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Interference of natural and anthropogenic forcings on variations in continental freshwater discharge from the Red River (Vietnam) to sea

机译:自然和人为强迫对从红河(越南)到海洋的大陆淡水排放量变化的干扰

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摘要

Continental freshwater discharge is vital to global human development. Intensive studies have been conducted on changes of river discharge around the world (Dai et al., 2009; Milliman and Farnsworth, 2011). However, little work has been carried out on the daily continental freshwater discharge of the Red River in response to influence of the natural and anthropogenic forcings. This paper presents results of change analysis of daily continental freshwater discharge over the period 1956-2009 in the Red River. The wavelet analysis results showed observable periodicities in the continental freshwater discharge series with 4-6 months, 8-12 months, 1.5-2 years, and 4-7 years (48-80 months), respectively. The results from Mann-Kendall test indicated insignificant trends in annual continental freshwater discharge during the study period, but there is clearly decrease in annual suspended particulate matter of the Red River. It is shown that the continental freshwater discharge from the Red River was dominated by precipitation over the catchments. Moreover, changes in the continental freshwater discharge are closely related to SASM (the South Asia Summer Monsoon) and ENSO (EI Nino Southern Oscillation). Variations in daily discharge are lagged behind SASM 13-29 days. It revealed that El Nino and La Nina events are likely to induce extreme low and extreme high continental freshwater discharge from the Red River into the Tokin Gulf, respectively. Meanwhile, continental freshwater discharge from the Red River into the Tonkin Gulf experienced abrupt changes with present characteristics as 'no flood in the flood season, no drought in the drought season' due to water regulation induced by dam. (C) 2015 Elsevier Ltd and INQUA. All rights reserved.
机译:大陆淡水排放对全球人类发展至关重要。已经对全球河流流量的变化进行了深入研究(Dai等,2009; Milliman和Farnsworth,2011)。但是,由于自然和人为强迫的影响,红河每天的大陆淡水排放工作很少。本文提出了红河地区1956-2009年期间每日大陆淡水排放量变化分析的结果。小波分析结果表明,大陆淡水排放序列的可观测周期分别为4-6个月,8-12个月,1.5-2年和4-7年(48-80个月)。曼恩·肯德尔试验的结果表明,在研究期间,年度大陆淡水排放量的趋势不明显,但红河的年度悬浮颗粒物明显减少。结果表明,红河的大陆淡水排放主要是流域的降水。此外,大陆淡水排放量的变化与SASM(南亚夏季风)和ENSO(EI Nino南方涛动)密切相关。每天排放量的变化滞后于SASM 13-29天。结果表明,厄尔尼诺现象和拉尼娜事件可能分别引起从红河到托金湾的极低和极高的大陆淡水排放。同时,由于大坝引起的水调节作用,从红河向吨金湾的大陆淡水排放突然发生了变化,表现为“汛期没有洪水,旱季没有干旱”。 (C)2015 Elsevier Ltd和INQUA。版权所有。

著录项

  • 来源
    《Quaternary International》 |2015年第4期|133-142|共10页
  • 作者单位

    E China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China.;

    E China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China.;

    E China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China.;

    E China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China.;

    E China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China.;

    E China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China.;

    E China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China.;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Continental freshwater discharge; Extreme condition; Red River; Anthropogenic activities;

    机译:大陆淡水排放;极端条件;红河;人为活动;

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