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Journal articles on the topic 'Sand spit morpho dynamic'

Author: Grafiati

Published: 7 July 2024

Last updated: 31 July 2025

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1

Sathish, S., R. S. Kankara, S. Chenthamil Selvan, M. Umamaheswari, and R. Arthur James. "Sedimentary Facies and Morpho-dynamics of Sand Spit and Island Inference as Coastal River Process." Journal of the Geological Society of India 99, no. 7 (2023): 951–64. http://dx.doi.org/10.1007/s12594-023-2416-8.

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2

Sapkale, J. B., M. M. Mane, N. K. Susware, and S. J. Sapkale. "Dynamic Changes in Coastal Geomorphology of Shiroda Coasts, using Remote Sensing and GIS: An Approach to Climate Change and Coastal Disaster Risk." Disaster Advances 16, no. 12 (2023): 20–32. http://dx.doi.org/10.25303/1612da020032.

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The coastline is a unique land feature formed through the interaction between land and sea. It is essential to monitor and detect hotspots and observe spatial and temporal influences of climate change in the coastal environment. Coastal landform changes can be best studied through remote sensing data. This study examines the dynamic changes in the sand spit and associated coastal area of the Shiroda coasts of Sindhudurg district. The Normalized Difference Water Index (NDWI) was used to distinguish land and water and the area was calculated by reclassifying the NDWI index of all images with two

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3

Georgiou, Ioannis Y., Francesca Messina, Md Mohiuddin Sakib, et al. "Hydrodynamics and Sediment-Transport Pathways along a Mixed-Energy Spit-Inlet System: A Modeling Study at Chincoteague Inlet (Virginia, USA)." Journal of Marine Science and Engineering 11, no. 5 (2023): 1075. http://dx.doi.org/10.3390/jmse11051075.

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Tidal-inlet systems are dynamic features that respond to short-term (e.g., storms) and longer-term processes (e.g., sea-level rise, changes in tidal prism). The Chincoteague Inlet system, located along the northern Eastern Shore of Virginia (USA), is a dynamic coastal complex that experiences rapid change associated with sediment redistribution and a shifting inlet throat due to the southern elongation of adjacent Assateague Island. In this study, a numerical model based on Delft3D with coupled flow–waves, multiclass sediment transport, and morphologic feedback was developed to quantify the hy

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4

Duc Anh, Nguyen Quang, Hitoshi Tanaka, Ho Sy Tam, Nguyen Xuan Tinh, Tran Thanh Tung, and Nguyen Trung Viet. "Comprehensive Study of the Sand Spit Evolution at Tidal Inlets in the Central Coast of Vietnam." Journal of Marine Science and Engineering 8, no. 9 (2020): 722. http://dx.doi.org/10.3390/jmse8090722.

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Tidal inlets along the central coast of Vietnam are located in a microtidal, wave-dominated coastal environment. In addition, the Vietnam coast is highly influenced by the seasonal monsoon regime, which is characterized by large northeast waves from October to March and calm southeast waves from April to September every year. Consequently, the tidal inlet entrance morphologies often suffer from a dynamic seasonal evolution due to distinct differences in the direction of wave-induced longshore sediment transport (LST) between the two monsoon seasons. The migration or closure of tidal inlets cau

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Escudero, Mireille, Gregorio Posada, Beatriz Edith Vega, and Edgar Mendoza. "MONITORING OF THE COASTAL DYNAMICS ON THE SAND SPIT AT TORTUGUEROS BEACH, MEXICO." Coastal Engineering Proceedings, no. 37 (September 1, 2023): 52. http://dx.doi.org/10.9753/icce.v37.management.52.

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Sand spits occur worldwide in different shapes, from a single, relatively simple arc to an irregular, crenulated, and complex barrier. Cross-shore and longshore sediment transport often influence spit dynamics (Nagarajan et al., 2015), strongly linked to wave energy and sediment supply. The present analysis focuses on a dynamic and complex spit at Tortugueros beach, a re-entrant bay, 1 km in length, on the Gulf of Mexico. Tortugueros beach is a wave-dominated beach with very fine to fine sand that forms a fairly gentle sloping beach profile. The sediment sources are longshore sediment transpor

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Nofridiansyah, Eko, Agus Hartoko, Max R. Muskananfola, and Muhammad Helmi. "Morpho-Dynamic Changes Based on Multitemporal Sentinel-2 Imagery in The Kungkai Baru Estuary, Bengkulu." IOP Conference Series: Earth and Environmental Science 1496, no. 1 (2025): 012022. https://doi.org/10.1088/1755-1315/1496/1/012022.

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Abstract Monitoring estuarine morpho-dynamics is critical to understanding interactions between freshwater and marine environments, especially in dynamic ecosystems like the Kungkai Baru Estuary. Seasonal closures of the estuary, lasting from two to six months, lead to notable ecological and geomorphological shifts, affecting sedimentation, water quality, and biodiversity. This study utilized multitemporal Sentinel-2 imagery to analyze morpho-dynamic changes in the estuary from 2019 to 2024. Three image processing techniques—Normalized Difference Water Index (NDWI) for water detection, supervi

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Karlonienė, Dovilė, Donatas Pupienis, Darius Jarmalavičius, Aira Dubikaltinienė, and Gintautas Žilinskas. "The Impact of Coastal Geodynamic Processes on the Distribution of Trace Metal Content in Sandy Beach Sediments, South-Eastern Baltic Sea Coast (Lithuania)." Applied Sciences 11, no. 3 (2021): 1106. http://dx.doi.org/10.3390/app11031106.

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Sandy coasts are one of the most dynamic spheres; continuously changing due to natural processes (severe weather and rising water levels) and human activities (coastal protection or port construction). Coastal geodynamic processes lead to beach sediment erosion or accumulation. The coast’s dynamic tendencies determine the changes in the volume of beach sediments; grain size; mineralogical; and geochemical composition of sediments. In addition to lithological and mineralogical analysis of sediments, geochemical analysis can provide valuable information about the local and regional patterns of s

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8

Nguyen, Minh Quang, Van Ha Vu, Thanh Tan Mai, et al. "Geomorphological sedimentary characteristics in the coastal area of Ma river delta, Thanh Hoa province." Tạp chí Khoa học và Công nghệ Biển 21, no. 3 (2021): 283–98. http://dx.doi.org/10.15625/1859-3097/15995.

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The coastal area of the Ma river delta is formed by the interaction of continental and marine processes, between neo-tectonic activities and exogenous processes, between natural factors and human activities during the Late Holocene. Using remote sensing and geoscience research methods (granulometry, paleontology, geochemistry, clay mineralogy) and geomorphological studies (geneses, morphology, dynamics) combined with field survey, this coastal area, except the denuded mountainous remnants, could be distinguished into 12 morpho-sedimentary units formed and developed by the dynamic interactions

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9

Wahyudi, Vierda Khairene Tiffany, Yeyes Mulyadi, et al. "Morpho-dynamic Induced Rip Currents in Klayar Beach, Pacitan, East Java, Indonesia." IOP Conference Series: Earth and Environmental Science 1298, no. 1 (2024): 012035. http://dx.doi.org/10.1088/1755-1315/1298/1/012035.

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Abstract Klayar Beach (KB), Pacitan, East Java, Indonesia is a rugged coast with a narrow sand beach, a relatively small embayment with rocky headlands, and a very exotic view as a coastal tourism destination. Despite its attractiveness, KB poses a hazard due to rip currents. From 2009 to 2022, KB visited more than 3 million people, and more than 30 people were reported dead due to drowning in rip currents. This paper presents the result of fieldwork to investigate morpho-dynamic driven rip current hazard of the study area. This study carried out bathymetric and topographic mapping and sedimen

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10

Kinsela, Michael, Chris Owers, Hannah Power, Tom Doyle, and David Hanslow. "MIGRATION AND WELDING OF AN ESTUARINE BARRIER-SPIT DRIVEN BY DELTA EVOLUTION AND STORMS." Coastal Engineering Proceedings, no. 37 (September 1, 2023): 75. http://dx.doi.org/10.9753/icce.v37.sediment.75.

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As sea levels rise globally in response to anthropogenic climate change, coastal depositional systems that persist in dynamic equilibrium with accommodation space, sediment supply and hydrodynamic processes may begin to respond by redistributing sediment, causing erosion or migration of landforms that may have appeared as stable over previous decades to centuries. In contrast, systems that have adjusted to inherited or changing boundary conditions over historical times offer insights on the modes and timescales of potential future change in remobilised coastal systems. We investigate the coupl

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11

Hakim, Erwin Hilman, Darsiharjo Darsiharjo, Ahmad Yani, and Nandi Nandi. "ANALISIS PERKEMBANGAN BENTUKLAHAN MARINE TERAPANNYA UNTUK PENGELOLAAN LINGKUNGAN WILAYAH PESISIR DI KABUPATEN PANGANDARAN." GEOGRAPHY : Jurnal Kajian, Penelitian dan Pengembangan Pendidikan 13, no. 1 (2025): 1. https://doi.org/10.31764/geography.v13i1.20892.

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Abstrak: Wilayah kepesisiran selatan Jawa Barat memiliki kondisi geologi dan geomorfologi serta aktivitas masyarakat yang kompleks, terlihat dari beragamnya jenis batuan, dan bentuk lahan marine seperti: cliff, tombolo, notch, spit, estuari, stump, stack, coastal dune, pasir putih berasosiasi Reeffrom. Tujuan penelitian menganalisis terhadap perubahan bentuk lahan marine relatif dinamis yang bersifat abrasi maupun akresi, analisis tersebut dapat dijadikan sebagai bahan rujukan atau referensi terhadap pengelolaan dan pemanfaatan wilayah pesisir di Kabupaten Pangandaran. Metode yang digunakan un

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12

Xiao, Heng, Yin Lu Young, and Jean H. Prévost. "Hydro- and morpho-dynamic modeling of breaking solitary waves over a fine sand beach. Part II: Numerical simulation." Marine Geology 269, no. 3-4 (2010): 119–31. http://dx.doi.org/10.1016/j.margeo.2009.12.008.

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13

Young, Yin Lu, Heng Xiao, and Timothy Maddux. "Hydro- and morpho-dynamic modeling of breaking solitary waves over a fine sand beach. Part I: Experimental study." Marine Geology 269, no. 3-4 (2010): 107–18. http://dx.doi.org/10.1016/j.margeo.2009.12.009.

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14

Albada, Edward, Elisabeth Mondon, and Richard Hinds. "APPLICATION OF HISTORICAL DATA FROM SATELLITE IMAGERY TO IMPROVE UNDERSTANDING OF COMPLEX NEARSHORE DYNAMICS." Coastal Engineering Proceedings, no. 37 (October 2, 2023): 149. http://dx.doi.org/10.9753/icce.v37.management.149.

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Collection of nearshore data such as bathymetry and benthic surveys are a requirement to all coastal projects. Typically, surveys are conducted in advance of a modelling exercise so as to replicate in-situ and existing conditions. These surveys only show one snapshot in time and as such do not represent conditions that are out of equilibrium from either seasonal or long-term changes. In these locations, an assessment of a timeseries of surveys would benefit the understanding of nearshore coastal dynamics. However, timeseries of nearshore data are seldom available. Traditional coastal survey te

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15

Larsen, B., and L. T. Andersen. "Late Quaternary stratigraphy and morphogenesis in the Danish eastern North Sea and its relation to onshore geology." Netherlands Journal of Geosciences 84, no. 2 (2005): 113–28. http://dx.doi.org/10.1017/s0016774600023003.

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AbstractGeological structures and Late Quaternary stratigraphy of the shallow subsurface along the southernmost Danish North Sea coast have been investigated using seismic data and shallow boreholes. A large-scale glaciotectonic thrust complex has been mapped in an area of 15 km by 40 km in the Fanø Bugt area. The affected succession consists of Neogene and Quaternary sediments deformed down to a depth of 200 – 360 m. A kineto-stratigraphic correlation to onshore glaciotectonic deformation suggests that the deformation took place during a westward advance stage of the Late Saalian (Warthe) gla

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16

Mane, Madhuri M., Shivam J. Sapkale, Nilesh K. Susware, and Jagdish B. Sapkale. "Comparative Study of the Coastal Geomorphology of Kajirbhati Sand-Spit Using Google Earth Pro Images (2005, 2011, 2023) and Landsat Satellite Data (2009, 2016, 2023): An Approach Towards the Impact of the Casuarina Plantation." Current World Environment 19, no. 2 (2024): 902–14. http://dx.doi.org/10.12944/cwe.19.2.30.

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Coastal geomorphology undergoes constant transformation due to a combination of coastal and fluvial processes and human intervention. Remote sensing and GIS tools are invaluable in identifying and studying these changes. Due to the dynamic interaction between land and sea, the coastline requires careful monitoring to detect hotspots and understand the spatial and temporal impacts of climate change on the coastal environment. Remote sensing data offers a comprehensive means of studying coastal landform changes. In a recent study, the focus was to analyze the impact of the Casuarina plantation o

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17

Lieou, Chinh, Serge Jolicoeur, Thomas Guyondet, Stéphane O’Carroll, and Tri Nguyen-Quang. "Hydrodynamic Modeling of Water Renewal Time and Potential Dissolved Matter Using TELEMAC: Applications to Shediac Bay (New Brunswick, Canada)." Journal of Marine Science and Engineering 12, no. 3 (2024): 461. http://dx.doi.org/10.3390/jmse12030461.

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This study examines the hydrodynamic regimes in Shediac Bay, located in New Brunswick, Canada, with a focus on the breach in the Grande-Digue sand spit. The breach, which was developed in the mid-1980s, has raised concerns about its potential impacts on water renewal time and water quality in the inner bay. The aims of this study, using mathematical modeling approaches, were to evaluate the flow regimes passing through the breach and influences on the distribution of dissolved matter, providing insights into whether the breach should be allowed to naturally evolve or be artificially infilled t

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18

Bollaert, Erik, Vincent Mano, Rafael Duarte, and Martin Jaeggi. "Numerical and physical modelling of future Rhône Delta (Switzerland)." La Houille Blanche, no. 2 (April 2018): 76–83. http://dx.doi.org/10.1051/lhb/2018021.

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The Rhône River on its Swiss course flows through the Lake of Geneva before traversing Geneva and continuing towards France. The river is entirely canalized upstream of the Lake of Geneva, over a length of about 160 km. Hence, a large river restoration project, the Third Rhône River Correction, is being planned for the upcoming 20-30 years. One of the first works to be realized will be the restoration of a delta estuary of the Rhône River into the lake. This delta will propose morphological diversity over a length of about 1.5 km, for a width of about 0.8 km, and will consist of a terrestrial

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19

Sarr, Mamadou Adama, Ibrahima Pouye, Aissatou Sene, et al. "Monitoring and Forecasting of Coastal Erosion in the Context of Climate Change in Saint Louis (Senegal)." Geographies 4, no. 2 (2024): 287–303. http://dx.doi.org/10.3390/geographies4020017.

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Owing to its unique physical and socio-economic characteristics, the Saint Louis region stands out as one of the most susceptible areas in Senegal to the adverse impacts of coastal erosion. The dynamics of erosion in this region are significantly influenced by the Langue de Barbarie (LB), a sand spit formed at the mouth of the Senegal River. Initially, in 2003, a 4 m wide artificial breach was strategically introduced to mitigate flooding; however, sediment dynamics expanded it to 6 km by 2020, thereby affecting the entire region. This study delves into the coastline change of the LB, specific

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20

Shampa, Binata Roy, Md Manjurul Hussain, A. K. M. Saiful Islam, Md Ashiqur Rahman, and Khaled Mohammed. "Assessment of Flood Hazard in Climatic Extreme Considering Fluvio-Morphic Responses of the Contributing River: Indications from the Brahmaputra-Jamuna’s Braided-Plain." GeoHazards 3, no. 4 (2022): 465–91. http://dx.doi.org/10.3390/geohazards3040024.

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Climate change is expected to raise river discharge and sea level in the future, and these near-term changes could alter the river flow regime and sedimentation pattern of future floods. Present hazard assessment studies have limitations in considering such morpho-dynamic responses in evaluating flood hazards or risks. Here, we present a multi-model-based approach to quantify such potential hazard parameters influenced by climate change for the most vulnerable communities living on river bars and islands of the Brahmaputra–Jamuna River. River flood-flow and flood wave propagation characteristi

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21

Bezzi, Annelore, Giulia Casagrande, Saverio Fracaros, et al. "Geomorphological Changes of a Migrating Sandbank: Multidecadal Analysis as a Tool for Managing Conflicts in Coastal Use." Water 13, no. 23 (2021): 3416. http://dx.doi.org/10.3390/w13233416.

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While beach erosion and sand loss are typically of great concern to the tourism industry, managing rapid morphological changes linked to large amounts of moving sediments is the challenge facing Grado, an important seaside resort in the northern Adriatic, Italy. The cause of the unusual management conflict is the presence of the Mula di Muggia Bank, a nearshore depositional system made up of relict and active migrating sandbanks extending up to 2 km seawards from the touristic beachfront. A reconstruction of the morpho-sedimentary evolution of the coastal system over a 200-year period was done

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22

Chapapría, Vicent Esteban, and José Serra Peris. "Vulnerability of Coastal Areas Due to Infrastructure: The Case of Valencia Port (Spain)." Land 10, no. 12 (2021): 1344. http://dx.doi.org/10.3390/land10121344.

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The vulnerability of coastal areas is related to the existence and functionality of infrastructure. Ports have had increased activity in the last few decades due to growing needs of the market. At the same time, there have been huge changes in maritime traffic, and some ports are specialized in container traffic. The port in Valencia developed notably in the last expansions, in the 1980s and in the recent northern expansion. Valencia’s port specializes in container traffic, and has become a Mediterranean leader and the metropolitan area is an important logistics center. Ports can create coasta

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23

Kumbhakarna Mallik and Krishna Pada Bauri. "Environmental aspects and their effects on blackish water lagoon management and ecosystem sustainability: A case study of Chilika Lagoon, India." World Journal of Advanced Research and Reviews 26, no. 3 (2025): 764–77. https://doi.org/10.30574/wjarr.2025.26.3.2215.

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The geomorphology, hydrodynamics, and ecological balance of blackish water lagoons are significantly shaped by environmental factors like wave action, tidal currents, longshore drift, and relative sea level rise. These factors also have a direct impact on the management and long-term sustainability of these lagoons. This study looks at shoreline dynamics and related environmental effects in the Chilika Lagoon in India as a representative case. Natural episodic events like waves, tides, currents, and global sea level rise are all responsible for the Chilika Lagoon's dynamic coastal environment'

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24

Žaromskis, Rimas, and Saulius Gulbinskas. "Reflection of the Baltic Sea Lithuanian nearshore bottom peculiarities in the historical maps." Geologija. Geografija 1, no. 4 (2016). http://dx.doi.org/10.6001/geol-geogr.v1i4.3243.

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Using the bathymetry information available from historical maps, the underwater slope of the Baltic Sea in the Lithuanian area of the shore is analysed south and north of the Klaipėda harbour. For this purpose, the old depth measurements have been converted into the metric system and cross profiles of the nearshore drawn, as well as, on this basis, the diagrams for the 3, 5, 7 and 10 m depth points have been constructed. The depth data from the maps compiled in 1743, 1855, 1875 and 1913 have been analysed. These periods correspond to specific conditions of the shore zone morpho- and litho-dyna

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25

Fick, Cristiano, Julia Favoreto, Leonardo Borghi, et al. "Sedimentological and biofabric patterns for hybrid coquina deposits: Insights from wave tank experiments." Sedimentology, July 2, 2025. https://doi.org/10.1111/sed.70028.

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ABSTRACTHybrid bioclastic/siliciclastic coquinas are sedimentary accumulations typical of coastal‐ and shallow‐water settings, where wave breaking, longshore drift and wave shoaling drive sediment transport and control the final accumulations. These processes resulted in thick packages of sediments, as identified in the Lower Cretaceous depositional record of Brazilian marginal basins. In this context, 3D physical modelling experiments were performed in a wave tank using a mixed sediment composition to reproduce the coastal processes at a small scale to verify their control on the sedimentolog

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26

Souza Filho, Pedro Walfir Martins, and Maâmar El-Robrini. "MORFOLOGIA, PROCESSOS DE SEDIMENTAÇÃO E LITOFÁCIES DOS AMBIENTES MORFO-SEDIMENTARES DA PLANÍCIE COSTEIRA BRAGANTINA, NORDESTE DO PARÁ, BRASIL." Geonomos, December 1, 1996. http://dx.doi.org/10.18285/geonomos.v4i2.197.

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The Bragança Coastal Plain is located in the Northeastern of Pará, in the Bragança-Viseu CoaxialBasin (Cretaceous), with an approximate surface area of 1,570 Km2. The geometry of the basin and itspaleotopography, associated with recent tectonic movements have controlled the distribution and thethickness of the tertiary and quaternary deposits. This coastal plain constitutes a macrotidal (6 m) depositionalsystem, developed in a hot and humid equatorial climate, with a dry and wet well defined seasons and anannual precipitation averaging 3,000 mm.The geomorphology of the area is subdivided into

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27

Watson, Robert. "E-Press and Oppress." M/C Journal 8, no. 2 (2005). http://dx.doi.org/10.5204/mcj.2345.

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   From elephants to ABBA fans, silicon to hormone, the following discussion uses a new research method to look at printed text, motion pictures and a teenage rebel icon. If by ‘print’ we mean a mechanically reproduced impression of a cultural symbol in a medium, then printing has been with us since before microdot security prints were painted onto cars, before voice prints, laser prints, network servers, record pressings, motion picture prints, photo prints, colour woodblock prints, before books, textile prints, and footprints. If we accept that higher mammals such as elepha

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