Iturup Island Pink and Chum Salmon Fishery
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30-Year Lidar Observations of the Stratospheric Aerosol Layer State Over Tomsk (Western Siberia, Russia) Vladimir V
Atmos. Chem. Phys. Discuss., doi:10.5194/acp-2016-792, 2016 Manuscript under review for journal Atmos. Chem. Phys. Published: 13 October 2016 c Author(s) 2016. CC-BY 3.0 License. 30-year lidar observations of the stratospheric aerosol layer state over Tomsk (Western Siberia, Russia) Vladimir V. Zuev1,2,3, Vladimir D. Burlakov4, Aleksei V. Nevzorov4, Vladimir L. Pravdin1, Ekaterina S. Savelieva1, and Vladislav V. Gerasimov1,2 5 1Institute of Monitoring of Climatic and Ecological Systems SB RAS, Tomsk, 634055, Russia 2Tomsk State University, Tomsk, 634050, Russia 3Tomsk Polytechnic University, Tomsk, 634050, Russia 4V.E. Zuev Institute of Atmospheric Optics SB RAS, Tomsk, 634055, Russia Correspondence to: Vladislav V. Gerasimov ([email protected]) 10 Abstract. There are only four lidar stations in the world, which have almost continuously performed observations of the stratospheric aerosol layer (SAL) state for over the last 30 years. The longest time series of the SAL lidar measurements have been accumulated at the Mauna Loa Observatory (Hawaii) since 1973, the NASA Langley Research Center (Hampton, Virginia) since 1974, and Garmisch-Partenkirchen (Germany) since 1976. The fourth lidar station we present started to perform routine observations of the SAL parameters in Tomsk (56.48 N, 85.05 E, Western Siberia, Russia) in 1986. In this 15 paper, we mainly focus on and discuss the stratospheric background period from 2000 to 2005 and the causes of the SAL perturbations over Tomsk in the 2006–2015 period. During the last decade, volcanic aerosol plumes from tropical Mt. Manam, Soufriere Hills, Rabaul, Merapi, Nabro, and Kelut, and extratropical (northern) Mt. -
Russia by Robert W
Russia by Robert W. Orttung Capital: Moscow Population: 142.2 million GNI/capita: US$12,740 The social data above was taken from the European Bank for Reconstruction and Development’s Transition Report 2007: People in Transition, and the economic data from the World Bank’s World Development Indicators 2008. Nations in Transit Ratings and Averaged Scores 1999 2001 2002 2003 2004 2005 2006 2007 2008 Electoral Process 4.00 4.25 4.50 4.75 5.50 6.00 6.25 6.50 6.75 Civil Society 3.75 4.00 4.00 4.25 4.50 4.75 5.00 5.25 5.50 Independent Media 4.75 5.25 5.50 5.50 5.75 6.00 6.00 6.25 6.25 Governance* 4.50 5.00 5.25 5.00 5.25 n/a n/a n/a n/a National Democratic 6.25 Governance n/a n/a n/a n/a n/a 5.75 6.00 6.00 Local Democratic 5.75 Governance n/a n/a n/a n/a n/a 5.75 5.75 5.75 Judicial Framework 5.25 and Independence 4.25 4.50 4.75 4.50 4.75 5.25 5.25 5.25 Corruption 6.25 6.25 6.00 5.75 5.75 5.75 6.00 6.00 6.00 Democracy Score 4.58 4.88 5.00 4.96 5.25 5.61 5.75 5.86 5.96 * With the 2005 edition, Freedom House introduced separate analysis and ratings for national democratic governance and local democratic governance to provide readers with more detailed and nuanced analysis of these two important subjects. -
USGS Open-File Report 2009-1133, V. 1.2, Table 3
Table 3. (following pages). Spreadsheet of volcanoes of the world with eruption type assignments for each volcano. [Columns are as follows: A, Catalog of Active Volcanoes of the World (CAVW) volcano identification number; E, volcano name; F, country in which the volcano resides; H, volcano latitude; I, position north or south of the equator (N, north, S, south); K, volcano longitude; L, position east or west of the Greenwich Meridian (E, east, W, west); M, volcano elevation in meters above mean sea level; N, volcano type as defined in the Smithsonian database (Siebert and Simkin, 2002-9); P, eruption type for eruption source parameter assignment, as described in this document. An Excel spreadsheet of this table accompanies this document.] Volcanoes of the World with ESP, v 1.2.xls AE FHIKLMNP 1 NUMBER NAME LOCATION LATITUDE NS LONGITUDE EW ELEV TYPE ERUPTION TYPE 2 0100-01- West Eifel Volc Field Germany 50.17 N 6.85 E 600 Maars S0 3 0100-02- Chaîne des Puys France 45.775 N 2.97 E 1464 Cinder cones M0 4 0100-03- Olot Volc Field Spain 42.17 N 2.53 E 893 Pyroclastic cones M0 5 0100-04- Calatrava Volc Field Spain 38.87 N 4.02 W 1117 Pyroclastic cones M0 6 0101-001 Larderello Italy 43.25 N 10.87 E 500 Explosion craters S0 7 0101-003 Vulsini Italy 42.60 N 11.93 E 800 Caldera S0 8 0101-004 Alban Hills Italy 41.73 N 12.70 E 949 Caldera S0 9 0101-01= Campi Flegrei Italy 40.827 N 14.139 E 458 Caldera S0 10 0101-02= Vesuvius Italy 40.821 N 14.426 E 1281 Somma volcano S2 11 0101-03= Ischia Italy 40.73 N 13.897 E 789 Complex volcano S0 12 0101-041 -
Articles Into the Strato- for Example (Mills Et Al., 2016)
Atmos. Chem. Phys., 17, 3067–3081, 2017 www.atmos-chem-phys.net/17/3067/2017/ doi:10.5194/acp-17-3067-2017 © Author(s) 2017. CC Attribution 3.0 License. 30-year lidar observations of the stratospheric aerosol layer state over Tomsk (Western Siberia, Russia) Vladimir V. Zuev1,2,3, Vladimir D. Burlakov4, Aleksei V. Nevzorov4, Vladimir L. Pravdin1, Ekaterina S. Savelieva1, and Vladislav V. Gerasimov1,2 1Institute of Monitoring of Climatic and Ecological Systems SB RAS, Tomsk, 634055, Russia 2Tomsk State University, Tomsk, 634050, Russia 3Tomsk Polytechnic University, Tomsk, 634050, Russia 4V.E. Zuev Institute of Atmospheric Optics SB RAS, Tomsk, 634055, Russia Correspondence to: Vladislav V. Gerasimov ([email protected]) Received: 1 September 2016 – Discussion started: 13 October 2016 Revised: 20 January 2017 – Accepted: 5 February 2017 – Published: 28 February 2017 Abstract. There are only four lidar stations in the world role of both tropical and northern volcanic eruptions in vol- which have almost continuously performed observations of canogenic aerosol loading of the midlatitude stratosphere is the stratospheric aerosol layer (SAL) state over the last also discussed. In addition to volcanoes, we considered other 30 years. The longest time series of the SAL lidar mea- possible causes of the SAL perturbations over Tomsk, i.e., surements have been accumulated at the Mauna Loa Obser- the polar stratospheric cloud (PSC) events and smoke plumes vatory (Hawaii) since 1973, the NASA Langley Research from strong forest fires. At least two PSC events were de- Center (Hampton, Virginia) since 1974, and Garmisch- tected in 1995 and 2007. We also make an assumption that Partenkirchen (Germany) since 1976. -
All Sides Claim Victory in 1996 Gubernatorial Elections
ALL SIDES CLAIM VICTORY IN 1996 GUBERNATORIAL ELECTIONS Although they did not receive nearly as much international attention as the July presidential election, the 48 Russian regional elections held between 1 September and 5 January were closely watched by Russian politicians and commentators. Gubernatorial elections were held in 45 oblasts, krais, and autonomous okrugs, forcing leaders appointed by President Boris Yeltsin to face the voters. Three ethnic republics also elected top executives. Both the Kremlin and opposition leaders have portrayed the elections as a success, but many new governors have pledged to use their mandates to benefit their own regions, and it is difficult to predict where their primary loyalties will lie. Who are the new governors? Of the 48 incumbent regional leaders who faced elections in 1996, 20 held on to their jobs and 24 were defeated. Another three continue to serve pending repeat elections in their regions, and Tyumen Governor Leonid Roketskii will contest a runoff on 12 January. (A complete list of election results is attached to this issue of the Russian Regional Report.) Fifteen of the 24 new governors were elected mainly with the backing of the Communist Party of the Russian Federation (KPRF) and its left-wing umbrella movement, the Popular-Patriotic Union of Russia (NPSR). Of the successful Communist-backed candidates, seven were chairmen of regional or local legislatures immediately before being elected governor (Krasnodar and Altai krais and Voronezh, Volgograd, Kaluga, Vladimir, and Kurgan oblasts). Four others were State Duma deputies (Kirov, Bryansk, and Chelyabinsk oblasts and Stavropol Krai), and one (Ryazan) worked in the parliament's Audit Chamber. -
Defense Security Brief
VOLUME 9 ISSUE 2 DEFENSE SECURITY BRIEF December 2020 Back to the Future: The Race for AI and National 1 Security Implications for Taiwan Tony Tai-Ting Liu The Legal Status of Unmanned Underwater 14 Vehicles and the Implications of China’s Development of UUVs Chiwen Ku and Yucheng Chen An Emerging Island Chain within the Island Chains 27 Jung-Ming Chang Futile Efforts: Abe’s Northern Territory Policy 38 Che-Jen Wang Institute for National Defense and Stuck in the Middle with You: Israel’s Geopolitical 54 Dance with Washington and Beijing Security Research Mor Sobol The Logic of the Strategic Thinking and Defensive 70 Measures of the Overall Defensive Concept of Taiwan Hsinbiao Jiang ISSN 2225360-2 INDSR The Institute for National Defense and Security Research (INDSR) is dedicated to fueling knowledge-based policy analyses and strategic assessments on Taiwan’s security. Our mission is to safeguard Taiwan’s democracy and prosperity by strengthening mutual understanding and advancing common interests in the defense and security community both globally and at home. INDSR was formally inaugurated on May 1, 2018, and is headquartered in Taipei, Taiwan. We are an independent, nonpartisan, nonprofit organization. To bring together great minds in policymaking, industry and research, we convene international forums, network civil societies, engage in Track Two dialogue and conduct wargame simulations. INDSR’s dynamic research agenda and activities are used to develop pragmatic policy recommendations for the Taiwan government. LEADERSHIP Shoou-Yeh Huoh (Chairman) Chen-Wei Lin (President) Si-Fu Ou (Acting Vice President) DEFENSE SECURITY BRIEF Defense Security Brief (DSB) is an English-language publication aimed at strengthening research exchanges with security-related experts both domestically and abroad. -
Newell, J. 2004. the Russian Far East: a Reference Guide for Conservation and Development
Appendix A Major topological features in the RFE Size Maximum Elevation (m Last Seas (000 sq. km) depth (m) Active volcanoes Location above sea level) eruption Beringovo (Bering Sea) 2,315 5,500 Kamchatka Okhotskoe (Sea of Okhotsk) 1,603 3,521 Klyuchevskoi Vostochny Yaponskoe (Sea of Japan) 1,602 3,720 (Eastern) Range 4,800 ongoing Vostochno-Sibirskoe (East Siberian Sea) 913 915 Tolbachik Vostochny Range 3,682 1976 Laptevykh (Laptev Sea) 662 3,385 Ichinsky Sredinny (Central) Range 3,621 unknown Chukotskoe (Chukchi Sea) 595 1,256 Kronotsky Gamchen Ridge 3,528 1923 Koryaksky Vostochny Range 3,456 1957 Length Basin size Shiveluch Vostochny Range 3,283 2001 Rivers and tributaries (km) (000 sq. km) Bezymyanny Vostochny Range 3,085 1998 Zhupanovsky Vostochny Range 2,927 1956 Amur (with Argun) 4,444 1,855 Avacha Vostochny Range 2,750 1991 Lena 4,400 2,490 Mutnovsky Vostochny Range 2,323 1999 Olenyok 2,270 219 Maly (Lesser) Kolyma 1,870 422 Semlyachik Vostochny Range 1,560 1952 Indigirka 1,726 360 Karymsky Vostochny Range 1,486 2001 Anadyr 1,150 191 Vilyui (tributary of Lena) 2,650 454 Kuril Islands Aldan (tributary of Lena) 2,273 729 Alaid Atlasov I. 2,339 2000 Olyokma (tributary of Lena) 1,436 210 Tyatya Kunashir I. 1,819 1973 Zeya (tributary of Amur) 1,242 233 Chikurachki Paramushir I. 1,816 1995 Markha (tributary of Vilyui) 1,181 99 Fussa Paramushir I. 1,772 1984 Omolon (tributary of Kolyma) 1,114 113 Sarychev Matua I. 1,446 1976 Krenitsyn Onekotan I. -
PDF for Print
RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 10, ES4002, doi:10.2205/2007ES000224, 2008 The deep structure of active continental margins of the Far East (Russia) A. G. Rodnikov,1 N. A. Sergeyeva,1 L. P. Zabarinskaya,1 N. I. Filatova,2 V. B. Piip,3 and V. A. Rashidov4 Received 6 March 2008; accepted 20 March 2008; published 24 May 2008. [1] In the frame of the international project “InterMARGINS”, the research in the deep structure of active continental margins of the transition zone from the Eurasian continent to the Pacific was conducted along the deep cross-section of the tectonosphere including the lithosphere and the asthenosphere. The deep section profile runs across the Mesozoic structures of Sikhote Alin, rift structure of Tatar Strait, Cenozoic formations of Sakhalin, Kuril Basin of the Sea of Okhotsk, volcanic structures of Kuril Island Arc, Kuril deep trench and the Mesozoic plate of Northwest Pacific Basin. The length of the profile is 2000 km. The depth of penetration into the earth’s interior is 100 km. A distinctive feature of the transition zone structure is the asthenospheric layer occurrence in the upper mantle; diapirs of hot anomalous mantle branch off from this layer and processes going on in them cause the formation of the region geological structures. A correlation is noted between geological structures, tectonic and magmatic activity and the upper mantle structure. Tectonically active regions like island arcs and rift structures of marginal seas correspond to thick and most distinct asthenosphere generating magma. INDEX TERMS: 0905 Exploration Geophysics: Continental structures; 0930 Exploration Geophysics: Oceanic structures; 1645 Global Change: Solid Earth; 3001 Marine Geology and Geophysics: Back-arc basin processes; 3002 Marine Geology and Geophysics: Continental shelf and slope processes; KEYWORDS: deep structure, active continental margins, transition zone, upper mantle, marginal seas. -
Rethinking Russian Federalism
Rethinking Russian Federalism The Politics of Intergovernmental Relations and Federal Reforms at the Turn of the Millennium Johnny Rodin Stockholm University Contents Preface .......................................................................................................................5 1. Introduction...........................................................................................................7 1.1. Aim and Approaches ....................................................................................10 1.2. Research Questions.......................................................................................12 1.3. Outline of Study............................................................................................14 2. Definitions and Theoretical Points of Departure .............................................17 2.1. Intergovernmental Relations and How They Vary .......................................17 2.2. Intergovernmental Relations and Why They Vary .......................................20 2.2.1. Ideas, Institutions, Policy Paradigms and Behaviour............................21 2.2.2. Policy Paradigm Shifts..........................................................................24 2.3. Conclusions...................................................................................................26 3. Method and Material..........................................................................................27 3.1. Research Design ...........................................................................................27 -
Sustainable Development Report 2020
SUSTAINABLE DEVELOPMENT REPORT 2020 Head Office: 35 Dzerzhinskogo St., Yuzhno-Sakhalinsk, Sakhalin Oblast, Russian Federation, 693020 Moscow Representative Office: 31 Novinsky Blvd, Moscow, Russian Federation, 123242 Теl.: +7 495 956 1750, fax: +7 495 956 1760 www.sakhalinenergy.com SUSTAINABLE DEVELOPMENT REPORT 2020 CONTENTS 8.2.7. Green LNG Strategy ____________________________________________________________________________________________________________153 9.5.6. Korsakov Sustainable Development Partnership Council _________ 240 8.2.8. Utilisation of Associated Gas in Production _____________________________________________154 9.5.7. Sakhalin Indigenous Minorities Development Plan __________________________241 th 8.2.9. Environmental Protection Costs and Payments 9.5.8. 75 Anniversary of the Victory Project ________________________________________________________ 244 for the Negative Impact ___________________________________________________________________________________________________155 9.5.9. Festival — Pristine Russia: Bound for Sakhalin ________________________________________245 8.3. ENVIRONMENTAL MONITORING 9.5.10. Special Projects for Capacity Building of the Sakhalin AND BIODIVERSITY CONSERVATION ____________________________________________________ 157 Oblast Non-Profit Sector and Developing Volunteering 8.3.1. General Information ____________________________________________________________________________________________________________ 157 in the Region _____________________________________________________________________________________________________________________________ -
Geothermal Potential of the Cascade and Aleutian Arcs, with Ranking of Individual Volcanic Centers for Their Potential to Host Electricity-Grade Reservoirs
DE-EE0006725 ATLAS Geosciences Inc FY2016, Final Report, Phase I Final Research Performance Report Federal Agency and Organization: DOE EERE – Geothermal Technologies Program Recipient Organization: ATLAS Geosciences Inc DUNS Number: 078451191 Recipient Address: 3372 Skyline View Dr Reno, NV 89509 Award Number: DE-EE0006725 Project Title: Geothermal Potential of the Cascade and Aleutian Arcs, with Ranking of Individual Volcanic Centers for their Potential to Host Electricity-Grade Reservoirs Project Period: 10/1/14 – 10/31/15 Principal Investigator: Lisa Shevenell President [email protected] 775-240-7323 Report Submitted by: Lisa Shevenell Date of Report Submission: October 16, 2015 Reporting Period: September 1, 2014 through October 15, 2015 Report Frequency: Final Report Project Partners: Cumming Geoscience (William Cumming) – cost share partner GEODE (Glenn Melosh) – cost share partner University of Nevada, Reno (Nick Hinz) – cost share partner Western Washington University (Pete Stelling) – cost share partner DOE Project Team: DOE Contracting Officer – Laura Merrick DOE Project Officer – Eric Hass Project Monitor – Laura Garchar Signature_______________________________ Date____10/16/15_______________ *The Prime Recipient certifies that the information provided in this report is accurate and complete as of the date shown. Any errors or omissions discovered/identified at a later date will be duly reported to the funding agency. Page 1 of 152 DE-EE0006725 ATLAS Geosciences Inc FY2016, Final Report, Phase I Geothermal Potential of -
Iturup Island Pink & Chum Salmon MSC Fishery Assessment Report
SCS Global Services Report Iturup Island Pink & Chum Salmon MSC Fishery Assessment Report Announcement Comment Draft Report Authors Client Contact Ray Beamesderfer, Principle 1 & Lead J. S. C. Gidrostroy, Ludmila Voronova 15 Altalyskiy Lane, Yuzhno-Sakhalinsk, Shelby Oliver, Principle 2 & Project Coordinator Sakhalin Oblast 693020 Russian Federation Geir Honneland, Principle 3 +7 (4242) 72 18 31 [email protected] JULY 30, 2019 2000 Powell Street, Ste. 600, Emeryville, CA 94608 USA +1.510.452.8000 main | +1.510.452.8001 fax SCS Global Services Report 1 Table of Contents 3 EXECUTIVE SUMMARY ......................................................................................................................... 6 4 REPORT DETAILS ................................................................................................................................ 8 4.1 Authorship and peer review details ..................................................................................... 8 4.2 Version details ...................................................................................................................... 9 5 UNIT(S) OF ASSESSMENT AND CERTIFICATION AND RESULTS OVERVIEW ..................................................... 10 5.1 Unit(s) of Assessment (UoA) and Unit(s) of Certification ................................................... 10 5.1.1 Unit(s) of Assessment ............................................................................................ 10 5.1.2 Scope of Assessment in Relation to Enhanced Fisheries