冰川融水径流
- 网络glacier melt runoff
冰川融水径流-
乌鲁木齐河源气候特性与冰川融水径流
Climatic Characteristic and Glacial Runoff in the Source of Urumqi River
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卡尔塔马克冰川融水径流主要集中在6~8月，其存在着明显的日变化过程，融水径流受控于温度及降水要素。
The meltwater runoff is dependent mainly on ambient temperature and precipitation .
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中国西部不同类型冰川区积雪及其融水径流中稳定同位素比率的时空变化及其气候效应
Spatial and Temporal Variations of the Stable Isotopes in Snowpacks and Glacial Runoff in Different Types of Glacier Areas in China