首页> 外文期刊>Journal of Hydrology >The use of retro- and scenario-modeling to assess effects of 100+years river of engineering and land-cover change on Middle and Lower Mississippi River flood stages
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The use of retro- and scenario-modeling to assess effects of 100+years river of engineering and land-cover change on Middle and Lower Mississippi River flood stages

机译:使用追溯模型和情景模型来评估100多年的工程河和土地覆盖变化对密西西比河中下游洪水阶段的影响

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Since the 19th century, the Middle and Lower Mississippi River (MMR and LMR) have been intensively modified for flood protection and commercial navigation. In order to quantify the effects of levee expansion, channel modification, and land-cover change upon flood stages, we have developed 1-D unsteady-flow models of multiple historical reference conditions ("retro-models") for three large study reaches (225-315 km each): one along the MMR and two reaches along the LMR. For each reference condition, four 1-D unsteady-flow models were developed. These models include a calibrated model of actual conditions and three "scenario" models: (1) a model with levees of the next time step, (2) a model with the channel geometry of the next time step, and (3) a model with floodplain roughness (i.e., land cover) of the next time step. Comparison of the model for actual conditions and the scenario models provide a quantitative assessment of levee expansion, channel modification, and land-cover change on stage. Scenario modeling suggests that the majority (38-70%) of the changes in flood stage on the LMR and MMR study reaches can be attributed to changes in channel geometry and hydraulic roughness. Levees were the next largest contributor to changes in flood stage. For time steps with significant levee expansion, these structures increase stage up to 1.0 m. Observed changes in floodplain land cover were associated with little (or none) of the increase in flood stage. These result show changes in channel geometry and roughness related to river engineering tools employed for improving navigation and flood protection are the principal drivers of historic changes in flood stages along these investigated reaches.
机译:自19世纪以来,密西西比河中下游地区(MMR和LMR)进行了大规模修改,以用于防洪和商业航行。为了量化堤防扩建,河道改造和土地覆盖变化对洪水阶段的影响,我们针对三个大型研究范围(以下简称“模型”)开发了具有多个历史参考条件的一维非恒定流模型(“复古模型”)每条225-315公里):一条沿着MMR,两条沿着LMR。对于每个参考条件,开发了四个一维非恒定流模型。这些模型包括经过校准的实际情况模型和三个“方案”模型:(1)带有下一个时间步长的堤坝的模型;(2)带有下一个时间步长的通道几何的模型;以及(3)一个模型下一个步骤的洪泛区粗糙度(即土地覆盖)。通过比较实际情况模型和情景模型,可以定量评估堤防扩建,河道改造和现阶段的土地覆被变化。方案建模表明,LMR和MMR研究河段洪水阶段的大部分变化(38-70%)可归因于通道几何形状和水力粗糙度的变化。堤防是洪水阶段变化的第二大贡献者。对于大堤扩建的时间步长,这些结构将台阶增加到1.0 m。观察到的洪泛区土地覆盖变化与洪水阶段增加很少(或没有)相关。这些结果表明,与用于改善航行和防洪功能的河流工程工具有关的河道几何形状和粗糙度变化是这些调查河段洪水阶段历史变化的主要驱动力。

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