本文通过理论分析发现:对百年以上的冰川进退基本上决定于温度变化,与降水的关系不大。
Theoretical analysis in this paper reveals that glacial fluctuation in time scale longer than century is controlled mainly by temperature, it is weak in the relation to precipitation.
本文通过理论分析发现:对百年以上的冰川进退基本上决定于温度变化,与降水的关系不大。
Theoretical analysis in this paper reveals that glacial fluctuation in time scale longer than century is controlled mainly by temperature, it is weak in the relation to precipitation.
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