2020
DOI: 10.1016/j.rsma.2020.101167
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Assessing the shoreline dynamics of Hatiya Island of Meghna estuary in Bangladesh using multiband satellite imageries and hydro-meteorological data

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Cited by 29 publications
(11 citation statements)
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References 31 publications
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“…As a transitional zone between land and water, the coastal zone is one of the most dynamic and unstable geomorphic units in Bangladesh (Minar et al 2013;Brammer 2014). The coastal environment is governed by terrestrial and marine forces (Kabir et al 2020), and the coastal vulnerability of Bangladesh is largely controlled by the geomorphic processes of the GBM river basins (Islam et al 2015a, b). Also, the external forces, including water-logging, soil erosion, salinity intrusions, sea level rise, cyclone, storm surge, and tsunami, adversely affect the morphological settings of the coastal environment and negatively impact coastal area development activities (CZPo 2005; Barua et al 2010).…”
Section: Coastal Featuresmentioning
confidence: 99%
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“…As a transitional zone between land and water, the coastal zone is one of the most dynamic and unstable geomorphic units in Bangladesh (Minar et al 2013;Brammer 2014). The coastal environment is governed by terrestrial and marine forces (Kabir et al 2020), and the coastal vulnerability of Bangladesh is largely controlled by the geomorphic processes of the GBM river basins (Islam et al 2015a, b). Also, the external forces, including water-logging, soil erosion, salinity intrusions, sea level rise, cyclone, storm surge, and tsunami, adversely affect the morphological settings of the coastal environment and negatively impact coastal area development activities (CZPo 2005; Barua et al 2010).…”
Section: Coastal Featuresmentioning
confidence: 99%
“…The ununiformed sea level rise along the coast due to high sediment dispersal from the GBM river system makes the delta system more complex and vulnerable (Islam 2011;Rashid et al 2013;Sarwar 2013;Karan 2015). Nevertheless, the coastal geomorphology of Bangladesh is poorly understood, where most of the coastal geomorphic studies are restricted to shoreline shifting (Shibly and Takewaka 2012;Islam et al 2013;Kabir et al 2020), coastal erosion and accretion (Rahman 2012;Alam and Uddin 2013;Sarker et al 2013;Sarwar and Woodroffe 2013;Hussain et al 2014), and morphological studies (Islam et al 2015a, b;Miah et al 2020) at small scale. Hereafter, further research is obligatory considering the long-term changes in the sediment supply from the GBM basin, associating the coastal morphological changes and relative sea level rise throughout the Bangladesh coast, which is critical to protect about 35 million people therein (Ahmad 2019).…”
Section: Plain Land and Coastal Areasmentioning
confidence: 99%
“…Transects are only generated once there is a parallel construction of baseline and historical coastlines [27]. This research manually generated the baseline along the shoreline with various directions as coastline data is not continuous [28]. Transects were created after setting attributes for both coastlines and baseline.…”
Section: Coastline Change Analysis By Applying Dsasmentioning
confidence: 99%
“…Ngoài ra, với sự phát triển của GIS, những hạn chế trong xác định đường bờ và biến động của nó theo thời gian và không gian được khắc phục [18,19]. Các kết quả chiết tách thông tin từ công nghệ viễn thám có thể sử dụng trong môi trường GIS như là một giải pháp xây dựng cơ sở dữ liệu và phân tích biến động hiệu quả [20], đóng vai trò quan trọng trong việc hỗ trợ ra quyết định nhanh trên phạm vi rộng với giá thành thấp so với các phương pháp truyền thống [21].…”
Section: Mở đầUunclassified