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Evaluation of Runoff Responses to Land Use Changes and Land Cover Changes in the Upper Huaihe River Basin, China

机译:淮河流域上游土地利用变化与土地覆盖变化的径流响应评价

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摘要

Runoff changes in response to land use and land cover changes in the Huaihe River were drastic in the last few decades and are poorly understood because results from those studies are often equivocal. Hitherto, the methodology to quantify the effects of land use and land cover changes on the runoff response has been mainly the paired catchment approach, which is a blackbox, and usually restricted to small headwater basins where a control can be established. A model-based change-detection approach is developed in this study as an alternative to paired catchment methods. This approach is particularly suited to evaluating effects of land use and land cover changes on the hydrologic response in large to mesoscale watersheds in which suitable control is not possible. The Xinanjiang model was used to evaluate the newly implemented approach in the Dapoling watershed (with an area of 1,640 km2) in the upper Huaihe river basin. Three schemes were used to examine changes in the data series: (1) Calibration for a period before (or after) changes and simulations of runoff that would have been observed without land use and land cover changes (reconstruction of runoff series); (2) comparison of calibrated parameter values for periods before and after the land use and land cover change; and (3) comparison of runoffs simulated with parameter sets calibrated for periods before and after the landcover change. The results show that, since 1976, the medium-coverage and high-coverage natural forest area has decreased, and the corresponding runoff has declined by nearly 25% from 1976 to 2005 attributable to the continuous expansion of tea gardens and human development. Model parameters, for example, the evapotranspiration coefficient KC, varied considerably from 0.64 to 0.94 attributable to the land use and land cover change within the watershed. This study demonstrates that the modeling approach may be a useful alternative to the paired watershed approach for examining land use and land cover changes and their impact on the runoff.
机译:在过去的几十年中,淮河的径流变化因土地利用和土地覆盖的变化而发生了剧烈变化,人们对它们的了解很少,因为这些研究的结果通常是模棱两可的。迄今为止,量化土地利用和土地覆盖变化对径流响应影响的方法主要是成对的集水区方法,这是一个黑箱,通常仅限于可以建立控制措施的小型水源流域。在这项研究中,开发了一种基于模型的变化检测方法,作为配对集水方法的替代方法。这种方法特别适合评估在无法进行适当控制的大型到中尺度流域的土地利用和土地覆盖变化对水文响应的影响。用新安江模型对淮河流域上游大坡岭流域(面积为1,640 km2)的新方法进行了评估。三种方案用于检验数据序列的变化:(1)在变化之前(或之后)进行一段时间的校准,以及在没有土地利用和土地覆被变化的情况下可以观察到的径流模拟(重建径流序列); (2)比较土地利用和土地覆盖变化前后的标定参数值; (3)用参数集模拟的径流的比较,这些参数集针对土地覆被变化前后进行了校准。结果表明,自1976年以来,由于茶园的不断扩大和人类的发展,中覆盖率和高覆盖率的天然林面积减少了,相应的径流量从1976年到2005年减少了近25%。模型参数,例如蒸散系数KC,在0.64到0.94之间变化很大,这归因于流域内的土地利用和土地覆盖变化。这项研究表明,建模方法可能是配对分水岭方法的有用替代方法,用于检查土地利用和土地覆被变化及其对径流的影响。

著录项

  • 来源
    《Journal of hydrologic engineering》 |2012年第7期|p.800-806|共7页
  • 作者单位

    State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai Univ., Nanjing,China 210098,Hohai Univ., Nanjing, China 210098;

    State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai Univ., Nanjing, China 210098,Hohai Univ., Nanjing, China 210098;

    State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai Univ., Nanjing, China 210098;

    State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai Univ., Nanjing, China 210098, Univ. of Nevada, Las Vegas 89154;

    Xinyang Hydrology and Water Resources Survey Bureau of Henan Province, Xinyang, China;

    Graduate Student, State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai Univ., Nanjing, China 210098, Nanjing,China 210098;

    600 E. University Ave., Apt 233, Las Vegas 89119;

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

    runoff response; change detection; xinanjiang model; dapoling basin;

    机译:径流响应;变更检测;新安江模式达泊灵盆地;

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