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Hydrologic Model Could Improve River Simulation, Flood Prediction Capabilities

机译:水文模型可以改善河流模拟和洪水预报能力

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AHYDROLOGIC MODEL under development by researchers at the University of Texas at Austin and International Business Machines Corporation (IBM), of Armonk, New York, is reputed to be much faster and more stable than existing models used to simulate large river networks, raising the possibility of issuing flood warnings far earlier than is currently possible. By linking the model to weather and runoff data, the researchers also expect to be able to provide much more precise flood warnings along individual waterways, particularly in urban areas. In creating the model, its developers aimed to overcome a long-standing "chicken-and-egg problem" that has stymied efforts to model large river networks, says Ben Hodges, Ph.D., A.M.ASCE, an associate professor in the civil, architectural, and environmental engineering department at the University of Texas and a member of the research team developing the model. Modeling a river network requires a "huge amount of data," Hodges notes, but existing models are not fast enough to accommodate such amounts. For users and developers of models, the situation poses a dilemma, Hodges explains. "Why would we gather all that data if we don't have a model that's fast enough to use it?" he asks. "Conversely, why would we build a model fast enough to use [the data] when there's no data to run it?"
机译:德克萨斯大学奥斯汀分校和纽约州阿蒙克市国际商业机器公司(IBM)的研究人员正在开发的AHYDROLOGIC模型比现有的用于模拟大型河网的模型要快得多,更稳定,这增加了可能性发出洪水警报的时间远远超过了目前的可能性。通过将模型与天气和径流数据联系起来,研究人员还期望能够在单个水道(尤其是在城市地区)内提供更精确的洪水预警。该模型的开发者旨在克服长期存在的“鸡与蛋问题”,该问题已阻碍了大型河网建模的努力,民政学副教授本·霍奇斯(Ben Hodges)表示。德克萨斯大学建筑与环境工程系,以及开发该模型的研究小组成员。霍奇斯指出,对河流网络进行建模需要“大量数据”,但是现有模型的速度不足以容纳此类数据。对于模型的用户和开发人员来说,这种情况造成了两难选择。 “如果没有足够快的模型来使用它,为什么我们要收集所有这些数据?”他问。 “相反,当没有数据运行时,为什么我们要建立一个足够快的模型来使用[数据]呢?”

著录项

  • 来源
    《Civil Engineering》 |2011年第11期|p.38-39|共2页
  • 作者

    JAY LANDERS;

  • 作者单位
  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-18 00:07:01

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