A Study on Low-Frequency Variability in Current and Sea Level in the Lombok Strait and Adjacent Region

Total Page:16

File Type:pdf, Size:1020Kb

A Study on Low-Frequency Variability in Current and Sea Level in the Lombok Strait and Adjacent Region Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1992 A Study on Low-Frequency Variability in Current and Sea Level in the Lombok Strait and Adjacent Region. Dharma Arief Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Arief, Dharma, "A Study on Low-Frequency Variability in Current and Sea Level in the Lombok Strait and Adjacent Region." (1992). LSU Historical Dissertations and Theses. 5289. https://digitalcommons.lsu.edu/gradschool_disstheses/5289 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand corner and continuing from left to right in equal sections with small overlaps. Each original is also photographed in one exposure and is included in reduced form at the back of the book. Photographs included in the original manuscript have been reproduced xerographically in this copy. Higher quality 6" x 9" black and white photographic prints are available for any photographs or illustrations appearing in this copy for an additional charge. Contact UMI directly to order. University Microfilms International A Bell & Howell Information Company 300 North Zeeb Road. Ann Arbor, Ml 48106-1346 USA 313/761-4700 800/521-0600 Order Number 9301036 A study on low-frequency variability in current and sea level in the Lombok Strait and adjacent region Arief, Dharma, Ph.D. The Louisiana State University and Agricultural and Mechanical Col., 1992 UMI 300 N. ZeebRd. Ann Arbor, MI 48106 A STUDY ON LOW FREQUENCY VARIABILITY IN CURRENT AND SEA-LEVEL IN THE LOMBOK STRAIT AND ADJACENT REGION A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College In partial fulfillment of the requirements for the degree of Doctor of Philosophy In Department of Oceanography and Coastal Sciences by Dharma Arief B.S., Bandung Institute of Technology, 1977 M.S., Louisiana State University 1988 May 1992 ACKNOWLEDGEMENTS I would like to thank to Dr.Stephen P. Murray, Coastal Studies Institute, Louisiana State University, for his guidance in conducting this research and during the writing of this manu­ script. Appreciations are extended to Dr. William J.Wiseman Jr., Dr. Masamichi Inoue, Dr. Harry H.Roberts, and Dr. S.A.Hsu for their valuable suggestions and advice. I also thank to Dr. Nan van Heerden, and all personnel of Coastal Studies Institute for their assistance during this research. Special acknowledgement is due to my parents, my wife Lya, and my children Ayusta and Riana for their support and understanding. ii TABLE OF CONTENTS ACKNOWLEDGEMENTS .............................................................................................................. ii TABLE OF CONTENTS ................................................................................................................. iii LIST OF TABLES............................................................................................................................ vi LIST OF FIGURES.......................................................................................................................... vii ABSTRACT....................................................................................................................................... X I. INTRODUCTION .......................................................................................................................... 1 II. BACKGROUND KNOWLEDGE .............................................................................................. 8 A. THE INDONESIAN SEAS .................................................................................................... 8 1. Topographic setting .......................................................................................................... 8 2. Circulation ........................................................................................................................... 9 3. Water m asses ..................................................................................................................... 10 B. THE SOUTH COAST OF JAVA - LOMBOK REGION ................................................. 11 1. Topographic s e ttin g .......................................................................................................... 11 2. Circulation ............... 11 C. THE LOMBOK STRAIT ....................................................................................................... 12 1. Topographic s e ttin g ................................................................................................... 12 2. Oceanographic measurements: ..................................................................................... 13 3. Water m asses ..................................................................................................................... 14 4. Circulation: .......................................................................................................................... 14 D. REGIONAL METEOROLOGICAL CONDITIONS......................................................... 15 1. S easonal P eriod ................................................................................................................. 15 2. Intraseasonal period .......................................................................................................... 16 3. Cyclones .............................................................................................................................. 17 4. Westerly Wind B urst .......................................................................................................... 18 E. CHAPTER SUMMARY......................................................................................................... 19 III. MATERIALS AND METHODS............................................................................................... 20 A. DATA......................................................................................................................................... 20 1. Current .................................................................................................................................. 20 2. Sea Level / Pressure G auge ............................................................................................ 22 3. Wind and Atmospheric Pressure .................................................................................... 22 B. M ETHODS.............................................................................................................................. 24 1. Interpolation for missing d a t a ........................................................................................ 24 i i i 2. Coordinate rotation ......................................................................................................... 27 3. Data Filtering .................................................................................................................... 27 4. Time domain analysis ..................................................................................................... 28 5. Spectral A nalysis.................................... 29 IV. DESCRIPTION OF PHYSICAL PROCESSES IN THE LOMBOK STRAIT................ 31 A. CURRENTS IN THE LOMBOK STRAIT........................................................................ 31 1. Directional and Vertical Properties .............................................................................. 31 2. Monthly C urrents ............................................................................................................ 36 3. Spectral Characteristics of AE25 C urrents................................................................. 39 4. Sub-tidal Currents at A E 25 ........................................................................................... 43 B. SEA LEVEL IN THE LOMBOK STRAIT ........................................................................ 46 1. S ea Level Characteristics ............................................................................................. 46 2. Spectral Characteristics ................................................................................................. 46 V. CURRENT AND SEA-LEVEL SLOPE RELATION IN THE LOMBOK STRAIT 51 A. CURRENTS - SEA-LEVEL SLOPES RELATIONSHIP .............................................
Recommended publications
  • EARTH OBSERVATION of OCEAN ACIDIFICATION
    EARTH OBSERVATION of OCEAN ACIDIFICATION: The case of Nusa Penida, Kelungkung, East Bali FAJAR EKO PRIYANTO February, 2019 SUPERVISORS: Dr. ir. S. Salama Dr. ir. C. M. M. Mannaerts EARTH OBSERVATION of OCEAN ACIDIFICATION: The case of Nusa Penida, Kelungkung, East Bali Submitted by: FAJAR EKO PRIYANTO S6036074 Enschede, The Netherlands, February 2019 SUPERVISORS: Dr. ir. S. Salama Dr. ir. C. M. M. Mannaerts REPORT ASSESSMENT BOARD: Dr. ir. C. Van der Tol (Chairman) Dr. A. Hommerssom (External Examiner, WaterInsight) Submitted to: Department of Water Resources and Environmental Management (WREM) Faculty of Geo-Information Science and Earth Observation, University of Twente, The Netherlands DISCLAIMER This document describes work undertaken as part of a programme of study at the Faculty of Geo-Information Science and Earth Observation of the University of Twente. All views and opinions expressed therein remain the sole responsibility of the author, and do not necessarily represent those of the Faculty. ABSTRACT In this century, increasing carbon dioxide anthropogenic concentration in the atmosphere becomes an important issue which causes environmental problems such as global warming and ocean acidification. Oceans are known to act as a buffer in the ocean acidification. The key marine organisms such as fish and coral reef could diminish due to the difficulty to survive and sustain because of ocean acidification. Bali, an island in Indonesia has a good quality of coral cover can also be affected by ocean acidification. Monitoring the Sea Surface Total Alkalinity would help us to know how far our ocean can survive from additional acid due to ocean acidification. It could give us a better understanding of the correlation between ocean acidification and ecological condition.
    [Show full text]
  • Climate Change Conference 2007
    1 climate chanuge cnonference 2OO7 c o n t e n t CONFERENCE OUTLINE 2 GENERAL INFORMATION 3 ACCOMMODATION 10 OPTIONAL TOURS 18 PRE / POST-CONFERENCE TOURS 19 conference outline general information CONFERENCE DATES 3 - 14 December 2007 VENUE Bali International Convention Centre (BICC) P.O. Box 36, Nusa Dua, Bali 80363, INDONESIA 2 Tel. (62 361) 771 906 3 Fax. (62 361) 772 047 http://www.baliconvention.com OVERVIEW SCHEDULE Thirteenth session of the Conference of the Parties (COP 13) Third session of the Conference of the Parties serving as the meeting of the Parties to the Kyoto Protocol (CMP 3) Twenty-seventh session of the Subsidiary Body for Scientific and Technological Advice (SBSTA 27) Twenty-seventh session of the Subsidiary Body for Implementation (SBI 27) Resumed fourth session of the Ad Hoc Working Group on Further Commitments for Annex I INDONESIA Parties under the Kyoto Protocol (AWG 4) Situated between two continents and two oceans, the Indian and Pacific oceans, Indonesia is the Note: world's largest archipelago comprising some 17,508 islands that stretch across the equator for This schedule is intended to assist participants with their planning prior to attending the sessions. more than 5,000 miles. Straddling the equator, Indonesia is distinctly tropical with two seasons: It will be updated as new information becomes available on the website of the United Nations dry and rainy season. With its geographical location in South East Asia, Indonesia is accessible for Framework Convention on Climate change <unfccc.int>. Once the sessions are underway, please delegates regardless of the region they are from.
    [Show full text]
  • Expedition Report Transport Indonesian Seas, Upwelling, and Mixing Physics (TRIUMPH) 2019
    Expedition Report Transport Indonesian seas, Upwelling, and Mixing Physics (TRIUMPH) 2019 Leg 1 & Leg 2 (37 Days) November 18th – December 24th 2019 Prepared by: Center of Deep-Sea Research, Indonesia Institute of Science LIPI (CDSR LIPI), Indonesia The First Institute of Oceanography, MNR (FIO MNR), China University of Maryland (UMD), USA Version 1, December, 24th 2019 EXPEDITION REPORT OF THE PROJECT: “TRansport Indonesian seas, Upwelling, and Mixing PHysics (TRIUMPH) 2019” Executive Summary The Indonesian seas provide a low-latitude pathway for the transfer of warm, relatively low salinity Pacific waters into the Indian Ocean, known as the Indonesia Through-flow (ITF) which has impacts on the basin budgets of the Pacific and the Indian Oceans. Indonesian seas host the strongest equatorial convective center that drives the global tropical circulation (Walker Circulation), which affects Madden-Julian Oscillation (MJO), Asian-Australian monsoon and interacts with El Niño-Southern Oscillation (ENSO). Indonesia Through-Flow (ITF), flow through several waters in Indonesia seas like Seram Sea, Banda Sea, Makassar Strait, Lombok Strait and Eastern Indian Ocean which classified as deep ocean. The Makassar Strait, Lifamatola Strait / Seram Sea, and Karimata Strait are three main inflow passages and Lombok, Alas, Sape Straits, and Timor passage are the exit pathways of the ITF which transmit water masses from the Pacific Ocean to the Indian Ocean and also transform the water mass by mixing and intensive internal-wave generation. The deep ocean is a dynamic, yet poorly explored system that provides critical climate regulation, host a wealth of hydrocarbon, mineral, and genetic resources, and represent a vast repository for biodiversity.
    [Show full text]
  • 1 Investigation of the Energy Potential from Tidal Stream
    INVESTIGATION OF THE ENERGY POTENTIAL FROM TIDAL STREAM CURRENTS IN INDONESIA Kadir Orhan1, Roberto Mayerle1, Rangaswami Narayanan1 and Wahyu Widodo Pandoe2 In this paper, an advanced methodology developed for the assessment of tidal stream resources is applied to several straits between Indian Ocean and inner Indonesian seas. Due to the high current velocities up to 3-4 m/s, the straits are particularly promising for the efficient generation of electric power. Tidal stream power potentials are evaluated on the basis of calibrated and validated high-resolution, three-dimensional numerical models. It was found that the straits under investigation have tremendous potential for the development of renewable energy production. Suitable locations for the installation of the turbines are identified in all the straits, and sites have been ranked based on the level of power density. Maximum power densities are observed in the Bali Strait, exceeding around 10kw/m2. Horizontal axis tidal turbines with a cut-in velocity of 1m/s are considered in the estimations. The highest total extractable power resulted equal to about 1,260MW in the Strait of Alas. Preliminary assessments showed that the power production at the straits under investigation is likely to exceed previous predictions reaching around 5,000MW. Keywords: renewable energy; tidal stream currents; numerical model; Indonesia INTRODUCTION The global energy supply is facing severe challenges in terms of long-term sustainability, fossil fuel reserve exhaustion, global warming and other energy related environmental concerns, geopolitical and military conflicts surrounding oil rich countries, and secure supply of energy. Renewable energy sources such as solar, wind, wave and tidal energy are capable of meeting the present and future energy demands with ease without inflicting any considerable damage to global ecosystem (Asif et al.
    [Show full text]
  • Short-Term Variation of the Surface Flow Pattern South of Lombok Strait Observed from the Himawari-8 Sea Surface Temperature †
    remote sensing Letter Short-Term Variation of the Surface Flow Pattern South of Lombok Strait Observed from the Himawari-8 Sea Surface Temperature † Naokazu Taniguchi 1 , Shinichiro Kida 2 , Yuji Sakuno 1,* , Hidemi Mutsuda 1 and Fadli Syamsudin 3 1 Graduate School of Engineering, Hiroshima University, Higashi-Hiroshima 739-8527, Japan; [email protected] (N.T.); [email protected] (H.M.) 2 Research Institute for Applied Mechanics, Kyushu University, Kasuga 816-8580, Japan; [email protected] 3 Agency for the Assessment and Application of Technology (BPPT), Jakarta 10340, Indonesia; [email protected] * Correspondence: [email protected]; Tel.: +81-82-424-7773 † This paper is an extended version of our paper published in SPIE Proceedings Volume 10778: Remote Sensing of the Open and Coastal Ocean and Inland Waters. Received: 6 May 2019; Accepted: 18 June 2019; Published: 24 June 2019 Abstract: Spatial and temporal information on oceanic flow is fundamental to oceanography and crucial for marine-related social activities. This study attempts to describe the short-term surface flow variation in the area south of the Lombok Strait in the northern summer using the hourly Himawari-8 sea surface temperature (SST). Although the uncertainty of this temperature is relatively high (about 0.6 ◦C), it could be used to discuss the flow variation with high spatial resolution because sufficient SST differences are found between the areas north and south of the strait. The maximum cross-correlation (MCC) method is used to estimate the surface velocity. The Himawari-8 SST clearly shows Flores Sea water intruding into the Indian Ocean with the high-SST water forming a warm thermal plume on a tidal cycle.
    [Show full text]
  • Land Use and Endemic Avian Biodiversity on Nusa Penida
    bioRxiv preprint doi: https://doi.org/10.1101/2021.06.20.449190; this version posted June 21, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. Land Use and Endemic Avian Biodiversity on Nusa Penida Ashlee A. Abrantes 1 and William D. Brown2 1 School of Environmental and Forest Sciences, University of Washington, Seattle, WA, USA 2 Department of Biology, State University of New York at Fredonia, Fredonia, NY, USA; email: [email protected] AAA: 3715 W. Stevens Way NE, Seattle, WA 98195 WDB: 280 Central Ave, Fredonia, NY, 14063, Summary Understanding anthropogenic alterations to land use and their effects can inform conservation efforts in tropical biodiversity hotspots. In 2004 the Indonesian Palau Penida Archipelago, off the coast of Bali, was established as an unofficial bird reserve; however, studies of the islands’ land use and avian biodiversity were never conducted and have not been monitored. I surveyed birds across 32 transects in land use categories designated: agriculture, deforested, developed, and forest. Forest transects presented the greatest endemic species richness, but overall, Shannon diversity different significantly among land use categories, particularly forested and deforested. ANOVA indicated exotic bird density was significantly higher than endemic bird density across all transects. Birds serve as a common biodiversity barometer and this study can serve to inform land use management decisions on the Archipelago and throughout reserves and protected areas throughout the tropics. bioRxiv preprint doi: https://doi.org/10.1101/2021.06.20.449190; this version posted June 21, 2021.
    [Show full text]
  • CHAPTER 1 6 DEFEAT in ABDA RILE the Japanese Surface Forces
    CHAPTER 1 6 DEFEAT IN ABDA RILE the Japanese surface forces stealing up the Musi River wer e W being continuously attacked by Allied air forces on the 15th Feb- ruary, Doorman's striking force was the target for repeated fierce attack s by Japanese aircraft to the east of Banka Island . The force weighed and left Oosthaven at 4 p .m. on the 14th, and formed in two columns . The Dutch cruisers, led by De Ruyter, were to starboard ; and the British, led by Hobart as Senior Officer, to port . The six U.S. destroyers screened ahead ; and three Dutch astern. One of the four Dutch ships had bee n sent on ahead to mark Two Brothers Island off the south-east coast o f Sumatra, and join later. Air reconnaissance on the 13th had indicated four groups of enemy vessels : two cruisers, two destroyers, and two transports about sixty miles south of the Anambas Islands, steering south-west a t 10 a.m. ; one cruiser, three destroyers and eight transports some twenty miles to the eastward of the first group, and steering south at 10.30 a.m. ; three cruisers, five destroyers and one transport, about sixty miles nort h of Banka Island and steering west at 3 .30 p.m.; and two destroyers with fourteen transports about 100 miles north of Billiton island, and steerin g S.S.W., at 4.30 p.m. Doorman led his force northwards in accordance with the decision s reached by him and Helfrich—to go northwards through Gaspar Strait, round Banka, and back through Banka Strait, "destroying any enemy force s seen".
    [Show full text]
  • Prakiraan Cuaca Wilayah Pelayanan
    BADAN METEOROLOGI KLIMATOLOGI DAN GEOFISIKA Jl Angkasa 1 No.2 Kemayoran, Jakarta 10720 Telp. 021-6546318 Fax. 021-6546314 / 6546315 Email : [email protected] INDONESIA WEATHER BULLETIN FOR SHIPPING Nomor : ME.301/WB/25/APM/XI/BMKG-2016 ISSUED BY BMKG AT 0230 UTC THURSDAY NOVEMBER 25, 2016 FORECAST VALID FOR 24 HOURS FROM 0300 UTC NOVEMBER 25, 2016 PART I WARNING TS TOKAGE 1000HPA POSITION 11.3N 122.5E MAXIMUM WINDSPEED NEAR CENTRE 35KT MOVE TO WNW. PART II GENERAL SITUATION FOR NOVEMBER 24, 2016 12.00 UTC LOW PRESSURE AREA 1007HPA IN INDIAN OCEAN WESTERN OF LAMPUNG. EDDY CIRCULATION AREA IN NORTHERN PART OF MALACCA STRAIT AND EASTERN PART OF CENDRAWASIH GULF. WESTERLY TO NORTHERLY LIGHT TO MODERATE FLOW IN NORTHERN PART OF INDONESIA EXCEPT SOUTHERLY LIGHT TO MODERATE FLOW IN NORTHERN PART OF MAKASSAR STRAIT AND MOLUCCA SEA. EASTERLY TO SOUTHERLY LIGHT TO MODERATE FLOW IN SOUTHERN PART OF INDONESIA EXCEPT SOUTHWESTERLY TO NORTHWESTERLY LIGHT TO MODERATE FLOW IN WESTERN OF SUMATRA WATERS. PART III FORECAST EASTERLY TO SOUTHERLY 3 TO 4 BF OCCURS IN SOUTHERN OF CENTRE JAVA TO SUMBA ISLAND WATERS, SAWU SEA, KUPANG – ROTE ISLAND WATERS, INDIAN OCEAN SOUTHERN OF CENTRE JAVA TO EAST NUSA TENGGARA, EASTERN PART OF JAVA SEA, BANDA SEA, ARAFURU SEA, SERMATA – LETI ISLAND WATERS, BABAR TANIMBAR ISLAND WATERS, YOS SUDARSO ISLAND TO MERAUKE WATERS. 4 TO 5 BF OCCURS IN INDIAN OCEAN SOUTHERN OF BANTEN TO WEST JAVA. SOUTHERLY TO SOUTHWESTERLY 3 TO 4 BF OCCURS IN MAKASSAR STRAIT, TOLO GULF, MOLUCCA SEA, WESTERN PART OF HALMAHERA WATERS.
    [Show full text]
  • Sustainable Development Plan in Coastal Area: Nusa Penida, Bali, Indonesia
    SUSTAINABLE DEVELOPMENT PLAN IN COASTAL AREA: NUSA PENIDA, BALI, INDONESIA A.A. Ayu Arun Suwi Arianty & Kadek Feni Aryati Sekolah Tinggi Pariwisata Bali Internasional, Indonesia. Corresponding Email: [email protected] _________________________________________________________________________________________________________________________ Abstract Bali is one of the most favorable tourist destinations in the world. It is proven by several awards putting Bali as one of the best destinations on earth. TripAdvisor Travellers’ Choice Awards awarded Bali as the fourth World’s Best Destination after Paris, London, and Rome. Internationale Tourismus Borse Berlin, Germany places Bali in Top 100 Destinations. Then, it is not surprising that the numbers of tourists coming to Bali is increasing year by year. According to Central Bureau of Statistic Bali, in 2018, the international tourist visiting Bali increased to 6.07 million from about 5.69 million in 2017(1). Bali has a lot of tourist destinations which can be visited by visitors, both domestic visitors and foreign visitors, such Kuta, Ubud, Jimbaran, and many more. In the last 10 years, one of islands in Bali, Nusa Penida has become one of the popular destinations in Bali. Bali has several islands which are separated from the main island, Bali Island(2). They are Nusa Penida, Nusa Lembongan, Nusa Ceningan. Menjangan Island, and Serangan Island. Nusa Penida Island, Nusa Lembongan Island, and Nusa Ceningan Island are well known as three-sister islands. Geographically, they are included in the Klungkung Regency. Nusa Penida Island is the biggest among those three. This island consistently develops itself as one of the famous destinations in Bali after Kuta, Ubud, and Jimabaran(3).
    [Show full text]
  • LESSER SUNDA NINE Lesser Sunda GLAUDY PERDANAHARDJA &HILDA LIONATA YEARS IN
    NINE YEARS IN Lesser Sunda NINE YEARS IN LESSER SUNDA Subject to misprints, errors and change without notice. This book produced by The Nature Conservancy ©, Jakarta, Indonesia. Not to be reproduced, wholly or in part, whithout written permission of The Nature Conservancy ©, Jakarta, Indonesia. GLAUDY PERDANAHARDJA & HILDA LIONATA NINE YEARS IN Lesser Sunda NINE YEARS IN LESSER SUNDA Author: Glaudy Perdanahardja Hilda Lionata Editor: Melati Kaye Photo Contributor: Benjamin Kahn Rizya Ardiwijaya Yusuf Fajariyanto Rynal Fadli Putu Oktavia Tommy Prasetyo Wibowo Wildlife Conservation Society Supported by: Recommended citation: Perdanahardja, G., Lionata, H. (2017) Nine Years In Lesser Sunda. Indonesia: The Nature Conservancy, Indonesia Coasts and Oceans Program © 2017 The Nature Conservancy First published 2017 by The Nature Conservancy Designed and produced by: Imaginarium (www.imaginariumind.com) All Rights Reserved. Reproduction for any purpose is prohibited without prior permission. Cover Photo: Documentations of The Nature Conservancy Available at: The Nature Conservancy Graha Iskandarsyah 3rd Floor Jl. Iskandarsyah Raya No. 66C Kebayoran Baru, Jakarta Selatan Indonesia Or via the worldwide web at: www.nature.or.id NINE YEARS IN LESSER SUNDA CONTENTS ACKNOWLEDGEMENT 03 FOREWORD 05 MESSAGE FROM THE 07 COUNTRY DIRECTOR I. Introduction 11 I.1. Why Lesser Sunda? 13 I.1.1 Ecological Importance of Lesser Sunda 15 I. Table 1.1: List of Species in Lesser Sunda and The Protection Status 17 According to IUCN, Cites and Govt Reg No. 7/99 I.1.2. Economic Importance of Lesser Sunda 20 I.1.3. Lesser Sunda in The Bigger Context 22 I.2. TNC’s Footpath in Lesser Sunda 23 II.
    [Show full text]
  • (Local Genius) As Sociocultural Capital to Develop Tourism
    Advances in Social Science, Education and Humanities Research, volume 394 3rd International Conference on Innovative Research Across Disciplines (ICIRAD 2019) Empowering Local Potentiality (Local Genius) as Sociocultural Capital to Develop Tourism I Wayan Kertih Universitas Pendidikan Ganesha Singaraja, Indonesia [email protected] Abstract— This study aimed at identifying local genius local genius. However, it has not been revealed, studied, and empowerment as socio-cultural capital to develop tourism in Nusa accommodated in a certain science and technology. Considering Penida, Bali province by using a cultural ethnographic study various studies and empirical experiences, it indicates that the approach. The respondents in this study were determined through support from the socio-cultural capital from the local genius helps snowball sampling. The result showed that there were various forms to prompt the development of tourism in Indonesia, [4,6,7], a and types of local potentiality which can be used as objects and more intensive study needs to be done to give the picture of the supporting capacity for developing tourism in Nusa Penida District; community socio-cultural capital from the internal perspective in local genius in the community has not been optimally empowered to which the inner power and inner beauty of the civilization makes develop tourism, and the local potentialities have not yet been it possible to find and to weave and maintain the local culture and socialized as interesting tourist objects. The result implies a need for increase the nation’s competitive advantage. a new approach in socializing to the supporting community for empowering local potentialities as socio-cultural capital to support tourism development in Nusa Penida; and a need for an academic II.
    [Show full text]
  • View Full Activity Guide
    Experience Guide Contents The Amankila Experience 4 Water Adventures 5 Cruising & Snorkelling 6 Diving 7 Surfing 10 Beach Club Activities 13 Adventures on Land 14 Nature & Adventure 15 Sport & Mindfulness 17 Cultural Insights 19 Balinese Celebrations 20 Cultural Tours & Parks 21 East Bali Tour 23 Temples 25 Helicopter Transfer & Tours 26 Culinary Experiences 27 All Day Enjoyments 28 Special Evenings 30 Kila Kids & Families 32 Amankila & Sustainability 35 The Amankila Experience Karangasem Regency, which sits in the shadow of the majestic Mount Agung, is known as one of the most traditional regencies in Bali. Showcasing some of Bali’s most beautiful hidden treasures, including famed Water Palaces and stunning temples, this peaceful corner of Eastern Bali also boasts a beautiful coastline. From cultural tours, to scenic treks and cycle rides, to chartered snorkelling trips on one of Amankila’s traditional outrigger boats, Amankila offers a wide variety of activities to keep guests of all interests entertained. With the Beach Club set back from our private black sand beach and our famed three-tiered swimming pool overlooking the Lombok Strait, secluded places to relax abound. Indulge in Aman Signature Rituals at our Spa or opt for a private sunrise breakfast or beachside dinner. The options are endless, and we hope that you will make this a truly memorable stay. At Amankila, we would be pleased to tailor any activity to your particular needs and interests. Should you wish to organise any of our activities, please speak with our Guest Hosts at Reception or by dialling ‘1’ from your Suite phone. I would also be happy to discuss your itinerary with you personally to share my own insights and recommendations for an unforgettable stay in East Bali.
    [Show full text]