冰川冰和冰川表面雪融水汇入河道形成的径流。多数为季节性径流，少数大冰川末端为常年性径流，是寒冷地区的重要水资源。
... Runoff decrease by water reuse 回用水造成的径流减少 glacier melt water runoff 冰川融水径流 ground water runoff 地下径流 ...
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冰川融水径流 glacier melt water runoff ; glacier melt runoff ; glacial runoff ; glacial meltwater runoff 冰川融水径流量 runoff of glacier meltwater ; amount of glacier meltrunoff .
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冰川融水径流 glacier melt water runoff ; glacier melt runoff ; glacial runoff ; glacial meltwater runoff 冰川融水径流量 runoff of glacier meltwater ; amount of glacier meltrunoff ..
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降水与冰川融水径流量增加百分率相比，增加幅度较小。
But, as compared to the increased percentage of runoff from glacier meltwater, the increase amplitude is smaller.
由于长江源区冰川变化幅度小，虽冰川退缩使冰川融水径流量有所增加，但对径流的影响程度相对较小。
Although retreat of glaciers causes increase in glacier melt water runoff, the effect of glacier retreat on sur - face runoff is relatively small because of small amplitude of glacier change.
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