Relevant bibliographies by topics / Sand spit morpho dynamic

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  1. Journal articles
  2. Dissertations / Theses
  3. Book chapters
  4. Conference papers

Academic literature on the topic 'Sand spit morpho dynamic'

Author: Grafiati
Published: 7 July 2024
Last updated: 31 July 2025

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Journal articles on the topic "Sand spit morpho dynamic"

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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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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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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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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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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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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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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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Dissertations / Theses on the topic "Sand spit morpho dynamic"

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Meslard, Florian. "Apports sableux par les fleuves côtiers méditerranéens et aléa de submersion marine (ASPLEC)." Electronic Thesis or Diss., Perpignan, 2023. http://www.theses.fr/2023PERP0053.

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Obtenir des estimations précises des bilans sédimentaires sur le continuum terre-mer et comprendre comment ces bilans affectent la dynamique des littoraux est devenu un enjeu crucial dans le contexte actuel de montée du niveau marin et de recul du trait de côte. Les fleuves côtiers méditerranéens, du fait d’un caractère torrentiel lié à des événements météorologiques intenses, sont caractérisés par des épisodes de crues brefs mais violents durant lesquels la majorité du flux d’eau et de sédiments est apportée à la zone côtière en quelques jours. Ce mode de fonctionnement épisodique impacte éga
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Book chapters on the topic "Sand spit morpho dynamic"

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Foyle*, Anthony M., and Patrick Burkhart*. "Shifting sands and anthropogenic modifications along the Presque Isle strandplain on the NW Pennsylvania coast of Lake Erie." In Coastal and Structural Geology, Paleontology, and Building Stones Along the Eastern Shore of Lake Erie. Geological Society of America, 2025. https://doi.org/10.1130/2025.0071(01).

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ABSTRACT This field guide reviews the coastal and engineering geology of Presque Isle State Park, a 9 km2 flying sand spit located on the NW Pennsylvania bluff coast of Lake Erie on the North American Great Lakes. Much of the spit’s shoreline is armored with offshore breakwaters, groynes, and riprap, and lakefront beaches have received regular beach nourishment for more than half a century. The guide describes a series of eight field-trip stops along this dynamic and anthropogenically modified depositional landform. The stops progress downdrift along the Lake Erie side of the spit to the North
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Conference papers on the topic "Sand spit morpho dynamic"

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Dorokhova, Evgenia, Evgenia Dorokhova, Dmitry Dorokhov, and Dmitry Dorokhov. "SEDIMENT MAPPING AND TRANSPORT PATHWAYS IN THE NEARSHORE ZONE OF THE RUSSIAN PART OF THE SOUTH-EASTERN BALTIC SEA." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b9489e8deb2.41910928.

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To achieve a more robust interpretation of sediment conditions and transport, our study combines the two different interpretation techniques. A side-scan sonar survey was used as a basis for detail sedimentological investigation. Grain-size analyses of grab samples provided sediment transport direction and decoding of sonar data. The new detail lithological map of the underwater shore slope of the northern Sambian peninsula and the Russian part of the Curonian spit in 1:50 000 scale is created. For the first time, the stretched zone of very fine sands is outlined at depths of 25-30 m of the Cu
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Dorokhova, Evgenia, Evgenia Dorokhova, Dmitry Dorokhov, and Dmitry Dorokhov. "SEDIMENT MAPPING AND TRANSPORT PATHWAYS IN THE NEARSHORE ZONE OF THE RUSSIAN PART OF THE SOUTH-EASTERN BALTIC SEA." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b43152071d3.

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To achieve a more robust interpretation of sediment conditions and transport, our study combines the two different interpretation techniques. A side-scan sonar survey was used as a basis for detail sedimentological investigation. Grain-size analyses of grab samples provided sediment transport direction and decoding of sonar data. The new detail lithological map of the underwater shore slope of the northern Sambian peninsula and the Russian part of the Curonian spit in 1:50 000 scale is created. For the first time, the stretched zone of very fine sands is outlined at depths of 25-30 m of the Cu
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TAKAGAWA, TOMOHIRO, YOSHIMITSU TAJIMA, HAIJIANG LIU, SATOSHI TAKEWAKA, and SHINJI SATO. "DYNAMIC TOPOGRAPHY CHANGES OF SAND SPIT OF THE TENRYU RIVER MOUTH DUE TO OVERTOPPING WAVES." In The Proceedings of the Coastal Sediments 2011. World Scientific Publishing Company, 2011. http://dx.doi.org/10.1142/9789814355537_0092.

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Fomin, Vladimir, Vladimir Fomin, Ludmila Kharitonova, et al. "MORPHODYNAMICS OF THE BAKALSKAYA SPIT OF THE BLACK SEA." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b93fae199c8.45419382.

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Studies of shape dynamics of the Bakalskaya Spit based on observation and numerical simulation are carries out. The Bakalskaya Spit is a dynamically active sand formation on the north-west coast of the Crimea Peninsula. Field observations and satellite image analyses showed that the erosion of spit west coast, eastward displacement of spit distal part and separation of distal part from the spit main part are the most significant processes. After the autumn storms in 2010 the isthmus between the distal part of spit and its main part was eroded and had not recovered till now. So the distal part
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Fomin, Vladimir, Vladimir Fomin, Ludmila Kharitonova, et al. "MORPHODYNAMICS OF THE BAKALSKAYA SPIT OF THE BLACK SEA." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b431521aa58.

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Studies of shape dynamics of the Bakalskaya Spit based on observation and numerical simulation are carries out. The Bakalskaya Spit is a dynamically active sand formation on the north-west coast of the Crimea Peninsula. Field observations and satellite image analyses showed that the erosion of spit west coast, eastward displacement of spit distal part and separation of distal part from the spit main part are the most significant processes. After the autumn storms in 2010 the isthmus between the distal part of spit and its main part was eroded and had not recovered till now. So the distal part
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Babakov, Alexander, Alexander Babakov, Boris Chubarenko, and Boris Chubarenko. "SEDIMENT TRANSPORT NEAR THE VISTULA SPIT (BALTIC SEA)." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b93751e4b25.42106675.

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The Vistula Spit is a sandy elongated barrier form which borders the Vistula Lagoon from the Baltic Sea. The evolution of the spit as well as nowadays sediment transport along the marine shore of it are still under discussion, especially due to existing of entrance jetties bordered the Strait of Baltiysk, the single inlet to the Vistula Lagoon, and advanced up to 10 m depth seaward. Different hypothesizes about ether uniform transport from north to south or contrary directed fluxes with convergence at various points at the spit shore are discussed. Most of them are based on fact of accumulatio
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Babakov, Alexander, Alexander Babakov, Boris Chubarenko, and Boris Chubarenko. "SEDIMENT TRANSPORT NEAR THE VISTULA SPIT (BALTIC SEA)." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b4315e36e45.

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The Vistula Spit is a sandy elongated barrier form which borders the Vistula Lagoon from the Baltic Sea. The evolution of the spit as well as nowadays sediment transport along the marine shore of it are still under discussion, especially due to existing of entrance jetties bordered the Strait of Baltiysk, the single inlet to the Vistula Lagoon, and advanced up to 10 m depth seaward. Different hypothesizes about ether uniform transport from north to south or contrary directed fluxes with convergence at various points at the spit shore are discussed. Most of them are based on fact of accumulatio
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