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Extreme events, intrinsic landforms and humankind: Post-tsunamiscenario along Nagore-Velankanni coast, Tamil Nadu, India

机译:极端事件,固有地貌和人类:印度泰米尔纳德邦纳戈尔-韦兰坎尼海岸沿海啸后的情景

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摘要

Extreme oceanographic episodes have regularly afflicted the east coast of India. Storm surges strike annually, devastating for a period of 24-36 h, and inducing a run-up of 9 m and inundations reaching 35 km. Comparatively, the December 2004 tsunami appeared after 63 years, lasted for 1 h and caused a run-up of 6.5 m, with flooding up to 0.8 km inland. Whereas storm surges devastate vast areas, the tsunami destroyed areas within 80 m from the dune. Major impacts are: erosion and breaching of dunes, destruction of shorefront dwellings, formation of inlets and new water bodies. Extreme events confirmed that sand dunes and dense forests possess an innate capacity of attenuating wave up-rush, evidenced respectively by negligible overwash, and by modest damage only to a narrow frontal casuarina strip of 10 m average width. Recurring storm surges are of greater societal concern than an occasional tsunami.
机译:极端的海洋事件经常困扰着印度东海岸。每年都有风暴潮袭击,破坏性持续24-36小时,并导致9m加速,洪水泛滥达35 km。相比之下,2004年12月的海啸历经63年,持续了1小时,并引发了6.5 m的加速,内陆洪水泛滥至0.8 km。尽管风暴潮席卷了广大地区,但海啸摧毁了距离沙丘80 m以内的地区。主要影响是:沙丘的侵蚀和破坏,沿岸民居的破坏,进水口的形成和新的水体。极端事件证实,沙丘和茂密的森林具有先天的减弱波涌的能力,这可以通过忽略不计的过冲和仅对平均宽度为10 m的狭窄额叶木麻黄带的适度破坏来证明。与偶尔的海啸相比,反复出现的风暴潮更引起社会关注。

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