CORAL REEF DEGRADATION in the INDIAN OCEAN Status Reports and Project Presentations 1999
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RP: Sri Lanka: Hikkaduwa-Baddegama Section Of
Resettlement Plan May 2011 Document Stage: Draft SRI: Additional Financing for National Highway Sector Project Hikkaduwa–Baddegama Section of Hikkaduwa–Baddegama–Nilhena Road (B153) Prepared by Road Development Authority for the Asian Development Bank. CURRENCY EQUIVALENTS (as of 11 May 2011) Currency unit – Sri Lanka rupee (Rs) Rs1.00 = $0.009113278 $1.00 = Rs109.730000 ABBREVIATIONS ADB – Asian Development Bank CEA – Central Environmental Authority CSC – Chief Engineer’s Office CSC – Construction Supervision Consultant CV – Chief Valuer DSD – Divisional Secretariat Division DS – Divisional Secretary ESD – Environment and Social Division GN – Grama Niladhari GND – Grama Niladhari Division GOSL – Government of Sri Lanka GRC – Grievance Redress Committee IOL – inventory of losses LAA – Land Acquisition Act LARC – Land Acquisition and Resettlement Committee LARD – Land Acquisition and Resettlement Division LAO – Land Acquisition Officer LARS – land acquisition and resettlement survey MOLLD – Ministry of Land and Land Development NEA – National Environmental Act NGO – nongovernmental organization NIRP – National Involuntary Resettlement Policy PD – project director PMU – project management unit RP – resettlement plan RDA – Road Development Authority ROW – right-of-way SD – Survey Department SES – socioeconomic survey SEW – Southern Expressway STDP – Southern Transport Development Project TOR – terms of reference WEIGHTS AND MEASURES Ha hectare km – kilometer sq. ft. – square feet sq. m – square meter NOTE In this report, "$" refers to US dollars. This resettlement plan is a document of the borrower. The views expressed herein do not necessarily represent those of ADB's Board of Directors, Management, or staff, and may be preliminary in nature. In preparing any country program or strategy, financing any project, or by making any designation of or reference to a particular territory or geographic area in this document, the Asian Development Bank does not intend to make any judgments as to the legal or other status of any territory or area. -
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VULNERABILITY LEVEL OF TRANSITIONAL SHELTER SITES GALLE DISTRICT TSST 2nd round - January 2007 HABARADUWA DS DIVISION Area Detail Migoda ! AngulugahaAkmeemana !! Annasiwathugoda Bogahamulugoda Legend Happawana Relative Vulnerability Hab_8 *# *# Severe *# High Unawatuna West Handogoda *# Moderate Bonavistawa Meepe Harumalgoda West Unawatuna East *# Low Unawatuna Dodampe ! Pitiduwa ! 0* Decommissioned Hab_7 Harumalgoda Central ! *# Maharamba Towns Halloluwagoda Godawatta Yaddehimulla Main Road Attaragoda Pelessa Unawatuna Central Minor Road Lanumodara Pitidoowa Track Road Harumalgoda East Dalawella GN Boundary Thalpe South Wellethota !Talpe DS Boundary Heenatigala South Thalpe East Kahawennagama Katukurunda Alawathuthisgoda Liyanagoda Implemented by Uragasgoda Koggala West Habaraduwa Koggala East Morampitigoda ! Kathluwa West Koggala Kathluwa Central Korahedigoda Meegahagoda Coordinated by Hab_6Koggala Powered by ! Hab_3 Danduhela *# Hab_5 Atadahewathugoda *# Hab_1 0*Hab_2 *# Kahawathugoda Hab_4 0* Kalapuwa *# Kathluwa East Meliyagoda Ahangamgoda Welhengoda Supported By Karandugoda Kalahegoda Digaredda Piyadigama West Indian Ocean Wadugegoda © 2006 UNOPS-TSST Ahangama Dommannegoda ! Transitional Shelter Site Tracking Project, UNOPS, 17, Park Avenue, Colombo 05. Tel. +94 11 2582798 Fax +94 11 2580962 Piyadigama East Email: [email protected] Website: http://www.unops.org.lk/tsst Site Code Site Name Total Vul. Hab-1 Eluketiya I - Sewalanka Camp Decom Hab-2 Eluketiya 11 - Sewalanka Camp Decom Note: The boundaries, names and the designations used on this map do not Hab-3 Arund TSS Camp - SK Land 2 imply official endorsement or acceptance Hab-4 IAK Village 3 by the United Nations. Hab-5 Sinha Deewara Gama 2 Hab-6 Arunagamdora / Koggala Depot 1 ® TSST - UNOPS Hab-7 Yaddehimulla - Ministry of Fisheries (JVP) 2 Kilometers Hab-8 Kashapana Road, Unawatuna - Ministry of Fisheries 3 Ref: M_TV_03154_02 Date: 22/02/2007 012 Decom - Decommissioned Site(s) Rev: - Updated: -. -
Emerging Stronger: Five Years After the Indian
Kampung Mulia Tibang Darussalam INDONESIA Pante Tengoh Jurong Tengoh Emperom Kramat Luar Jurong Ara Cempaka Lambhuk Lampoh Krueng Jurong Binje Lamgugop Gampong Cot Lam Kruet Lhok Nga BAND A AC EH Meunasah Beurembang Lham Lhom Kiran Krueng Leupung AC EH BESAR Sigli Meunasah Lueng Meunasah Mesjid Lhoong Jangka Buya PID IE STARIT OF MALACCA Lamgeurihe Blang Monlueng AC EH J AY A Meunasah Kulam Sampoinet-Lhok Kruet Alue Gro Blang Dalam Sampoinet- Keuda Patek Crak Mong Sayeung Setia Bakti Rigaih – Lhok Timun Jabi – Lhok Timun AC EH BARAT Arongan Arongan Lambalek Cot Kumbang Darat Samatiga Cot Kumbang Pulau Johan Pahlawan Meulaboh Peuribu Alue Raya Meurebo NAGAN RAY A Suak Kemude Gampong Tengoh Kuta Padang Kuala Ujong Beuso Cot Darat Cot Kumbang Pasung Medan Langung Kuala Tuha Meurebo Cot Mee Habitat Resource Center Sumatra Peunaga Rayeuk Cot Rambung S U M A T E R A Peunaga Cot Ujong Langkak Gunong Kleng Kuala Tadu APPENDICES Paya Peunaga Kuala Trang Padang Rubek Lueng Mane Peunaga Pasi Leung Teuku Ben Gampong Lhok. Sub-district Habitat project areas Current Habitat Resource Center Former Habitat Resource Center NIAS 0 50 kms100 42 Emerging stronger: Five years after the Indian Ocean tsunami Kampung Mulia Tibang Darussalam INDONESIA Pante Tengoh Jurong Tengoh Emperom Kramat Luar Jurong Ara Cempaka Lambhuk Lampoh Krueng Jurong Binje Lamgugop Gampong Cot Lam Kruet Lhok Nga BANDA ACEH Meunasah Beurembang Lham Lhom Kiran Krueng Leupung ACEH BESAR Sigli Meunasah Lueng Meunasah Mesjid Lhoong Jangka Buya PIDIE Lamgeurihe ACEH JAYA Blang Monlueng Meunasah -
Supplementary Material
Supplementary Material SM1. Post-Processing of Images for Automated Classification Imagery was collected without artificial light and using a fisheye lens to maximise light capture, therefore each image needed to be processed prior annotation in order to balance colour and to minimise the non-linear distortion introduced by the fisheye lens (Figure S1). Initially, colour balance and lenses distortion correction were manually applied on the raw images using Photoshop (Adobe Systems, California, USA). However, in order to optimize the manual post-processing time of thousands of images, more recent images from the Indian Ocean and Pacific Ocean were post- processed using compressed images (jpeg format) and an automatic batch processing in Photoshop and ImageMagick, the latter an open-source software for image processing (www.imagemagick.org). In view of this, the performance of the automated image annotation on images without colour balance was contrasted against images colour balanced using manual post-processing (on raw images) and the automatic batch processing (on jpeg images). For this evaluation, the error metric described in the main text (Materials and Methods) was applied to the images from following regions: the Maldives and the Great Barrier Reef (Figures S2 and S3). We found that the colour balance applied regardless the type of processing (manual vs automatic) had an important beneficial effect on the performance of the automated image annotation as errors were reduced for critical labels in both regions (e.g., Algae labels; Figures S2 and S3). Importantly, no major differences in the performance of the automated annotations were observed between manual and automated adjustments for colour balance. -
Tide Simplified by Phil Clegg Sea Kayaking Anglesey
Tide Simplified By Phil Clegg Sea Kayaking Anglesey Tide is one of those areas that the more you learn about it, the more you realise you don’t know. As sea kayakers, and not necessarily scientists, we don’t have to know every detail but a simplified understanding can help us to understand and predict what we might expect to see when we are out on the water. In this article we look at the areas of tide you need to know about without having to look it up in a book. Causes of tides To understand tide is convenient to imagine the earth with an envelope of water all around it, spinning once every 24 hours on its north-south axis with the moon on a line parallel to the equator. Moon Gravity A B Earth Ocean C The tides are primarily caused by the gravitational attraction of the moon. Simplifying a bit, at point A the gravitational pull is the strongest causing a high tide, point B experiences a medium pull towards the moon, while point C has the weakest pull causing a second high tide. Because the earth spins once every 24 hours, at any location on its surface there are two high tides and two low tides a day. There are approximately six hours between high tide and low tide. One way of predicting the approximate time of high tide is to add 50 minutes to the high tide of the previous day. The sun has a similar but weaker gravitational effect on the tides. On average this is about 40 percent of that of the moon. -
Zeszyt 10. Morza I Oceany
Uwaga: Niniejsza publikacja została opracowana według stanu na 2008 rok i nie jest aktualizowana. Zamieszczony na stronie internetowej Komisji Standaryzacji Nazw Geograficznych poza Granica- mi Rzeczypospolitej Polskiej plik PDF jest jedynie zapisem cyfrowym wydrukowanej publikacji. Wykaz zalecanych przez Komisję polskich nazw geograficznych świata (Urzędowy wykaz polskich nazw geograficznych świata), wraz z aktualizowaną na bieżąco listą zmian w tym wykazie, zamieszczo- ny jest na stronie internetowej pod adresem: http://ksng.gugik.gov.pl/wpngs.php. KOMISJA STANDARYZACJI NAZW GEOGRAFICZNYCH POZA GRANICAMI RZECZYPOSPOLITEJ POLSKIEJ przy Głównym Geodecie Kraju NAZEWNICTWO GEOGRAFICZNE ŚWIATA Zeszyt 10 Morza i oceany GŁÓWNY URZĄD GEODEZJI I KARTOGRAFII Warszawa 2008 KOMISJA STANDARYZACJI NAZW GEOGRAFICZNYCH POZA GRANICAMI RZECZYPOSPOLITEJ POLSKIEJ przy Głównym Geodecie Kraju Waldemar Rudnicki (przewodniczący), Andrzej Markowski (zastępca przewodniczącego), Maciej Zych (zastępca przewodniczącego), Katarzyna Przyszewska (sekretarz); członkowie: Stanisław Alexandrowicz, Andrzej Czerny, Janusz Danecki, Janusz Gołaski, Romuald Huszcza, Sabina Kacieszczenko, Dariusz Kalisiewicz, Artur Karp, Zbigniew Obidowski, Jerzy Ostrowski, Jarosław Pietrow, Jerzy Pietruszka, Andrzej Pisowicz, Ewa Wolnicz-Pawłowska, Bogusław R. Zagórski Opracowanie Kazimierz Furmańczyk Recenzent Maciej Zych Komitet Redakcyjny Andrzej Czerny, Joanna Januszek, Sabina Kacieszczenko, Dariusz Kalisiewicz, Jerzy Ostrowski, Waldemar Rudnicki, Maciej Zych Redaktor prowadzący Maciej -
Alejandro Anganuzzi Executive Secretary Indian Ocean Tuna Commission Mahe Seychelles 20 January 2010
18 Queen Street Tel: (+ 44) 020 7255 7755 London Fax: (+ 44) 020 7499 5388 W1J 5PN E-Mail: [email protected] United Kingdom Internet: www.mrag.co.uk Alejandro Anganuzzi Executive Secretary Indian Ocean Tuna Commission Mahe Seychelles 20 January 2010 Dear Dr Anganuzzi, Resolution 09/03. On establishing a list of vessels presumed to have carried out illegal, unregulated and unreported fishing in the IOTC area. On behalf of the British Indian Ocean Territory Administration as required under resolution 09/03 please find attached details of five vessels flagged to Sri Lanka carrying out IUU fishing activities in the IOTC Area, specifically within the BIOT Fisheries Conservation Management Zone during 2009. The Sri Lankan Authorities have been notified of this action. All vessel owners have paid their fines and the vessels have been released. We would be grateful if you could bring these details to the attention of the Compliance Committee for inclusion on the IUU list. Whilst none of the vessels had tuna onboard there were a large number of sharks and the vessels all used longline gear, associated with targeting tuna. This further highlights the continuing problem of IUU activity by vessels flagged to Sri Lanka, despite this issue having been raised at a number of levels in the past. Yours sincerely Dr C. C. Mees Head of UK Delegation to IOTC Marine Resources Assessment Group MRAG Ltd In association with Registered Company no. 291 2982 Marine Education and Conservation Trust VAT Registration No 877 7013 92 Reg. Charity No. 297 193 IOTC Reporting Form For Illegal Activity Recalling IOTC Resolution 2009/03 ³2Q Hstablishing a list of vessels presumed to have carried out illegal, unregulated and unreported fishing in the IOTC area´ attached are details of illegal activity recorded in the British Indian Ocean Territory. -
Settlement of Larvae from Four Families of Corals in Response to a Crustose Coralline Alga and Its Biochemical Morphogens Taylor N
www.nature.com/scientificreports OPEN Settlement of larvae from four families of corals in response to a crustose coralline alga and its biochemical morphogens Taylor N. Whitman1,2, Andrew P. Negri 1, David G. Bourne 1,2 & Carly J. Randall 1* Healthy benthic substrates that induce coral larvae to settle are necessary for coral recovery. Yet, the biochemical cues required to induce coral settlement have not been identifed for many taxa. Here we tested the ability of the crustose coralline alga (CCA) Porolithon onkodes to induce attachment and metamorphosis, collectively termed settlement, of larvae from 15 ecologically important coral species from the families Acroporidae, Merulinidae, Poritidae, and Diploastreidae. Live CCA fragments, ethanol extracts, and hot aqueous extracts of P. onkodes induced settlement (> 10%) for 11, 7, and 6 coral species, respectively. Live CCA fragments were the most efective inducer, achieving over 50% settlement for nine species. The strongest settlement responses were observed in Acropora spp.; the only non-acroporid species that settled over 50% were Diploastrea heliopora, Goniastrea retiformis, and Dipsastraea pallida. Larval settlement was reduced in treatments with chemical extracts compared with live CCA, although high settlement (> 50%) was reported for six acroporid species in response to ethanol extracts of CCA. All experimental treatments failed (< 10%) to induce settlement in Montipora aequituberculata, Mycedium elephantotus, and Porites cylindrica. Individual species responded heterogeneously to all treatments, suggesting that none of the cues represent a universal settlement inducer. These results challenge the commonly-held notion that CCA ubiquitously induces coral settlement, and emphasize the critical need to assess additional cues to identify natural settlement inducers for a broad range of coral taxa. -
2.02 Rajasuriya 2008
ARJAN RAJASURIYA National Aquatic Resources Research and Development Agency, Crow Island, Colombo 15, Sri Lanka [email protected]; [email protected] fringing and patch reefs (Swan, 1983; Rajasuriya et al., 1995; Rajasuriya & White, 1995). Fringing coral reef Selected coral reefs were monitored in the northern, areas occur in a narrow band along the coast except in western and southern coastal waters of Sri Lanka to the southeast and northeast of the island where sand assess their current status and to understand the movement inhibits their formation. The shallow recovery processes after the 1998 coral bleaching event continental shelf of Gulf of Mannar contains extensive and the 2004 tsunami. The highest rate of recovery coral patch reefs from the Bar Reef to Mannar Island was observed at the Bar Reef Marine Sanctuary where (Rajasuriya, 1991; Rajasuriya, et al. 1998a; Rajasuriya rapid growth of Acropora cytherea and Pocillopora & Premaratne, 2000). In addition to these coral reefs, damicornis has contributed to reef recovery. which are limited to a depth of about 10m, there are Pocillopora damicornis has shown a high level of offshore coral patches in the west and east of the recruitment and growth on most reef habitats island at varying distances (15 -20 km) from the including reefs in the south. An increase in the growth coastline at an average depth of 20m (Rajasuriya, of the calcareous alga Halimeda and high levels of 2005). Sandstone and limestone reefs occur as sedimentation has negatively affected some fringing discontinuous bands parallel to the shore from inshore reefs especially in the south. Reef surveys carried out areas to the edge of the continental shelf (Swan, 1983; for the first time in the northern coastal waters around Rajasuriya et al., 1995). -
Mangroves and Coral Reefs: David Stoddart and the Cambridge Physiographic Tradition Colin D
University of Wollongong Research Online Faculty of Science, Medicine and Health - Papers: Faculty of Science, Medicine and Health Part B 2018 Mangroves and coral reefs: David Stoddart and the Cambridge physiographic tradition Colin D. Woodroffe University of Wollongong, [email protected] Publication Details Woodroffe, C. D. (2018). Mangroves and coral reefs: David Stoddart and the Cambridge physiographic tradition. Atoll Research Bulletin, 619 121-145. Research Online is the open access institutional repository for the University of Wollongong. For further information contact the UOW Library: [email protected] Mangroves and coral reefs: David Stoddart and the Cambridge physiographic tradition Abstract Mangroves are particularly extensive on sheltered, macrotidal, muddy tropical coastlines, but also occur in association with coral reefs. Reefs attenuate wave energy, in some locations enabling the accretion of fine calcareous sediments which in turn favour establishment of seagrasses and mangroves. Knowledge of the distribution and ecology of both reefs and mangroves increased in the first half of the 20th century. J Alfred Steers participated in the Great Barrier Reef Expedition in 1928, and developed an interest in the geomorphological processes by which islands had formed in this setting. It became clear that many mangrove forests showed a zonation of species and some researchers inferred successional changes, even implying that reefs might transition through a mangrove stage, ultimately forming land. Valentine Chapman studied the ecology of mangroves, and Steers and Chapman described West Indian mangrove islands in the 1940s during the University of Cambridge expedition to Jamaica. These studies provided the background for David Stoddart's participation in the Cambridge Expedition to British Honduras and his PhD examination of three Caribbean atolls. -
WATER ENVIRONMENT A3d.1 INTRODUCTION
Offshore Energy SEA APPENDIX 3d - WATER ENVIRONMENT A3d.1 INTRODUCTION A number of aspects of the water environment are reviewed below in a UK context, and for individual Regional Seas: • The major water masses and residual circulation patterns in UK seas • Density stratification (influenced principally by temperature and salinity) and frontal zones between different water masses – these represent potentially important areas for biological productivity • Tidal flows • Overall patterns of temperature and salinity • Wave climate • Ambient noise Recent assessments of changes in hydrographic conditions are summarised, based mainly on reports by DEFRA (2004a, b) and MCCIP (2007). Overall, significant anomalies and changes have been noted in sea surface temperature (SST), thermal stratification, circulation patterns, wave climate, pH and sea level – many appear to be correlated to atmospheric climate variability as described by the North Atlantic Oscillation (NAO). Larger- scale trends and process changes have also been noted in the North Atlantic (e.g. in the strength of the Gulf Stream and Atlantic Heat Conveyor (more properly characterised as the Meridional Overturning Circulation (MOC), or the Atlantic Thermohaline circulation (THC) e.g. Trumper 2005), Northern Hemisphere (Weijerman et al. 2005) and globally (IPCC 2007a). There are varying degrees of confidence in the interpretation of observed data and prediction of future trends. Finally, the specific environmental issue of eutrophication is summarised. This is an area of concern in specific geographical areas, notably the southern North Sea and various coastal and estuarine locations. A3d.2 UK CONTEXT The history of broadscale studies of North Sea circulation and hydrographic patterns (e.g. temperature and salinity distribution) was briefly reviewed in SEA 2. -
Secret Seychelles Islands with Ponant Aboard Le Jacques Cartier
SECRET SEYCHELLES ISLANDS WITH PONANT ABOARD LE JACQUES CARTIER Embark with PONANT on an expedition cruise to discover the most beautiful islands of the Seychelles. This 13-day itinerary aboard Le Jacques-Cartier will be an opportunity to discover little-known places of breathtaking natural beauty and an original fauna and flora. Leaving from Victoria, the archipelago’s capital, fall under the spell of the idyllic landscapes, with their exceptional flora and fauna. In Praslin, don’t miss the chance to visit the Vallée de Mai Nature Reserve. There you will find sea coconuts, gigantic fruits with a very evocative shape, nicknamed the “love nut”. You will discover the island of Aride, an unspoiled delight of the Indian Ocean, home to thousands of birds including some endemic species. During your cruise, you will have many opportunities to dive or snorkel, notably in Poivre, Assomption, Astove, and at the heart of the sublime coral reef in the Alphonse lagoon. Another highlight of your trip will be the port of call at Cosmoledo. This magnificent atoll owes its nickname, the Galapagos of the Indian Ocean, to the beauty of its unique underwater world. Diving in this paradise lagoon becomes an extraordinary experience. Before you return to Mahé, Le Jacques-Cartier will chart a course for the coral island of Desroches and the sublime beaches of La Digue, some of the most renowned of the Seychelles. The encounters with the wildlife described above illustrate possible experiences ITINERARY only and cannot be guaranteed. Day 1 VICTORIA, MAHÉ Discover Mahé, the main island of the Seychelles and also the largest of the archipelago, home to the capital, Victoria.