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Patterns of coral damage associated with the 2004 Indian Ocean tsunami at Mu Ko Similan Marine National Park, Thailand

机译:泰国Mu Ko Similan海洋国家公园与2004年印度洋海啸相关的珊瑚破坏模式

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摘要

On 26 December 2004, a severe earthquake in Sumatra caused a series of tsunami waves to strike southwestern coastal areas of Thailand. In this study, we investigated the patterns of tsunami-related damage to coral reefs at Mu Ko Similan Marine National Park. The results showed that the percent of damaged corals ranged from 7.2% to 39.7% of the total live coral cover, and the intensity of the coral damage was high at depths deeper than 10 metres at most study sites. In addition, massive and tabulate coral forms were the most susceptible to tsunami damage. The surveys also revealed that a high degree of coral damage occurred where the reef slope gradually dropped away from the shoreline. Therefore, coral communities and coastal profiles can be major factors influencing the movement of the currents generated by the tsunami and consequently may affect the pattern of coral damage by the tsunami.
机译:2004年12月26日,苏门答腊岛发生了严重地震,泰国海啸袭击了泰国西南沿海地区。在这项研究中,我们调查了Mu Ko Similan海洋国家公园中与海啸有关的珊瑚礁破坏模式。结果表明,受损珊瑚的百分比范围为活珊瑚总覆盖率的7.2%至39.7%,并且在大多数研究地点中,深度超过10米的珊瑚的破坏强度都很高。此外,块状和片状珊瑚最容易遭受海啸破坏。调查还显示,在珊瑚礁坡度逐渐远离海岸线的地方发生了高度的珊瑚破坏。因此,珊瑚群落和沿海剖面可能是影响海啸产生的洋流运动的主要因素,因此可能影响海啸对珊瑚的破坏方式。

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