Abstract:Relative sea-level (RSL) rise associated with decreased fluvial sediment discharge and increased hurricane activity have contributed to the high rate of shoreline retreat and threatened coastal ecosystems in Port Fourchon, Louisiana, USA. This study, based on QuickBird/drone images (2004–2019) and LIDAR data (1998–2013), analyzed the impacts of shoreline dynamics on mangroves (Avicennia germinans) and marshes before and after the initiation of a beach nourishment project in 2013. The coastal barrier and dune c… Show more
“…During the past 5 years, we have published a total of 12 studies using this method to monitor the mangroves and coastal sedimentary dynamics from South and North America in the light of climate change [4] , [5] , [8] , [10] , [11] , [12] , [13] , [14] , [15] , and this method has attracted interests from numerous scholars from across the globe. Thus, we believe this procedure can provide an effective way for post-disaster assessment and coastal landscape survey in a timely fashion.…”
Section: Discussionmentioning
confidence: 99%
“…To date, remote sensing is still the most common method of studying coastal landform dynamics [ 4 , 5 ]. This method is time-tested and relies on high resolution satellite imagery such as lidar and QuickBird.…”
“…During the past 5 years, we have published a total of 12 studies using this method to monitor the mangroves and coastal sedimentary dynamics from South and North America in the light of climate change [4] , [5] , [8] , [10] , [11] , [12] , [13] , [14] , [15] , and this method has attracted interests from numerous scholars from across the globe. Thus, we believe this procedure can provide an effective way for post-disaster assessment and coastal landscape survey in a timely fashion.…”
Section: Discussionmentioning
confidence: 99%
“…To date, remote sensing is still the most common method of studying coastal landform dynamics [ 4 , 5 ]. This method is time-tested and relies on high resolution satellite imagery such as lidar and QuickBird.…”
“…The breakwaters are part of a shoreline stabilization effort that has been discussed since at least 2001 (Hill and Belhadjali, 2005). The system was a collaboration between the National Oceanographic and Atmospheric Association (NOAA), the Louisiana Coastal Protection and Restoration Authority (CPRA), Louisiana Department of Wildlife and Fisheries (LDWF), and the National Marine Fisheries Service, with $34 million of funding secured from the Coastal Wetlands Planning, Protection and Restoration Act (CWPPRA) to construct a 6.4 km transect of emergent breakwaters along the RWR shoreline designed for Category 1 conditions (Jafari et al, 2020;Cohen et al, 2021;Reid, 2021). Funded as "ME-18," the multi-million-dollar project incorporated a Light Weight Aggregate Concrete (LWAC) breakwater system.…”
Section: Study Site: Rockefeller Wildlife Refugementioning
The Rockefeller Wildlife Refuge, located along the Chenier Plain in Southwest Louisiana, was the location of the sequential landfall of two major hurricanes in the 2020 hurricane season. To protect the rapidly retreating coastline along the Refuge, a system of breakwaters was constructed, which was partially completed by the 2020 hurricane season. Multi-institutional, multi-disciplinary rapid response deployments of wave gauges, piezometers, geotechnical measurements, vegetation sampling, and drone surveys were conducted before and after Hurricanes Laura and Delta along two transects in the Refuge; one protected by a breakwater system and one which was the natural, unprotected shoreline. Geomorphological changes were similar on both transects after Hurricane Laura, while after Delta there was higher inland sediment deposition on the natural shoreline. Floodwaters drained from the transect with breakwater protection more slowly than the natural shoreline, though topography profiles are similar, indicating a potential dampening or complex hydrodynamic interactions between the sediment—wetland—breakwater system. In addition, observations of a fluidized mud deposit in Rollover Bayou in the Refuge are presented and discussed in context of the maintenance of wetland elevation and stability in the sediment starved Chenier Plain.
“…In China, the extension of the port facilities disrupts sedimentation along the Yellow Sea coast [3]. A beach nourishment project in Louisiana (USA) had impacts on the dynamics of the shoreline made of mangroves and marshes [4]. In the Po River estuary, which is not a tide-dominated delta, the importance of episodic events such as heavy floods has been highlighted [5].…”
The Mont-Saint-Michel is known worldwide for its unique combination of the natural site and the Medieval abbey at the top of the rocky islet. But the Mont is also located within an estuarine complex, which is considerably silting up. For two decades, large-scale works were planned to prevent the Mont from being surrounded by the expanding salt meadows. The construction of a new dam over the Couesnon River, the digging of two new channels, and the destruction of the causeway were the main operations carried out between 2007 and 2015. The remote sensing approach is fully suitable for evaluating the real impact of the engineering project in both time and space, particularly the expected large-scale hydrosedimentary effects, for reestablishing the maritime landscape around the Mont. Sentinel-2 satellite data have been used for the period from 2015 to 2023. Aster data were used for the previous period covering 2000 to 2017. Aerial photographs and an ALOS scene have been also used. The remote sensing approach is based on time-series images. It allows identifying local or regional consequences and temporary or permanent effects. The migration of the different channels (especially for the new west and east Couesnon river courses) and the erosion-progradation balance of the vegetation through space and time are the main features to study. Between 2007 and 2023, the erosion of the salt meadows is significant to the south-west of the Mont (− 150 ha) but more limited to the south-east (− 65 ha). The erosion effect is limited to the immediate environment because the vegetation fringe of the uppermost tidal flat along the main dike is slightly increasing (+ 35 ha) to the west and to the east (+ 40 ha). During the same period, the sedimentation considerably increased to the north-east of the Bay, between the Bec d’Andaine, the Grouin du Sud and Tombelaine islet, which seems now facing the same silting-up problem. At this stage, the remote-sensing survey indicates mixed results for the engineering project.
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