Ice-push disturbances in high-Boreal and Subarctic lakeshore ecosystems since AD 1830, northern Québec, Canada

• Published in: Holocene (Sevenoaks) Vol. 10; no. 2; pp. 179 - 189
• Main Author: BEGIN, Y
• Format: Journal Article
• Language: English
• Published: Thousand Oaks, CA SAGE Publications 2000; Turpin; Sage Publications Ltd
• Subjects: Art and archaeology; Canada, Quebec; Environmental assessment; Fauna; Generalities; Methods; Research principies; Canada; America; Quebec; Canada; Flood; Snow; Ice scar; Tree-ring; Ecosystem disturbance; Boreal; Subarctic; Ice Push; Lake Shoreline; Québec; Climatology; Hydrology; Vegetation study; Geomorphology; Geology; Dendrochronology
• ISSN: 0959-6836; 1477-0911
• DOI: 10.1191/095968300672152610

Ice scars on lakeshore trees were surveyed on the islands of two large lakes in northern Québec: Clearwater Lake (1270 km2) and Bienville Lake (900 km2), respectively at the southern edge of the Subarctic and at the northern limit of the Boreal zones. Correspondence of ice-scar chronologies with hydrological and climatological instrumental registers indicated that shore ice pushes are due to lake floods. In the AD 1930s, a shift in the flood regimes occurred. In the high Boreal, ice-push activity was much more frequent prior to 1930 than in the Subarctic. Major regional ice pushes occurred in AD 1854, 1903, 1914, 1936, 1947, 1954,1959-60, 1970 and 1979. Prior to 1930, local major events were concentrated south of the Subarctic zone, but the situation inverted after 1930. A northward shift in the average position of the Arctic front is postulated as having been the driving force of local hydrologic regimes that allowed ice disturbances to occur, especially A in controlling the amount of snowfall. Ice scars provide proxy indicators of an increase in the frequency of snowy winters between the mid-1930s and 1980. The recent period of low levels represents an anomalous incursion in the century trend, but equivalent long episodes of low seasonal lake levels occurred prior to 1930.