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首页> 外文期刊>Environmental Monitoring and Assessment >Hydrodynamic modelling of a flood-prone tidal river using the ID model MIKE HYDRO River: calibration and sensitivity analysis
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Hydrodynamic modelling of a flood-prone tidal river using the ID model MIKE HYDRO River: calibration and sensitivity analysis

机译:使用ID模型MIKE HYDRO River的易发潮汐河水动力模型:标定和敏感性分析

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Hydrodynamic modelling is a powerful tool to gain understanding of river conditions. However, as widely known, models vary in terms of how they respond to changes and uncertainty in their input parameters. A hydrodynamic river model (MIKE HYDRO River) was developed and calibrated for a flood-prone tidal river located in South East Queensland, Australia. The model was calibrated using Manning's roughness coefficient for the normal dry and flood periods. The model performance was assessed by comparing observed and simulated water level, and estimating performance indices. Results indicated a satisfactory agreement between the observed and simulated results. The hydrodynamic modelling results revealed that the calibrated Manning's roughness coefficient ranged between 0.011 and 0.013. The impacts of tidal variation at the river mouth and the river discharge from upstream are the major driving force for the hydrodynamic process. To investigate the impacts of the boundary conditions, a new sensitivity analysis approach, based on adding stochastic terms (random noise) to the time series of boundary conditions, was conducted. The main purpose of such new sensitivity analysis was to impose changes in magnitude and time of boundary conditions randomly, which is more similar to the real and natural water level variations compared to impose constant changes of water level. In this new approach, the possible number of variations in simulated results was separately evaluated for both downstream and upstream boundaries under 5%, 10%, and 15% perturbation. The sensitivity analysis results revealed that in the river under study, the middle parts of the river were shown to be more sensitive to downstream boundary condition as maximum water level variations can reach 8%, 12%, and 15% under 5%, 10%, and 15% changes in the downstream boundary, respectively. The outcomes of the present paper will benefit future modelling efforts through provision of a robust tool to enable prediction of water levels at ungauged points of the river under various scenarios of flooding and climate change for the purpose of city planning and decision-making.
机译:流体动力学建模是了解河流状况的强大工具。但是,众所周知,模型在如何响应输入参数的变化和不确定性方面会有所不同。针对位于澳大利亚昆士兰州东南部的洪水多发的潮汐河,开发并校准了水动力河模型(MIKE HYDRO河)。在正常的干旱和洪水时期,使用曼宁粗糙度系数对模型进行了校准。通过比较观察到的水位和模拟水位,并估算性能指标来评估模型性能。结果表明,观察到的结果与模拟结果令人满意。流体动力学建模结果表明,校准后的曼宁粗糙度系数在0.011至0.013之间。潮汐变化在河口的影响和上游的河流排放是水动力过程的主要驱动力。为了研究边界条件的影响,在边界条件的时间序列中添加了随机项(随机噪声)的基础上,进行了一种新的灵敏度分析方法。这种新的敏感性分析的主要目的是随机施加边界条件的大小和时间变化,与施加恒定水位变化相比,它更类似于真实和自然水位变化。在这种新方法中,分别针对5%,10%和15%扰动的下游边界和上游边界,分别评估了模拟结果中可能出现的变化数量。敏感性分析结果表明,在所研究的河流中,由于在5%,10%以下,最大水位变化可以达到8%,12%和15%,因此河中部地区对下游边界条件更加敏感。 ,并且下游边界的变化分别为15%。本文的结果将通过提供一个可靠的工具来使未来的建模工作受益,该工具可以在各种洪水和气候变化情况下预测河流未塞水点的水位,以进行城市规划和决策。

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