2017-2021 年遥感图像中探测到的年度沿海大石移动及其与海洋风暴的关系(地中海塔兰托湾)

M. Delle Rose
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引用次数: 0

摘要

海岸巨石的陆向位移是海水泛滥和侵蚀过程的地貌特征。在这项研究中,利用无需集成专业软件的开放式资源,探索了分布在塔兰托湾(意大利,地中海)东海岸约 100 公里范围内的中型、粗型和超粗型巨石在 2017 年至 2021 年期间的年度移动情况。通过地貌实地调查,对从遥感图像中获得的巨石位移数据进行了验证和完善。主要结果如下(1) 发现巨石流动性存在较大的年际变化;(2) 2019 年 11 月 11-13 日横穿地中海的德特勒夫风暴被认为是造成大规模位移现象的原因;(3) 推断了驱动所调查的形态动力学过程的海洋气候条件。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Annual Coastal Boulder Mobility Detected in 2017–2021 Remote Sensing Imagery and Its Relation to Marine Storms (Gulf of Taranto, Mediterranean Sea)
Landward displacements of coastal boulders are geomorphological signatures of sea flooding and erosion processes. In this study, using open-access resources that do not require the integration of specialist software, the 2017 to 2021 annual mobility of medium, coarse, and very coarse boulders spread over about 100 km of the eastern coast of the Gulf of Taranto (Italy, Mediterranean Sea) was explored. The boulder displacement data obtained from remote sensing imagery were verified and refined by means of geomorphological field investigation. The main results are the following: (1) A large interannual variability in the boulder mobility was found; (2) storm Detlef, which crossed over the Mediterranean during 11–13 November 2019, was recognized as the cause of a massive displacement phenomenon; and (3) the marine weather conditions driving the investigated morphodynamic process were inferred.
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