Report from the PAME Workshop on Ecosystem Approach to Management
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Fronts in the World Ocean's Large Marine Ecosystems. ICES CM 2007
- 1 - This paper can be freely cited without prior reference to the authors International Council ICES CM 2007/D:21 for the Exploration Theme Session D: Comparative Marine Ecosystem of the Sea (ICES) Structure and Function: Descriptors and Characteristics Fronts in the World Ocean’s Large Marine Ecosystems Igor M. Belkin and Peter C. Cornillon Abstract. Oceanic fronts shape marine ecosystems; therefore front mapping and characterization is one of the most important aspects of physical oceanography. Here we report on the first effort to map and describe all major fronts in the World Ocean’s Large Marine Ecosystems (LMEs). Apart from a geographical review, these fronts are classified according to their origin and physical mechanisms that maintain them. This first-ever zero-order pattern of the LME fronts is based on a unique global frontal data base assembled at the University of Rhode Island. Thermal fronts were automatically derived from 12 years (1985-1996) of twice-daily satellite 9-km resolution global AVHRR SST fields with the Cayula-Cornillon front detection algorithm. These frontal maps serve as guidance in using hydrographic data to explore subsurface thermohaline fronts, whose surface thermal signatures have been mapped from space. Our most recent study of chlorophyll fronts in the Northwest Atlantic from high-resolution 1-km data (Belkin and O’Reilly, 2007) revealed a close spatial association between chlorophyll fronts and SST fronts, suggesting causative links between these two types of fronts. Keywords: Fronts; Large Marine Ecosystems; World Ocean; sea surface temperature. Igor M. Belkin: Graduate School of Oceanography, University of Rhode Island, 215 South Ferry Road, Narragansett, Rhode Island 02882, USA [tel.: +1 401 874 6533, fax: +1 874 6728, email: [email protected]]. -
An Overview of the Hudson Bay Marine Ecosystem
5–1 5.0 OCEANOGRAPHY Chapter Contents 5.1 CIRCULATION........................................................................................................................................................5–5 5.2 TIDES......................................................................................................................................................................5–7 5.3 WAVE CLIMATE AND STORM SURGES............................................................................................................5–10 5.4 SEA ICE ................................................................................................................................................................5–10 5.4.1 Terminology.......................................................................................................................................................5–11 5.4.2 Seasonal Changes............................................................................................................................................5–12 5.5 SALINITY, TEMPERATURE, AND MIXING .........................................................................................................5–18 5.5.1 Surface Distributions .........................................................................................................................................5–20 5.5.2 Vertical Profiles .................................................................................................................................................5–22 5.6 WATER CLARITY -
Contemporary State of Glaciers in Chukotka and Kolyma Highlands ISSN 2080-7686
Bulletin of Geography. Physical Geography Series, No. 19 (2020): 5–18 http://dx.doi.org/10.2478/bgeo-2020-0006 Contemporary state of glaciers in Chukotka and Kolyma highlands ISSN 2080-7686 Maria Ananicheva* 1,a, Yury Kononov 1,b, Egor Belozerov2 1 Russian Academy of Science, Institute of Geography, Moscow, Russia 2 Lomonosov State University, Faculty of Geography, Moscow, Russia * Correspondence: Russian Academy of Science, Institute of Geography, Moscow, Russia. E-mail: [email protected] a https://orcid.org/0000-0002-6377-1852, b https://orcid.org/0000-0002-3117-5554 Abstract. The purpose of this work is to assess the main parameters of the Chukotka and Kolyma glaciers (small forms of glaciation, SFG): their size and volume, and changes therein over time. The point as to whether these SFG can be considered glaciers or are in transition into, for example, rock glaciers is also presented. SFG areas were defined from the early 1980s (data from the catalogue of the glaciers compiled by R.V. Sedov) to 2005, and up to 2017: these data were retrieved from sat- Key words: ellite images. The maximum of the SGF reduction occurred in the Chantalsky Range, Iskaten Range, Chukotka Peninsula, and in the northern part of Chukotka Peninsula. The smallest retreat by this time relates to the gla- Kolyma Highlands, ciers of the southern part of the peninsula. Glacier volumes are determined by the formula of S.A. satellite image, Nikitin for corrie glaciers, based on in-situ volume measurements, and by our own method: the av- climate change, erage glacier thickness is calculated from isogypsum patterns, constructed using DEMs of individu- glacier reduction, al glaciers based on images taken from a drone during field work, and using ArcticDEM for others. -
15 Canadian High Arctic-North Greenland
15/18: LME FACTSHEET SERIES CANADIAN HIGH ARCTIC-NORTH GREENLAND LME tic LMEs Arc CANADIAN HIGH ARCTIC-NORTH GREENLAND LME MAP 18 of Central Map Arctic Ocean LME North Pole Ellesmere Island Iceland Greenland 15 "1 ARCTIC LMEs Large ! Marine Ecosystems (LMEs) are defined as regions of work of the ArcNc Council in developing and promoNng the ocean space of 200,000 km² or greater, that encompass Ecosystem Approach to management of the ArcNc marine coastal areas from river basins and estuaries to the outer environment. margins of a conNnental shelf or the seaward extent of a predominant coastal current. LMEs are defined by ecological Joint EA Expert group criteria, including bathymetry, hydrography, producNvity, and PAME established an Ecosystem Approach to Management tropically linked populaNons. PAME developed a map expert group in 2011 with the parNcipaNon of other ArcNc delineaNng 17 ArcNc Large Marine Ecosystems (ArcNc LME's) Council working groups (AMAP, CAFF and SDWG). This joint in the marine waters of the ArcNc and adjacent seas in 2006. Ecosystem Approach Expert Group (EA-EG) has developed a In a consultaNve process including agencies of ArcNc Council framework for EA implementaNon where the first step is member states and other ArcNc Council working groups, the idenNficaNon of the ecosystem to be managed. IdenNfying ArcNc LME map was revised in 2012 to include 18 ArcNc the ArcNc LMEs represents this first step. LMEs. This is the current map of ArcNc LMEs used in the This factsheet is one of 18 in a series of the ArcCc LMEs. OVERVIEW: CANADIAN HIGH ARCTIC-NORTH GREENLAND LME The Canadian High Arcc-North Greenland LME (CAA) consists of the northernmost and high arcc part of Canada along with the adjacent part of North Greenland. -
Arctic Research of the United States, Volume 15
This document has been archived. About The journal Arctic Research of the United refereed for scientific content or merit since the States is for people and organizations interested journal is not intended as a means of reporting the in learning about U.S. Government-financed scientific research. Articles are generally invited Arctic research activities. It is published semi- and are reviewed by agency staffs and others as Journal annually (spring and fall) by the National Science appropriate. Foundation on behalf of the Interagency Arctic As indicated in the U.S. Arctic Research Plan, Research Policy Committee (IARPC) and the research is defined differently by different agencies. Arctic Research Commission (ARC). Both the It may include basic and applied research, moni- Interagency Committee and the Commission were toring efforts, and other information-gathering authorized under the Arctic Research and Policy activities. The definition of Arctic according to Act (ARPA) of 1984 (PL 98-373) and established the ARPA is “all United States and foreign terri- by Executive Order 12501 (January 28, 1985). tory north of the Arctic Circle and all United Publication of the journal has been approved by States territory north and west of the boundary the Office of Management and Budget. formed by the Porcupine, Yukon, and Kuskokwim Arctic Research contains Rivers; all contiguous seas, including the Arctic • Reports on current and planned U.S. Govern- Ocean and the Beaufort, Bering, and Chukchi ment-sponsored research in the Arctic; Seas; and the Aleutian chain.” Areas outside of • Reports of ARC and IARPC meetings; and the boundary are discussed in the journal when • Summaries of other current and planned considered relevant to the broader scope of Arctic Arctic research, including that of the State of research. -
Master of Science Sustainable Development Semester – 1 Paper
Master of Science Sustainable Development Semester – 1 Paper No Subject Name Contents of Syllabi -Brundtland Commission/ Word -Commission on Environment and Development. -What is Sustainable Development? -What is Sustainability? -History of Sustainability. -Sustainability Measurement. -Carrying Capacity. -Water Crisis. -Land Use Management. -Forestry Development. -Ecoforestry. -Sustainable Agriculture. -Extinction. GLOBAL SUSTAINABLE -Sustainable Energy. Paper-I DEVELOPMENT I -Water Resources. -Sustainability Science. -Education for Sustainable Development. -Maximum Sustainable Yield. -Sustainable Forest Management. -Susainopreneurship. -Sustainable Procurement. -Sustainable Business. -Sustainable National Income. -Sustainable Transport. -Sustainable Tourism. -Sustainable Design. -Sustainable Urban Infrastructure. Master of Science Sustainable Development -What is Biodiversity? -Measurement of Biodiversity. -Species Richness. -Shannon Index. -2010 Biodiversity Indicators- Partnership. -Evolution. -Evolutionary Thought. -How does Evolution Occur? -Timeline of Evolution. BIODIVERSITY -Social Effect of Evolutionary Theory. Paper-II CONSERVATION & -Objections of Evolution. MANAGEMENT I -Population Genetics. -Genetics. -Heredity. -Mutation. -Molecular Evolution. -Genetic Recombination. -Sexual Reproduction. -Gene Flow. -Hybrid. -What is Energy? -History of Energy. -Timeline of Thermodynamics. -Units of Energy. -Potential Energy. -Elastic Energy. -Kinetic Energy. -Internal Energy. -Electromagnetism. -Electricity. GLOBAL ENERGY POLICIES Paper-III -
Shadwick, E. H., Et Al. Seasonal Variability of the Inorganic Carbon
Limnol. Oceanogr., 56(1), 2011, 303–322 E 2011, by the American Society of Limnology and Oceanography, Inc. doi:10.4319/lo.2011.56.1.0303 Seasonal variability of the inorganic carbon system in the Amundsen Gulf region of the southeastern Beaufort Sea E. H. Shadwick,a,* H. Thomas,a M. Chierici,b B. Else,c A. Fransson,d C. Michel,e L. A. Miller,f A. Mucci,g A. Niemi,e T. N. Papakyriakou,c and J.-E´ . Tremblayh a Department of Oceanography, Dalhousie University, Halifax, Nova Scotia, Canada bDepartment of Chemistry, University of Gothenburg, Go¨teborg, Sweden c Center for Earth Observation Science, University of Manitoba, Winnipeg, Manitoba, Canada dDepartment of Earth Sciences, University of Gothenburg, Go¨teborg, Sweden e Freshwater Institute, Fisheries and Oceans Canada, Winnipeg, Manitoba, Canada f Institute of Ocean Sciences, Fisheries and Oceans Canada, Sidney, British Columbia, Canada g Department of Earth and Planetary Sciences, McGill University, Montreal, Que´bec, Canada hDepartment de Biologie, Universite´ Laval, Que´bec, Que´bec, Canada Abstract During a year-round occupation of Amundsen Gulf in the Canadian Arctic Archipelago dissolved inorganic and organic carbon (DIC, DOC), total alkalinity (TA), partial pressure of CO2 (pCO2) and related parameters were measured over a full annual cycle. A two-box model was used to identify and assess physical, biological, and chemical processes responsible for the seasonal variability of DIC, DOC, TA, and pCO2. Surface waters were undersaturated with respect to atmospheric CO2 throughout the year and constituted a net sink of 22 21 1.2 mol C m yr , with ice coverage and ice formation limiting the CO2 uptake during winter. -
Sources and Pathways 4.1
Chapter 4 Persistant toxic substances (PTS) sources and pathways 4.1. Introduction Chapter 4 4.1. Introduction 4.2. Assessment of distant sources: In general, the human environment is a combination Longrange atmospheric transport of the physical, chemical, biological, social and cultur- Due to the nature of atmospheric circulation, emission al factors that affect human health. It should be recog- sources located within the Northern Hemisphere, par- nized that exposure of humans to PTS can, to certain ticularly those in Europe and Asia, play a dominant extent, be dependant on each of these factors. The pre- role in the contamination of the Arctic. Given the spa- cise role differs depending on the contaminant con- tial distribution of PTS emission sources, and their cerned, however, with respect to human intake, the potential for ‘global’ transport, evaluation of long- chain consisting of ‘source – pathway – biological avail- range atmospheric transport of PTS to the Arctic ability’ applies to all contaminants. Leaving aside the region necessarily involves modeling on the hemi- biological aspect of the problem, this chapter focuses spheric/global scale using a multi-compartment on PTS sources, and their physical transport pathways. approach. To meet these requirements, appropriate modeling tools have been developed. Contaminant sources can be provisionally separated into three categories: Extensive efforts were made in the collection and • Distant sources: Located far from receptor sites in preparation of input data for modeling. This included the Arctic. Contaminants can reach receptor areas the required meteorological and geophysical informa- via air currents, riverine flow, and ocean currents. tion, and data on the physical and chemical properties During their transport, contaminants are affected by of both the selected substances and of their emissions. -
British Virgin Islands
British Virgin Islands Clive Petrovic, Esther Georges and Nancy Woodfield Andy McGowan Great Tobago General introduction The British Virgin Islands comprise more than 60 islands, and the Virgin Islands. These include the globally cays and rocks, with a total land area of approximately 58 threatened Cordia rupicola (CR), Maytenus cymosa (EN) and square miles (150 square km). This archipelago is located Acacia anegadensis (CR). on the Puerto Rican Bank in the north-east Caribbean at A quarter of the 24 reptiles and amphibians identified are approximately 18˚N and 64˚W. The islands once formed a endemic, including the Anegada Rock Iguana Cyclura continuous land mass with the US Virgin Islands and pinguis (CR), which is now restricted to Anegada. Other Puerto Rico, and were isolated only in relatively recent endemics include Anolis ernestwilliamsii, Eleutherodactylus geologic time. With the exception of the limestone island of schwartzi, the Anegada Ground Snake Alsophis portoricensis Anegada, the islands are volcanic in origin and are mostly anegadae, the Virgin Gorda Gecko Sphaerodactylus steep-sided with rugged topographic features and little flat parthenopian, the Virgin Gorda Worm Snake Typlops richardi land, surrounded by coral reefs. naugus, and the Anegada Worm Snake Typlops richardi Situated at the eastern end of the Greater Antilles chain, the catapontus. Other globally threatened reptiles within the islands experience a dry sub-tropical climate dominated by BVI include the Anolis roosevelti (CR) and Epicrates monensis the prevailing north-east trade winds. Maximum summer granti (EN). temperatures reach 31˚C; minimum winter temperatures Habitat alteration during the plantation era and the are 19˚C, and there is an average rainfall of 700 mm per introduction of invasive alien species has had major year with seasonal hurricane events. -
UK Overseas Territories
INFORMATION PAPER United Kingdom Overseas Territories - Toponymic Information United Kingdom Overseas Territories (UKOTs), also known as British Overseas Territories (BOTs), have constitutional and historical links with the United Kingdom, but do not form part of the United Kingdom itself. The Queen is the Head of State of all the UKOTs, and she is represented by a Governor or Commissioner (apart from the UK Sovereign Base Areas that are administered by MOD). Each Territory has its own Constitution, its own Government and its own local laws. The 14 territories are: Anguilla; Bermuda; British Antarctic Territory (BAT); British Indian Ocean Territory (BIOT); British Virgin Islands; Cayman Islands; Falkland Islands; Gibraltar; Montserrat; Pitcairn, Henderson, Ducie and Oeno Islands; Saint Helena, Ascension and Tristan da Cunha; South Georgia and the South Sandwich Islands; Turks and Caicos Islands; UK Sovereign Base Areas. PCGN recommend the term ‘British Overseas Territory Capital’ for the administrative centres of UKOTs. Production of mapping over the UKOTs does not take place systematically in the UK. Maps produced by the relevant territory, preferably by official bodies such as the local government or tourism authority, should be used for current geographical names. National government websites could also be used as an additional reference. Additionally, FCDO and MOD briefing maps may be used as a source for names in UKOTs. See the FCDO White Paper for more information about the UKOTs. ANGUILLA The territory, situated in the Caribbean, consists of the main island of Anguilla plus some smaller, mostly uninhabited islands. It is separated from the island of Saint Martin (split between Saint-Martin (France) and Sint Maarten (Netherlands)), 17km to the south, by the Anguilla Channel. -
ISO Country Codes
COUNTRY SHORT NAME DESCRIPTION CODE AD Andorra Principality of Andorra AE United Arab Emirates United Arab Emirates AF Afghanistan The Transitional Islamic State of Afghanistan AG Antigua and Barbuda Antigua and Barbuda (includes Redonda Island) AI Anguilla Anguilla AL Albania Republic of Albania AM Armenia Republic of Armenia Netherlands Antilles (includes Bonaire, Curacao, AN Netherlands Antilles Saba, St. Eustatius, and Southern St. Martin) AO Angola Republic of Angola (includes Cabinda) AQ Antarctica Territory south of 60 degrees south latitude AR Argentina Argentine Republic America Samoa (principal island Tutuila and AS American Samoa includes Swain's Island) AT Austria Republic of Austria Australia (includes Lord Howe Island, Macquarie Islands, Ashmore Islands and Cartier Island, and Coral Sea Islands are Australian external AU Australia territories) AW Aruba Aruba AX Aland Islands Aland Islands AZ Azerbaijan Republic of Azerbaijan BA Bosnia and Herzegovina Bosnia and Herzegovina BB Barbados Barbados BD Bangladesh People's Republic of Bangladesh BE Belgium Kingdom of Belgium BF Burkina Faso Burkina Faso BG Bulgaria Republic of Bulgaria BH Bahrain Kingdom of Bahrain BI Burundi Republic of Burundi BJ Benin Republic of Benin BL Saint Barthelemy Saint Barthelemy BM Bermuda Bermuda BN Brunei Darussalam Brunei Darussalam BO Bolivia Republic of Bolivia Federative Republic of Brazil (includes Fernando de Noronha Island, Martim Vaz Islands, and BR Brazil Trindade Island) BS Bahamas Commonwealth of the Bahamas BT Bhutan Kingdom of Bhutan -
Flow of Pacific Water in the Western Chukchi
Deep-Sea Research I 105 (2015) 53–73 Contents lists available at ScienceDirect Deep-Sea Research I journal homepage: www.elsevier.com/locate/dsri Flow of pacific water in the western Chukchi Sea: Results from the 2009 RUSALCA expedition Maria N. Pisareva a,n, Robert S. Pickart b, M.A. Spall b, C. Nobre b, D.J. Torres b, G.W.K. Moore c, Terry E. Whitledge d a P.P. Shirshov Institute of Oceanology, 36, Nakhimovski Prospect, Moscow 117997, Russia b Woods Hole Oceanographic Institution, 266 Woods Hole Road, Woods Hole, MA 02543, USA c Department of Physics, University of Toronto, 60 St. George Street, Toronto, Ontario M5S 1A7, Canada d University of Alaska Fairbanks, 505 South Chandalar Drive, Fairbanks, AK 99775, USA article info abstract Article history: The distribution of water masses and their circulation on the western Chukchi Sea shelf are investigated Received 10 March 2015 using shipboard data from the 2009 Russian-American Long Term Census of the Arctic (RUSALCA) pro- Received in revised form gram. Eleven hydrographic/velocity transects were occupied during September of that year, including a 25 August 2015 number of sections in the vicinity of Wrangel Island and Herald canyon, an area with historically few Accepted 25 August 2015 measurements. We focus on four water masses: Alaskan coastal water (ACW), summer Bering Sea water Available online 31 August 2015 (BSW), Siberian coastal water (SCW), and remnant Pacific winter water (RWW). In some respects the Keywords: spatial distributions of these water masses were similar to the patterns found in the historical World Arctic Ocean Ocean Database, but there were significant differences.