Alam Lestari Vol. IX October 2008-April 2009
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Estimation of Sea Current Energy Potential by Using Calculation
Bulletin of the Marine Geology, Vol. 32, No. 2, December 2017, pp. 51 to 60 Estimation of Sea Current Energy Potential by Using Calculation Models of Horizontal Axis Current Turbine in Toyapakeh Strait, Nusa Penida, Bali Estimasi Potensi Energi Arus Laut Dengan Menggunakan Perhitungan Model Turbine Arus Poros Horizontal di Selat Toyapakeh, Nusa Penida, Bali Beben Rachmat and Delyuzar Ilahude Marine Geological Institute, Jl. Dr. Djundjunan No. 236, Bandung, 40174 Corresponding author : [email protected] (Received 27 February 2017; in revised from 04 August 2017; accepted 02 November 2017) ABSTRACT: Toyapakeh Strait has a fairly strong ocean current velocity with a velocity between 0.5 m/s – 3.2 m/s. The duration of the strong current (V> 0.5 m/s) ranges from 13-22 hours per day. The location of the strong current occurrence is located to the east of Nusa Lembongan Island, precisely at the stationary current measurement location. Vertical distribution of the direction and velocity currents at this location are not uniform from the top to the bottom, especially in the water column depths of 2 m, 4 m and 6 m, whereas at the water column depths of 8 m to 16 m are relatively uniform. Calculation results of potential electrical power by using the horizontal axis turbine model with a capacity of 35.9 kW (Rite Verdan), 100 kW (Tocardo DD702HT) and 250 kW (Tocardo DD1001HT) show that all of the values have the optimal electric powers, especially during the spring tide, whereas during the neap tide only the turbine with a capacity of 35.9 kW can retrieved an optimal electrical power. -
From the Jungles of Sumatra and the Beaches of Bali to the Surf Breaks of Lombok, Sumba and Sumbawa, Discover the Best of Indonesia
INDONESIAThe Insiders' Guide From the jungles of Sumatra and the beaches of Bali to the surf breaks of Lombok, Sumba and Sumbawa, discover the best of Indonesia. Welcome! Whether you’re searching for secluded surf breaks, mountainous terrain and rainforest hikes, or looking for a cultural surprise, you’ve come to the right place. Indonesia has more than 18,000 islands to discover, more than 250 religions (only six of which are recognised), thousands of adventure activities, as well as fantastic food. Skip the luxury, packaged tours and make your own way around Indonesia with our Insider’s tips. & Overview Contents MALAYSIA KALIMANTAN SULAWESI Kalimantan Sumatra & SUMATRA WEST PAPUA Jakarta Komodo JAVA Bali Lombok Flores EAST TIMOR West Papua West Contents Overview 2 West Papua 23 10 Unique Experiences A Nomad's Story 27 in Indonesia 3 Central Indonesia Where to Stay 5 Java and Central Indonesia 31 Getting Around 7 Java 32 & Java Indonesian Food 9 Bali 34 Cultural Etiquette 1 1 Nusa & Gili Islands 36 Sustainable Travel 13 Lombok 38 Safety and Scams 15 Sulawesi 40 Visa and Vaccinations 17 Flores and Komodo 42 Insurance Tips Sumatra and Kalimantan 18 Essential Insurance Tips 44 Sumatra 19 Our Contributors & Other Guides 47 Kalimantan 21 Need an Insurance Quote? 48 Cover image: Stocksy/Marko Milovanović Stocksy/Marko image: Cover 2 Take a jungle trek in 10 Unique Experiences Gunung Leuser National in Indonesia Park, Sumatra Go to page 20 iStock/rosieyoung27 iStock/South_agency & Overview Contents Kalimantan Sumatra & Hike to the top of Mt. -
Data Peminat Dan Terima Di Universitas Mulawarman
DATA PEMINAT DAN TERIMA DI UNIVERSITAS MULAWARMAN JALUR SNMPTN 2020 PEMINAT PEMINAT Nama Provinsi Nama Kota NAMA SEKOLAH LULUS PL1 LULUS PL2 JML LULUS PL1 PL2 Kalimantan Timur Kab Berau MAN BERAU 20 4 15 4 SMA IT ASH SHOHWAH 1 SMA NEGERI 12 BERAU 26 8 25 1 9 SMAN 1 BERAU 33 13 28 13 SMAN 10 BERAU 1 1 SMAN 11 BERAU 6 1 6 1 SMAN 13 BERAU 3 1 SMAN 14 BERAU 1 1 SMAN 2 BERAU 37 8 33 8 SMAN 3 BERAU 20 5 18 1 6 SMAN 4 BERAU 28 7 21 2 9 SMAN 5 BERAU 17 2 9 1 3 SMAN 6 BERAU 14 1 12 1 SMAN 7 BERAU 28 6 19 6 SMAN 8 BERAU 37 8 34 1 9 SMAS MUHAMADIYAH TANJUNG REDEB 2 2 SMAS PGRI 13 TANJUNG REDEB 15 2 11 2 SMK NEGERI 8 BERAU 8 3 6 3 SMKN 1 BERAU 12 11 SMKN 2 BERAU 4 1 2 1 2 SMKN 6 BERAU 2 2 Kab Berau Total 315 69 257 7 76 Kab Kutai Barat MAN KUTAI BARAT 6 1 5 1 SMAN 1 BENTIAN BESAR 2 1 SMAN 1 BONGAN 6 5 SMAN 1 JEMPANG 6 1 4 1 SMAN 1 LINGGANG BIGUNG 39 11 29 1 12 SMAN 1 LONG IRAM 11 2 11 2 SMAN 1 MUARA LAWA 11 2 10 2 SMAN 1 MUARA PAHU 5 1 5 1 PEMINAT PEMINAT Nama Provinsi Nama Kota NAMA SEKOLAH LULUS PL1 LULUS PL2 JML LULUS PL1 PL2 SMAN 1 PENYINGGAHAN 10 3 7 3 SMAN 1 SENDAWAR 47 15 34 1 16 SMAN 1 SILUQ NGURAI 4 3 SMAN 2 SENDAWAR 19 10 15 10 SMAN 3 SENDAWAR 6 1 4 1 SMKN 1 SENDAWAR 16 5 16 5 SMKN 2 SENDAWAR 8 1 6 1 Kab Kutai Barat Total 196 53 155 2 55 Kab Kutai Kartanegara MA DDI KARYA BARU LOA JANAN 6 1 6 1 MA Negeri 1 Kutai Kartanegara 13 3 12 3 MAN 2 KUTAI KARTANEGARA 70 20 57 20 MAS AS ADIYAH SANTAN TENGAH 6 2 6 2 MAS MIFTAHUL ULUM ANGGANA 18 5 18 5 SMA AL HAYAT SAMBOJA 1 1 SMA ISLAM ULUMUDDIN SAMBOJA 2 1 2 1 SMA IT NURUL ILMI TENGGARONG 10 1 9 1 -
Obtaining World Heritage Status and the Impacts of Listing Aa, Bart J.M
University of Groningen Preserving the heritage of humanity? Obtaining world heritage status and the impacts of listing Aa, Bart J.M. van der IMPORTANT NOTE: You are advised to consult the publisher's version (publisher's PDF) if you wish to cite from it. Please check the document version below. Document Version Publisher's PDF, also known as Version of record Publication date: 2005 Link to publication in University of Groningen/UMCG research database Citation for published version (APA): Aa, B. J. M. V. D. (2005). Preserving the heritage of humanity? Obtaining world heritage status and the impacts of listing. s.n. Copyright Other than for strictly personal use, it is not permitted to download or to forward/distribute the text or part of it without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license (like Creative Commons). Take-down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. Downloaded from the University of Groningen/UMCG research database (Pure): http://www.rug.nl/research/portal. For technical reasons the number of authors shown on this cover page is limited to 10 maximum. Download date: 23-09-2021 Appendix 4 World heritage site nominations Listed site in May 2004 (year of rejection, year of listing, possible year of extension of the site) Rejected site and not listed until May 2004 (first year of rejection) Afghanistan Península Valdés (1999) Jam, -
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. -
The Kelay Punan in East Kalimantan
TROPICS Vol. r(213),pp. 143-153 Issued December, 1991 Changes ln Economic Life of the Hunters and Gatherers : the Kelay Punan in East Kalimantan Makoto INoun Faculty of Agriculnre, University of Tokyo, l-1-l Yayoi, Bunkyo-ku, Tokyo 113, Japan LucnN Faculty of reaching and Education, Mulawarman University, Kampus Gunung Kelua, Samarinda, Kalimantan Timur, Indonesia Icrn Bilung Tiopical Rain Forest Research Center, Mulawarman University, Kampus Gunung Kelua, Samarinda, Kalimantan Timur, Indonesia Abstract : The Punan people in Bomeo island had traded forest products for the necessities of life with the Dayak people, who traded them with the brokers. At present, the Kelay Punan people in East Kalimantan rade directly with the brokers and merchants, who control the rade of the forest products from the region. They are degraded to debtors now and still carrying out hunting and gathering to pay back the debt" Besides, the inroduction of swidden cultivation is one of the most important factors to affect their life style. Their swidden system might not be so sustainable, since they were not tradirional swidden cultivators like the Kenyah Dayak people. Key Words: East Kalimantan / Punan / swidden cultivation / trade The "Punan" is a generic term for hunters and gatherers living in Borneo island. The Punan people have the same physical characteristics as the Dayaks practicing swidden cultivation, since the Punans are also the protd-Malayan people. The bodies of the Punans, however, are generally better-built than those of the Dayaks. According to Hoffman (1983), Bock's description of the Punan (Bock, 1881) is one of the earliest to appear in print. -
Chapter Ii the Description of Plastic Dumps Issues in Bali's Ocean And
CHAPTER II THE DESCRIPTION OF PLASTIC DUMPS ISSUES IN BALI’S OCEAN AND COASTLINES On this chapter, the writer would focus on the explanation about how plastic dumps in Bali, Indonesia became one of important issues and concern. The writer argued that was very needed to show a short information about Bali and the plastic dumps issues there. The existence of plastic dumps has caused my responds from both domestic and international community. Many people there have just realized that they are living in danger and this issue has to be risen and problem solving is necessary. A. Bali Geographical Location Bali is one of islands in Indonesia that is very popular among foreign tourists as a favorite destination to visit. Not only among foreign tourists, Bali is also a favorite place for domestic tourists. Enchanting beaches, cool mountains and a culture that was always preserved are attractions that makes tourists always wanted to come back. Bali Island is located between Java Island and West Nusa Tenggara Island. The island has an area of 5,636km². (Geost, 2019) The island of Bali in the east is bordered by the Lombok Strait and West Nusa Tenggara Island. In the West Bali is bordered by the Bali Strait and East Java Province, in the north it borders the Bali Sea and while in the south it borders the Indonesian Ocean. Bali is known as a tropical paradise in Indonesia. Bali's climate is a tropical climate where the change of seasons was influenced by monsoons that change every 6 months. Just like the season that occured in Indonesia in general, the Province of Bali experienced a rainy season in October-April and the dry season started from April to October. -
Report on Biodiversity and Tropical Forests in Indonesia
Report on Biodiversity and Tropical Forests in Indonesia Submitted in accordance with Foreign Assistance Act Sections 118/119 February 20, 2004 Prepared for USAID/Indonesia Jl. Medan Merdeka Selatan No. 3-5 Jakarta 10110 Indonesia Prepared by Steve Rhee, M.E.Sc. Darrell Kitchener, Ph.D. Tim Brown, Ph.D. Reed Merrill, M.Sc. Russ Dilts, Ph.D. Stacey Tighe, Ph.D. Table of Contents Table of Contents............................................................................................................................. i List of Tables .................................................................................................................................. v List of Figures............................................................................................................................... vii Acronyms....................................................................................................................................... ix Executive Summary.................................................................................................................... xvii 1. Introduction............................................................................................................................1- 1 2. Legislative and Institutional Structure Affecting Biological Resources...............................2 - 1 2.1 Government of Indonesia................................................................................................2 - 2 2.1.1 Legislative Basis for Protection and Management of Biodiversity and -
Laporan Statistik Tahun 2015 Sumber Dana : DIPA BA
KEMENTERIAN LINGKUNGAN HIDUP DAN KEHUTANAN DIREKTORAT JENDERAL KONSERVASI SUMBER DAYA ALAM DAN EKOSISTEM i BALAI TAMAN NASIONAL GUNUNG HALIMUN SALAK Jl. Raya Cipanas Kec. Kabandungan Sukabumi 43368 Jawa Barat Telp/Fax. (0266) 621256/ 621257 email: [email protected]//www.tnhalimunsalak.dephut.go.id SSTTAATTIISSTTIIKK BBAALLAAII TTAAMMAANN NNAASSIIOONNAALL GGUUNNUUNNGG HHAALLIIMMUUNN SSAALLAAKK TTAAHHUUNN 22001155 Kabandungan, Januari 2016 ii LEMBAR PENGESAHAN Nama Kegiatan : Penyusunan Laporan Statistik Tahun 2015 Sumber Dana : DIPA BA. 29 Tahun 2016 Waktu Pelaksanaan : Januari 2016 Untuk selanjutnya dokumen ini berlaku sebagai bukti otentik pelaksanaan kegiatan. Kabandungan, Januari 2016 Dinilai Oleh: Disusun Oleh: Kepala Sub Bagian tata Usaha, Pelaksana Kegiatan, Ir. Agus Bambang Haryono Wardi Septiana, S.Hut. NIP. 19610816 199303 1 001 NIP. 19790929 199903 1 002 Disahkan Oleh: Kepala Balai, Ir. Tri Siswo Rahardjo, M.Si. NIP. 19600512 198603 1 009 iii KATA PENGANTAR Pada zaman Romawi, kata “statistik” diartikan sebagai informasi-informasi yang dibutuhkan oleh negara dan berguna bagi negara. Lambat laun, kemudian “statistik” diartikan sebagai sebuah data kuantitatif baik yang sudah tersusun dalam bentuk tabel atau belum tersusun. Kemudian “statistik” dikenal sebagai kumpulan data yang berisikan angka-angka. Buku Statistik Balai Taman Nasional Gunung Halimun Salak (BTNGHS) ini merupakan penerbitan lanjutan dari buku statistik BTNGHS tahun-tahun sebelumnya dan dimaksudkan sebagai upaya memenuhi kebutuhan data dan informasi pada tahun -
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. -
Structural and Stratigraphic Evolution of the Savu Basin, Indonesia
Structural and stratigraphic evolution of the Savu Basin, Indonesia JAMES W. D. RIGG* & ROBERT HALL SE Asia Research Group, Department of Earth Sciences, Royal Holloway University of London, Egham, Surrey TW20 0EX, UK *Corresponding author (e-mail: [email protected]) Abstract: The Savu Basin is located in the Sunda–Banda fore-arc at the position of change from oceanic subduction to continent–arc collision. It narrows eastward and is bounded to the west by the island of Sumba that obliquely crosses the fore-arc. New seismic data and published geological observations are used to interpret Australia–Sundaland convergence history. We suggest the basin is underlain by continental crust and was close to sea level in the Early Miocene. Normal faulting in the Middle Miocene and rapid subsidence to several kilometres was driven by subduction rollback. Arc-derived volcaniclastic turbidites were transported ESE, parallel to the Sumba Ridge, and then NE. The ridge was elevated as the Australian continental margin arrived at the Banda Trench, causing debris flows and turbidites to flow northwards into the basin which is little deformed except for tilting and slumping. South of the ridge fore-arc sediments and Australian sedimentary cover were incorporated in a large accretionary complex formed as continental crust was thrust beneath the fore-arc. This is bounded to the north by the Savu and Roti Thrusts and to the south by a trough connecting the Java Trench and Timor Trough which formed by south-directed thrust- ing and loading. The Savu Basin is situated in the fore-arc of the Roti and the Savu Basin connects the Timor Trough Sunda–Banda Arc (Fig. -
Observed Estimates of Convergence in the Savu Sea, Indonesia James T
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, NO. C1, 3001, doi:10.1029/2002JC001507, 2003 Observed estimates of convergence in the Savu Sea, Indonesia James T. Potemra,1 Janet Sprintall,2 Susan L. Hautala,3 and Wahyu Pandoe4,5 Received 11 June 2002; revised 25 September 2002; accepted 10 October 2002; published 2 January 2003. [1] The Indonesian seas are known to be a region where various Pacific and Indian Ocean water masses converge and are transformed into uniquely characterized Indonesian Sea Water (ISW). The volume of Pacific surface waters that are stored in the Indonesian seas and the timescales for this volume to change are important factors in the formulation of ISW that ultimately enters the Indian Ocean as the Indonesian throughflow (ITF). In this study, data from a recent deployment of pressure gauges surrounding the Savu Sea are used to estimate volume, heat, and freshwater convergence within approximately the upper 100 m. A pair of gauges on the northeastern side (North Ombai and South Ombai) is used to estimate inflow from the Banda Sea through the Ombai Strait, and two pairs (Sumbawa/North Sumba and South Sumba/Roti) are used to estimate outflow to the Indian Ocean via the Sumba and Savu/Dao Straits. The data are used in conjunction with numerical model results to show that at times, for example, November and December of 1996, there can be up to a 10 Sv imbalance between the inflow and the outflow transport. Most of the variability in estimated convergence occurs intraseasonally and seems to be controlled by the flow through the Sumba Strait on the eastern side of the sea.