收藏设为首页 广告服务联系我们在线留言

干旱区地理 ›› 1989, Vol. 12 ›› Issue (1): 11-16.doi: 10.13826/j.cnki.cn65-1103/x.1989.01.003

• • 上一篇    下一篇

叶尔羌河1987年洪水予报与未来洪水趋势予测

陈亚宁1, 王志超1, 由希尧2   

  1. 1.中国科学院新疆地理研究所
    2.新疆水利厅
  • 出版日期:1989-03-25 发布日期:2025-12-25

The Prediction of the 1987 Flood and the Estimation of the Tendency of Floods, Yarkand R. Xinjiang

Cheng Yaning, Wang Zhichao, You Xiyiao   

  • Published:1989-03-25 Online:2025-12-25

摘要: 叶尔河是南疆最大河流,洪水问题十分突出,以冰雪融水洪水和冰川突发性洪水危害最大。本文分析了不同类型洪水特点,揭示了洪水发生规律,通过资料、航片解译分析结合野外实地考察测量,对叶尔羌河1987年洪水进行了予报,并对叶尔羌河未来洪水发展变化趋势作了初步予测。

关键词: 冰川, 突发性洪水, 洪水成因

Abstract: It is little possible that the glacier-outburst flood would oc-cur in 1987.The reason given as below:first, the glacier dammed lake was just released water last year and it was empty on June thirteenth day, this year when we explored the lake;second, the air temperature is 2-4℃ lower than the other years;It will not be more than 25003 m/s , if flood occur in 1987, because the total of the lake can only store wa- ter 6000 m3 and stored as much as it can did before 2130 m3/s flood occurred last year.The tendency of this discharge of Jokulhlaups is decreasing because the size of the lake is reducing as the thickness of the glacier-dam geadually go-ingdown.
The glacier-melting floods is as usual, and the total of the run-off is probably lower than usual, because the air temperature is lower in the carly part of the year.
The average of the run-off will not be reduced in the Yarkand River within this century