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PICES Sci. Rep. No. 2, 1995
TABLE OF CONTENTS Page FOREWORD vii Part 1. GENERAL INTRODUCTION AND RECOMMENDATIONS 1.0 RECOMMENDATIONS FOR INTERNATIONAL COOPERATION IN THE OKHOTSK SEA AND KURIL REGION 3 1.1 Okhotsk Sea water mass modification 3 1.1.1Dense shelf water formation in the northwestern Okhotsk Sea 3 1.1.2Soya Current study 4 1.1.3East Sakhalin Current and anticyclonic Kuril Basin flow 4 1.1.4West Kamchatka Current 5 1.1.5Tides and sea level in the Okhotsk Sea 5 1.2 Influence of Okhotsk Sea waters on the subarctic Pacific and Oyashio 6 1.2.1Kuril Island strait transports (Bussol', Kruzenshtern and shallower straits) 6 1.2.2Kuril region currents: the East Kamchatka Current, the Oyashio and large eddies 7 1.2.3NPIW transport and formation rate in the Mixed Water Region 7 1.3 Sea ice analysis and forecasting 8 2.0 PHYSICAL OCEANOGRAPHIC OBSERVATIONS 9 2.1 Hydrographic observations (bottle and CTD) 9 2.2 Direct current observations in the Okhotsk and Kuril region 11 2.3 Sea level measurements 12 2.4 Sea ice observations 12 2.5 Satellite observations 12 Part 2. REVIEW OF OCEANOGRAPHY OF THE OKHOTSK SEA AND OYASHIO REGION 15 1.0 GEOGRAPHY AND PECULIARITIES OF THE OKHOTSK SEA 16 2.0 SEA ICE IN THE OKHOTSK SEA 17 2.1 Sea ice observations in the Okhotsk Sea 17 2.2 Ease of ice formation in the Okhotsk Sea 17 2.3 Seasonal and interannual variations of sea ice extent 19 2.3.1Gross features of the seasonal variation in the Okhotsk Sea 19 2.3.2Sea ice thickness 19 2.3.3Polynyas and open water 19 2.3.4Interannual variability 20 2.4 Sea ice off the coast of Hokkaido 21 -
Of the Inuit Bowhead Knowledge Study Nunavut, Canada
english cover 11/14/01 1:13 PM Page 1 FINAL REPORT OF THE INUIT BOWHEAD KNOWLEDGE STUDY NUNAVUT, CANADA By Inuit Study Participants from: Arctic Bay, Arviat, Cape Dorset, Chesterfield Inlet, Clyde River, Coral Harbour, Grise Fiord, Hall Beach, Igloolik, Iqaluit, Kimmirut, Kugaaruk, Pangnirtung, Pond Inlet, Qikiqtarjuaq, Rankin Inlet, Repulse Bay, and Whale Cove Principal Researchers: Keith Hay (Study Coordinator) and Members of the Inuit Bowhead Knowledge Study Committee: David Aglukark (Chairperson), David Igutsaq, MARCH, 2000 Joannie Ikkidluak, Meeka Mike FINAL REPORT OF THE INUIT BOWHEAD KNOWLEDGE STUDY NUNAVUT, CANADA By Inuit Study Participants from: Arctic Bay, Arviat, Cape Dorset, Chesterfield Inlet, Clyde River, Coral Harbour, Grise Fiord, Hall Beach, Igloolik, Iqaluit, Kimmirut, Kugaaruk, Pangnirtung, Pond Inlet, Qikiqtarjuaq, Rankin Inlet, Nunavut Wildlife Management Board Repulse Bay, and Whale Cove PO Box 1379 Principal Researchers: Iqaluit, Nunavut Keith Hay (Study Coordinator) and X0A 0H0 Members of the Inuit Bowhead Knowledge Study Committee: David Aglukark (Chairperson), David Igutsaq, MARCH, 2000 Joannie Ikkidluak, Meeka Mike Cover photo: Glenn Williams/Ursus Illustration on cover, inside of cover, title page, dedication page, and used as a report motif: “Arvanniaqtut (Whale Hunters)”, sc 1986, Simeonie Kopapik, Cape Dorset Print Collection. ©Nunavut Wildlife Management Board March, 2000 Table of Contents I LIST OF TABLES AND FIGURES . .i II DEDICATION . .ii III ABSTRACT . .iii 1 INTRODUCTION 1 1.1 RATIONALE AND BACKGROUND FOR THE STUDY . .1 1.2 TRADITIONAL ECOLOGICAL KNOWLEDGE AND SCIENCE . .1 2 METHODOLOGY 3 2.1 PLANNING AND DESIGN . .3 2.2 THE STUDY AREA . .4 2.3 INTERVIEW TECHNIQUES AND THE QUESTIONNAIRE . .4 2.4 METHODS OF DATA ANALYSIS . -
The Shantar Tidal Mixing Front
Tidally driven system around the Shantar Islands (the Sea of Okhotsk). I.A. Zhabin V.I.Il'ichev Pacific Oceanological Institute, Vladivostok, RUSSIA PICES-2011, Khabarovsk, Russia The Shantar Islands are located in the southwestern part of the Sea of Okhotsk (Russia, Khabarovsk Region). The Shantar Islands National Park The Shantar Islands area is a unique marine ecosystem that features complex oceanographic processes maintains a high biological diversity of marine life The Sea of Okhotsk is a region of strong tidal currents. According to Kowalik and Polyakov (1998) the major energy sink for diurnal tides is Shelikhov Bay. The major portion of semidiurnal tide energy is dissipated in the southwestern region (Shantar Islands area). The tidal current enhanced over Kashevarov Bank. Vertical stirring assosiated with strong tidal currents is sufficient in some area to mix downward the seasonal buoyancy input and prevent or partly destroy the summer stratification. The boundary between the mixed and stratified waters is delineated by a well defined fronts with sharp change in SST and another properties. The rate of energy dissipation per unit surface in the Okhotsk Sea (erg s-1 cm-2) due to the K1 and M2 tidal components from Kowalik and Polyakov, 1998. The Shantar tidal mixing front The location and seasonal variability of the tidal mixing front (TMF) around the Shantar Islands were studied using satellite and hydrographic data. The Shantar TMF is the dominant feature of the summer hydrographic structure of the southwestern shelf of the Sea of Okhotsk . The mean positions of TMF are compared to the distribution of Simpson and Hunter's (1974) tidal mixing parameter. -
Press Release Neas Awarded New Exclusive Carrier Contracts for Nunavut
PRESS RELEASE NEAS AWARDED NEW EXCLUSIVE CARRIER CONTRACTS FOR NUNAVUT - New for 2019: NEAS is now the Government of Nunavut’s (GN) dedicated carrier for Iqaluit, Cape Dorset, Kimmirut, Pangnirtung, Arctic Bay, Qikiqtarjuaq, Clyde River, Grise Fiord, Pond Inlet, Resolute Bay, Baker Lake, Chesterfield Inlet, Rankin Inlet, Whale Cove, Arviat, Coral Harbour, Kugaaruk, Sanikiluaq, and the Churchill, MB, to Kivalliq service. - Another arctic sealift first for 2019: Kugaaruk customers can now reserve direct with NEAS for the Valleyfield to Kugaaruk service, with no need to reserve through the GN; - “The team at NEAS is thankful for the Government of Nunavut’s vote of confidence in our reliable arctic sealift operations,” said Suzanne Paquin, President and CEO, NEAS Group. “We look forward to delivering our customer service excellence and a better overall customer sealift experience for all peoples, communities, government departments and agencies, stores, construction projects, mines, defence contractors and businesses across Canada’s Eastern and Western Arctic.” IQALUIT, NU, April 25, 2019 – The 2019 Arctic sealift season is underway, and the team of dedicated professionals at the NEAS Group is ready to help you enjoy the most reliable sealift services available across Canada’s Eastern and Western Arctic. New this season, NEAS is pleased to have been awarded the exclusive carrier contracts for the Government of Nunavut including Iqaluit and now Cape Dorset, Kimmirut, Pangnirtung, Arctic Bay, Qikiqtarjuaq, Clyde River, Grise Fiord, Pond Inlet, Resolute Bay, Baker Lake, Chesterfield Inlet, Rankin Inlet, Whale Cove, Arviat, Coral Harbour, Kugaaruk, Sanikiluaq, and the Churchill, MB, to Kivalliq service. No matter where you are across the Canadian Arctic, the NEAS team of dedicated employees and our modern fleet of Inuit-owned Canadian flag vessels is ready to deliver a superior sealift experience for you. -
Naalakkersuisoq Karl-Kristian Kruses Tale Nordatlantisk
Naalakkersuisoq Karl-Kristian Kruses tale Nordatlantisk Fiskeriministerkonference i Shediac 29. august 2017 Dear friends and colleagues I would like to thank our hosts for this chance to visit beautiful New Brunswick and appreciate the hospitality we have been greeted with here. For Greenland, Canada is our closest neighbour and especially with Nunavut, we share a strong sense of culture. We experience similar challenges. We have strong partnerships on many issues as we share a like-minded approach to a safe and sustainable Arctic development with respect for local culture and traditional ways of life. Together Greenland and Nunavut communicate the cultural and social values of the indigenous peoples of the Arctic. Through cooperation we are able to promote greater understanding of the issues that are important to the people of the Arctic. Therefore, it is indeed a pleasure for us to meet with our friends and colleagues here in New Brunswick to talk about measures to protect our Arctic and North Atlantic Oceans. Intro The protection of the marine environment in Greenland falls under the remit of different ministries. The Ministry of Nature and Environment is responsible for the international agreements and conventions regarding biodiversity and overall nature conservation in Greenland, including protection of the marine environment. The Ministry of Fisheries and Hunting is responsible for the management of all living resources. It is therefore essential, when we talk about ocean governance, that we have close cooperation across sectors. It is also essential that we work across borders as we share marine ecosystems and resources among us. What we have done to protect the marine environment We have in Greenland almost 5 % marine protected areas according to IUCN standards. -
Sakhalin Island: Nivkh
70 Chapter 3 Chapter 3 Sakhalin Island: Nivkh The Nivkh (or Gilyak in older literature) have traditionally inhabited the north- ern half of Sakhalin Island and adjacent regions of the mainland. They are relatively homogeneous in the cultural sense; their differences are mainly based on local adaptations to geographic environments, and the two distinct dialects, Sakhalin and mainland, are mutually intelligible. Their ethnic compo- sition is more homogeneous than that of their Tungusic-speaking Amur neigh- bors as it consists of a large core of kin groups of Nivkh origin and a minority of lineages that trace their descent to non-Nivkh ethnic ancestors, mainly those of Amur groups and Ainu. Nivkh culture, with its emphasis on sedentary fishing, is to a large extent analogous to those of their Amur and Ainu neighbors; however, the specialized maritime hunting of the coastal Nivkh was of a significance equal to fishing, and their sea-mammal hunting technology as well as the belief system empha- sizing marine animal cults connect the Nivkh with North Pacific coastal cul- tures of both sides of the Bering Strait, and archaeologically, with the maritime Okhotsk culture of the southern Sea of Okhotsk and the Old Koryak culture of northern Sea of Okhotsk. Other traits that distinguish the traditional Nivkh culture from their neighbors are aspects of their non-material culture such as corpse disposal by cremation and the alliance of three lineage units based on asymmetric connubium that contrasts with the reciprocal connubium charac- teristic for the mainland Tungus society as well as for the Amur ethnic com- plex. -
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. -
Simushir (January 15, 2009) and Samoa (September 30, 2009) Tsunami Recording in the Area of South Kuril Islands
Geophysical Research Abstracts Vol. 12, EGU2010-13331-1, 2010 EGU General Assembly 2010 © Author(s) 2010 Simushir (January 15, 2009) and Samoa (September 30, 2009) tsunami recording in the area of South Kuril Islands Georgy Shevchenko (1), Anton Chernov (1), Peter Kovalev (1), Tatyana Ivelskaya (2), Artem Loskutov (1), and Alexander Shishkin (1) (1) Institute of Marine Geology and Geophysics, Russian Academy of Sciences. Yuzhno-Sakhalinsk, Russia, (2) Sakhalin Tsunami Warning Center, Federal Service of Russia for Hydrometeorology and Environmental Monitoring, Yuzhno-Sakhalinsk, Russia Institute of Marine Geology & Geophysics (the Far East Branch of Russian Academy of Sciences) carried out long wave measurements in the area of South Kuril Islands with the purpose of tsunami recording closely to the seismic active zone and study long wave spectra variability depending of weather conditions. Bottom pressure gauges were installed in several harbors of Shikotan Island, near Cape Lovtsov (north-eastern end of Kunashir Island), in the Kitoviy Bay (Iturup Island) and near Cape Van-der-Lind (Urup Island). Sakhalin Tsunami Center has a cable telemetry tsunami warning station in the Severo-Kurilsk (Paramushir Island). Two tsunamis - a remote Samoa (September 30) and nearby Simushir tsunami (January 15) were recorded by different gauges in the area of South Kuril Islands and by telemetry station in Severo-Kurilsk. To examine spectral properties of long wave oscillations at each gauge, we calculated power spectral estimation using two different data segments (both 1 day length): the period preceding the tsunami event, we identified as “normal” and selected for analysis of the background signal; the “tsunami period” included tsunami caused oscillations. -
Preliminary Mass-Balance Food Web Model of the Eastern Chukchi Sea
NOAA Technical Memorandum NMFS-AFSC-262 Preliminary Mass-balance Food Web Model of the Eastern Chukchi Sea by G. A. Whitehouse U.S. DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Administration National Marine Fisheries Service Alaska Fisheries Science Center December 2013 NOAA Technical Memorandum NMFS The National Marine Fisheries Service's Alaska Fisheries Science Center uses the NOAA Technical Memorandum series to issue informal scientific and technical publications when complete formal review and editorial processing are not appropriate or feasible. Documents within this series reflect sound professional work and may be referenced in the formal scientific and technical literature. The NMFS-AFSC Technical Memorandum series of the Alaska Fisheries Science Center continues the NMFS-F/NWC series established in 1970 by the Northwest Fisheries Center. The NMFS-NWFSC series is currently used by the Northwest Fisheries Science Center. This document should be cited as follows: Whitehouse, G. A. 2013. A preliminary mass-balance food web model of the eastern Chukchi Sea. U.S. Dep. Commer., NOAA Tech. Memo. NMFS-AFSC-262, 162 p. Reference in this document to trade names does not imply endorsement by the National Marine Fisheries Service, NOAA. NOAA Technical Memorandum NMFS-AFSC-262 Preliminary Mass-balance Food Web Model of the Eastern Chukchi Sea by G. A. Whitehouse1,2 1Alaska Fisheries Science Center 7600 Sand Point Way N.E. Seattle WA 98115 2Joint Institute for the Study of the Atmosphere and Ocean University of Washington Box 354925 Seattle WA 98195 www.afsc.noaa.gov U.S. DEPARTMENT OF COMMERCE Penny. S. Pritzker, Secretary National Oceanic and Atmospheric Administration Kathryn D. -
Proceedings Template
Canadian Science Advisory Secretariat (CSAS) Research Document 2020/032 Central and Arctic Region Ecological and Biophysical Overview of the Southampton Island Ecologically and Biologically Significant Area in support of the identification of an Area of Interest T.N. Loewen1, C.A. Hornby1, M. Johnson2, C. Chambers2, K. Dawson2, D. MacDonell2, W. Bernhardt2, R. Gnanapragasam2, M. Pierrejean4 and E. Choy3 1Freshwater Institute Fisheries and Oceans Canada 501 University Crescent Winnipeg, MB R3T 2N6 2North/South Consulting Ltd. 83 Scurfield Blvd, Winnipeg, MB R3Y 1G4 3McGill University. 845 Sherbrooke Rue, Montreal, QC H3A 0G4 4Laval University Pavillon Alexandre-Vachon 1045, , av. of Medicine Quebec City, QC G1V 0A6 July 2020 Foreword This series documents the scientific basis for the evaluation of aquatic resources and ecosystems in Canada. As such, it addresses the issues of the day in the time frames required and the documents it contains are not intended as definitive statements on the subjects addressed but rather as progress reports on ongoing investigations. Published by: Fisheries and Oceans Canada Canadian Science Advisory Secretariat 200 Kent Street Ottawa ON K1A 0E6 http://www.dfo-mpo.gc.ca/csas-sccs/ [email protected] © Her Majesty the Queen in Right of Canada, 2020 ISSN 1919-5044 Correct citation for this publication: Loewen, T. N., Hornby, C.A., Johnson, M., Chambers, C., Dawson, K., MacDonell, D., Bernhardt, W., Gnanapragasam, R., Pierrejean, M., and Choy, E. 2020. Ecological and Biophysical Overview of the Southampton proposed Area of Interest for the Southampton Island Ecologically and Biologically Significant Area. DFO Can. Sci. Advis. Sec. Res. -
Acoustic Monitoring of Beluga Whales (Delphinapterus Leucas): Spatio-Temporal Habitat
Acoustic monitoring of beluga whales (Delphinapterus leucas): spatio-temporal habitat preference and geographic variation in Canadian populations By Karyn Victoria Booy A Thesis submitted to the Faculty of Graduate Studies of The University of Manitoba in partial fulfillment of the requirements of the degree of MASTER OF SCIENCE Department of Biological Sciences University of Manitoba Winnipeg. Manitoba, Canada JUNE, 2018 Copyright © 2018 by Karyn Booy Abstract Acoustic monitoring is an effective means by which to study cetaceans, such as beluga whales (Delphinapterus leucas), and can be useful in determining habitat preference and geographic variation among populations. Acoustic monitoring data were analyzed using a combination of automated detection and manual analysis to determine habitat preference of Cumberland Sound beluga in their summering range. Belugas were primarily detected in the northernmost site in Clearwater Fiord, with diel variation in call patterns at two separate sites in different years. No correlation was evident between tidal cycles and beluga detections. A second study examined geographic variation in simple contact calls (SCC’s) among four Canadian beluga populations. Results indicate variation in the measured parameters (duration, peak frequency and pulse repetition rate) among four populations and align with genetic variation previously described in the literature. These findings provide important information necessary for the conservation and management of beluga populations in Canada. i Acknowledgements I thank my supervisor Dr. Marianne Marcoux for her guidance and support throughout this project. You have been a fantastic mentor throughout this process and I could not have completed this project without your patient tutorials in both statistical and acoustic analyses. -
Arctic Marine Transport Workshop 28-30 September 2004
Arctic Marine Transport Workshop 28-30 September 2004 Institute of the North • U.S. Arctic Research Commission • International Arctic Science Committee Arctic Ocean Marine Routes This map is a general portrayal of the major Arctic marine routes shown from the perspective of Bering Strait looking northward. The official Northern Sea Route encompasses all routes across the Russian Arctic coastal seas from Kara Gate (at the southern tip of Novaya Zemlya) to Bering Strait. The Northwest Passage is the name given to the marine routes between the Atlantic and Pacific oceans along the northern coast of North America that span the straits and sounds of the Canadian Arctic Archipelago. Three historic polar voyages in the Central Arctic Ocean are indicated: the first surface shop voyage to the North Pole by the Soviet nuclear icebreaker Arktika in August 1977; the tourist voyage of the Soviet nuclear icebreaker Sovetsky Soyuz across the Arctic Ocean in August 1991; and, the historic scientific (Arctic) transect by the polar icebreakers Polar Sea (U.S.) and Louis S. St-Laurent (Canada) during July and August 1994. Shown is the ice edge for 16 September 2004 (near the minimum extent of Arctic sea ice for 2004) as determined by satellite passive microwave sensors. Noted are ice-free coastal seas along the entire Russian Arctic and a large, ice-free area that extends 300 nautical miles north of the Alaskan coast. The ice edge is also shown to have retreated to a position north of Svalbard. The front cover shows the summer minimum extent of Arctic sea ice on 16 September 2002.