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通过在北欧Ａｕｓｔｒｅ Ｏｋｓｔｉｎｄｂｒｅｅｎ 冰川积雪内的实际测定结果，证明野外测量积雪内液体水含量的新方法———酒精量热法是可行和适用的，解决了过去测定积雪内液体水含量时遇到的困难。５ 个雪坑剖面的测定结果清楚地显示出雪内液体水含量的区带性和随高度的变化，积雪内液体水含量的垂直变化与雪层中物理结构、温度和密度的分布有关。
Based on the actual measurements of the snow in the Austre Okstindbreen glacier in the northern Europe, it is proved that the new method of measuring the liquid water content in the snow - alcohol calorimetry - is feasible and applicable, which solves the problem of measuring the liquid water content in the snow problems at hand. The results of the five snow pit sections clearly show the zonality and height variation of the water content in the snow. The vertical variation of the water content in the snow is related to the physical structure, temperature and density distribution in the snow layer.