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变化环境下北江下游年径流量的加权马尔可夫链预测
引用本文:王亚雄,黄淑娴,刘祖发,林凯荣,卓文珊,刘珍珍,徐珲. 变化环境下北江下游年径流量的加权马尔可夫链预测[J]. 生态环境, 2011, 20(4): 754-760
作者姓名:王亚雄  黄淑娴  刘祖发  林凯荣  卓文珊  刘珍珍  徐珲
作者单位:中山大学水资源与环境系//华南地区水循环与水安全广东省普通高校重点实验室,广东广州,510275
基金项目:国家自然科学基金重点项目,国家自然科学基金,中央高校基本科研业务费专项资金
摘    要:在气候变化和人类活动的影响下,西北江的水文环境发生了重大变化,导致北江下游的来水条件发生变化。采用斯波曼检验(Spearman’s rho test)和Mann-kendall法系统地分析了北江下游的年径流量的变化趋势和变异情况,在此基础上建立了北江下游变化环境下年径流量的加权马尔可夫链预测模型。结果表明:西北江近50年来的大规模联围筑闸、大规模无序采掘河床泥沙等剧烈的人类活动,导致北江下游三水水文站年径流量在1990年左右发生了变异;所建立的加权马尔可夫链预测结果表明,从变异后的序列中统计出来的状态"转移概率"矩阵,能准确地反映出环境变化后年径流量之间的关系,所建立的加权马尔可夫链法预测变化环境下的年径流量是可行的,预测效果也比较好;按文章确定的分级标准,依现有的资料信息推断,环境发生变化后,在未来长期过程中,北江下游出现平水年的机会最大,但年际间的丰枯波动概率也不小。这一结果值得水资源管理部门注意。

关 键 词:变化环境  北江下游  加权马尔可夫链  年径流量  预测

Forecast of yearly river runoff in lower reaches of Beijiang River by Weighted Markov-Chain Method in changing environments
Wang Yaxiong,Huang Shuxian,Liu Zufa,Lin Kairong,Zhuo Wenshan,Liu Zhenzhen,Xu Hui. Forecast of yearly river runoff in lower reaches of Beijiang River by Weighted Markov-Chain Method in changing environments[J]. Ecology and Environmnet, 2011, 20(4): 754-760
Authors:Wang Yaxiong  Huang Shuxian  Liu Zufa  Lin Kairong  Zhuo Wenshan  Liu Zhenzhen  Xu Hui
Affiliation:Wang Yaxiong,Huang Shuxian,Liu Zufa*,Lin Kairong,Zhuo Wenshan,Liu Zhenzhen,Xu Hui Department of Water Resources and Environment,Sun Yat-Sen University//Key Laboratory of Water Cycle and Water Security in Southern China of Guangdong High Education Institute,Guangzhou 510275,China
Abstract:Hydrological conditions of Xijiang and Beijiang River(two tributaries of the Pearl River in south China,intersecting at Sixianjiao) have changed greatly due to climate changes and human activities,resulting in the change of flow in lower reaches of Beijiang River.Spearman's rho test and Mann-kendall method were used to analyze the trend change of yearly discharge and associated causes in lower reaches of Beijiang River,and a Weighted Markov-Chain model was thus proposed to forecast the yearly flow series.La...
Keywords:changing environments  lower reaches of Beijiang River  Weighted Markov-Chain  yearly river runoff  forecast  
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