Bibliografías temáticas / Ocean circulation

Literatura académica sobre el tema "Ocean circulation"

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Publicado: 4 de junio de 2021
Última modificación: 29 de julio de 2024

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Artículos de revistas sobre el tema "Ocean circulation"

1

Cunningham, Stuart A. "Southern Ocean circulation". Archives of Natural History 32, n.º 2 (octubre de 2005): 265–80. http://dx.doi.org/10.3366/anh.2005.32.2.265.

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The Discovery Investigations of the 1930s provided a compelling description of the main elements of the Southern Ocean circulation. Over the intervening years, this has been extended to include ideas on ocean dynamics based on physical principles. In the modern description, the Southern Ocean has two main circulations that are intimately linked: a zonal (west-east) circumpolar circulation and a meridional (north-south) overturning circulation. The Antarctic Circumpolar Current transports around 140 million cubic metres per second west to east around Antarctica. This zonal circulation connects the Atlantic, Indian and Pacific Oceans, transferring and blending water masses and properties from one ocean basin to another. For the meridional circulation, a key feature is the ascent of waters from depths of around 2,000 metres north of the Antarctic Circumpolar Current to the surface south of the Current. In so doing, this circulation connects deep ocean layers directly to the atmosphere. The circumpolar zonal currents are not stable: meanders grow and separate, creating eddies and these eddies are critical to the dynamics of the Southern Ocean, linking the zonal circumpolar and meridional circulations. As a result of this connection, a global three-dimensional ocean circulation exists in which the Southern Ocean plays a central role in regulating the Earth's climate.
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2

Ferrari, Raffaele, Louis-Philippe Nadeau, David P. Marshall, Lesley C. Allison y Helen L. Johnson. "A Model of the Ocean Overturning Circulation with Two Closed Basins and a Reentrant Channel". Journal of Physical Oceanography 47, n.º 12 (diciembre de 2017): 2887–906. http://dx.doi.org/10.1175/jpo-d-16-0223.1.

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AbstractZonally averaged models of the ocean overturning circulation miss important zonal exchanges of waters between the Atlantic and Indo-Pacific Oceans. A two-layer, two-basin model that accounts for these exchanges is introduced and suggests that in the present-day climate the overturning circulation is best described as the combination of three circulations: an adiabatic overturning circulation in the Atlantic Ocean associated with transformation of intermediate to deep waters in the north, a diabatic overturning circulation in the Indo-Pacific Ocean associated with transformation of abyssal to deep waters by mixing, and an interbasin circulation that exchanges waters geostrophically between the two oceans through the Southern Ocean. These results are supported both by theoretical analysis of the two-layer, two-basin model and by numerical simulations of a three-dimensional ocean model.
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3

Smith, H. J. "OCEANS: Tracing Ocean Circulation". Science 288, n.º 5474 (23 de junio de 2000): 2097e—2099. http://dx.doi.org/10.1126/science.288.5474.2097e.

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Olson, Donald B. "Ocean Circulation". Marine Geology 103, n.º 1-3 (enero de 1992): 534. http://dx.doi.org/10.1016/0025-3227(92)90044-i.

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Bigg, Grant R. "Ocean circulation". Endeavour 14, n.º 2 (enero de 1990): 101. http://dx.doi.org/10.1016/0160-9327(90)90091-5.

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Jansen, Malte F., Wanying Kang, Edwin S. Kite y Yaoxuan Zeng. "Energetic Constraints on Ocean Circulations of Icy Ocean Worlds". Planetary Science Journal 4, n.º 6 (1 de junio de 2023): 117. http://dx.doi.org/10.3847/psj/acda95.

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Abstract Globally ice-covered oceans have been found on multiple moons in the solar system and may also have been a feature of Earth’s past. However, relatively little is understood about the dynamics of these ice-covered oceans, which affect not only the physical environment but also any potential life and its detectability. A number of studies have simulated the circulation of icy-world oceans, but have come to seemingly widely different conclusions. To better understand and narrow down these diverging results, we discuss the energetic constraints for the circulation on ice-covered oceans, focusing in particular on Snowball Earth, Europa, and Enceladus. The energy input that can drive ocean circulation on ice-covered bodies can be associated with heat and salt fluxes at the boundaries as well as ocean tides and librations. We show that heating from the solid core balanced by heat loss through the ice sheet can drive an ocean circulation, but the resulting flows would be relatively weak and strongly affected by rotation. Salt fluxes associated with freezing and melting at the ice sheet boundary are unlikely to energetically drive a circulation, although they can shape the large-scale circulation when combined with turbulent mixing. Ocean tides and librations may provide an energy source for such turbulence, but the magnitude of this energy source remains highly uncertain for the icy moons, which poses a major obstacle to predicting the ocean dynamics of icy worlds and remains an important topic for future research.
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Semtner, A. J. "Modeling Ocean Circulation". Science 269, n.º 5229 (8 de septiembre de 1995): 1379–85. http://dx.doi.org/10.1126/science.269.5229.1379.

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Ladant, Jean-Baptiste, Christopher J. Poulsen, Frédéric Fluteau, Clay R. Tabor, Kenneth G. MacLeod, Ellen E. Martin, Shannon J. Haynes y Masoud A. Rostami. "Paleogeographic controls on the evolution of Late Cretaceous ocean circulation". Climate of the Past 16, n.º 3 (9 de junio de 2020): 973–1006. http://dx.doi.org/10.5194/cp-16-973-2020.

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Abstract. Understanding of the role of ocean circulation on climate during the Late Cretaceous is contingent on the ability to reconstruct its modes and evolution. Geochemical proxies used to infer modes of past circulation provide conflicting interpretations for the reorganization of the ocean circulation through the Late Cretaceous. Here, we present climate model simulations of the Cenomanian (100.5–93.9 Ma) and Maastrichtian (72.1–66.1 Ma) stages of the Cretaceous with the CCSM4 earth system model. We focus on intermediate (500–1500 m) and deep (> 1500 m) ocean circulation and show that while there is continuous deep-water production in the southwestern Pacific, major circulation changes occur between the Cenomanian and Maastrichtian. Opening of the Atlantic and Southern Ocean, in particular, drives a transition from a mostly zonal circulation to enhanced meridional exchange. Using additional experiments to test the effect of deepening of major ocean gateways in the Maastrichtian, we demonstrate that the geometry of these gateways likely had a considerable impact on ocean circulation. We further compare simulated circulation results with compilations of εNd records and show that simulated changes in Late Cretaceous ocean circulation are reasonably consistent with proxy-based inferences. In our simulations, consistency with the geologic history of major ocean gateways and absence of shift in areas of deep-water formation suggest that Late Cretaceous trends in εNd values in the Atlantic and southern Indian oceans were caused by the subsidence of volcanic provinces and opening of the Atlantic and Southern oceans rather than changes in deep-water formation areas and/or reversal of deep-water fluxes. However, the complexity in interpreting Late Cretaceous εNd values underscores the need for new records as well as specific εNd modeling to better discriminate between the various plausible theories of ocean circulation change during this period.
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9

Wu, Yang, Xiaoming Zhai y Zhaomin Wang. "Impact of Synoptic Atmospheric Forcing on the Mean Ocean Circulation". Journal of Climate 29, n.º 16 (27 de julio de 2016): 5709–24. http://dx.doi.org/10.1175/jcli-d-15-0819.1.

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Abstract The impact of synoptic atmospheric forcing on the mean ocean circulation is investigated by comparing simulations of a global eddy-permitting ocean–sea ice model forced with and without synoptic atmospheric phenomena. Consistent with previous studies, transient atmospheric motions such as weather systems are found to contribute significantly to the time-mean wind stress and surface heat loss at mid- and high latitudes owing to the nonlinear nature of air–sea turbulent fluxes. Including synoptic atmospheric forcing in the model has led to a number of significant changes. For example, wind power input to the ocean increases by about 50%, which subsequently leads to a similar percentage increase in global eddy kinetic energy. The wind-driven subtropical gyre circulations are strengthened by about 10%–15%, whereas even greater increases in gyre strength are found in the subpolar oceans. Deep convection in the northern North Atlantic becomes significantly more vigorous, which in turn leads to an increase in the Atlantic meridional overturning circulation (AMOC) by as much as 55%. As a result of the strengthened horizontal gyre circulations and the AMOC, the maximum global northward heat transport increases by almost 50%. Results from this study show that synoptic atmospheric phenomena such as weather systems play a vital role in driving the global ocean circulation and heat transport, and therefore should be properly accounted for in paleo- and future climate studies.
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Stanton, B. R. "Ocean circulation and ocean-atmosphere exchanges". Climatic Change 18, n.º 2-3 (abril de 1991): 175–94. http://dx.doi.org/10.1007/bf00138996.

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Tesis sobre el tema "Ocean circulation"

1

Nelkien, Haim. "Thermally driven circulation". Woods Hole, Mass. : Woods Hole Oceanographic Institution, 1987. http://hdl.handle.net/1912/3152.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric and Planetary Sciences, and (Ph. D.)--Woods Hole Oceanographic Institution, 1987.
Cover title. Includes bibliographical references (leaves 181-186).
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2

Jones, Matthew Stephen. "Satellite techniques for studying ocean circulation". Thesis, University College London (University of London), 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.568439.

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Noble, Taryn Lee. "Southern Ocean circulation and sediment sourcing". Thesis, University of Cambridge, 2012. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.610485.

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Villanoy, Cesar Laurel. "Modification of the throughflow water properties in the Indonesian seas". Thesis, The University of Sydney, 1993. https://hdl.handle.net/2123/26591.

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Vertical mixing in the Indonesian Seas has been considered to be responsible for the apparent freshness of the throughflow when 'it enters the Indian Down. A three-dimensional primitive equation numerical model of the Indonesian Seas forced with a prescribed throughflow, transport consisting of North Pacific waters, is used to determine local dynamic processes which may modify the characteristics of the throughflow properties. The lack of long-term current measurements in the Indonesian Seas presents some difficulties in determining the certainty of the derived velocity fields. As an alternative, the model temperature and salinity fields are compared to observed hydrographic data which has a relatively better coverage throughout the Indonesian Seas. A 15 Sv net transport through the Indonesian Seas is suggested based on the model’s more realistic reproduction of the hydrographic structure compared to a throughflow with a smaller magnitude. A pure North Pacific source for the throughflow is also not capable of producing the salinity structure in the Banda Sea as suggested by previous studies and the required amount of salt to fit the model salinity structure with observations in the Banda Sea is estimated to be 3.3x10‘3 kg. Most of the throughflow transport occurs in western boundary flows and is largely topographically controlled. The separation of an upper and lower layer circulation pattern is controlled by the depth of the sill in Makassar Strait. Vertical excursions in the vicinity of this sill seen level of the in model results coincide upper salinity maximum with regions where are found. Seasonal large horizontal gradients at the upwelling and longer residence times due to weaker flows in the Banda Sea results in a more effective mixing of the already weakened salinity structure of the waters from Makassar Strait/Flores Sea. Net heat and freshwater flux estimates also reveal significant departures at 200 up to 100 m between the Pacific inflow and Indian outflow, suggesting the considerable redistribution of heat and salt in the Indonesian Seas.
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Bean, Mark Shawn. "Modelling the thermohaline circulation". Thesis, University of Southampton, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.242716.

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Bermejo-Bermejo, Rodolfo. "A finite element model of ocean circulation". Thesis, University of British Columbia, 1986. http://hdl.handle.net/2429/26166.

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Preliminary results of a two-layer quasi-geostrophic box model of a wind-driven ocean are presented. The new aspects of this work in relation with conventional eddy models are a finite element formulation of the quasi-geostrophic equations and the use of no-slip boundary condition on the horizontal solid boundaries. In contrast to eddy resolving models that utilize free-slip boundary conditions our results suggest that the obtention of ocean eddies with the no-slip constraints requires a more restricted range of parameters, in particular much lower horizontal eddy viscosity eddy coefficients AH and higher Froude numbers F₁ and F₂. We show explicitly that a given range of parameters, which is eddy generating when the free-slip boundary condition is used, leads to a quasi-laminar flow in both, upper and lower, layers. An analytical model to interpret the numerical results is put forth. It is an extension of an earlier model of Ierley and Young (1983) in that the relative vorticity terms are of primary importance for the dynamics. Thus, it is shown that the boundary layer dynamics is active in the interior of the second layer, and it can be concluded from our method that for given F₁ and F₂ such that the lower layer geostrophic contours are closed, to the existence of the western boundary layer will prevent the homogenization of the potential vorticity so long as AH is large enough to stabilize the northwestern undulations of the flow.
Science, Faculty of
Earth, Ocean and Atmospheric Sciences, Department of
Graduate
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7

Mohammad, Rezwan. "Some aspects of the Atlantic ocean circulation". Doctoral thesis, Stockholm : Department of Meteorology, Stockholm University, 2005. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-473.

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McAufield, Ewa Katarzyna. "Lagrangian study of the Southern Ocean circulation". Thesis, University of Cambridge, 2019. https://www.repository.cam.ac.uk/handle/1810/288743.

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The Southern Ocean is an important region for the sequestration of heat, carbon dioxide and other tracers. The Southern Ocean circulation is typically described in a circumpolarly averaged sense as a Meridional Overturning Circulation (MOC), but the detailed 3-D pathways that make up this circulation remain poorly understood. We use Lagrangian particle trajectories, obtained from eddy permitting numerical models, to map out and quantify different aspects of the 3-D circulation. We first introduce various definitions used to quantify efficient export from the Antarctic Circumpolar Current (ACC) to the subtropical gyres. Using these definitions, we show that the permanent northward export varies by water mass and occurs in localised regions; with 11 key pathways identified. We then examine the dynamics setting the location and efficiency of the identified pathways, which includes the investigation of the role of diapycnal mixing and the impact of short and long time variability in the flow. Although we show that the flow of particles in the 3-D model is predominantly isopycnal, we find that particles that are forced to remain on isopycnals lead to approx. 60% lower export (mainly via three pathways) than identical releases where the diapycnal component of advection is included. Enhanced upward mixing near rough topography, and downward mixing in the southeast Pacific, were shown to be mostly responsible for the export. In addition, we show that most of the export pathways are mainly influenced by timescales from 90 days to 20 years, which suggests that mesoscale eddies are not the leading-order importance in the northward export from the ACC to the subtropical gyres. However, we also find that mesoscale eddies and the mean-ACC flow play a significant role in setting the export from the ACC in some pathways. These results highlight the role of temporal variability and vertical transport in enhancing the northward flow from the ACC by allowing transport across barotropic streamlines and onto more efficiently exporting isopycnals. In addition, the asymmetrical response of the studied quantities emphasises the importance of the three dimensions in understanding the dynamics driving the overturning circulation. We also demonstrated that the annually repeating velocity fields, which are commonly used for trajectory calculations, increase the diapycnal transport of particles and as a consequence, increase the overall 20-year northward export from the ACC by approx. 10%. In the study of the meridional overturning circulation, we diagnose the geographical distribution of the streamwise averaged diffusivity calculated from meridional displacements of the Lagrangian particles. We examine streamwise averaging using both latitude and equivalent latitude and argue that the latter gives a more useful measure. Reconciling tracer and particle horizontal diffusivities, we show that in the ACC, the average diffusivity peaks between 1500m and 2500m with an average value of 1500 m$^{2}$/s and that it is highest near the topographic features. We compare the exact diffusivity and its approximation to show that an assumption of time homogeneity does not hold and therefore that standard expressions for diffusivity that assume time homogeneity are of limited usefulness. Finally, we use the calculated trajectories to provide a streamwise averaged 2-D advection-diffusion model of the Southern Ocean MOC and then examine the extent to which this 2-D model can capture the overall effect of the actual 3-D transport.
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Wang, Xiaoli Ph D. Massachusetts Institute of Technology. "Global thermohaline circulation and ocean-atmosphere coupling". Thesis, Massachusetts Institute of Technology, 1997. http://hdl.handle.net/1721.1/58357.

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Li, Hui. "Numerical modeling of South China Sea circulation /". View abstract or full-text, 2005. http://library.ust.hk/cgi/db/thesis.pl?AMCE%202005%20LI.

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Libros sobre el tema "Ocean circulation"

1

Angela, Colling y Open University. Oceanography Course Team., eds. Ocean circulation. 2a ed. Boston: Butterworth Heinemann, in association with the Open University, 2001.

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Open University. Oceanography Course Team., ed. Ocean circulation. Oxford, England: Pergamon Press, 1989.

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Pedlosky, Joseph. Ocean Circulation Theory. Berlin, Heidelberg: Springer Berlin Heidelberg, 1996. http://dx.doi.org/10.1007/978-3-662-03204-6.

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Pedlosky, Joseph. Ocean circulation theory. Berlin: Springer, 1996.

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A, Beckmann, ed. Numerical ocean circulation modeling. London: Imperial College Press, 1999.

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Nelkien, Haim. Thermally driven circulation. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1987.

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Marchuk, G. I. y A. S. Sarkisyan. Mathematical Modelling of Ocean Circulation. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-61376-0.

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Abarbanel, Henry D. I. y W. R. Young, eds. General Circulation of the Ocean. New York, NY: Springer New York, 1987. http://dx.doi.org/10.1007/978-1-4612-4636-7.

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I, Abarbanel H. D. y Young W. R. 1955-, eds. General circulation of the ocean. New York: Springer-Verlag, 1987.

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Wunsch, Carl. The ocean circulation inverse problem. Cambridge: Cambridge University Press, 1996.

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Capítulos de libros sobre el tema "Ocean circulation"

1

Hastenrath, Stefan. "Ocean Circulation". En Climate and circulation of the tropics, 37–71. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5388-8_4.

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Hastenrath, Stefan. "Ocean Circulation". En Climate Dynamics of the Tropics, 37–77. Dordrecht: Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3156-8_4.

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Thompson, Andrew F. y Stefan Rahmstorf. "Ocean circulation". En Surface Ocean—Lower Atmosphere Processes, 99–118. Washington, D. C.: American Geophysical Union, 2009. http://dx.doi.org/10.1029/2008gm000842.

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Pedlosky, Joseph. "Abyssal Circulation". En Ocean Circulation Theory, 379–450. Berlin, Heidelberg: Springer Berlin Heidelberg, 1996. http://dx.doi.org/10.1007/978-3-662-03204-6_7.

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Bryan, Kirk. "Modeling Ocean Circulation". En Physical Oceanography, 29–44. New York, NY: Springer New York, 2006. http://dx.doi.org/10.1007/0-387-33152-2_3.

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Tolmazin, David. "Deep-ocean circulation". En Elements of Dynamic Oceanography, 128–51. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-4856-3_7.

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Olbers, Dirk, Jürgen Willebrand y Carsten Eden. "The Wind-Driven Circulation". En Ocean Dynamics, 445–86. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-23450-7_14.

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Pedlosky, Joseph. "Sverdrup Theory". En Ocean Circulation Theory, 1–23. Berlin, Heidelberg: Springer Berlin Heidelberg, 1996. http://dx.doi.org/10.1007/978-3-662-03204-6_1.

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Pedlosky, Joseph. "Homogeneous Models of the Ocean Circulation". En Ocean Circulation Theory, 25–92. Berlin, Heidelberg: Springer Berlin Heidelberg, 1996. http://dx.doi.org/10.1007/978-3-662-03204-6_2.

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Pedlosky, Joseph. "Vertical Structure: Baroclinic Quasi-Geostrophic Models". En Ocean Circulation Theory, 93–170. Berlin, Heidelberg: Springer Berlin Heidelberg, 1996. http://dx.doi.org/10.1007/978-3-662-03204-6_3.

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Actas de conferencias sobre el tema "Ocean circulation"

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Poon, Ying-Keung, Bob Stein y Laura Peters. "Newport Bay Circulation Improvement Study". En California and the World Ocean 2002. Reston, VA: American Society of Civil Engineers, 2005. http://dx.doi.org/10.1061/40761(175)114.

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Haynes, Shannon J., Kenneth G. MacLeod y Ellen E. Martin. "PACIFIC OCEAN CIRCULATION DURING THE LATE CRETACEOUS". En GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-286820.

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Tsubogo, Koichi, Takahiro Yasuhara y Mitsunori Ouchi. "Development of a New Analysis Method for Wastewater Purification Circulation Equipment". En 2018 OCEANS - MTS/IEEE Kobe Techno-Ocean (OTO). IEEE, 2018. http://dx.doi.org/10.1109/oceanskobe.2018.8559098.

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Talley, Lynne D., Rana Fine, Rick Lumpkin, Nikolai Maximenko y Rosemary Morrow. "Surface Ventilation and Circulation". En OceanObs'09: Sustained Ocean Observations and Information for Society. European Space Agency, 2010. http://dx.doi.org/10.5270/oceanobs09.pp.38.

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Barbelet, Thea C., Bethany Royce, Charlotte Heo, Molly O. Patterson y Jeffrey T. Pietras. "PLIOCENE DEEP OCEAN CIRCULATION IN THE SOUTHWEST PACIFIC". En Joint 72nd Annual Southeastern/ 58th Annual Northeastern Section Meeting - 2023. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023se-386043.

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DeRose, L., K. Gallivan y E. Gallopoulos. "Experiments with an ocean circulation model on CEDAR". En the 6th international conference. New York, New York, USA: ACM Press, 1992. http://dx.doi.org/10.1145/143369.143440.

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Wang, Ping, Daniel S. Katz y Yi Chao. "Optimization of a parallel ocean general circulation model". En the 1997 ACM/IEEE conference. New York, New York, USA: ACM Press, 1997. http://dx.doi.org/10.1145/509593.509618.

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Altuntas, Alper y John Baugh. "Verifying Concurrency in an Adaptive Ocean Circulation Model". En SC '17: The International Conference for High Performance Computing, Networking, Storage and Analysis. New York, NY, USA: ACM, 2017. http://dx.doi.org/10.1145/3145344.3145346.

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Sallee, Jean baptiste. "Southern Ocean dynamic, circulation, and role on climate". En Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.12208.

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Barbelet, Thea, Bethany Royce, Charlotte Heo, Molly O. Patterson y Jeffrey Pietras. "PLIOCENE DEEP OCEAN CIRCULATION IN THE SOUTHWEST PACIFIC". En GSA Connects 2023 Meeting in Pittsburgh, Pennsylvania. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023am-390618.

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Informes sobre el tema "Ocean circulation"

1

Niiler, Peter. Upper Ocean Circulation. Fort Belvoir, VA: Defense Technical Information Center, octubre de 1997. http://dx.doi.org/10.21236/ada330409.

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Whitehead, John A. Laboratory Models of Ocean Circulation. Fort Belvoir, VA: Defense Technical Information Center, junio de 1997. http://dx.doi.org/10.21236/ada326697.

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Centurioni, Luca. Planning Joint Vietnam Ocean Circulation Studies. Fort Belvoir, VA: Defense Technical Information Center, septiembre de 2012. http://dx.doi.org/10.21236/ada572166.

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Centurioni, Luca. Planning Joint Vietnam Ocean Circulation Studies. Fort Belvoir, VA: Defense Technical Information Center, septiembre de 2013. http://dx.doi.org/10.21236/ada601135.

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Duffy, P. B. y K. C. Caldeira. Global warming and changes in ocean circulation. Office of Scientific and Technical Information (OSTI), febrero de 1998. http://dx.doi.org/10.2172/641334.

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Holloway, Greg y William Merryfield. Statistical Prediction of Ocean Circulation and Trajectories. Fort Belvoir, VA: Defense Technical Information Center, septiembre de 1999. http://dx.doi.org/10.21236/ada630969.

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Iskandarani, Mohamed, Omar Knio, Ashwanth Srinivasan y William C. Thacker. Quantifying Prediction Fidelity in Ocean Circulation Models. Fort Belvoir, VA: Defense Technical Information Center, septiembre de 2012. http://dx.doi.org/10.21236/ada590693.

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Iskandarani, Mohamed, Omar Knio, Ashwanth Srinivasan y William C. Thacker. Quantifying Prediction Fidelity in Ocean Circulation Models. Fort Belvoir, VA: Defense Technical Information Center, septiembre de 2013. http://dx.doi.org/10.21236/ada601423.

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Poulain, Pierre-Marie. Coastal Ocean Circulation Experiment off Senegal (COCES). Fort Belvoir, VA: Defense Technical Information Center, septiembre de 2011. http://dx.doi.org/10.21236/ada557112.

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Holloway, Greg y William Merryfield. Statistical Prediction of Ocean Circulation and Trajectories. Fort Belvoir, VA: Defense Technical Information Center, agosto de 2001. http://dx.doi.org/10.21236/ada625413.

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