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Keywords = Oluvil harbor

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21 pages, 15896 KiB  
Article
Analysis of Multi-Temporal Shoreline Changes Due to a Harbor Using Remote Sensing Data and GIS Techniques
by Sanjana Zoysa, Vindhya Basnayake, Jayanga T. Samarasinghe, Miyuru B. Gunathilake, Komali Kantamaneni, Nitin Muttil, Uttam Pawar and Upaka Rathnayake
Sustainability 2023, 15(9), 7651; https://doi.org/10.3390/su15097651 - 6 May 2023
Cited by 11 | Viewed by 4468
Abstract
Coastal landforms are continuously shaped by natural and human-induced forces, exacerbating the associated coastal hazards and risks. Changes in the shoreline are a critical concern for sustainable coastal zone management. However, a limited amount of research has been carried out on the coastal [...] Read more.
Coastal landforms are continuously shaped by natural and human-induced forces, exacerbating the associated coastal hazards and risks. Changes in the shoreline are a critical concern for sustainable coastal zone management. However, a limited amount of research has been carried out on the coastal belt of Sri Lanka. Thus, this study investigates the spatiotemporal evolution of the shoreline dynamics on the Oluvil coastline in the Ampara district in Sri Lanka for a two-decade period from 1991 to 2021, where the economically significant Oluvil Harbor exists by utilizing remote sensing and geographic information system (GIS) techniques. Shorelines for each year were delineated using Landsat 5 Thematic Mapper (TM), Landsat 7 Enhanced Thematic Mapper Plus (ETM+), and Landsat 8 Operational Land Imager images. The Normalized Difference Water Index (NDWI) was applied as a spectral value index approach to differentiate land masses from water bodies. Subsequently, the Digital Shoreline Analysis System (DSAS) tool was used to assess shoreline changes, including Shoreline Change Envelope (SCE), Net Shoreline Movement (NSM), End Point Rate (EPR), and Linear Regression Rate (LRR). The results reveal that the Oluvil coast has undergone both accretion and erosion over the years, primarily due to harbor construction. The highest SCE values were calculated within the Oluvil harbor region, reaching 523.8 m. The highest NSM ranges were recorded as −317.1 to −81.3 m in the Oluvil area and 156.3–317.5 m in the harbor and its closest point in the southern direction. The maximum rate of EPR was observed to range from 3 m/year to 10.7 m/year towards the south of the harbor, and from −10.7 m/year to −3.0 m/year towards the north of the harbor. The results of the LRR analysis revealed that the rates of erosion anomaly range from −3 m/year to −10 m/year towards the north of the harbor, while the beach advances at a rate of 3 m/year to 14.3 m/year towards the south of the harbor. The study area has undergone erosion of 40 ha and accretion of 84.44 ha. These findings can serve as valuable input data for sustainable coastal zone management along the Oluvil coast in Sri Lanka, safeguarding the coastal habitats by mitigating further anthropogenic vulnerabilities. Full article
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Figure 1
<p>Location map of the study area—Oluvil Harbor, Sri Lanka.</p>
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<p>Schematic diagram of methodological procedures.</p>
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<p>Extracted shorelines from Landsat satellite imageries (1991–2021).</p>
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<p>Spatial variation of Oluvil coastline trends: (<b>a</b>) For 1991–2000; (<b>b</b>) For 2000–2008; (<b>c</b>) For 2008–2021.</p>
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<p>Google Earth Pro Images used to study the periodic change of Oluvil Coastline from 2000–2021 (accessed on 30 December 2022).</p>
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<p>DSAS Statics of the Oluvil coast area: (<b>a</b>) For SCE; (<b>b</b>) For NSM; (<b>c</b>) For EPR; (<b>d</b>) For LRR.</p>
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<p>DSAS Statics of the Oluvil coast area: (<b>a</b>) For SCE; (<b>b</b>) For NSM; (<b>c</b>) For EPR; (<b>d</b>) For LRR.</p>
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<p>Eroded and accreted areas in the Oluvil coast during 2008–2021 (accessed on 30 December 2022).</p>
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<p>Eroded and accreted areas in the Oluvil coastline (accessed on 7 January 2023).</p>
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12 pages, 5217 KiB  
Article
Exploring the Ever-Changing Seashore Using Geoinformatics Technology
by Ibra Lebbe Mohamed Zahir, Buddhika Madurapperuma, Atham Lebbe Iyoob and Kafoor Nijamir
Earth 2021, 2(3), 544-555; https://doi.org/10.3390/earth2030032 - 28 Aug 2021
Cited by 2 | Viewed by 2712
Abstract
Detecting coastal morphodynamics is a crucial task for monitoring shoreline changes and coastal zone management. However, modern technology viz., Geoinformatics paves the way for long-term monitoring and observation with precise output. Therefore, this study aimed to produce explicit shoreline change maps and [...] Read more.
Detecting coastal morphodynamics is a crucial task for monitoring shoreline changes and coastal zone management. However, modern technology viz., Geoinformatics paves the way for long-term monitoring and observation with precise output. Therefore, this study aimed to produce explicit shoreline change maps and analyze the historical changes of the coastline at the east coast of the Ampara District in Sri Lanka. The histogram threshold method is used to extract data from satellite images. The time-series satellite images, acquired from 1987 to 2017, toposheet, and Google Earth historical images were compared having adjusted with the ground-truth to find the seashore changes in the study area. The histogram threshold method is used on band 5 (mid-infrared) for separating land from water pixels which means that the water pixel values were classified to one (1) and land pixel values to zero (0). The extracted shoreline vectors were associated with each other to determine the dynamics of changing shoreline of the study area. The Digital Shoreline Analysis System (DSAS) was used to find shoreline movements for each period of time. As a result, it was observed by the cross-section analysis within 100 m shoreline—seaward range along the study area—in which severe erosion has occurred northward of the Oluvil Harbor and anomalous accretion southward of the harbor because of the breakwaters constructed in the port entrance which hinder the long shore sediment transport along the study area. This situation has resulted in many ramifications to the coastal zone of the study area in socio-economic and environmental aspects in which the coastal protection mechanisms have not been well implemented to curb such issues. Full article
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Figure 1
<p>Study area between Nintavur and Addalaichchenai.</p>
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<p>Landsat images of false-color combination for 1987 and 2017 period at the east coast of the Ampara District in Sri Lanka. The coordinate system of the study area is WGS 84 UTM Zone 44 N.</p>
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<p>Satellite-derived shorelines northwards of the harbor.</p>
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<p>Profile of shoreline change vs. shoreline change envelope northwards of the harbor.</p>
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<p>Heavy sediments, i.e., coarse sand deposited in Nochchiyadi paddy land area in Nintavur: (<b>a</b>) area before coastal erosion, (<b>b</b>) area after coastal erosion (note that bank collapse ca. 1 m in height).</p>
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<p>Accretion and shoreline changes southwards of the harbor.</p>
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<p>Profile of shoreline change vs. shoreline change envelope in the south of the harbor.</p>
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<p>Morphological changes of the littoral zones of the east coast from 2009 to 2017. (Image pixel: 30 m × 30 m, positional accuracy: 39.7 m and RMSE: 0.4–171.6 m.). Note that the 2011 image is different from other images because the harbor construction work was in progress.</p>
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