利用无人机获取的地形数据,对屏障沉积物迁移进行半经验建模,以响应流体动力强迫(新泽西州霍尔盖特)

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL
W. John Schmelz, Ashlyn Spector, Lauren Neitzke-Adamo, Kenneth G. Miller
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引用次数: 0

摘要

从2020年10月到2021年5月,我们对新泽西州霍尔盖特的沿海地形进行了月度调查。利用无人机(UAV)摄影测量和RTK-GNSS设备,我们生成了数字高程模型和横截面剖面图,捕捉了体积变化的时空变化。通过这项研究,我们测量到总共损失了27500±10500立方米的地面沉积物。2020年10月至2021年2月,侵蚀沙量超过59 600±10 500 m3, 2021年2月至5月,侵蚀沙量为32 100±10 500 m3。我们建立了一个将测量到的地貌变化与波浪能和水位变化相关联的半经验模型。经过校准的模型确定了造成侵蚀的风暴条件,并且从南到东南的波浪比从东到东北的波浪造成的侵蚀更多。这些结果强调,沿岸输运是与海滩侵蚀相关的泥沙输运动力学的关键组成部分。利用校正后的模型,我们量化了水位变化和波浪能对一段屏障海岸线净沉积物输运的影响。具体而言,水位增加0.14 m(相当于1σ变化)产生的侵蚀量(1.18 m3/m / 48 h)略低于基于相同方差的波能增加(1.44 m3/m / 48 h)。这些变量强协变。沿岸运输调节了这种关系,随着沿岸波能的1σ位移,每48 h的侵蚀量增加0.9 m3/m。根据8年资料的后预报,强风暴的强迫作用每48小时可产生15-20立方米/米的侵蚀。这种建模方法代表了一种在预测风暴条件下产生潜在侵蚀估计的方法,这对海岸管理和恢复规划具有内在价值。我们的研究展示了具有成本效益的数据收集和强大的分析方法,可以在全球范围内应用,通过数据驱动的自然资源管理,有利于对沿海地貌和当地社区的理解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Semi-empirically modelling barrier sediment transport in response to hydrodynamic forcing using UAV-derived topographical data (Holgate, New Jersey)

Semi-empirically modelling barrier sediment transport in response to hydrodynamic forcing using UAV-derived topographical data (Holgate, New Jersey)

We conducted monthly surveys, from October 2020 to May 2021, of coastal topography in Holgate, New Jersey. Using unmanned aerial vehicle (UAV)-photogrammetry and RTK-GNSS equipment, we generated digital elevations models and cross-section profiles, capturing spatiotemporal variability in volumetric change. We measured a total loss of 27 500 ± 10 500 m3 of subaerial sediment through the study. From October 2020 to February 2021, over 59 600 ± 10 500 m3 of sediment was eroded, followed by 32 100 ± 10 500 m3 of deposition from February to May 2021. We developed a semi-empirical model correlating the measured geomorphological change to wave energy and water-level variations. The calibrated model identified storm conditions that caused erosion and that waves from the south to southeast caused more erosion than those from the east to northeast. These results emphasise that alongshore transport represents a critical component of sediment transport dynamics relevant to beach erosion. Using the calibrated model, we quantified the impact of water-level variations and wave energy on net sediment transport for a stretch of barrier coastline. Specifically, a water-level increase of 0.14 m (equivalent to a 1σ variation) generated slightly less erosion (1.18 m3/m per 48 h) than the same variance-based increase in wave energy, which generates 1.44 m3/m of erosion per 48 h. These variables strongly covary. Alongshore transport modulates the relationship, increasing erosion 0.9 m3/m per 48 h with a 1σ shift in wave energy directed alongshore. Forcing from strong storms, hindcast from 8 years of data, can produce 15–20 m3/m of erosion per 48 h. This modelling approach represents a methodology to produce estimates of potential erosion under predicted storm conditions, which is inherently valuable to coastal management and resilience planning. Our study demonstrates cost-effective data collection and robust analytical methods that can be applied globally to benefit both the understanding of coastal geomorphology and local communities through data-driven natural resource management.

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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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