Bibliografías temáticas / Indian Ocean

Literatura académica sobre el tema "Indian Ocean"

Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 22 de junio de 2024

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Artículos de revistas sobre el tema "Indian Ocean"

1

Van der Land, J., Barbara Kwiatkowska, Jan H. Stel, Pervez Ahmed Butt y S. H. Niaz Rizvi. "Indian Ocean". International Journal of Marine and Coastal Law 8, n.º 1 (1993): 164–67. http://dx.doi.org/10.1163/157180893x00279.

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2

Jin, Xiaolin, Young-Oh Kwon, Caroline C. Ummenhofer, Hyodae Seo, Franziska U. Schwarzkopf, Arne Biastoch, Claus W. Böning y Jonathon S. Wright. "Influences of Pacific Climate Variability on Decadal Subsurface Ocean Heat Content Variations in the Indian Ocean". Journal of Climate 31, n.º 10 (30 de abril de 2018): 4157–74. http://dx.doi.org/10.1175/jcli-d-17-0654.1.

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Abstract Decadal variabilities in Indian Ocean subsurface ocean heat content (OHC; 50–300 m) since the 1950s are examined using ocean reanalyses. This study elaborates on how Pacific variability modulates the Indian Ocean on decadal time scales through both oceanic and atmospheric pathways. High correlations between OHC and thermocline depth variations across the entire Indian Ocean Basin suggest that OHC variability is primarily driven by thermocline fluctuations. The spatial pattern of the leading mode of decadal Indian Ocean OHC variability closely matches the regression pattern of OHC on the interdecadal Pacific oscillation (IPO), emphasizing the role of the Pacific Ocean in determining Indian Ocean OHC decadal variability. Further analyses identify different mechanisms by which the Pacific influences the eastern and western Indian Ocean. IPO-related anomalies from the Pacific propagate mainly through oceanic pathways in the Maritime Continent to impact the eastern Indian Ocean. By contrast, in the western Indian Ocean, the IPO induces wind-driven Ekman pumping in the central Indian Ocean via the atmospheric bridge, which in turn modifies conditions in the southwestern Indian Ocean via westward-propagating Rossby waves. To confirm this, a linear Rossby wave model is forced with wind stresses and eastern boundary conditions based on reanalyses. This linear model skillfully reproduces observed sea surface height anomalies and highlights both the oceanic connection in the eastern Indian Ocean and the role of wind-driven Ekman pumping in the west. These findings are also reproduced by OGCM hindcast experiments forced by interannual atmospheric boundary conditions applied only over the Pacific and Indian Oceans, respectively.
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3

Kajtar, Jules B., Agus Santoso, Matthew H. England y Wenju Cai. "Indo-Pacific Climate Interactions in the Absence of an Indonesian Throughflow". Journal of Climate 28, n.º 13 (1 de julio de 2015): 5017–29. http://dx.doi.org/10.1175/jcli-d-14-00114.1.

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Abstract The Pacific and Indian Oceans are connected by an oceanic passage called the Indonesian Throughflow (ITF). In this setting, modes of climate variability over the two oceanic basins interact. El Niño–Southern Oscillation (ENSO) events generate sea surface temperature anomalies (SSTAs) over the Indian Ocean that, in turn, influence ENSO evolution. This raises the question as to whether Indo-Pacific feedback interactions would still occur in a climate system without an Indonesian Throughflow. This issue is investigated here for the first time using a coupled climate model with a blocked Indonesian gateway and a series of partially decoupled experiments in which air–sea interactions over each ocean basin are in turn suppressed. Closing the Indonesian Throughflow significantly alters the mean climate state over the Pacific and Indian Oceans. The Pacific Ocean retains an ENSO-like variability, but it is shifted eastward. In contrast, the Indian Ocean dipole and the Indian Ocean basinwide mode both collapse into a single dominant and drastically transformed mode. While the relationship between ENSO and the altered Indian Ocean mode is weaker than that when the ITF is open, the decoupled experiments reveal a damping effect exerted between the two modes. Despite the weaker Indian Ocean SSTAs and the increased distance between these and the core of ENSO SSTAs, the interbasin interactions remain. This suggests that the atmospheric bridge is a robust element of the Indo-Pacific climate system, linking the Indian and Pacific Oceans even in the absence of an Indonesian Throughflow.
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4

Ming, Wan. "Zheng He’s Seven Voyages into the Namoli Ocean–the Indian Ocean". China and Asia 1, n.º 1 (11 de febrero de 2019): 92–125. http://dx.doi.org/10.1163/2589465x-00101004.

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In the history of the development of human civilization, the Silk Road has been an important route of traffic and exchange between the East and the West. From Zhang Qian’s 張騫 opening up of the Silk Road across the Western Regions (Xiyue 西域) to Zheng He’s 鄭和 sailing to the Western Oceans (xia xiyang 下西洋) more than 1500 years later, China had a continuous desire to explore beyond its borders. At the time of Zheng He, the term “Western Oceans” (xiyang 西洋) had a specific meaning. As shown by the account of Ma Huan 馬歡, who personally joined Zheng He on the voyages, the people of Ming China considered the “Western Oceans” to be the Namoli Ocean (Namoli yang 那没黎洋), later called the Indian Ocean. Thus, it could be concluded that the Western Oceans where Zheng He’s fleet went meant the Indian Ocean. Even today most scholars still divide the Eastern and Western Oceans at Brunei, with no clear understanding of where the Western Oceans to which Zheng He sailed were actually located. It is therefore important to make clear that the Western Oceans in his time referred to the Indian Ocean, before moving on to investigate the purpose of the voyages and related historical issues. Even more important is to point out that Zheng He’s expeditions in the early fifteenth century reflected that Chinese people took to the seas on a scale larger than ever before and joined the maritime and overland silk routes together. The place where this occurred was the Indian Ocean.
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Brown, J., C. A. Clayson, L. Kantha y T. Rojsiraphisal. "North Indian Ocean variability during the Indian Ocean dipole". Ocean Science Discussions 5, n.º 2 (9 de junio de 2008): 213–53. http://dx.doi.org/10.5194/osd-5-213-2008.

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Abstract. The circulation in the North Indian Ocean (NIO henceforth) is highly seasonally variable. Periodically reversing monsoon winds (southwesterly during summer and northeasterly during winter) give rise to seasonally reversing current systems off the coast of Somalia and India. In addition to this annual monsoon cycle, the NIO circulation varies semiannually because of equatorial currents reversing four times each year. These descriptions are typical, but how does the NIO circulation behave during anomalous years, during an Indian Ocean dipole (IOD) for instance? Unfortunately, in situ observational data are rather sparse and reliance has to be placed on numerical models to understand this variability. In this paper, we estimate the surface current variability from a 12-year hindcast of the NIO for 1993–2004 using a 1/2° resolution circulation model that assimilates both altimetric sea surface height anomalies and sea surface temperature. Presented in this paper is an examination of surface currents in the NIO basin during the IOD. During the non-IOD period of 2000–2004, the typical equatorial circulation of the NIO reverses four times each year and transports water across the basin preventing a large sea surface temperature difference between the western and eastern NIO. Conversely, IOD years are noted for strong easterly and westerly wind outbursts along the equator. The impact of these outbursts on the NIO circulation is to reverse the direction of the currents – when compared to non-IOD years – during the summer for negative IOD events (1996 and 1998) and during the fall for positive IOD events (1994 and 1997). This reversal of current direction leads to large temperature differences between the western and eastern NIO.
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Han, Weiqing, Jérôme Vialard, Michael J. McPhaden, Tong Lee, Yukio Masumoto, Ming Feng y Will P. M. de Ruijter. "Indian Ocean Decadal Variability: A Review". Bulletin of the American Meteorological Society 95, n.º 11 (1 de noviembre de 2014): 1679–703. http://dx.doi.org/10.1175/bams-d-13-00028.1.

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The international scientific community has highlighted decadal and multidecadal climate variability as a priority area for climate research. The Indian Ocean rim region is home to one-third of the world's population, mostly living in developing countries that are vulnerable to climate variability and to the increasing pressure of anthropogenic climate change. Yet, while prominent decadal and multidecadal variations occur in the Indian Ocean, they have been less studied than those in the Pacific and Atlantic Oceans. This paper reviews existing literature on these Indian Ocean variations, including observational evidence, physical mechanisms, and climatic impacts. This paper also identifies major issues and challenges for future Indian Ocean research on decadal and multidecadal variability.
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7

Kapur, Ashok y Robert H. Bruce. "The Modern Indian Navy and the Indian Ocean: Studies in Indian Ocean". Pacific Affairs 63, n.º 3 (1990): 398. http://dx.doi.org/10.2307/2759541.

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Phillips, Helen E., Amit Tandon, Ryo Furue, Raleigh Hood, Caroline C. Ummenhofer, Jessica A. Benthuysen, Viviane Menezes et al. "Progress in understanding of Indian Ocean circulation, variability, air–sea exchange, and impacts on biogeochemistry". Ocean Science 17, n.º 6 (26 de noviembre de 2021): 1677–751. http://dx.doi.org/10.5194/os-17-1677-2021.

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Abstract. Over the past decade, our understanding of the Indian Ocean has advanced through concerted efforts toward measuring the ocean circulation and air–sea exchanges, detecting changes in water masses, and linking physical processes to ecologically important variables. New circulation pathways and mechanisms have been discovered that control atmospheric and oceanic mean state and variability. This review brings together new understanding of the ocean–atmosphere system in the Indian Ocean since the last comprehensive review, describing the Indian Ocean circulation patterns, air–sea interactions, and climate variability. Coordinated international focus on the Indian Ocean has motivated the application of new technologies to deliver higher-resolution observations and models of Indian Ocean processes. As a result we are discovering the importance of small-scale processes in setting the large-scale gradients and circulation, interactions between physical and biogeochemical processes, interactions between boundary currents and the interior, and interactions between the surface and the deep ocean. A newly discovered regional climate mode in the southeast Indian Ocean, the Ningaloo Niño, has instigated more regional air–sea coupling and marine heatwave research in the global oceans. In the last decade, we have seen rapid warming of the Indian Ocean overlaid with extremes in the form of marine heatwaves. These events have motivated studies that have delivered new insight into the variability in ocean heat content and exchanges in the Indian Ocean and have highlighted the critical role of the Indian Ocean as a clearing house for anthropogenic heat. This synthesis paper reviews the advances in these areas in the last decade.
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9

Watanabe, Hiromi Kayama, Chong Chen, Daniel P. Marie, Ken Takai, Katsunori Fujikura y Benny K. K. Chan. "Phylogeography of hydrothermal vent stalked barnacles: a new species fills a gap in the Indian Ocean ‘dispersal corridor’ hypothesis". Royal Society Open Science 5, n.º 4 (abril de 2018): 172408. http://dx.doi.org/10.1098/rsos.172408.

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Phylogeography of animals provides clues to processes governing their evolution and diversification. The Indian Ocean has been hypothesized as a ‘dispersal corridor’ connecting hydrothermal vent fauna of Atlantic and Pacific oceans. Stalked barnacles of the family Eolepadidae are common associates of deep-sea vents in Southern, Pacific and Indian oceans, and the family is an ideal group for testing this hypothesis. Here, we describe Neolepas marisindica sp. nov. from the Indian Ocean, distinguished from N. zevinae and N. rapanuii by having a tridentoid mandible in which the second tooth lacks small elongated teeth. Morphological variations suggest that environmental differences result in phenotypic plasticity in the capitulum and scales on the peduncle in eolepadids. We suggest that diagnostic characters in Eolepadidae should be based mainly on more reliable arthropodal characters and DNA barcoding, while the plate arrangement should be used carefully with their intraspecific variation in mind. We show morphologically that Neolepas specimens collected from the South West Indian Ridge, the South East Indian Ridge and the Central Indian Ridge belong to the new species. Molecular phylogeny and fossil evidence indicated that Neolepas migrated from the southern Pacific to the Indian Ocean through the Southern Ocean, providing key evidence against the ‘dispersal corridor’ hypothesis. Exploration of the South East Indian Ridge is urgently required to understand vent biogeography in the Indian Ocean.
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10

Meehl, Gerald A., Julie M. Arblaster y Johannes Loschnigg. "Coupled Ocean–Atmosphere Dynamical Processes in the Tropical Indian and Pacific Oceans and the TBO". Journal of Climate 16, n.º 13 (1 de julio de 2003): 2138–58. http://dx.doi.org/10.1175/2767.1.

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Abstract The transitions (from relatively strong to relatively weak monsoon) in the tropospheric biennial oscillation (TBO) occur in northern spring for the south Asian or Indian monsoon and northern fall for the Australian monsoon involving coupled land–atmosphere–ocean processes over a large area of the Indo-Pacific region. Transitions from March–May (MAM) to June–September (JJAS) tend to set the system for the next year, with a transition to the opposite sign the following year. Previous analyses of observed data and GCM sensitivity experiments have demonstrated that the TBO (with roughly a 2–3-yr period) encompasses most ENSO years (with their well-known biennial tendency). In addition, there are other years, including many Indian Ocean dipole (or zonal mode) events, that contribute to biennial transitions. Results presented here from observations for composites of TBO evolution confirm earlier results that the Indian and Pacific SST forcings are more dominant in the TBO than circulation and meridional temperature gradient anomalies over Asia. A fundamental element of the TBO is the large-scale east–west atmospheric circulation (the Walker circulation) that links anomalous convection and precipitation, winds, and ocean dynamics across the Indian and Pacific sectors. This circulation connects convection over the Asian–Australian monsoon regions both to the central and eastern Pacific (the eastern Walker cell), and to the central and western Indian Ocean (the western Walker cell). Analyses of upper-ocean data confirm previous results and show that ENSO El Niño and La Niña events as well as Indian Ocean SST dipole (or zonal mode) events are often large-amplitude excursions of the TBO in the tropical Pacific and Indian Oceans, respectively, associated with anomalous eastern and western Walker cell circulations, coupled ocean dynamics, and upper-ocean temperature and heat content anomalies. Other years with similar but lower-amplitude signals in the tropical Pacific and Indian Oceans also contribute to the TBO. Observed upper-ocean data for the Indian Ocean show that slowly eastward-propagating equatorial ocean heat content anomalies, westward-propagating ocean Rossby waves south of the equator, and anomalous cross-equatorial ocean heat transports contribute to the heat content anomalies in the Indian Ocean and thus to the ocean memory and consequent SST anomalies, which are an essential part of the TBO.
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Tesis sobre el tema "Indian Ocean"

1

Elfadli, Kasem. "Indian Ocean Dipole impacts on northwestern Indian Ocean climate variability". Thesis, University of Southampton, 2015. https://eprints.soton.ac.uk/396586/.

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The Indian Ocean Dipole (IOD) is a coupled ocean-atmosphere phenomenon in the equatorial Indian Ocean, with a positive mode characterized by anomalous warming of sea surface temperatures in the west and anomalous cooling in the east. The IOD has been shown to affect inter-annual variability of the Indian monsoon. There is also evidence that the IOD may affect the formation, strength and duration of monsoon-related oceanic features in the North West Indian Ocean (NWIO), including fronts and eddies, the Somali upwelling and the ‘Great Whirl’ system. However, the mechanism by which the IOD develops and details of its connection with monsoon-related oceanic phenomena in the NWIO remain unclear. Satellite datasets of sea surface temperature anomalies (SSTA) and sea surface height anomalies (SSHA) over the past two decades have been examined, mainly to investigate the relationship between the IOD and large-scale climate modes like the Indian monsoon, El Niño Southern Oscillation (ENSO) and Rossby/Kelvin Waves. Early results show SSHA in NWIO; is more correlated with the IOD than with the ENSO. Also the results indicate an impact of Rossby wave patterns on the Somali Current system. Satellite datasets of sea surface temperature anomalies (SSTA) and sea surface height anomalies (SSHA) over the past two decades have been examined, mainly to investigate the relationship between the IOD and large-scale climate modes like the Indian monsoon, El Niño Southern Oscillation (ENSO) and Rossby/Kelvin Waves. Early results show SSHA in NWIO; is more correlated with the IOD than with the ENSO. Also the results indicate an impact of Rossby wave patterns on the Somali Current system. Satellite datasets of sea surface temperature anomalies (SSTA) and sea surface height anomalies (SSHA) over the past two decades have been examined, mainly to investigate the relationship between the IOD and large-scale climate modes like the Indian monsoon, El Niño Southern Oscillation (ENSO) and Rossby/Kelvin Waves. Early results show SSHA in NWIO; is more correlated with the IOD than with the ENSO. Also the results indicate an impact of Rossby wave patterns on the Somali Current system.
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2

Haynes, Annette M. "Indian naval development power projection in the Indian Ocean? /". Thesis, Monterey, California : Naval Postgraduate School, 1990. http://handle.dtic.mil/100.2/ADA242460.

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Thesis (M.S. in National Security Affairs)--Naval Postgraduate School, December 1990.
Thesis Advisor(s): Winterford, David. Second Reader: Wood, Glynn. "December 1990." Description based on title screen as viewed on March 31, 2010. DTIC Identifier(s): India, Naval Plalnning, Military Forces (United States), Military Force (Foreign), Foreign Policy, Pakistan, China, Indian Ocean, Power Projection, Theses. Author(s) subject terms: India, Pakistan, China, United States, Soviet Union, Foreign Policy, Military, Indian Naval Development, Power Projection. Includes bibliographical references. Also available in print.
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Gibbons, Ana D. "Regional plate tectonic reconstructions of the Indian Ocean". Thesis, The University of Sydney, 2012. http://hdl.handle.net/2123/8580.

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This thesis outlines and tackles the major outstanding issues of early Indian Ocean plate tectonic reconstructions using recent advancements in data and technology. The first chapter is focussed on the original extent of Greater India, using information from the abyssal plains offshore West Australia to incorporate tectonic boundaries that include several major submarine plateaus. In this chapter we also describe the methods employed to construct our plate kinematic models. The second chapter investigates the seafloor off East Antarctica, relating it to the conjugate seafloor off East India, where there are several anomalous tectonic features, with disputed origins. This chapter also solves the enigmatic, curved fracture zones located several kilometres off West Australia and East Antarctica, and predicts a diachronous separation between Madagascar and India. The final chapter investigates the implications of the plate reconstruction model further afield, matching the accretions of Greater India, Argoland and various Tethyan oceanic arcs, to the geological evidence in the Eurasia and Southeast Asian margins.
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Hermes, Juliet C. "Ocean model diagnosis of variability in the South Indian Ocean". Doctoral thesis, University of Cape Town, 2005. http://hdl.handle.net/11427/8649.

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Includes bibliographical references (leaves 180-195).
Evidence exists that sea surface temperature (SST) variability in the South Indian Ocean may significantly influence weather and climate patterns in the southern African region. SST, in tum, can be influenced by variability in ocean fluxes, observations of which are limited in the South Indian Ocean and it is necessary to augment them with estimates derived from models. Two sets of variability in this region are examined in this thesis. The first concerns the large-scale interannual variability of the oceans neighbouring South Africa and the second, inter-ocean fluxes south of Africa on meso-through to interannual timescales. In terms of the former, a global ocean model forced with 50 years of NCEP (National Centre for Environmental Prediction) re-analyses winds and heat fluxes, has been used to investigate the evolution and forcing of interannual SST variability in the South Indian Ocean and co-variability patterns in the South Atlantic. Secondly, an eddy- permitting model is used to investigate volume, heat and salt fluxes in the oceanic region south of Africa and the effect of variations in the strength of wind forcing. Interannual dipole-like SST variability in the South Indian and South Atlantic Oceans were realistically simulated using the global ocean model, ORCA2. The model results imply that there are connections between large-scale modulations of the midlatitude atmospheric circulation of the Southern Hemisphere and co-evolving SST variability in the South Atlantic and South Indian Oceans. The atmospheric variability results in an increase (decrease) in strength of the anticyclonic wind fields over each ocean during positive (negative) dipole events. The resulting wind anomalies lead to changes in surface heat fluxes, short wave radiation, meridional Ekman heat transport and upwelling, all of which contribute to the evolution of these SST dipole patterns. Evidence is found of links between these dipole patterns and the Antarctic Oscillation and ENSO (El Niño Southern Oscillation).
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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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Rana, Haris Sarwar. "Indian Ocean surface circulations and their connection to Indian Ocean dipole, identified from Ocean Surface Currents Analysis Real Time (OSCAR) data". Thesis, Monterey, Calif. : Naval Postgraduate School, 2008. http://handle.dtic.mil/100.2/ADA483452.

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Thesis (M.S. in Physical Oceanography)--Naval Postgraduate School, June 2008.
Thesis Advisor(s): Chu, Peter C. "June 2008." Description based on title screen as viewed on August 26, 2008. Includes bibliographical references (p. 67-71). Also available in print.
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7

Ly, Tio Fane-Pineo Huguette. "Chinese diaspora in Western Indian Ocean /". [Rose Hill : [Mauritius] : Mauritius] : Éditions de l'Océan Indien ; Chinese catholic mission, 1985. http://catalogue.bnf.fr/ark:/12148/cb36631208d.

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Que, Wen Jun. "String of pearls, myth or reality? : Sino-Indian interaction in Indian Ocean". Thesis, University of Macau, 2012. http://umaclib3.umac.mo/record=b2595577.

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Sparrow, Michael Dylan. "Current structure of the South Indian Ocean". Thesis, University of East Anglia, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.309941.

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Tabrez, Ali Rashid. "Slope sedimentation around the NW Indian Ocean". Thesis, University of Southampton, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.295607.

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Libros sobre el tema "Indian Ocean"

1

Indian Ocean. Minneapolis, MN: Bellwether Media, Inc., 2016.

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2

Spilsbury, Louise. Indian Ocean. London: Raintree, 2015.

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3

Prevost, John F. Indian Ocean. Minneapolis: Abdo Pub. Co., 2003.

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4

Green, Jen. Indian Ocean. Milwaukee, WI: World Almanac Library, 2006.

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5

W, Gotthold Donald, ed. Indian Ocean. Oxford, England: Clio Press, 1988.

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Gupta, Manoj. Indian Ocean Region. New York, NY: Springer New York, 2010. http://dx.doi.org/10.1007/978-1-4419-5989-8.

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Gray, Susan Heinrichs. The Indian Ocean. Chicago: Childrens Press, 1986.

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8

Pam, Max. Indian Ocean journals. Göttingen: Steidl, 2000.

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Taylor, L. R. The Indian Ocean. Woodbridge, Conn: Blackbirch Press, 1999.

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10

United States. Dept. of State. Bureau of Public Affairs, ed. Indian Ocean region. [Washington, D.C.?]: Bureau of Public Affairs, Dept. of State, 1987.

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Capítulos de libros sobre el tema "Indian Ocean"

1

Bird, Eric C. F. "Indian Ocean". En The World’s Coasts: Online, 1288–302. Dordrecht: Springer Netherlands, 2003. http://dx.doi.org/10.1007/0-306-48369-6_19.

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Mukherjee, Rila. "Seeing the Indian Ocean". En India in the Indian Ocean World, 27–58. Singapore: Springer Singapore, 2022. http://dx.doi.org/10.1007/978-981-16-6581-3_2.

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Kumar, Yogendra. "India and the Indian Ocean". En India's Foreign Policy: Surviving in a Turbulent World, 357–72. B1/I-1 Mohan Cooperative Industrial Area, Mathura Road New Delhi 110 044: SAGE Publications Pvt Ltd, 2020. http://dx.doi.org/10.4135/9789353885793.n22.

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Morris, Michael A. "The Indian Ocean". En Expansion of Third-World Navies, 229–41. London: Palgrave Macmillan UK, 1987. http://dx.doi.org/10.1007/978-1-349-08821-8_11.

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Naqvi, S. W. A. "Indian Ocean Margins". En Global Change – The IGBP Series, 171–210. Berlin, Heidelberg: Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-540-92735-8_4.

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Poh, Wong Poh. "Indian Ocean Islands". En Encyclopedia of the World's Coastal Landforms, 1097–110. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-1-4020-8639-7_205.

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Natland, James. "Indian ocean crust". En Oceanic Basalts, 289–310. Boston, MA: Springer US, 1991. http://dx.doi.org/10.1007/978-1-4615-3540-9_12.

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Montaggioni, Lucien F. "Western Indian Ocean". En Encyclopedia of Modern Coral Reefs, 1184–86. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2639-2_167.

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Gischler, Eberhard. "Indian Ocean Reefs". En Encyclopedia of Modern Coral Reefs, 586–94. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2639-2_96.

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Natland, James. "Indian ocean crust". En Oceanic Basalts, 289–310. Dordrecht: Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3042-4_12.

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Actas de conferencias sobre el tema "Indian Ocean"

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Андрианова, О., O. Andrianova, А. Батырев, A. Batyrev, Р. Белевич y R. Belevich. "TRENDS OF THE INTERANNUAL FLUCTUATIONS IN THE WORLD OCEAN LEVEL DURING THE LAST CENTURY". En Sea Coasts – Evolution ecology, economy. Academus Publishing, 2018. http://dx.doi.org/10.31519/conferencearticle_5b5ce386bb7293.29087345.

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The changes of the sea level in the Atlantic, Pacific, Indian Oceans and the whole World Ocean for the period from 1880 till 2010 years were examined. The estimates of the values of the sea level increasing for that time period in each of the oceans and on the west and east coasts of the Atlantic and Pacific oceans were made. For this purpose, the annual sea level data were averaged over years for 68 stations in the Atlantic Ocean, 71 stations – in the Pacific and 33 stations – the Indian. Analysis of the temporary distributions of the sea level shows that increasing of the Atlantic sea level during that period (131 years) is 24,2 cm. Sea levels of Pacific and Indian Oceans during the same period increased on smaller value, 14,5 and 12,4 cm respectively. The reason for difference between the Atlantic and the Pacific Ocean in values of sea level rising, as it seems, is significant rising of the land (raising of the East coast of the Asian continent), which was occurred in about half of the stations on the west coast of the Pacific. In the Indian Ocean the zero level of water posts was not correct for many stations, and in some cases there were low quality data. The highest maxima in the sea level in the generalized curves of the temporary distributions appear with about 10-year cycles on the sea level of all oceans that is in good correlation with El Niño years.
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Behera, Manasa Ranjan, K. Murali y V. Sundar. "Modeling of the Indian Ocean Tsunami". En ASME 2007 26th International Conference on Offshore Mechanics and Arctic Engineering. ASMEDC, 2007. http://dx.doi.org/10.1115/omae2007-29691.

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Shallow Water Equations are solved using an Unstructured Explicit Finite Element Method (UEFEM) to simulate long waves in the ocean. The formulation of the UEFEM has been described and found to be computationally efficient for large problems such as basin level modeling of tsunamis. Different domains have been considered to simulate the propagation of the waves due to an artificially imposed initial disturbance. The domain of Bay of Bengal has been considered for simulation with an initial disturbance which resembles the type and location of the 2004 Indian Ocean Tsunami. The Wave elevation and deformations as well as time of travel of tsunami are reproduced. The method hence has high potential of being attractive for application of simulation of global tsunamis.
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Masumoto, Y., Y. Masumoto, Y. Masumoto, Y. Masumoto, Y. Masumoto, Y. Masumoto, Y. Masumoto et al. "Observing Systems in the Indian Ocean". En OceanObs'09: Sustained Ocean Observations and Information for Society. European Space Agency, 2010. http://dx.doi.org/10.5270/oceanobs09.cwp.60.

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Swain, D. y Samar K. Ghose. "Latent and Sensible heat flux variation in north Indian Ocean during ENSO and Indian Ocean dipole years". En 2020 XXXIIIrd General Assembly and Scientific Symposium of the International Union of Radio Science (URSI GASS). IEEE, 2020. http://dx.doi.org/10.23919/ursigass49373.2020.9232005.

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Roueff, A., M. Aupetit, Y. Cansi y P. F. Piserchia. "Discrimination of events in the Indian Ocean". En Oceans 2005 - Europe. IEEE, 2005. http://dx.doi.org/10.1109/oceanse.2005.1513214.

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Kalcic, M. "Indian Ocean GDEM Development: Editing the Data". En OCEANS '86. IEEE, 1986. http://dx.doi.org/10.1109/oceans.1986.1160319.

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Heidarzadeh, Mohammad, Moharram D. Pirooz y Nasser H. Zaker. "Tsunami Hazards in the Northwestern Indian Ocean". En ASME 2008 27th International Conference on Offshore Mechanics and Arctic Engineering. ASMEDC, 2008. http://dx.doi.org/10.1115/omae2008-57837.

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Although northwestern Indian Ocean has experienced some deadly tsunamis in the past, this region remains one of the least studied regions in the world and little research work has been devoted to its tsunami hazard assessment. In this study, we compile and analyze historical tsunami in the northwestern Indian Ocean and present a tsunami list for this region. Then, a deterministic method has been employed to give a preliminary estimation of the tsunami hazard faced by different coastlines in this region. Different source scenarios are considered and for each scenario, numerical modeling of tsunami is performed. For each case, the maximum positive tsunami wave heights along the coasts are calculated which provide a preliminary estimation of tsunami hazard and show which locations face the greatest threat from a large tsunami.
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Mahajan, Akshath, Deap Daru, Aditya Thaker, Meera Narvekar y Debajyoti Mukhopadhyay. "Forecasting North Indian Ocean Tropical Cyclone Intensity". En 2022 Smart Technologies, Communication and Robotics (STCR). IEEE, 2022. http://dx.doi.org/10.1109/stcr55312.2022.10009275.

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Amaranti, P., R. Mau y J. Tedesco. "Rottnest Island, Indian Ocean: moving towards sustainability". En SUSTAINABLE DEVELOPMENT AND PLANNING 2013. Southampton, UK: WIT Press, 2013. http://dx.doi.org/10.2495/sdp130321.

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Ponomarev, Vladimir, Vladimir Ponomarev, Elena Dmitrieva, Elena Dmitrieva, Svetlana Shkorba, Svetlana Shkorba, Irina Mashkina, Irina Mashkina, Alexander Karnaukhov y Alexander Karnaukhov. "CLIMATIC REGIME CHANGE IN THE ASIAN PACIFIC REGION, INDIAN AND SOUTHERN OCEANS AT THE END OF THE 20TH CENTURY". En Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b9475504153.46587602.

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Multiple scale climate variability in Asia of temperate and high latitudes, Pacific, Indian and South Oceans, their features and linkages are studied by using statistical analyses of monthly mean time series of Hadley, Reynolds SST, surface net heat flux (Q), atmospheric pressure (SLP), air temperature (SAT) from NCEP NCAR reanalyses (1948-2015). Three multidecadal climatic regimes were revealed for the whole area studied by using cluster analyses via Principal Components of differences between values of Q, SLP, SAT in tropical and extratropical regions of the Asian Pacific, Indian and Southern Oceans. The climate regime change in 70s of the 20th century in this area is confirmed by this method. It is also found that the climate regime is significantly changed at the end of the 20th century in both same area and World Ocean. The characteristic features of recent climate regime after 1996-1998 are SLP increase in the central extratropic area of Indian Ocean, North and South Pacific being prevailing in boreal winter. It is accompanying SLP increase and precipitation decrease in South Siberia and Mongolia prevailing in boreal summer. Inversed SLP and precipitation anomaly associated with increase of cyclone activity and extreme events in the land-ocean marginal zones including Southern Ocean, eastern Arctic, eastern Indian, western and eastern Pacific margins. It is known that low frequency PDO phase is also changed at the same time.
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Informes sobre el tema "Indian Ocean"

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Rusina, Tamara. Map of Indian Ocean. Editado por Nikolay Komedchikov y Aleksandr Khropov. Entsiklopediya, enero de 2010. http://dx.doi.org/10.15356/dm2015-12-02-14.

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Regeon, Paul y Wallace Harrison. Indian Ocean METOC Imager. Fort Belvoir, VA: Defense Technical Information Center, septiembre de 2002. http://dx.doi.org/10.21236/ada633970.

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Hashmi, Syed Kamran Hamid. Major Powers’ Interests in IOR including Partnerships like QUAD, AUKUS, etc., and Implications for the Region especially for Pakistan. National Institute of Maritime Affairs (NIMA), marzo de 2023. http://dx.doi.org/10.53963/mpip.2023.978.969.nima003.

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Geo-economics and geopolitics are the indicators of competition between major powers in the pursuit of their strategic goals. The US, China, and India together make up about half of the world's GDP and are vying for dominance in the Indian Ocean. In this perspective, while being smaller than Pacific and Atlantic Oceans, Indian Ocean Region continues to be crucial because of its enormous oil and gas reserves, choke points, nautical traffic, and the interests of foreign powers. The US and Europe are heading for recession, and the Asian economic situation is better, China and India will be major engine of growth this year. Therefore, Indian Ocean will remain the focus of attention for the world. New alliances are taking place in which US and India are the key players, the sole aim being is to contain China. On the other end, China’s presence in Indian Ocean is increased in the last decade due to BRI/CPEC and military base in Djibouti. Chinese Navy is regularly patrolling and exercising with the littoral countries of the Indian Ocean. This paper endeavors to study major powers’ interests in IOR and how developing a strategic alliance requires Pakistan to be vigilant and adopt a strategy to safeguard its interests.
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Samaranayake, Nilanthi, Catherine Lea y Dmitry Gorenburg. Improving U.S.-India HA/DR Coordination in the Indian Ocean. Fort Belvoir, VA: Defense Technical Information Center, julio de 2014. http://dx.doi.org/10.21236/ada608782.

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Olson, Donald B. Theory and Observation of Ocean Fronts: Indian Ocean Drifters. Fort Belvoir, VA: Defense Technical Information Center, octubre de 1995. http://dx.doi.org/10.21236/ada306623.

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Sen Gupta, A. K. Strategic Importance of Indian Ocean Region. Fort Belvoir, VA: Defense Technical Information Center, marzo de 1988. http://dx.doi.org/10.21236/ada192367.

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Christopher Andrew Surman, Christopher Andrew Surman. Where is this vulnerable Indian Ocean seabird feeding? Using micro-GPS to track seabirds in the Indian Ocean. Experiment, junio de 2016. http://dx.doi.org/10.18258/7305.

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Sepanski, R. J. Indian Ocean radiocarbon: Data from the INDIGO 1, 2, and 3 cruises. Office of Scientific and Technical Information (OSTI), enero de 1991. http://dx.doi.org/10.2172/5896261.

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McCreary, Julian P. y Pijush K. Kindu. Modelling of the Circulation of the Western Indian Ocean. Fort Belvoir, VA: Defense Technical Information Center, enero de 1988. http://dx.doi.org/10.21236/ada204876.

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McCreary, Jr y Julian P. Mixed-Layer Parameterization in Models of the Indian Ocean. Fort Belvoir, VA: Defense Technical Information Center, septiembre de 1992. http://dx.doi.org/10.21236/ada255937.

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