Gotowe bibliografie tematyczne / The Southern Ocean

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Gotowa bibliografia na temat „The Southern Ocean”

Autor: Grafiati

Data publikacji: 21 września 2024

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Artykuły w czasopismach na temat "The Southern Ocean"

Cunningham, Stuart A. "Southern Ocean circulation". Archives of Natural History 32, nr 2 (październik 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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Smith, H. J. "OCEANS: Carbonate Deficit in the Southern Ocean". Science 289, nr 5480 (4.08.2000): 697b—697. http://dx.doi.org/10.1126/science.289.5480.697b.

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Smirnov, A., B. N. Holben, D. M. Giles, I. Slutsker, N. T. O'Neill, T. F. Eck, A. Macke i in. "Maritime Aerosol Network as a component of AERONET – first results and comparison with global aerosol models and satellite retrievals". Atmospheric Measurement Techniques Discussions 4, nr 1 (8.01.2011): 1–32. http://dx.doi.org/10.5194/amtd-4-1-2011.

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Abstract. The Maritime Aerosol Network (MAN) has been collecting data over the oceans since November 2006. Over 80 cruises were completed through early 2010 with deployments continuing. Measurements areas included various parts of the Atlantic Ocean, the Northern and Southern Pacific Ocean, the South Indian Ocean, the Southern Ocean, the Arctic Ocean and inland seas. MAN deploys Microtops hand-held sunphotometers and utilizes a calibration procedure and data processing traceable to AERONET. Data collection included areas that previously had no aerosol optical depth (AOD) coverage at all, particularly vast areas of the Southern Ocean. The MAN data archive provides a valuable resource for aerosol studies in maritime environments. In the current paper we present results of AOD measurements over the oceans, and make a comparison with satellite AOD retrievals and model simulations.

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Smirnov, A., B. N. Holben, D. M. Giles, I. Slutsker, N. T. O'Neill, T. F. Eck, A. Macke i in. "Maritime aerosol network as a component of AERONET – first results and comparison with global aerosol models and satellite retrievals". Atmospheric Measurement Techniques 4, nr 3 (21.03.2011): 583–97. http://dx.doi.org/10.5194/amt-4-583-2011.

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Abstract. The Maritime Aerosol Network (MAN) has been collecting data over the oceans since November 2006. Over 80 cruises were completed through early 2010 with deployments continuing. Measurement areas included various parts of the Atlantic Ocean, the Northern and Southern Pacific Ocean, the South Indian Ocean, the Southern Ocean, the Arctic Ocean and inland seas. MAN deploys Microtops hand-held sunphotometers and utilizes a calibration procedure and data processing traceable to AERONET. Data collection included areas that previously had no aerosol optical depth (AOD) coverage at all, particularly vast areas of the Southern Ocean. The MAN data archive provides a valuable resource for aerosol studies in maritime environments. In the current paper we present results of AOD measurements over the oceans, and make a comparison with satellite AOD retrievals and model simulations.

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Heimdal, Thea H., Galen A. McKinley, Adrienne J. Sutton, Amanda R. Fay i Lucas Gloege. "Assessing improvements in global ocean pCO₂ machine learning reconstructions with Southern Ocean autonomous sampling". Biogeosciences 21, nr 8 (30.04.2024): 2159–76. http://dx.doi.org/10.5194/bg-21-2159-2024.

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Abstract. The Southern Ocean plays an important role in the exchange of carbon between the atmosphere and oceans and is a critical region for the ocean uptake of anthropogenic CO2. However, estimates of the Southern Ocean air–sea CO2 flux are highly uncertain due to limited data coverage. Increased sampling in winter and across meridional gradients in the Southern Ocean may improve machine learning (ML) reconstructions of global surface ocean pCO2. Here, we use a large ensemble test bed (LET) of Earth system models and the “pCO2-Residual” reconstruction method to assess improvements in pCO2 reconstruction fidelity that could be achieved with additional autonomous sampling in the Southern Ocean added to existing Surface Ocean CO2 Atlas (SOCAT) observations. The LET allows for a robust evaluation of the skill of pCO2 reconstructions in space and time through comparison to “model truth”. With only SOCAT sampling, Southern Ocean and global pCO2 are overestimated, and thus the ocean carbon sink is underestimated. Incorporating uncrewed surface vehicle (USV) sampling increases the spatial and seasonal coverage of observations within the Southern Ocean, leading to a decrease in the overestimation of pCO2. A modest number of additional observations in Southern Hemisphere winter and across meridional gradients in the Southern Ocean leads to an improvement in reconstruction bias and root-mean-squared error (RMSE) of as much as 86 % and 16 %, respectively, as compared to SOCAT sampling alone. Lastly, the large decadal variability of air–sea CO2 fluxes shown by SOCAT-only sampling may be partially attributable to undersampling of the Southern Ocean.

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Keane, James Tuttle. "Southern Ocean mixing". Nature Geoscience 10, nr 11 (30.10.2017): 805. http://dx.doi.org/10.1038/ngeo3057.

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Mantoura, Samia. "Southern Ocean saturated". Nature Climate Change 1, nr 707 (18.06.2007): 18. http://dx.doi.org/10.1038/climate.2007.15.

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Gordon, Arnold L. "Southern Ocean polynya". Nature Climate Change 4, nr 4 (26.03.2014): 249–50. http://dx.doi.org/10.1038/nclimate2179.

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Rae, James W. B., i Wally Broecker. "What fraction of the Pacific and Indian oceans' deep water is formed in the Southern Ocean?" Biogeosciences 15, nr 12 (21.06.2018): 3779–94. http://dx.doi.org/10.5194/bg-15-3779-2018.

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Abstract. In this contribution we explore constraints on the fractions of deep water present in the Indian and Pacific oceans which originated in the northern Atlantic and in the Southern Ocean. Based on PO4* we show that if ventilated Antarctic shelf waters characterize the Southern contribution, then the proportions could be close to 50–50. If instead a Southern Ocean bottom water value is used, the Southern contribution is increased to 75 %. While this larger estimate may best characterize the volume of water entering the Indo-Pacific from the Southern Ocean, it contains a significant portion of entrained northern water. We also note that ventilation may be highly tracer dependent: for instance Southern Ocean waters may contribute only 35 % of the deep radiocarbon budget, even if their volumetric contribution is 75 %. In our estimation, the most promising approaches involve using CFC-11 to constrain the amount of deep water formed in the Southern Ocean. Finally, we highlight the broad utility of PO4* as a tracer of deep water masses, including descending plumes of Antarctic Bottom Water and large-scale patterns of deep ocean mixing, and as a tracer of the efficiency of the biological pump.

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Kay, Jennifer E., Casey Wall, Vineel Yettella, Brian Medeiros, Cecile Hannay, Peter Caldwell i Cecilia Bitz. "Global Climate Impacts of Fixing the Southern Ocean Shortwave Radiation Bias in the Community Earth System Model (CESM)". Journal of Climate 29, nr 12 (10.06.2016): 4617–36. http://dx.doi.org/10.1175/jcli-d-15-0358.1.

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Abstract A large, long-standing, and pervasive climate model bias is excessive absorbed shortwave radiation (ASR) over the midlatitude oceans, especially the Southern Ocean. This study investigates both the underlying mechanisms for and climate impacts of this bias within the Community Earth System Model, version 1, with the Community Atmosphere Model, version 5 [CESM1(CAM5)]. Excessive Southern Ocean ASR in CESM1(CAM5) results in part because low-level clouds contain insufficient amounts of supercooled liquid. In a present-day atmosphere-only run, an observationally motivated modification to the shallow convection detrainment increases supercooled cloud liquid, brightens low-level clouds, and substantially reduces the Southern Ocean ASR bias. Tuning to maintain global energy balance enables reduction of a compensating tropical ASR bias. In the resulting preindustrial fully coupled run with a brighter Southern Ocean and dimmer tropics, the Southern Ocean cools and the tropics warm. As a result of the enhanced meridional temperature gradient, poleward heat transport increases in both hemispheres (especially the Southern Hemisphere), and the Southern Hemisphere atmospheric jet strengthens. Because northward cross-equatorial heat transport reductions occur primarily in the ocean (80%), not the atmosphere (20%), a proposed atmospheric teleconnection linking Southern Ocean ASR bias reduction and cooling with northward shifts in tropical precipitation has little impact. In summary, observationally motivated supercooled liquid water increases in shallow convective clouds enable large reductions in long-standing climate model shortwave radiation biases. Of relevance to both model bias reduction and climate dynamics, quantifying the influence of Southern Ocean cooling on tropical precipitation requires a model with dynamic ocean heat transport.

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Rozprawy doktorskie na temat "The Southern Ocean"

Flaviani, Flavia. "Microbial biodiversity in the southern Indian Ocean and Southern Ocean". Doctoral thesis, University of Cape Town, 2017. http://hdl.handle.net/11427/25058.

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The multi-phylotype and ecologically important community of microbes in aquatic environments ranges from the numerically dominant viruses to the diverse climate-change regulating phytoplankton. Recent advances in next generation sequencing are starting to reveal the true diversity and biological complexity of this previously invisible component of Earth's hydrosphere. An increased awareness of this microbiome's importance has led to the rise of microbial studies with marine environmental samples being collected and sequenced daily around the globe. Despite the rapid advancement in knowledge of marine microbial diversity, technical difficulties have constrained the ability to perform basin wide physical and chemical oceanographic assessments in tandem with microbiological screening with the majority of studies only looking at a single component of the microbial community. In this study the full microbial diversity, from viruses to protists, was characterised within the southern Indian Ocean and the Southern Ocean from a small volume of seawater collected using the same CTD equipment used by oceanographers. Throughout this study it will be demonstrated how this small volume is sufficient to describe the core microbial taxa in the marine environment. The application of a bespoke bioinformatics pipeline, integrated with sequencing replication, improved the description of the dominant core microbiome whilst removing OTUs present due to PCR and sequencing artefacts thereby improving the accurate description of rare phylotypes. Analyses confirmed the dominance of Cyanobacteria, Alphaproteobacteria and Gammaproteobacteria in the pelagic prokaryotic microbiome, while the Stramenopiles-Alveolata-Rhizaria (SAR) cluster dominates the eukaryotic microbiome. A decrease in the SAR community will be reported for the Southern Ocean with a concomitant increase in the haptophyte community. Whilst the virome confirmed the dominance of tailed phages and giant viruses across all stations, there was a significant variation caudoviruses and Nucleocytoplasmic Large DNA viruses (NCLDV) across defined biogeographical boundaries. The described method will allow the characterisation of the microbial biodiversity as well as future integration with oceanographic data with a much reduced sampling effort. The characterisation of the whole microbial community from a single water sample will improve the understanding of microbial interactions and represent a step towards in the inclusion of viruses into biogeochemical models.

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Bednarsek, Nina. "Vulnerability of Southern ocean pteropods to anthropogenic ocean acidification". Thesis, University of East Anglia, 2010. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.533722.

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Murphy, Darryl Guy. "Rossby waves in the Southern Ocean". Thesis, University of Exeter, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.303178.

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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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Giannelli, Virginia. "Dissolved organic matter in the Southern Ocean". Thesis, Bangor University, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.247270.

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Grigorov, Ivo. "Southern Ocean palaeoceanography from Thalassiothrix antarctica deposits". Thesis, University of Southampton, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.413434.

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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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Damerell, Gillian. "Aspects of southern ocean transport and mixing". Thesis, University of East Anglia, 2012. https://ueaeprints.uea.ac.uk/45642/.

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Understanding and quantifying the circulation of the oceans and the driving mechanisms thereof is an important step in developing models which can accurately predict future climate change. In particular, model studies have shown that the spatial variability of diapycnal diffusivity, which represents the rate at which deep water returns to shallower depths by means of turbulent diapycnal mixing, is a critical factor controlling the strength and structure of the circulation. Efforts are therefore ongoing to measure diffusivity as extensively as possible, but temporal variability in diffusivity has not been widely addressed. Results from three Southern Ocean studies are presented in this thesis. Firstly, a high resolution hydrographic survey carried out on the northern flank of the Kerguelen Plateau identifies a complex meandering current system carrying a total eastward volume transport of 174 ± 22 Sv, mostly associated with the blended Subtropical Front/Subantarctic Front. Significant water mass transformation across isopycnals is not required to balance the budgets in this region. Secondly, results are presented which cast doubt on the advisability of using density profiles acquired using Conductivity-Temperature-Depth instruments to estimate diapycnal diffusivity (an attractive proposition due to low cost and widespread data availability) in areas of weak stratification such as the Southern Ocean, because the noise characteristics of the data result in inaccurate diffusivity estimates. Finally, a method is developed for estimating diffusivity from profiles of velocity shear acquired by moored acoustic Doppler current profilers. An 18-month time series of diffusivity estimates is derived with a median of 3.3 × 10−4 m2 s−1 and a range of 0.5 × 10−4 m2 s−1 to 57 × 10−4 m2 s−1. There is no significant signal at annual or semiannual periods, but there is evidence of signals at periods of approximately fourteen days (likely due to the spring-neaps tidal cycle), and at periods of 3.8 and 2.6 days most likely due to topographically-trapped waves propagating around the local seamount. More widespread application of this method would allow for an assessment of natural climate variability in diapycnal diffusivity.

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Bell, James Benjamin. "Sedimented chemosynthetic ecosystems of the Southern Ocean". Thesis, University of Leeds, 2017. http://etheses.whiterose.ac.uk/17252/.

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Sedimented chemosynthetic ecosystems (SCEs) are complex seafloor environments that combine several potential sources of organic matter. Their physical similarity to the vast soft-sediment habitats on the seafloor means that they can be inhabited by a diverse range of more ubiquitous fauna. This is in stark contrast to ecosystems such as hard substratum hydrothermal vents, which are typically almost totally dominated by a few specialist species. Another characteristic of these ecosystems is that they exhibit diffuse environmental gradients, relating to chemosynthetic production potential and environmental toxicity. Consequently, it is often difficult to determine their spatial extent, and the ecological responses along such gradients. A central theme of the research presented in this thesis has been to determine the role of habitat-structuring processes at two contrasting SCEs in the Atlantic sector of the Southern Ocean. I demonstrate that these environments elicit significant changes in assemblage structure, trophodynamics and carbon cycles. Chemosynthetic activity generally did not constitute a major proportion of the diet of any assemblage, even at the most hydrothermally active sites, but was detected in macrofaunal food webs at very surprising distances (~ 100km) from the (known) sites of active venting. This research illustrates and examines the impacts that these environments can have upon a range of ecological processes and raises questions about the full extent and significance of chemosynthetic organic matter production in seafloor ecosystems.

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Patoux, Jérôme. "Frontal wave development over the Southern Ocean /". Thesis, Connect to this title online; UW restricted, 2003. http://hdl.handle.net/1773/10067.

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Książki na temat "The Southern Ocean"

Oachs, Emily Rose. Southern Ocean. Minneapolis, MN: Bellwether Media, Inc., 2016.

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Spilsbury, Louise. Southern ocean. London: Raintree, a Capstone Company, 2015.

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Gonzales, Doreen. The stormy southern ocean. Berkeley Heights, NJ: Enslow Publishers, Inc., 2013.

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Mikhalev, Yuri. Whales of the Southern Ocean. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-29252-2.

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Smith, J. M. B. Specks in the southern ocean. Armidale, N.S.W., Australia: Dept. of Geography and Planning, University of New England, 1986.

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1949-, Gon O., i Heemstra Phillip C, red. Fishes of the southern ocean. Grahamstown, South Africa: J.L.B. Smith Institute of Ichthyology, 1990.

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Hislop, Cheryle. Protecting the Antarctic and Southern Ocean. Hobart: University of Tasmania Law School Press, 2004.

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1926-, El-Sayed Sayed Z., i BIOMASS Colloquium (1991 : Bremerhaven, Germany), red. Southern Ocean ecology: The BIOMASS perspective. Cambridge [England]: Cambridge University Press, 1994.

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Jürgen, Olbers Dirk, Alfred-Wegener-Institut für Polar-und Meeresforschung i Arkticheskiĭ i antarkticheskiĭ nauchno-issledovatelʹskiĭ institut (Saint Petersburg, Russia), red. Hydrographic atlas of the southern ocean. Bremerhaven: Alfred Wegener Institute, 1992.

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Hoflehner, Josef. Southern Ocean: Photographs of a journey. Wels, Austria: J. Hoflehner, 2002.

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Części książek na temat "The Southern Ocean"

Miller, Denzil G. M. "Southern Ocean Fisheries". W Exploring the Last Continent, 429–61. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-18947-5_21.

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Williams, Michael J. M. "The Southern Ocean". W Exploring the Last Continent, 115–27. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-18947-5_7.

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Gille, Sarah T., i Michael P. Meredith. "The Southern Ocean". W Satellite Altimetry over Oceans and Land Surfaces, 297–314. Boca Raton, FL : Taylor & Francis, 2017.: CRC Press, 2017. http://dx.doi.org/10.1201/9781315151779-9.

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Rothwell, Donald R. "The Southern Ocean". W The GeoJournal Library, 297–311. Dordrecht: Springer Netherlands, 2004. http://dx.doi.org/10.1007/978-1-4020-2780-2_16.

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Andrews, Sean A. G. "The Southern Ocean". W Naval Constabulary Operations and Fisheries Governance, 153–76. London: Routledge, 2024. http://dx.doi.org/10.4324/9781032641928-7.

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Vincent, Dayton G. "Pacific Ocean". W Meteorology of the Southern Hemisphere, 101–17. Boston, MA: American Meteorological Society, 1998. http://dx.doi.org/10.1007/978-1-935704-10-2_4.

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Olbers, Dirk, Jürgen Willebrand i Carsten Eden. "The Circulation of the Southern Ocean". W Ocean Dynamics, 561–628. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-23450-7_16.

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Aguirre, Luis. "The Southern Andes". W The Ocean Basins and Margins, 265–376. Boston, MA: Springer US, 1985. http://dx.doi.org/10.1007/978-1-4613-2351-8_7.

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Brandt, A., C. De Broyer, B. Ebbe, K. E. Ellingsen, A. J. Gooday, D. Janussen, S. Kaiser i in. "Southern Ocean Deep Benthic Biodiversity". W Antarctic Ecosystems, 291–334. Chichester, UK: John Wiley & Sons, Ltd, 2012. http://dx.doi.org/10.1002/9781444347241.ch10.

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Yi, Yuchan, C. K. Shum, Ole Andersen i Per Knudsen. "Extreme Southern Ocean Tide Modeling". W International Association of Geodesy Symposia, 225–29. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-642-18861-9_27.

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Streszczenia konferencji na temat "The Southern Ocean"

Rintoul, S. R., S. R. Rintoul, S. R. Rintoul, S. R. Rintoul, S. R. Rintoul, S. R. Rintoul, S. R. Rintoul i in. "Southern Ocean Observing System (SOOS): Rationale and Strategy for Sustained Observations of the Southern Ocean". W OceanObs'09: Sustained Ocean Observations and Information for Society. European Space Agency, 2010. http://dx.doi.org/10.5270/oceanobs09.cwp.74.

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Young, Ian R. "The Wave Climate of the Southern Ocean". W ASME 2019 38th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2019. http://dx.doi.org/10.1115/omae2019-95168.

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Abstract An analysis of the wind and wave climate of the Southern Ocean is provided based on a combination of more than 30-years of satellite altimeter data plus insitu buoy measurements at 5 locations in the Southern Ocean. The analysis shows that the Southern Ocean is a unique environment where there are strong winds year-round which blow over exceptionally long distances. This unique situation results in spectral forms which are not seen in any other oceanic basin.

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Terrill, E., S. Peck, L. Hazard, R. E. Davis, P. DiGiacomo, B. Jones, C. Keen i in. "The Southern California Coastal Ocean Observing System". W OCEANS 2006. IEEE, 2006. http://dx.doi.org/10.1109/oceans.2006.306877.

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Schultz, A. "A multidisciplinary ocean observatory system for the North Atlantic and Southern Ocean". W 3rd International Workshop on Scientific Use of Submarine Cables and Related Technologies. IEEE, 2003. http://dx.doi.org/10.1109/ssc.2003.1224147.

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Tsujii, Koki, Mayuko Otsuki, Tomonari Akamatsu, Ikuo Matsuo, Minoru Kitamura, Takashi Kikuchi, Kazuo Amakasu, Kazushi Miyashita i Yoko Mitani. "Migration monitoring of fin whales in the southern Chukchi Sea with acoustic methods during 2012–2015". W 2016 Techno-Ocean (Techno-Ocean). IEEE, 2016. http://dx.doi.org/10.1109/techno-ocean.2016.7890746.

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

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Buchanan, Kris, Lu Xu, Chris Dilay i David Hilton. "Pacific Ocean HF Noise Distributions off Southern California". W 2019 URSI International Symposium on Electromagnetic Theory (EMTS). IEEE, 2019. http://dx.doi.org/10.23919/ursi-emts.2019.8931498.

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Strzepek, Robert, Pauline Latour, Michael Ellwood i Philip Boyd. "Microbial competition for iron in the Southern Ocean". W Goldschmidt2023. France: European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.16258.

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Robinson, Stephen P., Peter M. Harris, Lian Wang, Sei-Him Cheong i Valerie Livina. "Evaluation of long-term trends in deep-ocean noise in the Southern Ocean". W OCEANS 2019 - Marseille. IEEE, 2019. http://dx.doi.org/10.1109/oceanse.2019.8867509.

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Waters, Kirk, John Brock, Ajit Subramaniam, Richard P. Stumpf i Edward Armstrong. "Satellite assessment of hurricane-induced ocean turbidity for the southern U.S. coastline". W Ocean Optics XIII, redaktorzy Steven G. Ackleson i Robert J. Frouin. SPIE, 1997. http://dx.doi.org/10.1117/12.266410.

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Raporty organizacyjne na temat "The Southern Ocean"

Large, William G., i Todd Ringler. Southern Ocean Uptake in the MPAS-Ocean Model. Office of Scientific and Technical Information (OSTI), listopad 2018. http://dx.doi.org/10.2172/1480355.

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Jones, Philip W. DOE Modeling Activities in the Antarctic/Southern Ocean Region. Office of Scientific and Technical Information (OSTI), maj 2014. http://dx.doi.org/10.2172/1132538.

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Phillips, Helen. A new wave of research in the Southern Ocean. Redaktor James Goldie. Monash University, styczeń 2024. http://dx.doi.org/10.54377/d982-486e.

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Sarmiento, Jorge L., Haidi Chen i Alison R. Gray. Collaborative Project: Three-Dimensional Structure of the Southern Ocean Overturning Circulation. Office of Scientific and Technical Information (OSTI), luty 2019. http://dx.doi.org/10.2172/1495703.

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Guilderson, T. P. Determination of the Prebomb Southern (Antartic) Ocean Radiocarbon in Organic Matter. Office of Scientific and Technical Information (OSTI), luty 2001. http://dx.doi.org/10.2172/15013549.

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Lindsey Peavey, Lindsey Peavey. Comprehensive Conservation of Southern Resident Killer Whales in the Modern Ocean. Experiment, styczeń 2016. http://dx.doi.org/10.18258/6457.

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Hubertz, J. M., J. B. Payne i P. D. Farrar. Hindcasting Swell from the Southern Ocean Along the U.S. Pacific Coast. Fort Belvoir, VA: Defense Technical Information Center, marzec 1995. http://dx.doi.org/10.21236/ada294220.

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Weijer, Wilbert, i Caroline M. Kinstle. An investigation of Bjerknes Compensation in the Southern Ocean in the CCSM4. Office of Scientific and Technical Information (OSTI), sierpień 2012. http://dx.doi.org/10.2172/1049994.

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Muench, Robin D. Dense Outflows and Deep Convection in the Antarctic Zone of the Southern Ocean. Fort Belvoir, VA: Defense Technical Information Center, wrzesień 2009. http://dx.doi.org/10.21236/ada531830.

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Chipman, D. W., S. I. Rubin i T. Takahashi. Measurements of carbon dioxide in the Southern Ocean along the WOCE S-4 section. Office of Scientific and Technical Information (OSTI), sierpień 1992. http://dx.doi.org/10.2172/7270359.

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