Majuro Benthic Mapping
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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) -
Enhancing Safety, Security and Sustainability of Apia Port: Due
Due Diligence Report Project Number: 47358-002 May 2019 SAM: Enhancing Safety, Security and Sustainability of Apia Port Project (Grant xxxx) Prepared by the Samoa Ports Authority for the Asian Development Bank. This due diligence report 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. Your attention is directed to the “terms of use” section of this website. In preparing any country program or strategy, financing any project, or by making any designation of or reference to a territory or geographic area in this document, the Asian Development Bank does not intend to make any judgements as to the legal or other status of any territory or area. Enhancing Safety, Security and Sustainability of Apia Port – Social and Poverty Assessment Report CURRENCY EQUIVALENTS (as of 4 April 2016) Tala – Samoan Tala (SAT) = $1.00 = ABBREVIATIONS ADB - Asian Development Bank AUA - Apia Urban Area DDR - Due Diligence Report EA - Executing Agency EMP - Environmental Management Plan EPA - Environmental Protection Agency GOS - Government of the Samoa GRM - Grievance Redress Mechanism HIES - Household Income and Expenditures Survey IA - Implementing Agency IP - Indigenous People IR - Involuntary Resettlement MNRE - Ministry of Natural Resources and Environment MOF - Ministry of Finance MOR - Ministry of Revenue PIC - Pacific Island Countries PUMA - Planning and Urban Management Authority RP - Resettlement Plan SPA - Samoa Ports Authority -
INTERTIDAL ZONATION Introduction to Oceanography Spring 2017 The
INTERTIDAL ZONATION Introduction to Oceanography Spring 2017 The Intertidal Zone is the narrow belt along the shoreline lying between the lowest and highest tide marks. The intertidal or littoral zone is subdivided broadly into four vertical zones based on the amount of time the zone is submerged. From highest to lowest, they are Supratidal or Spray Zone Upper Intertidal submergence time Middle Intertidal Littoral Zone influenced by tides Lower Intertidal Subtidal Sublittoral Zone permanently submerged The intertidal zone may also be subdivided on the basis of the vertical distribution of the species that dominate a particular zone. However, zone divisions should, in most cases, be regarded as approximate! No single system of subdivision gives perfectly consistent results everywhere. Please refer to the intertidal zonation scheme given in the attached table (last page). Zonal Distribution of organisms is controlled by PHYSICAL factors (which set the UPPER limit of each zone): 1) tidal range 2) wave exposure or the degree of sheltering from surf 3) type of substrate, e.g., sand, cobble, rock 4) relative time exposed to air (controls overheating, desiccation, and salinity changes). BIOLOGICAL factors (which set the LOWER limit of each zone): 1) predation 2) competition for space 3) adaptation to biological or physical factors of the environment Species dominance patterns change abruptly in response to physical and/or biological factors. For example, tide pools provide permanently submerged areas in higher tidal zones; overhangs provide shaded areas of lower temperature; protected crevices provide permanently moist areas. Such subhabitats within a zone can contain quite different organisms from those typical for the zone. -
The Political, Security, and Climate Landscape in Oceania
The Political, Security, and Climate Landscape in Oceania Prepared for the US Department of Defense’s Center for Excellence in Disaster Management and Humanitarian Assistance May 2020 Written by: Jonah Bhide Grace Frazor Charlotte Gorman Claire Huitt Christopher Zimmer Under the supervision of Dr. Joshua Busby 2 Table of Contents Executive Summary 3 United States 8 Oceania 22 China 30 Australia 41 New Zealand 48 France 53 Japan 61 Policy Recommendations for US Government 66 3 Executive Summary Research Question The current strategic landscape in Oceania comprises a variety of complex and cross-cutting themes. The most salient of which is climate change and its impact on multilateral political networks, the security and resilience of governments, sustainable development, and geopolitical competition. These challenges pose both opportunities and threats to each regionally-invested government, including the United States — a power present in the region since the Second World War. This report sets out to answer the following questions: what are the current state of international affairs, complexities, risks, and potential opportunities regarding climate security issues and geostrategic competition in Oceania? And, what policy recommendations and approaches should the US government explore to improve its regional standing and secure its national interests? The report serves as a primer to explain and analyze the region’s state of affairs, and to discuss possible ways forward for the US government. Given that we conducted research from August 2019 through May 2020, the global health crisis caused by the novel coronavirus added additional challenges like cancelling fieldwork travel. However, the pandemic has factored into some of the analysis in this report to offer a first look at what new opportunities and perils the United States will face in this space. -
Remote Sensing for Drought Monitoring & Impact Assessment
1 Remote Sensing for Drought Monitoring & Impact Assessment: Progress, Past 2 Challenges and Future Opportunities 3 4 Harry West, Nevil Quinn & Michael Horswell 5 Centre for Water, Communities & Resilience; Department of Geography & Environmental 6 Management; University of the West of EnglanD, Bristol 7 8 CorresponDing Author: Harry West ([email protected]) 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 1 24 Remote Sensing for Drought Monitoring & Impact Assessment: Progress, Past 25 Challenges and Future Opportunities 26 27 Abstract 28 Drought is a common hydrometeorological phenomenon anD a pervasive global hazarD. As 29 our climate changes, it is likely that Drought events will become more intense anD frequent. 30 Effective Drought monitoring is therefore critical, both to the research community in 31 Developing an unDerstanDing of Drought, anD to those responsible for Drought management 32 anD mitigation. Over the past 50 years remote sensing has shifteD the fielD away from 33 reliance on traditional site-baseD measurements anD enableD observations anD estimates of 34 key drought-relateD variables over larger spatial anD temporal scales than was previously 35 possible. This has proven especially important in Data poor regions with limiteD in-situ 36 monitoring stations. Available remotely senseD Data proDucts now represent almost all 37 aspects of Drought propagation anD have contributeD to our unDerstanDing of the 38 phenomena. In this review we chart the rise of remote sensing for Drought monitoring, 39 examining key milestones anD technologies for assessing meteorological, agricultural anD 40 hyDrological Drought events. We reflect on challenges the research community has faceD to 41 Date, such as limitations associateD with Data recorD length anD spatial, temporal anD 42 spectral resolution. -
Assessing Long-Term Changes in the Beach Width of Reef Islands Based on Temporally Fragmented Remote Sensing Data
Remote Sens. 2014, 6, 6961-6987; doi:10.3390/rs6086961 OPEN ACCESS remote sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Assessing Long-Term Changes in the Beach Width of Reef Islands Based on Temporally Fragmented Remote Sensing Data Thomas Mann 1,* and Hildegard Westphal 1,2 1 Leibniz Center for Tropical Marine Ecology, Fahrenheitstrasse 6, D-28359 Bremen, Germany; E-Mail: [email protected] 2 Department of Geosciences, University of Bremen, D-28359 Bremen, Germany * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +49-421-2380-0132; Fax: +49-421-2380-030. Received: 30 May 2014; in revised form: 7 July 2014 / Accepted: 18 July 2014 / Published: 25 July 2014 Abstract: Atoll islands are subject to a variety of processes that influence their geomorphological development. Analysis of historical shoreline changes using remotely sensed images has become an efficient approach to both quantify past changes and estimate future island response. However, the detection of long-term changes in beach width is challenging mainly for two reasons: first, data availability is limited for many remote Pacific islands. Second, beach environments are highly dynamic and strongly influenced by seasonal or episodic shoreline oscillations. Consequently, remote-sensing studies on beach morphodynamics of atoll islands deal with dynamic features covered by a low sampling frequency. Here we present a study of beach dynamics for nine islands on Takú Atoll, Papua New Guinea, over a seven-decade period. A considerable chronological gap between aerial photographs and satellite images was addressed by applying a new method that reweighted positions of the beach limit by identifying “outlier” shoreline positions. -
Life in the Intertidal Zone
Life in the Rocky Intertidal Zone Tidepools provide a home for many animals. Tidepools are created by the changing water level, or tides. The high energy waves make this a harsh habitat, but the animals living here have adapted over time. When the earth, sun and moon align during the full and new moon we have extreme high and low tides. Generally, there are two high tides and two low tides a day. An example of low and high tide is seen on the right. There are three zones within the tidepools: the high zone, the middle zone, and the low zone. Animals are distributed based on their adaptations to different living (competition and predation) and non living (wave action and water loss) factors. The tidepools at Cabrillo are protected and have been monitored by the National Park Service since 1990. You may notice bolts in Low Tide the rocky intertidal, these are used to assist scientists in gathering data to monitor changes. Tidepool Etiquette: Human impact can hurt the animals. As you explore the tidepools, you may touch the animals living here, but only as gently as you would touch your own eyeball. Some animals may die if moved even a few inches from where they are found. Federal law prohibits collection and removal of any shells, rocks and marine specimens. Also, be aware of the changing tides, slippery rocks and unstable cliffs. Have fun exploring! High Tide High Zone The high zone is covered by the highest tides. Often this area is only sprayed by the (Supralittoral or crashing waves. -
Spatial Patterns of Macrozoobenthos Assemblages in a Sentinel Coastal Lagoon: Biodiversity and Environmental Drivers
Journal of Marine Science and Engineering Article Spatial Patterns of Macrozoobenthos Assemblages in a Sentinel Coastal Lagoon: Biodiversity and Environmental Drivers Soilam Boutoumit 1,2,* , Oussama Bououarour 1 , Reda El Kamcha 1 , Pierre Pouzet 2 , Bendahhou Zourarah 3, Abdelaziz Benhoussa 1, Mohamed Maanan 2 and Hocein Bazairi 1,4 1 BioBio Research Center, BioEcoGen Laboratory, Faculty of Sciences, Mohammed V University in Rabat, 4 Avenue Ibn Battouta, Rabat 10106, Morocco; [email protected] (O.B.); [email protected] (R.E.K.); [email protected] (A.B.); [email protected] (H.B.) 2 LETG UMR CNRS 6554, University of Nantes, CEDEX 3, 44312 Nantes, France; [email protected] (P.P.); [email protected] (M.M.) 3 Marine Geosciences and Soil Sciences Laboratory, Associated Unit URAC 45, Faculty of Sciences, Chouaib Doukkali University, El Jadida 24000, Morocco; [email protected] 4 Institute of Life and Earth Sciences, Europa Point Campus, University of Gibraltar, Gibraltar GX11 1AA, Gibraltar * Correspondence: [email protected] Abstract: This study presents an assessment of the diversity and spatial distribution of benthic macrofauna communities along the Moulay Bousselham lagoon and discusses the environmental factors contributing to observed patterns. In the autumn of 2018, 68 stations were sampled with three replicates per station in subtidal and intertidal areas. Environmental conditions showed that the range of water temperature was from 25.0 ◦C to 12.3 ◦C, the salinity varied between 38.7 and 3.7, Citation: Boutoumit, S.; Bououarour, while the average of pH values fluctuated between 7.3 and 8.0. -
Intertidal Sand and Mudflats & Subtidal Mobile
INTERTIDAL SAND AND MUDFLATS & SUBTIDAL MOBILE SANDBANKS An overview of dynamic and sensitivity characteristics for conservation management of marine SACs M. Elliott. S.Nedwell, N.V.Jones, S.J.Read, N.D.Cutts & K.L.Hemingway Institute of Estuarine and Coastal Studies University of Hull August 1998 Prepared by Scottish Association for Marine Science (SAMS) for the UK Marine SACs Project, Task Manager, A.M.W. Wilson, SAMS Vol II Intertidal sand and mudflats & subtidal mobile sandbanks 1 Citation. M.Elliott, S.Nedwell, N.V.Jones, S.J.Read, N.D.Cutts, K.L.Hemingway. 1998. Intertidal Sand and Mudflats & Subtidal Mobile Sandbanks (volume II). An overview of dynamic and sensitivity characteristics for conservation management of marine SACs. Scottish Association for Marine Science (UK Marine SACs Project). 151 Pages. Vol II Intertidal sand and mudflats & subtidal mobile sandbanks 2 CONTENTS PREFACE 7 EXECUTIVE SUMMARY 9 I. INTRODUCTION 17 A. STUDY AIMS 17 B. NATURE AND IMPORTANCE OF THE BIOTOPE COMPLEXES 17 C. STATUS WITHIN OTHER BIOTOPE CLASSIFICATIONS 25 D. KEY POINTS FROM CHAPTER I. 27 II. ENVIRONMENTAL REQUIREMENTS AND PHYSICAL ATTRIBUTES 29 A. SPATIAL EXTENT 29 B. HYDROPHYSICAL REGIME 29 C. VERTICAL ELEVATION 33 D. SUBSTRATUM 36 E. KEY POINTS FROM CHAPTER II 43 III. BIOLOGY AND ECOLOGICAL FUNCTIONING 45 A. CHARACTERISTIC AND ASSOCIATED SPECIES 45 B. ECOLOGICAL FUNCTIONING AND PREDATOR-PREY RELATIONSHIPS 53 C. BIOLOGICAL AND ENVIRONMENTAL INTERACTIONS 58 D. KEY POINTS FROM CHAPTER III 65 IV. SENSITIVITY TO NATURAL EVENTS 67 A. POTENTIAL AGENTS OF CHANGE 67 B. KEY POINTS FROM CHAPTER IV 74 V. SENSITIVITY TO ANTHROPOGENIC ACTIVITIES 75 A. -
The Contribution of Wind-Generated Waves to Coastal Sea-Level Changes
1 Surveys in Geophysics Archimer November 2011, Volume 40, Issue 6, Pages 1563-1601 https://doi.org/10.1007/s10712-019-09557-5 https://archimer.ifremer.fr https://archimer.ifremer.fr/doc/00509/62046/ The Contribution of Wind-Generated Waves to Coastal Sea-Level Changes Dodet Guillaume 1, *, Melet Angélique 2, Ardhuin Fabrice 6, Bertin Xavier 3, Idier Déborah 4, Almar Rafael 5 1 UMR 6253 LOPSCNRS-Ifremer-IRD-Univiversity of Brest BrestPlouzané, France 2 Mercator OceanRamonville Saint Agne, France 3 UMR 7266 LIENSs, CNRS - La Rochelle UniversityLa Rochelle, France 4 BRGMOrléans Cédex, France 5 UMR 5566 LEGOSToulouse Cédex 9, France *Corresponding author : Guillaume Dodet, email address : [email protected] Abstract : Surface gravity waves generated by winds are ubiquitous on our oceans and play a primordial role in the dynamics of the ocean–land–atmosphere interfaces. In particular, wind-generated waves cause fluctuations of the sea level at the coast over timescales from a few seconds (individual wave runup) to a few hours (wave-induced setup). These wave-induced processes are of major importance for coastal management as they add up to tides and atmospheric surges during storm events and enhance coastal flooding and erosion. Changes in the atmospheric circulation associated with natural climate cycles or caused by increasing greenhouse gas emissions affect the wave conditions worldwide, which may drive significant changes in the wave-induced coastal hydrodynamics. Since sea-level rise represents a major challenge for sustainable coastal management, particularly in low-lying coastal areas and/or along densely urbanized coastlines, understanding the contribution of wind-generated waves to the long-term budget of coastal sea-level changes is therefore of major importance. -
Pacific Remote Islands Marine National Monument
U.S. Fish & Wildlife Service Pacific Remote Islands Marine National Monument The Pacific Remote Islands Marine National Monument falls within the Central Pacific Ocean, ranging from Wake Atoll in the northwest to Jarvis Island in the southeast. The seven atolls and islands included within the monument are farther from human population centers than any other U.S. area. They represent one of the last frontiers and havens for wildlife in the world, and comprise the most widespread collection of coral reef, seabird, and shorebird protected areas on the planet under a single nation’s jurisdiction. At Howland Island, Baker Island, Jarvis Island, Palmyra Atoll, and Kingman Reef, the terrestrial areas, reefs, and waters out to 12 nautical miles (nmi) are part of the National Wildlife Refuge System. The land areas at Wake Atoll and Johnston Atoll remain under the jurisdiction of The giant clam, Tridacna gigas, is a clam that is the largest living bivalve mollusk. the U.S. Air Force, but the waters from Photo: © Kydd Pollock 0 to 12 nmi are protected as units of the National Wildlife Refuge System. For all of the areas, fishery-related Marine National Monument, and orders long time periods throughout their entire activities seaward from the 12-nmi refuge of magnitude greater than the reefs near cultural and geological history. These boundaries out to the 50-nmi monument heavily populated islands. Expansive refuges are unique in that they were and boundary are managed by the National shallow coral reefs and deep coral forests, are still largely pristine, though many Oceanic and Atmospheric Administration. -
Users, Uses, and Value of Landsat Satellite Imagery— Results from the 2012 Survey of Users
Users, Uses, and Value of Landsat Satellite Imagery— Results from the 2012 Survey of Users By Holly M. Miller, Leslie Richardson, Stephen R. Koontz, John Loomis, and Lynne Koontz Open-File Report 2013–1269 U.S. Department of the Interior U.S. Geological Survey i U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette Kimball, Acting Director U.S. Geological Survey, Reston, Virginia 2013 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Suggested citation: Miller, H.M., Richardson, Leslie, Koontz, S.R., Loomis, John, and Koontz, Lynne, 2013, Users, uses, and value of Landsat satellite imagery—Results from the 2012 survey of users: U.S. Geological Survey Open-File Report 2013–1269, 51 p., http://dx.doi.org/10.3133/ofr20131269. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Contents Contents ......................................................................................................................................................... ii Acronyms and Initialisms ...............................................................................................................................