首页> 外文期刊>Journal of great lakes research >Hydrodynamic and sediment-accommodation controls on headland-beach geomorphology evaluated by statistical methods, southern Lake Erie coast
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Hydrodynamic and sediment-accommodation controls on headland-beach geomorphology evaluated by statistical methods, southern Lake Erie coast

机译:伊利湖南部海岸通过统计方法评估的陆岬-海滩地貌的水动力和沉积物调节控制

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The wave- and erosion-dominated south-central Lake Erie coast is one of the most heavily human-modified shorelines of the Laurentian Great Lakes. Three prominent harbor breakwaters, installed in the early 1900s, have fragmented this sand-deprived littoral system, trapping bluff-derived sands and gravels to form harbor headland beaches. These depositional systems offer an unique opportunity to investigate littoral sedimentary dynamics from headland geomorphologic data, having served as sites of continued sand sequestration along an similar to 65 km stretch of coastline dominated by eroding coastal cliffs and bluffs. Former foreshore deposits are mapped in dip-orientation beneath modern backshore regions using ground-penetrating radar, documenting the nature of beach progradation. Chronologic control of landform succession is attained from delineated historic shoreline positions. Multiple regression analysis of established beach-growth metrics versus lake-level and ice-cover variances suggests high lake levels are more strongly associated with shoreline advance, counterintuitive to the idea that lake-level rise should promote accommodation creation. Beach-growth phases during elevated lake levels are thus likely facilitated by increased sediment influxes from sourcing bluffs, more susceptible to erosion when impacted more directly by wave action during high water levels. Ice cover plays a lesser, yet important role in headland evolution as both erosional and depositional mechanism while hard structure design dictates the overall bounds of beach form. Changes in decadal beach-progradation rates are associated with sectional changes in breakwater orientation, an intrinsic control on accommodation distribution along strike. Correlations between headland geomorphology and hydrologic regime provide insight into the coastal margin's littoral dynamics, difficult to assess directly. (C) 2017 International Association for Great Lakes Research. Published by Elsevier B.V. All rights reserved.
机译:以波浪和侵蚀为主的伊利湖中南部海岸是劳伦山脉五大湖中人为改造最多的海岸线之一。 1900年代初安装的三个著名的港口防波堤使这个被沙子剥夺的滨海系统破碎化,捕获了钝sand的沙子和砾石,形成了港口岬角海滩。这些沉积系统提供了一个独特的机会,可以从岬角地貌数据研究沿岸沉积动力学,这些沉积物一直是沿约65公里长的海岸线(以侵蚀着沿海悬崖和悬崖的土地为主)持续固沙的地点。使用探地雷达,将前滨沉积物以现代倾斜方向绘制在现代后海区域下方,记录了海滩扩张的性质。根据划定的历史海岸线位置,可以按时间顺序控制地貌演替。已建立的海滩增长指标与湖泊水位和冰盖变化之间的多元回归分析表明,湖泊高水位与海岸线的发展有更强的联系,这与湖泊水位的上升应促进住宿创造的想法背道而驰。因此,湖泊水位上升期间的海滩生长阶段可能是由于源水流造成的沉积物涌入量增加,当在高水位期间受到波浪作用的直接影响时,更容易受到侵蚀。由于侵蚀和沉积机制,冰盖在岬角演变中起着较小但重要的作用,而硬质结构设计决定了海滩形态的整体界限。年代际海滩进水速度的变化与防波堤方位的剖面变化有关,防波堤方位是沿罢工的住宿分布的内在控制。岬角地貌和水文状况之间的相关性提供了对沿海边缘沿海动态的洞察力,难以直接评估。 (C)2017年国际大湖研究协会。由Elsevier B.V.发布。保留所有权利。

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