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Formation and adjustment of typhoon-impacted reef islands interpreted from remote imagery: Nadikdik Atoll, Marshall Islands

机译:从遥远的影像解读受台风影响的礁岛的形成和调整:马绍尔群岛纳迪克迪克环礁

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In 1905, a devastating typhoon hit Nadikdik Atoll (5°54' N and 172°09' E) in the southern Marshall Islands. Evidence suggests that large sections of reef islands on Nadikdik were overwashed and destroyed. Comparison of aerial photographs taken in 1945 and modern satellite imagery provides a unique record of the geomorphic adjustment of islands after the typhoon. Between 1945 and 2010 the vegetated area of islands on Nadikdik grew from 0.74 to 0.90 km~2. Observed changes to Nadikdik reef islands manifested through a range of styles and were largely accretionary. Of note, the formation of a new island was tracked from an embryonic deposit to a fully vegetated and stable island over a 61 year period. Similarly, a number of previously discrete islands have agglomerated and formed a single larger island. These changes were rapid and indicate that reef island formation can occur quickly. Evidence suggests that despite the typhoon occurring over a century ago the geomorphic adjustment of islands is still on-going.
机译:1905年,一场毁灭性的台风袭击了南部马绍尔群岛的纳迪克迪环礁(北纬5°54'和东经172°09')。有证据表明,纳迪克迪克岛上的大片礁岛被过度冲洗和破坏。将1945年拍摄的航空照片与现代卫星图像进行比较,可以提供台风发生后岛屿的地貌调整的独特记录。从1945年到2010年,纳迪克迪克群岛的植被面积从0.74公里增加到0.90公里〜2。观察到的纳迪克迪克礁岛的变化通过多种样式表现出来,并且在很大程度上是增生的。值得注意的是,在61年的时间里,新岛的形成已从胚胎沉积追踪到完全植被稳定的岛。类似地,许多先前离散的岛已经聚结并形成了一个较大的岛。这些变化很快,表明珊瑚礁岛的形成可以迅速发生。有证据表明,尽管台风已经发生了一个多世纪,但岛屿的地貌调整仍在进行中。

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