首页> 外文会议>International Conference on Hydroinformatics 2004(HIC2004) vol.2; 20040621-24; Singapore(SG) >CLIMATE CHANGE IMPACTS AND FLOOD RISK ANALYSIS IN MACKENZIE RIVER BASIN: A MODELING BASED COMPARATIVE STUDY CONSIDERING AND NOT CONSIDERING TRENDS IN HYDROLOGIC VARIABLE
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CLIMATE CHANGE IMPACTS AND FLOOD RISK ANALYSIS IN MACKENZIE RIVER BASIN: A MODELING BASED COMPARATIVE STUDY CONSIDERING AND NOT CONSIDERING TRENDS IN HYDROLOGIC VARIABLE

机译:麦肯锡河流域的气候变化影响和洪灾风险分析:一种基于模型的比较研究,考虑或不考虑水文变量趋势

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An attempt has been taken here primarily to evaluate climate change impacts in a substantial as well as the principal portion (Liard River basin) within the Mackenzie River basin of North-West Canada and then to accomplish flood risk analysis for the same area. After selecting the representative stations for the basin and collecting data for 'extreme annual flow', trend analysis is accomplished to determine climate change effect on this hydrologic variable. The results showed that most of the stations didn't have any statistically significant trend, while only one station showed to have significant increasing trend and two stations showed significant decreasing trends in flow data with time. These outcomes tend to indicate that climate change might not have that much significant effect on 'extreme annual flow' in the basin. Then, Monte Carlo simulation is applied to perform risk analyses for the individual stations and for a set of combined data mainly for two options: without considering any trend in flow data, and considering significant trends in flow data. Risk has been evaluated for the 50 years return period flood and interpreted by a term 'Threshold Flood Flow' defined as the minimum 'extreme annual flow' required to cause flood in a particular year. Results from the individual stations proclaim that flood risk seems to be less in magnitude with decreasing trend and high in magnitude with increasing trend in data, both compared to the risk estimated in no trend case. Results from the combined data set seem to proclaim that flood risk is actually slightly decreasing in Mackenzie River basin day by day.
机译:在这里,我们主要尝试评估加拿大西北部Mackenzie流域内大部分和主要部分(Liard河流域)的气候变化影响,然后对同一地区进行洪水风险分析。在为流域选择了代表站并收集了“年度最大流量”数据之后,便完成了趋势分析,以确定气候变化对该水文变量的影响。结果表明,大多数站没有任何统计上的显着趋势,而只有一个站显示了显着的上升趋势,而两个站显示了随时间推移的显着下降趋势。这些结果倾向于表明气候变化可能对流域的“极端年流量”没有太大影响。然后,将蒙特卡罗模拟应用于单个站点和一组组合数据的风险分析,主要针对以下两个选项:不考虑流量数据的任何趋势,而考虑流量数据的重要趋势。已经评估了50年回归期洪水的风险,并用“阈值洪水流量”一词来解释,该术语被定义为在特定年份引发洪水的最低“年度最大流量”。各个站点的结果都表明,与没有趋势情况下估计的风险相比,随着趋势的下降,洪水风险的大小似乎较小,而随着数据趋势的增加,洪水风险似乎较大。综合数据集的结果似乎表明,Mackenzie流域的洪水风险实际上正在逐日降低。

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