Assessing the effectiveness of “River Morphodynamic Corridors” for flood hazard mapping

IF 3.1 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL Geomorphology Pub Date : 2024-10-24 DOI:10.1016/j.geomorph.2024.109460
Andrea Brenna, Giacomo Poletto, Nicola Surian
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Abstract

In dynamic rivers the assessment of flood hazard related to geomorphological dynamics assumes crucial importance. Recently, some geomorphological approaches have been developed to assess channel dynamics in response to floods. In this study we explore the River Morphodynamic Corridors which include the current active channel and areas of the alluvial plain that may be (re)activated by channel dynamics during floods. In order to assess the effectiveness of such corridors for mapping flood hazard, we delineated the morphodynamic corridors along a river network of 74 km in the Cordevole River catchment (Italy) and compared the corridors with the channel changes that were triggered by a high-magnitude event (Vaia Storm) that hit the study area in October 2018. We observed that the morphodynamic corridors are capable to define areas where channel dynamics are most likely to occur and have proven satisfactorily effective in predicting channel widenings triggered by a severe flood. The results show that it is crucial to adopt different procedures for corridor delineation based on channel width, i.e., for small streams (width < 30 m) a more precautionary approach should be adopted that considers the entire alluvial plain as an area potentially affected by channel dynamics. The study highlighted an inherent limitation of the approach, since erosion that can affect valley slopes or fluvial terraces (i.e., widening of the alluvial plain) is not taken into account. This application represents the first validation of the River Morphodynamic Corridors approach through comparison with observed flood channel changes. Through this analysis, it can be inferred that, notwithstanding its relatively simple procedure, the approach allows a robust mapping and delineation of flood hazard due to river channel dynamics. The River Morphodynamic Corridors, when applied jointly with hydraulic model for assessing inundation processes, allow an overall assessment of flood hazard, particularly in dynamic river contexts.
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评估 "河流形态动力学走廊 "在绘制洪水灾害图方面的有效性
在动态河流中,与地貌动态相关的洪水灾害评估至关重要。最近,人们开发了一些地貌学方法来评估河道对洪水的响应动态。在这项研究中,我们探索了河流形态动力学走廊,其中包括当前的活动河道以及洪水期间可能因河道动力学而(重新)激活的冲积平原区域。为了评估此类走廊在绘制洪水灾害图方面的有效性,我们沿着科代沃勒河流域(意大利)74 公里的河网划定了形态动力学走廊,并将走廊与 2018 年 10 月袭击研究区域的高强度事件(维亚风暴)引发的河道变化进行了比较。我们观察到,形态动力学走廊能够确定最有可能发生河道动态变化的区域,并证明在预测严重洪水引发的河道拓宽方面效果令人满意。研究结果表明,根据河道宽度采用不同的程序来划定河道走廊是至关重要的,例如,对于小河流(宽度等于或小于 30 米),应采用更谨慎的方法,将整个冲积平原视为可能受河道动力学影响的区域。该研究强调了该方法的固有局限性,因为可能影响河谷斜坡或河流阶地的侵蚀(即冲积平原的拓宽)并未考虑在内。这项应用通过与观测到的洪水河道变化进行比较,首次验证了河流形态动力学走廊方法。通过分析可以推断出,尽管该方法的程序相对简单,但却可以对河道动态引起的洪水灾害进行可靠的绘图和划界。当河流形态动力学走廊与评估淹没过程的水力模型联合应用时,可以对洪水危害进行整体评估,尤其是在动态河流环境中。
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来源期刊
Geomorphology
Geomorphology 地学-地球科学综合
CiteScore
8.00
自引率
10.30%
发文量
309
审稿时长
3.4 months
期刊介绍: Our journal''s scope includes geomorphic themes of: tectonics and regional structure; glacial processes and landforms; fluvial sequences, Quaternary environmental change and dating; fluvial processes and landforms; mass movement, slopes and periglacial processes; hillslopes and soil erosion; weathering, karst and soils; aeolian processes and landforms, coastal dunes and arid environments; coastal and marine processes, estuaries and lakes; modelling, theoretical and quantitative geomorphology; DEM, GIS and remote sensing methods and applications; hazards, applied and planetary geomorphology; and volcanics.
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