Arafura and Timor Seas Ecosystem Action (ATSEA)
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This Keyword List Contains Indian Ocean Place Names of Coral Reefs, Islands, Bays and Other Geographic Features in a Hierarchical Structure
CoRIS Place Keyword Thesaurus by Ocean - 8/9/2016 Indian Ocean This keyword list contains Indian Ocean place names of coral reefs, islands, bays and other geographic features in a hierarchical structure. For example, the first name on the list - Bird Islet - is part of the Addu Atoll, which is in the Indian Ocean. The leading label - OCEAN BASIN - indicates this list is organized according to ocean, sea, and geographic names rather than country place names. The list is sorted alphabetically. The same names are available from “Place Keywords by Country/Territory - Indian Ocean” but sorted by country and territory name. Each place name is followed by a unique identifier enclosed in parentheses. The identifier is made up of the latitude and longitude in whole degrees of the place location, followed by a four digit number. The number is used to uniquely identify multiple places that are located at the same latitude and longitude. For example, the first place name “Bird Islet” has a unique identifier of “00S073E0013”. From that we see that Bird Islet is located at 00 degrees south (S) and 073 degrees east (E). It is place number 0013 at that latitude and longitude. (Note: some long lines wrapped, placing the unique identifier on the following line.) This is a reformatted version of a list that was obtained from ReefBase. OCEAN BASIN > Indian Ocean OCEAN BASIN > Indian Ocean > Addu Atoll > Bird Islet (00S073E0013) OCEAN BASIN > Indian Ocean > Addu Atoll > Bushy Islet (00S073E0014) OCEAN BASIN > Indian Ocean > Addu Atoll > Fedu Island (00S073E0008) -
Oceania & Antarctica, Locate and Describe
Oceania & Antarctica, locate and describe » Activity 1. In pairs, match geographical features names in the word bank with the correct description. ___ Antarctic Peninsula ___ Ayers Rock/Uluru ___ Darling River ___ Great Barrier Reef ___ Great Dividing Range ___ Melanesia ___ Micronesia ___ New Zealand ___ Polynesia ___ Tasmania 'Meeting points': Torres Strait Note: In bold, description verbs for your cards. southern Pacific Ocean. Historically, the islands have been known as South Sea Islands even | 1 | • It is a group of islands situated some 1,500 though the Hawaiian Islands are located in the North kilometres east of Australia. In fact, it is an island Pacific. country in the southwestern Pacific Ocean and it comprises two main landmasses and around 600 | 6 | • It is an island located 240 km to the south of smaller islands. the Australian mainland, separated by the Bass Strait. The island covers 64,519 km². | 2 | • It is a large sandstone rock formation in central Australia. This rock is sacred to the Aboriginal | 7 | • It is Australia's most substantial mountain people of the area. It lies 335 km south west of the range. It stretches more than 3,500 kmfrom the nearest large town, Alice Springs. The area around northeastern tip of Queensland, running the entire the formation is home to ancient paintings. length of the eastern coastline. | 3 | • It is a subregion of Oceania extending from | 8 | • It is the third longest river in Australia, New Guinea island in the southwestern Pacific measuring 1,472 km from its source in northern Ocean to the Torres Strait, and eastward to Fiji. -
Pelagic Regionalisation
Cover image by Vincent Lyne CSIRO Marine Research Cover design by Louise Bell CSIRO Marine Research I Table of Contents Summary------------------------------------------------------------------------------------------------------ 1 1 Introduction--------------------------------------------------------------------------------------------- 3 1.1 Project background----------------------------------------------------------------------------- 3 1.2 Bioregionalisation background --------------------------------------------------------------- 5 2 Project Scope and Objectives -----------------------------------------------------------------------12 3 Pelagic Regionalisation Framework----------------------------------------------------------------13 3.1 Introduction ------------------------------------------------------------------------------------13 3.2 A Pelagic Classification ----------------------------------------------------------------------14 3.3 Levels in the pelagic classification framework--------------------------------------------17 3.3.1 Oceans ----------------------------------------------------------------------------------17 3.3.2 Level 1 Oceanic Zones and Water Masses-----------------------------------------17 3.3.3 Seas: Circulation Regimes -----------------------------------------------------------19 3.3.4 Fields of Features ---------------------------------------------------------------------19 3.3.5 Features --------------------------------------------------------------------------------20 3.3.6 Feature Structure----------------------------------------------------------------------20 -
Northern Large Marine Domain
Collation and Analysis of Oceanographic Datasets for National Marine Bioregionalisation: The Northern Large Marine Domain. A report to the Australian Government, National Oceans Office. May 2005 CSIRO Marine Research Peter Rothlisberg Scott Condie Donna Hayes Brian Griffiths Steve Edgar Jeff Dunn Cover Image designed by Vincent Lyne CSIRO Marine Researchi Cover Design Lea Crosswell and Louise Bell CSIRO Marine Research Collation and Analysis of Oceanographic Datasets – The Northern Large Marine Domain Contents Contents...........................................................................................................................................i List of Figures.................................................................................................................................ii 1. Summary................................................................................................................................1 2. Project Objectives..................................................................................................................2 3. Background............................................................................................................................2 4. Data Storage and Metadata....................................................................................................2 5 Setting for the Northern Large Marine Domain ....................................................................3 5.1 Geomorphology..............................................................................................................4 -
Chapter 10 Adjacent Seas of the Pacific Ocean Although The
Chapter 10 Adjacent seas of the Pacific Ocean Although the adjacent seas of the Pacific Ocean do not impact much on the hydrography of the oceanic basins, they cover a substantial part of its area and deserve separate discussion. All are located along the western rim of the Pacific Ocean. From the point of view of the global oceanic circulation, the most important adjacent sea is the region on either side of the equator between the islands of the Indonesian archipelago. This region is the only mediterranean sea of the Pacific Ocean and is called the Australasian Mediterranean Sea. Its influence on the hydrography of the world ocean is far greater in the Indian than in the Pacific Ocean, and a detailed discussion of this important sea is therefore postponed to Chapter 13. The remaining adjacent seas can be grouped into deep basins with and without large shelf areas, and shallow seas that form part of the continental shelf. The Japan, Coral and Tasman Seas are deep basins without large shelf areas. The circulation and hydrography of the Coral and Tasman Seas are closely related to the situation in the western South Pacific Ocean and were already covered in the last two chapters; so only the Japan Sea will be discussed here. The Bering Sea, the Sea of Okhotsk, and the South China Sea are also deep basins but include large shelf areas as well. The East China Sea and Yellow Sea are shallow, forming part of the continental shelf of Asia. Other continental shelf seas belonging to the Pacific Ocean are the Gulf of Thailand and the Java Sea in South-East Asia and the Timor and Arafura Seas with the Gulf of Carpentaria on the Australian shelf. -
The Northern Planning Area (PDF – 3.79
Atlas - Northern Chapter 3 The Northern Planning Area Planning is now underway in the Northern Planning Area (figure 2). The Northern Planning Area covers about 800 000 km2 of water off the Northern Territory and Queensland coasts, and includes the Torres Strait, the Gulf of Carpentaria Fisheries Uses and Social Indicators in Australia’s Marine Jurisdiction and eastern Arafura Sea (to a line 133°23’ east, which coincides with the Goulburn Islands). Maps in this Atlas are of the Northern Planning Area. The Northern Planning Area covers a significant proportion of the Northern Marine Region. The Northern Planning Area is a region of great diversity in its land and sea scapes, its biodiversity and its people. It is an area of rich Indigenous cultural diversity but with a sparse population, located chiefly in isolated communities. Its main industries are fishing and mining, but compared with much of Australia’s marine domain, it is economically largely undeveloped. Marine planning in the Torres Strait is being considered as part of a separate process and was not covered by the arrangements agreed between the Queensland and Australian Governments for scoping the northern marine planning process. This is in recognition of the distinct ecological, cultural and institutional arrangements that characterise the Torres Strait. Figure 2: Indicative map of the Northern Planning Area 6 > Chapter 3 7 > Chapter 3 Atlas - Northern Map 1A - The Northern Planning Area Satellite Overview MODIS satellite imagery mosaic. NASA Earth Observatory. 135°E 140°E 145°E Indonesia This map uses a mosaic of data from the MODIS Papua New Guinea (Moderate Resolution Imaging Spectroradiometer) sensor aboard the Earth Observer System satellites operated by NASA. -
Pilot Investigation of the Origins and Pathways of Marine Debris Found in the Northern Australian Marine Environment
SUMMARY Pilot investigation of the origins and pathways of marine debris found in the northern Australian marine environment Introduction Every year hundreds of lost or abandoned fishing nets are found along parts of the northern Australian coastline, especially areas of the Gulf of Carpentaria. To find out where these derelict nets come from, and the paths they may drift to reach the coast, a pilot project was commissioned. The project involved the use of a computer model and floating satellite transmitters to predict the likely pathways of these derelict nets in waters north and east of Australia. The pilot project found that derelict nets entering the Gulf of Carpentaria could originate in the South Pacific and Coral Sea (off Australia’s east coast), before being blown through the Torres Strait during the dry season by the south-east trade winds. This document provides a non-technical summary of the full technical report of the pilot project undertaken by Dr David Griffin (CSIRO, Centre for Australian Weather and Climate Research), entitled ‘Pilot investigation of the origins and pathways of marine debris found in the northern Australian marine environment’ http://www.environment.gov.au/coasts/publications/index.html). Project background Marine debris is a growing global problem that many nations are trying to address. Fishing nets that have been lost accidentally or deliberately abandoned at sea are a particularly concerning component of this marine debris, because of the navigational hazards they pose and the number of marine creatures that they harm and kill as they drift through the oceans with the currents and tides. -
2020 SOUTHEAST ASIA REGIONAL ENVIRONMENTAL SECURITY FORUM Pacific Environmental Security Forum Proposal for 2020
2020 SOUTHEAST ASIA REGIONAL ENVIRONMENTAL SECURITY FORUM Pacific Environmental Security Forum Proposal for 2020 CDR LAZARO ERNESTO VALDEZ JR PCG J.D LLM Chief of Staff, National Coast Watch Center Office of the President, Republic of the Philippines 17 Seas Andaman Sea Arafura Sea TOTAL SEA Balabac Strait SURFACE AREA: Banda Sea Celebes Sea Flores Sea Gulf of Tonkin COMBINED Gulf of Thailand COASTAL LENGTH: Java Sea Malacca Strait Makassar Strait Molucca Sea Philippine Sea SUPPORTS South China Sea Sulu Sea Timor Sea Visayan Sea 17 Seas SEA Maritime Domain Andaman Sea is recognized as: the FAUNISTIC CENTRE Arafura Sea of the entire Indo-Pacific Balabac Strait Banda Sea a GLOBAL MARINE Celebes Sea BIODIVERSITY HOTSPOT Flores Sea Gulf of Tonkin GLOBAL HOTSPOT Gulf of Thailand Java Sea for coral reefs Malacca Strait Makassar Strait Molucca Sea 80% of the world’s 50% of seagrass Philippine Sea hard corals species South China Sea Sulu Sea Timor Sea 60% of mangrove species Visayan Sea 17 Seas very rich and important Andaman Sea INCOME SOURCE and RESOURCE FOR SEAFOOD Arafura Sea e.g. South China Sea Balabac Strait Banda Sea Celebes Sea over 3 million people <> 300 million people Flores Sea per day rely on fishing for their main dependent on the SCS for nutrition income sources and socioeconomic well-being Gulf of Tonkin Gulf of Thailand Java Sea Malacca Strait Makassar Strait Molucca Sea Philippine Sea South China Sea Sulu Sea Timor Sea Visayan Sea mid-1960S RAPID ECONOMIC FAST-EXPANDING GROWTH POPULATION Major CAUSES of Marine Environmental Degradation HUMAN ACTIVITIES/ NATURAL PHENOMENON ANTHROPOGENIC 1 PRESSURES 2 CLIMATE 3 CHANGE “MARINE ENVIRONMENTAL ACTIVISM IN SOUTHEAST ASIA” Environmental Activism Marine Environmental Concerns in SEA Marine Environmental Activism in SEA Future of Marine Environmental Activism in SEA THANK YOU AND MABUHAY!!!. -
Hydro News Asia
56 HYDRONEWS HEART OF THE CORAL TRIANGLE The Southeastern Pacific (known as Melanesia) is a subregion of Oceania extending from New Guinea in the western side of the eastern Pacific to the Arafura Sea. Melanesia includes the four independent countries of Vanuatu, Solomon Islands, Fiji, and Papua New Guinea, as well as French New Caledonia and oth- ers. The more than 2,000 Melanesian islands have rich natural SOUTHEASTERN PACIFIC resources and live mostly off subsistence farming and fishing, tourism, and exports of palm oil, coffee, and sugar. HYDROPOWER Most of the islands depend on fossil fuels for electricity. While countries like New Caledonia or Fiji have an almost 100% elec- trification rate, Papua New Guinea and the Solomon Islands are striving to improve electricity access, with only about 54% and 62%, respectively. Population: 10,719 million Papua New Guinea formed the Papua New Guinea Electrifica- Installed hydro capacity: 425 MW tion Partnership to increase electricity access up to 70% by Hydropower under construction: 67 MW 2030. The initiative will support hydropower investments to tap a Technically feasible annual hydropower potential of about 45,000 MW. potential per year: 47,712 GWh Fiji has an installed capacity of 187 MW from three hydropower plants. The vast rivers of the mountainous country are ideal for ANDRITZ Hydro: development of small hydropower. Total installed / rehabilitated GENERAL FACTS GENERAL capacity: 215 MW ANDRITZ HYDRO IN SOUTHEASTERN PACIFIC Total installed / rehabilitated units: 28 ANDRITZ has been active in the region for many years and has A installed and/or rehabilitated numerous units in Papua New Guinea. -
A Review of the Indonesian Shrimp Fishery and Its Present Developments
MFR PAPER 103 0 An important shrimp fishery has blossomed in Indonesia since 1965. A Review of the Indonesian Shrimp Fishery and Its Present Developments M.UNAR INTRODUCTION modern o nes were operating in th ese waters. In the beginning of the devel opment of this fishery. s hrimp \0\ as Although there has been a shrimp the main objective. H owever. owing fis hery for a long time in Indonesia. to the great demand for fish in the . it attracted specia l attenti o n only after surrounding regions. such as Java 1960 a nd grew rapidly some ti me after which traditionall y has become a ma r 1965 when modern shrimp fishing Location of IndoneSia In wt'I ket for salted fish processed from the technology was introduced in I ndone catches of tidal traps in this region. sia n waters. Some of the meth ods of J a)..arta. F-rom there thc\ \\cre c por the new shrimp fishery has fin a ll y de catching shrimp which have been ap cd along ,\ Ith catche\ Irl)1ll other .1rt:a veloped into a conve nti onal tra "",1 fi sh pli ed locall y for many years include The great dcmand lor tJr Illp III ery in which shrimp constitute th e the use of bottom gi II nets. beach o,er~ca~ mar)..ch has dttrdctcd th" most valuable component of the catch. sei nes. the "chant rang" Danish sei ne. attention of 1ll1l onl\ dl)IllC,tIL c, plt,d. In the meantime th ere were increas push nets. -
The Languages of Melanesia: Quantifying the Level of Coverage
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by ScholarSpace at University of Hawai'i at Manoa Language Documentation & Conservation Special Publication No. 5 (December 2012) Melanesian Languages on the Edge of Asia: Challenges for the 21st Century, ed. by Nicholas Evans and Marian Klamer, pp. 13–33 http://nflrc.hawaii.edu/ldc/sp05/ 2 http://hdl.handle.net/10125/4559 The languages of Melanesia: Quantifying the level of coverage Harald Hammarström Max Plank Institute for Evolutionary Anthopology Sebastian Nordhoff Max Plank Institute for Evolutionary Anthopology The present paper assesses the state of grammatical description of the languages of the Melanesian region based on database of semi- automatically annotated aggregated bibliographical references. 150 years of language description in Melanesia has produced at least some grammatical information for almost half of the languages of Melanesia, almost evenly spread among coastal/non-coastal, Austronesian/non- Austronesian and isolates/large families. Nevertheless, only 15.4% of these languages have a grammar and another 18.7% have a grammar sketch. Compared to Eurasia, Africa and the Americas, the Papua- Austronesian region is the region with the largest number of poorly documented languages and the largest proportion of poorly documented languages. We conclude with some dicussion and remarks on the documentational challenge and its future prospects. 1. INTRODUCTION. We will take Melanesia to be the sub-region of Oceania extending from the Arafura Sea and Western Pacific in the west to Fiji in the east – see the map in figure 1.1 This region is home to no fewer than 1347 (1315 living + 32 recently extinct) attested indigenous languages as per the language/dialect divisions of Lewis (2009), with small adjustments and adding attested extinct languages given in table 1. -
Physical Oceanography of the Southeast Asian Waters
UC San Diego Naga Report Title Physical Oceanography of the Southeast Asian waters Permalink https://escholarship.org/uc/item/49n9x3t4 Author Wyrtki, Klaus Publication Date 1961 eScholarship.org Powered by the California Digital Library University of California NAGA REPORT Volume 2 Scientific Results of Marine Investigations of the South China Sea and the Gulf of Thailand 1959-1961 Sponsored by South Viet Nam, Thailand and the United States of America Physical Oceanography of the Southeast Asian Waters by KLAUS WYRTKI The University of California Scripps Institution of Oceanography La Jolla, California 1961 PREFACE In 1954, when I left Germany for a three year stay in Indonesia, I suddenly found myself in an area of seas and islands of particular interest to the oceanographer. Indonesia lies in the region which forms the connection between the Pacific and Indian Oceans, and in which the monsoons cause strong seasonal variations of climate and ocean circulation. The scientific publications dealing with this region show not so much a lack of observations as a lack of an adequate attempt to synthesize these results to give a comprehensive description of the region. Even Sverdrup et al. in “The Oceans” and Dietrich in “Allgemeine Meereskunde” treat this region superficially except in their discussion of the deep sea basins, whose peculiarities are striking. Therefore I soon decided to devote most of my time during my three years’ stay in Indonesia to the preparation of a general description of the oceanography of these waters. It quickly became apparent, that such an analysis could not be limited to Indonesian waters, but would have to cover the whole of the Southeast Asian Waters.