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Literatura académica sobre el tema "SEA"

Autor: Grafiati

Publicado: 4 de junio de 2021

Última modificación: 30 de julio de 2024

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Artículos de revistas sobre el tema "SEA"

1

Becker, J., K. Rademann y F. Hensel. "Electronic and Geometrical Structure of Se5, Se6, Se7, and Se8". Zeitschrift für Naturforschung A 46, n.º 5 (1 de mayo de 1991): 453–61. http://dx.doi.org/10.1515/zna-1991-0513.

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AbstractThe vacuum-UV-photoelectron spectra of Se2, Se5, Se6, Se7, and Se8 have been recorded at a photon energy of h ν= 10.0 eV. The isolated molecules are examined in a supersonic molecular beam employing a new photoelectron-photoion coincidence technique. The structure of the photoelectron spectra of selenium molecules with even and odd numbers of atoms differs in a characteristic manner. While the spectra of Se6 and Se8 show one single broad band, three separated bands with different intensities are observed for Se5 and two for Se7. The spectra are compared to molecular orbital energy calculations based on theoretically supposed geometries. The comparison indicates that Se6 and Se8 have Dnd-symmetrical ring structures, whereas Se5 and Se7 are C1h-symmetrical rings

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2

Gao, Fei, Le Wang, Rong Zhao, Yixiong Wang, Yankun Ma, Rulan Yang, Qi Zhang y Chuangyun Wang. "Rational Combination of Selenium Application Rate and Planting Density to Improve Selenium Uptake, Agronomic Traits, and Yield of Dryland Maize". Plants 13, n.º 10 (11 de mayo de 2024): 1327. http://dx.doi.org/10.3390/plants13101327.

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Exogenous selenium application could effectively improve the selenium absorption of crops affected by different climatic conditions due to changes in the planting environment and planting conditions. We planted maize at planting densities of 67,500 plants ha−1 (D1) and 75,000 plants ha−1 (D2). Five selenium fertilizer gradients of 0 mg m−2 (Se0), 7.5 mg m−2 (Se1), 15.0 mg m−2 (Se2), 22.5 mg m−2 (Se3), and 30.0 mg m−2 (Se4) were applied to investigate the response of the plants to selenium fertilizer application in terms of the gradient selenium absorption and substance accumulation. With the increase in the amount of selenium fertilizer applied, more of the selenium fertilizer will be absorbed and transported from the leaves to the grains, and the selenium content of the grains will gradually increase and exceed the selenium content of leaves. Under the D2 density in 2022, the selenium content of the grains under Se1, Se2, Se3, and Se4 treatments increased by 65.67%, 72.71%, and 250.53%, respectively, compared with that of Se0. A total of 260.55% of the plants showed a gradient of grain > leaf > cob > stalk from the Se2 treatment, and the overall selenium content of the plants increased first and then decreased. Under the D1 density, compared with the Se0, the dry matter mass of the Se1, Se2, Se3, and Se4 treatments significantly improved by 5.84%, 1.49%, and 14.26% in 2021, and significantly improved by 4.84%, 3.50%, and 2.85% in 2022. The 1000-grain weight under Se2, Se3, and Se4 treatments improved by 8.57%, 9.06%, and 15.56% compared to that under the Se0 treatment, and the yield per ha under the Se2, Se3, and Se4 treatments was 18.58%, 9.09%, and 21.42% higher than that under Se0 treatment, respectively. In addition, a reasonable combination of selenium application rate and density could improve the chlorophyll content and stem growth of dryland maize. This lays a foundation for the efficient application of selenium fertilizer and provides an important reference.

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3

D'Onghia, Gianfranco, Domingo Lloris, Chrissi-Yianna Politou, Letizia Sion y John Dokos. "New records of deep-water teleost fish in the Balearic Sea and Ionian Sea (Mediterranean Sea)". Scientia Marina 68, S3 (30 de diciembre de 2004): 171–83. http://dx.doi.org/10.3989/scimar.2004.68s3171.

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4

Speroff, Leon. "Sea to sea". Menopause 18, n.º 1 (enero de 2011): 3–4. http://dx.doi.org/10.1097/gme.0b013e3181faa801.

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5

Wang, Le, Fei Gao, Liguang Zhang, Li Zhao, Yan Deng, Hongxia Guo, Lixia Qin y Chuangyun Wang. "Effects of Basal Selenium Fertilizer Application on Agronomic Traits, Yield, Quality, and Se Content of Dryland Maize". Plants 11, n.º 22 (15 de noviembre de 2022): 3099. http://dx.doi.org/10.3390/plants11223099.

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To explore the efficiency of selenium (Se) fertilizer application in dryland maize, we tested five Se fertilizer application treatments: 0 g ha−1 (Se0), 75 g ha−1 (Se1), 150 g ha−1 (Se2), 225 g ha−1 (Se3), and 300 g ha−1 (Se4). Compared with Se0, Se2 increased the leaf area, chlorophyll content, internode length, plant height, and ear height by 7.95%, 3.20%, 13.19%, 1.89%, and 7.98%, respectively. Se2 and Se3 significantly affected the stem internode diameter, cortex thickness, and cellulose content, which were positively correlated with lodging resistance. Compared with Se0, Se3 promoted the contents of soluble sugar, crude protein, crude fat, and starch in grains, which increased by 9.48%, 6.59%, 1.56%, and 4.82%, respectively. It implies that maize grain application of Se significantly improves their Se content. Se1 did not observably influence the growth of maize, and the promoting effect of Se4 on maize decreased. The lodging resistance of maize as analyzed by Pearson correlation analysis correlated with the application of Se fertilizer. It proved that higher yield, grain quality, grain Se content, and lodging resistance of stems were concerned with Se fertilizer application in the range of 150–225 g ha−1. The results provide useful information for Se fertilizer treatment in dryland maize.

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6

Williams, Susan L. "From sea to sea". Nature 530, n.º 7590 (20 de enero de 2016): 290–91. http://dx.doi.org/10.1038/nature16869.

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MacInnes, Mairi. "The Sea! The Sea!" Sewanee Review 115, n.º 1 (2007): 1–19. http://dx.doi.org/10.1353/sew.2007.0014.

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Marshall, Michael. "Lost treasures: The sea-monster seal". New Scientist 213, n.º 2850 (febrero de 2012): 44. http://dx.doi.org/10.1016/s0262-4079(12)60313-3.

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9

Howard, Virginia J. "From Sea to Shining Sea". Stroke 38, n.º 8 (agosto de 2007): 2210–12. http://dx.doi.org/10.1161/strokeaha.107.490425.

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10

Rutledge, Steven A., V. Chandrasekar, Brody Fuchs, Jim George, Francesc Junyent, Brenda Dolan, Patrick C. Kennedy y Kyla Drushka. "SEA-POL Goes to Sea". Bulletin of the American Meteorological Society 100, n.º 11 (noviembre de 2019): 2285–301. http://dx.doi.org/10.1175/bams-d-18-0233.1.

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AbstractA new, advanced radar has been developed at Colorado State University (CSU). The Sea-Going Polarimetric (SEA-POL) radar is a C-band, polarimetric Doppler radar specifically designed to deploy on research ships. SEA-POL is the first such weather radar developed in the United States. Ship-based weather radars have a long history, dating back to GATE in 1974. The GATE radars measured only reflectivity. After GATE, ship radars also provided Doppler measurements. SEA-POL represents the next advancement by adding dual-polarization technology, the ability to transmit and receive both horizontal and vertical polarizations. This configuration provides information about hydrometeor size, shape, and phase. As a result, superior rain-rate estimates are afforded by the dual-polarization technology, along with hydrometeor identification and overall improved data quality. SEA-POL made its first deployment as part of the Salinity Processes in the Upper Ocean Regional Study, second field phase (SPURS-2) fall 2017 cruise to the eastern tropical Pacific, sailing on the R/V Roger Revelle. SPURS-2 was a field project to investigate the fate of freshwater deposited on the ocean’s surface. Oceanographers are keenly interested in how fast these freshwater patches mix out by wind and upper-ocean turbulence, as the less dense rainfall sitting atop the salty ocean inhibits mixing through increased stability. To this end, during SPURS-2, SEA-POL produced rain maps identifying the location of freshwater lenses on the ocean’s surface thereby providing context for measurements of SST and salinity. Examples of SEA-POL polarization measurements are also discussed to assess microphysical processes within oceanic convection. Future ocean-based field campaigns will now benefit from SEA-POL’s advanced dual-polarization technology.

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Tesis sobre el tema "SEA"

1

Brigham, Lawson Walter. "Sea ice variability in Russian Arctic coastal seas : influences on the northern sea route". Thesis, University of Cambridge, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.621873.

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2

Damer, Mouminat. "From Syrian Sea to Shining Sea". Thesis, California State University, Long Beach, 2018. http://pqdtopen.proquest.com/#viewpdf?dispub=10751850.

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From Syrian Sea to Shining Sea is a collection of poetry that reflects the lives of Arab-Americans. Whether they may be first generation, Muslim, or immigrants, there is a piece within their self that reflects a longing for the homeland, ties to the motherland, and struggles that arose as a result of the Syrian Civil War. As a first-generation, Arab-American, Muslim woman I wrote these poems through the raw lens that is my experience.

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3

Babb, David. "Sea ice motion within the Beaufort Sea". American Geophysical Union, 2013. http://hdl.handle.net/1993/23694.

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Sea ice drift and associated forcing mechanisms within the Beaufort Sea are examined within the context of a mechanically weakening Arctic ice pack. Extensive in situ observations of ice drift, ice mass balance and surface winds are supplemented by remotely sensed and modeled data to analyse the forcing of sea ice motion. First we analyse the anomalous export of 13.4 x 103 km2 of sea ice through the Bering Strait during winter 2011-2012. The event highlights a tendency towards increased ice transport through the Bering Strait since 2008 as a result of climate induced weakening of the arctic ice pack. Secondly, as part of the Beaufort Regional Environmental Assessment we analyse the seasonal evolution of ice drift in the Beaufort Sea during Spring as the ice pack transitions from mechanically strong conditions in late winter to weak summer conditions that foster free drift and thus increased ice drift speeds.

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4

Wilkinson, Jeremy. "Sea ice, convection and the Greenland Sea". Thesis, University of Southampton, 2005. https://eprints.soton.ac.uk/25132/.

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The region where deep open-ocean convection occurs in the Greenland Sea corresponds to that where a sea ice winter feature, the Odden, usually forms. The role of sea ice in modifying the surface waters to overturn to depth is evaluated through the combination of in siu measurements, satellite imagery, meteorological measurements and drifting buoy data. Results suggest local meteorological and oceanographic conditions govern the ice conditions over the region. The high ambient wave energy precludes the formation of ice beyond the frazil-pancake stage; the changing surface pressure field, due to passing storm systems, influences the daily shape and extent of the Odden and enables pancake ice to expel brine at an increased rate. Finally, the analysis of drifting buoy data reveal that the ice is in free drift. t These characteristics suggests the Odden may be regarded as a large scale latent heat polynya, with the predominately northerly winds blowing newly formed sea-ice constantly southward such that it melts in a different area from that of its formation. This salt separation process whereby the majority of brine is deposited where the ice was formed, and a smaller amount being released, through brine drainage, as the ice drifts with the prevailing wind has important consequences for the spatial and temporal distribution of the salt flux and hence surrounding hydrography. This is clearly demonstrated through the development of a salt flux model, which involves brine drainage and drift. A simple one-dimensional mixed layer model, driven by results of the salt flux model, predicts a strong density enhancement and deepening of the mixed layer over time. It is therefore envisaged that the formation of sea ice, brine drainage and drift are fundamental in eroding the pycnocline between the surface waters and those below. Sea ice should therefore be viewed as a preconditioning activity to deep overturning of the waters of the central Greenland Sea.

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5

Pettenuzzo, Daniele <1977&gt. "Sea Surface Temperature variations and air-sea physics parametrizations in the Mediterranean Sea". Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2010. http://amsdottorato.unibo.it/2867/1/Pettenuzzo_Daniele_tesi.pdf.

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Pettenuzzo, Daniele <1977&gt. "Sea Surface Temperature variations and air-sea physics parametrizations in the Mediterranean Sea". Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2010. http://amsdottorato.unibo.it/2867/.

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7

Hui, Tabitha Cheng Yee. "Steller sea lions and fisheries : competition at sea?" Thesis, University of British Columbia, 2011. http://hdl.handle.net/2429/32588.

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A leading hypothesis to explain the decline of Steller sea lions (Eumetopias jubatus) in western Alaska is the reduction of prey abundance or change in prey distributions caused by commercial fisheries. We sought to improve on past studies that attempted to assess competition between sea lions and fisheries by estimating the local amounts of prey accessible to sea lions. We explored the relationships between sea lion population trends, fishery catches and the prey biomass accessible to sea lions around 33 rookeries from 2000-2008. We focused on three commercially important species that dominate the sea lion diet: walleye pollock, Pacific cod and Atka mackerel. We estimated available prey biomass by removing fishery catches from predicted prey biomass distributions in the Aleutian Islands, Bering Sea and Gulf of Alaska; and modelled the likelihood of sea lions foraging at different distances from rookeries (accessibility) using satellite telemetry locations of tracked animals. We combined this accessibility model with the prey distributions to estimate the prey biomass accessible to sea lions by rookery. For each rookery, we compared sea lion population change to accessible prey biomass (estimated using our accessibility model and also within 10, 20 and 50 km of each rookery). Of the 304 statistical models we constructed to compare accessible prey biomass and catch to sea lion population trends, only three relationships were significant. These three suggest that sea lion population change rates increased (became less negative) with increasing accessible pollock biomass in the Aleutian Islands and with cod biomass in the Gulf of Alaska. No relationships were found between sea lion population trends and Atka mackerel biomass. Given that the majority of the relationships we explored were insignificant, it seems unlikely that the availability of pollock, cod or Atka mackerel was limiting sea lion populations in the 2000s. Sea lion population trends appeared to be affected by some unknown factor associated with regional differences. Removing fish catches or adding catch to our predicted distributions of groundfish abundances had no measurable effect on sea lion population trends. These observations suggest that sea lion populations were largely unaffected by fishery removals during this period.

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8

Von, Eye Maxine Jutta Erika. "Sea ice and convection in the Greenland Sea". Thesis, University of Cambridge, 2014. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.648527.

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9

Bonaduce, Antonio <1980&gt. "Sea-Level climate variability in the Mediterranean Sea". Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2012. http://amsdottorato.unibo.it/4645/1/Bonaduce_Antonio_tesi.pdf.

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Sea-level variability is characterized by multiple interacting factors described in the Fourth Assessment Report (Bindoff et al., 2007) of the Intergovernmental Panel on Climate Change (IPCC) that act over wide spectra of temporal and spatial scales. In Church et al. (2010) sea-level variability and changes are defined as manifestations of climate variability and change. The European Environmental Agency (EEA) defines sea level as one of most important indicators for monitoring climate change, as it integrates the response of different components of the Earths system and is also affected by anthropogenic contributions (EEA, 2011). The balance between the different sea-level contributions represents an important source of uncertainty, involving stochastic processes that are very difficult to describe and understand in detail, to the point that they are defined as an enigma in Munk (2002). Sea-level rate estimates are affected by all these uncertainties, in particular if we look at possible responses to sea-level contributions to future climate. At the regional scale, lateral fluxes also contribute to sea-level variability, adding complexity to sea-level dynamics. The research strategy adopted in this work to approach such an interesting and challenging topic has been to develop an objective methodology to study sea-level variability at different temporal and spatial scales, applicable in each part of the Mediterranean basin in particular, and in the global ocean in general, using all the best calibrated sources of data (for the Mediterranean): in-situ, remote-sensig and numerical models data. The global objective of this work was to achieve a deep understanding of all of the components of the sea-level signal contributing to sea-level variability, tendency and trend and to quantify them.

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10

Bonaduce, Antonio <1980&gt. "Sea-Level climate variability in the Mediterranean Sea". Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2012. http://amsdottorato.unibo.it/4645/.

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Sea-level variability is characterized by multiple interacting factors described in the Fourth Assessment Report (Bindoff et al., 2007) of the Intergovernmental Panel on Climate Change (IPCC) that act over wide spectra of temporal and spatial scales. In Church et al. (2010) sea-level variability and changes are defined as manifestations of climate variability and change. The European Environmental Agency (EEA) defines sea level as one of most important indicators for monitoring climate change, as it integrates the response of different components of the Earths system and is also affected by anthropogenic contributions (EEA, 2011). The balance between the different sea-level contributions represents an important source of uncertainty, involving stochastic processes that are very difficult to describe and understand in detail, to the point that they are defined as an enigma in Munk (2002). Sea-level rate estimates are affected by all these uncertainties, in particular if we look at possible responses to sea-level contributions to future climate. At the regional scale, lateral fluxes also contribute to sea-level variability, adding complexity to sea-level dynamics. The research strategy adopted in this work to approach such an interesting and challenging topic has been to develop an objective methodology to study sea-level variability at different temporal and spatial scales, applicable in each part of the Mediterranean basin in particular, and in the global ocean in general, using all the best calibrated sources of data (for the Mediterranean): in-situ, remote-sensig and numerical models data. The global objective of this work was to achieve a deep understanding of all of the components of the sea-level signal contributing to sea-level variability, tendency and trend and to quantify them.

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Libros sobre el tema "SEA"

1

Stevens, Serita. Red Sea, Dead Sea. New York: St. Martin's Press, 1991.

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2

Shapiro, Lisa. Sea to shining sea. Tallahassee, Fla: Naiad Press, 1997.

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3

Birch, Beverley. Sea hawk, sea moon. London: Hodder Children's, 2000.

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4

Iris, Murdoch. The sea, the sea. New York: Penguin Books, 2001.

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5

editor, Eccher Danilo, ed. Sean Scully: Land and sea. Milan]: Skira, 2015.

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6

Grovier, Kelly, Danilo Eccher y Sean Scully. Sean Scully: Land Sea. Skira Editore, 2015.

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7

Orr, Tamra. Seal or Sea Lion. Cherry Lake Publishing, 2019.

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8

Bloom, Paul. Seal or Sea Lion? Stevens Publishing LLLP, Gareth, 2015.

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9

Orr, Tamra. Seal or Sea Lion. Cherry Lake Publishing, 2019.

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10

Orr, Tamra. Seal or Sea Lion. Cherry Lake Publishing, 2019.

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Capítulos de libros sobre el tema "SEA"

1

Conradi, Peter J. "The Sea, The Sea". En Iris Murdoch: The Saint and the Artist, 230–54. London: Palgrave Macmillan UK, 1986. http://dx.doi.org/10.1007/978-1-349-18236-7_10.

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Conradi, Peter J. "The Sea, The Sea". En Iris Murdoch: The Saint and the Artist, 230–54. London: Palgrave Macmillan UK, 1989. http://dx.doi.org/10.1007/978-1-349-19651-7_10.

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3

Colivicchi, Fabio. "From Sea to Sea". En The Routledge Handbook of the Archaeology of Urbanism in Italy in the Age of Roman Expansion, 289–91. London: Routledge, 2024. http://dx.doi.org/10.4324/9781003271895-21.

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4

Bährle-Rapp, Marina. "sea". En Springer Lexikon Kosmetik und Körperpflege, 496. Berlin, Heidelberg: Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-71095-0_9222.

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5

Bintley, Michael y Kate Franklin. "Sea". En Landscapes and Environments of the Middle Ages, 50–61. London: Routledge, 2023. http://dx.doi.org/10.4324/9781003122036-5.

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Chee, Lilian. "The Sea, and the Sea". En Architecture and Affect, 257–99. London: Routledge, 2023. http://dx.doi.org/10.4324/9781315604565-13.

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Yamashiro, Shin. "Introduction: On the Sea, By the Sea, Beneath the Sea". En American Sea Literature, 1–11. New York: Palgrave Macmillan US, 2014. http://dx.doi.org/10.1057/9781137463302_1.

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Arens, Werner y Henning Thies. "Murdoch, Iris: The Sea, the Sea". En Kindlers Literatur Lexikon (KLL), 1–2. Stuttgart: J.B. Metzler, 2020. http://dx.doi.org/10.1007/978-3-476-05728-0_14382-1.

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Yamashiro, Shin. "American Sea Literature—on the Sea". En American Sea Literature, 12–47. New York: Palgrave Macmillan US, 2014. http://dx.doi.org/10.1057/9781137463302_2.

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Yamashiro, Shin. "American Sea Literature—by the Sea". En American Sea Literature, 48–80. New York: Palgrave Macmillan US, 2014. http://dx.doi.org/10.1057/9781137463302_3.

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Actas de conferencias sobre el tema "SEA"

1

Kalla, Praveen, Jörg Henkel y Xiaobo Sharon Hu. "SEA". En the 2003 conference. New York, New York, USA: ACM Press, 2003. http://dx.doi.org/10.1145/1119772.1119909.

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Serrano Rubio, Juan Pablo, Arturo Hernández Aguirre y Rafael Herrera Guzmán. "SEA". En GECCO '14: Genetic and Evolutionary Computation Conference. New York, NY, USA: ACM, 2014. http://dx.doi.org/10.1145/2598394.2598492.

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Wang, Yaqiong, Hongfu Liu, Hao Lin, Junjie Wu, Zhiang Wu y Jie Cao. "SEA". En KDD' 13: The 19th ACM SIGKDD International Conference on Knowledge Discovery and Data Mining. New York, NY, USA: ACM, 2013. http://dx.doi.org/10.1145/2487575.2487719.

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Onsay, Sebnem. "Object-Oriented SEA Modeling (OO-SEA)". En SAE 2003 Noise & Vibration Conference and Exhibition. 400 Commonwealth Drive, Warrendale, PA, United States: SAE International, 2003. http://dx.doi.org/10.4271/2003-01-1551.

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Fernandes, Antonio Carlos, Janou Hennig, Marcio Domingues Maia, Hans Cozijn y Joel Sena Sales. "Worst Sea–Best Sea Wave Group Spectra From Random Sea States". En ASME 2008 27th International Conference on Offshore Mechanics and Arctic Engineering. ASMEDC, 2008. http://dx.doi.org/10.1115/omae2008-57821.

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The paper presents a proposition called the worst sea-best sea (WS-BS) method that intends to identify wave group spectra that yield time series that lead, respectively, to the highest wave group excitation (worst sea) and the smallest wave group excitation (best sea) to the second order slowly varying response for a floating structure model submitted to random waves in a wave basin. The methodology is based on the estimation theory. Based on the fact that even with the same wave spectrum it is possible to devise different wave group spectrum, the paper proposes a method to identify the WS-BS time series. Both simulations and concrete model testing are shown indicating the feasibility of the approach.

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Mudersbach, Christoph y Jürgen Jensen. "RECENT SEA LEVEL VARIATIONS AT THE NORTH SEA AND BALTIC SEA COASTLINES". En Proceedings of the 30th International Conference. World Scientific Publishing Company, 2007. http://dx.doi.org/10.1142/9789812709554_0149.

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Ismail, M., M. Zamurad Shah y A. Mughal. "Deep sea motion under higher sea states". En 2012 International Bhurban Conference on Applied Sciences and Technology (IBCAST). IEEE, 2012. http://dx.doi.org/10.1109/ibcast.2012.6177537.

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Fritzner, Sindre M. y Trond Sagerup. "Sea Ice Distribution in the Barents Sea". En ASME 2016 35th International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2016. http://dx.doi.org/10.1115/omae2016-54817.

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This paper provides a statistical description of the sea ice occurrence in the Barents Sea, using yearly maximum sea ice data for the last 36 years from the European Centre for Medium-Range Weather Forecasts (ECMWF). A set of four distribution functions have been estimated with the maximum likelihood method. The distribution functions used were Extreme Value distribution, Gumbel distribution, Normal distribution and kernel density estimation. The normal distribution was found to fit the data best and provide the most likely result. Our results verify dependency of the North Atlantic current on the sea ice edge. Warm water northwards prevents the ice from extending south; this makes the extreme value distribution unlikely since this will prevent long tailed distributions. The results for sea ice occurrence are compared to the boundaries given in the proposed revision to NORSOK N-003. These boundaries were found to be too simplistic and not necessarily conservative. Here we have proposed new and more accurate boundaries for the sea ice occurrence. We have found trends indicating northwards movement of the sea ice edge in the Norwegian Sea and eastern parts of the Barents Sea. These trends are mostly due to less ice in the last ten years and not trends for the whole period. In the south-western parts of the Barents Sea where oil and gas operations are imminent no trends have been discovered. The lack of trend is related to the islands in the western Barents Sea.

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9

Chekole, Eyasu Getahun y Guo Huaqun. "ICS-SEA". En ICSS: Fifth Annual Industrial Control System Security Workshop. New York, NY, USA: ACM, 2019. http://dx.doi.org/10.1145/3372318.3372325.

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10

Churchill, Steven. "Sea dance". En ACM SIGGRAPH 99 Electronic art and animation catalog. New York, New York, USA: ACM Press, 1999. http://dx.doi.org/10.1145/312379.313073.

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Informes sobre el tema "SEA"

1

Brian Clark, Brian Clark. Sex in the sea: Uncovering the mating behavior of Giant Sea Bass. Experiment, enero de 2014. http://dx.doi.org/10.18258/1883.

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2

Clague, J. J. Sea level change: factors affecting sea level. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/213910.

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3

Fratarangelo, P., P. A. Gale, W. J. Hancock, D. J. Katz, E. R. Kohn, W. A. Neal, R. W. Ness, N. Polmar, J. T. Tozzi y G. E. Webber. Sea Basing. Fort Belvoir, VA: Defense Technical Information Center, marzo de 2005. http://dx.doi.org/10.21236/ada444704.

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4

Bell, J. S. Labrador Sea. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127152.

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5

Novichkova, Tatiana. Caspian Sea. Editado por Nikolay Komedchikov. Entsiklopediya, enero de 2012. http://dx.doi.org/10.15356/dm2015-12-02-4.

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6

Hurley, Michael y Christopher Powell. Sea Node. Fort Belvoir, VA: Defense Technical Information Center, septiembre de 2009. http://dx.doi.org/10.21236/ada532127.

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7

Golding, Heidi L. W. y David Gregory. Sea Tours and Sea Pay: Patterns in Sailors' Completion and Extension of Sea Duty. Fort Belvoir, VA: Defense Technical Information Center, abril de 2001. http://dx.doi.org/10.21236/ada407367.

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8

Le, Tom. A Japanese Security Sea Change? Let’s See Change First. Critical Asian Studies, enero de 2023. http://dx.doi.org/10.52698/wajo6699.

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9

Boyd, Janice D. Descriptive Physical Oceanography of the North Pacific, Sea of Japan (East Sea) and Sea of Okhotsk. Fort Belvoir, VA: Defense Technical Information Center, enero de 1995. http://dx.doi.org/10.21236/ada311009.

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10

Franks Taylor, R. The Sweetwater Sea. The Nature Conservancy, junio de 2010. http://dx.doi.org/10.3411/col.09141617.

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