首页> 外文期刊>Journal of the American Water Resources Association >MANAGING UNCERTAINTY IN RUNOFF ESTIMATION WITH THE U.S. ENVIRONMENTAL PROTECTION AGENCY NATIONAL STORMWATER CALCULATOR
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MANAGING UNCERTAINTY IN RUNOFF ESTIMATION WITH THE U.S. ENVIRONMENTAL PROTECTION AGENCY NATIONAL STORMWATER CALCULATOR

机译:使用美国环境保护署国家暴风雨计算器计算径流估算中的不确定性

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摘要

The U.S. Environmental Protection Agency National Stormwater Calculator (NSWC) simplifies the task of estimating runoff through a straightforward simulation process based on the EPA Stormwater Management Model. The NSWC accesses localized climate and soil hydrology data, and options to experiment with low-impact development (LID) features for parcels up to 5ha in size. We discuss how the NSWC treats the urban hydrologic cycle and focus on the estimation uncertainty in soil hydrology and its impact on runoff simulation by comparing field-measured soil hydrologic data from 12 cities to corresponding NSWC estimates in three case studies. The default NSWC hydraulic conductivity is 10.1mm/h, which underestimates conductivity measurements for New Orleans, Louisiana (95 +/- 27mm/h) and overestimates that for Omaha, Nebraska (3.0 +/- 1.0mm/h). Across all cities, the NSWC prediction, on average, underestimated hydraulic conductivity by 10.5mm/h compared to corresponding measured values. In evaluating how LID interact with soil hydrology and runoff response, we found direct hydrologic interaction with pre-existing soil shows high sensitivity in runoff prediction, whereas LID isolated from soils show less impact. Simulations with LID on higher permeability soils indicate that nearly all of pre-LID runoff is treated; while features interacting with less-permeable soils treat only 50%. We highlight the NSWC as a screening-level tool for site runoff dynamics and its suitability in stormwater management.
机译:美国环境保护局国家雨水计算器(NSWC)通过基于EPA雨水管理模型的直接模拟过程简化了估算径流的任务。 NSWC可以访问局部的气候和土壤水文学数据,还可以选择使用低影响力开发(LID)功能来测试最大5公顷的包裹。我们讨论了NSWC如何处理城市水文循环,并通过在三个案例研究中将来自12个城市的实地测得的土壤水文数据与相应的NSWC估计进行比较,着重​​于土壤水文学的估计不确定性及其对径流模拟的影响。 NSWC的默认水力传导率是10.1mm / h,这低估了路易斯安那州新奥尔良的传导率测量值(95 +/- 27mm / h),高估了内布拉斯加州的奥马哈(3.0 +/- 1.0mm / h)。在所有城市中,与相应的测量值相比,NSWC预测平均将水力传导率低估了10.5mm / h。在评估LID与土壤水文学和径流响应之间的相互作用时,我们发现与现有土壤的直接水文相互作用在径流预测中显示出很高的敏感性,而从土壤中分离出来的LID则显示出较小的影响。在高渗透性土壤上用LID进行的模拟表明,几乎所有LID之前的径流都得到了处理。与渗透性较差的土壤相互作用的特征仅处理50%。我们强调NSWC是用于站点径流动力学及其在雨水管理中的适用性的筛查级工具。

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