Department of Physical Geography and Regional Geographic Analysis, University of Seville, Seville 41004, Spain; School of Geography and Environmental Sciences, Ulster University, Coleraine, BT5241SA, Northern Ireland, United Kingdom.
School of Geography and Environmental Sciences, Ulster University, Coleraine, BT5241SA, Northern Ireland, United Kingdom.
Sci Total Environ. 2018 Jul 15;630:287-301. doi: 10.1016/j.scitotenv.2018.02.188. Epub 2018 Feb 23.
Low frequency, high magnitude storm events can dramatically alter coastlines, helping to relocate large volumes of sediments and changing the configuration of landforms. Increases in the number of intense cyclones occurring in the Northern Hemisphere since the 1970s is evident with more northward tracking patterns developing. This brings added potential risk to coastal environments and infrastructure in northwest Europe and therefore understanding how these high-energy storms impact sandy coasts in particular is important for future management. This study highlights the evolution of Storm (formally Hurricane) Ophelia in October 2017 as it passed up and along the western seaboard of Ireland. The largest ever recorded Hurricane to form in the eastern Atlantic, we describe, using a range of environmental measurements and wave modelling, its track and intensity over its duration whilst over Ireland. The impact on a stretch of sandy coast in NW Ireland during Storm Ophelia, when the winds were at their peak, is examined using terrestrial laser scanning surveys pre- and post-storm to describe local changes of intertidal and dune edge dynamics. During maximum wind conditions (>35 knots) waves no >2m were recorded with an oblique to parallel orientation and coincident with medium to low tide (around 0.8m). Therefore, we demonstrate that anticipated widespread coastal erosion and damage may not always unfold as predicted. In fact, around 6000m of net erosion occurred along the 420m stretch of coastline with maximum differences in beach topographic changes of 0.8m. The majority of the sediment redistribution occurred within the intertidal and lower beach zone with some limited dune trimming in the southern section (10% of the total erosion). Asynchronous high water (tide levels), localised offshore winds as well as coastline orientation relative to the storm winds and waves plays a significant role in reducing coastal erosional impact.
低频、高强度的风暴事件可以极大地改变海岸线,帮助搬运大量沉积物并改变地貌形态。自 20 世纪 70 年代以来,北半球强气旋的数量增加,其向北追踪的模式也越来越明显。这给西北欧的沿海环境和基础设施带来了额外的潜在风险,因此了解这些高能风暴对沙质海岸的具体影响非常重要,这对未来的管理具有重要意义。本研究重点介绍了 2017 年 10 月风暴(前称飓风)奥菲莉亚的演变过程,它在爱尔兰西海岸北上和沿海岸线移动。这是东大西洋有记录以来最大的一次飓风,我们使用一系列环境测量和波浪模型来描述它在爱尔兰期间的轨迹和强度。当风暴奥菲莉亚的风力达到峰值时,对爱尔兰西北部一段沙质海岸的影响通过风暴前后的地面激光扫描调查进行了检查,以描述潮间带和沙丘边缘动态的局部变化。在最大风速(>35 节)下,记录到的波高不超过 2 米,波向为斜向或平行,与中低潮(约 0.8 米)一致。因此,我们证明,预期的广泛海岸侵蚀和破坏可能并不总是如预测的那样发生。事实上,在 420 米长的海岸线上,大约有 6000 米的净侵蚀发生,海滩地形变化的最大差异为 0.8 米。大部分泥沙再分配发生在潮间带和海滩下部区域,南部区域的沙丘略有修剪(占总侵蚀的 10%)。异步高潮(潮位)、局部海上风以及海岸线相对于风暴风和波浪的方向,在减少海岸侵蚀影响方面发挥了重要作用。