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Uncertainty assessments and hydrological implications of climate change in two adjacent agricultural catchments of a rapidly urbanizing watershed

机译:快速城市化流域两个相邻农业流域气候变化的不确定性评估和水文影响

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摘要

Lake Simcoe is the most important inland lake in Southern Ontario. The watershed is predominantly agricultural and under increasing pressure from urbanization, leading to changing runoff patterns in rivers draining to the lake. Uncertainties in rainfall-runoff modeling in tributary catchments of the Lake Simcoe Watershed (LSW) can be an order of magnitude larger than pristine watersheds, hampering water quality predictions arid export calculations. Here we conduct a robust assessment to constrain the uncertainty in hydrological simulations and projections in the LSW using two representative adjacent agricultural catchments. Downscaled CGCM 3 projections using Al B and A2 emission scenarios projected increases of 4 ℃ in air temperature and a 26% longer growing season. The fraction of precipitation falling as snow will decrease. Spring runoff is an important event in LSW but individual HBV best calibrated parameter sets under-predicted peak flows by up to 32%. Using an ensemble of behavioral parameter sets achieved credible representations of present day hydrology and constrained uncertainties in future projections. Parameter uncertainty analysis showed that the catchments differ in terms of their snow accumulation/melt and groundwater dynamics. Human activities exacerbate the differences in hydro-logical response. Model parameterization in one catchment could not generate credible hydrological simulations in the other. We cautioned against extrapolating results from monitored to ungauged catchments in managed watersheds like the LSW.
机译:西姆科湖是安大略省南部最重要的内陆湖。该分水岭主要是农业,受到城市化压力的增加,导致流向湖泊的河流径流格局发生变化。西姆科湖流域(LSW)支流汇流模型的不确定性可能比原始流域大一个数量级,从而影响了水质预测和出口计算。在这里,我们进行了可靠的评估,以使用两个相邻的有代表性的农业流域来限制LSW的水文模拟和预测中的不确定性。使用Al B和A2排放情景进行的CGCM 3缩减投影预测,气温升高4℃,生长季节延长26%。随着降雪量的减少,降水所占比例将下降。春季径流是LSW中的重要事件,但单个HBV最佳校准参数集的预测峰值流量低了多达32%。使用一组行为参数集可以实现对当今水文学的可靠表示,并可以在未来的预测中约束不确定性。参数不确定性分析表明,流域在积雪/融雪和地下水动力学方面存在差异。人类活动加剧了水文响应的差异。一个流域的模型参数化无法在另一个流域产生可靠的水文模拟。我们告诫不要在LSW之类的受管理流域中将监测到的流域的结果推算为未覆盖的流域。

著录项

  • 来源
    《Science of the total environment》 |2014年第1期|326-337|共12页
  • 作者单位

    Environmental and Life Sciences Graduate Program, Trent University, 1600 West Bank Drive, Peterborough, ON K9J 7B8, Canada,Department of Aquatic Sciences and Assessment, Swedish University of Agricultural Sciences, Uppsala, Sweden;

    Department of Aquatic Sciences and Assessment, Swedish University of Agricultural Sciences, Uppsala, Sweden,Environmental and Resource Studies, Trent University, 1600 West Bank Drive, Peterborough, ON K9J 7B8, Canada;

    Faculty of Environmental Studies, York University, 4700 Keele Street, Toronto, ON M3J 1P3, Canada;

    Environmental and Resource Studies, Trent University, 1600 West Bank Drive, Peterborough, ON K9J 7B8, Canada;

    Environmental and Resource Studies, Trent University, 1600 West Bank Drive, Peterborough, ON K9J 7B8, Canada;

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

    Statistical downscaling; Phenology; Climate change; Lake Simcoe; Hydrological change; Uncertainty analysis;

    机译:统计缩减;物候学气候变化;西姆科湖;水文变化;不确定度分析;

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