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Dissertations / Theses on the topic 'Eastern Equatorial Indian Ocean'

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Published: 4 June 2021

Last updated: 4 February 2022

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1

Ma, Ruifang. "Millennial-scale variations of the intermediate water circulation in the Indian Ocean since the last glacial period inferred from assemblages and geochemistry of benthic foraminifera." Thesis, Université Paris-Saclay (ComUE), 2019. http://www.theses.fr/2019SACLS159.

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L'objectif principal de cette thèse était de reconstituer l'évolution de la circulation intermédiaire depuis la dernière période glaciaire à partir de carottes de sédiments marins prélevées dans le golfe du Bengale GB, la Mer d’Arabie MA et l’océan Indien équatorial oriental OIEO. La stratégie scientifique mise en œuvre inclut l’étude des assemblages et de la géochimie des foraminifères benthiques, afin de reconstruire les changements de source et de ventilation des masses d’eau. Les résultats obtenus dans le GB ont permis de restituer les changements hydrologiques à profondeur intermédiaire à

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2

Senan, Retish. "Intraseasonal Variability Of The Equatorial Indian Ocean Circulation." Thesis, Indian Institute Of Science, 2004. http://hdl.handle.net/2005/297.

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Climatological winds over the equatorial Indian Ocean (EqlO) are westerly most of the year. Twice a year, in April-May ("spring") and October-December ("fall"), strong, sustained westerly winds generate eastward equatorial jets in the ocean. There are several unresolved issues related to the equatorial jets. They accelerate rapidly to speeds over lms"1 when westerly wind stress increases to about 0.7 dyne cm"2 in spring and fall, but decelerate while the wind stress continues to be westerly; each jet is followed by westward flow in the upper ocean lasting a month or longer. In addition to the

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3

Johnson, 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.

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Thesis (Ph. D.)--Woods Hole Oceanographic Institution and Massachusetts Institute of Technology, 1990.<br>Funding was provided by the Office of Naval Research and a Secretary of the Navy Graduate Fellowship in Oceanography. References : p. 117-121.

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4

Soares, Jacyra Ramos. "On the reflection of the equatorial waves at eastern ocean boundaries." Thesis, University of Southampton, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.239653.

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5

Chandana, K. R., Ravi Bhushan, and A. J. T. Jull. "Evidence of Poor Bottom Water Ventilation during LGM in the Equatorial Indian Ocean." FRONTIERS MEDIA SA, 2017. http://hdl.handle.net/10150/626606.

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Multi-proxy approach for the reconstruction of paleo-redox conditions is attempted on a radiocarbon (C-14) dated sediment core near the equatorial Indian Ocean. Based on the behavior and distribution of redox sensitive and productivity proxies, study demonstrates prevalence of anoxic bottom water conditions during LGM due to poorly ventilated bottom waters augmented by high surface productivity resulting in better preservation of organic carbon (OC). During early Holocene, the equatorial Indian Ocean witnessed high sedimentation rates resulting in high organic carbon (OC) with depleted redox s

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6

Hanson, Christine Elizabeth. "Oceanographic forcing of phytoplankton dynamics in the coastal eastern Indian Ocean." University of Western Australia. Centre for Water Research, 2004. http://theses.library.uwa.edu.au/adt-WU2005.0033.

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[Truncated abstract] This work was the first large-scale biological oceanographic study to be undertaken in the coastal eastern Indian Ocean adjacent to Western Australia, and covered both northwest (Exmouth Peninsula to the Abrolhos Islands) and southwest (Cape Naturaliste to Cape Leeuwin) regions. The study area was dominated by the Leeuwin Current (LC), an anomalous eastern boundary current that transports tropical water poleward and prevents deep nutrients from reaching the surface by creating large-scale downwelling. Indeed, LC and offshore waters were consistently associated with low nit

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7

Palacz, Artur Piotr. "Control Mechanisms in Nutrient Dynamics and Biological Productivity in the Eastern Equatorial Pacific Ocean." Fogler Library, University of Maine, 2011. http://www.library.umaine.edu/theses/pdf/PalaczA2011.pdf.

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8

Brookshire, Brian Neville Jr. "Character of the diatom assemblage spanning a depositional transition in the Eastern Equatorial Pacific Ocean at 6.6 Ma." Thesis, Texas A&M University, 2003. http://hdl.handle.net/1969.1/1626.

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Approximately 6.6 million years ago in the Eastern Equatorial Pacific a large increase in biogenic mass accumulation rates (MARs) occurred. This increased level of biogenic mass accumulation persisted until about 4.4 Ma at which time levels returned to those similar to before the transition at 6.6 Ma. The exact nature of the change that facilitated this transition in biogenic MARs, however, was not understood. Here we present the results of a study which characterizes the diatom assemblage spanning the depositional transition at 6.6 Ma from sediments taken from ODP Hole 850B. A close ins

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9

Brown, Jaclyn Nicole School of Mathematics UNSW. "The kinematics and dynamics of cross-hemispheric flow in the Central and Eastern Equatorial Pacific." Awarded by:University of New South Wales. School of Mathematics, 2005. http://handle.unsw.edu.au/1959.4/20831.

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This thesis concerns two topics: the kinematics of Pacific cross-equatorial flow ??? the location, timing and magnitude of the flow; and their dynamics???what are the driving forces controlling the flow? Despite extensive observations in the central and eastern Pacific, observations of these flows remain contradictory. We use output from an Ocean General Circulation Model (OGCM) viewed from a Lagrangian framework on density layers. This addresses the problem of high variability due to features such as Tropical Instability Waves. The annual mean flow is found to be southward nearly everywhere

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10

Krishnan, Tharishini. "Emerging security paradigm in the Eastern Indian Ocean Region : a blue ocean of Malaysia-India Maritime Security Cooperation." Thesis, King's College London (University of London), 2017. https://kclpure.kcl.ac.uk/portal/en/theses/emerging-security-paradigm-in-the-eastern-indian-ocean-region(8d16846f-34c0-4c0b-b986-4c90d09f28c5).html.

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This study investigates the emergence of Malaysia-India Maritime Security Cooperation (MIMSC) in response to traditional threats and non-traditional security threats at the Eastern Indian Ocean Region (EIOR). This thesis argues that although both Malaysia and India have identified the maritime significance of the EIOR to them, the common threat faced by them in that region, and have recognised the need for cooperation in maritime security, it appears at present that MIMSC in EIOR projects a lack of robustness in its engagement. This is despite both an appreciation of the relations between the

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11

Böschen, Tebke [Verfasser]. "Deglacial to Holocene Changes in Eastern Equatorial Pacific Upper‐Ocean Dynamics – Indications from Foraminiferal (Isotope) Geochemistry / Tebke Böschen." Kiel : Universitätsbibliothek Kiel, 2014. http://d-nb.info/1050808398/34.

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12

Swallow, Jane E. "Plio-Pleistocene paleoceanography of the Equatorial Indian Ocean : (quantitative and geochemical analyses of planktonic foraminifera from ODP Hole 709C." Thesis, University of East Anglia, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.306138.

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13

Bloomer, Stephen F. "Examination of the potential of seismic reflection data for paleoceanographic studies, case study from the eastern equatorial Pacific Ocean." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0033/NQ65452.pdf.

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14

Cardenas, Amores Jorge A. "Intraseasonal oscillations over the tropical western Pacific and eastern Indian Ocean for the northern summers of 1989-1991." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 1994. http://handle.dtic.mil/100.2/ADA284527.

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15

Wood, Marilee. "Interconnections : Glass beads and trade in southern and eastern Africa and the Indian Ocean - 7th to 16th centuries AD." Doctoral thesis, Uppsala universitet, Afrikansk och jämförande arkeologi, 2012. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-162650.

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Glass beads comprise the most frequently found evidence of trade between southern Africa and the greater Indian Oceanbetween the 7th and 16th centuries AD. In this thesis beads recovered from southern African archaeological sites are organized into series, based on morphology and chemical composition determined by LA-ICP-MS analysis. The results are used to interpret the trade patterns and partners that linked eastern Africa to the rest of the Indian Ocean world, as well as interconnections between southern Africa andEast Africa. Comprehensive reports on bead assemblages from several archa

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16

van, Dijk Jeroen. "Size and Abundance of Late Pleistocene Reticulofenestrid Coccoliths from the Eastern Indian Ocean in Relation to Temperature and Aridity." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-325273.

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Measurements on coccolith abundance and mass can be used as a signal of primary productivity and pelagic calcification in response to environmental change. The Leeuwin Current (LC) is known to transport warm and low-salinity waters from the Indo-Pacific Warm Pool (IPWP) southwards along the coast of West Australia. Along with the onset of continental aridity during late Neogene, increased strength of the LC may have played a role in reef expansion on the Northwest Shelf. In this study the morphological variation in size and mass of reticulofenestrid coccoliths was assessed in material from IOD

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17

Ranasinghage, Pradeep Nalaka. "Holocene Coastal Development in Southeastern-Eastern Sri Lanka: Paleo-Depositional Environments and Paleo-coastal Hazards." Kent State University / OhioLINK, 2010. http://rave.ohiolink.edu/etdc/view?acc_num=kent1286816740.

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18

Regenberg, Anke [Verfasser]. "Climate variability in the Eastern Indian Ocean during marine isotope stage 3 : high-resolution proxy studies from the Timor Sea / Anke Dürkop." Kiel : Universitätsbibliothek Kiel, 2010. http://d-nb.info/1019982810/34.

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19

Nguyen, Xuan Vy [Verfasser]. "Application of genetic markers for identification of Halophila members and genetic variation of Halophila ovalis from Western Pacific to Eastern Indian Ocean / Xuan Vy Nguyen." Hannover : Technische Informationsbibliothek und Universitätsbibliothek Hannover (TIB), 2014. http://d-nb.info/1057897493/34.

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20

Chen, Wenwen [Verfasser], Gesine [Akademischer Betreuer] Mollenhauer, and Heiko [Akademischer Betreuer] Pälike. "Temperature reconstructions for the Eastern Indian Ocean based on organic-geochemical proxies (UK' 37 and TEX86) / Wenwen Chen. Betreuer: Gesine Mollenhauer. Gutachter: Gesine Mollenhauer ; Heiko Pälike." Bremen : Staats- und Universitätsbibliothek Bremen, 2016. http://d-nb.info/1094955922/34.

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21

Setiawan, Riza [Verfasser], Dierk [Akademischer Betreuer] Hebbeln, and Heiko [Akademischer Betreuer] Pälike. "The role of the Sunda Strait in the glacial to Holocene development of the eastern tropical Indian Ocean hydrography / Riza Setiawan. Betreuer: Dierk Hebbeln. Gutachter: Dierk Hebbeln ; Heiko Pälike." Bremen : Staats- und Universitätsbibliothek Bremen, 2015. http://d-nb.info/1077864396/34.

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22

Tangunan, Deborah [Verfasser], Rüdiger [Akademischer Betreuer] Henrich, Rüdiger [Gutachter] Henrich, and Villarejo Jose Abel [Gutachter] Flores. "Late Neogene to Quaternary paleoproductivity of the western Indian Ocean and the eastern South Atlantic from coccolithophore assemblage and coccolith geochemistry / Deborah Tangunan ; Gutachter: Rüdiger Henrich, Jose Abel Flores Villarejo ; Betreuer: Rüdiger Henrich." Bremen : Staats- und Universitätsbibliothek Bremen, 2017. http://d-nb.info/115083398X/34.

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23

Domingues, Catia Motta, and Catia Domingues@csiro au. "Kinematics and Heat Budget of the Leeuwin Current." Flinders University. SOCPES, 2006. http://catalogue.flinders.edu.au./local/adt/public/adt-SFU20060612.211358.

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This study investigates the upper ocean circulation along the west Australian coast, based on recent observations (WOCE ICM6, 1994/96) and numerical output from the 1/6 degree Parallel Ocean Program model (POP11B 1993/97). Particularly, we identify the source regions of the Leeuwin Current, quantify its mean and seasonal variability in terms of volume, heat and salt transports, and examine its heat balance (cooling mechanism). This also leads to further understanding of the regional circulation associated with the Leeuwin Undercurrent, the Eastern Gyral Current and the southeast Indian Subtrop

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24

Jiang, Shijun. "Applications of calcareous nannofossils and stable isotopes to Cenozoic paleoceanography examples from the Eastern Equatorial Pacific, Western Equatorial Atlantic and Southern Indian Oceans /." 2007. http://etd.lib.fsu.edu/theses/available/etd-07262007-144559.

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Thesis (Ph. D.)--Florida State University, 2007.<br>Advisor: Sherwood W. Wise, Jr., Florida State University, College of Arts and Sciences, Dept. of Geological Sciences. Title and description from dissertation home page (viewed Mar. 26, 2008). Document formatted into pages; contains xvi, 173 pages. Includes bibliographical references.

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25

Robertson, Angela K. "EASTERN EQUATORIAL PACIFIC PRODUCTIVITY VIA TWO GEOCHEMICAL PROXIES." Thesis, 2012. http://hdl.handle.net/1805/2740.

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Indiana University-Purdue University Indianapolis (IUPUI)<br>Drivers that influence oceanic productivity are not clearly constrained. However, sea level changes during glacial cycles have been proposed as a potential driver for productivity variations observed over warm and cold climate periods. In order to determine this, additional oceanic paleoproductivity data collection is necessary to estimate the ocean’s feedback in response to a dynamic climate. The eastern equatorial Pacific (EEP) is an ideal site for productivity studies due to its high levels of nutrients and deep upwelling. Thi

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26

Singh, Ajay 1980. "Eastern Equatorial Pacific Ocean Sedimentation: Investigating Constant Flux Proxies." Thesis, 2012. http://hdl.handle.net/1969.1/148258.

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Age-model derived sediment mass accumulation rates (MARs) are consistently higher than 230Th-normalized MARs in the Equatorial Pacific Ocean during the past 25 ka. The offset, being highest in the Panama Basin, suggests sediment redistribution in this region is prominent. I test the hypothesis that downslope transport of sediments from topographically highs that surround the Panama Basin is the cause of higher-than-expected xs230Th inventories in the deeper parts of the basin. There is little difference in xs230Th inventories between the highest and lowest reaches of the basin suggesting that

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27

Mack, Andrew P. "High-frequency internal waves in the upper eastern equatorial Pacific." 1997. http://catalog.hathitrust.org/api/volumes/oclc/41182637.html.

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28

Yu, Hung-Jui, and 尤虹叡. "Quasi-2-day Convective Disturbances in the Equatorial Indian Ocean: DYNAMO Observation." Thesis, 2018. http://ndltd.ncl.edu.tw/handle/63r9xf.

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博士<br>國立臺灣大學<br>大氣科學研究所<br>106<br>This study examines the westward-propagating convective disturbances with quasi-2-day intervals of occurrence identified over Gan Island in the central Indian Ocean from mid to late October 2011 during the Dynamics of the Madden-Julian Oscillation (DYNAMO) field campaign. Atmospheric sounding, satellite, and radar data are used to develop a composite of seven such disturbances. Composites and spectral analyses reveal that: (1) the quasi-2-day convective events comprise westward-propagating diurnal convective disturbances with phase speeds of 10–12 m/s whose am

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29

Snoeckx, Hilde. "Late Pleistocene history of ocean-atmosphere interaction in the eastern Equatorial Pacific." 1996. http://catalog.hathitrust.org/api/volumes/oclc/37357033.html.

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30

Hale, Sarah Beth. "PALEOPRODUCTIVITY VARIATIONS IN THE EASTERN CENTRAL EQUATORIAL PACIFIC OCEAN ON GLACIAL TIMESCALES." Thesis, 2008. http://hdl.handle.net/1805/1671.

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Indiana University-Purdue University Indianapolis (IUPUI)<br>Paleoproductivity records during the late Pleistocene are sparse. The equatorial Pacific and the Southern Ocean are collectively responsible for the majority of the new production in the oceans. The nutrient and carbon mass balances of these regions must be constrained in order to fully understand net global biological productivity on glacial timescales. The geochemistry of two east-central equatorial Pacific Ocean cores (02° 33.48 N; 117° 55.06 W) and (00° 15.42 S; 113° 00.57 W) are used to examine changes in biological productivi

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31

Fan, Chen-Shuo, and 范辰碩. "Inter-annual Rainfall Variability of Specific Area In The Eastern Equatorial Pacific Ocean." Thesis, 2017. http://ndltd.ncl.edu.tw/handle/jeeyw7.

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碩士<br>國立中央大學<br>大氣科學學系<br>105<br>This research is inspired by Floating City Project which is going to be implemented by American and Netherland Cooperated Institution in 2020. The floating city has been planned to construct over the eastern equatorial Pacific Ocean near Central America in the project. Consider to the future water resource problem of the floating city, this research is dedicated to understand inter-annual precipitation variation over Target Area (6N-12N, 86W-94W) in rainy season. Target Area is actually a place where the floating city would be built in 2020. In this research, c

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32

Gruenburg, Laura Kristen. "Indonesian Throughflow Heat Transport, and Spreading within the Eastern Tropical Indian Ocean." Thesis, 2021. https://doi.org/10.7916/d8-s7eg-ke09.

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The Indonesian Throughflow (ITF) is the only low latitude connector between the Pacific and Indian Oceans affecting upper ocean stratification and regional climate. Here we focus on the Indian Ocean side of this connection, first identifying changes within the primary throughflow pathway within the Indonesian Seas, then following the throughflow as it moves within the eastern tropical Indian Ocean. Moored velocity measurements and an ENSO varying temperature profile developed from all available observations within the Makassar Strait are used to determine the southward heat flux anomaly (HFa)

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33

Kaupp, Lauren Johanna. "Distributions of dissolved iron and aluminum in the eastern equatorial Pacific : results from the 2004 biocomplexity cruise." Thesis, 2005. http://hdl.handle.net/10125/20796.

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34

YANG, MEI-HUI, and 楊美慧. "Shelf fish communities and resource availability in the Eastern Indian Ocean near Australia." Thesis, 1989. http://ndltd.ncl.edu.tw/handle/23684496052753504368.

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35

Finney, Bruce Preston. "Paleoclimatic influence on sedimentation and manganese nodule growth during the past 400,000 years at MANOP Site H (eastern equatorial Pacific)." Thesis, 1986. http://hdl.handle.net/1957/26611.

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36

Putri, Mutiara Rachmat [Verfasser]. "Study of ocean climate variability (1959 - 2002) in the eastern Indian Ocean, Java Sea and Sunda Strait using the HAMburg shelf ocean model / vorgelegt von Mutiara Rachmat Putri." 2005. http://d-nb.info/974465585/34.

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37

Lopez, Karem. "Nature and Evolution of Deep Water Carbonate Drifts in the past 3 Million years, Inner Sea of the Maldives Archipelago, Equatorial Indian Ocean." Thesis, 2012. http://hdl.handle.net/1911/71669.

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The Maldives atolls, the very top of one of the largest modern carbonate platforms, occupy the central and largest part of the Chagos-Laccadives ridge located in the equatorial Indian Ocean. In the central part of the archipelago, the large atolls form two parallel north-south relatively continuous chains surrounding an internal basin, the Inner Sea, with water depths not exceeding 550 m. The Maldives carbonate system, uniquely evolved through a combination of global sea level fluctuations, subsiding history, and more regional seasonally varying monsoon circulation. Although the long-term evol

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38

Maity, Rajib. "Impact Of Large-Scale Coupled Atmospheric-Oceanic Circulation On Hydrologic Variability And Uncertainty Through Hydroclimatic Teleconnection." Thesis, 2007. http://hdl.handle.net/2005/721.

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In the recent scenario of climate change, the natural variability and uncertainty associated with the hydrologic variables is of great concern to the community. This thesis opens up a new area of multi-disciplinary research. It is a promising field of research in hydrology and water resources that uses the information from the field of atmospheric science. A new way to identify and capture the variability and uncertainty associated with the hydrologic variables is established through this thesis. Assessment of hydroclimatic teleconnection for Indian subcontinent and its use in basin-scale hydr

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39

Karmakar, Nirupam. "Space-Time Evolution of the Intraseasonal Variability in the Indian Summer Monsoon and its Association with Extreme Rainfall Events : Observations and GCM Simulations." Thesis, 2016. http://hdl.handle.net/2005/3205.

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In this thesis, we investigated modes of intraseasonal variability (ISV) observed in the Indian monsoon rainfall and how these modes modulate rainfall over India. We identified a decreasing trend in the intensity of low-frequency intraseasonal mode with increasing strength in synoptic variability over India. We also made an attempt to understand the reason for these observed trends using numerical simulations. In the first part of the thesis, satellite rainfall estimates are used to understand the spatiotem-poral structures of convection in the intraseasonal timescale and their intensity durin

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