| 博格达峰区南坡晚更新世晚期冰水河的出山地表径流估算 |
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| 引用本文： | 王宗太. 博格达峰区南坡晚更新世晚期冰水河的出山地表径流估算[J]. 干旱区资源与环境, 1989, 0(2) |
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| 作者姓名： | 王宗太 |
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| 作者单位： | 中国科学院兰州冰川冻土研究所 |
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| 摘 要： | 本文使用了有关冰川面积、融水量、气温及地表迳流等实测数据,对博格达峰区南坡晚更新世晚期冰水河的出山地表迳流进行了估算。估算表明,其迳流量高达5.7亿m~3左右,是现在迳流量的2.1倍。同时还表明,利用现代冰川同冰融水的相关性,估算其古冰期的地表迳流,是可行的。
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THE RUN-OFF EVALUATION ON THE OUTFLOW OF THE GLACIOFLUCIAL RIVERS IN THE LATE EPIPLEISTOCENE PERIOD ON THE SOUTH SLOPE OF THE BUGEDA MOUNTAIN PEAK AREA |
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| Abstract: | The paper, using measured datum on glacier, meltwater, temperatureand run-off, estimates the outflow run-off in the late Epipleistocene on thesouth slope of the Bugeda mountain peak.The evaluation indicates that theamount of the run-off in this area is as high as 5. 7 thousand million m~3,which is 2. 1 times of its present size. Meanwhile, the evaluation also.indicates the possibility of estimating the run-off in the ancient Ice Age, byutilizing the correlations of the modern glacier and ice meltwater. |
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