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Shoreline responses to storm impacts: North Norfolk coast, southern North Sea

机译:海岸线对风暴影响的反应:北诺福克海岸,北海南部

摘要

Recent phases of enhanced mid-latitude storminess (e.g. NW European winter of 2013 – 14) have led to a growingudawareness of the considerable impacts of storms on coastal landscapes and their communities. Using aerial photography,udbi-annual cross-shore profiles, detailed alongshore ground survey, and offshore/inshore wave buoy andudregional tide gauge datasets, this paper considers storm impacts on the barrier coastline of North Norfolk, UK.udFirstly, at Scolt Head Island, we show that the barrier dune crest has been progressively set back landwards sinceud2006 in three storm-related phases, with each shoreline translation being of the order of 5-8 m. However, a fourthudstorm produced no significant shoreline change, demonstrating that the threshold for morphological change is a function of the combined effects of still water level and wave height at the shore, the magnitude and duration ofudthese components, and the timing of their interaction. Secondly, we consider recovery times
机译:最近的中纬度暴风雨增强阶段(例如2013年14月14日欧洲西北冬季)使人们越来越意识到风暴对沿海景观及其社区的巨大影响。通过使用航空摄影, udbi年度跨岸剖面,详细的近岸地面调查以及近海/近海波浪浮标和 udregion潮汐仪数据集,本文考虑了风暴对英国北诺福克郡屏障海岸线的影响。斯科特黑德岛(Scolt Head Island),我们显示自2006年 ud以来,障碍沙丘波峰已逐渐向内倾斜,分为三个与风暴有关的阶段,每个海岸线平移为5-8 m。然而,第四次 udstorm没有产生明显的海岸线变化,表明形态变化的阈值是海岸静止水位和波高,这些分量的大小和持续时间以及他们的互动。其次,我们考虑恢复时间

著录项

  • 作者

    Brooks Susan; Spencer T.;

  • 作者单位
  • 年度 2016
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  • 原文格式 PDF
  • 正文语种 en
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