Allard, Michel, Fortier, Richard (1990) The thermal regime of a permafrost body at Mont du Lac des Cygnes, Quebec. Canadian Journal of Earth Sciences, 27 (5) 694-697 doi:10.1139/e90-067
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | The thermal regime of a permafrost body at Mont du Lac des Cygnes, Quebec | ||
| Journal | Canadian Journal of Earth Sciences | ||
| Authors | Allard, Michel | Author | |
| Fortier, Richard | Author | ||
| Year | 1990 (May 1) | Volume | 27 |
| Issue | 5 | ||
| Publisher | Canadian Science Publishing | ||
| DOI | doi:10.1139/e90-067Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 480899 | Long-form Identifier | mindat:1:5:480899:6 |
| GUID | 0 | ||
| Full Reference | Allard, Michel, Fortier, Richard (1990) The thermal regime of a permafrost body at Mont du Lac des Cygnes, Quebec. Canadian Journal of Earth Sciences, 27 (5) 694-697 doi:10.1139/e90-067 | ||
| Plain Text | Allard, Michel, Fortier, Richard (1990) The thermal regime of a permafrost body at Mont du Lac des Cygnes, Quebec. Canadian Journal of Earth Sciences, 27 (5) 694-697 doi:10.1139/e90-067 | ||
| In | (1990, May) Canadian Journal of Earth Sciences Vol. 27 (5) Canadian Science Publishing | ||
| Abstract/Notes | A low peat plateau in the alpine forest–tundra at Mont du Lac des Cygnes, 100 km northeast of Québec City, contains a permafrost body 2 m thick. At an elevation of 960 m, this is the southernmost known occurrence of alpine permafrost in eastern Canada. The terrain over the permafrost is windblown and bears a very thin and discontinuous snow cover. One year of continuous temperature records indicates that the mean annual air temperature at this site is about −1.3 °C. The permafrost remains at temperatures very near the freezing point for most of the year. | ||
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