Indonesian Avifauna: Some Physical and Biological Relationships
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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. -
Lombok Island, Sumbawa Island, and Samalas Volcano
ECOLE DOCTORALE DE GEOGRAPHIE DE PARIS (ED 4434) Laboratoire de Géographie Physique - UMR 8591 Doctoral Thesis in Geography Bachtiar Wahyu MUTAQIN IMPACTS GÉOMORPHIQUES DE L'ÉRUPTION DU SAMALAS EN 1257 LE LONG DU DÉTROIT D'ALAS, NUSA TENGGARA OUEST, INDONÉSIE Defense on: 11 December 2018 Supervised by : Prof. Franck LAVIGNE (Université Paris 1 – Panthhéon Sorbonne) Prof. HARTONO (Universitas Gadjah Mada) Rapporteurs : Prof. Hervé REGNAULD (Université de Rennes 2) Prof. SUWARDJI (Universitas Mataram) Examiners : Prof. Nathalie CARCAUD (AgroCampus Ouest) Dr. Danang Sri HADMOKO (Universitas Gadjah Mada) 1 Abstract As the most powerful event in Lombok’s recent eruptive history, volcanic materials that were expelled by the Samalas volcano in 1257 CE covered the entire of Lombok Island and are widespread in its eastern part. Almost 800 years after the eruption, the geomorphological impact of this eruption on the island of Lombok remains unknown, whereas its overall climatic and societal consequences are now better understood. A combination of stratigraphic information, present-day topography, geophysical measurement with two-dimensional resistivity profiling technique, local written sources, as well as laboratory and computational analysis, were used to obtain detailed information concerning geomorphic impacts of the 1257 CE eruption of Samalas volcano on the coastal area along the Alas Strait in West Nusa Tenggara Province, Indonesia. This study provides new information related to the geomorphic impact of a major eruption volcanic in coastal areas, in this case, on the eastern part of Lombok and the western coast of Sumbawa. In the first place, the study result shows that since the 1257 CE eruption, the landscape on the eastern part of Lombok is still evolved until the present time. -
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. -
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. -
Tropical Cyclone Cempaka 'Visiting' Indonesia Right After Facing Bali's
Tropical Cyclone Cempaka ‘Visiting’ Indonesia Right after facing Bali's Mount Agung eruption, Indonesia encounters another natural event when tropical cyclone ‘Cempaka’ hits Indonesia on 27th November 2017. Jakarta- Tropical Cyclone Warning Center (TCWC) Jakarta detected a tropical cyclone developing very close to the Southern Coast of Java. The tropical cyclone named ‘Cempaka’, has made BMKG to warn the public to prepare for extreme weather impacts for the next three days. BMKG inform the public that there are some extreme conditions causes by Cempaka such as heavy reainfall, strong winds and thunderstorms that will hit some areas of Indonesia. These heavy rains with strong winds up to 30 knots will hit Jakarta, West Java, Central Java Tengah, Yogyakarta, East Java, Kangean Island, Bali, Nusa Tenggara, and the Southern part of Java Sea. TCWC Jakarta predicts that Cempaka will remain for the next two to three days. TCWC also sending alert to public about high wave potential cause by this cyclone that up to 2.5 - 6 meters in, South Coast of East Java, the Eastern part of Java Sea, Bali Waters, Bali Strait, Alas Strait, Southern part of Lombok Strait, and Sumbawa Sea. BMKG issued warning to the public and advised people to remain calm but be aware about the following impacts that can be caused by the cyclone, such as floods, landslides, flash floods, puddles, strong winds, fallen trees, and slippery roads. Flight activities at several airports in Java may also be affected due to heavy rain and strong winds. Due to possible high sea waves, people and passing vessels are encouraged to remain on alert, especially traditional fishermen operating in the Southern Waters of Java. -
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. -
The Malay Archipelago
BOOKS & ARTS COMMENT The Malay Archipelago: the land of the orang-utan, and the bird of paradise; a IN RETROSPECT narrative of travel, with studies of man and nature ALFRED RUSSEL WALLACE The Malay Macmillan/Harper Brothers: first published 1869. lfred Russel Wallace was arguably the greatest field biologist of the nine- Archipelago teenth century. He played a leading Apart in the founding of both evolutionary theory and biogeography (see page 162). David Quammen re-enters the ‘Milky Way of He was also, at times, a fine writer. The best land masses’ evoked by Alfred Russel Wallace’s of his literary side is on show in his 1869 classic, The Malay Archipelago, a wondrous masterpiece of biogeography. book of travel and adventure that wears its deeper significance lightly. The Malay Archipelago is the vast chain of islands stretching eastward from Sumatra for more than 6,000 kilometres. Most of it now falls within the sovereignties of Malaysia and Indonesia. In Wallace’s time, it was a world apart, a great Milky Way of land masses and seas and straits, little explored by Europeans, sparsely populated by peoples of diverse cul- tures, and harbouring countless species of unknown plant and animal in dense tropical forests. Some parts, such as the Aru group “Wallace paid of islands, just off the his expenses coast of New Guinea, by selling ERNST MAYR LIB., MUS. COMPARATIVE ZOOLOGY, HARVARD UNIV. HARVARD ZOOLOGY, LIB., MUS. COMPARATIVE MAYR ERNST were almost legend- specimens. So ary for their remote- he collected ness and biological series, not just riches. Wallace’s jour- samples.” neys throughout this region, sometimes by mail packet ship, some- times in a trading vessel or a small outrigger canoe, were driven by a purpose: to collect animal specimens that might help to answer a scientific question. -
Sepia Bandensis Adam, 1939 Fig
72 FAO Species Catalogue for Fishery Purposes No. 4, Vol. 1 Sepia bandensis Adam, 1939 Fig. 122; Plate IV, 21–22 Sepia bandensis Adam, 1939b. Bulletin du Musée royal d’Histoire naturelle de Belgique, 15(18): 1 [type locality: Indonesia: Banda Sea, Banda Neira]. Frequent Synonyms: Sepia baxteri (Iredale, 1940) and Sepia bartletti (Iredale, 1954) are possible synonyms. Misidentifications: None. FAO Names: En – Stumpy cuttlefish; Fr – Seiche trapue; Sp – Sepia achaparrada. Diagnostic Features: Club with 5 suckers in transverse rows, central 3 suckers enlarged. Swimming keel extends beyond base of club. Dorsal and ventral protective membranes joined at base of club, separated from stalk by a membrane. Cuttlebone outline broad, oval; bone bluntly rounded anteriorly and posteriorly; dorsal surface evenly convex; calcified with reticulate sculpture; dorsal median and lateral ribs absent. Spine reduced to tiny, blunt tubercle. Sulcus shallow, narrow, extends along striated zone only. Anterior striae are inverted U-shape. Inner cone limbs are narrow anteriorly, broaden posteriorly, slightly convex; outer cone narrow anteriorly, broadens posteriorly. Dorsal mantle has longitudinal row of ridge-like papillae along each side, adjacent to base of each fin and scattered short ridges dorsal to cuttlebone dorsal view ventral view (corresponding to whitish bars). Head tentacular club cuttlebone and arms with short, scattered, bar-like (illustrations: K. Hollis) papillae positioned dorsally and laterally. Colour: Light brown, or Fig. 122 Sepia bandensis greenish yellow-brown when fresh, and with whitish mottle. Head with scattered white spots. Dorsal mantle has white blotches concentrated into short, longitudinal bars. It often shows a pair of brown patches on the posterior end of the mantle, often accompanied by white patches over the eye orbits. -
Ocean Drilling Program Scientific Results Volume
Weissel, J., Peirce, J., Taylor, E., Alt, J., et al., 1991 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 121 4. PLANKTONIC FORAMINIFER FAUNAL VARIATIONS IN THE NORTHEASTERN INDIAN OCEAN: A HIGH-RESOLUTION RECORD OF THE PAST 800,000 YEARS FROM SITE 7581 Min-Te Chen2 and John Farrell2 ABSTRACT We present a high-resolution (6 k.y. sample interval) record of planktonic foraminifer faunal variations for the past 800 k.y. from ODP Site 758 in the northeastern Indian Ocean. The record is examined within the context of a coarse fraction stratigraphy which is a lithologic index of CaCθ3 preservation, and an oxygen isotope stratigraphy which provides a chronostratigraphy and a record of climate change. Variations in the relative abundance of 27 planktonic foraminifer species primarily reflect fluctuations in the intensity of CaCθ3 dissolution. CaCθ3 dissolution covaries with climate fluctuations at a cyclicity of about 100 k.y. Glacial-aged sediments are generally well preserved, as indicated by faunal and lithologic indices. Interglacial-aged sediments show poorer preservation. The -100-k.y. cycles are superimposed upon the long-term Brunhes Dissolution Cycle. This cycle is characterized by an interval of poor preservation centered between 400 and 550 ka and is bounded by good preservation events at 25 and 750 ka. Ecological factors also control variations in the foraminifer fauna. Changes in ecology are inferred from downcore fluctuations in the relative abundances of foraminifer species that have a similar level of resistance to dissolution. We focus on three species (Neogloboquadrina dutertrei, Pulleniatina obliquiloculata, Globorotalia menardii) with a relatively high resistance to dissolution. -
Dutch East Indies)
.1" >. -. DS 6/5- GOiENELL' IJNIVERSIT> LIBRARIES riilACA, N. Y. 1483 M. Echols cm Soutbeast. Asia M. OLIN LIBRARY CORNELL UNIVERSITY LlflfiAfiY 3 1924 062 748 995 Cornell University Library The original of tiiis book is in tine Cornell University Library. There are no known copyright restrictions in the United States on the use of the text. http://www.archive.org/details/cu31924062748995 I.D. 1209 A MANUAL OF NETHERLANDS INDIA (DUTCH EAST INDIES) Compiled by the Geographical Section of the Naval Intelligence Division, Naval Staff, Admiralty LONDON : - PUBLISHED BY HIS MAJESTY'S STATIONERY OFFICE. To be purchased through any Bookseller or directly from H.M. STATIONERY OFFICE at the following addresses: Imperial House, Kinqswat, London, W.C. 2, and ,28 Abingdon Street, London, S.W.I; 37 Peter Street, Manchester; 1 St. Andrew's Crescent, Cardiff; 23 Forth Street, Edinburgh; or from E. PONSONBY, Ltd., 116 Grafton Street, Dublin. Price 10s. net Printed under the authority of His Majesty's Stationery Office By Frederick Hall at the University Press, Oxford. ill ^ — CONTENTS CHAP. PAGE I. Introduction and General Survey . 9 The Malay Archipelago and the Dutch possessions—Area Physical geography of the archipelago—Frontiers and adjacent territories—Lines of international communication—Dutch progress in Netherlands India (Relative importance of Java Summary of economic development—Administrative and economic problems—Comments on Dutch administration). II. Physical Geography and Geology . .21 Jaya—Islands adjacent to Java—Sumatra^^Islands adja- — cent to Sumatra—Borneo ^Islands —adjacent to Borneo CeLel3^—Islands adjacent to Celebes ^The Mpluoeas—^Dutoh_ QQ New Guinea—^Islands adjacent to New Guinea—Leaser Sunda Islands. -
Edition 7 No's
11 April 2008 Edition 7 Australian Notices to Mariners are the authority for correcting Australian Charts and Publications AUSTRALIAN NOTICES TO MARINERS © Commonwealth of Australia 2008 - Copyright restrictions apply to Notices to Mariners Notices 317 – 363 List of Temporary and Preliminary Notices in force Cumulative List – April 2008 Published fortnightly by the Australian Hydrographic Service Captain R. NAIRN RAN Hydrographer of Australia SECTIONS. I. Australian Notices to Mariners, including blocks and notes. II. Amendments to Admiralty List of Lights and Fog Signals, Vol K III. Navigational Warnings. IV. Hydrographic Reports. V. Amendments to Admiralty List of Radio Signals (NP 281(2), 282, 283(2), 285, 286(4)) VI. Amendments to Admiralty Sailing Directions (NP 9, 13, 14, 15, 33, 34, 35, 36, 39, 44, 51, 60, 61, 62, 100, 136) British Admiralty Notices to Mariners New Zealand Notices to Mariners The substance of these notices should be inserted on the charts affected. Bearings are referred to the true compass and are reckoned clockwise from North; those relating to lights are given as seen by an observer from seaward. Positions quoted in permanent notices relate to the horizontal datum for the chart(s). When preliminary or temporary notices affect multiple charts, positions will be provided in relation to only one horizontal datum and that datum will be specified. When the multiple charts do not have a common horizontal datum, mariners will be required to adjust the position(s) for those charts not on the specified datum. The range quoted for a light is its nominal range. Depths are with reference to the chart datum of each chart.