| Title | Effects of observed and experimental climate change on terrestrial ecosystems in northern Canada: Results from the Canadian IPY program |
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| Author | Henry, G H R; Harper, K A; Chen, W ; Deslippe, J R; Grant, R F; Lafleur, P M; Lévesque, E; Siciliano, S D; Simard, S W |
| Source | Climatic Change; vol. 115, no. 1, 2012 p. 207-234, https://doi.org/10.1007/s10584-012-0587-1  Open Access |
| Year | 2012 |
| Alt Series | Natural Resources Canada, Contribution Series 20181360 |
| Publisher | Springer Nature |
| Document | serial |
| Lang. | English |
| Media | paper; on-line; digital |
| File format | pdf |
| Subjects | geophysics; Nature and Environment; remote sensing; Climate change |
| Program | Climate Change
Geoscience |
| Released | 2012 10 02 |
| Abstract | Tundra and taiga ecosystems comprise nearly 40 % of the terrestrial landscapes of Canada. These permafrost ecosystems have supported humans for more than 4500 years, and are currently home to ca.
115,000 people, the majority of whom are First Nations, Inuit and Métis. The responses of these ecosystems to the regional warming over the past 30-50 years were the focus of four Canadian IPY projects. Northern residents and researchers reported
changes in climate and weather patterns and noted shifts in vegetation and other environmental variables. In forest-tundra areas tree growth and reproductive effort correlated with temperature, but seedling establishment was often hindered by other
factors resulting in site-specific responses. Increased shrub cover has occurred in sites across the Arctic at the plot and landscape scale, and this was supported by results from experimental warming. Experimental warming increased vegetation cover
and nutrient availability in most tundra soils; however, resistance to warming was also found. Soil microbial diversity in tundra was no different than in other biomes, although there were shifts in mycorrhizal diversity in warming experiments. All
sites measured were sinks for carbon during the growing season, with expected seasonal and latitudinal patterns. Modeled responses of a mesic tundra system to climate change showed that the sink status will likely continue for the next 50-100 years,
after which these tundra systems will likely become a net source of carbon dioxide to the atmosphere. These IPY studies were the first comprehensive assessment of the state and change in Canadian northern terrestrial ecosystems and showed that the
inherent variability in these systems is reflected in their site-specific responses to changes in climate. They also showed the importance of using local traditional knowledge and science, and provided extensive data sets, sites and researchers
needed to study and manage the inevitable changes in the Canadian North. © 2012 The Author(s). |
| GEOSCAN ID | 311714 |
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