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《Journal of Arid Land Resources & Environment》 1989-02
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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

Wang zong-tai Institute of Glacier and Frozen Earth, Lan Zhou, Academia Sinica  
The paper, using measured datum on glacier, meltwater, temperature and run-off, estimates the outflow run-off in the late Epipleistocene on the south slope of the Bugeda mountain peak.The evaluation indicates that the amount 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, by utilizing the correlations of the modern glacier and ice meltwater.
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