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Examination of the Impact of Recent LaTex Hurricanes on Shelf Geomorphology

机译:近期乳胶飓风对货架地貌的影响

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摘要

Rapid response offshore field campaigns conducted immediately after recent large hurricanes to strike the northern Gulf Coast including Lili (2002), Ivan (2004), Katrina and Rita (2005), and Ike (2008) have been combined with monitoring data during the storms and pre-storm observational datasets to allow their shelf geomorphological impact to be assessed. The work of multiple investigators shows that, although there are unique aspects to each storm related to storm characteristics and the sedimentary character of the shelf section they traversed, several common sediment transport phenomenon can be recognized. Ebb surge transport associated with the seaward return of the storm surge has a major impact on the ultimate shelf depositional pattern observed after each event. Event layers tend to show a recognizable erosional-depositional couplet marked by a basal hiatal surface and normally graded bedding. Resuspension of sediments caused by currents above critical erosion stress occurring during storm maximum has been observed to take place in water depths up to 35-40 m (115-148 ft) in the northern Gulf. The presentation will also suggest a way forward in creating predictive-forecast models for coastal geomorphological changes caused by large tropical events.
机译:快速反应近海野外活动在近期大型飓风袭击北湾海岸,包括Lili(2002),Ivan(2004),Katrina和Rita(2005),而Ike(2008)已与风暴期间的监测数据相结合。预测预测观测数据集以允许其妥善评估其架子地貌影响。多个调查人员的工作表明,尽管对风暴特征的每个风暴有独特的方面以及他们穿过的货架部分的沉积特性,但是可以识别出几种常见的沉积物传输现象。与风暴浪涌的海背返回相关的EBB电涌运输对每次事件后观察到的最终货架沉积模式具有重大影响。事件层倾向于显示由基底腔体表面标记的可识别的侵蚀性沉积对联,通常是渐变的床上用品。已经观察到在暴风雨最大值期间发生的临界侵蚀压力的电流引起的沉积物重新悬浮在北墨西哥湾北部的水深在水深度达到35-40米(115-148英尺)。介绍还将建议在为大型热带事件引起的沿海地貌变革创造预测预测模型的前进方向。

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