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Lake- and channel-bottom temperatures in the Mackenzie Delta, Northwest Territories
被引:10
|作者:
Ensom, T. P.
[1
]
Burn, C. R.
[1
]
Kokelj, S. V.
机构:
[1] Carleton Univ, Dept Geog & Environm Studies, Ottawa, ON K1S 5B6, Canada
基金:
加拿大自然科学与工程研究理事会;
关键词:
LATE QUATERNARY HISTORY;
WESTERN ARCTIC COAST;
PERMAFROST TEMPERATURES;
BEAUFORT REGION;
CANADA;
RIVER;
NWT;
D O I:
10.1139/E2012-001
中图分类号:
P [天文学、地球科学];
学科分类号:
07 ;
摘要:
Temperature loggers were placed in 17 lakes and 13 channels throughout the Mackenzie Delta to determine the annual mean bottom temperature ((Tb) over bar) and its spatial and temporal variation for June 2009 - June 2010. The lakes were classified as perched or connected, depending on the duration of their connection to the channel hydrologic system. Average (Tb) over bar values for nine perched lakes, five channels, and eight connected lakes distributed throughout the Mackenzie Delta were 5.5, 4.6, and 3.4 degrees C, respectively. The range of (Tb) over bar among all instrumented water bodies in the Delta was 4.0 degrees C. Over the year, bottom temperatures ranged from >20 degrees C in midsummer to -5 degrees C in midwinter, with relative stability between freezeup in mid-October and breakup at the beginning of June. Channel, perched, and connected lake Tb, and mean annual near-surface ground temperatures of -4 degrees C in alluvial sedge wetlands and -2.25 degrees C in forest, were used to estimate that about 60% of Delta lakes and nearly the entire channel network maintain through-taliks.
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页码:963 / 978
页数:16
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