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This Keyword List Contains Indian Ocean Place Names of Coral Reefs, Islands, Bays and Other Geographic Features in a Hierarchical Structure
CoRIS Place Keyword Thesaurus by Ocean - 8/9/2016 Indian Ocean This keyword list contains Indian Ocean place names of coral reefs, islands, bays and other geographic features in a hierarchical structure. For example, the first name on the list - Bird Islet - is part of the Addu Atoll, which is in the Indian Ocean. The leading label - OCEAN BASIN - indicates this list is organized according to ocean, sea, and geographic names rather than country place names. The list is sorted alphabetically. The same names are available from “Place Keywords by Country/Territory - Indian Ocean” but sorted by country and territory name. Each place name is followed by a unique identifier enclosed in parentheses. The identifier is made up of the latitude and longitude in whole degrees of the place location, followed by a four digit number. The number is used to uniquely identify multiple places that are located at the same latitude and longitude. For example, the first place name “Bird Islet” has a unique identifier of “00S073E0013”. From that we see that Bird Islet is located at 00 degrees south (S) and 073 degrees east (E). It is place number 0013 at that latitude and longitude. (Note: some long lines wrapped, placing the unique identifier on the following line.) This is a reformatted version of a list that was obtained from ReefBase. OCEAN BASIN > Indian Ocean OCEAN BASIN > Indian Ocean > Addu Atoll > Bird Islet (00S073E0013) OCEAN BASIN > Indian Ocean > Addu Atoll > Bushy Islet (00S073E0014) OCEAN BASIN > Indian Ocean > Addu Atoll > Fedu Island (00S073E0008) -
Banda Islands, Indonesia
INSULARITY AND ADAPTATION INVESTIGATING THE ROLE OF EXCHANGE AND INTER-ISLAND INTERACTION IN THE BANDA ISLANDS, INDONESIA Emily J. Peterson A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy University of Washington 2015 Reading Committee: Peter V. Lape, Chair James K. Feathers Benjamin Marwick Program Authorized to Offer Degree: Anthropology ©Copyright 2015 Emily J. Peterson University of Washington Abstract Insularity and Adaptation Investigating the role of exchange and inter-island interaction in the Banda Islands, Indonesia Emily J. Peterson Chair of the Supervisory Committee: Professor Peter V. Lape Department of Anthropology Trade and exchange exerted a powerful force in the historic and protohistoric past of Island Southeast Asian communities. Exchange and interaction are also hypothesized to have played an important role in the spread of new technologies and lifestyles throughout the region during the Neolithic period. Although it is clear that interaction has played an important role in shaping Island Southeast Asian cultures on a regional scale, little is known about local histories and trajectories of exchange in much of the region. This dissertation aims to improve our understanding of the adaptive role played by exchange and interaction through an exploration of change over time in the connectedness of island communities in the Banda Islands, eastern Indonesia. Connectedness is examined by measuring source diversity for two different types of archaeological materials. Chemical characterization of pottery using LA-ICP-MS allows the identification of geochemically different paste groups within the earthenware assemblages of two Banda Islands sites. Source diversity measures are employed to identify differences in relative connectedness between these sites and changes over time. -
Vertical Variability and Its Relation to ENSO in the North Natuna Sea
ILMU KELAUTAN: Indonesian Journal of Marine Sciences June 2021 Vol 26(2):63-70 e-ISSN 2406-7598 Natuna Off-Shelf Current (NOC) Vertical Variability and Its Relation to ENSO in the North Natuna Sea Hariyadi1,2*, Johanes Hutabarat3, Denny Nugroho Sugianto1,4, Muhammad Faiq Marwa Noercholis1, Niken Dwi Prasetyani,1 Widodo S. Pranowo5, Kunarso1, Parichat Wetchayount6, Anindya Wirasatriya1,4 1Department of Oceanography, Faculty of Fisheries and Marine Science, Diponegoro University 2Doctoral Program of Marine Science, Diponegoro University 3Department of Aquaculture, Faculty of Fisheries and Marine Science, Diponegoro University 4Center for Coastal Rehabilitation and Disaster Mitigation Studies (CoREM), Diponegoro University Jl. Prof. H. Soedharto, SH, Tembalang Semarang. 50275 Indonesia 5Marine Research Center, Agency for Marine & Fisheries Research & Human Resources, Ministry of Marine and Fisheries Gedung Mina Bahari I 5th Floor, Jl. Medan Merdeka Timur No. 16 Jakarta Pusat 10110 Indonesia 6Department of Geography, Faculty of Social Science, Srinakharinwirot University 8 114 Sukhumvit 23, Bangkok, Thailand Email: [email protected] Abstract During the northwest monsoon (NWM), southerly flow off the Natuna Islands appeared as the extension of the turning Vietnam coastal jet, known as Natuna off-shelf current (NOC). NOC is generated by the interaction of wind stress and the North Natuna Sea’s bottom topography. The purposes of the present study is to investigate the vertical variability of NOC and its relation to El Niňo Southern Oscillation (ENSO) using Marine Copernicus reanalysis data. The vertical variability refers to the spatial distribution of NOC pattern at the surface layer, thermocline layer, and deep/bottom layer. in 2014 as representative of normal ENSO condition. -
SCHAPPER, Antoinette and Emilie WELLFELT. 2018. 'Reconstructing
Reconstructing contact between Alor and Timor: Evidence from language and beyond a b Antoinette SCHAPPER and Emilie WELLFELT LACITO-CNRSa, University of Colognea, and Stockholm Universityb Despite being separated by a short sea-crossing, the neighbouring islands of Alor and Timor in south-eastern Wallacea have to date been treated as separate units of linguistic analysis and possible linguistic influence between them is yet to be investigated. Historical sources and oral traditions bear witness to the fact that the communities from both islands have been engaged with one another for a long time. This paper brings together evidence of various types including song, place names and lexemes to present the first account of the interactions between Timor and Alor. We show that the groups of southern and eastern Alor have had long-standing connections with those of north-central Timor, whose importance has generally been overlooked by historical and linguistic studies. 1. Introduction1 Alor and Timor are situated at the south-eastern corner of Wallacea in today’s Indonesia. Alor is a small mountainous island lying just 60 kilometres to the north of the equally mountainous but much larger island of Timor. Both Alor and Timor are home to a mix of over 50 distinct Papuan and Austronesian language-speaking peoples. The Papuan languages belong to the Timor-Alor-Pantar (TAP) family (Schapper et al. 2014). Austronesian languages have been spoken alongside the TAP languages for millennia, following the expansion of speakers of the Austronesian languages out of Taiwan some 3,000 years ago (Blust 1995). The long history of speakers of Austronesian and Papuan languages in the Timor region is a topic in need of systematic research. -
Ocean Wave Characteristics in Indonesian Waters for Sea Transportation Safety and Planning
IPTEK, The Journal for Technology and Science, Vol. 26, No. 1, April 2015 19 Ocean Wave Characteristics in Indonesian Waters for Sea Transportation Safety and Planning Roni Kurniawan1 and Mia Khusnul Khotimah2 AbstractThis study was aimed to learn about ocean wave characteristics and to identify times and areas with vulnerability to high waves in Indonesian waters. Significant wave height of Windwaves-05 model output was used to obtain such information, with surface level wind data for 11 years period (2000 to 2010) from NCEP-NOAA as the input. The model output data was then validated using multimission satellite altimeter data obtained from Aviso. Further, the data were used to identify areas of high waves based on the high wave’s classification by WMO. From all of the processing results, the wave characteristics in Indonesian waters were identified, especially on ALKI (Indonesian Archipelagic Sea Lanes). Along with it, which lanes that have high potential for dangerous waves and when it occurred were identified as well. The study concluded that throughout the years, Windwaves-05 model had a magnificent performance in providing ocean wave characteristics information in Indonesian waters. The information of height wave vulnerability needed to make a decision on the safest lanes and the best time before crossing on ALKI when the wave and its vulnerability is likely low. Throughout the years, ALKI II is the safest lanes among others since it has been identified of having lower vulnerability than others. The knowledge of the wave characteristics for a specific location is very important to design, plan and vessels operability including types of ships and shipping lanes before their activities in the sea. -
Regional Maritime Issues, Can the Indian Ocean Be Collaboratively Managed?
Regional Maritime Issues, Can the Indian Ocean be Collaboratively Managed? First Admiral Anuar bin Mohamed Assistant Chief of Staff Human Resource, Royal Malaysian Navy Can the Indian Ocean be Collaboratively Managed? It covers an area of 68.556 million sq km, which includes amongst others, the Andaman The Hypothesis: Collaboration could not be Sea, Arabian Sea, Bay of Bengal, Flores Sea, fully achieved in IOR, as long as there is a great Great Australian Bight, Gulf of Aden, Gulf of power politics that enhance the geopolitical and Oman, Java Sea, Mozambique Channel, Persian geostrategic struggles in the region. Gulf, Red Sea, Savu Sea, Strait of Malacca and Timor Sea. This is viewed through the lens of neo-realism, where the structural defects would eventually By comparison, it consists of an area that is make efforts for collaboration/cooperation almost 7 times the size of the United States. impossible. Bordering this ocean and the states around it is the 66,526 km coastlines. In arguing this, we need to understand the features of the IOR iot determined factors that In a nutshell, it covers 30% of the global ocean would affect the argument. area home to 30% of the world’s population and 30% of the world’s coral reef cover. Background Geographically : Economically: This ocean hosts abundant of natural Indian Ocean Region (IOR) has unique resources of oil and gas fields, fish, shrimp, characteristics compared to other oceanic sand and gravel aggregates, placer deposits and regions. poly-metallic nodules. It is the third largest of the world's five oceans, It also provide various major sea routes after the Pacific and the Atlantic Ocean. -
Chapter 13 Anatomy of the Andaman–Nicobar Subduction System From
Downloaded from http://mem.lyellcollection.org/ by guest on September 29, 2021 Chapter 13 Anatomy of the Andaman–Nicobar subduction system from seismic reflection data SATISH C. SINGH* & RAPHAE¨ LE MOEREMANS Laboratoire de Geoscience Marine, Institut de Physique du Globe de Paris, 1 rue Jussieu, 75238 Paris Cedex 05, France *Correspondence: [email protected] Abstract: The Andaman–Nicobar subduction system is the northwestern segment of the Sunda subduction system, where the Indian Plate subducts beneath the Sunda Plate in a nearly arc-parallel direction. The entire segment ruptured during the 2004 great Andaman–Sumatra earthquake (Mw ¼ 9.3). Using recently acquired high-resolution seismic reflection data, we charac- terize the shallow structure of the whole Andaman–Nicobar subduction system from west to east, starting from the nature of the subducting plate in the Bay of Bengal to back-arc spreading in the Andaman Sea. We find that the Ninety-East Ridge is overlain by thick continental margin sediments beneath the recent Bengal Fan sediments. The boundary between these two sedimentary units defines the plate interface. We observe evidence of re-activation of fracture zones on the subducting plate beneath the forearc, influencing the morphology of the upper plate. The forearc region, which includes the accretionary wedge, the forearc high and the forearc basin, is exceptionally wide (250 km). We observe an unusually large bathymetric depression within the forearc high. The forearc high is bounded in the east by a normal fault, whereas the forearc basin contains an active backthrust. The forearc basin is floored by the continental crust of Malayan Peninsula origin. -
Some Physical Aspects of the Surface Waters Around the Little Andaman
Indian Journal of Marine Sciences Vo\. 10, September 1981, pp. 221-227 Some Physical Aspects of the Surface Waters around the Little Andaman . Island ..., C S MURTY, P K DAS & A D GOUVEIA National Institute of Oceanography, Dona Paula, Goa, 403004 Received 15 December 1980; revised received 27 April 1981 Along with the thermal and haline characteristics of the waters during the peak northeast monsoon period (February), observations on stratifications, inversions, mixed layers, nature and depth of thermocline, wind-induced surface drifts, zones of surface and sub-surface salinity parameters are discussed. The major objective, however, is to present the surface water circulation pattern around this island. It is shown that the surface water around this island flows towards the SSW from the NNE and that the surface water characteristics such as Hienature of the mixed layer and the deepening of the mixed layer on the southwestern side of the island result not only as a 'lee' effect but also lends further evidence to the fact that the waters on the western side of the Andaman Island arc as a whole are slightly different from the waters on the eastern side i.e. the Andaman Sea water. Oceanic Islands or rather a group of islands, far away oceanic islands (barring a few) is the yearly cycle of the from continental margins, significantly influence, N-E and S-W monsoonal wind systems reversing the modify and change the general physico-chemical atmospheric circulation and the surface currents of the properties of the wateJ!.6around them mainly by Bay of Bengal and the Andaman Sea from December changing the general circulation patterns and the to April and June to October with intervening associated stratification-mixing processes. -
Eurasia Asia & Oceania
Segment Overview Asia & Eurasia Oceania u p. 28 u p. 20 Number of countries 7 4 1,551 ,296 1 1,245 1,218 1 16 14 Number of projects 1 3 In production 2 43 1 1 6 Under development 10 Preparation for development Under exploration (oil and gas reservoirs confirmed) Under exploration Other 466 Production/Reserves 367 Proved reserves (million boe) 214 201 195 210 207 191 Net production (thousand boed) 179 197 190 188 167 166 28 27 27 26 25 25 2010 2011 2012 2013 2014 2015 2010 2011 2012 2013 2014 2015 485,275 485,069 483,187 406,828 409,776 / 352,383 Net sales 299,599 281,623 Operating income 264,849 235,814 Net sales (¥ million) 191,070 178,225 Operating income (¥ million) 96,341 94,050 85,541 84,325 73,574 68,319 47,076 41,752 42,601 39,769 36,461 32,228 2010 2011 2012 2013 2014 2015 2010 2011 2012 2013 2014 2015 018 INPEX CORPORATION Annual Report 2015 Middle East Americas Japan & Africa u p. 32 u p. 36 u p. 30 6 7 1 Minami-Nagaoka 1 2 Gas Field 1 Naoetsu LNG 3 Terminal 9 7 1 16 10 Natural gas pipeline network (Approx. 1,400 km) etc. 783 857 636 4 Project Overview Project 583 518 505 174 168 169 158 163 155 138 135 132 130 126 117 74 68 65 40 36 30 29 30 27 28 20 25 25 21 21 21 17 18 2010 2011 2012 2013 2014 2015 2010 2011 2012 2013 2014 2015 2010 2011 2012 2013 2014 2015 524,528 520,835 500,033 621,513 421,184 357,343 354,136 350,735 333,213 303,819 243,113 205,572 129,522 120,268 118,937 ) 113,662 104,525 93,959 32,555 28,568 25,959 22,771 24,607 16,692 16,693 12,673 11,435 13,351 15,303 5,945 5,525 (7,646) (3,035) 1,028 (6,089) (5,518) ( 2010 2011 2012 2013 2014 2015 2010 2011 2012 2013 2014 2015 2010 2011 2012 2013 2014 2015 INPEX CORPORATION Annual Report 2015 019 Project Overview by Region Asia & Oceania In the Asia and Oceania region, INPEX holds participating interests in the Offshore Mahakam Block in Indonesia, which is contributing significantly to earnings, and the large-scale Ichthys and Abadi LNG projects, where development and preparatory development activities are under way. -
The Birds of Babar, Romang, Sermata, Leti and Kisar, Maluku, Indonesia
Colin R. Trainor & Philippe Verbelen 272 Bull. B.O.C. 2013 133(4) New distributional records from forgoten Banda Sea islands: the birds of Babar, Romang, Sermata, Leti and Kisar, Maluku, Indonesia by Colin R. Trainor & Philippe Verbelen Received 5 July 2011; fnal revision accepted 10 September 2013 Summary.—Many of the Banda Sea islands, including Babar, Romang, Sermata and Leti, were last surveyed more than 100 years ago. In October–November 2010, birds were surveyed on Romang (14 days), Sermata (eight days), Leti (fve days) and Kisar (seven days), and on Babar in August 2009 (ten days) and August 2011 (11 days). Limited unpublished observations from Damar, Moa, Masela (of Babar) and Nyata (of Romang) are also included here. A total of 128 bird species was recorded (85 resident landbirds), with 104 new island records, among them fve, 12, 20, four and three additional resident landbirds for Babar, Romang, Sermata, Leti and Kisar, respectively. The high proportion of newly recorded and apparently overlooked resident landbirds on Sermata is puzzling but partly relates to limited historical collecting. Signifcant records include Ruddy-breasted Crake Porzana fusca (Romang), Red-legged Crake Rallina fasciata (Sermata), Bonelli’s Eagle Aquila fasciata renschi (Romang), Elegant Pita Pita elegans vigorsii (Babar, Romang, Sermata), Timor Stubtail Urosphena subulata (Babar, Romang), the frst sound-recordings of Kai Cicadabird Coracina dispar (Babar?, Romang) and endemic subspecies of Southern Boobook Ninox boobook cinnamomina (Babar) and N. b. moae (Romang, Sermata?). The frst ecological notes were collected for Green Oriole Oriolus favocinctus migrator on Romang, the lowland-dwelling Snowy-browed Flycatcher Ficedula hyperythra audacis on Babar, the endemic subspecies of Yellow- throated (Banda) Whistler Pachycephala macrorhyncha par on Romang, and Grey Friarbird Philemon kisserensis on Kisar and Leti. -
Beyond the Wall: Chinese Far Seas Operation
U.S. Naval War College U.S. Naval War College Digital Commons CMSI Red Books China Maritime Studies Institute 5-2015 Beyond the Wall: Chinese Far Seas Operation Peter A. Dutton Ryan D. Martinson Follow this and additional works at: https://digital-commons.usnwc.edu/cmsi-red-books Recommended Citation Dutton, Peter A. and Martinson, Ryan D., "Beyond the Wall: Chinese Far Seas Operation" (2015). CMSI Red Books, Study No. 13. This Book is brought to you for free and open access by the China Maritime Studies Institute at U.S. Naval War College Digital Commons. It has been accepted for inclusion in CMSI Red Books by an authorized administrator of U.S. Naval War College Digital Commons. For more information, please contact [email protected]. Beyond the Wall Chinese Far Seas Operations Peter A. Dutton and Ryan D. Martinson, Editors CHINA MARITIME STUDIES INSTITUTE U.S. NAVAL WAR COLLEGE Newport, Rhode Island www.usnwc.edu/Research---Gaming/China-Maritime-Studies-Institute.aspx Naval War College The China Maritime Studies are extended research projects Newport, Rhode Island that the editor, the Dean of Naval Warfare Studies, and the Center for Naval Warfare Studies President of the Naval War College consider of particular China Maritime Study No. 13 interest to policy makers, scholars, and analysts. May 2015 Correspondence concerning the China Maritime Studies President, Naval War College may be addressed to the director of the China Maritime Rear Admiral P. Gardner Howe III, U.S. Navy Studies Institute, www.usnwc.edu/Research---Gaming/ Provost China-Maritime-Studies-Institute.aspx. To request ad- Dr. -
Indonesian Seas by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO
An Atlas of Oceanic Internal Solitary Waves (February 2004) Indonesian Seas by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO Indonesian Seas • Bali Sea • Flores Sea • Molucca Sea • Banda Sea • Java Sea • Savu Sea • Cream Sea • Makassar Strait Overview The Indonesian Seas are the regional bodies of water in and around the Indonesian Archipelago. The seas extend between approximately 12o S to 3o N and 110o to 132oE (Figure 1). The region separates the Pacific and Indian Oceans. Figure 1. Bathymetry of the Indonesian Archipelago. [Smith and Sandwell, 1997] Observations Indonesian Archipelago is most extensive archipelago in the world with more than 15,000 islands. The shallow bathymetry and the strong tidal currents between the islands give rise to the generation of internal waves throughout the archipelago. As a result there are a very 453 An Atlas of Oceanic Internal Solitary Waves (February 2004) Indonesian Seas by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO large number of internal wave sources throughout the region. Since the Indonesian Seas boarder the equator, the stratification of the waters in this sea area does not change very much with season, and internal wave activity is expected to take place all year round. Table 2 shows the months of the year during which internal waves have been observed in the Bali, Molucca, Banda and Savu Seas Table 1 - Months when internal waves have been observed in the Bali Sea. (Numbers indicate unique dates in that month when waves have been noted) Jan Feb Mar Apr May Jun Jul Aug Sept Oct Nov Dec 12111 11323 Months when Internal Waves have been observed in the Molucca Sea.