Interpretationofδ₁8OinSnowandFirnataNorwegianAlpineGlacierandItsImplicationtotheLocalClimate——(挪威山地冰川上雪和粒雪中δ₁8O的解释及对区域气候的指示意义)

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• 出版年：2001
• 作者：HE Yuan-qing(何元庆)；SHEN Yong-ping(沈永平)；Wilfred H.Theakstone；YAO Tan-dong(姚檀栋)；CHENTuo(陈拓)；YANG Mei-xue(杨梅学)
• 单位1：Cold and Arid Regions Environmental and Engineering Research Institute
• 出生年：1957
• 学历：PhD
• 职称：professor
• 语种：中文
• 作者关键词：δ₁8O;snow and firn;climate; Norwegian
• 起始页：258
• 总页数：6
• 经费资助：National Natural Science Foundation of China(40071023);the Knowledge Innovation Key Project of the Chinese Acade- my of Sciences (KZCX-2-301); the Knowledge-Innovation Funds（CACX210506；CACX 210019) from the Laboratory of Ice Core and Co
• 刊名：冰川冻土
• 是否内版：否
• 创刊时间：1979
• 主办单位：中国地理学会；中国科学院寒区旱区环境与工程研究所
• 主编：陈国栋
• 卷：23
• 期：3
• 核心期刊：中国自然科学核心期刊

摘要

Variations of 180 in the snow which accumulates at a Nordic temperate glacier during the winterare not entirely eliminated after a few months of ablation in the following summer. Survive of isotopicsignals closely relates to the re-freezing capacity of snow accumulated in winter when its temperature wasbelow 0 .C. The melt-water re-freezing ice layers formed in winter hindered subsequent melt-water percolationin summer when snow temperature was at melting point and. therefore. varied isotopic record wasreserved between these ice layers.