2021 年 5 月和 2022 年 6 月的地中海流星雨

Pub Date : 2023-11-22 DOI:10.15233/gfz.2023.40.8
Mia Pupić Vurilj, Tina Brnas, Krešimir Ruić, J. Šepić, Marijana Balić
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引用次数: 0

摘要

地中海经常观测到气象海啸(即源自大气的类似海啸的波浪)。在单次事件中,破坏性洪水通常发生在一个地点或有限区域。然而,在 2021 年 5 月和 2022 年 6 月,强烈的流星海啸袭击了相距 500 公里的多个地中海地点。2021 年 5 月 24 日上午,一个流星海袭击了科西嘉岛(西地中海,法国)的博尼法西奥,同日下午,另一个流星海袭击了伊斯特岛(亚得里亚海,克罗地亚)的希罗卡湾,相距 500 公里。大约 13 个月后,即 2022 年 6 月 26 日,流星海袭击了梅诺卡岛(西班牙)的 Ciutadella,两天后又袭击了 400 公里外的 Bonifacio。对与这两次事件相关的海平面和大气压力数据、卫星图像以及天气状况进行了详细分析。现已证实,在地中海地区,当流星雨发生时,该地区上空会出现流星雨同步条件,其中最重要的条件是在动态或对流不稳定的大气层中蕴藏着一股强大的西南喷流。对三个海湾(Ciutadella、Bonifacio、Široka 海湾)中每个海湾的气象日变化潜力进行了研究,研究考虑了以下因素:(1) 海湾近海陆架的普鲁德曼共振潜力,(2) 海湾口的朝向,(3) 该地区气象日变化同步条件的频率。在陆架特征(宽度、深度、方位)、湾口方位和一般合流条件的分布有利于长海浪放大并向湾口传播的地点,发生的流星雨最强、最频繁。
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Mediterranean meteotsunamis of May 2021 and June 2022
Meteorological tsunamis (i.e., tsunami-like waves of atmospheric origin) are regularly observed in the Mediterranean Sea. During a single event, destructive flooding usually occurs in one location or limited area. However, in May 2021 and June 2022, strong meteotsunamis hit several Mediterranean locations up to 500 km apart. In the morning hours of the 24th of May 2021, a meteotsunami hit Bonifacio on the island of Corsica (western Mediterranean, France) and in the afternoon hours of the same day, another meteotsunami hit Široka Bay on the island of Ist (Adriatic Sea, Croatia), 500 km away. About 13 months later, on the 26th of June 2022, a meteotsunami hit Ciutadella on the island of Menorca (Spain) and two days later Bonifacio, 400 km away. Sea-level and atmospheric pressure data and satellite imagery, as well as synoptic conditions, associated with both events were analysed in detail. It has been confirmed that in the Mediterranean, meteotsunamis occur when meteotsunamigenic synoptic conditions prevail over the area, with a strong southwesterly jet stream embedded in dynamically or convectively unstable atmospheric layers standing out as the most important condition. The meteotsunamigenic potential of each of the three bays (Ciutadella, Bonifacio, Široka Bay) was investigated by considering: (1) the potential for Proudman resonance on the shelves offshore of the bays, (2) the orientation of the mouth of the bay and (3) the frequency of meteotsunamigenic synoptic conditions over the area. The strongest and most frequent meteotsunamis occur at locations where the shelf characteristics (width, depth, orientation), bay mouth orientation and distribution of general synoptic conditions, have characteristics that support the amplification of long-ocean waves and their propagation toward the bay mouth.
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