A little tsunami at Ras El-Bar, Nile Delta, Egypt; consequent to the 2023 Kahramanmaraş Turkey earthquakes

IF 4.3 3区 材料科学 Q1 ENGINEERING, ELECTRICAL & ELECTRONIC
Hesham M. El-Asmar , Mahmoud Sh. Felfla , Sameh B. El-Kafrawy , Ahmed Gaber , Doaa M. Naguib , Mohamed Bahgat , Hoda M. El Safty , Maysa M.N. Taha
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Abstract

From the 6th to 7th of February 2023, a storm surge struck Ras El-Bar, Nile Delta coast and attacked the resort facilities, with a wave height and velocity in deep water of 7.2 m and 12.7 m/sec respectively. The wind speed was 12.84 m/s, blowing from the NW and the WSW quadrants. This was an unwitnessed event revealed from the study of similar time interval from 1998 to 2022. Synchronizing with this event on the 6th of February 2023, was Kahramanmaraş Turkey Earthquakes. Consequently, the shoreline receded for about −30 m and with a drop in sea-level of about −40 cm. Furthermore, considerable changes in the beach morphology from a dissipative to a cuspate-related, intermediate tidal flat transverse bar with a rip profile. These are either related to the change in the morphodynamic or sedimentary budget, and resulting due to seawater scouring of bottom sediments for more than −30 cm. Two days preceding the Earthquakes an isostatic rise in sea-level (+20 cm) at the Turkish coast compared to the Mediterranean records, which is interpreted due to regional underwater seismic activities. The drop in the sea-surface height does not happen due to seawater outflow to the Atlantic Ocean. However, the sea-level regained its normal position because of the refill occurring from the Atlantic Ocean to the Mediterranean Sea. The pumice pieces, organic peat, and starfish distributed at Ras El-Bar coast, and thrown from the Northern Mediterranean indicate that the Egyptian coast was subjected to a little tsunami with average height of 14 cm. It is minimized due to enforced wave shifting from high pressure over Egypt to the low-pressure sinks.

埃及尼罗河三角洲 Ras El-Bar,2023 年土耳其 Kahramanmaraş 地震引发的小海啸
2023 年 2 月 6 日至 7 日,风暴潮袭击了尼罗河三角洲沿岸的 Ras El-Bar,并袭击了度假村设施,深水区的浪高和浪速分别为 7.2 米和 12.7 米/秒。风速为 12.84 米/秒,从西北和西南方向吹来。这是从 1998 年至 2022 年类似时间间隔的研究中发现的一次未经目击的事件。与 2023 年 2 月 6 日的地震同时发生的是土耳其卡赫拉曼马拉什地震。因此,海岸线后退了约 -30 米,海平面下降了约 -40 厘米。此外,海滩形态也发生了巨大变化,从耗散型变为与穴状相关的、中间潮汐平横向条带型。这些变化可能与形态动力学或沉积预算的变化有关,也可能是海水冲刷海底沉积物造成的,冲刷深度超过-30 厘米。地震前两天,土耳其海岸的海平面与地中海的记录相比出现了等静压上升(+20 厘米),这被解释为区域水下地震活动所致。海面高度的下降并不是由于海水流向大西洋。然而,由于大西洋向地中海的补给,海平面恢复了正常位置。分布在 Ras El-Bar 海岸的浮石碎片、有机泥炭和海星,以及从地中海北部抛出的海星表明,埃及海岸曾遭受过一次平均高度为 14 厘米的小海啸。由于海浪被迫从埃及上空的高压移向低压汇,海啸被减至最小。
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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CiteScore
7.20
自引率
4.30%
发文量
567
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