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首页> 外文期刊>Arctic: Journal of the Arctic Institute of North America >A rare second year - lake ice cover in the Canadian High Arctic
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A rare second year - lake ice cover in the Canadian High Arctic

机译:罕见的第二年-加拿大高北极地区的湖泊冰盖

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摘要

Colour Lake, Axel Heiberg Island, N.W.T. (79 25 N; 90 45 W), remained largely ice covered from autumn 1985 to summer 1987. This is a relatively rare event. Observations and measurements of the thickness and specific conductance of the lake ice cover were made at the end of the 1986 summer and again in the following spring. The residual ice cover (second-year ice with first-year ice beneath it) was significantly thicker and had a lower specific conductance than first-year ice formed in marginal leads (moat) that had been ice free in 1986. The first-year ice that grew beneath the residual ice cover had the lowest specific conductance. Distribution of snow on the lake was affected by the roughness of the second-year ice (as compared to the smoother moat ice) and differences in elevation between second-year (high) and moat ice.
机译:N.W.T. Axel Heiberg Island的彩色湖(79 25 N; 90 45 W),从1985年秋季到1987年夏季,大部分时间仍被冰覆盖。这是一个相对罕见的事件。 1986年夏末和次年春天再次对湖冰盖的厚度和比电导进行了观测和测量。与1986年无冰的边际铅(护城河)中形成的第一年冰相比,残余的冰盖(第二年冰及其下的第一年冰)厚得多,比电导也较低。在残留冰盖下生长的冰的电导率最低。湖泊中雪的分布受第二年冰的粗糙度(与较光滑的mo河冰相比)以及第二年(高)和mo冰之间的海拔差异的影响。

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