长江科学院院报 ›› 2019, Vol. 36 ›› Issue (3): 19-25.DOI: 10.11988/ckyyb.20170749

• 水资源与环境 • 上一篇    下一篇

澜沧江流域旱涝特征变化及其与季风之间的关联性研究

唐见1,2, 翟文亮1,2, 曹慧群1,2   

  1. 1. 长江科学院 流域水环境研究所,武汉 430010;
    2.长江科学院 流域水资源与生态环境科学湖北省重点实验室,武汉 430010
  • 收稿日期:2017-06-28 出版日期:2019-03-01 发布日期:2019-03-20
  • 通讯作者: 曹慧群(1984-),女,江西景德镇人,高级工程师,博士,主要从事流域水生态环境过程演变研究。E-mail: caohuiqun@163.com
  • 作者简介:唐 见(1985-),男,安徽巢湖人,高级工程师,博士(后),主要从事流域水文过程变化及其生态效应研究。E-mail: tang0815@yeah.net
  • 基金资助:
    水利部公益性行业科研专项(201501002);国家自然科学基金项目(51609008);中央级公益性科研院所基本科研业务费项目(CKSF2015015/SH)

Changes in Characteristics of Drought/Flood and Its Connections with Monsoons in the Lancang River Basin

TANG Jian1,2, ZHAI Wen-liang1,2, CAO Hui-qun1,2   

  1. 1.Basin Water Environment Department,Yangtze River Scientific Research Institute, Wuhan 430010, China;
    2.Hubei Provincial Key Laboratory of River Basin in Water Resources and Eco-environmental Sciences, Yangtze River Scientific Research Institute, Wuhan 430010,China
  • Received:2017-06-28 Online:2019-03-01 Published:2019-03-20

摘要: 探讨澜沧江流域旱涝特征变化与季风之间的关联性,对于区域旱涝灾害的成因、机理和预测等重大科学问题的理解具有重要的意义。区域研究多侧重于揭示流域旱涝时空演变规律,而关于澜沧江流域的旱涝与季风的相互关系研究还较少。基于标准化降水指数(SPI12)、季风指数和水汽通量对澜沧江流域1957—2015年旱涝时空变化特征进行分析,探究澜沧江流域旱涝变化与季风指数的相互关系,并从水汽通量输送角度出发,进一步揭示季风对澜沧江流域旱涝变化影响的潜在驱动机制。研究结果表明:①流域旱涝特征具有明显的区域差异,下游区域是旱涝多发区;②流域干旱多于雨涝,且干旱频次在年和季节时间尺度上都呈现增加变化趋势;③澜沧江流域干旱和雨涝的频次主要存在3~5,8~15,20~25 a的3种周期性变化特征;④干旱和雨涝发生时段,南亚季风和高原季风指数与流域的SPI12指数相关性较强,受南亚季风和高原季风的输送距离影响,2种季风指数与SPI12指数的相互关系呈现区域差异性。研究结果有助于了解澜沧江流域旱涝时空变化特征,能够为防御旱涝灾害提供科学决策依据。

关键词: 旱涝, 季风, 标准化降水指数, 水汽通量, 澜沧江流域

Abstract: Studying the connections between drought/flood characteristics and monsoons in the Lancang River basin is of vital significance for understanding the causes, mechanisms and prediction of regional drought/flood disasters; yet the vast majority of existing studies are focused on the temporal and spatial evolution characteristics of drought/flood rather than on the connections between drought/flood characteristics and monsoons in the Lancang River basin. In this paper, the temporal and spatial changes in characteristics of drought/flood in 1957-2015 are investigated in terms of standard precipitation index (SPI12), monsoon index, and water vapor flux; the connections between drought/flood changes and monsoon index are examined, and the mechanism of drought/flood changes driven by monsoons and water vapor fluxes is further revealed. Results indicated that: (1) flood/drought has obvious regional difference, and the downstream area is prone to flood and drought; (2) the frequency of drought is superior to that of flood, showing an increasing trend in annual and seasonal time scales; (3) the frequencies of flood and drought mainly varied periodically at 3-5 years, 8-15 years, and 20-25 years; (4) in drought/flood period, indices of the South Asian monsoon and the Plateau monsoon have relatively strong correlations with the standard precipitation index (SPI12) in the Lancang River basin; such correlation varies in different regions due to the limited transportation distance of monsoons. The results are helpful in understanding the temporal and spatial change characteristics of drought/flood in the Lancang River basin, and also offer scientific basis for the decision-making of drought/flood prevention.

Key words: drought and flood, monsoon, standard precipitation index, water vapor flux, Lancang River basin

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