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Satellite-derived shoreline detection at a high-energy meso-macrotidal beach

机译:高能量Meso-Macrotidal Beach的卫星衍生的海岸线检测

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摘要

Publicly available satellite imagery can now provide multi-decadal time series of shoreline data from local to global scale, enabling analysis of sandy beach shoreline variability across a spectrum of temporal scales. Such data can, however, be associated with large uncertainties, particularly for beaches experiencing a large tidal range (2 m) and energetic incident waves. We use a decade of bi-monthly topographic surveys at the high-energy meso-macrotidal beach of Truc Vert, southwest France, and concurrent wave and water-level hindcast to investigate the uncertainties associated with satellite-derived time series of the shoreline position. We show that consideration of the water level and wave runup elevation is critical for accurately estimating waterline po-sition and, in turn, shoreline position. At Truc Vert, including non-tidal water level residuals (e.g. wind-driven surge) and accounting for time-and elevation-varying beach slope for horizontal correction did not improve satellite-derived shoreline position. A new total water level threshold is proposed to maximize the number of us-able images while minimizing errors. Accounting for wave runup and the new water level threshold at Truc Vert, the number of usable satellite images is doubled and shoreline position errors are at least halved compared to previous work at this site. Using the 1984 & ndash;2019 reconstructed shoreline, we also show that the satellite-derived shoreline trends and interannual variability are in better agreement with field measurements. Although the approach proposed here needs to be tested on other sites in different tidal/wave forcing environments with different morphological and sediment characteristics, we anticipate that it will improve the temporal and spatial description of shoreline change on most surf tidal beaches where accurate continuous water level and wave hindcasts and/or observations are available.(c) 2021 Elsevier B.V. All rights reserved.
机译:公开可用的卫星图像现在可以提供从本地到全球规模的多码时间系列海岸线数据,从而在跨越时间尺度的频谱上实现了砂滩海岸线变异性。然而,这种数据可以与大的不确定性相关联,特别是对于经历大型潮汐范围(& 2米)和精力充沛的入射波的海滩。我们使用双月地形测量十年在特吕克韦尔的高能量细观macrotidal海滩,法国西南部和并发波和水位后报调查与卫星获得的时间序列的海岸线位置相关的不确定性。我们表明,考虑水位和波浪运行高程对于准确估算水线PO-SITITION,以及轮流定位,这是至关重要的。在Truc Vert,包括非潮汐水位残差(例如风力驱动的浪涌)和用于水平校正的时间和高度不同的海滩斜率的核算并未改善卫星衍生的海岸线位置。提出了新的总水位阈值,以最大限度地减少错误的误差的数量。在Truc Vert的波浪运行和新的水位阈值下,可用卫星图像的数量增加了一倍,并且与本网站上以前的工作相比,海岸线位置错误至少减半。使用1984年和Ndash; 2019年重建海岸线,我们还表明,卫星衍生的海岸线趋势和续际变异性与现场测量更好。尽管需要对不同的潮汐其他网站测试这里提出的方法/波迫使具有不同的形态和泥沙特点的环境,我们预计这将提高海岸线变化对大多数冲浪潮滩时空描述需要精确连续水位和波形和/或观察可获得。(c)2021 Elsevier BV保留所有权利。

著录项

  • 来源
    《Geomorphology》 |2021年第15期|107707.1-107707.13|共13页
  • 作者单位

    CNRS UMR EPOC Pessac France|Univ Bordeaux UMR EPOC Pessac France;

    Univ Plymouth Sch Biol & Marine Sci Coastal Proc Res Grp Plymouth Devon England;

    Univ Plymouth Sch Biol & Marine Sci Coastal Proc Res Grp Plymouth Devon England;

    Univ Plymouth Sch Biol & Marine Sci Coastal Proc Res Grp Plymouth Devon England;

    Univ Plymouth Sch Biol & Marine Sci Coastal Proc Res Grp Plymouth Devon England;

    CNRS UMR EPOC Pessac France|Univ Bordeaux UMR EPOC Pessac France;

    CNRS UMR EPOC Pessac France|Univ Bordeaux UMR EPOC Pessac France;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Shoreline change; Long-term trend; Satellite; Wave runup;

    机译:海岸线变化;长期趋势;卫星;波浪润滑;

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