Дисертації з теми "Oceano Indiano"
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SCHIERANO, PAOLA. "Da Mayotte a La Réunion. Mobilità, convivenze e fratture in due Oltremare europei (Oceano Indiano)." Doctoral thesis, Università degli Studi di Milano-Bicocca, 2021. http://hdl.handle.net/10281/329921.
Повний текст джерелаThe islands of La Réunion and Mayotte, located in the heart of the southwestern Indian Ocean, represent the "France of the Indian Ocean": these two Overseas Departments and Outermost Regions of Europe are very different from each other, but they share a relative prosperity that makes them an attractive destination for migrants in the area. Crystallized in a sui generis postcolonial situation until 2011, when it became the 101st French Department, the island of Mayotte is crossing important social, cultural and structural transformations nowadays, strongly intertwined with its political history and geographical location. Mayotte’s departmentalization process has contributed to profoundly modifying the way to « be Mahorais » on the island and elsewhere. Despite the efforts to reduce structural backwardness, Mayotte remains France’s poorest Department: the migration crisis linked to the rapid population growth, structural shortages and deep economic and social inequalities set up a chain reaction that brought a large number of Mahorais to move to La Réunion to improve their life conditions. Most of Mahorais families have mobility life stories reflecting the outcomes of postcolonial splitting boundaries. The impact of assimilation mechanisms – required by the institutional alignment program recently launched – is evident at structural level in Mayotte, but at cultural and social level the impact is less obvious. On the contrary, strong signals of Westernization can be observed among the lifestyles of Mahorais families permanently resident in La Réunion. Mobility experiences seems to multiplicated identity markers among Mahorais young people contributing to the creation of a generational fracture with the elders. Mahorais community in La Réunion face integration and stigmatisation problems because of their particular linguistic and cultural specificities, unknown or misunderstood by most Reunionese people. It appears, nevertheless, that social exclusion is not similarly experienced by the younger « Mahoreunioneses » – Mahorais born or raised in La Réunion – and by the elders, the « Pioneers » of mahorais mobility. The young « Mahoreunioneses » express a partial belonging to the two cultural systems which may contributing to a progressive integration of Mahorais in Réunionese society. The aim of the study, based on biographical approach and participant observation method, is to observe the short-term impact of Mayotte's departmentalization on regional mobility dynamics, as well as on collective representations of Mahorais group in La Réunion and their self-representation modalities. This socio-anthropological reflection highlights the different sense of belonging between the generations of Mahorais, as well as their strategies of adaptation and integration to reunionese context. In particular, this study aims to enhance understanding of how "mahority" (mahorité) is experienced by the community – on the island and on the move – influenced by migratory movements, leveraging on exogenous and endogenous pressures (attractions, resistances and reinventions).
LIUZZO, Marco. "Interazioni crosta-mantello e connessioni con il sistema geodinamico nell’origine e circolazione dei fluidi dell’Arcipelago delle Comore - Oceano Indiano." Doctoral thesis, Università degli studi di Ferrara, 2022. http://hdl.handle.net/11392/2486768.
Повний текст джерелаThe study area focuses on two islands of the Comoros archipelago, Grande Comore and Mayotte, located within the Mozambique Channel and in a complicated geodynamic system of great interest due to the volcanic and seismic activity that currently exists and of which a complete descriptive picture is currently lacking. In particular, there is still very limited knowledge of gas and fluid geochemistry. On Grande Comore, the focus was on the Karthala volcano, the most active volcano in the western Indian Ocean after Piton de la Fournaise in La Reunion. Karthala is a basaltic shield volcano that has erupted regularly over the last century, fourteen eruptions are listed from 1904 to the present, with the last eruption in 2007. The knowledge of the diffuse degassing of the Karthala volcano, with particular attention to the emission of CO2 from the flanks and of the summit fumarolic area is fundamental for the assessment of the state of activity of the volcano. Mayotte is the oldest island in the archipelago and no recent eruptions have been recorded since the last one around 2050 BC ± 500; however, volcanic activity in Mayotte is still present in the form of a large area of subaerial and underwater outgassing on the small island to the north-east of Mayotte: Petite Terre. Two areas of high outgassing are present here: the south-eastern beach (BAS); and Lake Dziani located in the northern part of the island of Petite Terre. The island was recently affected by a seismic crisis that lasted several months, and was accompanied by the formation of the largest submarine volcano in recent centuries, about 50 km from its coast. The thesis is divided into two sections: the first focuses on gas emissions from Karthala and the BAS area at Petite Terre, with the aim of identifying the main characteristics, similarities and differences; the second section of the thesis focuses on the difference between the two bubbling areas at Petite Terre, where the study of gas emissions from Lake Dziani, which have only been investigated in more recent surveys, will be included. The results of this thesis converge towards the recognition of some remarkable peculiarities: 1. Soil CO2 emissions are spatially distributed along the main structural features of both Grande Comore and Petite Terre; however, the carbon isotopic signature of soil CO2 emissions shows a low magmatic contribution in the distal areas of Karthala volcano, and vice-versa a higher magmatic contribution in CO2 emissions at Petite Terre, relative to the period of observation. 2. The helium isotopic signature is typically low and in the range of ~6 ≤ Rc/Ra ≤ ~7.5 at Petite Terre and ~4.6 ≤ Rc/Ra ≤ ~5.8 at Karthala. 3. The bubbling area on the sea (BAS) and at Dziani lake (Mayotte) are likely fed by a common source; however, Dziani lake is significantly affected by secondary processes that are mainly related to biotic activities in the lake, which result in the higher variability of gas chemistry, 13C in methane and CO2 than BAS. 4. The increased value of Rc/Ra between 2008 and 2018-19, and a not-reached isotopic equilibrium of 13CCH4 from the hydrothermal fluid, may be ascribed to the volcanic activity that generated the new submarine volcano 50 km offshore from Petite Terre. The latter consideration is also consistent with the final interpretation of this work, where the input of heated CO2-rich fluid into the Petite Terre hydrothermal system is a consequence of the perturbation of the shallow plumbing system by the offshore submarine eruption, resulting in higher equilibrium temperatures in 2018 and subsequent cooling down during and after the seismo-volcanic activity.
Elfadli, Kasem. "Indian Ocean Dipole impacts on northwestern Indian Ocean climate variability." Thesis, University of Southampton, 2015. https://eprints.soton.ac.uk/396586/.
Повний текст джерелаGibbons, Ana D. "Regional plate tectonic reconstructions of the Indian Ocean." Thesis, The University of Sydney, 2012. http://hdl.handle.net/2123/8580.
Повний текст джерелаMavume, Alberto Francisco. "Tropical cyclones in the South-West Indian Ocean : intensity changes, oceanic interaction and impacts." Doctoral thesis, University of Cape Town, 2008. http://hdl.handle.net/11427/11314.
Повний текст джерелаIncludes bibliographical references (p. 229-253).
This study investigates the climatology, intensification and ocean atmosphere interaction in relation to the passage of tropical cyclones (TCs) in the South-West Indian Ocean (SWIO). A Climatology of TCs in the SWIO including landfall in the area of Mozambique and Madagascar was developed for the 1952-2007 and 1980-2007 periods.
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.
Повний текст джерелаThesis 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.
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.
Повний текст джерелаEvidence 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).
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.
Повний текст джерелаLy, 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.
Повний текст джерелаAlevras, Dimitrios. "Simulating tsunamis in the Indian Ocean with real bathymetry by using a high-order triangular discontinuous Galerkin oceanic shallow water model." Thesis, Monterey, Calif. : Naval Postgraduate School, 2009. http://edocs.nps.edu/npspubs/scholarly/theses/2009/March/09Mar%5FAlevras.pdf.
Повний текст джерелаThesis Advisor(s): Giraldo, Francis X. ; Radko, Timour. "March 2009." Description based on title screen as viewed on April 24, 2009. Author(s) subject terms: Tsunami Simulation, Indian Ocean Tsunami 2004, Triangular Discontinuous Galerkin Method, Propagation stage, Oceanic Shallow Water Model. Includes bibliographical references (p. 91-93). Also available in print.
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.
Повний текст джерелаThesis 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.
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.
Повний текст джерелаZampierin, Daniele. "Multi-analytical characterization of ceramics from Dhofar (Southern Oman): provenance and trade." Master's thesis, Universidade de Évora, 2020. http://hdl.handle.net/10174/29046.
Повний текст джерелаSparrow, 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.
Повний текст джерелаTabrez, 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.
Повний текст джерелаBoersch-Supan, Philipp Hanno. "The ecology of scattering layer biota around Indian Ocean seamounts and islands." Thesis, University of St Andrews, 2014. http://hdl.handle.net/10023/11440.
Повний текст джерелаLong, Erik Christopher. "An analysis of an eddy-resolving global ocean model in the tropical Indian Ocean." Thesis, Monterey, California : Naval Postgraduate School, 1990. http://handle.dtic.mil/100.2/ADA241009.
Повний текст джерелаThesis Advisor(s): Semtner, Albert J. Jr. Second Reader: Batteen, Mary L. "September 1990." Description based on title screen as viewed on March 19, 2010. DTIC Descriptors: Climatology, Currents, Cycles, East (Direction), Equations, Equatorial Regions, Global, Heat Flux, Horizontal Orientation, Indian Ocean, Invariance, Mass, Mean, Models, Monsoons, Ocean Currents, Ocean Models, Resolution, Seasonal Variations, Simulation, Surface Temperature, Temperature, Tropical Regions, Velocity, West (Direction), Wind, Wind Stress. DTIC Identifier(s): Leeuwin Current. Author(s) subject terms: Oceanographic Numerical Modeling, Indian Ocean, Ocean General Circulation Model, Eddy-Resolving, Somali Current, Tropical, Equitorial. Includes bibliographical references (p. 137-143). Also available in print.
Achuthavarier, Deepthi. "Role of the Indian and Pacific Oceans in the Indian summer monsoon variability." Fairfax, VA : George Mason University, 2009. http://hdl.handle.net/1920/4524.
Повний текст джерелаVita: p. 179. Thesis director: V. Krishnamurthy. Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Climate Dynamics. Title from PDF t.p. (viewed June 10, 2009). Includes bibliographical references (p. 171-178). Also issued in print.
Mawren, Daneeja. "Upper ocean variability and tropical cyclones in the South West Indian Ocean." Doctoral thesis, University of Cape Town, 2018. http://hdl.handle.net/11427/29219.
Повний текст джерелаMellet, Bernice. "Ecological risk assessment of fisheries on sea turtles in the South Western Indian Ocean." Thesis, Nelson Mandela Metropolitan University, 2015. http://hdl.handle.net/10948/9957.
Повний текст джерелаSenan, Retish. "Intraseasonal Variability Of The Equatorial Indian Ocean Circulation." Thesis, Indian Institute Of Science, 2004. http://hdl.handle.net/2005/297.
Повний текст джерелаGood, Jonathan T. "The PLA Navy looks to the Indian Ocean." Thesis, Monterey, California. Naval Postgraduate School, 2002. http://hdl.handle.net/10945/6059.
Повний текст джерелаThis thesis examines the implications of China's security needs for the modernization and role of the People's Liberation Army Navy (PLAN). The main argument is that the expansion of China into a new maritime area of operation is likely to solidify Beijing's current regional relationships and possibly lead to a naval arms buildup in the Indian Ocean region. Although the 2001 Quadrennial Defense Review does not explicitly name China, its conclusion that a "military competitor with a formidable resource base will emerge" in Asia clearly implies that the United States will have to take into account China's aspirations to become a regional and potentially global maritime power in the 21st century.
Holbourn, Ann Elizabeth Lucette. "Lower cretaceous benthic formanifera of the Indian Ocean." Thesis, University College London (University of London), 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.336285.
Повний текст джерелаSands, Carla Marie. "Hydrothermal plumes and processes in the Indian Ocean." Thesis, University of Southampton, 2006. https://eprints.soton.ac.uk/48828/.
Повний текст джерелаWibawa, Teja Arief. "Modélisation globale et régionale de la dynamique de population du thon obèse de l'océan Indien avec le modèle SEAPODYM." Thesis, Toulouse 3, 2017. http://www.theses.fr/2017TOU30149/document.
Повний текст джерелаThe Indonesian tuna fishery has suffered from a management problem due to incomplete and less reliability of tuna data leading to lack of understanding about tuna population dynamics in its region. The government of Indonesia initiated the Infrastructure Development of Space Oceanography (INDESO) programme to support marine resource management and monitoring of the Country. One application concerns the tuna fisheries with a challenging objective of real-time and forecast modeling of three tuna species biomass distributions: bigeye, yellowfin and skipjack. The model used is SEAPODYM (Spatial Ecosystem and Population Dynamics Model). The present thesis is dealing with bigeye tuna only, and had three major objectives: the preparation of a geo-referenced fishing dataset, the production of initial conditions for the regional INDESO model configuration, and the simulation of regional population dynamics. The georeferenced fishing catch and effort dataset of the Indian Ocean bigeye tuna was standardized throughout five procedures: standardization of spatial resolution, conversion and standardization of catch and effort units, raising of geo-referenced catch to nominal catch level, screening and correction of outliers, and detection of major catchability changes over long time series of fishing data. . The standardized geo-referenced catch dataset covers two-third of total nominal catch due to lack of geographic references for several fishing fleets. The regional model was configured along three steps: the parameterization of coarse resolution model over a long historical period, the downscaling and parameterization of operational global configuration, and the downscaling to the operational regional model. The first step provided model parameterization over the Pacific and Indian Ocean for thirty-nine years period at 2° monthly resolution, allowing to establish initial conditions of the population for the second configuration starting in 1998 at resolution 1/4° weekly. This second model configuration required a downscaling method to revise the parameterization and achieve the same solution despite some differences in the physical forcing. This global operational model provided initial conditions of the population and open boundary conditions (OBCs) constraining the fluxes of fish through the regional borders of INDESO model (1/12° daily resolution). The standardized Indian Ocean fishing dataset was used for including fishing mortality and validate the optimization achieved in the Pacific Ocean. Model simulation outputs suggest that bigeye is distributed in higher concentration in the North Indian Ocean (north of 20°S), with an extension through the Mozambique Channel and along an eastward prolongation between 35° and 40°S.. The operational model configurations (global and regional) are using VGPM net primary production and euphotic depth derived from satellite data, and climatological dissolved oxygen monthly maps from the World Ocean Atlas (WOA) as biogeochemical forcings. A regional simulation using the INDESO biogeochemical PISCES model forcing as an alternative to the satellite derived products was tested. The preliminary results show that once the PISCES primary production is scaled to the VGPM mean value, both products provide similar results, suggesting that longer time scale forecast based on the coupled physical biogeochemical model can be proposed
Trampp, David A. "Upper Ocean Characteristics in the Tropical Indian Ocean from AXBT and AXCTD Measurements." Thesis, Monterey, California. Naval Postgraduate School, 2012. http://hdl.handle.net/10945/6882.
Повний текст джерелаMajodina, Mark. "The structure of the upper ocean, atmosphere and heat fluxes - Tropical Indian Ocean." Master's thesis, University of Cape Town, 1998. http://hdl.handle.net/11427/18489.
Повний текст джерелаCobb, Matthew Adam. "Roman trade in the Indian Ocean during the Principate." Thesis, Swansea University, 2011. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.678420.
Повний текст джерелаRojsiraphisal, Thaned. "A study of variability in the North Indian Ocean." Connect to online resource, 2007. http://gateway.proquest.com/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:3273676.
Повний текст джерелаKarunatilleke, Upali. "The law of the sea and the Indian ocean." Thesis, Southampton Solent University, 2004. http://ssudl.solent.ac.uk/775/.
Повний текст джерелаBuchanan, Sarah. "Seismicity and tectonics of the Central Indian Ocean Basin." Thesis, University of Edinburgh, 1998. http://hdl.handle.net/1842/13246.
Повний текст джерелаManyilizu, Majuto Clement. "Simulation of variability in the tropical Western Indian Ocean." Doctoral thesis, University of Cape Town, 2014. http://hdl.handle.net/11427/9310.
Повний текст джерелаThe oceanic circulation and properties in the Tanzanian shelf region in the tropical western Indian Ocean have been studied in this thesis using a regional ocean model. The study investigated the influences of the Northeast Madagascar Current (NEMC) in the Tanzanian shelf waters at the annual cycle. Furthermore, the thesis examined the interannual variability of the sea surface temperature (SST) in the Tanzanian shelf region, and compares it with that offshore or with subsurface temperature. At the annual cycle, the westward-flowing NEMC advects relatively warm and fresh waters from the north of Madagascar towards the Tanzanian shelf region by interrupting the upwelled water from the Seychelles-Chagos ridge. At interannual timescales, the weakest interannual SST variations, which lie over the weak subsurface waters variations, occur in the coastal waters off Tanzania, where its variance is shared with waters to the north of Madagascar. Such SST variations are dominated by variability at about five year periods. The strongest interannual SST variations, which lie over the strongest subsurface temperature variations, occur offshore, being dominated by two periods, one at about 2.7 and the other near five years. The interannual variability of the region seems to be linked to El Niño- Southern Oscillation (ENSO) and Indian Ocean Dipole (IOD) events, which induce changes in the thermocline and surface forcing in the region. Local surface heat flux exchanges driven by the anomalous shortwave radiation dominate the weakest interannual SST variability in the Tanzanian shelf region, with some contribution by the advection of heat anomalies from the NEMC. Further offshore, the strongest interannual variability of the SST is dominated by the thermocline variations induced by local Ekman pumping from local wind stress curl and by remote forcing from large-scale climate modes.|
Steele, Nikita. "Geographical variation in effects of nutrient levels and grazing intensity on community structure between upwelling and non-upwelling regions of South Africa." Thesis, Rhodes University, 2014. http://hdl.handle.net/10962/d1013013.
Повний текст джерелаCowburn, Benjamin. "Coral reefs and climate change in the Indian ocean : a case study of Watamu Marine National Park, Kenya and other Indian Ocean locations." Thesis, University of Oxford, 2015. https://ora.ox.ac.uk/objects/uuid:22c16252-bdf9-4724-a2f8-dbd4c6fe7f09.
Повний текст джерелаJohnson, Gregory Conrad. "Near-equatorial deep circulation in the Indian and Pacific Oceans /." Thesis, Woods Hole, Mass. : Woods Hole Oceanographic Institution, 1990. http://hdl.handle.net/1912/2637.
Повний текст джерелаFunding was provided by the Office of Naval Research and a Secretary of the Navy Graduate Fellowship in Oceanography. References : p. 117-121.
Hagan, Annelise Baugh. "Reef regeneration at Alphonse Atoll, western Indian Ocean following the 1997-98 ocean warming event." Thesis, University of Cambridge, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.599825.
Повний текст джерелаChen, Shuiming. "Vertical structure of mesoscale ocean currents in the Indian Ocean observation, numerical modeling and theory /." Thesis, University of Hawaii at Manoa, 2003. http://proquest.umi.com/pqdweb?index=0&did=765960941&SrchMode=2&sid=8&Fmt=2&VInst=PROD&VType=PQD&RQT=309&VName=PQD&TS=1209408688&clientId=23440.
Повний текст джерелаLayton, Simon. "Commerce, authority and piracy in the Indian Ocean world, c. 1780-1850." Thesis, University of Cambridge, 2013. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.608198.
Повний текст джерелаDay, John Frederick. "British Admiralty control and naval power in the Indian Ocean (1793-1815)." Thesis, University of Exeter, 2012. http://hdl.handle.net/10036/3919.
Повний текст джерелаMeuleners, Michael Joseph. "A numerical study of the mesoscale eddy dynamics of the Leeuwin Current system." University of Western Australia. School of Environmental Systems Engineering, 2007. http://theses.library.uwa.edu.au/adt-WU2007.0134.
Повний текст джерелаPOINT, GRAZIELLA. "Medecins du monde : ocean indien et madagascar." Clermont-Ferrand 1, 1994. http://www.theses.fr/1994CLF1M021.
Повний текст джерелаBader, Jürgen. "The role of the tropical Indian Ocean in global climate." [S.l. : s.n.], 2005. http://deposit.ddb.de/cgi-bin/dokserv?idn=974330051.
Повний текст джерелаCirano, Mauro School of Mathematics UNSW. "Wintertime Circulation within the Southeast Indian Ocean: a Numerical Study." Awarded by:University of New South Wales. School of Mathematics, 2000. http://handle.unsw.edu.au/1959.4/17820.
Повний текст джерелаBertram, Caroline Jane. "Rare earth elements and neodymium isotopes in the Indian Ocean." Thesis, University of Cambridge, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.277641.
Повний текст джерелаBull, Jonathan Mark. "The structural style of intraplate deformation, central Indian Ocean Basin." Thesis, University of Edinburgh, 1990. http://hdl.handle.net/1842/15535.
Повний текст джерелаMitchell, Kimbriel Armistead. "American strategic policy for the Indian Ocean area, 1970-1980." Thesis, London School of Economics and Political Science (University of London), 1991. http://etheses.lse.ac.uk/1149/.
Повний текст джерелаHuussen, Tycho Nout. "Is the Indian Ocean MOC driven by internal wave breaking?" Thesis, University of Southampton, 2010. https://eprints.soton.ac.uk/209663/.
Повний текст джерелаMotah, Beenesh Anand. "Environmental influences on tuna movement patterns in the Indian Ocean." Doctoral thesis, University of Cape Town, 2017. http://hdl.handle.net/11427/24518.
Повний текст джерелаParker, Bhawoodien Abbasmia. "Composite structure of tropical cyclones in the SW Indian Ocean." Master's thesis, University of Cape Town, 1994. http://hdl.handle.net/11427/19524.
Повний текст джерелаHughes, Lindsay. "A Rising Tide: The Growing Nuclearisation of the Indian Ocean." Thesis, Curtin University, 2021. http://hdl.handle.net/20.500.11937/86667.
Повний текст джерела