Chapter 4 Sea Lane Security in the Selected EAS Countries
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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) -
South China Sea Overview
‹ Countries South China Sea Last Updated: February 7, 2013 (Notes) full report Overview The South China Sea is a critical world trade route and a potential source of hydrocarbons, particularly natural gas, with competing claims of ownership over the sea and its resources. Stretching from Singapore and the Strait of Malacca in the southwest to the Strait of Taiwan in the northeast, the South China Sea is one of the most important trade routes in the world. The sea is rich in resources and holds significant strategic and political importance. The area includes several hundred small islands, rocks, and reefs, with the majority located in the Paracel and Spratly Island chains. Many of these islands are partially submerged land masses unsuitable for habitation and are little more than shipping hazards. For example, the total land area of the Spratly Islands encompasses less than 3 square miles. Several of the countries bordering the sea declare ownership of the islands to claim the surrounding sea and its resources. The Gulf of Thailand borders the South China Sea, and although technically not part of it, disputes surround ownership of that Gulf and its resources as well. Asia's robust economic growth boosts demand for energy in the region. The U.S. Energy Information Administration (EIA) projects total liquid fuels consumption in Asian countries outside the Organization for Economic Cooperation and Development (OECD) to rise at an annual growth rate of 2.6 percent, growing from around 20 percent of world consumption in 2008 to over 30 percent of world consumption by 2035. Similarly, non-OECD Asia natural gas consumption grows by 3.9 percent annually, from 10 percent of world gas consumption in 2008 to 19 percent by 2035. -
A Move from the Himalayas to the High Seas?
India-China conflict: A move from the Himalayas to the high seas? A risky naval blockade in the Indian Ocean is touted by some as a way to pressure China’s vital energy routes. By Dr David Brewster Last month’s clash between Indian and Chinese troops in Ladakh was the most significant conflict between the two countries since 1967. Despite signs of a partial tactical pullback in some places, there is considerable risk of further confrontations and even escalation along the disputed border. Some have been urging the Indian government to respond to China’s moves in the Himalayas by placing pressure on Beijing in the Indian Ocean. What are India’s options and how likely is it to take such actions? The Indian Ocean holds a particular place in the India-China strategic relationship. In almost every dimension, whether it be economic, nuclear or the conventional strategic balance along the Line of Actual Control in the Himalayas, India is probably at a considerable strategic disadvantage to China. Only in the Indian Ocean, which includes China’s vital energy routes from the Persian Gulf and Africa, does India have the upper hand. This has important implications for the strategy dynamic. Decades ago, prominent US Sinologist John Garver argued that in the event of a conflict between the two countries, India might be tempted to escalate from the land dimension, where it may suffer reverses, to the maritime dimension, where it enjoys substantial advantages, and employ those advantages to restrict China’s vital Indian Ocean trade. In strategic jargon, the Indian Ocean represents “interior lines” for India – where the Indian Navy is close to its own bases and logistics – and “exterior lines” for China, where its navy is operating with limited logistical support, away from home. -
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. -
The Seasonal Variability of Sea Surface Temperature and Chlorophyll-A Concentration in the South of Makassar Strait
Available online at www.sciencedirect.com ScienceDirect Procedia Environmental Sciences 33 ( 2016 ) 583 – 599 The 2nd International Symposium on LAPAN-IPB Satellite for Food Security and Environmental Monitoring 2015, LISAT-FSEM 2015 The seasonal variability of sea surface temperature and chlorophyll-a concentration in the south of Makassar Strait Bisman Nababan*, Novilia Rosyadi, Djisman Manurung, Nyoman M. Natih, and Romdonul Hakim Department of Marine Science and Technology, Bogor Agricultural University, Jl. Lingkar Akademik, Kampus IPB Darmaga, Bogor 16680, Indonesia Abstract The sea surface temperature (SST) and chlorophyll-a (Chl-a) variabilities in the south of Makassar Strait were mostly affected by monsoonal wind speed/directions and riverine freshwater inflows. The east-southeast (ESE) wind (May-October) played a major role in an upwelling formation in the region starting in the southern tip of the southern Sulawesi Island. Of the 17 years time period, the variability of the SST values ranged from 25.7°C (August 2004) - 30.89°C (March 2007). An upwelling initiation typically occurred in early May when ESE wind speed was at <5 m/s, a fully developed upwelling event usually occurred in June when ESE wind speed reached >5 m/s, whereas the largest upwelling event always occurred in August of each year. Upwelling event generally diminished in September and terminated in October. At the time of the maximum upwelling events (August), the formation of upwelling could be observed up to about 330 km toward the southwest of the southern tip of the Sulawesi island. Interannually, El Niño Southern Oscillation (ENSO) intensified the upwelling event during the east season through an intensification of the ESE wind speed. -
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. -
Impact of the December 2018 Volcano-Triggered Tsunami in Krakatau Complex on the Coastal Geomorphology and the Buildings of the Sunda Strait (Indonesia)
Geophysical Research Abstracts Vol. 21, EGU2019-15880, 2019 EGU General Assembly 2019 © Author(s) 2019. CC Attribution 4.0 license. Impact of the December 2018 volcano-triggered tsunami in Krakatau complex on the coastal geomorphology and the buildings of the Sunda Strait (Indonesia) Efthymios Lekkas (1), Spyridon Mavroulis (1), Marilia Gogou (1), Panayotis Carydis (2), and Dimitrios Milios (1) (1) National and Kapodistrian University of Athens, Faculty of Geology and Geoenvironment, Department of Dynamic Tectonic Applied Geology, Athens, Greece ([email protected]), (2) National Technical University of Athens, Greece On December 22, 2018, a tsunami was generated near the Krakatau volcano complex in Sunda Strait between the Western Java and the Southern Sumatra (Indonesia). It is attributed to the collapse of the flank of the Anak Krakatau volcano, especially in its southern and southwestern sectors. The volcano-triggered tsunami devastated the coastal areas of western Java and southern Sumatra, and in particular Banten Province and Lampung Province respectively. It caused 437 fatalities and about 14059 injured people mainly attributed to the tsunami generation during the night and to absence of early tsunami warning. The tsunami arrived at the coastal areas of western Java and southern Sumatra in 24 to 37 minutes after the eruption of Anak Krakatau occurred at 21:03 of December 22 and with heights varying from almost 1 to 6 m based on recordings of tidal stations, eyewitnesses and tsunami marks on structures and vegetation. The research team of the University of Athens visited the worst tsunami-affected areas shortly after the disaster aiming to investigate the impact on the natural and built coastal environment. -
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. -
CSIRO Report Template
OCEANS AND ATMOSPHERE Bioregions of the Indian Oceans Piers K Dunstan, Donna Hayes, Skipton N C Woolley, Lamona Bernawis, Scott D Foster, Emmanuel Chassot, Eugenie Khani, Rowana Walton , Laura Blamey, Uvicka Bristol, Sean Porter, Arul Ananthan Kanapatipillai, Natasha Karenyi, Babin Ingole, Widodo Pranowo, RA Sreepada, Mohamed Shimal, Natalie Bodin, Shihan Mohamed, Will White, Peter Last, Nic Bax, Mat Vanderklift, Rudy Kloser, Rudy Kloser, Leo Dutra and Brett Molony Bioregions of the Indian Oceans | i Citation Dunstan et al. 2020. Bioregions of the Indian Ocean. CSIRO, Australia. Copyright © Commonwealth Scientific and Industrial Research Organisation 20XX. To the extent permitted by law, all rights are reserved and no part of this publication covered by copyright may be reproduced or copied in any form or by any means except with the written permission of CSIRO. Important disclaimer CSIRO advises that the information contained in this publication comprises general statements based on scientific research. The reader is advised and needs to be aware that such information may be incomplete or unable to be used in any specific situation. No reliance or actions must therefore be made on that information without seeking prior expert professional, scientific and technical advice. To the extent permitted by law, CSIRO (including its employees and consultants) excludes all liability to any person for any consequences, including but not limited to all losses, damages, costs, expenses and any other compensation, arising directly or indirectly from using this publication (in part or in whole) and any information or material contained in it. CSIRO is committed to providing web accessible content wherever possible. -
Summary: This Manuscript Contributes a Reconstruction of Paleo Sea-Level Position at 24 Points in Time Throughout the Mid to Late Holocene
cp-2019-63 Review Feb. 2020 Late Holocene (0-6ka) sea-level changes in the Makassar Strait, Indonesia (Bender et al.) Summary: This manuscript contributes a reconstruction of paleo sea-level position at 24 points in time throughout the mid to late Holocene. Authors interpret the new sea-level index points from the age, elevation, and paleo-water depth interpretation of fossil fringing reefs across SE Sulawesi near Makassar, Indonesia. In contrast to other coral-based reconstructions of past sea- level changes, but in keeping with other Holocene reconstructions from the SW Pacific (e.g. Hallmann et al., 2018), authors evaluate fossil reef growth in a fascinating morphology – microatolls – highlighting the potential for reconstructing past sea-level in great detail using this approach. Additionally, authors combine new data with previous data from two other islands near Makassar (recalculated results of three previous studies to directly compare them), which demonstrate higher-than-present relative (local) sea-level (RSL) during the late Holocene. Results and methods described here underscore the importance of evaluating fossil microatolls in the context of nearby living microatolls. Authors directly compare the elevations of fossil microatolls with their modern counterparts to evaluate the relationship between highest living coral (HLC) and the tidal cycle. Similar to previous works, this study finds that this relationship varies greatly on small spatial scales. To reconstruct paleo sea-level from fossil microatoll elevation requires the assumption that the relationship between HLC and the tidal cycle at that site has remained the same since the microatoll formed. Wisely, this study does not attempt to “connect the dots” and provide an RSL curve, but instead provides sea-level index points that can be compared with other Holocene RSL reconstructions and RSL predictions from GIA modeling. -
Bay of Bengal: from Monsoons to Mixing Ocethe Officiala Magazinen Ogof the Oceanographyra Societyphy
The Oceanography Society Non Profit Org. THE OFFICIAL MAGAZINE OF THE OCEANOGRAPHY SOCIETY P.O. Box 1931 U.S. Postage Rockville, MD 20849-1931 USA PAID Washington, DC ADDRESS SERVICE REQUESTED Permit No. 251 OceVOL.29, NO.2,a JUNEn 2016 ography Register now to attend this conference for international scientific profes- sionals and students. Virtually every facet of ocean color remote sensing and optical oceanography will be presented, including basic research, technological development, environmental management, and policy. October 23–28, 2016 | Victoria, BC, Canada Registration is open! The oral presentation schedule is available on the conference website Submission of abstracts for poster presentation remains open through summer 2016. www.oceanopticsconference.org Bay of Bengal: From Monsoons to Mixing OceTHE OFFICIALa MAGAZINEn ogOF THE OCEANOGRAPHYra SOCIETYphy CITATION Susanto, R.D., Z. Wei, T.R. Adi, Q. Zheng, G. Fang, B. Fan, A. Supangat, T. Agustiadi, S. Li, M. Trenggono, and A. Setiawan. 2016. Oceanography surrounding Krakatau Volcano in the Sunda Strait, Indonesia. Oceanography 29(2):264–272, http://dx.doi.org/10.5670/oceanog.2016.31. DOI http://dx.doi.org/10.5670/oceanog.2016.31 COPYRIGHT This article has been published in Oceanography, Volume 29, Number 2, a quarterly journal of The Oceanography Society. Copyright 2016 by The Oceanography Society. All rights reserved. USAGE Permission is granted to copy this article for use in teaching and research. Republication, systematic reproduction, or collective redistribution of any portion of this article by photocopy machine, reposting, or other means is permitted only with the approval of The Oceanography Society. Send all correspondence to: [email protected] or The Oceanography Society, PO Box 1931, Rockville, MD 20849-1931, USA.