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Sensitivity of Peatlands to Climate Change

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Abstract

Sensitivity of peatlands to climate warming is shown here. Peatlands are massive deposits of peat, a material consisting largely of organic residue that acts as a natural sink for carbon. With global warming, however, they have the potential to become immense sources of greenhouse gases, and contribute significantly to further warming. The geographic areas where peatland will be most affected are the Hudson Bay lowlands, the Mackenzie River valley region and the northern parts of Alberta and Manitoba.

The Theme

Peat is a material consisting largely of organic residues, originating under somewhat water-saturated conditions through the incomplete decomposition of plant and animal matter. Peatlands are defined as areas that form massive deposits of peat - peat thicknesses reach at least 40 centimetres. Much of Canada's peatland area lies atop permafrost. Approximately 12% of the Canadian landmass is covered with peatlands.

At present, peatlands are natural sinks of carbon. With global warming, however, they have the potential to become immense sources of greenhouse gases due to the lowering of the water table and, with the associated feedback mechanism, to contribute significantly to further warming. This map shows the sensitivity of peatlands to climate warming. This map shows the sensitivity of peatlands to climate warming.

Sensitivity Projection

Approximately 60% of the peatlands in Canada lie within areas that are expected to be severely affected by climate warming. The geographic areas where peatland will be most affected are the Hudson Bay lowlands, the Mackenzie River valley region and the northern parts of Alberta and Manitoba.

In terms of ecoclimatic provinces, the most pronounced changes are expected to occur in the Boreal, Sub-Arctic and Arctic regions. In these regions, many peatland areas are found overlying permafrost. With warming, it is likely that the upper part of the permafrost would melt and much of the surface water that is essential for peatland development would drain thereby allowing the peat to decompose. This would result in a decrease in methane production and an increase in the release of carbon dioxide. On the other hand, a deep-enough thaw of permafrost would allow hydrates to thaw and thereby produce methane. Thus the depth of both the permafrost and the peat are important in determining the amount of greenhouse gas production. At the same time, the poor drainage conditions and subsidence associated with thawing are expected to increase the problems for construction and maintenance of buildings, highways and pipelines in these northern regions.

Data Source

Tarnocai C., I.M. Kettles, and B. Lacelle. 2000. Peatlands of Canada. Geological Survey of Canada, Open File 3834. Scale 1:6 500 000. Ottawa. Natural Resources Canada.

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Date modified: 2004-01-21 Top of Page Important Notices