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首页> 外文期刊>The Science of the Total Environment >Identifying how future climate and land use/cover changes impact streamflow in Xinanjiang Basin, East China
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Identifying how future climate and land use/cover changes impact streamflow in Xinanjiang Basin, East China

机译:确定未来气候和土地利用/覆盖变化如何影响中国东部新安江盆地的水流

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摘要

Climate and land use/cover changes are the main factors altering hydrological regimes. To understand the impacts of climate and land use/cover changes on streamflow within a specific catchment, it is essential to accurately quantify their changes given many possibilities. We propose an integrated framework to assess how individual and combined climate and land use/cover changes impact the streamflow of Xinanjiang Basin, in East China, in the future. Five bias-corrected and downscaled General Circulation Model (GCM) projections are used to indicate the inter-model uncertainties under three Representative Concentration Pathways (RCPs). Additionally, three land use/cover change scenarios representing a range of tradeoffs between ecological protection (EP) and urban development (UD) are projected by Cellular Automata - Markov (CA-Markov). The streamflow in 2021-2050 is then assessed using the calibrated Soil and Water Assessment Tool (SWAT) with 15 scenarios and 75 possibilities. Finally, the uncertainty and attribution of streamflow changes to climate and land use/ cover changes at monthly and annual scale are analyzed. Results show that while both land use/cover change alone and combined changes project an increase in streamflow, there is a disagreement on the direction of streamflow change under climate change alone. Future streamflow may undergo a more blurred boundary between the flood and non-flood seasons, potentially easing the operation stress of Xinanjiang Reservoir for water supply or hydropower generation. We find that the impacts of climate and land use/cover changes on monthly mean streamflow are sensitive to the impermeable area (IA).The impacts of climate change are stronger than those induced by land use/cover change under EP (i.e., lower IA); and land use/cover change has a greater impact in case of UD (i.e., higher IA). However, changes in annual mean streamflow are mainly driven by land use/cover change, and climate change may decrease the influence attributed to land use/cover change.
机译:气候和土地利用/覆盖变化是改变水文状况的主要因素。要了解气候和土地利用/覆盖变化对特定流域内溪流的影响,在有多种可能性的情况下,准确量化其变化至关重要。我们提出了一个综合框架,以评估未来气候变化和气候变化以及土地利用/覆盖的综合变化如何影响新安江盆地的径流。使用五个偏差校正和缩减的通用流通模型(GCM)预测来表示三种代表性浓度途径(RCP)下的模型间不确定性。此外,Cellular Automata-Markov(CA-Markov)预测了三种土地利用/覆盖变化方案,这些方案代表了生态保护(EP)与城市发展(UD)之间的权衡范围。然后,使用校准的土壤和水评估工具(SWAT)对2021-2050中的流量进行评估,并具有15种情况和75种可能性。最后,分析了流量变化对气候和土地利用/覆盖率月度和年度变化的不确定性和归因。结果表明,虽然仅土地利用/覆盖面积变化和综合变化都预示着径流量的增加,但仅在气候变化下,径流量变化的方向就存在分歧。未来的水流可能会在洪涝季节和非洪涝季节之间处于更加模糊的边界,从而可能缓解新安江水库用于供水或水力发电的运行压力。我们发现气候和土地利用/覆盖变化对月平均流量的影响对不透水区(IA)敏感。气候变化的影响要强于EP下土地利用/覆盖变化所引起的影响(即较低的IA );土地使用/覆被变化对土地使用变化的影响更大(即IA更高)。但是,年平均流量的变化主要是由土地利用/覆盖变化引起的,而气候变化可以减少归因于土地利用/覆盖变化的影响。

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  • 来源
    《The Science of the Total Environment》 |2020年第25期|136275.1-136275.13|共13页
  • 作者

  • 作者单位

    Institute of Hydrology and Water Resources Civil Engineering and Architecture Zhejiang University Hangzhou 310058 China;

    College of Water Conservancy and Hydropower Engineering Hohai University Nanjing 210098 China;

    Department of Water Management Faculty of Civil Engineering and Ceosciences Delft University of Technology Delft 2623CN the Netherlands;

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  • 原文格式 PDF
  • 正文语种 eng
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  • 关键词

    Multiple scenarios; Climate change; Land use/cover change; Streamflow response; Uncertainty; Attribution;

    机译:多种情况;气候变化;土地利用/覆盖变化;流量响应;不确定;归因;

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