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Analyses of landuse change impacts on catchment runoff using different time indicators based on SWAT model

机译:基于SWAT模型的不同时间指标的土地利用变化对流域径流的影响分析

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摘要

Previous researches mainly focused on the runoff responses to landuse change based on annual, seasonal or monthly time scales, there are few studies based on daily scale. We conducted a comprehensive investigation into runoff responses on the daily scale as well as annual and monthly time scales using SWAT, and compared the impacts of time scales with different time indicators quantitatively. Jinjiang, a coastal catchment of southeast China with a humid sub-tropical climate, was used for simulations. A calibrated SWAT model produced satisfactory reproduction of annual, monthly and daily runoff processes over a nine-year (2002-2010) period at three gauging stations. Runoff was then simulated and compared using the same meteorological input but two different landuse scenarios (1985 and 2006, with reduced forest and increased cropland and urbanized area). The results showed varying change in runoff among three time scales and three catchments. The annual runoff had the smallest increase between two scenarios, monthly runoffs had medium rates (increasing in all months except October November), and daily runoff had the largest rates with the increase in flood peaks but decrease in drought flows, because of the variable influence on interception/evapotranspiration loss, percolation and antecedent soil water storage. Indicators of different time scales (annual runoff, monthly runoff, maximum 1-day and 5-day flood runoff, minimum 1-day and 7-day runoff) proved appropriate for analysing landuse change impacts. (C) 2015 Elsevier Ltd. All rights reserved.
机译:以前的研究主要集中在基于年度,季节或每月时间尺度的径流对土地利用变化的响应上,很少有基于每日尺度的研究。我们使用SWAT对日尺度,年尺度和月尺度的径流响应进行了全面调查,并定量比较了时间尺度与不同时间指标的影响。晋江是中国东南沿海湿润亚热带气候的集水区,被用于模拟。校准的SWAT模型在三个测量站的九年(2002-2010年)期间产生了令人满意的年,月和日径流过程的再现。然后使用相同的气象输入但使用两种不同的土地利用情景(1985年和2006年,森林减少,农田和城市化面积增加)对径流进行了模拟和比较。结果表明,径流在三个时标和三个流域之间变化不一。在两种情况下,年径流量增幅最小,月径流量呈中等速率(除11月以外的所有月份都呈上升趋势),而日径流量的最大值最大,洪水高峰增加而干旱流量减少,这是因为影响力可变截留/蒸散损失,渗滤和土壤水的前期储藏。事实证明,不同时间尺度的指标(年径流量,月径流量,最大1天和5天洪水径流量,最小1天和7天径流量)适用于分析土地利用变化的影响。 (C)2015 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Ecological indicators》 |2015年第11期|55-63|共9页
  • 作者单位

    Fujian Normal Univ, Inst Geog, Fuzhou 350007, Fujian, Peoples R China;

    Fujian Normal Univ, Inst Geog, Fuzhou 350007, Fujian, Peoples R China|Cultivat Base State Key Lab Humid Subtrop Mt Ecol, Fuzhou, Peoples R China;

    Dorset Environm Sci Ctr, Ontario Minist Environm & Climate Change, Dorset, ON P0A 1E0, Canada|Nipissing Univ, Dept Geog, North Bay, ON P1B 8L7, Canada;

    Fujian Normal Univ, Inst Geog, Fuzhou 350007, Fujian, Peoples R China;

    Fujian Normal Univ, Inst Geog, Fuzhou 350007, Fujian, Peoples R China;

    Fujian Normal Univ, Inst Geog, Fuzhou 350007, Fujian, Peoples R China;

    Nipissing Univ, Dept Geog, North Bay, ON P1B 8L7, Canada;

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

    Landuse change; Change in runoff; Flood indicator; Drought indicator; SWAT model; Jinjiang catchment;

    机译:土地利用变化径流变化洪水指标干旱指标SWAT模型晋江流域;

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