冰雪融水径流
- 网络ice-snow melt runoff
冰雪融水径流-
随着气候变化，冰雪融水径流将发生明显变化。
There will bd pronounced alterations to glacier and snow runoff as the climate change .
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乌鲁木齐河源冰雪融水径流近期变化的分析
Analysis of Recent Change on Runoff of Melt Ice and Snow in Head of Urumqi River
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由于夏季冰雪融水作用，径流泥沙可比降雨提前到达峰值。
Due to the thaw of snow and ice in early summer , the peaks of runoff and sediment yield could precede that of rainfall .
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长江-黄河源区属典型寒区，降水、冰雪融水等共同成为径流的补给来源，径流量的变化同时受到区域内降水量和气温变化的影响。
Runoff at source regions of the Yangtze and Yellow Rivers were derived mostly from precipitation and melt-water of glaciers , snow and frozen earth .