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Understanding the 2011 Upper Missouri River Basin floods in the context of a changing climate

机译:了解气候变化背景下2011年上密苏里河流域洪水

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摘要

Study Region: Upper Missouri River Basin. Study Focus: The semi-arid Upper Missouri River Basin (UMRB) has experienced notable volatility in high and low streamflow extremes in recent decades, punctuated by the record 2011 flood. This study provides a new perspective into the relative importance of precipitation and antecedent moisture conditions in driving extreme streamflow. Ensemble streamflow simulations demonstrate that precipitation is largely the dominant driver for high streamflows. Applying the observed atmospheric forcing in 2011 with initial conditions of antecedent hydrologic conditions from 64 historic years consistently produces large streamflow events exceeding the 85th percentile of historical peak flows. This study attributes the individual roles of atmospheric conditions and antecedent soil moisture on extreme streamflow production. It uses a novel modeling framework that provides a greater understanding for the role that heterogeneity in basin-scale hydrologic features have in extreme streamflow generation. New hydrologic insights for the region: A detailed analysis of the record 2011 flood event shows that streamflow generated over the region’s easternmost sub-basin is acutely sensitive to antecedent moisture. Yet, the 2011 record streamflow cannot be explained by a single factor or as the result of long-term trends, with the basin responding to several independent factors; significantly high (p < 0.05) antecedent moisture and significant cold-season precipitation. Perhaps most importantly was the record-setting May precipitation, which limited the ability of ensemble streamflow simulations initialized on 1-March from reliably predicting the record June streamflows. The recent volatility of UMRB streamflow may be a harbinger of future decades based on our analysis of climate projections that indicate increased hydroclimate variability by the latter half of the 21st century. Keywords: Hydrologic modeling, Hydrologic extremes, Hydrologic sensitivity, Hydroclimatology
机译:研究区:上密苏里河流域。研究重点:半干旱上部密苏里河流域(UMRB)在近几十年来,近几十年来,在近几十年来的,在2011年洪水的纪录时突出了显着波动。本研究提供了一种新的视角,进入驾驶极端流流程中降水和前进水分条件的相对重要性。合奏流仿真表明,降水主要是高流出的主要驱动器。在2011年应用观察到的大气强制迫使初始条件从64个历史性年度始终生产超过85百分位的历史峰值流动的大型流流事件。本研究将大气条件和前一种土壤水分对极端流流量产生的个人作用。它使用了一种新颖的建模框架,为盆地水文特征中的异质性具有极端流流流的作用提供了更大的理解。该地区的新水文见解:对2011年洪水事件的详细分析表明,在该地区的东部底座上产生的流流对前进的水分敏锐。然而,2011年记录流流不能通过单一因素或作为长期趋势的结果来解释,盆地响应了几个独立因素;明显高(P <0.05)前一种水分和显着的寒冷季节沉淀。也许最重要的是记录设置可以降水,这限制了合奏流仿真的能力,从1-3月开始初始化,从可靠地预测记录六月的流式流。最近UMRB流出的波动可能是未来几十年的预兆,基于我们对气候预测的分析,表示21世纪下半叶的水准化变异性增加。关键词:水文建模,水文极端,水文敏感性,水加工学

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