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Relevant bibliographies by topics / Open-ocean convection

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Academic literature on the topic 'Open-ocean convection'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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Journal articles on the topic "Open-ocean convection"

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Vreugdenhil, Catherine A., and Bishakhdatta Gayen. "Ocean Convection." Fluids 6, no. 10 (2021): 360. http://dx.doi.org/10.3390/fluids6100360.

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Ocean convection is a key mechanism that regulates heat uptake, water-mass transformation, CO2 exchange, and nutrient transport with crucial implications for ocean dynamics and climate change. Both cooling to the atmosphere and salinification, from evaporation or sea-ice formation, cause surface waters to become dense and down-well as turbulent convective plumes. The upper mixed layer in the ocean is significantly deepened and sustained by convection. In the tropics and subtropics, night-time cooling is a main driver of mixed layer convection, while in the mid- and high-latitude regions, winte

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Schloesser, Fabian. "Large-Scale Dynamics of Circulations with Open-Ocean Convection." Journal of Physical Oceanography 45, no. 12 (2015): 2933–51. http://dx.doi.org/10.1175/jpo-d-15-0088.1.

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AbstractFormation of the densest water masses in the North Atlantic and its marginal seas involves open-ocean convection. The main goal of this study is to contribute to the general understanding of how such convective regions connect to the large-scale ocean circulation. Specifically, analytic and numerical versions of a variable density layer model are used to explore the processes underlying the circulation in an idealized ocean basin. The models are forced by a surface buoyancy flux, which generates a density maximum in the ocean interior. In response to the forcing, a region forms that is

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Sohail, Taimoor, Bishakhdatta Gayen, and Andrew McC. Hogg. "The Dynamics of Mixed Layer Deepening during Open-Ocean Convection." Journal of Physical Oceanography 50, no. 6 (2020): 1625–41. http://dx.doi.org/10.1175/jpo-d-19-0264.1.

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AbstractOpen-ocean convection is a common phenomenon that regulates mixed layer depth and ocean ventilation in the high-latitude oceans. However, many climate model simulations overestimate mixed layer depth during open-ocean convection, resulting in excessive formation of dense water in some regions. The physical processes controlling transient mixed layer depth during open-ocean convection are examined using two different numerical models: a high-resolution, turbulence-resolving nonhydrostatic model and a large-scale hydrostatic ocean model. An isolated destabilizing buoyancy flux is imposed

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Marshall, John, and Friedrich Schott. "Open-ocean convection: Observations, theory, and models." Reviews of Geophysics 37, no. 1 (1999): 1–64. http://dx.doi.org/10.1029/98rg02739.

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Brickman, David. "Heat Flux Partitioning in Open-Ocean Convection." Journal of Physical Oceanography 25, no. 11 (1995): 2609–23. http://dx.doi.org/10.1175/1520-0485(1995)025<2609:hfpioo>2.0.co;2.

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Alverson, Keith, and W. Brechner Owens. "Topographic Preconditioning of Open-Ocean Deep Convection." Journal of Physical Oceanography 26, no. 10 (1996): 2196–213. http://dx.doi.org/10.1175/1520-0485(1996)026<2196:tpoood>2.0.co;2.

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Kuhlbrodt, Till, and Adam Hugh Monahan. "Stochastic Stability of Open-Ocean Deep Convection." Journal of Physical Oceanography 33, no. 12 (2003): 2764–80. http://dx.doi.org/10.1175/1520-0485(2003)033<2764:ssoodc>2.0.co;2.

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Sander, Johannes, Dieter Wolf-Gladrow, and Dirk Olbers. "Numerical studies of open ocean deep convection." Journal of Geophysical Research 100, no. C10 (1995): 20579. http://dx.doi.org/10.1029/95jc02405.

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Herrmann, Marine, Jérome Bouffard, and Karine Béranger. "Monitoring open-ocean deep convection from space." Geophysical Research Letters 36, no. 3 (2009): n/a. http://dx.doi.org/10.1029/2008gl036422.

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Bacon, Sheldon, W. John Gould, and Yanli Jia. "Open-ocean convection in the Irminger Sea." Geophysical Research Letters 30, no. 5 (2003): n/a. http://dx.doi.org/10.1029/2002gl016271.

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Dissertations / Theses on the topic "Open-ocean convection"

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Alves, J. O. S. "Open-ocean deep convection : understanding and parametrization." Thesis, University of Reading, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.262034.

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Alverson, Keith D. 1965. "Topographic preconditioning of open ocean deep convection." Thesis, Massachusetts Institute of Technology, 1995. http://hdl.handle.net/1721.1/53023.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 1995.<br>Includes bibliographical references (leaves 143-146).<br>by Keith D. Alverson.<br>Ph.D.

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Kuhlbrodt, Till. "Stability and variability of open-ocean deep convection in deterministic and stochastic simple models." Phd thesis, [S.l. : s.n.], 2002. http://pub.ub.uni-potsdam.de/2002/0033/kuhlb.pdf.

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Mertens, Christian. "Open-ocean convection in the Labrador and Greenland seas plume scales and interannual Variability /." [S.l. : s.n.], 2000. http://e-diss.uni-kiel.de/diss/d363.pdf.

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Roberts, Zoe Louise. "The application of adaptive mesh modelling techniques to the study of open ocean deep convection." Thesis, University of Southampton, 2008. https://eprints.soton.ac.uk/65672/.

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The rapid cooling of the waters at high latitudes creates an unstable strati cation which in turn leads to localised overturning (sinking) of the water column. This process is called open ocean deep convection (OODC). The process of OODC occurs in stages. Initially, individual convective elements known as plumes form and cold, dense water descends from the surface. Over time these plumes build up to produce a well-mixed `chimney' of cold dense uid. This chimney then slumps and sinks, and restratication (the return to a stable state throughout the water column) occurs. It is widely accepted tha

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Lavender, Kara L. "The general circulation and open-ocean deep convection in the Labrador Sea : a study using subsurface floats /." Diss., Connect to a 24 p. preview or request complete full text in PDF format. Access restricted to UC campuses, 2001. http://wwwlib.umi.com/cr/ucsd/fullcit?p3035893.

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Kuhlbrodt, Till [Verfasser]. "Stability and variability of open-ocean deep convection in deterministic and stochastic simple models / von Till Kuhlbrodt." 2002. http://d-nb.info/967536936/34.

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Mertens, Christian [Verfasser]. "Open-ocean convection in the Labrador and Greenland seas : plume scales and interannual Variability / vorgelegt von Christian Mertens." 2000. http://d-nb.info/972088172/34.

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Books on the topic "Open-ocean convection"

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Alverson, Keith D. Topographic preconditioning of open ocean deep convection / by Keith D. Alverson. Woods Hole Oceanographic Institution, 1995.

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Benestad, Rasmus. Climate in the Barents Region. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.655.

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The Barents Sea is a region of the Arctic Ocean named after one of its first known explorers (1594–1597), Willem Barentsz from the Netherlands, although there are accounts of earlier explorations: the Norwegian seafarer Ottar rounded the northern tip of Europe and explored the Barents and White Seas between 870 and 890 ce, a journey followed by a number of Norsemen; Pomors hunted seals and walruses in the region; and Novgorodian merchants engaged in the fur trade. These seafarers were probably the first to accumulate knowledge about the nature of sea ice in the Barents region; however, scienti

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Book chapters on the topic "Open-ocean convection"

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Schott, F., M. Visbeck, and U. Send. "Open Ocean Deep Convection, Mediterranean and Greenland Seas." In Ocean Processes in Climate Dynamics: Global and Mediterranean Examples. Springer Netherlands, 1994. http://dx.doi.org/10.1007/978-94-011-0870-6_9.

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Kovalevsky, Dmitry V., and Igor L. Bashmachnikov. "Nonlinear Dynamics of Deep Open-Ocean Convection: An Analytical Approach." In Nonlinear Physical Science. Springer Singapore, 2021. http://dx.doi.org/10.1007/978-981-16-2853-5_10.

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Soloviev, A., and B. Klinger. "Open Ocean Convection." In Encyclopedia of Ocean Sciences. Elsevier, 2001. http://dx.doi.org/10.1006/rwos.2001.0118.

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Soloviev, A., and B. Klinger. "Open Ocean Convection." In Encyclopedia of Ocean Sciences. Elsevier, 2001. http://dx.doi.org/10.1016/b978-012374473-9.00118-1.

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Soloviev, A., and B. Klinger. "Open Ocean Convection." In Encyclopedia of Ocean Sciences. Elsevier, 2001. http://dx.doi.org/10.1016/b978-0-12-813081-0.00118-x.

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Martinson, D. G. "Open Ocean Convection in the Southern Ocean." In Elsevier Oceanography Series. Elsevier, 1991. http://dx.doi.org/10.1016/s0422-9894(08)70059-x.

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Brugge, R., H. L. Jones, and J. C. Marshall. "Non-Hydrostatic Ocean Modelling for Studies of Open-Ocean Deep Convection." In Elsevier Oceanography Series. Elsevier, 1991. http://dx.doi.org/10.1016/s0422-9894(08)70075-8.

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Gascard, Jean-Claude. "Open Ocean Convection and Deep Water Formation Revisited in the Mediterranean, Labrador, Greenland and Weddell Seas." In Elsevier Oceanography Series. Elsevier, 1991. http://dx.doi.org/10.1016/s0422-9894(08)70066-7.

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Chu, P. C. "Vertical Cells Driven by Vortices - A Possible Mechanism for the Preconditioning of Open-Ocean Deep Convection." In Elsevier Oceanography Series. Elsevier, 1991. http://dx.doi.org/10.1016/s0422-9894(08)70072-2.

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Conference papers on the topic "Open-ocean convection"

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Nishida, Tomoya, and Takuji Waseda. "The Impact of Winter Northwest Monsoon on Gust Factor." In ASME 2013 32nd International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2013. http://dx.doi.org/10.1115/omae2013-10815.

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This paper examines temporal variation of ocean wind gust factor and turbulence intensity in the Northwest Pacific. Observation data at coastal and open oceans near Japan are analyzed to investigate the relationship between gust factor and turbulence intensity, and the seasonal variation of probability distribution of gust factor. The contrast of the winter monsoon cold air and relatively warmer sea surface temperature is the trigger for growth of the marine boundary layer. Downdraft by developed convection enhances sea surface gustiness. The relative significance of sensible heat flux to mome

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Kim, Young Jun, Benjamin Bouscasse, Sopheak Seng, and David Le Touze. "Numerical Study on the Temporal Discretization Schemes in Two-Phase Wave Simulation." In ASME 2019 38th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2019. http://dx.doi.org/10.1115/omae2019-96278.

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Abstract The generation and propagation of waves in a viscous flow solver are indispensable part of naval computational fluid dynamic (CFD) applications. This paper presents numerical simulations of two-dimensional wave propagation in the framework of two-phase finite volume method (FVM) with different temporal discretization schemes. Implicit Euler, Crank-Nicolson (CN) and second-order backward temporal discretization schemes are compared by using viscous flow solver based on the open source library OpenFOAM. The combinations of each temporal discretization scheme and explicit limiter are use

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Kamath, Arun, Tobias Martin, and Hans Bihs. "Numerical Modelling of Wave Interaction With an FPSO Under Different Incident Wave Conditions." In ASME 2019 38th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2019. http://dx.doi.org/10.1115/omae2019-96004.

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Abstract Numerical modelling of wave interaction with offshore structures provides deep insights into the complex wave hydrodynamics and the wave-structure interaction problem. Offshore structures such as an FPSO vessel are susceptible to continuous wave loading under operational conditions and catastrophically large wave loadings under extreme conditions. It is essential to obtain accurate information on the environmental forcing due to waves on an FPSO to reliably predict the operational conditions to optimise the operational times while considering operational safety. In addition, the wave

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Bihs, Hans, Arun Kamath, Mayilvahanan Alagan Chella, and Øivind A. Arntsen. "Extreme Wave Generation, Breaking and Impact Simulations With REEF3D." In ASME 2017 36th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2017. http://dx.doi.org/10.1115/omae2017-61524.

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An accurate description of extreme waves is necessary in order to estimate maximum wave forces on offshore structures. On several occasions freak waves have been observed in the past, some causing severe damage. In order to model such extreme wave conditions with a computational fluid dynamics (CFD) model, emphasize needs to be put on the wave generation. One possibility is to use focused waves of first or second order based on irregular sea state wave spectra. For focused waves, the wave phase is chosen, so that the waves focus in a predetermined location at a specified time. Numerical tests

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Bihs, Hans, Mayilvahanan Alagan Chella, Arun Kamath, and Øivind A. Arnsten. "Wave-Structure Interaction of Focussed Waves With REEF3D." In ASME 2016 35th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2016. http://dx.doi.org/10.1115/omae2016-54917.

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For the stability of offshore structures, such as offshore wind foundations, extreme wave conditions need to be taken into account. Waves from extreme events can become critical from design perspective. In a numerical wave tank, extreme waves can be generated through focussed waves. Here, linear waves are generated from a wave spectrum. The wave crests of the generated waves coincide at a pre-selected location and time. In order to test the generated waves, the time series of the free surface elevation are compared with experimental benchmark cases. The numerically simulated free surface shows

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Kamath, Arun, Hans Bihs, and Csaba Pakozdi. "Investigation of Higher-Harmonic Wave Forces and Ringing Using CFD Simulations." In ASME 2018 37th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2018. http://dx.doi.org/10.1115/omae2018-77925.

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Typical offshore structures are designed as tension-leg platforms or gravity based structures with cylindrical substructures. The interaction of waves with the vertical cylinders in high sea states can result in a resonant response called ringing. Here, the frequency of the structural response is close to the natural frequency of the structure itself and leads to large amplitude motions. This is a case of extreme wave loading in high sea states. This understanding of higher-order wave forces in extreme sea states is an essential parameter for obtaining a safe, reliable and economical design of

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Reports on the topic "Open-ocean convection"

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Marshall, John. Modeling Open-ocean Deep Convection. Defense Technical Information Center, 1997. http://dx.doi.org/10.21236/ada628813.

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Marshall, John. Modeling Open-Ocean Deep Convection. Defense Technical Information Center, 1999. http://dx.doi.org/10.21236/ada630259.

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Marshall, John C. Modelling Studies in Support of Open-Ocean Convection Field Programs. Defense Technical Information Center, 1992. http://dx.doi.org/10.21236/ada258324.

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Testor, Pierre, Thibaut Wagener, Anthony Bosse, Remy Asselot, Virginie Thierry, and Johannes Karstensen. Estimate of magnitude and drivers of regional carbon variability for both regions. EuroSea, 2022. http://dx.doi.org/10.3289/eurosea_d7.3.

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This deliverable provides an overview of EuroSea outcomes related to interior ocean carbon variability in deep convection areas in order to assess the linkage of these processes for the use in national climate action (NCA) plans delivered in the framework of the Paris Agreement. In summary, large-scale connectivity in the ocean does not allow clear delineation of patterns of regional carbon uptake across national boundaries, limiting an assessment of the Exclusive Economic Zones (EEZ) in light of NCA plans. This problem becomes already clear by a simple scale estimation: considering sluggish,

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