines were projected across much of Douglas-fir's distribution, with largest relative decreases in the semiarid U.S. Interior West and smallest in the mesic Pacific Northwest. We further highlight the strengths of mixed-effects modeling for reviving a conceptual cornerstone of dendroecology, Cook's 1987 aggregate growth model, and the great potential to use tree-ring networks and results as a calibration target for next-generation vegetation models.