Large Marine Ecosystems (Lmes) of the Arctic Area Revision of the Arctic LME Map 15Th of May 2013
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Russia and the Eurasian Republics THIS REGION Spans the Continents of Europe and Asia
390-391 U5 CH14 UO TWIP-860976 3/15/04 5:21 AM Page 390 Unit Workers on the statue Russians in front of Motherland Calls, St. Basil’s Cathedral, Volgograd Moscow 224 390-391 U5 CH14 UO TWIP-860976 3/15/04 5:22 AM Page 391 RussiaRussia andand the the EurasianEurasian f you had to describe Russia RepublicsRepublics Iin one word, that word would be BIG! Russia is the largest country in the world in area. Its almost 6.6 million square miles (17 million sq. km) are spread across two continents—Europe and Asia. As you can imagine, such a large country faces equally large challenges. In 1991 Russia emerged from the Soviet Union as an independent country. Since then it has been struggling to unite its many ethnic groups, set up a demo- cratic government, and build a stable economy. ▼ Siberian tiger in a forest NGS ONLINE in eastern Russia www.nationalgeographic.com/education 225 392-401 U5 CH14 RA TWIP-860976 3/15/04 5:28 AM Page 392 REGIONAL ATLAS Focus on: Russia and the Eurasian Republics THIS REGION spans the continents of Europe and Asia. It includes Russia—the world’s largest country—and the neigh- boring independent republics of Armenia, Georgia, Azerbaijan, Kazakhstan, Uzbekistan, Turkmenistan, Kyrgyzstan, and Tajikistan. Russia and the Eurasian republics cover about 8 million square miles (20.7 million sq. km). This is greater than the size of Canada, the United States, and Mexico combined. The Caspian Sea is actually a salt lake that lies at the base of the Caucasus Mountains in The Land Russia’s southwest. -
Boreogadus Saida) and Safron Cod (Eleginus Gracilis) Early Life Stages in the Pacifc Arctic
Polar Biology https://doi.org/10.1007/s00300-019-02494-4 ORIGINAL PAPER Spatio‑temporal distribution of polar cod (Boreogadus saida) and safron cod (Eleginus gracilis) early life stages in the Pacifc Arctic Cathleen D. Vestfals1 · Franz J. Mueter2 · Janet T. Dufy‑Anderson3 · Morgan S. Busby3 · Alex De Robertis3 Received: 24 September 2018 / Revised: 15 March 2019 / Accepted: 18 March 2019 © Springer-Verlag GmbH Germany, part of Springer Nature 2019 Abstract Polar cod (Boreogadus saida) and safron cod (Eleginus gracilis) are key fshes in the Arctic marine ecosystem, serving as important trophic links between plankton and apex predators, yet our understanding of their life histories in Alaska’s Arctic is extremely limited. To improve our knowledge about their early life stages (ELS), we described the spatial and temporal distributions of prefexion larvae to late juveniles (to 65 mm in length) in the Chukchi and western Beaufort seas based on surveys conducted between 2004 and 2013, and examined how their abundances varied in response to environmental factors. Species-specifc diferences in habitat use were found, with polar cod having a more ofshore and northern distribution than safron cod, which were found closer inshore and farther south. Polar cod prefexion and fexion larvae were encountered throughout the sampling season across much of the shelf, which suggests that spawning occurs over several months and at multiple locations, with Barrow Canyon potentially serving as an important spawning and/or retention area. Polar cod ELS were abundant at intermediate temperatures (5.0–6.0 °C), while safron cod were most abundant at the highest temperatures, which suggests that safron cod may beneft from a warming Arctic, while polar cod may be adversely afected. -
2021 Alaska Studies Plan
U.S. Department of the Interior Bureau of Ocean Energy Management Alaska Outer Connental Shelf Region Anchorage, Alaska November 2020 Prepared by U.S. Department of the Interior Bureau of Ocean Energy Management Anchorage, Alaska Office 3801 Centerpoint Drive, Suite 500 Anchorage, Alaska 99503-5823 November 2020 The Environmental Studies Program has chosen to “go green.” This document can be accessed in electronic format at http://www.boem.gov/akstudies/. For assistance accessing the document or for further information about the Studies Program and our planning process, please contact [email protected] or Dr. Heather Crowley at [email protected]. The inclusion of study profiles in this document does not constitute a commitment by the U.S. Department of the Interior, Bureau of Ocean Energy Management to conduct or fund any or all of the studies. Method of procurement may be selected at the discretion of BOEM. The scope of the studies is subject to change prior to initiation of any work. Any use of trade names is for descriptive purposes only and does not constitute endorsement of these products by the Bureau of Ocean Energy Management. Cover Image: Sea urchins in the intertidal zone, Cook Inlet, Alaska. Photo credit: “ShoreZone Imaging and Mapping along the Alaska Peninsula” project team; OCS Study BOEM 2018-037. United States Department of the Interior BUREAU OF OCEAN ENERGY MANAGEMENT Alaska Regional Office 3801 Centerpoint Drive, Suite 500 Anchorage, Alaska 99503-5823 November 2, 2020 Dear Stakeholder: Thank you for your interest in the Environmental Studies Program (ESP) of the Bureau of Ocean Energy Management (BOEM). -
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. -
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 -
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. -
Re-Evaluation of Strike-Slip Displacements Along and Bordering Nares Strait
Polarforschung 74 (1-3), 129 – 160, 2004 (erschienen 2006) In Search of the Wegener Fault: Re-Evaluation of Strike-Slip Displacements Along and Bordering Nares Strait by J. Christopher Harrison1 Abstract: A total of 28 geological-geophysical markers are identified that lich der Bache Peninsula und Linksseitenverschiebungen am Judge-Daly- relate to the question of strike slip motions along and bordering Nares Strait. Störungssystem (70 km) und schließlich die S-, später SW-gerichtete Eight of the twelve markers, located within the Phanerozoic orogen of Kompression des Sverdrup-Beckens (100 + 35 km). Die spätere Deformation Kennedy Channel – Robeson Channel region, permit between 65 and 75 km wird auf die Rotation (entgegen dem Uhrzeigersinn) und ausweichende West- of sinistral offset on the Judge Daly Fault System (JDFS). In contrast, eight of drift eines semi-rigiden nördlichen Ellesmere-Blocks während der Kollision nine markers located in Kane Basin, Smith Sound and northern Baffin Bay mit der Grönlandplatte zurückgeführt. indicate no lateral displacement at all. Especially convincing is evidence, presented by DAMASKE & OAKEY (2006), that at least one basic dyke of Neoproterozoic age extends across Smith Sound from Inglefield Land to inshore eastern Ellesmere Island without any recognizable strike slip offset. INTRODUCTION These results confirm that no major sinistral fault exists in southern Nares Strait. It is apparent to both earth scientists and the general public To account for the absence of a Wegener Fault in most parts of Nares Strait, that the shape of both coastlines and continental margins of the present paper would locate the late Paleocene-Eocene Greenland plate boundary on an interconnected system of faults that are 1) traced through western Greenland and eastern Arctic Canada provide for a Jones Sound in the south, 2) lie between the Eurekan Orogen and the Precam- satisfactory restoration of the opposing lands. -
Arctic Report Card 2009
October 2009 Citing the complete report: Richter-Menge, J., and J.E. Overland, Eds., 2009: Arctic Report Card 2009, http://www.arctic.noaa.gov/reportcard. Citing an essay (example): Perovich, D., R. Kwok, W. Meier, S. V. Nghiem, and J. Richter-Menge, 2009: Sea Ice Cover [in Arctic Report Card 2009], http://www.arctic.noaa.gov/reportcard. Authors and Affiliations I. Ashik, Arctic and Antarctic Research Institute, St. Petersburg, Russia L.-S. Bai, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio R. Benson, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio U. S. Bhatt, Geophysical Institute, University of Alaska–Fairbanks, Fairbanks, Alaska I. Bhattacharya, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio J. E. Box, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio D. H. Bromwich, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio R. Brown, Climate Research Division, Environment Canada J. Cappelen, Danish Meteorological Institute, Copenhagen, Denmark E. Carmack, Institute of Ocean Sciences, Sidney, Canada B. Collen, Institute of Zoology, Zoological Society of London, Regent’s Park, London, UK J. E. Comiso, NASA Goddard Space Flight Center, Greenbelt, Maryland D. Decker, Byrd Polar Research Center, The Ohio State University, Columbus, Ohio C. Derksen, Climate Research Division, Environment Canada N. DiGirolamo, Science Systems Applications Inc. and NASA Goddard Space Flight Center, Greenbelt, Maryland D. Drozdov, Earth Cryosphere Institute, Tumen, Russia B. Ebbinge, Alterra, Wageningen H. E. Epstein, University of Virginia, Charlottesville, Virginia X. Fettweis, Department of Geography, University of Liège, Liège, Belgium I. Frolov, Arctic and Antarctic Research Institute, St. -
Transits of the Northwest Passage to End of the 2020 Navigation Season Atlantic Ocean ↔ Arctic Ocean ↔ Pacific Ocean
TRANSITS OF THE NORTHWEST PASSAGE TO END OF THE 2020 NAVIGATION SEASON ATLANTIC OCEAN ↔ ARCTIC OCEAN ↔ PACIFIC OCEAN R. K. Headland and colleagues 7 April 2021 Scott Polar Research Institute, University of Cambridge, Lensfield Road, Cambridge, United Kingdom, CB2 1ER. <[email protected]> The earliest traverse of the Northwest Passage was completed in 1853 starting in the Pacific Ocean to reach the Atlantic Oceam, but used sledges over the sea ice of the central part of Parry Channel. Subsequently the following 319 complete maritime transits of the Northwest Passage have been made to the end of the 2020 navigation season, before winter began and the passage froze. These transits proceed to or from the Atlantic Ocean (Labrador Sea) in or out of the eastern approaches to the Canadian Arctic archipelago (Lancaster Sound or Foxe Basin) then the western approaches (McClure Strait or Amundsen Gulf), across the Beaufort Sea and Chukchi Sea of the Arctic Ocean, through the Bering Strait, from or to the Bering Sea of the Pacific Ocean. The Arctic Circle is crossed near the beginning and the end of all transits except those to or from the central or northern coast of west Greenland. The routes and directions are indicated. Details of submarine transits are not included because only two have been reported (1960 USS Sea Dragon, Capt. George Peabody Steele, westbound on route 1 and 1962 USS Skate, Capt. Joseph Lawrence Skoog, eastbound on route 1). Seven routes have been used for transits of the Northwest Passage with some minor variations (for example through Pond Inlet and Navy Board Inlet) and two composite courses in summers when ice was minimal (marked ‘cp’). -
Atlantic Walrus Odobenus Rosmarus Rosmarus
COSEWIC Assessment and Update Status Report on the Atlantic Walrus Odobenus rosmarus rosmarus in Canada SPECIAL CONCERN 2006 COSEWIC COSEPAC COMMITTEE ON THE STATUS OF COMITÉ SUR LA SITUATION ENDANGERED WILDLIFE DES ESPÈCES EN PÉRIL IN CANADA AU CANADA COSEWIC status reports are working documents used in assigning the status of wildlife species suspected of being at risk. This report may be cited as follows: COSEWIC 2006. COSEWIC assessment and update status report on the Atlantic walrus Odobenus rosmarus rosmarus in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. ix + 65 pp. (www.sararegistry.gc.ca/status/status_e.cfm). Previous reports: COSEWIC 2000. COSEWIC assessment and status report on the Atlantic walrus Odobenus rosmarus rosmarus (Northwest Atlantic Population and Eastern Arctic Population) in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. vi + 23 pp. (www.sararegistry.gc.ca/status/status_e.cfm). Richard, P. 1987. COSEWIC status report on the Atlantic walrus Odobenus rosmarus rosmarus (Northwest Atlantic Population and Eastern Arctic Population) in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. 1-23 pp. Production note: COSEWIC would like to acknowledge D.B. Stewart for writing the status report on the Atlantic Walrus Odobenus rosmarus rosmarus in Canada, prepared under contract with Environment Canada, overseen and edited by Andrew Trites, Co-chair, COSEWIC Marine Mammals Species Specialist Subcommittee. For additional copies contact: COSEWIC Secretariat c/o Canadian Wildlife Service Environment Canada Ottawa, ON K1A 0H3 Tel.: (819) 997-4991 / (819) 953-3215 Fax: (819) 994-3684 E-mail: COSEWIC/[email protected] http://www.cosewic.gc.ca Également disponible en français sous le titre Évaluation et Rapport de situation du COSEPAC sur la situation du morse de l'Atlantique (Odobenus rosmarus rosmarus) au Canada – Mise à jour. -
Hudson Bay Ice Conditions
Hudson Bay Ice Conditions ERIC W. DANIELSON, JR.l ABSTRACT.Monthly mean ice cover distributions for Hudson Bay have been derived, based upon an analysis of nine years of aerial reconnaissance and other data. Information is presented in map form, along with diseussian Of significant features. Ice break-up is seen to work southward from the western, northern, and eastern edges of the Bay; the pattern seems to be a result of local topography, cur- rents, and persistent winds. Final melting occurs in August. Freeze-up commences in October, along the northwestern shore, and proceeds southeastward. The entire Bay is ice-covered by early January,except for persistent shore leads. RÉSUMÉ. Conditions de la glace dans la mer d’Hudson. A partir de l’analyse de neuf années de reconnaissances aériennes et d’autres données, on a pu déduire des moyennes mensuelles de distribution de la glace pour la mer d’Hudson. L‘informa- tion est présentte sous formes de cartes et de discussion des Cléments significatifs. On y voit que la débâcle progresse vers le sud à partir des marges ouest, nord et est dela mer; cette séquence sembleêtre le résultat de la topographielocale, des courants et .des vents dominants. La fonte se termine en aofit. L’enge€wommence en octobre le long de la rive nord-ouest et progresse vers le sud-est. Sauf pow les chenaux côtiers persistants, la mer est entihrement gelée au début de janvier. INTRODUCTION In many respects, ice cover is a basic hydrometeorological variable. In Hudson Bay (Fig. 1) it might be considered the most basic of all, as it influences all other conditions so decisively.