Relevant bibliographies by topics / Slab ocean

Contents

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

Academic literature on the topic 'Slab ocean'

Author: Grafiati
Published: 4 June 2025
Last updated: 1 August 2025

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Journal articles on the topic "Slab ocean"

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Beaussier, Stéphane J., Taras V. Gerya, and Jean-Pierre Burg. "3D numerical modelling of the Wilson cycle: structural inheritance of alternating subduction polarity." Geological Society, London, Special Publications 470, no. 1 (2018): 439–61. http://dx.doi.org/10.1144/sp470.15.

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AbstractAlternating subduction polarity along suture zones has been documented in several orogenic systems. Yet the mechanisms leading to this geometric inversion and the subsequent interplay between the contra-dipping slabs have been little studied. To explore such mechanisms, 3D numerical modelling of the Wilson cycle was conducted from continental rifting, breakup and oceanic spreading to convergence and self-consistent subduction initiation. In the resulting models, near-ridge subduction initiating with the formation of contra-dipping slab segments is an intrinsically 3D process controlled
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Dommenget, Dietmar. "The slab ocean El Niño." Geophysical Research Letters 37, no. 20 (2010): n/a. http://dx.doi.org/10.1029/2010gl044888.

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Agard, Philippe, and Mark R. Handy. "Ocean Subduction Dynamics in the Alps." Elements 17, no. 1 (2021): 9–16. http://dx.doi.org/10.2138/gselements.17.1.9.

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The Alps preserve abundant oceanic blueschists and eclogites that exemplify the selective preservation of fragments of relatively short-lived, small, slow-spreading North Atlantic–type ocean basins whose subducting slabs reach down to the Mantle Transition Zone at most. Whereas no subducted fragments were returned during the first half of the subduction history, those exhumed afterwards experienced conditions typical of mature subduction zones worldwide. Sedimentary-dominated units were under-plated intermittently, mostly at ~30–40 km depth. Some mafic–ultramafic-dominated units formed close t
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Graff, Lise S., Trond Iversen, Ingo Bethke, et al. "Arctic amplification under global warming of 1.5 and 2 °C in NorESM1-Happi." Earth System Dynamics 10, no. 3 (2019): 569–98. http://dx.doi.org/10.5194/esd-10-569-2019.

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Abstract. Differences between a 1.5 and 2.0 ∘C warmer climate than 1850 pre-industrial conditions are investigated using a suite of uncoupled (Atmospheric Model Intercomparison Project; AMIP), fully coupled, and slab-ocean experiments performed with Norwegian Earth System Model (NorESM1)-Happi, an upgraded version of NorESM1-M. The data from the AMIP-type runs with prescribed sea-surface temperatures (SSTs) and sea ice were provided to a model intercomparison project (HAPPI – Half a degree Additional warming, Prognosis and Projected Impacts; http://www.happimip.org/, last access date: 14 Septe
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Danabasoglu, Gokhan, and Peter R. Gent. "Equilibrium Climate Sensitivity: Is It Accurate to Use a Slab Ocean Model?" Journal of Climate 22, no. 9 (2009): 2494–99. http://dx.doi.org/10.1175/2008jcli2596.1.

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Abstract The equilibrium climate sensitivity of a climate model is usually defined as the globally averaged equilibrium surface temperature response to a doubling of carbon dioxide. This is virtually always estimated in a version with a slab model for the upper ocean. The question is whether this estimate is accurate for the full climate model version, which includes a full-depth ocean component. This question has been answered for the low-resolution version of the Community Climate System Model, version 3 (CCSM3). The answer is that the equilibrium climate sensitivity using the full-depth oce
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Kay, Jennifer E., Marika M. Holland, Cecilia M. Bitz, et al. "The Influence of Local Feedbacks and Northward Heat Transport on the Equilibrium Arctic Climate Response to Increased Greenhouse Gas Forcing." Journal of Climate 25, no. 16 (2012): 5433–50. http://dx.doi.org/10.1175/jcli-d-11-00622.1.

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Abstract This study uses coupled climate model experiments to identify the influence of atmospheric physics [Community Atmosphere Model, versions 4 and 5 (CAM4; CAM5)] and ocean model complexity (slab ocean, full-depth ocean) on the equilibrium Arctic climate response to an instantaneous CO2 doubling. In slab ocean model (SOM) experiments using CAM4 and CAM5, local radiative feedbacks, not atmospheric heat flux convergence, are the dominant control on the Arctic surface response to increased greenhouse gas forcing. Equilibrium Arctic surface air temperature warming and amplification are greate
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Bercovici, David, Gerald Schubert, and Yanick Ricard. "Abrupt tectonics and rapid slab detachment with grain damage." Proceedings of the National Academy of Sciences 112, no. 5 (2015): 1287–91. http://dx.doi.org/10.1073/pnas.1415473112.

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A simple model for necking and detachment of subducting slabs is developed to include the coupling between grain-sensitive rheology and grain-size evolution with damage. Necking is triggered by thickened buoyant crust entrained into a subduction zone, in which case grain damage accelerates necking and allows for relatively rapid slab detachment, i.e., within 1 My, depending on the size of the crustal plug. Thick continental crustal plugs can cause rapid necking while smaller plugs characteristic of ocean plateaux cause slower necking; oceanic lithosphere with normal or slightly thickened crust
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Bitz, C. M., K. M. Shell, P. R. Gent, et al. "Climate Sensitivity of the Community Climate System Model, Version 4." Journal of Climate 25, no. 9 (2012): 3053–70. http://dx.doi.org/10.1175/jcli-d-11-00290.1.

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Equilibrium climate sensitivity of the Community Climate System Model, version 4 (CCSM4) is 3.20°C for 1° horizontal resolution in each component. This is about a half degree Celsius higher than in the previous version (CCSM3). The transient climate sensitivity of CCSM4 at 1° resolution is 1.72°C, which is about 0.2°C higher than in CCSM3. These higher climate sensitivities in CCSM4 cannot be explained by the change to a preindustrial baseline climate. This study uses the radiative kernel technique to show that, from CCSM3 to CCSM4, the global mean lapse-rate feedback declines in magnitude and
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Pendergrass, Angeline G., Gregory J. Hakim, David S. Battisti, and Gerard Roe. "Coupled Air–Mixed Layer Temperature Predictability for Climate Reconstruction." Journal of Climate 25, no. 2 (2012): 459–72. http://dx.doi.org/10.1175/2011jcli4094.1.

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Abstract A central issue for understanding past climates involves the use of sparse time-integrated data to recover the physical properties of the coupled climate system. This issue is explored in a simple model of the midlatitude climate system that has attributes consistent with the observed climate. A quasigeostrophic (QG) model thermally coupled to a slab ocean is used to approximate midlatitude coupled variability, and a variant of the ensemble Kalman filter is used to assimilate time-averaged observations. The dependence of reconstruction skill on coupling and thermal inertia is explored
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Yang, Jianjin, Shengyang Zhu, and Wanming Zhai. "Modeling Slab Track for Vehicle –Track-Coupled Dynamics Analysis Using Spline Function Method." International Journal of Structural Stability and Dynamics 20, no. 02 (2020): 2050026. http://dx.doi.org/10.1142/s0219455420500261.

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This paper presents a new approach for modeling the slab tracks by using the spline function to derive an element that is capable of describing the vertical motions of the entire slab. The accuracy and advantages of the method are verified through comparison with the finite element method (FEM) by the frequency response analysis for the CRTS-III slab track system. With this, a three-dimensional train–slab track-coupled dynamic (TSTCD) model is developed and solved by a hybrid explicit–implicit time integration method. Finally, the characteristics and feasibility of the developed TSTCD model ar
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Dissertations / Theses on the topic "Slab ocean"

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De, Vos Marc. "The impact of assimilating along-track SLA data on simulated Eddy characteristics in the Agulhas system." Master's thesis, University of Cape Town, 2016. http://hdl.handle.net/11427/20503.

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The Agulhas Current System is a vital element of the global ocean-climate system by virtue of its role in the transfer of energy, nutrients and organic material. In the context of working towards better climate change projections, it is necessary to develop a robust understanding of the complex dynamical mechanisms which facilitate this transfer. Mesoscale cyclonic and anticyclonic eddies transport heat, salt, organic matter and nutrients from the Indian Ocean into the South Atlantic Ocean. In so doing, they are key drivers of the Atlantic Meridional Overturning Circulation (AMOC). As such, it
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Nag, Bappaditya. "Difference In Land-Ocean Response And The Regional Impact Of Geo-Engineering." Thesis, 2010. https://etd.iisc.ac.in/handle/2005/1658.

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Nag, Bappaditya. "Difference In Land-Ocean Response And The Regional Impact Of Geo-Engineering." Thesis, 2010. http://etd.iisc.ernet.in/handle/2005/1658.

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Thomas, Giles(Giles Anthony). "Wave slam response of large high-speed catamarans." Thesis, 2003. https://eprints.utas.edu.au/22112/1/whole_ThomasGilesAnthony2003_thesis.pdf.

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The rapid evolution of high-speed sea transportation has led to the development of large, fast, lightweight vessels. The structural design optimisation of such vessels requires knowledge of the effect of sea loads on their structure. Of particular importance for high-speed catamarans are severe wet-deck slam events, which can impart a large global load onto a vessel's structure and as a consequence cause significant structural damage. The dynamic whipping response of the structure may also be important by making a significant contribution to fatigue damage. Extensive full-scale hull stre
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Wung, Bor-Yann, and 翁博彥. "Numerical Simulation of transport of slag and sludge in ocean dumping." Thesis, 1995. http://ndltd.ncl.edu.tw/handle/00882837982337563393.

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碩士<br>國立中央大學<br>土木工程研究所<br>83<br>Numerical modeling of ocean dumping process of solid waste is studied in this research. During the process,the dumped solid waste generates waste clouds, and the clouds are classified into two regimes. There are the short-term fate and long-term fate subsequently. In the short-term fate, transport of waste clouds can be categorized into three phases: 1) Convective Descent,during which the waste cloud falls under the influence of initial momentum and grav
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Books on the topic "Slab ocean"

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Kerry, Isaac. Boyan Slat: Pioneering the Ocean Cleanup. Capstone, 2021.

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Kerry, Isaac. Boyan Slat: Pioneering the Ocean Cleanup. Capstone, 2021.

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Kerry, Isaac. Boyan Slat: Pioneering the Ocean Cleanup. Capstone, 2021.

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Kerry, Isaac. Boyan Slat: Pioneering the Ocean Cleanup. Capstone, 2021.

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Kerry, Isaac. Boyan Slat: Pioneering the Ocean Cleanup. Capstone, 2021.

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Kerry, Isaac. Boyan Slat: Pioneering the Ocean Cleanup. Capstone Press, 2021.

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Kerry, Isaac. Boyan Slat: Pioneering the Ocean Cleanup. Capstone, 2021.

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Kerry, Isaac. Boyan Slat and the Ocean Cleanup. Raintree Publishers, 2021.

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Kerry, Isaac. Boyan Slat and the Ocean Clean-Up. Raintree Publishers, 2021.

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Kresse, Kai, and Edward Simpson. Struggling with History: Slam and Cosmopolitanism in the Western Indian Ocean. Oxford University Press, 2008.

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Book chapters on the topic "Slab ocean"

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Gonzalez, F. I., E. D. Cokelet, J. F. R. Gower, and M. R. Mulhern. "SLAR and In-Situ Observations of Wave-Current Interaction on the Columbia River Bar." In The Ocean Surface. Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-015-7717-5_41.

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Kellhammer, Oliver. "Neo-Eocene." In Making the Geologic Now. punctum books, 2012. https://doi.org/10.21983/p3.0014.1.35.

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Back in the mid-1960s, I was a feral sort of a child who loved scampering around construc-tion sites, climbing the huge, grey piles of excavated shale that were popping up all over my rapidly developing Toronto suburb. I might have been six or so when I first really noticed the slabs of muddy smelling rock often contained the imprints of scallop shells, snails, and fragments of coral, things I recognized from picture books but hadn’t yet seen in real life as we lived hundreds of miles from the near-est ocean. Yet 450 million years before, during the Ordovician era, where I was playing would ha
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Glover, Robert. "Corrosion Processes of Steel-Hulled Potentially Polluting Wrecks." In Threats to Our Ocean Heritage: Potentially Polluting Wrecks. Springer Nature Switzerland, 2024. http://dx.doi.org/10.1007/978-3-031-57960-8_4.

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AbstractSubmerged metals are continuously affected by the chemical processes of corrosion, the destructive degradation of metal by chemical or electrochemical reactions within the marine environment (Valenca et al., 2022:2–3; Venugopal, 1994:35). Over time, metal ions at anodic sites defuse into electrolytic solutions from the oxidising reactions occurring at cathodic sites, causing the creation of corrosion byproducts, like rust on iron, and the loss of structural mass. The different reduction reactions in the microstructures of alloys and the imperfections found within refined materials, lik
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Zhu, Junjiang, Sanzhong Li, Huilin Xing, et al. "Large-magnitude oceanic intraplate seismicity: Implications for lithosphere evolution." In In the Footsteps of Warren B. Hamilton: New Ideas in Earth Science. Geological Society of America, 2022. http://dx.doi.org/10.1130/2021.2553(10).

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ABSTRACT We analyzed 37 large oceanic intraplate earthquakes (M &amp;gt;6). The largest (M &amp;gt;7) are mainly concentrated under the Indian Ocean. Moderate events (6 &amp;lt; M &amp;lt; 7) are sparsely distributed under the Indian Ocean and other oceans where lithospheric ages are between 90 Ma and 20 Ma. Oceanic intraplate events related to mantle plumes or hotspots are rare, though low-velocity anomalies beneath hotspots are a common feature. Tomographic cross sections for Indian Ocean areas with large intraplate earthquakes indicate strong heterogeneity in the mantle. These earthquakes a
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Kirk, John T. O. "The Relationship between the Inherent and the Apparent Optical Properties of Surface Waters and its Dependence on the Shape of the Volume Scattering Function." In Ocean Optics. Oxford University Press, 1994. http://dx.doi.org/10.1093/oso/9780195068436.003.0006.

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Let us begin by reminding ourselves just what we mean by “the inherent optical properties” and “the apparent optical properties” of surface waters. The inherent optical properties are those that belong to the aquatic medium itself: properties that belong to a small sample of the aquatic medium taken out of the water body just as much as they belong to a great mass of the medium existing within the water body itself. The properties of particular concern to us are the absorption coefficient, a, the scattering coefficient, b, and the volume scattering function, β(θ). The absorption coefficient at
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Konopelko, Dmitry L. "Chapter 4. Paleozoic granitoid magmatism of South and Middle Tien Shan in Uzbekistan." In PALEOZOIC GRANITOID MAGMATISM OF WESTERN TIEN SHAN. St. Petersburg State University, 2020. http://dx.doi.org/10.21638/11701/9785288060250.05.

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The Paleozoic evolution of the Southern and Middle Tien Shan terranes is generally associated with the history of two ocean basins - the Turkestan and Paleotethys. Ages of ophiolites indicate the opening of the oceans in Cambrian – Ordovician, and partial closure with formation of an island arc in the northern part of the basin in Ordovician - Silurian. At the northern margin of the Turkestan ocean, the northward subduction under the Middle Tien Shan continued until Devonian, which led to formation of an active margin with granitoids emplaced between 429 and 416 Ma. In the late Devonian, subdu
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Hallam, Anthony. "Late Mesozoic." In An Outline of Phanerozoic Biogeography. Oxford University PressOxford, 1994. http://dx.doi.org/10.1093/oso/9780198540618.003.0008.

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Abstract The Cretaceous Period was a time of considerable geological activity associated primarily with the disintegration of Pangaea and a considerable increase in volcanism, which had significant biogeographic consequences. As in previous chapters attention will be directed initially to the framework of major geological events before considering organic distributions. The most up-to-date plate tectonic reconstructions for the Cretaceous are those of Scotese et al. (1988), which have utilized an interactive computer graphics method. The three dimensional capabilities of this method allow the
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Molnar, Peter. "4. Subduction of oceanic lithosphere." In Plate Tectonics: A Very Short Introduction. Oxford University Press, 2015. http://dx.doi.org/10.1093/actrade/9780198728269.003.0004.

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‘Subduction of oceanic lithosphere’ begins with the notion that for the Earth not to expand, the sum total of new lithosphere made at a spreading centre (or mid-ocean ridge) must be matched by the removal, by subduction, of an equal amount of lithosphere elsewhere. The subduction process is asymmetric: one plate will slide beneath the other at island arcs and continental margins like the Andes of South America. Before it plunges beneath the island arc, the subducting plate of lithosphere bends down gently to cause a deep-sea trench. The subducting plate slides beneath the region between the tr
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Mottl, M. J. "Pore Waters from Serpentinite Seamounts in the Mariana and Izu-Bonin Forearcs, Leg 125: Evidence for Volatiles from the Subducting Slab." In Proceedings of the Ocean Drilling Program, 125 Scientific Results. Ocean Drilling Program, 1992. http://dx.doi.org/10.2973/odp.proc.sr.125.121.1992.

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Kroner, Uwe, Tobias Stephan, and Rolf L. Romer. "Paleozoic orogenies and relative plate motions at the sutures of the Iapetus-Rheic Ocean." In New Developments in the Appalachian-Caledonian- Variscan Orogen. Geological Society of America, 2022. http://dx.doi.org/10.1130/2021.2554(001).

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ABSTRACT Early Ordovician to late Permian orogenies at different plate-boundary zones of western Pangea affected continental crust derived from the plates of North America (Laurentia), Europe (East European Craton including Baltica plus Arctida), and Gondwana. The diachronic orogenic processes comprised stages of intraoceanic subduction, formation and accretion of island arcs, and collision of several continents. Using established plate-tectonic models proposed for different regions and time spans, we provide for the first time a generic model that explains the tectonics of the entire Gondwana
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Conference papers on the topic "Slab ocean"

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Loi, Nicola, Yan Zhi Tan, Eng Wei Goh, and Marcelo H. Ang. "Sonar SLAM in Structured Underwater Environments." In OCEANS 2024 - SINGAPORE. IEEE, 2024. http://dx.doi.org/10.1109/oceans51537.2024.10682261.

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Manuel Pirozzo, Bernardo, Mariano De Paula, Sebastián Aldo Villar, and Gerardo Gabriel Acosta. "Underwater Rat-SLAM with Memristive Spiking Neural Networks." In OCEANS 2024 - Halifax. IEEE, 2024. http://dx.doi.org/10.1109/oceans55160.2024.10754319.

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Oliveira, António J., Bruno M. Ferreira, and Nuno A. Cruz. "A Clustering-Aided Template Matching Algorithm Towards Underwater SLAM Using Imaging Sonar." In OCEANS 2024 - Halifax. IEEE, 2024. http://dx.doi.org/10.1109/oceans55160.2024.10753953.

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Hosoi, Hiroki, and Takumi Matsuda. "Robust Monocular Visual SLAM of Multiple Autonomous Underwater Vehicles against the Keypoint Loss." In OCEANS 2024 - SINGAPORE. IEEE, 2024. http://dx.doi.org/10.1109/oceans51537.2024.10741895.

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Basov, Alexander, Georgii Boos, Vladimir P. Budak, Anton Grimailo, and Dmitrii Efremenko. "Slab radiance factor calculating methods." In 27th International Symposium on Atmospheric and Ocean Optics, Atmospheric Physics, edited by Oleg A. Romanovskii and Gennadii G. Matvienko. SPIE, 2021. http://dx.doi.org/10.1117/12.2603756.

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Budak, Vladimir P., Oleg V. Shagalov, and Victor S. Zheltov. "Numerical radiative transfer modeling in turbid medium slab." In 20th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics, edited by Oleg A. Romanovskii. SPIE, 2014. http://dx.doi.org/10.1117/12.2074692.

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Beppu, Masuhiro, and Shinnosuke Kataoka. "Failure Behavior of RC Slabs Subjected to Medium Velocity Impact." In ASME 2016 35th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2016. http://dx.doi.org/10.1115/omae2016-54256.

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This study is intended to investigate failure mechanism of plain concrete and reinforced concrete slabs subjected to a medium-velocity impact by conducting impact tests. In a series of tests, a steel projectile with a mass of 8.3kg collided a concrete slab with a thickness of 18cm. In order to examine impact response of the concrete specimen, impact load and reaction force were measured. Test results revealed that the impact velocity corresponding to the scabbing limit was about 40m/s and the failure mode of the concrete specimen subjected to the medium-velocity was similar to the punching she
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Abbas, Husain, Tarek Almusallam, Yousef Al-Salloum, Nadeem Siddiqui, and Aref Abadel. "TRM Versus FRP as Strengthening Material for Improving Impact Resistance of RC Slabs." In ASME 2016 35th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2016. http://dx.doi.org/10.1115/omae2016-54737.

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This study experimentally investigates the effectiveness of textile reinforced mortar (TRM) in controlling the local damage in reinforced concrete (RC) slabs subjected to impact loads. The results are then compared with that of conventional FRP strengthening of RC slabs. The impact tests were conducted using the strike of hemispherical nosed steel projectile on TRM- and FRP-strengthened RC slabs. The unstrengthened specimens considered as control were 600 mm square, 90 mm thick RC slabs. The slabs were reinforced with 8 mm diameter steel rebars at 100 mm c/c spacing both-ways. The slabs were s
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Li, Yuzhu, Muk Chen Ong, Ove Tobias Gudmestad, and Bjørn Helge Hjertager. "Numerical Analysis of Steep Wave-Induced Seabed Response and Liquefaction Around Gravity-Based Offshore Foundations." In ASME 2018 37th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2018. http://dx.doi.org/10.1115/omae2018-77046.

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Gravity-based offshore foundations generally consist of a bottom slab and one or more cylindrical shafts on top of it. The geometry of the structure can strongly affect the flow pattern, dynamic wave pressure and further soil response and the liquefaction risk in the vicinity of the foundation. In this work, gravity-based foundations with bottom slabs of cylindrical shape and hexagonal prismatic shape are investigated. An integrated wave-structure-seabed interaction model applied in this work is developed in Open-FOAM, incorporating a nonlinear wave solver, a linear elastic structure solver an
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Ong, Muk Chen, Eirik Trygsland, and Dag Myrhaug. "Numerical Study of Seabed Boundary Layer Flow Around Monopile and Gravity-Based Wind Turbine Foundations." In ASME 2016 35th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2016. http://dx.doi.org/10.1115/omae2016-54643.

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Computational fluid dynamics (CFD) has been used to study the seabed boundary layer flow around monopile and gravity-based offshore wind turbine foundations. The gravity-based foundation has a hexagonal bottom slab (bottom part). The objective of the present study is to study the flow structures around the bottom-fixed offshore wind turbine foundations in order to provide essential hydrodynamic coefficients for engineering design and an assessment of potential scour erosion. Three-dimensional CFD simulations have been performed using Spalart-Allmaras Delayed Detached Eddy Simulation (SADDES) a
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