Climate insensitivity of treeline in the Canadian Rocky Mountains
Abstract
Successful modelling efforts demonstrate that tree presence over a ~ 200 km2 alpine/subalpine area in the Front Ranges of the Canadian Rocky Mountains results from a multi-scale spatiotemporal process competition involving not only growing season temperatures but also topographical shelter, water availability, and substrate stability and availability. The study area was selected to represent the diversity of substrates and geomorphologic processes found in the Canadian Rockies, and ranges in elevation from 1400 to > 2800 meters above sea level. Tree presence was mapped at 10m resolution using a combination of remote sensing imagery (taken in 2008) and intensive ground truthing, and modelled with an ensemble of state-of-the-art environmental envelope models. Explanatory variables chosen represented not only temperature and moisture availability (computed over 1971-2000 climate normals), but also substrate diversity, slope angle and type, geomorphologic features, modelled regolith depth, and concavity/convexity of the terrain. Such variables were meant to serve as proxies for known convergent and divergent processes that occur on steep landscapes and that have profound influence on tree establishment and survival. Model performance was very high and revealed substrate and geomorphology to be the most important explanatory variables for tree presence in the area. Available high-resolution imagery for 1954 enabled the mapping of tree presence over most of the study area and the identification of changes in the distribution of trees over the last nearly six decades. Overall, the only major observed changes were related to post-fire stand recovery, and areas with treeline advance were insignificant at the landscape scale. Tree suitable sites were projected onto high resolution grids of late 21st century climatic conditions predicted by regional climate models driven by atmosphere-ocean general circulation models. Emissions scenario was A2 (as defined in the Special Report on Emissions Scenarios used by the Intergovernmental Panel on Climate Change), at the higher end of emissions scenarios, and thus at the higher end of forecasted temperature increases. Projected changes in tree site availability were minimal at the landscape scale, as the presence of trees in the uppermost part of these forests largely depends on the existence of suitable sites largely linked to topography. Such places are the result of geomorphologic processes acting on a framework set by the structural geology of the region, and thus the appearance of new sites suitable for tree growth does not depend on short (i.e. yearly to decadal) time scales but on longer ones (i.e. centuries to millennia). This work has the strength of studying treeline over a whole area, thus avoiding potential biases in the regional representativity of local study sites, and warns against careless upscaling of site-based studies. Moreover, we suggest that the term 'treeline' is weak at a high-resolution landscape scale in our study area (i.e. young glaciated terrain) because the distribution of trees over the landscape is spatially irregular and most of the processes enabling or preventing tree presence occur over its whole elevational range.
- Publication:
-
AGU Fall Meeting Abstracts
- Pub Date:
- December 2011
- Bibcode:
- 2011AGUFM.B13D0603J
- Keywords:
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- 0439 BIOGEOSCIENCES / Ecosystems;
- structure and dynamics;
- 0476 BIOGEOSCIENCES / Plant ecology;
- 0480 BIOGEOSCIENCES / Remote sensing;
- 1630 GLOBAL CHANGE / Impacts of global change