Monitoring the sedimentary budget and dislocated boulders in western Greece – results since 2008

摘要

Abstract > Dislocated boulders are one sign of high‐energy wave impacts on coasts. These high‐energy impacts, caused by severe storms or tsunamis, can trigger initial cracking and transport of boulders. Monitoring of these boulders, as well as the associated coastal sites is important in distinguishing between gradual coastal processes and high‐energy events. Western Greece is a seismically active area, where tsunamis and high‐energetic storms might occur and such past events are documented by historic and geoscientific research, making it an ideal location for monitoring dislocated boulders. Since 2008, monitoring of eight different coastal sites in this region was conducted by terrestrial laser scanning and photogrammetric approaches, with low‐cost unmanned aerial vehicles. The re‐use of similar surveying points in following years, allowed highly accurate monitoring. Point clouds derived from these methods were evaluated for change detection by point cloud comparisons. The data were also used to establish accurate three‐dimensional models of dislocated boulders ( n ?=?70). The determined boulder volumes of these accurate three‐dimensional models were incorporated in wave transport equations and wave decay curves, and compared with monitoring results. A comprehensive overview of dislocated boulders in western Greece is presented. Three‐dimensional boulder reconstruction is compared to an approach which uses a tape‐based measuring of boulder axes, with the tape‐based measurement showing a mean overestimation of mass by 32%. Accurate monitoring over time by both methods, is achieved by using fixed networks of reference points. Changes for each site over time, detected by direct point cloud comparisons, are fit to the possible inundation calculated by wave decay curves based on computed minimum wave heights for boulder transport. Both storm and tsunami waves may have initiated movement from the cliff edge and further transport is also possible. However, boulders showed no further movement from their current position in the area for the time period of this study. </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><Abstract Type =“Main”XML：ID =“SED12723-ABS-AB-0001”XML：LANG =“EN”> <标题类型=“main”>抽象</ title> > 脱臼的巨石是海岸高能量波的影响的一个标志。由严重风暴或海啸引起的这些高能量影响，可以触发巨石的初始开裂和运输。监测这些巨石以及相关的沿海网站在区分渐变的沿海流程和高能量事件方面是重要的。希腊西部是一个地震活动区域，可能会发生海啸和高能量风暴，并通过历史和地球科学研究的这种过去的事件进行了记录，使其成为监控脱位巨石的理想地点。自2008年以来，通过陆地激光扫描和摄影测量方法进行了监测该地区的八个不同沿海网站，具有低成本的无人空中车辆。在多年来重复使用类似测量点，允许高度准确的监测。评估来自这些方法的点云进行通过点云比较来改变检测。数据还用于建立脱位巨石的准确三维模型（ n </ i> ？=？70）。确定这些精确的三维模型的确定的巨石体积纳入波传输方程和波衰减曲线，并与监测结果进行比较。展示了西希腊脱位巨石的全面概述。将三维巨石重建与采用基于胶带轴测量的方法进行比较，具有基于带基的测量，显示出质量的平均估高32％。通过使用固定的参考点来实现两种方法的准确监测，通过使用固定的参考点来实现。通过直接点云比较检测的每个站点的改变，通过直接点云比较检测，适应通过基于巨晶巨石传输的计算最小波高度的波衰减曲线计算的可能的淹没。风暴和海啸波可能已经开始从悬崖边缘开始，也可以进一步运输。然而，在本研究时间段的时间内，巨石没有从其当前位置的进一步运动。 </ p> </摘要> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-28547/'>《Sedimentology: Journal of the International Association of Sedimentologists》</a> <b style="margin: 0 2px;">|</b><span>2020年第3期</span><b style="margin: 0 2px;">|</b><span>共20页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/165.html" title="地质学">地质学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Beaches&option=203" rel="nofollow">Beaches;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=boulders&option=203" rel="nofollow">boulders;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=monitoring&option=203" rel="nofollow">monitoring;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=terrestrial laser scanning&option=203" rel="nofollow">terrestrial laser scanning;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=UAV&option=203" rel="nofollow">UAV;</a> </p> <div class="translation"> 机译：海滩;巨石;监测;陆地激光扫描;无人机; 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