美属萨摩亚奥福岛礁盘上的极端低频海浪

IF 2.7 2区 生物学 Q1 MARINE & FRESHWATER BIOLOGY
Olivia M. Cheriton, Curt D. Storlazzi, Ferdinand K. J. Oberle, Kurt J. Rosenberger, Eric K. Brown
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引用次数: 0

摘要

美属萨摩亚奥福沿岸的南部边缘礁一直是珊瑚研究的重点,原因是礁石平地上存在超高温池,珊瑚在这里的海温升高的环境中茁壮成长。在这里,我们首次记录了在这个珊瑚礁平地上出现的异常大的低频(周期为 100 秒)海浪。在一次大的南向涌浪事件中,内礁平地上的低频波平均高度为 0.7 米,周期为 2-4 分钟,估计占总水位的 50%。观测到的一个低频波的波谷到波峰的垂直高度为 1.5 米,可能是在礁石平地上直接观测到的最大低频波。这些大的低频波可能被礁石共振放大,是洪水和侵蚀等沿海灾害的重要因素,也可能与珊瑚的健康和恢复力有关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Extreme low-frequency waves on the Ofu, American Samoa, reef flat

Extreme low-frequency waves on the Ofu, American Samoa, reef flat

The southern fringing reef along Ofu, American Samoa, has been a focus of coral research owing to the presence of super-heated pools on the reef flat, where corals thrive in elevated sea temperatures. Here, we present the first documentation of exceptionally large low-frequency (periods > 100 s) waves over this reef flat. During a large, southerly swell event, low-frequency waves on the inner reef flat had mean heights of 0.7 m and periods of 2–4 min and are estimated to have contributed up to 50% of the total water levels. One observed low-frequency wave had a trough-to-peak vertical height of 1.5 m, possibly representing the largest low-frequency wave ever directly observed on a reef flat. These large, low-frequency waves, which were likely amplified by reef resonance, are important factors in coastal hazards such as flooding and erosion and may also be relevant to coral health and resilience.

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来源期刊
Coral Reefs
Coral Reefs 生物-海洋与淡水生物学
CiteScore
6.80
自引率
11.40%
发文量
111
审稿时长
4-8 weeks
期刊介绍: Coral Reefs, the Journal of the International Coral Reef Society, presents multidisciplinary literature across the broad fields of reef studies, publishing analytical and theoretical papers on both modern and ancient reefs. These encourage the search for theories about reef structure and dynamics, and the use of experimentation, modeling, quantification and the applied sciences. Coverage includes such subject areas as population dynamics; community ecology of reef organisms; energy and nutrient flows; biogeochemical cycles; physiology of calcification; reef responses to natural and anthropogenic influences; stress markers in reef organisms; behavioural ecology; sedimentology; diagenesis; reef structure and morphology; evolutionary ecology of the reef biota; palaeoceanography of coral reefs and coral islands; reef management and its underlying disciplines; molecular biology and genetics of coral; aetiology of disease in reef-related organisms; reef responses to global change, and more.
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