Relevant bibliographies by topics / Eastern Equatorial Indian Ocean

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Eastern Equatorial Indian Ocean'

Author: Grafiati
Published: 4 June 2021
Last updated: 4 February 2022

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Journal articles on the topic "Eastern Equatorial Indian Ocean"

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Lee Drbohlav, Hae-Kyung, and V. Krishnamurthy. "Spatial Structure, Forecast Errors, and Predictability of the South Asian Monsoon in CFS Monthly Retrospective Forecasts." Journal of Climate 23, no. 18 (2010): 4750–69. http://dx.doi.org/10.1175/2010jcli2356.1.

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Abstract The spatial structure of the boreal summer South Asian monsoon in the ensemble mean of monthly retrospective forecasts by the Climate Forecast System of the National Centers for Environmental Prediction is examined. The forecast errors and predictability of the model are assessed. Systematic errors in the forecasts consist of deficient rainfall over India, excess rainfall over the Arabian Sea, and a dipole structure over the equatorial Indian Ocean. On interannual time scale during 1981–2003, two different characteristics of the monsoon are recognized—both in observation and forecasts
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Wang, Jing, and Dongliang Yuan. "Roles of Western and Eastern Boundary Reflections in the Interannual Sea Level Variations during Negative Indian Ocean Dipole Events." Journal of Physical Oceanography 45, no. 7 (2015): 1804–21. http://dx.doi.org/10.1175/jpo-d-14-0124.1.

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AbstractThe equatorial wave dynamics of sea level variations during negative Indian Ocean dipole (nIOD) events are investigated using the LICOM ocean general circulation model forced with the European Centre for Medium-Range Weather Forecast reanalysis wind stress and heat flux from 1990 to 2001. The work is a continuation of the study by Yuan and Liu, in which the equatorial wave dynamics during positive IOD events are investigated. The model has reproduced the sea level anomalies of satellite altimeter data well. Long equatorial waves extracted from the model output suggest two kinds of nega
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Brown, J., C. A. Clayson, L. Kantha, and T. Rojsiraphisal. "North Indian Ocean variability during the Indian Ocean dipole." Ocean Science Discussions 5, no. 2 (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 o
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Joseph, Sudheer, M. Ravichandran, B. Praveen Kumar, Raju V. Jampana, and Weiqing Han. "Ocean atmosphere thermal decoupling in the eastern equatorial Indian ocean." Climate Dynamics 49, no. 1-2 (2016): 575–94. http://dx.doi.org/10.1007/s00382-016-3359-1.

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Kido, Shoichiro, and Tomoki Tozuka. "Salinity Variability Associated with the Positive Indian Ocean Dipole and Its Impact on the Upper Ocean Temperature." Journal of Climate 30, no. 19 (2017): 7885–907. http://dx.doi.org/10.1175/jcli-d-17-0133.1.

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Abstract Both surface and subsurface salinity variability associated with positive Indian Ocean dipole (pIOD) events and its impacts on the sea surface temperature (SST) evolution are investigated through analysis of observational/reanalysis data and sensitivity experiments with a one-dimensional mixed layer model. During the pIOD, negative (positive) sea surface salinity (SSS) anomalies appear in the central-eastern equatorial Indian Ocean (southeastern tropical Indian Ocean). In addition to these SSS anomalies, positive (negative) salinity anomalies are found near the pycnocline in the easte
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Chen, Gengxin, Weiqing Han, Yuanlong Li, Dongxiao Wang, and Michael J. McPhaden. "Seasonal-to-Interannual Time-Scale Dynamics of the Equatorial Undercurrent in the Indian Ocean." Journal of Physical Oceanography 45, no. 6 (2015): 1532–53. http://dx.doi.org/10.1175/jpo-d-14-0225.1.

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AbstractThis paper investigates the structure and dynamics of the Equatorial Undercurrent (EUC) of the Indian Ocean by analyzing in situ observations and reanalysis data and performing ocean model experiments using an ocean general circulation model and a linear continuously stratified ocean model. The results show that the EUC regularly occurs in each boreal winter and spring, particularly during February and April, consistent with existing studies. The EUC generally has a core depth near the 20°C isotherm and can be present across the equatorial basin. The EUC reappears during summer–fall of
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Han, Weiqing, Julian P. McCreary, Yukio Masumoto, Jérôme Vialard, and Benét Duncan. "Basin Resonances in the Equatorial Indian Ocean." Journal of Physical Oceanography 41, no. 6 (2011): 1252–70. http://dx.doi.org/10.1175/2011jpo4591.1.

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Abstract Previous studies have investigated how second-baroclinic-mode (n = 2) Kelvin and Rossby waves in the equatorial Indian Ocean (IO) interact to form basin resonances at the semiannual (180 day) and 90-day periods. This paper examines unresolved issues about these resonances, including the reason the 90-day resonance is concentrated in the eastern ocean, the time scale for their establishment, and the impact of complex basin geometry. A hierarchy of ocean models is used: an idealized one-dimensional (1D) model, a linear continuously stratified ocean model (LCSM), and an ocean general cir
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Chen, Gengxin, Weiqing Han, Yuanlong Li, Jinglong Yao, and Dongxiao Wang. "Intraseasonal Variability of the Equatorial Undercurrent in the Indian Ocean." Journal of Physical Oceanography 49, no. 1 (2019): 85–101. http://dx.doi.org/10.1175/jpo-d-18-0151.1.

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AbstractBy analyzing in situ observations and conducting a series of ocean general circulation model experiments, this study investigates the physical processes controlling intraseasonal variability (ISV) of the Equatorial Undercurrent (EUC) of the Indian Ocean. ISV of the EUC leads to time-varying water exchanges between the western and eastern equatorial Indian Ocean. For the 2001–14 period, standard deviations of the EUC transport variability are 1.92 and 1.77 Sv (1 Sv ≡ 106 m3 s−1) in the eastern and western basins, respectively. The ISV of the EUC is predominantly caused by the wind forci
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Yuan, Dongliang, Jing Wang, Tengfei Xu, et al. "Forcing of the Indian Ocean Dipole on the Interannual Variations of the Tropical Pacific Ocean: Roles of the Indonesian Throughflow." Journal of Climate 24, no. 14 (2011): 3593–608. http://dx.doi.org/10.1175/2011jcli3649.1.

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Abstract Controlled numerical experiments using ocean-only and ocean–atmosphere coupled general circulation models show that interannual sea level depression in the eastern Indian Ocean during the Indian Ocean dipole (IOD) events forces enhanced Indonesian Throughflow (ITF) to transport warm water from the upper-equatorial Pacific Ocean to the Indian Ocean. The enhanced transport produces elevation of the thermocline and cold subsurface temperature anomalies in the western equatorial Pacific Ocean, which propagate to the eastern equatorial Pacific to induce significant coupled evolution of the
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Zhou, Zhen-Qiang, Renhe Zhang, and Shang-Ping Xie. "Interannual Variability of Summer Surface Air Temperature over Central India: Implications for Monsoon Onset." Journal of Climate 32, no. 6 (2019): 1693–706. http://dx.doi.org/10.1175/jcli-d-18-0675.1.

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Abstract Year-to-year variability of surface air temperature (SAT) over central India is most pronounced in June. Climatologically over central India, SAT peaks in May, and the transition from the hot premonsoon to the cooler monsoon period takes place around 9 June, associated with the northeastward propagation of intraseasonal convective anomalies from the western equatorial Indian Ocean. Positive (negative) SAT anomalies during June correspond to a delayed (early) Indian summer monsoon onset and tend to occur during post–El Niño summers. On the interannual time scale, positive SAT anomalies
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Dissertations / Theses on the topic "Eastern Equatorial Indian Ocean"

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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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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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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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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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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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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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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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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 (MAR’s) 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 MAR’s, 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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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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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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Books on the topic "Eastern Equatorial Indian Ocean"

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Johnson, Gregory Conrad. Near-equatorial deep circulation in the Indian and Pacific Oceans. Woods Hole Oceanographic Institution, 1990.

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Johnson, Gregory Conrad. Near-equatorial deep circulation in the Indian and Pacific Oceans. Woods Hole Oceanographic Institution, 1990.

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Hare, Jeffrey. Cloud, radiation, and surface forcing in the equatorial eastern Pacific. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Office of Oceanic and Atmospheric Research, Earth System Research Laboratory, Physical Sciences Division, 2005.

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1953-, Droxler André W., and American Association of Petroleum Geologists., eds. Seismic expressions and interpretation of carbonate sequences: The Maldives platform, equatorial Indian Ocean. American Association of Petroleum Geologists, 2004.

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Bornmalm, Lennart. Taxonomy and paleoecology of late Neogene benthic forminifera from the Caribbean Sea and eastern equatorial Pacific Ocean. Scandinavian University Press, 1997.

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West Indian ocean islands: Strategic dimensions of regional cooperation. Kalinga Publications, 2000.

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Swallow, Jane E. Plio-pleistocene palaeoceanography of the Equatorial Indian Ocean: (quantitative and geochemical analyses of planktonic foraminifera from ODP hole 709C). University of East Anglia, 1992.

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Richmond, Matt. A field guide to the seashores of eastern Africa and the western Indian Ocean islands. 2nd ed. Edited by Sweden Beredningen för u-landsforskning and Chuo Kikuu cha Dar es Salaam. SIDA, Dept. for Research Cooperation, 2002.

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Richmond, Matt. A field guide to the seashores of eastern Africa and the western Indian Ocean islands. 3rd ed. SIDA, WIOMSA, 2011.

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Happee, T. J. W. Behaviour of trace- and major elements in sediments in an upwelling zone of the Somalia and Oman continental margin and the equatorial Indian Ocean. Netherlands Institute for Sea Research, 1994.

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Book chapters on the topic "Eastern Equatorial Indian Ocean"

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Ambrosimov, Albert K., Dmitry I. Frey, and Sergey M. Shapovalov. "Tareev Equatorial Undercurrent in the Indian Ocean." In The Ocean in Motion. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-71934-4_31.

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Brown, Barbara E. "Eastern Indian Ocean – Northern Sector." In Encyclopedia of Modern Coral Reefs. Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2639-2_272.

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Lodhi, Abdulaziz Yusuf. "Linguistic and Cultural Contributions of Gujarat in Eastern Africa." In Knowledge and the Indian Ocean. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-96839-1_13.

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Chew, Emrys. "The Arms Trade in the Eastern Indian Ocean." In Arming the Periphery. Palgrave Macmillan UK, 2012. http://dx.doi.org/10.1057/9781137006608_5.

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Beaufort, Luc, Franck Bassinot, and Edith Vincent. "Primary Production Response to Orbitally Induced Variations of the Southern Oscillation in the Equatorial Indian Ocean." In Reconstructing Ocean History. Springer US, 1999. http://dx.doi.org/10.1007/978-1-4615-4197-4_15.

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Agnihotri, Rajesh, S. Wajih A. Naqvi, Siby Kurian, Mark A. Altabet, and J. F. Bratton. "Is δ15N of sedimentary organic matter a good proxy for paleodenitrification in coastal waters of the eastern Arabian Sea?" In Indian Ocean Biogeochemical Processes and Ecological Variability. American Geophysical Union, 2009. http://dx.doi.org/10.1029/2008gm000770.

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Sprey, Ilicia J., and Kenneth R. Hall. "Ayutthaya’s Seventeenth-Century Deerskin Trade in the Extended Eastern Indian Ocean and South China Sea." In Animal Trade Histories in the Indian Ocean World. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-42595-1_8.

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Yadav, Ramesh Kumar, and Bhupendra Bahadur Singh. "North Equatorial Indian Ocean Convection and Indian Summer Monsoon June Progression: a Case Study of 2013 and 2014." In Geoinformatics and Atmospheric Science. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-66092-9_2.

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Palat, Ravi. "Global Roots of Local Politics: State Formation in an Eastern Mirror." In The Making of an Indian Ocean World-Economy, 1250–1650. Palgrave Macmillan US, 2015. http://dx.doi.org/10.1057/9781137562265_3.

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Ogg, James G., Felix M. Gradstein, Julie A. Dumoulin, Massimo Sarti, and Paul Bown. "Sedimentary History of the Tethyan Margins of Eastern Gondwana During the Mesozoic." In Synthesis of Results from Scientific Drilling in the Indian Ocean. American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm070p0203.

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Conference papers on the topic "Eastern Equatorial Indian Ocean"

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Shkorba, Svetlana, Svetlana Shkorba, Elena Dmitrieva, et al. "CLIMATIC ANOMALIES IN FAR EASTERN MARGINAL SEAS, BAIKAL LAKE BASIN AND THEIR LINKAGES." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b4316b9d9e4.

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Winter climatic anomalies of various time scales in the Japan, Okhotsk seas and Baikal Lake Basin are revealed and compared with anomalies in the Pacific, Indian and Arctic oceans. Time series of ice extent in the Japan and Okhotsk seas, ice thickness and seasonal duration of the ice cover in the Baykal Lake, as well as Hadley SST, surface heat fluxes, wind velocity, atmospheric pressure fields (SLP) and different climatic indices are analyzed. The decadal climate anomalies in the Japan and Okhotsk seas in mid winter, as compared to the Northeast Pacific and South Siberia regions, could have a
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Shkorba, Svetlana, Svetlana Shkorba, Elena Dmitrieva, et al. "CLIMATIC ANOMALIES IN FAR EASTERN MARGINAL SEAS, BAIKAL LAKE BASIN AND THEIR LINKAGES." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b939727b3b4.55522289.

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Winter climatic anomalies of various time scales in the Japan, Okhotsk seas and Baikal Lake Basin are revealed and compared with anomalies in the Pacific, Indian and Arctic oceans. Time series of ice extent in the Japan and Okhotsk seas, ice thickness and seasonal duration of the ice cover in the Baykal Lake, as well as Hadley SST, surface heat fluxes, wind velocity, atmospheric pressure fields (SLP) and different climatic indices are analyzed. The decadal climate anomalies in the Japan and Okhotsk seas in mid winter, as compared to the Northeast Pacific and South Siberia regions, could have a
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Iskandar, I., W. Mardiansyah, D. Setiabudidaya, A. K. Affandi, and F. Syamsuddin. "Surface and subsurface oceanic variability observed in the eastern equatorial Indian Ocean during three consecutive Indian Ocean dipole events: 2006 - 2008." In 3RD INTERNATIONAL CONFERENCE ON THEORETICAL AND APPLIED PHYSICS 2013 (ICTAP 2013). AIP Publishing LLC, 2014. http://dx.doi.org/10.1063/1.4897101.

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Yu, Siyao, James D. Wright, Richard Mortlock, Silvia Spezzaferri, Stephanie Stainbank та Dick Kroon. "SOUTHERN OCEAN DRIVEN δ13C MINIMA ACROSS TERMINATION I AND II IN THE EQUATORIAL INDIAN OCEAN". У GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-359838.

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Somayajulu, Y. K., V. S. N. Murty, C. Neelima, and P. S. V. Jagadeesh. "Interannual variability of the equatorial jets in the Indian Ocean from merged altimetry data." In Asia-Pacific Remote Sensing Symposium, edited by Robert J. Frouin, Vijay K. Agarwal, Hiroshi Kawamura, Shailesh Nayak, and Delu Pan. SPIE, 2006. http://dx.doi.org/10.1117/12.693802.

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Mizuno, Keisuke, Yukio Masumoto, Hideaki Hase, et al. "Development of buoy array in the Eastern tropical Indian Ocean and observed variability." In OCEANS 2008 - MTS/IEEE Kobe Techno-Ocean. IEEE, 2008. http://dx.doi.org/10.1109/oceanskobe.2008.4531102.

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Hirawake, Toru, Hiroo Satoh, Tsutomu Morinaga, Takashi Ishimaru, and Motoaki Kishino. "In-water algorithms for estimation of chlorophyll a and primary production in the Arabian Sea and the eastern Indian Ocean." In Ocean Optics XIII, edited by Steven G. Ackleson and Robert J. Frouin. SPIE, 1997. http://dx.doi.org/10.1117/12.266458.

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Neethu, Sukumaran. "Tracing the Himalayan Erosion and Weathering Products in the Equatorial Indian Ocean Using Sedimentary Lead Isotopes." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1902.

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"Variability of sea surface temperature differences between western Pacific Ocean and eastern Indian Ocean related to ENSO events." In Proceeding of Marine Safety and Maritime Installation. Clausius Scientific Press, 2018. http://dx.doi.org/10.23977/msmi.2018.82619.

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Satapathy, P. K., S. Basu, and C. P. S. Rana. "Imaging near surface ocean bottom using 2D HR survey for shallow hazard studies: A case study from Eastern offshore, India." In 1st Indian Near Surface Geophysics Conference & Exhibition. European Association of Geoscientists & Engineers, 2019. http://dx.doi.org/10.3997/2214-4609.201979018.

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Reports on the topic "Eastern Equatorial Indian Ocean"

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Banerjee, Arjun. Redefining Maritime Security Threats in the Eastern Indian Ocean Region. Office of Scientific and Technical Information (OSTI), 2017. http://dx.doi.org/10.2172/1378251.

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Melville, W. K. Ship-Based UAV Measurements of Air-Sea Interaction in Marine Atmospheric Boundary Layer Processes in the Equatorial Indian Ocean. Defense Technical Information Center, 2013. http://dx.doi.org/10.21236/ada598312.

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