Understanding and Combating Piracy in the Sulu Sea
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Intra-Seasonal Variability of Pacific-Origin Sea Level Anomalies
J Oceanogr (2015) 71:239–249 DOI 10.1007/s10872-015-0281-9 ORIGINAL ARTICLE Intra‑seasonal variability of Pacific‑origin sea level anomalies around the Philippine Archipelago Xiao Chen1,2,3 · Bo Qiu3 · Xuhua Cheng1 · Yiquan Qi1 · Yan Du1 Received: 1 October 2014 / Revised: 23 February 2015 / Accepted: 2 March 2015 / Published online: 20 March 2015 © The Oceanographic Society of Japan and Springer Japan 2015 Abstract Intra-seasonal variability of sea level anomalies 1 Introduction (SLAs) originated in the Pacific Ocean around the Philippine Archipelago was investigated using merged altimetry SLA The Philippine Archipelago is a critical region that plays measurements and eddy-resolving ocean model outputs. an important role in the oceanic exchanges between the The results suggest the SLA signals from the tropical North South China Sea (SCS) and the western Pacific. This region Pacific propagate westward as baroclinic Rossby waves on is characterized by multi-connected ocean passages and an intra-seasonal time scale. Upon impinging the east coast channels (Fig. 1). To the north, the Luzon Strait (sill depth of the Philippines, these Rossby wave signals transform into ~2,200 m) is the main oceanic linkage of the SCS and the coastal trapped waves (CTWs), propagate clockwise along western Pacific. To the south, the Mindoro (sill depth of the coast of the Philippine Archipelago and enter into the ~500 m) and the shallow Balabac Straits connect the Sulu eastern South China Sea (SCS) through the Sibutu Passage Sea and the SCS. The Sibutu Passage (deeper than 200 m) and Mindoro Strait. The SLA signals, however, cannot prop- connects the Sulu and Sulawesi Seas. -
Toward an Enhanced Strategic Policy in the Philippines
Toward an Enhanced Strategic Policy in the Philippines EDITED BY ARIES A. ARUGAY HERMAN JOSEPH S. KRAFT PUBLISHED BY University of the Philippines Center for Integrative and Development Studies Diliman, Quezon City First Printing, 2020 UP CIDS No part of this book may be reprinted or reproduced or utilised in any form or by any electronic, mechanical, or other means, now known or hereafter invented, without written permission from the publishers. Recommended Entry: Towards an enhanced strategic policy in the Philippines / edited by Aries A. Arugay, Herman Joseph S. Kraft. -- Quezon City : University of the Philippines, Center for Integrative Studies,[2020],©2020. pages ; cm ISBN 978-971-742-141-4 1. Philippines -- Economic policy. 2. Philippines -- Foreign economic relations. 2. Philippines -- Foreign policy. 3. International economic relations. 4. National Security -- Philippines. I. Arugay, Aries A. II. Kraft, Herman Joseph S. II. Title. 338.9599 HF1599 P020200166 Editors: Aries A. Arugay and Herman Joseph S. Kraft Copy Editors: Alexander F. Villafania and Edelynne Mae R. Escartin Layout and Cover design: Ericson Caguete Printed in the Philippines UP CIDS has no responsibility for the persistence or accuracy of urls for external or third-party internet websites referred to in this publication, and does not guarantee that any content on such websites is, or will remain, accurate or appropriate. TABLE OF CONTENTS Acknowledgements ______________________________________ i Foreword Stefan Jost ____________________________________________ iii Teresa S. Encarnacion Tadem _____________________________v List of Abbreviations ___________________________________ ix About the Contributors ________________________________ xiii Introduction The Strategic Outlook of the Philippines: “Situation Normal, Still Muddling Through” Herman Joseph S. Kraft __________________________________1 Maritime Security The South China Sea and East China Sea Disputes: Juxtapositions and Implications for the Philippines Jaime B. -
Guidance on Abduction of Crew in the Sulu-Celebes Seas and Waters Off Eastern Sabah
Guidance on Abduction of Crew in the Sulu-Celebes Seas and Waters off Eastern Sabah Produced by: In collaboration with: Supported by: July 2019 ACKNOWLEDGEMENT This guidance was produced by the ReCAAP ISC in collaboration with the Philippine Coast Guard (PCG), and supported by the Asian Shipowners’ Association (ASA) and the Singapore Shipping Association (SSA). This guidance complements the general guidance contained in the ‘Regional Guide to Counter Piracy and Armed Robbery against Ships in Asia’. DISCLAIMER This Guidance, compiled for the Sulu-Celebes Seas and waters off Eastern Sabah, has been prepared for general advisory purpose. This Guidance does not and shall not be construed to impose any obligation or requirement on ship owners or managers to implement any of the measures or advice therein, and any person or entity who wishes to implement the same is advised to exercise due care and discretion in doing so, having due regard to their own requirements and resource capabilities. 2 Contents Introduction 02 Advisory by ReCAAP ISC 04 Measures adopted by the 07 littoral States in the area Modus operandi of past incidents 14 of abduction of crew Case studies of past incidents 20 Information on the Abu Sayyaf 25 Group (ASG) Annex 1 26 Notice to Mariners issued by the Philippines (NOTAM 148-2017 by Philippine Coast Guard) Annex 2 29 Notice to Mariners issued by Malaysia (NOTAM 14 of 2017 by Marine Department of Malaysia, Sabah Region) Annex 3 34 Establishment of Recommended Transit Corridor at Moro Gulf and Basilan Strait issued by the Philippine’s Department of Transportation (Memorandum Circular Number 2017-002 dated 31 March 2017) Annex 4 44 ReCAAP ISC and Supporting Organisations 1 Guidance on Abduction of Crew in the Sulu-Celebes Seas and Waters off Eastern Sabah Introduction This guidance focuses on the incidents of abduction of crew from ships for ransom in the Sulu-Celebes Seas and waters off Eastern Sabah. -
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. -
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. -
PHL-OCHA-Zambo City 3W 25Oct2013
Philippines: Zamboanga Emergency Who-does What Where (3W) as of 25 October 2013 Interventions/Activities Lumbangan SCI Boy Scout Camp Lumbangan ES SCI Camp NDR, WHO UNFPA/FPOP, WHO Pasobolong Elementary School (Closed) Pasabulong ES ! Pasobolong Culianan Community Lunzaran UNFPA/FPOP Taluksangay Capisan Pasonanca Dulian Salaan DOH-CHD SCI SCI Lumbangan Clusters SCI Food Security Lunzaran Hall Boalan ES Pasabolong Health incl. RH UNFPA/FPOP, DOH Maasin UNFPA/FPOP, DOH, PNP SCI Pasonanca ES WVI Protection incl. GBV and CP WVI, SCI SCI UNFPA/FPOP, NDR, ICRC/PRC WASH WHO ICRC/PRC, UNICEF WVI, SAC/CAPIN ICRC/PRC Education ICRC/PRC Logistics Lumbangan BH UNFPA/FPOP, WHO Shelter Taluksangay Nutrition Lunzuran Sta. Maria ES Taluksangay National High School Early Recovery UNFPA/FPOP, Cabatangan DPWH Compound (Closed) ICRC/PRC, WHO, CCCM Minda ! Talabaan ! Livelihood Health/USAID, NDR Boy Scout Camp (Closed) Lunzuran Barangay Hall WVI, UNFPA/FPOP ! ! Lumbangan Brgy. Hall IOM Divisoria ! Boalan Elementary School (Closed) ICRC/PRC Pasonanca ! Zamboanga City Boalan ! Mercedes Pasonanca Elementary School Divisoria Elementary School Taluksangay Bunk House WFP ! Sta. Maria San Roque ! ! Zambowood Elementary School (ZES) Malagutay SCI Mercedes ES Holy Trinity Parish (Closed) Zambowood! ICRC/PRC Divisoria National High School UNFPA/FPOP ! Divisoria ES UNFPA/FPOP, WHO, Tumaga DOH, NCMH, PNP, DepEd Al-Jahara Mosque Putik SCI Taluksangay ES UNFPA/FPOP La Ciudad Montessori School Archdiocese of ZC, UNFPA/FPOP, Merlin, Santa Maria DSWD, Guiwan, ICRC/PRC ! MEMPCO -
The Plate Tectonics of Cenozoic SE Asia and the Distribution of Land and Sea
Cenozoic plate tectonics of SE Asia 99 The plate tectonics of Cenozoic SE Asia and the distribution of land and sea Robert Hall SE Asia Research Group, Department of Geology, Royal Holloway University of London, Egham, Surrey TW20 0EX, UK Email: robert*hall@gl*rhbnc*ac*uk Key words: SE Asia, SW Pacific, plate tectonics, Cenozoic Abstract Introduction A plate tectonic model for the development of SE Asia and For the geologist, SE Asia is one of the most the SW Pacific during the Cenozoic is based on palaeomag- intriguing areas of the Earth$ The mountains of netic data, spreading histories of marginal basins deduced the Alpine-Himalayan belt turn southwards into from ocean floor magnetic anomalies, and interpretation of geological data from the region There are three important Indochina and terminate in a region of continen- periods in regional development: at about 45 Ma, 25 Ma and tal archipelagos, island arcs and small ocean ba- 5 Ma At these times plate boundaries and motions changed, sins$ To the south, west and east the region is probably as a result of major collision events surrounded by island arcs where lithosphere of In the Eocene the collision of India with Asia caused an the Indian and Pacific oceans is being influx of Gondwana plants and animals into Asia Mountain building resulting from the collision led to major changes in subducted at high rates, accompanied by in- habitats, climate, and drainage systems, and promoted dis- tense seismicity and spectacular volcanic activ- persal from Gondwana via India into SE Asia as well -
Maritime Boundary Agreements 172 6.1 Introduction 172 6.2 Saudi-Bahrain 1958 Agreement 172 6.2.1 Historic Background 174 6.2.2 Boundary Delimitation 176
Durham E-Theses Maritime boundary delimitation of the kingdom of Saudi Arabia a study in political geography Al-Muwaled, Faraj Mobarak Jam'an How to cite: Al-Muwaled, Faraj Mobarak Jam'an (1993) Maritime boundary delimitation of the kingdom of Saudi Arabia a study in political geography, Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/10368/ Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in Durham E-Theses • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk 2 MARITIME BOUNDARY DELIMITATION OF THE KINGDOM OF SAUDI ARABIA A STUDY IN POLITICAL GEOGRAPHY Fara.i Mobarak Jam'an AI-Muwaled The copyright of this thesis rests with the author. No quotation from it should be published without his prior written consent and information derived from it should be acknowledged. Thesis submitted for the Degree of Doctor of Philosophy in Social Science in the Department of Geography, Faculty of Social Sciences, University of Durham, U.K. -
VIII-16 Sulu-Celebes Sea: LME #37
VIII East Asian Seas 309 VIII-16 Sulu-Celebes Sea: LME #37 S. Heileman The Sulu-Celebes Sea LME is comprised of the Sulu and Celebes Seas, which are separated from each other by a deep trough and a chain of islands known as the Sulu Archipelago. The LME is bounded by northern Borneo (Malaysia), the southwest coast of the Philippines and Sulawesi Island (northern coast of Indonesia), but most of the LME falls within the archipelagic waters of either the Philippines or Indonesia. The LME covers an area of about one million km2, of which 1.03% is protected, and contains 6.17% and 0.22% of the world’s coral reefs and sea mounts, respectively (Sea Around Us 2007). A complex oceanography results from the Celebes’ strong currents, deep sea trenches, seamounts and active volcanic islands. The LME’s tropical climate is governed by the monsoon regime. During the southwest monsoon months, the northern and central parts of the region are affected by typhoons, which bring intense rains and destructive winds to coastal areas. There are more than 300 major watersheds and 14 major estuaries in the region. A report pertaining to this LME is UNEP (2005). I. Productivity The Sulu-Celebes Sea LME is considered a Class II, moderate productivity ecosystem (150-300 gCm-2yr-1). The tropical climate, warm waters, ocean currents and upwellings make this LME one of the world’s most biologically diverse marine environments. Located near the confluence of three major biogeographic zones and within the Indo- West Pacific centre of biodiversity, the region supports mega-diversity (Roberts et al. -
Geographic Names
GEOGRAPHIC NAMES CORRECT ORTHOGRAPHY OF GEOGRAPHIC NAMES ? REVISED TO JANUARY, 1911 WASHINGTON GOVERNMENT PRINTING OFFICE 1911 PREPARED FOR USE IN THE GOVERNMENT PRINTING OFFICE BY THE UNITED STATES GEOGRAPHIC BOARD WASHINGTON, D. C, JANUARY, 1911 ) CORRECT ORTHOGRAPHY OF GEOGRAPHIC NAMES. The following list of geographic names includes all decisions on spelling rendered by the United States Geographic Board to and including December 7, 1910. Adopted forms are shown by bold-face type, rejected forms by italic, and revisions of previous decisions by an asterisk (*). Aalplaus ; see Alplaus. Acoma; township, McLeod County, Minn. Abagadasset; point, Kennebec River, Saga- (Not Aconia.) dahoc County, Me. (Not Abagadusset. AQores ; see Azores. Abatan; river, southwest part of Bohol, Acquasco; see Aquaseo. discharging into Maribojoc Bay. (Not Acquia; see Aquia. Abalan nor Abalon.) Acworth; railroad station and town, Cobb Aberjona; river, IVIiddlesex County, Mass. County, Ga. (Not Ackworth.) (Not Abbajona.) Adam; island, Chesapeake Bay, Dorchester Abino; point, in Canada, near east end of County, Md. (Not Adam's nor Adams.) Lake Erie. (Not Abineau nor Albino.) Adams; creek, Chatham County, Ga. (Not Aboite; railroad station, Allen County, Adams's.) Ind. (Not Aboit.) Adams; township. Warren County, Ind. AJjoo-shehr ; see Bushire. (Not J. Q. Adams.) Abookeer; AhouJcir; see Abukir. Adam's Creek; see Cunningham. Ahou Hamad; see Abu Hamed. Adams Fall; ledge in New Haven Harbor, Fall.) Abram ; creek in Grant and Mineral Coun- Conn. (Not Adam's ties, W. Va. (Not Abraham.) Adel; see Somali. Abram; see Shimmo. Adelina; town, Calvert County, Md. (Not Abruad ; see Riad. Adalina.) Absaroka; range of mountains in and near Aderhold; ferry over Chattahoochee River, Yellowstone National Park. -
Origin of Marginal Basins of the NW Pacific and Their Plate Tectonic
Earth-Science Reviews 130 (2014) 154–196 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Origin of marginal basins of the NW Pacificandtheirplate tectonic reconstructions Junyuan Xu a,⁎, Zvi Ben-Avraham b,TomKeltyc, Ho-Shing Yu d a Department of Petroleum Geology, China University of Geosciences, Wuhan, 430074, China. b Department of Geophysics and Planetary Sciences, Tel Aviv University, Ramat Aviv 69978, Israel c Department of Geological Sciences, California State University, Long Beach, CA 90840, USA d Institute of Oceanography, National Taiwan University, Taipei, Taiwan article info abstract Article history: Geometry of basins can indicate their tectonic origin whether they are small or large. The basins of Bohai Gulf, Received 4 March 2013 South China Sea, East China Sea, Japan Sea, Andaman Sea, Okhotsk Sea and Bering Sea have typical geometry Accepted 3 October 2013 of dextral pull-apart. The Java, Makassar, Celebes and Sulu Seas basins together with grabens in Borneo also com- Available online 16 October 2013 prise a local dextral, transform-margin type basin system similar to the central and southern parts of the Shanxi Basin in geometry. The overall configuration of the Philippine Sea resembles a typical sinistral transpressional Keywords: “pop-up” structure. These marginal basins except the Philippine Sea basin generally have similar (or compatible) Marginal basins of the NW Pacific Dextral pull-apart rift history in the Cenozoic, but there do be some differences in the rifting history between major basins or their Sinistral transpressional pop-up sub-basins due to local differences in tectonic settings. Rifting kinematics of each of these marginal basins can be Uplift of Tibetan Plateau explained by dextral pull-apart or transtension.