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Beaufort Sea Monitoring Program
Outer Continental Shelf Environmental Assessment Program Beaufort Sea Monitoring Program: Proceedings of a Workshop and Sampling Design Recommendations Beaufort Sea Monitoring Program: Proceedings of a Workshop (September 1983) and Sampling Design Recommendations ; Prepared for the Outer Continental Shelf Environmental Assessment Program Juneau, Alaska by J. P. Houghton Dames & Moore 155 N.E. lOOth Street Seattle, WA 98125 with D. A Segar J. E. Zeh SEAM Ocean Inc. Department of Statistics Po. Box 1627 University of Washington Wheaton, MD 20902 Seattle, WA 98195 April 1984 UNITED STATES UNITED STATES DEPARTMENT OF COMMERCE DEPARTMENT OF THE INTERIOR Malcolm Baldridge, Secretary William P Clark, Secretary NATIONAL OCEANIC AND MINERALS MANAGEMENT SERVICE ATMOSPHERIC ADMINISTRATION William D. Bettenberg, Director John V. Byrne, Administrator r. NOTICES i? I This report has been reviewed by the US. Department of Commerce, National Oceanic and Atmospheric Administration's Outer Continental Shelf Environmental Assessment Program office, and approved for publication. The interpretation of data and opinions expressed in this document are those of the authors and workshop participants. Approval does not necessarily signify that the contents reflect the views and policies of the Department of Commerce or those of the Department of the Interior. The National Oceanic and Atmospheric Administration (NOAA) does not approve, recommend, or endorse any proprietary product or proprietary material mentioned in this publica tion. No reference shall be made to NOAA or to this publication in any advertising or sales promotion which would indicate or imply that NOAA approves, recommends, or endorses any proprietary'product or proprietary material mentioned herein, or which has as its purpose an intent to cause directly or indirectly the advertised product to be used or purchas'ed because of this publication. -
Mediterranean, Black and Caspian Seas Region
MEDITERRANEAN, BLACK AND CASPIAN SEAS REGION 1 INTRODUCTION • Fellows from the region • National and Regional needs for the Region • Actions to be taken. • Recent developments on Maritime issues 2 Fellows from the Region • Republic of Bulgaria – 1 • Georgia – 1 • Islamic Republic of Iran – 3 • Turkey – 1 • Libya – 1 • Republic of Azerbaijan – 1 3 Republic of Bulgaria • To comply, implement and enforce the IMO Conventions namely Ballast Water Management Convention, Recycling Convention and HNS Convention. • To conclude agreement with neighboring countries e.g with Romania on delimitation of maritime spaces in Black Sea. • To assist the States in the region in their endeavor to comply with, implement and enforce the IMO conventions because the ratification and enforcement of existing IMO conventions by all Black sea countries will ensure a global level playing field. 4 • To elaborate the national Maritime Transport Strategy with its priority areas, namely shipping in globalized markets, human resources, quality shipping, short sea shipping, research and innovation • To conclude search and rescue agreements between the countries in the Black Sea region • These are national and regional needs for the Republic of Bulgaria. 5 Islamic Republic of Iran Issues regarding environmental legislation, national action and delimitation of maritime boundaries •Inadequate marine and coastal management laws. •Insufficient legislation to protect coastal and marine natural resources. •Overlapping and conflicting laws regarding marine and coastal management. • Lack of internationally legally recognized regime applicable to exploration and exploitation of the shared natural resources. 6 Actions to be taken • Strengthen the legal framework regarding coastal and marine environment protection • Coordinating and managing environmental conflicts among various organizations. -
A 2020 Vision for the Black Sea Region a Report by the Commission on the Black Sea
A 2020 Vision for the Black Sea Region A Report by the Commission on the Black Sea www.blackseacom.eu An initiative of: The Black eaS Trust for Regional Cooperation A 2020 Vision for the Black Sea Region A Report by the Commission on the Black Sea Contents Why read this Report? 4 What is the Commission on the Black Sea? 7 Executive Summary 12 Резюме выводов 15 Yönetici Özeti 19 The Report Introduction: The State of Play 22 Peace and Security 28 Economic Development and Welfare 31 Democratic Institutions and Good Governance 34 Regional Cooperation 36 Conclusions 38 Policy Recommendations 40 The Black Sea in Figures 45 Abbreviations 65 Initiators 67 The Rapporteurs, Editor and Acknowledgements 69 Imprint 70 3 Why read this Report? Why read this Report? … because the Black Sea matters The Black Sea region is coming into its own - but it is a contested and sometimes dangerous neighbourhood. It has undergone countless political transformations over time. And now, once again, it is becoming the subject of an intense debate. This reflects the changing dynamics of the Black Sea countries and the complex realities of their politics and conflicts, economies and societies. Geography, the interests of others and the region’s relations with the rest of the world in large part explain its resurgence. Straddling Europe and Asia, the Black Sea links north to south and east to west. Oil, gas, transport and trade routes are all crucial in explaining its increasing relevance. In the last two decades the Black Sea has changed beyond recognition. We have witnessed the transformation of the former communist societies and the impact of globalisation. -
Recent Declines in Warming and Vegetation Greening Trends Over Pan-Arctic Tundra
Remote Sens. 2013, 5, 4229-4254; doi:10.3390/rs5094229 OPEN ACCESS Remote Sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Recent Declines in Warming and Vegetation Greening Trends over Pan-Arctic Tundra Uma S. Bhatt 1,*, Donald A. Walker 2, Martha K. Raynolds 2, Peter A. Bieniek 1,3, Howard E. Epstein 4, Josefino C. Comiso 5, Jorge E. Pinzon 6, Compton J. Tucker 6 and Igor V. Polyakov 3 1 Geophysical Institute, Department of Atmospheric Sciences, College of Natural Science and Mathematics, University of Alaska Fairbanks, 903 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 2 Institute of Arctic Biology, Department of Biology and Wildlife, College of Natural Science and Mathematics, University of Alaska, Fairbanks, P.O. Box 757000, Fairbanks, AK 99775, USA; E-Mails: [email protected] (D.A.W.); [email protected] (M.K.R.) 3 International Arctic Research Center, Department of Atmospheric Sciences, College of Natural Science and Mathematics, 930 Koyukuk Dr., Fairbanks, AK 99775, USA; E-Mail: [email protected] 4 Department of Environmental Sciences, University of Virginia, 291 McCormick Rd., Charlottesville, VA 22904, USA; E-Mail: [email protected] 5 Cryospheric Sciences Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mail: [email protected] 6 Biospheric Science Branch, NASA Goddard Space Flight Center, Code 614.1, Greenbelt, MD 20771, USA; E-Mails: [email protected] (J.E.P.); [email protected] (C.J.T.) * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +1-907-474-2662; Fax: +1-907-474-2473. -
Modeling of the Turkish Strait System Using a High Resolution Unstructured Grid Ocean Circulation Model
Journal of Marine Science and Engineering Article Modeling of the Turkish Strait System Using a High Resolution Unstructured Grid Ocean Circulation Model Mehmet Ilicak 1,* , Ivan Federico 2 , Ivano Barletta 2,3 , Sabri Mutlu 4 , Haldun Karan 4 , Stefania Angela Ciliberti 2 , Emanuela Clementi 5 , Giovanni Coppini 2 and Nadia Pinardi 3 1 Eurasia Institute of Earth Sciences, Istanbul Technical University, Istanbul 34469, Turkey 2 Fondazione Centro Euro-Mediterraneo sui Cambiamenti Climatici, Ocean Predictions and Applications Division, 73100 Lecce, Italy; [email protected] (I.F.); [email protected] (I.B.); [email protected] (S.A.C.); [email protected] (G.C.) 3 Department of Physics and Astronomy, Universita di Bologna Alma Mater Studiorum, 40126 Bologna, Italy; [email protected] 4 TUBITAK MRC Environment and Cleaner Production Institute, Kocaeli 41470, Turkey; [email protected] (S.M.); [email protected] (H.K.) 5 Fondazione Centro Euro-Mediterraneo sui Cambiamenti Climatici, Ocean Modeling and Data Assimilation Division, 40126 Bologna, Italy; [email protected] * Correspondence: [email protected] Abstract: The Turkish Strait System, which is the only connection between the Black Sea and the Mediterranean Sea, is a challenging region for ocean circulation models due to topographic constraints and water mass structure. We present a newly developed high resolution unstructured finite element grid model to simulate the Turkish Strait System using realistic atmospheric forcing and lateral open boundary conditions. We find that the jet flowing from the Bosphorus Strait into the Marmara creates Citation: Ilicak, M.; Federico, I.; an anticyclonic circulation. The eddy kinetic energy field is high around the jets exiting from the Barletta, I.; Mutlu, S.; Karan, H.; Ciliberti, S.A.; Clementi, E.; Coppini, Bosphorus Strait, Dardanelles Strait, and also the leeward side of the islands in the Marmara Sea. -
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. -
Archaeology Resources
Archaeology Resources Page Intentionally Left Blank Archaeological Resources Background Archaeological Resources are defined as “any prehistoric or historic district, site, building, structure, or object [including shipwrecks]…Such term includes artifacts, records, and remains which are related to such a district, site, building, structure, or object” (National Historic Preservation Act, Sec. 301 (5) as amended, 16 USC 470w(5)). Archaeological resources are either historic or prehistoric and generally include properties that are 50 years old or older and are any of the following: • Associated with events that have made a significant contribution to the broad patterns of our history • Associated with the lives of persons significant in the past • Embody the distinctive characteristics of a type, period, or method of construction • Represent the work of a master • Possess high artistic values • Present a significant and distinguishable entity whose components may lack individual distinction • Have yielded, or may be likely to yield, information important in history These resources represent the material culture of past generations of a region’s prehistoric and historic inhabitants, and are basic to our understanding of the knowledge, beliefs, art, customs, property systems, and other aspects of the nonmaterial culture. Further, they are subject to National Historic Preservation Act (NHPA) review if they are historic properties, meaning those that are on, or eligible for placement on, the National Register of Historic Places (NRHP). These sites are referred to as historic properties. Section 106 requires agencies to make a reasonable and good faith efforts to identify historic properties. Archaeological resources may be found in the Proposed Project Area both offshore and onshore. -
The Black Sea Region After EU Enlargement Occasional Paper
Occasional Paper June 2004 n°53 Mustafa Aydin Europe’s next shore: the Black Sea region after EU enlargement published by the European Union Institute for Security Studies 43 avenue du Président Wilson F-75775 Paris cedex 16 phone: + 33 (0) 1 56 89 19 30 fax: + 33 (0) 1 56 89 19 31 e-mail: [email protected] www.iss-eu.org In January 2002 the EU Institute for Security Studies (EUISS) was created as a Paris- based autonomous agency of the European Union. Following an EU Council Joint Action of 20 July 2001, it is now an integral part of the new structures that will support the fur- ther development of the CFSP/ESDP. The Institute’s core mission is to provide analyses and recommendations that can be of use and relevance to the formulation of EU policies. In carrying out that mission, it also acts as an interface between experts and decision-mak- ers at all levels. Occasional Papers are essays or reports that the Institute considers should be made avail- able as a contribution to the debate on topical issues relevant to European security. They may be based on work carried out by researchers granted awards by the EUISS, on contri- butions prepared by external experts, and on collective research projects or other activities organised by (or with the support of) the Institute. They reflect the views of their authors, not those of the Institute. Publication of Occasional Papers will be announced in the EUISS Newsletter and they will be available on request in the language - either English or French - used by authors. -
Beaufort Sea
160°W 159°W 158°W 157°W 156°W 155°W 154°W 153°W 152°W 151°W 150°W 149°W 148°W 147°W 146°W 145°W 144°W 143°W 142°W 141°W 140°W Beaufort Sea !Barrow N ° N 1 ° 14 7 1 7 15 13 12 !Wainwright 16 11 Prudhoe 17 Bay 10 Camden N 9 ° N Bay Kaktovik 0 ° 8 7 !Kaktovik Nuiqsut 7 0 ! 7 6 5 4 3 2 1 N ational P e C troleum Reserv e - Alaska a U n a . S d . a N - ° N - 9 ° A 6 9 s s Y 6 n e d e r l W i l a u s k k o a Index Map 1 of 3 n U.S./Canada Border to Wainwright ife Refuge Final Designation ic National Wildl of Critical Barrier Islands and Arct Denning Habitat Maps N ° N 8 ° 6 8 6 0 10 20 30 40 50 60 70 80 90 100 miles 0 10 20 30 40 50 60 70 80 90 100 km Map N ° N 7 ° Area 6 7 Pacific Ocean 6 158°W 157°W 156°W 155°W 154°W 153°W 152°W 151°W 150°W 149°W 148°W 147°W 146°W 145°W 144°W 143°W 142°W 99-0136 142°20'W 142°10'W 142°W 141°50'W 141°40'W 141°30'W 141°20'W 141°10'W 141°W Beaufort Sea N N ' ' 0 0 5 5 ° ° 9 9 6 6 r e v i R k a sr ak Eg N N ' ' 0 0 4 r Demarcation 4 ° ° 9 e 9 6 v 6 i Bay R t u k a g n o K N N ' ' 0 0 3 3 ° ° 9 9 6 6 C U a n . -
Natural Variability of the Arctic Ocean Sea Ice During the Present Interglacial
Natural variability of the Arctic Ocean sea ice during the present interglacial Anne de Vernala,1, Claude Hillaire-Marcela, Cynthia Le Duca, Philippe Robergea, Camille Bricea, Jens Matthiessenb, Robert F. Spielhagenc, and Ruediger Steinb,d aGeotop-Université du Québec à Montréal, Montréal, QC H3C 3P8, Canada; bGeosciences/Marine Geology, Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, 27568 Bremerhaven, Germany; cOcean Circulation and Climate Dynamics Division, GEOMAR Helmholtz Centre for Ocean Research, 24148 Kiel, Germany; and dMARUM Center for Marine Environmental Sciences and Faculty of Geosciences, University of Bremen, 28334 Bremen, Germany Edited by Thomas M. Cronin, U.S. Geological Survey, Reston, VA, and accepted by Editorial Board Member Jean Jouzel August 26, 2020 (received for review May 6, 2020) The impact of the ongoing anthropogenic warming on the Arctic such an extrapolation. Moreover, the past 1,400 y only encom- Ocean sea ice is ascertained and closely monitored. However, its pass a small fraction of the climate variations that occurred long-term fate remains an open question as its natural variability during the Cenozoic (7, 8), even during the present interglacial, on centennial to millennial timescales is not well documented. i.e., the Holocene (9), which began ∼11,700 y ago. To assess Here, we use marine sedimentary records to reconstruct Arctic Arctic sea-ice instabilities further back in time, the analyses of sea-ice fluctuations. Cores collected along the Lomonosov Ridge sedimentary archives is required but represents a challenge (10, that extends across the Arctic Ocean from northern Greenland to 11). Suitable sedimentary sequences with a reliable chronology the Laptev Sea were radiocarbon dated and analyzed for their and biogenic content allowing oceanographical reconstructions micropaleontological and palynological contents, both bearing in- can be recovered from Arctic Ocean shelves, but they rarely formation on the past sea-ice cover. -
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’). -