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RAPID: 2018 Hurricane Season: Sedimentological and Morphological Characteristics of Hurricane Michael Induced Storm Deposits in Apalachicola Bay

RAPID: 2018 Hurricane Season: Sedimentological and Morphological Characteristics of Hurricane Michael Induced Storm Deposits in Apalachicola Bay
RAPID:2018 年飓风季节:迈克尔飓风引发的阿巴拉契科拉湾风暴沉积物的沉积学和形态特征
批准号:
1904055
负责人:
Ping Wang
金额:
$3.91万
依托单位:
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2018
资助国家:
美国
项目状态:
已结题
起止时间:
2018-12-15 至 2019-11-30

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中文摘要
翻译
2018 年 10 月,极强的飓风迈克尔袭击了佛罗里达州狭长地带,对海岸线造成了毁灭性的破坏。 记录这场破纪录的风暴对海滩等各种沿海环境造成的损害;沙丘;海湾;障壁岛屿;沼泽可以及时向沿海社区和资源管理者通报强烈热带风暴的危险和频率。更好地科学了解这些影响并提高公众对此类风暴影响的认识和了解对于灾害准备工作至关重要。这项研究涉及沿着佛罗里达海岸通常受微潮范围影响的区域收集样本并进行测量。沉积物和大型动物样本将通过岩芯收集,并沿着从佛罗里达州南部阿巴拉契科拉湾辐射到障壁群岛近海的两条横断面进行取样。将对样线的地下部分进行其他表征,以记录沙丘的形态变化以及名义上的地下和浅水下环境的海拔变化。为了记录地层记录中风暴沉积物的保存潜力,将对样线进行两次采样。暴风雨过后尽快进行一次,六个月后进行一次。这项研究的数据和结果,加上向更大的沿海社区传播该项目的结果,将帮助公众和机构评估与沿海地区相关的风险,了解强风暴对各种沿海环境的影响,从而更好地准备和了解这一重大自然灾害的恢复力。这项研究利用难得的机会,系统地记录了迈克尔飓风沿阿巴拉契科拉湾海岸产生的沉积记录。 表面沉积物和沉积物岩心是沿着两条横断面收集的,这两条横断面从障壁岛向海延伸到沿着流入阿巴拉契科拉湾的两条河流的沿海沼泽。 来自障壁岛、后障壁、海湾和沿海沼泽的沉积物核心将用于建立风暴沉积物的区域尺度特征。 将进行两次现场采样活动,第一次是在风暴影响后不久,第二次是在大约 6 个月后,目的是调查风暴沉积物的保存情况。 低能量(即微潮)环境(例如沿海沼泽和沿海湖泊或天坑)中的极端飓风沉积的风暴沉积物已被广泛用于重建古飓风记录,从而为气候和风暴强度如何随时间变化提供有价值的见解。此外,在面临往往会抹去这些记录的过程(例如生物扰动和侵蚀)时,通常会检查非常薄的风暴沉积物的保存情况。 由于现有地貌特征之上沉积物层的风暴沉积物构成了沿海沼泽海拔升高的主要机制,因此像迈克尔飓风这样的强风暴可能在应对海平面上升导致的沼泽和其他沿海环境淹没方面发挥着重要作用。该奖项反映了 NSF 的法定使命,并通过使用基金会的智力价值和更广泛的影响审查标准进行评估,被认为值得支持。
英文摘要
An extremely strong Hurricane Michael hit the Florida Panhandle in October 2018 and caused devastating destruction along the coastline. Documenting damage by this record-breaking storm in various coastal environments, such as beaches; dunes; bays; barrier islands; and marshes, in a timely fashion, can inform the coastal community and resource managers about the dangers and frequency of energetic tropical storms. A better scientific understanding of these impacts and raising public awareness and knowledge of such storm impacts plays a crucial role in hazard preparation. This research involves collecting samples and making measurements along an area of the Florida coast subject normally to microtidal ranges. Sediment and macrofaunal samples will be collected via cores and grab sampling along two transects radiating out of Apalachicola Bay in southern Florida and ending in the sea offshore of the barrier islands. Other characterization of subaerial parts of the transects will be carried out to document morphological changes in dunes and changes in elevation of nominally subaerial and shallow subaqueous environments. To document the preservation potential of storm deposits in the stratigraphic record, transects will be sampled twice. Once as soon as possible after the storm and once six months later. Data and findings from this study, in combination with dissemination of the results of the project to the greater coastal community, will help the public and institutions that assess risk associated with coastal areas, understand the impacts of strong storms on a wide variety of coastal environments resulting in better preparation and knowledge of resiliency for this significant natural hazard.This study takes advantage of the rare opportunity to systematically document the sedimentary record produced by Hurricane Michael along the Apalachicola Bay coast. Surface sediment and sediment cores are collected along two transects extending from seaward of the barrier islands to the coastal marshes along the two rivers that discharge into Apalachicola Bay. Sediment cores from the barrier islands, back-barrier, bay, and coastal marsh will be used to establish regional scale characteristics of storm deposits. Two field sampling campaigns will be conducted, with the first one shortly after the storm impact and the second one roughly 6 months later with the goals of investigating the preservation of the storm deposits. Storm deposits by extreme hurricanes in low-energy (i.e., microtidal) environments, e.g., coastal marsh and coastal lakes or sinkholes, have been broadly used to reconstruct paleo-hurricane records, thereby providing valuable insights to how climate and storm strength have changed with time. Furthermore, preservation of, often, very thin storm deposits in the face of processes that tend to erase these records (e.g., bioturbation and erosion) will be examined. Because storm deposits of layers of sediment on top of existing geomorphic features constitutes a major mechanism for coastal marshes to gain elevation, strong storms, like Hurricane Michael, likely play an important role in combating the drowning of marshes and other coastal environments due to sea-level rise.This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
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