Expedition to the Shantar Islands
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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 -
256 P111. the Influence of Sea Ice on the Sea Coast Of
EMECS 11 – Sea Coasts XXVI, August 22-27, 2016, St Petersburg, Russia P111. THE INFLUENCE OF SEA ICE ON THE SEA COAST OF SHANTAR ISLANDS Margarita Illarionova1 1Far Eastern Federal University (FEFU), Russia [email protected] The Shantar Islands is the group of islands satiated in the Sea of Okhotsk near the exit of Uda Bay, Tugur Bay and Ulban Bay. The islands separated from the mainland and started to exist only 6000 years ago. It happened under the influence of the sea transgression followed by flooding of some parts of the land surface and isolation of the most elevated mountain parts from the mainland. The climate of The Shantar Island is more severe than the climate in the North part of the Sea of Okhotsk due to its proximity to cold regions of Yakutia, complex system of wind and tidal currents, the duration of the ice period, loads of fog and frequent storm winds. The height of tides on the islands can reach 8 meters, and these tidal currents are considered as one of the fastest tides of the World Ocean. The ice near the islands appears in the beginning of November and doesn’t melt for 8-9 months, usually, till mid-July, but some years - till mid-August. Such severe ice conditions cannot be observed anywhere else in the Sea of Okhotsk. The variety of forms of the Shantar Islands is a consequence of severe ice conditions, unusual tidal currents and irregularity of the seashore. The most important seashores forming factor is considered to be the activity of sea ice. -
Abstract Book.Pdf
Executive Committee Motoyuki Suzuki, International EMECS Center, Japan Toshizo Ido, International EMECS Center, Governor of Hyogo Prefecture, Japan Leonid Zhindarev, Working Group “Sea Coasts” RAS, Russia Valery Mikheev, Russian State Hydrometeorological University, Russia Masataka Watanabe, International EMECS Center, Japan Robert Nigmatullin, P.P. Shirshov Institute of Oceanology RAS, Russia Oleg Petrov, A.P. Karpinsky Russian Geological Research Institute, Russia Scientific Programme Committee Ruben Kosyan, Southern Branch of the P.P. Shirshov Institute of Oceanology RAS, Russia – Chair Masataka Watanabe, Chuo University, International EMECS Center, Japan – Co-Chair Petr Brovko, Far Eastern Federal University, Russia Zhongyuan Chen, East China Normal University, China Jean-Paul Ducrotoy, Institute of Estuarine and Coastal Studies, University of Hull, France George Gogoberidze, Russian State Hydrometeorological University, Russia Sergey Dobrolyubov, Academic Council of the Russian Geographical Society, M.V. Lomonosov Moscow State University, Russia Evgeny Ignatov, M.V. Lomonosov Moscow State University, Russia Nikolay Kasimov, Russian Geographical Society, Technological platform “Technologies for Sustainable Ecological Development” Igor Leontyev, P.P. Shirshov Institute of Oceanology RAS, Russia Svetlana Lukyanova, M.V. Lomonosov Moscow State University, Russia Menasveta Piamsak, Royal Institute, Thailand Erdal Ozhan, MEDCOAST Foundation, Turkey Daria Ryabchuk, A.P. Karpinsky Russian Geological Research Institute, Russia Mikhail Spiridonov, -
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. -
University of Copenhagen
Organ system development in recent lecithotrophic brachiopod larvae Altenburger, Andreas; Martinez, Pedro; Wanninger, Andreas Wilhelm Georg Published in: Geological Society of Australia. Abstracts Series Publication date: 2010 Document version Publisher's PDF, also known as Version of record Citation for published version (APA): Altenburger, A., Martinez, P., & Wanninger, A. W. G. (2010). Organ system development in recent lecithotrophic brachiopod larvae. Geological Society of Australia. Abstracts Series, 3-3. http://www.deakin.edu.au/conferences/ibc/spaw2/uploads/files/6IBC_Program%20&%20Abstracts%20volume.p df Download date: 25. Sep. 2021 Geological Society of Australia ABSTRACTS Number 95 6th International Brachiopod Congress Melbourne, Australia 1-5 February 2010 Geological Society of Australia, Abstracts No. 95 6th International Brachiopod Congress, Melbourne, Australia, February 2010 Geological Society of Australia, Abstracts No. 95 6th International Brachiopod Congress, Melbourne, Australia, February 2010 Geological Society of Australia Abstracts Number 95 6th International Brachiopod Congress, Melbourne, Australia, 1‐5 February 2010 Editors: Guang R. Shi, Ian G. Percival, Roger R. Pierson & Elizabeth A. Weldon ISSN 0729 011X © Geological Society of Australia Incorporated 2010 Recommended citation for this volume: Shi, G.R., Percival, I.G., Pierson, R.R. & Weldon, E.A. (editors). Program & Abstracts, 6th International Brachiopod Congress, 1‐5 February 2010, Melbourne, Australia. Geological Society of Australia Abstracts No. 95. Example citation for papers in this volume: Weldon, E.A. & Shi, G.R., 2010. Brachiopods from the Broughton Formation: useful taxa for the provincial and global correlations of the Guadalupian of the southern Sydney Basin, eastern Australia. In: Program & Abstracts, 6th International Brachiopod Congress, 1‐5 February 2010, Melbourne, Australia; Geological Society of Australia Abstracts 95, 122. -
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. -
Of the Shantar Islands (Khabarovsk Krai, Russia)
Ecologica Montenegrina 34: 43-48 (2020) This journal is available online at: www.biotaxa.org/em http://dx.doi.org/10.37828/em.2020.34.5 Longicorn beetles (Coleoptera, Cerambycidae) of the Shantar Islands (Khabarovsk Krai, Russia) NIKOLAY S. ANISIMOV1* & VITALY G. BEZBORODOV2 1All-Russian Scientific Research Institute of Soybean, Ignatevskoye Shosse 19, Blagoveshchensk 675027 Russia. 2Amur Branch of the Botanical Garden-Institute FEB RAS, Ignatevskoye Shosse 2-d km, Blagoveshchensk 675000 Russia. *Corresponding Author: e-mail: [email protected] Received: 25 July 2020│ Accepted by V. Pešić: 30 August 2020 │ Published online: 7 September 2020. The Shantar Islands are located in the western part of the Sea of Okhotsk, near the eastern coast of Eurasia. They are administratively included in the Tuguro-Chumikansky district of Khabarovsk Krai of Russia. The archipelago consists of 15 large and small islands, the largest of which is the Bоlshoy Shantar.The total area of the islands is 550 thousand hectares. The entire archipelago has the status of the National Park. The islands are dominated by mountainous relief with river valleys. Heights are up to 721 m. The climate is temperate monsoon with excessive summer moisture. Strong northwest winds prevail, they delay the phenological cycles of biota by 1-1,5 months in comparison with the nearest mainland areas. The boreal component of the middle taiga subzone dominates in the flora of the archipelago. Nemoral flora is represented by single species in phytocenoses of deep valleys of the large islands (Nechaev, 1955). There are two altitudinal vegetation belts in the Shantar Islands – mountain taiga belt and subalpine altitudinal belt (mountain tundra occupies 2% of the territory). -
Newell, J. 2004. the Russian Far East
Industrial pollution in the Komsomolsky, Solnechny, and Amursky regions, and in the city of Khabarovsk and its Table 3.1 suburbs, is excessive. Atmospheric pollution has been increas- Protected areas in Khabarovsk Krai ing for decades, with large quantities of methyl mercaptan in Amursk, formaldehyde, sulfur dioxide, phenols, lead, and Type and name Size (ha) Raion Established benzopyrene in Khabarovsk and Komsomolsk-on-Amur, and Zapovedniks dust prevalent in Solnechny, Urgal, Chegdomyn, Komso- molsk-on-Amur, and Khabarovsk. Dzhugdzhursky 860,000 Ayano-Maysky 1990 Between 1990 and 1999, industries in Komsomolsky and Bureinsky 359,000 Verkhne-Bureinsky 1987 Amursky Raions were the worst polluters of the Amur River. Botchinsky 267,400 Sovetsko-Gavansky 1994 High concentrations of heavy metals, copper (38–49 mpc), Bolonsky 103,600 Amursky, Nanaisky 1997 KHABAROVSK zinc (22 mpc), and chloroprene (2 mpc) were found. Indus- trial and agricultural facilities that treat 40 percent or less of Komsomolsky 61,200 Komsomolsky 1963 their wastewater (some treat none) create a water defi cit for Bolshekhekhtsirsky 44,900 Khabarovsky 1963 people and industry, despite the seeming abundance of water. The problem is exacerbated because of: Federal Zakazniks Ⅲ Pollution and low water levels in smaller rivers, particular- Badzhalsky 275,000 Solnechny 1973 ly near industrial centers (e.g., Solnechny and the Silinka River, where heavy metal levels exceed 130 mpc). Oldzhikhansky 159,700 Poliny Osipenko 1969 Ⅲ A loss of soil fertility. Tumninsky 143,100 Vaninsky 1967 Ⅲ Fires and logging, which impair the forests. Udylsky 100,400 Ulchsky 1988 Ⅲ Intensive development and quarrying of mineral resourc- Khekhtsirsky 56,000 Khabarovsky 1959 es, primarily construction materials. -
Research of Natural Renewable Energy Resources of Coasts And
ISES Solar World Congress 2017 IEA SHC International Conference on Solar Heating and Cooling for Buildings and Industry Research of Natural Renewable Energy Resources of Coast and Seas of the Far East Valeriy V. Knyazhev and Vladimir V. Loshchenkov Institute of Marine Technology Problems FEB RAS, Vladivostok (Russia) Abstract In article renewed energy sources on Far East of Russia are considered: thermal energy, energy of salinity gradients, tide, waves, currents, a wind and solar power. Estimations of power resources of these energy sources are given. Places in which they are offered can are effectively used. A system of autonomous power supply for a coastal facility for the cultivation of hydrobionts from renewable sources on the island of Popov is proposed. A device for growing hydrobionts on artificial automated plantations in the water column without diving with an autonomous power supply from renewable sources has been developed.. Keywords: source of energy, thermal, salinity, tide, wave, current, wind, solar, hydrobionts 1. Introduction The Far East of Russia is the region of Russia where the primary start of development and use of ocean energy sources is possible, this is facilitated by the fact that the Far East has a long coastline and most of the territory of the Far East is not connected to the unified energy system. And as the population density in these territories is small, it is economically justified to use autonomous energy sources, and, first of all, renewable energy sources of the ocean. The territory of the Far East stretching from the south to the north of 4500 km, more than 70% of the length of its borders falls on the shorelines of the seas of the Arctic and Pacific Oceans, covers different natural areas, and almost everywhere the potential of renewable energy sources is very high. -
Some Features of Biology of the Siberian Taimen Hucho Taimen (Pallas, 1773) (Salmonidae) from the Tugur River Basin S
ISSN 0032-9452, Journal of Ichthyology, 2018, Vol. 58, No. 5, pp. 765–768. © Pleiades Publishing, Ltd., 2018. Original Russian Text © S.E. Kul’bachnyi, A.V. Kul’bachnaya, 2018, published in Voprosy Ikhtiologii, 2018, Vol. 58, No. 5, pp. 629–632. SHORT COMMUNICATIONS Some Features of Biology of the Siberian Taimen Hucho taimen (Pallas, 1773) (Salmonidae) from the Tugur River Basin S. E. Kul’bachnyi* and A. V. Kul’bachnaya Pacific Research Fisheries Center, Khabarovsk Branch, Khabarovsk, 680000 Russia *e-mail: [email protected] Received January 30, 2017 Abstract—Data on the size-age and sex structure, as well as the magnitude, of Siberian taimen Hucho taimen population from the Tugur River Basin are presented. Keywords: Siberian taimen Hucho taimen, length, age, Tugur River Basin DOI: 10.1134/S0032945218050120 INTRODUCTION northwest in some rivers facing the mouth of the Amur River. It also occurs in lakes. It is a large fish reaching At present, sport fishing is of considerable interest 80 kg (Berg, 1948; Nikolskii, 1956; Zolotukhin et al., and there are great prospects for fishing tourism. This 2000). Lindbergh and Dulkate (1929) noted that tai- also applies to the northeastern region of Russia, men with a weight of up to 95 kg was captured in the where a number of attractive fish species live. This is Uda River. Taimen becomes sexually mature at the age especially the case for the Siberian taimen Hucho tai- of 4+ after reaching a length of 40–50 cm. Sex ratio is men. A sharp increase in the fishing load on the taimen close to 1 : 1. -
Stopping the Use, Sale and Trade of Whales and Dolphins in Canada How Protection Is Consistent with WTO Obligations
Stopping the use, sale and trade of whales and dolphins in Canada How protection is consistent with WTO obligations Prepared by Leesteffy Jenkins, Attorney at Law 219 West Main St., P.O. Box 634 Hillsborough, NH 03244-0634 Phone (603) 464-4395 For ZOOCHECK CANADA INC. 3266 Yonge Street, Suite 1417 Toronto, Ontario M4N 3P6 (416) 285-1744 (p) (416) 285-4670 (f ) [email protected] www.zoocheck.com This legal analysis was commissioned by Zoocheck Canada as part of a research initiative looking into how trade laws impact the trade and use of whales and dolphins in Canada, and to educate the public about the same. Page 1 April 25, 2003 QUESTION PRESENTED Whether a Canadian ban on the import and export of live cetaceans, wild-caught, captive born or those caught earlier in the wild and now considered captive, would violate Canada's obligations pursuant to the World Trade Organization (WTO) Agreements. CONCLUSION It is my understanding that there is currently no specific Canadian legislation banning the import/export of live cetaceans. Based on the facts* presented to me, however, it is my opinion that such legislation could be enacted consistent with WTO rules. This memorandum attempts to outline both the conditions under which Canadian regulation of trade in live cetaceans may be consistent with the WTO Agreements, as well as provide some guidance in the crafting of future legislation. PEER REVIEW & COMMENTS Chris Wold, Steve Shrybman, Esq Clinical Professor of Law and Director Sack, Goldblatt, Mitchell International Environmental Law Project 20 Dundas Street West, Ste 1130 Northwestern School of Law Toronto, Ontario M5G 2G8 Lewis and Clark College Tel.: (416) 979-2235 10015 SW Terwilliger Blvd Email: [email protected] Portland, Oregon, U.S.A. -
Annual Report 2017
Annual Report 2017 Nansen International Environmental and Remote Sensing Centre St. Petersburg, Russia Non-profit international centre for environmental and climate research Founded in 1992 Founders of the Nansen Centre REPORT FROM THE GENERAL Bergen University Research Foundation (UNIFOB) Bergen, Norway MEETING OF FOUNDERS Max-Planck Society (MPS) Munich, Germany Nansen Environmental and Remote Sensing Centre (NERSC) Vision Bergen, Norway Northern Water Problems Institute of Russian Academy of Sciences (NWPI RAS) The Scientific Foundation “Nansen International Environ- Petrozavodsk, Republic of Karelia, Russia mental and Remote Sensing Centre” (Nansen Centre, Saint-Petersburg State University (SPbSU) Saint-Petersburg, Russia NIERSC) vision is to understand, monitor and predict Scientific Research Centre for Ecological Safety of RAS (SRCES RAS) climate and environmental changes in the high northern Saint-Petersburg, Russia latitudes for serving the Society. With the initial support from The Joint Research Centre of the European Commission (JRC EC) Major Research Areas Associate Partners of the Nansen Centre DLR Maritime Security Lab (DLR MSL) Climate Variability and Change in High Northern Latitudes Bremen, Germany Finnish Meteorological Institute (FMI) Aquatic Ecosystems in Response to Global Change Helsinki, Finland Global Climate Forum (GCF) Applied Meteorological and Oceanographic Research for Berlin, Germany Industrial Activities Helsinki University (HU) Helsinki, Finland Socioeconomic Impact of Climate Change Nansen Scientific Society