Book 31 Oyashio Current.Indb
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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 -
The Mean Flow Field of the Tropical Atlantic Ocean
Deep-Sea Research II 46 (1999) 279—303 The mean flow field of the tropical Atlantic Ocean Lothar Stramma*, Friedrich Schott Institut fu( r Meereskunde, an der Universita( t Kiel, Du( sternbrooker Weg 20, 24105 Kiel, Germany Received 26 August 1997; received in revised form 31 July 1998 Abstract The mean horizontal flow field of the tropical Atlantic Ocean is described between 20°N and 20°S from observations and literature results for three layers of the upper ocean, Tropical Surface Water, Central Water, and Antarctic Intermediate Water. Compared to the subtropical gyres the tropical circulation shows several zonal current and countercurrent bands of smaller meridional and vertical extent. The wind-driven Ekman layer in the upper tens of meters of the ocean masks at some places the flow structure of the Tropical Surface Water layer as is the case for the Angola Gyre in the eastern tropical South Atlantic. Although there are regions with a strong seasonal cycle of the Tropical Surface Water circulation, such as the North Equatorial Countercurrent, large regions of the tropics do not show a significant seasonal cycle. In the Central Water layer below, the eastward North and South Equatorial undercurrents appear imbedded in the westward-flowing South Equatorial Current. The Antarcic Intermediate Water layer contains several zonal current bands south of 3°N, but only weak flow exists north of 3°N. The sparse available data suggest that the Equatorial Intermediate Current as well as the Southern and Northern Intermediate Countercurrents extend zonally across the entire equatorial basin. Due to the convergence of northern and southern water masses, the western tropical Atlantic north of the equator is an important site for the mixture of water masses, but more work is needed to better understand the role of the various zonal under- and countercur- rents in cross-equatorial water mass transfer. -
Oceanographic Structure in the Bering Sea
Title OCEANOGRAPHIC STRUCTURE IN THE BERING SEA Author(s) OHTANI, Kiyotaka Citation MEMOIRS OF THE FACULTY OF FISHERIES HOKKAIDO UNIVERSITY, 21(1), 65-106 Issue Date 1973-10 Doc URL http://hdl.handle.net/2115/21855 Type bulletin (article) File Information 21(1)_P65-106.pdf Instructions for use Hokkaido University Collection of Scholarly and Academic Papers : HUSCAP OCEANOGRAPHIC STRUCTURE IN THE BERING SEA Kiyotaka OHTANI Faculty of Fisherie8, Hokkaido Univer8ity, Hakodate, Japan Contents 1. Introduction ..•••••....•.•.•...•.•••••.....•.••.•.•.•..••......... 65 1. Preface ...................................................... 65 2. Subarctic region ............................................. 66 3. Sources of data . .. 67 4. Bottom configuration ............................................ 68 II. Waters Coming into the Bering Sea from the Pacific Ocean .............. 70 ill. Current Pattern in the Bering Sea . .. 73 IV. Waters in the Bering Sea Basin . .. 76 1. Vertical structure of the basin water ..... .. .. .. .. .. .. .. .. .. ... 76 2. Types of vertical distribution of salinity and temperature .. .. 81 3. Process of formation of various Types .............................. 82 V. Waters on the Continental Shelf ...................................... 85 1. Horizontal distribution of salinity and temperature ............... 85 2. Vertical section ............................................... 91 3. Classification to type of vertical structure ....................... 94 VI. Interaction between the Shelf Waters and the Basin Waters -
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]]. -
191652225.Pdf
Journal of Volcanology and Geothermal Research 296 (2015) 40–54 Contents lists available at ScienceDirect Journal of Volcanology and Geothermal Research journal homepage: www.elsevier.com/locate/jvolgeores Geochemistry and solute fluxes of volcano-hydrothermal systems of Shiashkotan, Kuril Islands Elena Kalacheva a,YuriTaranb,⁎, Tatiana Kotenko a a Institute of Volcanology and Seismology, Russian Academy of Sciences, Petropavlovsk-Kamchatsky 683006, Russia b Institute of Geophysics, Universidad Nacional Autónoma de México, Coyoacán, México D.F., 04510, Mexico article info abstract Article history: Shiashkotan Island belongs to the Northern Kuril island arc and consists of two joined volcanoes, Sinarka and Received 7 December 2014 Kuntomintar, with about 18 km of distance between the summits. Both volcanoes are active, with historic Accepted 13 March 2015 eruptions, and both emit fumarolic gases. Sinarka volcano is degassing through the extrusive dome with inacces- Available online 24 March 2015 sible strong and hot (N400 °C) fumaroles. A large fumarolic field of the Kuntomintar volcano situated in a wide eroded caldera-like crater hosts many fumarolic vents with temperatures from boiling point to 480 °C. Both Keywords: Volcano-hydrothermal systems volcanoes are characterized by intense hydrothermal activity discharging acid SO4-Cl waters, which are drained Shiashkotan, Kuril Islands to the Sea of Okhotsk by streams. At least 4 groups of near-neutral Na-Mg-Ca-Cl-SO4 springs with temperatures in He-C-H-O isotopes the range of 50–80 °C are located at the sea level, within tide zones and discharge slightly altered diluted seawa- Gas and water chemistry ter. Volcanic gas of Kuntomintar as well as all types of hydrothermal manifestations of both volcanoes were col- Solute fluxes, chemical erosion lected and analyzed for major and trace elements and water isotopes. -
Northwest African Upwelling Scenario
OCEANOLOGICA ACTA ⋅ VOL. 24 – Supplement Northwest African upwelling scenario Eberhard HAGEN* Baltic Sea Research Institute, Seestrasse 15, 18119 Warnemuende, Germany Received 24 December 1999; revised 15 May 2000; accepted 16 May 2000 Abstract − Observations, hypotheses and derived scenarios are discussed for the Northwest-African coastal upwelling area. The process of coastal upwelling is considered to be composed of a climatic steady-state part and fluctuations acting on different spatial and temporal scales. Attention is focused on disturbances acting globally on the inter-annual time-scale. El Niño-like changes occur in the system of trade winds and modify the equatorial regime of currents as well as the coastal upwelling regimes on both flanks of the Inter-tropical Convergence Zone. There is an opposite thermal response in near-surface layers along the zonal coast in the Gulf of Guinea and along the meridional coast off NW-Africa. Off the continental slope of Senegal and Mauritania, the poleward undercurrent is linked with the system of eastward flowing equatorial undercurrents via the transport of South Atlantic Central Water (SACW) around the eastern flank of the Guinea Dome. The upwelling undercurrent partly feeds its SACW properties into the belt of coastal upwelling and contributes significantly to the biological productivity during ‘normal’ and ‘abnormal’ upwelling years. Future investigations should focus on changes in the time-scale of decades. © 2001 Ifremer/CNRS/IRD/Éditions scientifiques et médicales Elsevier SAS Résumé − Upwelling au nord-ouest de l‘Afrique. La zone d’upwelling située au nord-ouest des côtes africaines est étudiée dans le cadre d‘une discussion portant sur les observations, les hypothèses et les scénarios qui en dérivent. -
The Issues of War with Japan Coverage in the Presidential Project «Fundamental Multi-Volume Work» the Great Patriotic War of 1941 - 1945 «»
Vyatcheslav Zimonin Captain (Russia NAVY) Doctor of Historical Sciences, Professor of Military University, Honored Scientist Of The Russian Federation and Academy of Natural Sciences The issues of war with Japan coverage in the Presidential project «Fundamental multi-volume work» The Great Patriotic War of 1941 - 1945 «» Fundamental multi-volume work «The Great Patriotic War of 1941-1945» is being developed in accordance with the Decree № 240-рп of May 5, 2008 of the President of the Russian Federation. The work is developed under the organizational leadership of the main drafting committee headed by the Minister of Defense of the Russian Federation Army General Sergey Shoigu. Major General V.A. Zolotarev, well-known Russian scientist, Doctor of Historical and Legal Sciences, Professor, Academician of the Academy of Natural Sciences, State Councilor of the Russian Federation Deputy Chairman of the GRK is appointed as scientific director of the multi-volume work. Fundamental structure of a multivolume work: Volume 1 - «The main facts of the war,» Volume 2 - «The origin and the beginning of the war» Volume 3 - «Battles and actions that changed the course of the war,» Volume 4 - «Freeing of the USSR, 1944 « Volume 5 - «The final victory. Final operations of World War II in Europe. War with Japan « Volume 6 - «The Secret War. Intelligence and counterintelligence in the Great Patriotic War « Volume 7 - «Economy and weapons of war» Volume 8 - «Foreign policy and diplomacy of the Soviet Union during the war» Volume 9 - «Allies of the USSR in the war» Volume 10 - «The power, society and war» Volume 11 - «Policy and Strategy of Victory. -
ATOC 5051: Introduction to Physical Oceanography HW #1: Given Sep 2; Due Sep 16, 2014 Answerkey
ATOC 5051: Introduction to Physical Oceanography HW #1: Given Sep 2; Due Sep 16, 2014 Answerkey Note: you may use any “reliable” resources (peer-reviewed journal articles, books, official websites such as NOAA website, etc.) – in addition to the class materials - to complete this homework. Please list the extra-references (if you have used any) at the end of your homework. 1. Ocean basin and climate (30pts) 1a) Draw a schematic diagram showing the common features of ocean basins; specify the percentage (in volume) that each part roughly occupies. (5pts) Although each ocean basin varies in its location and size, all oceans have common features. They have continental shelf (7.4% of the ocean volume), continental slope, continental rise (slope+rise 15.9%), and abyssal plain (76.7%) with ridges and trenches. See schematic diagram below. Schematic diagram showing the common features of ocean basins. 1b) In which ocean is the thermohaline circulation strong? (2pts) Discuss its basin geometry (including the area, zonal and meridional extent, mean depth) (3pts); Provide a reason for why you think this ocean favors the thermohaline circulation. (2pts) The Atlantic. The Atlantic Ocean has a total meridional extent: It extends from the Arctic to Antarctic. Its zonal largest extent, however, spans little more than 8300km from the Gulf of Mexico to the coast of northwest Africa. It has the largest number of adjacent seas. With all its adjacent seas, Atlantic Ocean covers 106 ×106 km2. Its mean depth is 3300m. 1 The full North-South extent of the Atlantic allows the ocean to extend farther north, where it is cold enough to produce heavier surface water than the subsurface water and thus cause convection and deep- water formation. -
Notes on the Kuril Islands
895 Memni. NOTES ON THE KUKIL ISLANDS. BY CAPTAIN H. J. SNOW, F.R.G.S. LONDON: JOHN MURRAY, ALBEMARLE STREET. 1897. J'l ^"^c^^^n^,^^ ^)4^ ^'<-..^-^yz.rz. J^<=^ ^<^^~?' ; J)3 " NOTES ON THE KUKIL ISLANDS^ BY CAPTAIN H. J. SNOW, F.R.G.S. LONDOK JOHN MUEEAY, ALBEMARLE STREET. 1897. NOTE. By PROFESSOR JOHN MILNE, P.R.S. The only maps in which very many of the places mentioned in the following notes can be found are the Admiralty Charts, numbered 2128 and 240o.* Any one wlio compares these notes and charts, tlie originals of which were drawn by Captain H. J. Snow, with the scanty literature and imperfect maps previously existing, will at once recognize how very much has been accom- plished by the patience and perseverance of an individual. New rocks and shoals have been indicated, whilst supposed dangers of a like character have been removed. The position of islands have been corrected relatively and in longitude, whilst anchorages* tide rips, watering-places, sea-lion and seal rookeries, have been located and described. The shortest route between Vancouver and certain ports on the Asiatic coast has been freed from un- certainties and dangers, while Canadian-Pacific steamers, whalers, and a large fleet of pelagic hunters have now harbours of refuge opened which may be approached with comparative safety. In short, after shipwrecks, risks, and dangers, the escapes from which have often seemed incredible, independently of the geological, natural history, and general scientific notes which have been collected, Captain H. J. Snow, whilst sacrificing by his publica- tions his own professional interests as a hunter, has entitled himself to recognition from all who navigate and patrol the fog-bound shores of the rocky Kurils. -
©Copyright 2011 Stephen Colby Phillips
©Copyright 2011 Stephen Colby Phillips Networked Glass: Lithic Raw Material Consumption and Social Networks in the Kuril Islands, Far Eastern Russia Stephen Colby Phillips A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy University of Washington 2011 Program Authorized to Offer Degree: Anthropology University of Washington Abstract Networked Glass: Lithic Raw Material Consumption and Social Networks in the Kuril Islands, Far Eastern Russia Stephen Colby Phillips Chair of the Supervisory Committee: Associate Professor J. Benjamin Fitzhugh Anthropology This research assesses the effects of environmental conditions on the strategic decisions of low-density foragers in regards to their stone tool raw material procurement and consumption behavior. Social as well as technological adaptations allow human groups to meet the challenges of environments that are circumscribed due to geographic isolation, low biodiversity, and the potential impacts of natural events. Efficient resource management and participation in social networks can be viewed within the framework of human behavioral ecology as optimal forms of behavior aimed at increasing the chances of successful adaptations to dynamic island environments. A lithic resource consumption behavioral model is constructed and predictions derived from the model are tested through the analysis of lithic flake debitage from artifact assemblages representing 2,100 years of human occupation in the Kuril Islands of Far Eastern Russia in the North Pacific Ocean. The relative proportions of debitage across lithic reduction sequence stages provides a measure of lithic reduction intensity, which is compared with the model predictions based on the environmental conditions and local availability of lithic resources in six archaeological sites. -
LA-ICP-MS Analysis of Obsidian Artefacts from the Kurile Islands of the Russian Far East
CHAPTER 7 BRIDGING THE GAP BETWEEN TWO OBSIDIAN SOURCE AREAS IN NORTHEAST ASIA: LA-ICP-MS ANALYSIS OF OBSIDIAN ARTEFACTS FROM THE KURILE ISLANDS OF THE RUSSIAN FAR EAST S. Colby Phillips Abstract: Recent archaeological excavations in the Kurile Islands of the Russian Far East have recovered almost 2000 obsidian artefacts in the form of finished stone tools and flake debitage. While artefacts made of obsidian are present throughout the island chain, obsidian native to the Kurile Islands is not known to have been used prehistorically. An initial source provenance study of Kurile Island artefacts indicated that obsidian raw material was brought into the islands at least 2500 years ago from sources located on the Japanese island of Hokkaido and from the Kamchatka Peninsula (Russian Far East). This chapter reports on a larger provenance study using Laser Ablation Inductively-Coupled-Plasma Mass Spectrometry (LA-ICP-MS) that expands the initial research and provides the largest sample to date of obsidian artefacts from the Kurile Islands that can be assigned to obsidian source groups located in Northeast Asia. Identifying the sources used to produce obsidian artefacts is a key element necessary for reconstructing prehistoric Kurile Island migrations, colonisation events, and social network structures. Keywords: Obsidian, Sourcing, Archaeology, Kurile Islands, Russian Far East, Kamchatka Peninsula, Hokkaido Island Introduction bridge between northern Japan and the northern Russian Far East. The distribution of obsidian from these areas Imported items found in archaeological sites are often seen across the Kuriles has great potential to inform us about as evidence for transport of materials via the movement/ the migration movements and exchange relationships, migration of people or through trade/exchange networks and in turn the larger social organisational structure of the (Pires-Ferreira 1978). -
WILD KAMCHATKA with the KURIL ISLANDS © Sergey Frolov May 20 – June 4, 2020 | 16 Days | Aboard the Caledonian Sky Expedition Highlights
WILD KAMCHATKA WITH THE KURIL ISLANDS © Sergey Frolov May 20 – June 4, 2020 | 16 Days | Aboard the Caledonian Sky Expedition Highlights • Witness huge concentrations of RUSSIA seabirds in a frenzy of breeding KAMCHATKA activity—northern fulmars, horned and PENINSULA SEA OF tufted puffins, guillemots, black-legged OKHOTSK Zhuponova River Petropavlovsk kittiwakes, and more. Russkaya Bay SAKHALIN ISLAND Atlasova Island • Cruise by Zodiac along rocky islets and KURIL ISLANDS uninhabited shores to search for the Tyuleniy Island Srednego Islands Onekotan Island area’s prolific marine and wildlife— Yankicha Island Korsakov Lovyshki Islands including bears, Arctic foxes, seals, and Teuri Island / Rishiri Island Broutona Island/ Chirpoy Island whales. Otaru HOKKAIDO Sapporo • Photograph a variety of stunning PACIFIC OCEAN scenery, from snowcapped volcanoes to JAPAN wildflower-studded tundra. • Enjoy a performance of traditional Russian songs and dances in Sakhalin BLACK-LEGGED SEA OTTER KITTIWAKE Island’s capital, Yuzhno-Sakhalinsk. • Itinerary .................................... page 2 > • Flight Information ...................... page 4 > • Ship, Deck Plan & Rates ............ page 5 > • Featured Leaders ....................... page 6 > • Know Before You Go ................. page 6 > • Optional Pre-voyage Extension ... page 7 > © John Buchanan © Andy Cornelius Andy © HORNED PUFFIN the 1880s, the city became a Japanese prefect capital when Itinerary the southern half of the island was declared a Japanese colony in 1905; after WWII it was returned to Russia. Highlights Based on the expeditionary nature of our trips, there may be ongoing of your exploration include a visit to the Russian Orthodox enhancements to this itinerary. church, the Regional Museum, housed in an impressive former Japanese mansion, and the bustling market. Enjoy a performance of traditional Cossack song and dance from a Wednesday & Thursday, May 20 & 21, 2020 group dressed in colorful costumes.