Pan Jinjun, Bai Meilan. Ice runs of the Yellow River and its defense in Inner Mongolia. J Appl Meteor Sci, 2008, 19(1): 106-110. .
Citation: Pan Jinjun, Bai Meilan. Ice runs of the Yellow River and its defense in Inner Mongolia. J Appl Meteor Sci, 2008, 19(1): 106-110. .

Ice Runs of the Yellow River and Its Defense in Inner Mongolia

More Information
  • Ice run is a kind of nature disaster mainly induced by meteorological factors. The regions along the Yellow River bank in Inner Mongolia are frequently influenced by the disaster and it may result in losses of properties and menace to human safety. The disaster's characters, forming mechanism, occurrence prone period, tendency prediction as well as hazard estimation are studied and analyzed. Based on these analyses, some conclusions are obtained as follow. The ice run is a kind of special natural disasters resulted from both the climatic and geographical factors in specific area; the ice run occurs only in ice river's opening and closing periods which are about one month long respectively in spring and autumn season; with the global warming trend, the ice river opening time is becoming earlier and the closing time is being postponed gradually, so the disaster's hazards will increase; according to both the disaster particularity and its present defending situation, some countermeasures are proposed to be taken such as strengthening the infrastructure project construction, and the disaster forecasting and monitoring system construction as well as paying attention to enhance the public prevention awareness etc.
  • Fig  1.   The distribution of the Yellow River bank in Inner Mongolia

    Fig  2.   The ice thawing trend variation of Dengkou station

    Fig  3.   The ice closing trend variation of Dengkou station

    (January in the figure refers to that of the next year)

    Table  1   The geographical and temperature features of the major stations along the Yellow River bank from Lanzhou to Inner Mongolia

    DownLoad: CSV

    Table  2   The gradient and curvature of each section along the Yellow River bank from Lanzhou to Inner Mongolia

    DownLoad: CSV

    Table  3   The stations and its temperature features of the major stations along the Yellow River bank in Inner Mongolia

    DownLoad: CSV
  • 王京堂.黄河凌汛灾害的成因分析与对策研究.中国减灾, 1996, 3:39-41. http://www.cnki.com.cn/Article/CJFDTOTAL-ZGJI603.012.htm
    白美兰, 郝润全, 那琳.黄河内蒙古段凌汛气象预报服务系统.内蒙古水利, 2002, 1:31-34. http://www.cnki.com.cn/Article/CJFDTOTAL-NMSL200201014.htm
    宫德吉, 白美兰, 王秋晨.黄河凌汛及其预报方法研究.气象, 2001, 27(5):38-42. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXX200105011.htm
    蔡振中.内蒙古水资源的利用.呼和浩特:内蒙古水利勘察设计院, 1990.
    闫新光.影响内蒙古黄河凌汛的三大要素.内蒙古水利, 2002, 1:19-21. http://www.cnki.com.cn/Article/CJFDTOTAL-NMSL200201006.htm
  • Related Articles

    [1]Huo Zhiguo, Li Chunhui, Kong Rui, Mao Hongdan, Jiang Mengyuan, Song Yanling. Review on Disaster of Wire Icing in China[J]. Journal of Applied Meteorological Science, 2021, 32(5): 513-529. DOI: 10.11898/1001-7313.20210501
    [2]Shen Xinyong, Huang Wenyan, Wang Weiguo, Guo Chunyan. Contrastive Study on Two Boundary Layer Parameterization Schemes Using TWP-ICE Experiment Data[J]. Journal of Applied Meteorological Science, 2014, 25(4): 385-396.
    [3]Liu Yonghong, Hu Haibo, Fang Xiaoyi, Xie Pu. Early Warning and Evaluating Impacts of Ice and Snow Disasters on Beijing Urban Transportation[J]. Journal of Applied Meteorological Science, 2013, 24(3): 373-379.
    [4]Liang Feng, Tao Shiyan, Zhang Xiaoling. Diagnostic Analysis of a Heavy Rain Event in North China Caused by the Development of Yellow River Cyclone[J]. Journal of Applied Meteorological Science, 2006, 17(3): 257-265.
    [5]Yang Xianmin, Zeng Yan, Qiu Xinfa, Jiang Aijun. THE CLIMATIC CHANGE OF GLOBAL SOLAR RADIATION OVER THE YELLOW RIVER BASIN DURING 1960 —2000[J]. Journal of Applied Meteorological Science, 2005, 16(2): 243-248.
    [6]Wang Guoqing, Wang Yunzhang, Kang Lingling. ANALYSIS ON THE SENSITIVITY OF RUNOFF IN YELLOW RIVER TO CLIMATE CHANGE[J]. Journal of Applied Meteorological Science, 2002, 13(1): 117-121.
    [7]Ma Lan, Xu Xi, Gao Yun, Ma Zailan. ANALYSIS OF WATER VAPOR TRANSPORTATION OVER THE UPPER REACHES OF THE CHANGJIANG RIVER AND ITS RELATION WITH THE RUN-OFF IN 1997 AND 1998[J]. Journal of Applied Meteorological Science, 2000, 11(4): 491-498.
    [8]The Clues for Prediction of Torrential Rain over Yangtze River and Yellow River Valleys[J]. Journal of Applied Meteorological Science, 1998, 9(1): 109-113.
    [9]Yu Shuqiu, Lin Xuechun. Abrupt Change of Drorght/Flood for the Last 522 Years in the Middle Reaches of Yellow River[J]. Journal of Applied Meteorological Science, 1996, 7(1): 89-95.
    [10]Hu Zengzhen.. The Effect of Greenland Sea Ice Anomaly in June on the Drought-flood in Upper-middle Reaches of Yellow River in July[J]. Journal of Applied Meteorological Science, 1995, 6(3): 366-372.

Catalog

    Figures(3)  /  Tables(3)

    Article views3792 PDF downloads2294 Cited by: 
    • Received : 2006-12-17
    • Accepted : 2007-07-10
    • Published : 2008-02-28

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return