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Journal articles on the topic 'World ocean'

Author: Grafiati

Published: 4 June 2021

Last updated: 26 July 2025

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1

Andrianova, O. R. "ACTUALS PROBLEMS OF THE RESEARCH OF WORLD OCEAN LEVEL." Odesa National University Herald. Geography and Geology 19, no. 4(23) (2015): 55–68. http://dx.doi.org/10.18524/2303-9914.2014.4(23).39300.

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The features of the sea level changes and the related dynamics of the coastal zone are the subject of the discussions in the economic planning as in the regionally as in globally scale. The work’s purpose is analysis of changes of World Ocean level under the influence of different factors from the viewpoint of physical geography – the interdependence of nature of the ocean and continents, large-scale connections between oceanosphera and other elements of the Earth’s environment and evaluation of the modern established knowledge about thetendencies of the development of processes in the coastal

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2

Kumar, Amar, and Vishal a. "INDIAN OCEAN 21 WORLDS WORLD POLITICS CENTER." International Journal of Advanced Research 9, no. 5 (2021): 1118–26. http://dx.doi.org/10.21474/ijar01/12948.

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The life base of the South Asian states is the Indian Ocean. This ocean depends on the geographical security, sovereignty, development, destruction, life of these states on this natural heritage. The only ocean in the world whose name is named after a country (India, Hind). It has many resources by providing these states and the world. 1971 Menyhdomhanvicharokatkravdeknekomilaawrakaakyhkshetranykshetronsemhtwpuarnhogyaksandhion, Sanyabyas, Senakitanati, Ityadikiakaakjdilggiawrajayhkshetr 21 Visdimenvishwarajnitikakendrabngyahabiswkimahashktionamerika, China, France, Russia, China, Britain, Jap

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3

Showstack, Randy. "World Ocean Database." Eos, Transactions American Geophysical Union 90, no. 49 (2009): 472. http://dx.doi.org/10.1029/2009eo490003.

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4

Hurgobin, Yoshina, and Subho Basu. "“Oceans without Borders”: Dialectics of Transcolonial Labor Migration from the Indian Ocean World to the Atlantic Ocean World." International Labor and Working-Class History 87 (2015): 7–26. http://dx.doi.org/10.1017/s0147547915000071.

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AbstractBy investigating the hitherto unstudied trans-colonial migration between Mauritius and the Caribbean in the nineteenth century, this article complicates liberal Eurocentric perceptions of global labor force formation under the auspices of colonial capital. Indeed, coercion, as depicted in liberal historiography, was a crucial component of indentured migration but indentured workers themselves sometimes availed of the opportunity of the global demand for their labor by engaging in trans-colonial migration. The dialectic of the formation of globalized indentured labor regime was such tha

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5

Rhoden, Alyssa Rose. "Mimas: Frozen Fragment, Ring Relic, or Emerging Ocean World?" Annual Review of Earth and Planetary Sciences 51, no. 1 (2023): 367–87. http://dx.doi.org/10.1146/annurev-earth-031621-061221.

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Mimas, the smallest and innermost of Saturn's mid-sized moons, has a heavily cratered surface devoid of the intricate fracture systems of its neighbor, Enceladus. However, Cassini measurements identified a signature of an ocean under Mimas’ ice shell, although a frozen ice shell over a rocky interior could not be ruled out. The Mimas ocean hypothesis has stimulated inquiry into Mimas’ geologic history and orbital evolution. Here, we summarize the results of these investigations, which (perhaps surprisingly) are consistent with an ocean-bearing Mimas as long as it is geologically young. In that

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6

SHNYUKOV, Ye F., and I. V. TOPACHEVSKY. "World ocean gas seeps." Geology and Mineral Resources of World Ocean 15, no. 2 (2019): 3–15. http://dx.doi.org/10.15407/gpimo2019.02.003.

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7

Figueroa, Horacio A. "World Ocean Density Ratios." Journal of Physical Oceanography 26, no. 2 (1996): 267–75. http://dx.doi.org/10.1175/1520-0485(1996)026<0267:wodr>2.0.co;2.

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8

Levitus, S., J. I. Antonov, O. K. Baranova, et al. "The World Ocean Database." Data Science Journal 12 (2013): WDS229—WDS234. http://dx.doi.org/10.2481/dsj.wds-041.

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9

Jansen, Malte F., Wanying Kang, Edwin S. Kite, and Yaoxuan Zeng. "Energetic Constraints on Ocean Circulations of Icy Ocean Worlds." Planetary Science Journal 4, no. 6 (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, f

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10

Moran, Mary Ann, Elizabeth B. Kujawinski, Aron Stubbins, et al. "Deciphering ocean carbon in a changing world." Proceedings of the National Academy of Sciences 113, no. 12 (2016): 3143–51. http://dx.doi.org/10.1073/pnas.1514645113.

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Dissolved organic matter (DOM) in the oceans is one of the largest pools of reduced carbon on Earth, comparable in size to the atmospheric CO2reservoir. A vast number of compounds are present in DOM, and they play important roles in all major element cycles, contribute to the storage of atmospheric CO2in the ocean, support marine ecosystems, and facilitate interactions between organisms. At the heart of the DOM cycle lie molecular-level relationships between the individual compounds in DOM and the members of the ocean microbiome that produce and consume them. In the past, these connections hav

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11

Shuisky, Yuriy D. "Physical-geographical natural systems within waters of the World Ocean." Journal of the Belarusian State University. Geography and Geology, no. 1 (June 8, 2021): 35–49. http://dx.doi.org/10.33581/2521-6740-2021-1-35-49.

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Based on the data of theoretical developments in the fields of ocean geography and system-geographical analysis, a hierarchical scheme of natural systems in the water layer of the World Ocean has been examined. The aim of the work is to carry out the first attempt to compare landscapes on land, natural systems in the coastal zone (the zone of contact between land and the World Ocean) and those in the World Ocean. The differentiation of the oceanic natural environment which is a possible version of a systematised list of systems ranging from individual oceans to individual eddies (or impulses)

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12

García-García, David, Isabel Vigo, and Mario Trottini. "Water transport among the world ocean basins within the water cycle." Earth System Dynamics 11, no. 4 (2020): 1089–106. http://dx.doi.org/10.5194/esd-11-1089-2020.

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Abstract. The global water cycle involves water-mass transport on land, in the atmosphere, in the ocean, and among them. Quantification of such transport, especially its time evolution, is essential to identify the footprints of climate change, and it also helps to constrain and improve climatic models. In the ocean, net water-mass transport among the ocean basins is a key process, but it is currently a poorly estimated parameter. We propose a new methodology that incorporates the time-variable gravity observations from the Gravity Recovery and Climate Experiment (GRACE) satellite (2003–2016)

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13

Chu, Peter C., and Chenwu Fan. "World Ocean Thermocline Weakening and Isothermal Layer Warming." Applied Sciences 10, no. 22 (2020): 8185. http://dx.doi.org/10.3390/app10228185.

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This paper identifies world thermocline weakening and provides an improved estimate of upper ocean warming through replacement of the upper layer with the fixed depth range by the isothermal layer, because the upper ocean isothermal layer (as a whole) exchanges heat with the atmosphere and the deep layer. Thermocline gradient, heat flux across the air–ocean interface, and horizontal heat advection determine the heat stored in the isothermal layer. Among the three processes, the effect of the thermocline gradient clearly shows up when we use the isothermal layer heat content, but it is otherwis

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14

Vaughan, Adam. "World misses ocean conservation target." New Scientist 250, no. 3336 (2021): 20. http://dx.doi.org/10.1016/s0262-4079(21)00908-8.

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15

Showstack, Randy. "World Ocean Assessment experts needed." Eos, Transactions American Geophysical Union 93, no. 31 (2012): 303. http://dx.doi.org/10.1029/2012eo310005.

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16

Woods, J. D. "The World Ocean Circulation Experiment." Nature 314, no. 6011 (1985): 501–11. http://dx.doi.org/10.1038/314501a0.

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17

Anonymous. "The World Ocean Circulation Experiment." Eos, Transactions American Geophysical Union 73, no. 3 (1992): 34. http://dx.doi.org/10.1029/91eo10034.

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18

Tréguer, Paul J., and Christina L. De La Rocha. "The World Ocean Silica Cycle." Annual Review of Marine Science 5, no. 1 (2013): 477–501. http://dx.doi.org/10.1146/annurev-marine-121211-172346.

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19

Levitus, S. "Warming of the World Ocean." Science 287, no. 5461 (2000): 2225–29. http://dx.doi.org/10.1126/science.287.5461.2225.

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20

Döös, Kristofer, Johan Nilsson, Jonas Nycander, Laurent Brodeau, and Maxime Ballarotta. "The World Ocean Thermohaline Circulation*." Journal of Physical Oceanography 42, no. 9 (2012): 1445–60. http://dx.doi.org/10.1175/jpo-d-11-0163.1.

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Abstract A new global streamfunction is presented and denoted the thermohaline streamfunction. This is defined as the volume transport in terms of temperature and salinity (hence no spatial variables). The streamfunction is used to analyze and quantify the entire World Ocean conversion rate between cold/warm and fresh/saline waters. It captures two main cells of the global thermohaline circulation, one corresponding to the conveyor belt and one corresponding to the shallow tropical circulation. The definition of a thermohaline streamfunction also enables a new method of estimating the turnover

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21

Tanhua, Toste, Sören B. Gutekunst, and Arne Biastoch. "A near-synoptic survey of ocean microplastic concentration along an around-the-world sailing race." PLOS ONE 15, no. 12 (2020): e0243203. http://dx.doi.org/10.1371/journal.pone.0243203.

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Litter and plastic pollution in the marine environment is of major concern when considering the health of ocean ecosystems, and have become an important focus of ocean research during recent years. There is still significant uncertainty surrounding the distribution and impact of marine plastic litter on ocean ecosystems, and in particular on the nano- and microplastic fractions that are difficult to observe and may be harmful to marine organisms. Current estimates of ocean plastic concentrations only account for a small fraction of the approximated 8 million tons of plastic litter entering the

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22

Shepherd, John G., Peter G. Brewer, Andreas Oschlies, and Andrew J. Watson. "Ocean ventilation and deoxygenation in a warming world: introduction and overview." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 375, no. 2102 (2017): 20170240. http://dx.doi.org/10.1098/rsta.2017.0240.

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Changes of ocean ventilation rates and deoxygenation are two of the less obvious but important indirect impacts expected as a result of climate change on the oceans. They are expected to occur because of (i) the effects of increased stratification on ocean circulation and hence its ventilation, due to reduced upwelling, deep-water formation and turbulent mixing, (ii) reduced oxygenation through decreased oxygen solubility at higher surface temperature, and (iii) the effects of warming on biological production, respiration and remineralization. The potential socio-economic consequences of reduc

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23

Turley, C. "Impacts of changing ocean chemistry in a high-CO2 world." Mineralogical Magazine 72, no. 1 (2008): 359–62. http://dx.doi.org/10.1180/minmag.2008.072.1.359.

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AbstractOver the last ∼200 years, since the start of the industrial revolution, the increase in the burning of fossil fuels, cement manufacturing and changes to land use has increased atmospheric CO2 concentrations from ∼80 to 385 ppm. These are the highest levels experienced on Earth for at least the last 800,000 years, possibly for the past 10’s of millions of years. The 2007 IPCC report on climate change predicts a continued rapid rise in atmospheric CO2 leading to significant temperature increases in the atmosphere and ocean in the coming decades, as well as other climate changes. The IPCC

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24

Mishukova, G. I., A. V. Yatsuk, and R. B. Shakirov. "Distribution of methane fluxes on the water–atmosphere interface in different regions of the World Ocean." Geosystems of Transition Zones 5, no. 3 (2021): 240–54. http://dx.doi.org/10.30730/gtrz.2021.5.3.240-247.247-254.

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For the first time, methane fluxes at the water-atmosphere interface were calculated for the water area of Pacific, Indian, and Atlantic oceans (for the area about 30,000 miles) on the basis of the expeditionary measurements of methane concentrations in the surface layer of water and subsurface layer of the atmosphere along the entire course of the vessel. Methane fluxes at the water-atmosphere interface were calculated for the water areas of the Pacific, Indian and Atlantic oceans. In the result of the studies carried out in various regions of the World Ocean, an uneven spatial distribution o

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25

ZELENKO, A. A., S. A. MYSLENKOV, YU D. RESNYANSKII, B. S. STRUKOV, and M. YU ZAICHENKO. "COMPLEX SYSTEM FOR WIND WAVE FORECASTING IN THE WORLD OCEAN AND RUSSIAN SEAS." Meteorologiya i Gidrologiya, no. 8 (August 2024): 20–35. https://doi.org/10.52002/0130-2906-2024-8-20-35.

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The paper describes a system for wind wave forecasting in the World Ocean, which has resulted from the development of the operational forecast technology functioning at the Hydrometcenter of Russia since 2014. The system is built on the linked “ocean-sea-coastal zone” scheme designed for making forecasts over the entire World Ocean and individual Russian seas. The developed model configurations make it possible to compute wave parameters with a horizontal resolution of 10-20 km in oceans and 1-5 km in Russian seas. To detail the forecasts in the coastal zone of the seas, unstructured triangula

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26

Bremner, Lindsay. "Folded ocean: The spatial transformation of the Indian Ocean world." Journal of the Indian Ocean Region 10, no. 1 (2013): 18–45. http://dx.doi.org/10.1080/19480881.2013.847555.

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27

Döös, K. "The wind-driven overturning circulation of the World Ocean." Ocean Science Discussions 2, no. 5 (2005): 473–505. http://dx.doi.org/10.5194/osd-2-473-2005.

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Abstract. The wind driven aspects of the meridional overturning circulation of the world ocean and the Conveyor Belt is studied making use of a simple analytical model. The model consists of three reduced gravity layers with an inviscid Sverdrupian interior and a western boundary layer. The net north-south exchange is made possible by setting appropriate western boundary conditions, so that most of the transport is confined to the western boundary layer, while the interior is the Sverdrupian solution to the wind stress. The flow across the equator is made possible by the change of potential vo

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28

Pandey, Hemant Kumar, and Akhilesh Dwivedi. "STRATEGIC ROLE OF INDIAN NAVY IN IOR AT PRESENT." SCHOLARLY RESEARCH JOURNAL FOR HUMANITY SCIENCE AND ENGLISH LANGUAGE 9, no. 46 (2021): 11318–25. http://dx.doi.org/10.21922/srjhsel.v9i46.1541.

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The Indian Ocean Region (IOR) turned out to be the most engaging region for global activities in recent years. The Indian Ocean consists of the most important trade routes of the world. The Indian Ocean provides a way to move through various regions of the world. World's huge economic players always keep an eye on the IOR for its strategic importance. The Indian Ocean is a gateway to the Atlantic Ocean through the Mediterranean Sea via the Red Sea and it also provides a way to the Pacific Ocean through the Strait of Malacca. It is the main shipping channel for the Pacific and Atlantic oceans.

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29

Ginga, Damião. "Economia azul: a economia do futuro para Angola." Revista Internacional em Língua Portuguesa, no. 45 (October 1, 2024): 81–102. http://dx.doi.org/10.31492/2184-2043.rilp2024.45/pp.81-102.

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More than 70% of the planet is covered by the ocean, making it a central element in the world economy. It is the largest ecosystem in the world, as the economy of exploration and sustainable use of ocean resources, if it were considered a single economy, would be the seventh largest economy in the world, integrating the G7. With this article, under the theme “Blue economy: the economy of the future for Angola,” it is intended to present the framework for exploiting the blue economy for the sustainable development of Angola, through a deductive approach, through document analysis, aiming to pre

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30

Shinkaretskaya, Galina G. "The level of the World Ocean and International Law." Gosudarstvo i pravo, no. 9 (2023): 172. http://dx.doi.org/10.31857/s102694520027738-2.

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As a result of the work of the Third UN Conference on the Law of the Sea, which adopted the UN Convention on the Law of the Sea, a single international legal order was established in the oceans covering 2/3 of our planet and approved by virtually all States. An important part of it is the procedure for allocating from the common space of the World Ocean part of the waters and the bottom, lawfully subject to the jurisdiction of coastal States. With the warming of the climate on Earth, the water level of the World&apos;s oceans began to rise, and the established limits of the zones of jurisd

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31

Druzhinin, A. G., and S. S. Lachininskii. "Russia at the World Ocean: geoeconomic and geopolitical interests, scale and formats of «presence»." Известия Русского географического общества 151, no. 6 (2019): 1–19. http://dx.doi.org/10.31857/s0869-607115161-19.

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One of the modern global trends is the accelerated formation of ablue economy based on transport and logistics, resource-raw materials and other capabilities of the seas and oceans, which occupy more than 70% of the Earths surface. The article substantiates the growth of the geo-economic and geopolitical significance of the World Ocean for Russia and the realization of its geopolitical and geo-economic interests. Based on acritical review of research and the views of domestic and foreign scientists concerned the implementation of the geo-economic and geopolitical strategies of world and some l

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32

Huo, Chuan Lin, Cheng Huo, and Dao Ming Guan. "Advances in Studies of Ocean Acidification." Applied Mechanics and Materials 295-298 (February 2013): 2191–94. http://dx.doi.org/10.4028/www.scientific.net/amm.295-298.2191.

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During the past 200 years, approximately one-half of the carbon dioxide from human activities is being taken up by the oceans. The uptake of carbon dioxide has led to a reduction of the pH value of surface seawater of 0.1 units, equivalent to a 30% increase in the concentration of hydrogen ions. If global emission of carbon dioxide from human activities continues to rise at the current rates, the average pH value of the oceans could fall by 0.5 units by the year 2100. This was equivalent to a three fold increase in the concentration of hydrogen ions. Global ocean acidification has become one o

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33

Litun, T. A., S. N. Semenova, O. V. Statsenko, and V. I. Statsenko. "The Current State of the World Ocean." ТЕНДЕНЦИИ РАЗВИТИЯ НАУКИ И ОБРАЗОВАНИЯ 98, no. 7 (2023): 152–55. http://dx.doi.org/10.18411/trnio-06-2023-396.

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The work is devoted to the characteristics of today world ocean state. The paper considers the sources of pollution. The problems related to the general world ocean state are analyzed in the paper. The activities of international organizations aimed at reducing emissions into the world ocean are considered.

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34

Gattuso, Jean-Pierre, and François Houllier. "June 2025: Nice, capital of the world ocean." Arts et sciences 9, no. 2 (2025): 3–8. https://doi.org/10.21494/iste.op.2025.1287.

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We outline the critical importance of the ocean for planetary health, economic prosperity, and human well-being, while highlighting the urgent threats it faces from climate change, pollution, overfishing, and poor governance. It presents the One Ocean Science Congress (OOSC) and the 3rd United Nations Ocean Conference (UNOC3), scheduled for June 2025 in Nice, France, as pivotal events aimed at promoting ocean sustainability through science-based policy, innovation, and global cooperation. The OOSC will deliver scientific recommendations to Heads of States and Govern-ments, while additional hig

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35

Miller, Gregory J., and M. N. Pearson. "Spices in the Indian Ocean World." Sixteenth Century Journal 29, no. 1 (1998): 310. http://dx.doi.org/10.2307/2544511.

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36

A.T., Zverev. "Eustatic fluctuations in world ocean level." Geodesy and Aerophotosurveying 64, no. 2 (2020): 157–63. http://dx.doi.org/10.30533/0536-101x-2020-64-2-157-163.

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37

Pearson, Michael. "Places in the Indian Ocean World." Journal of Indian Ocean World Studies 1, no. 1 (2017): 4. http://dx.doi.org/10.26443/jiows.v1i1.28.

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We all enact change over time, but are not nearly as concerned with where we are writing about. One recent trend in general historiography may help our maritime studies. This is the matter of place. To illustrate this, let me say a little about three particular spaces, that is, ships, then coasts, and finally port cities.

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38

Gudev, Pavel. "THE US POLICY IN WORLD OCEAN." International Trends / Mezhdunarodnye protsessy 14, no. 1(44) (2016): 106–20. http://dx.doi.org/10.17994/it.2016.14.1.44.9.

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39

Lutjeharms, J. R. E., and M. L. Gründlingh. "The World Ocean Circulation Experiment (WOCE)." Suid-Afrikaanse Tydskrif vir Natuurwetenskap en Tegnologie 6, no. 2 (1987): 64–71. http://dx.doi.org/10.4102/satnt.v6i2.946.

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An international research programme of enormous scope, WOCE (World Ocean Circulation Experiment), is being planned for the last decade of this century. It is aimed at increasing our knowledge and understanding of the world ocean circulation by a quantum leap, thereby contributing to a better understanding of world climate changes. This programme is of great interest to South Africa and, while lacking the resources of the larger countries. South Africans can make key contributions in certain specific areas and have started preparing to do so.

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40

Kashirsky, A. S., and Y. V. Kirichenko. "WORLD OCEAN - LAST RESERVE OF HUMANITY." Mining science and technology, no. 1 (January 1, 2017): 67–76. http://dx.doi.org/10.17073/2500-0632-2017-1-67-74.

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41

Tirpak, Elizabeth, and David Halpern. "World Ocean Assessment: Opportunities for geoscientists." Eos, Transactions American Geophysical Union 93, no. 50 (2012): 521–22. http://dx.doi.org/10.1029/2012eo500001.

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42

Smart, Jeffrey. "World-wide Ocean Optics Database (WOOD)." Oceanography 13, no. 3 (2000): 70–74. http://dx.doi.org/10.5670/oceanog.2000.13.

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43

Takashima, Reishi, Hiroshi Nishi, Brian Huber, and R. Mark Leckie. "Greenhouse World and the Mesozoic Ocean." Oceanography 19, no. 4 (2006): 82–92. http://dx.doi.org/10.5670/oceanog.2006.07.

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44

Cudaback, Cynthia. "BOOK REVIEW | Exploring the World Ocean." Oceanography 20, no. 4 (2007): 174–75. http://dx.doi.org/10.5670/oceanog.2007.23.

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45

Keeling, Ralph F., Arne Körtzinger, and Nicolas Gruber. "Ocean Deoxygenation in a Warming World." Annual Review of Marine Science 2, no. 1 (2010): 199–229. http://dx.doi.org/10.1146/annurev.marine.010908.163855.

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46

Bannon, Peter R., and Raymond G. Najjar. "Available energy of the world ocean." Journal of Marine Research 72, no. 4 (2014): 219–42. http://dx.doi.org/10.1357/002224014815460650.

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47

Campbell, Gwyn. "Piracy in the Indian Ocean World." Interventions 16, no. 6 (2014): 775–94. http://dx.doi.org/10.1080/1369801x.2014.936958.

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48

Rai, Adwita. "The Indian Ocean in World History." Maritime Affairs: Journal of the National Maritime Foundation of India 11, no. 1 (2015): 137–40. http://dx.doi.org/10.1080/09733159.2015.1027075.

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49

Smith, Hance D. "The industrialisation of the world ocean." Ocean & Coastal Management 43, no. 1 (2000): 11–28. http://dx.doi.org/10.1016/s0964-5691(00)00028-4.

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Smith, H. D. "The industrialisation of the world ocean." Ocean & Coastal Management 44, no. 9-10 (2001): 563–66. http://dx.doi.org/10.1016/s0964-5691(01)00068-0.

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