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Analysis of Low Impact Development Using Continuous Simulation Hydrologic Modeling

机译:使用连续仿真水文建模分析低影响开发

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Continuous simulation (CS) refers to the computational modeling of a physical system in which the model continuously tracks and accounts for system responses to changes over time. This branch of deterministic modeling is well suited to the study of complex systems with multiple interactive feedback mechanisms. There are a wide range of applications in fields that include medicine, engineering, space exploration, and defense. The use of CS in hydrologic analyses was first implemented in the United States in 1960, with the development of the Stanford watershed model under Dr. Ray Linsley at Stanford University. Hydrologic analysis using CS remained fairly uncommon outside of academia up to and beyond the advent of modern desktop computing and the age of big data. This has remained so due in part to the perception that the data needs are too large and the processing times are too extensive. Another barrier to a more broad use of this technique is perhaps the lack of guidance and documentation for using this technique within existing and well established modeling platforms such as the U.S. Army Corps of Engineers Hydrologic Engineering Center hydrologic modeling system (HEC-HMS) and the U.S. Environmental Protection Agency's storm water management model (SWMM). The application of CS in the hydrologic analysis of low impact development (LID) implementation in the urban and suburban watershed offers the ability to perform predictive analysis of system performance under both static and changing land use and watershed management strategies. It offers a tool to evaluate the potential influence of LID on the sources of hydromodification and pollutant loading. Applying statistical analyses to the output from CS provides the ability to assign probability to observed system responses. For instance, what effect does a particular watershed management or development activity have on the recurrence interval for the bank full flow within a receiving stream? This paper presents a brief introduction to CS, a discussion of the LID modeling capabilities of SWMM, an introduction to CS capabilities of SWMM, and a simple example of a CS simulation of LID.
机译:连续仿真(CS)是指物理系统的计算建模,其中模型连续跟踪和考虑系统响应随时间变化的变化。该确定性建模的该分支非常适合于具有多个交互式反馈机制的复杂系统的研究。包括医学,工程,空间探索和防御的领域中有广泛的应用。在1960年,在美国首次在美国实施了水文分析中的使用,随着斯坦福大学雷德林博士下的斯坦福流域模型的发展。在往返于超出现代桌面计算和大数据的年龄的学术界,使用CS的水文分析仍然相当罕见。这仍然是如此,部分是因为数据需求太大并且处理时间过于广泛。更广泛使用这种技术的另一个障碍可能缺乏在现有和建立的建立的建模平台中使用这种技术的指导和文档,例如美国陆军工程中心水文建模系统(HEC-HMS)和美国环境保护局的雨水管理模型(SWMM)。 CS在城市和郊区流域的低影响开发(盖子)实施中的水文分析中的应用提供了在静态和变化的土地利用和流域管理策略下对系统性能进行预测分析的能力。它提供了一种评估盖子对水力计和污染物载荷来源的潜在影响的工具。将统计分析应用于CS的输出提供了分配观察系统响应的概率的能力。例如,特定流域管理或开发活动对接收流内的银行全流程的复发间隔有什么影响?本文介绍了CS的简要介绍,讨论了SWMM的盖子建模能力,SWMM的CS能力介绍,以及盖子的CS仿真的简单示例。

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