Mean Sea Level and Tides Variations at Alexandria, Egypt over 1906-2020

G. Dawod, H. Mohamed, Ghada Haggag
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引用次数: 1

Abstract

Sea Level Rise (SLR) is a vital outcome of the environmental global warming phenomenon. This paper aims to investigate the basic properties of tides in Alexandria, Egypt and to analyze SLR in Egypt over a long period to examine the differences in Egypt's vertical geodetic datum. The annual relative SLR at Alexandria between 1906 and 2020 was found to be 2.6 mm/year. Moreover, the relative SLR has been 3.1 mm/y for the last two decades, 2001-2020. It could be considered the most appropriate value to be taken into consideration in Egypt's coastal management activities. Carrying out additional investigations is suggested to investigate possible major variations of MSL in Egypt at other TG sites over both the Mediterranean and Red seas. Based on available data and accomplished results, it is recommended to regard Egypt's MSL datum as a semi-kinematic rather than a fixed one.
1906-2020年埃及亚历山大的平均海平面和潮汐变化
海平面上升(SLR)是环境全球变暖现象的重要结果。本文旨在研究埃及亚历山大港潮汐的基本特性,并分析埃及长时间的SLR,以检验埃及垂直大地基准的差异。从1906年到2020年,亚历山大的年相对单反为2.6 mm/年。此外,在2001-2020年的过去20年里,相对单反为3.1毫米/年。它可以被认为是埃及沿海管理活动中应考虑的最适当的价值。建议进行进一步调查,以调查埃及地中海和红海上其他TG站点的MSL可能的主要变化。根据现有数据和已完成的结果,建议将埃及的MSL基准视为半运动学而不是固定的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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