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Russia in Figures. 2017: Statistical Handbook/Rosstat - M., 2017 - 511 P
FEDERAL STATE STATISTICS SERVICE (Rosstat) RUSSIA IN FIGURES 2017 STATISTICAL HANDBOOK Moscow 2017 UDK 31(470) Editorial Board: A. Surinov - Chairman of the Editorial Board E. Baranov, N. Bugakova, M. Gelvanovsky, L. Gokhberg, S. Egorenko, V. Elizarov, V. Zhitkov, Yu. Ivanov, A. Kevesh, A. Kosarev, K. Laikam, I. Masakova, V. Nesterov, G. Oksenoit, O. Rybak, B. Ryabushkin, A. Tatarinov, A. Khoroshilov Russia in Figures. 2017: Statistical Handbook/Rosstat - M., 2017 - 511 p. ISBN 978-5-89476-436-8 The handbook contains information on the social and eco- nomic situation of Russia in 2016 as compared with the previous years. It presents data characterizing the state structure of the Russian Federation, production and use of the Gross Domestic Product. Information is published on the population, its employ- ment and money incomes. The handbook highlights problems of social field, results of R&D work and innovation activities, fin- ances, investments, prices and tariffs. Some materials are dedi- cated to situation in organizations of different economic activi- ties. Reflected are the external economic activities of the Rus- sian Federation. Selected international comparisons are also given. The handbook is intended for managerial personnel, man- agers and employees of enterprises and organizations, scientif- ic, entrepreneurial and banking circles, professors and lecturers, under-graduate and post-graduate students of higher economic education institutions and other users. UDK 31(470) ISBN 978-5-89476-436-8 Federal State Statistics Service, 2017 E-mail: [email protected] http://www.gks.ru PREFACE The concise statistical handbook comprises main indicators cha- racterizing socio-economic situation of Russia in 2016 as compared with a number of previous years. -
English Online Exclusive January 2018
President of the Syrian Arab Republic Bashar Assad (second from left), Russian President Vladimir Putin (center left), Russian minister of defense General of the Army Sergey Shoygu (second from right), and chief of the general staff of the Russian Federation armed forces General of the Army Valery Gerasimov (right) meet 21 November 2017 in Sochi, Russia, to discuss the closing phases of Russian support for operations in Syria. (Photo courtesy of Administration of the President of Russia) What Kind of Victory for Russia in Syria? Michael Kofman Matthew Rojansky, JD he war in Syria has ground on for more than to house them, while others have sought safety as far half a decade. Hundreds of thousands have away as Europe and North America, exacerbating died, entire cities and towns have been de- divisive battles over immigration, jobs, and cultural Tstroyed, and billions of dollars in infrastructure have identity in Western democracies. been decimated. Millions of refugees have flooded into Syria has tested every world leader individually and neighboring Middle Eastern states that can ill afford collectively, and has laid bare the failure of international 2 January 2018 MILITARY REVIEW ONLINE EXCLUSIVE VICTORY FOR RUSSIA? institutions to deal effectively with the problems those hardly the centerpiece of either state’s global strategy, institutions were designed to manage and prevent. or even their respective regional policies. Despite a prolonged commitment of U.S. military and Russian-Syrian relations draw on a Cold War legacy, diplomatic resources to the conflict, a peaceful settlement since Moscow first began to support Syria after the remains remote, and the bloody-handed Assad regime 1956 Suez Crisis. -
DCS L-39ZA Albatros Guide
DCS GUIDE L-39ZA ALBATROS LAST UPDATED: 21/12/2016 By Chuck 1 TABLE OF CONTENTS • PART 1 – INTRODUCTION • PART 2 – CONTROLS SETUP • PART 3 – COCKPIT & GAUGES • PART 4 – START-UP PROCEDURE • PART 5 – TAKEOFF • PART 6 – LANDING • PART 7 – ENGINE MANAGEMENT • PART 8 – FLIGHT CHARACTERISTICS • PART 9 – WEAPONS & ARMAMENT • PART 10 – RADIO TUTORIAL • PART 11 – NAVIGATION & ILS LANDING • PART 12 – AEROBATIC FLYING • PART 13 – TRAINING & FAILURE SIMULATION • PART 14 – OTHER RESOURCES Special thanks to Paul "Goldwolf" Whittingham for creating the guide icons. 2 With over 3,000 aircraft produced, the L-39 Albatros has become one of the most popular and widespread trainer aircraft in the world. Developed in Czechoslovakia by Aero Vodochody, it was designed during the 1960s as a replacement for the Aero L-29 Delfin as a principal training aircraft. The Albatros has the distinction of being the first of the second-generation jet trainers to be produced, as well as being the first trainer aircraft to be equipped 39ZA - ALBATROS L with a turbofan powerplant. Designed to be a cost-effective trainer aircraft, the L-39 was also capable of performing ground attack missions. For operational flexibility, simplicity, and affordability, the majority of onboard systems have been simplified to avoid incurring high levels of maintenance, as well as to minimize damage caused by mishandling when flown by inexperienced air crew. It could be readily flown from austere airstrips such as frozen lakebeds, enabled through the rugged design of the landing gear and favourable low landing speeds. The aircraft's flying qualities are reportedly simple, which is made easier by way of a rapid throttle response, making it easier for students who had never previously flown before to successfully control. -
Russian Federation State Actors of Protection
European Asylum Support Office EASO Country of Origin Information Report Russian Federation State Actors of Protection March 2017 SUPPORT IS OUR MISSION European Asylum Support Office EASO Country of Origin Information Report Russian Federation State Actors of Protection March 2017 Europe Direct is a service to help you find answers to your questions about the European Union. Free phone number (*): 00 800 6 7 8 9 10 11 (*) Certain mobile telephone operators do not allow access to 00800 numbers or these calls may be billed. More information on the European Union is available on the Internet (http://europa.eu). Print ISBN 978-92-9494-372-9 doi: 10.2847/502403 BZ-04-17-273-EN-C PDF ISBN 978-92-9494-373-6 doi: 10.2847/265043 BZ-04-17-273-EN-C © European Asylum Support Office 2017 Cover photo credit: JessAerons – Istockphoto.com Neither EASO nor any person acting on its behalf may be held responsible for the use which may be made of the information contained herein. EASO Country of Origin Report: Russian Federation – State Actors of Protection — 3 Acknowledgments EASO would like to acknowledge the following national COI units and asylum and migration departments as the co-authors of this report: Belgium, Cedoca (Center for Documentation and Research), Office of the Commissioner General for Refugees and Stateless Persons Poland, Country of Origin Information Unit, Department for Refugee Procedures, Office for Foreigners Sweden, Lifos, Centre for Country of Origin Information and Analysis, Swedish Migration Agency Norway, Landinfo, Country of -
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. -
78 Ukrainian Population of Crimea in 1989-2014: Specifics
ISSN 2414-1143 Научный альманах стран Причерноморья. 2021. Том 26. № 2 DOI 10.23947/2414-1143-2021-26-2-78-84 UDC 39:314 UKRAINIAN POPULATION OF CRIMEA IN 1989-2014: SPECIFICS OF DEMOGRAPHIC TRANSFORMATIONS1 Dmitry I. Uznarodov Federal Research Centre the Southern Scientific Centre of the Russian Academy of Sciences, Rostov-on-Don, Russian Federation [email protected] The specificity of the demographic transformations of the Ukrainian population of Crimea in the period from 1989 to 2014 is considered. Based on the analysis of the population censuses of 1989, 2001 and 2014, demo- graphic changes within the Ukrainian ethnos are revealed during two periods: from 1989 to 2001 and from 2001 to 2014. The analysis of changes in the number of the Ukrainian ethnic group in the context of the municipalities of the Crimean Peninsula is carried out. It is concluded that the percentage of the Ukrainian ethnic group in the struc- ture of the population of the Crimean Peninsula, which we could observe in the period from 1989 to 2001, was formed as a result of the policy of resettlement of citizens to this region in the late 1940-s and early 1950-s from various republics of the Soviet Union, mainly the RSFSR and the Ukrainian SSR. It is noted that the regions with the maximum number of the Ukrainian ethnic group are historically located in the northern regions of the Crimean Peninsula, and with the smallest – in the southern regions. The study showed that changes in the ethnic structure began to occur after the events of 2014 and the entry of Crimea into the Russian Federation, when, according to the 2014 population census, the number of Ukrainians in the republic, compared to 2001, decreased by almost 9%. -
Who Is Who in Pakistan & Who Is Who in the World Study Material
1 Who is Who in Pakistan Lists of Government Officials (former & current) Governor Generals of Pakistan: Sr. # Name Assumed Office Left Office 1 Muhammad Ali Jinnah 15 August 1947 11 September 1948 (died in office) 2 Sir Khawaja Nazimuddin September 1948 October 1951 3 Sir Ghulam Muhammad October 1951 August 1955 4 Iskander Mirza August 1955 (Acting) March 1956 October 1955 (full-time) First Cabinet of Pakistan: Pakistan came into being on August 14, 1947. Its first Governor General was Muhammad Ali Jinnah and First Prime Minister was Liaqat Ali Khan. Following is the list of the first cabinet of Pakistan. Sr. Name of Minister Ministry 1. Liaqat Ali Khan Prime Minister, Foreign Minister, Defence Minister, Minister for Commonwealth relations 2. Malik Ghulam Muhammad Finance Minister 3. Ibrahim Ismail Chundrigar Minister of trade , Industries & Construction 4. *Raja Ghuzanfar Ali Minister for Food, Agriculture, and Health 5. Sardar Abdul Rab Nishtar Transport, Communication Minister 6. Fazal-ul-Rehman Minister Interior, Education, and Information 7. Jogendra Nath Mandal Minister for Law & Labour *Raja Ghuzanfar’s portfolio was changed to Minister of Evacuee and Refugee Rehabilitation and the ministry for food and agriculture was given to Abdul Satar Pirzada • The first Chief Minister of Punjab was Nawab Iftikhar. • The first Chief Minister of NWFP was Abdul Qayum Khan. • The First Chief Minister of Sindh was Muhamad Ayub Khuro. • The First Chief Minister of Balochistan was Ataullah Mengal (1 May 1972), Balochistan acquired the status of the province in 1970. List of Former Prime Ministers of Pakistan 1. Liaquat Ali Khan (1896 – 1951) In Office: 14 August 1947 – 16 October 1951 2. -
Explosive Basaltic Volcanism of the Chikurachki Volcano (Kurile Arc
Journal of Volcanology and Geothermal Research 147 (2005) 203–232 www.elsevier.com/locate/jvolgeores Explosive basaltic volcanism of the Chikurachki Volcano (Kurile arc, Russia): Insights on pre-eruptive magmatic conditions and volatile budget revealed from phenocryst-hosted melt inclusions and groundmass glasses A.A. Gurenkoa,b,*, A.B. Belousovc,d, R.B. Trumbullb, A.V. Soboleva,e aMax Planck Institute for Chemistry, Geochemistry, P.O. Box 3060, 55020 Mainz, Germany bGeoForschungsZentrum Potsdam, Section 4.2, Telegrafenberg, 14473 Potsdam, Germany cInstitute of Marine Geology and Geophysics, 693022 Yuzno-Sakhalinsk, Russia dInstitute of Volcanic Geology and Geochemistry, 683006 Petropavlovsk-Kamchatsky, Russia eVernadsky Institute of Geochemistry and Analytical Chemistry, 117975 Moscow, Russia Received 13 December 2004; accepted 6 April 2005 Abstract Highly explosive eruptions of basaltic composition are relatively rare and poorly understood, yet they may be quite important in terms of atmospheric impact because of the generally much higher concentrations of S in basaltic systems compared with the typical explosive felsic eruptions. We have determined concentrations of H2O, major, trace and volatile (S, Cl) elements by EPMA and SIMS from melt inclusions and groundmass glasses of the 1986, 1853 and prehistoric explosive eruptions of basaltic magmas from the Chikurachki volcano, northern Kurile arc. Melt inclusions are hosted by olivine (Fo72–78), orthopyroxene (mg#=72–75), clinopyroxene (mg#=71–77) and plagioclase (An74–96) phenocrysts. Estimated crystallization conditions were in the range from 910 to 1180 8C at less than 400 MPa total pressure and oxygen fugacity of NNO+1 to +2 log units. Inclusion glasses are basaltic to andesitic in composition. -
The 2019 Eruption Dynamics and Morphology at Ebeko Volcano Monitored by Unoccupied Aircraft Systems (UAS) and Field Stations
remote sensing Article The 2019 Eruption Dynamics and Morphology at Ebeko Volcano Monitored by Unoccupied Aircraft Systems (UAS) and Field Stations Thomas R. Walter 1,* , Alexander Belousov 2, Marina Belousova 2, Tatiana Kotenko 2 and Andreas Auer 3 1 Department of Geophysics, GFZ Potsdam, Telegrafenberg, 14473 Potsdam, Germany 2 Institute of Volcanology and Seismology, FED RAS, 683006 Petropavlovsk, Russia; [email protected] (A.B.); [email protected] (M.B.); [email protected] (T.K.) 3 Department of Geoscience, Shimane University, Matsue 690-8504, Japan; [email protected] * Correspondence: [email protected] Received: 20 May 2020; Accepted: 16 June 2020; Published: 18 June 2020 Abstract: Vulcanian explosions are hazardous and are often spontaneous and direct observations are therefore challenging. Ebeko is an active volcano on Paramushir Island, northern Kuril Islands, showing characteristic Vulcanian-type activity. In 2019, we started a comprehensive survey using a combination of field station records and repeated unoccupied aircraft system (UAS) surveys to describe the geomorphological features of the edifice and its evolution during ongoing activity. Seismic data revealed the activity of the volcano and were complemented by monitoring cameras, showing a mean explosion interval of 34 min. Digital terrain data generated from UAS quadcopter photographs allowed for the identification of the dimensions of the craters, a structural architecture and the tephra deposition at cm-scale resolution. The UAS was equipped with a thermal camera, which in combination with the terrain data, allowed it to identify fumaroles, volcano-tectonic structures and vents and generate a catalog of 282 thermal spots. The data provide details on a nested crater complex, aligned NNE-SSW, erupting on the northern rim of the former North Crater. -
2002 Volcanic Activity in Alaska and Kamchatka: Summary of Events and Response of the Alaska Volcano Observatory by Christina A
2002 Volcanic Activity in Alaska and Kamchatka: Summary of Events and Response of the Alaska Volcano Observatory by Christina A. Neal, Robert G. McGimsey, and Olga Girina Open-File Report 2004-1058 U.S. Department of the Interior U.S. Geological Survey 2002 Volcanic Activity in Alaska and Kamchatka: Summary of Events and Response of the Alaska Volcano Observatory By Christina A. Neal1, Robert G. McGimsey1, and Olga Girina2 1Alaska Volcano Observatory, 4200 University Dr., Anchorage, AK 99508-4664 2Kamchatka Volcanic Eruptions Response Team, Institute of Volcanic Geology and Geochemistry, Piip Blvd, 9 Petropavlovsk- Kamchatsky, 683006, Russia AVO is a cooperative program of the U.S. Geological Survey, University of Alaska Fairbanks Geophysical Institute, and the Alaska Division of Geological and Geophysical Surveys. AVO is funded by the U.S. Geological Survey Volcano Hazards Program and the State of Alaska Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government Open-File Report 2004-1058 U.S. Department of the Interior U.S. Geological Survey TABLE OF CONTENTS Introduction..................................................................................................................................1 Volcanic.Activity.in.Alaska..........................................................................................................4 Wrangell.Volcano.........................................................................................................................4 -
Defining and Identifying Russia's Elite Groups
Defining and identifying Russia’s elite groups Siloviki representation during Putin’s third term Master’s Thesis Russian and Eurasian Studies Leiden University, The Netherlands 23 January 2017 Sam Broekman Student Number: 1605062 Word Count: 18,005 Supervisor: Dr. M. Frear Table of contents Introduction ............................................................................................................................................. 2 Introducing the siloviki ......................................................................................................................... 2 General research gaps ......................................................................................................................... 2 Research question ............................................................................................................................... 3 Methodology ....................................................................................................................................... 4 Chapter overview ................................................................................................................................. 4 Section 1: Rise of the siloviki..................................................................................................................... 6 1.1 The Politburo 2.0 ........................................................................................................................... 6 1.2 Putin’s return to the presidency ................................................................................................. -
Supporting Online Material
Journal of Geophysical Research - Atmospheres Supporting Information for Evidence for added value of convection-permitting models for studying changes in extreme precipitation E. P. Meredith1, D. Maraun1,2, V. A. Semenov1,3,4,5, W. Park1 1GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany 2Wegener Center for Climate and Global Change, University of Graz, Graz, Austria 3A.M. Obukhov Institute of Atmospheric Physics, Russian Academy of Sciences, Moscow, Russia 4P.P. Shirshov Institute of Oceonology, Russian Academy of Sciences, Moscow, Russia 5Institute of Geography, Russian Academy of Sciences, Moscow, Russia Contents of this file Text S1 (with accompanying figures S1-3) Figures S4 to S6 Introduction This supporting information document provides Text S1 and Figures S4 to S6, as referred to in the main document. 1 Text S1 – Synoptic Discussion of the Krymsk Precipitation Extreme A slow moving cyclone was centered over the north-eastern Black Sea on July 6 th 2012, advecting warm and moist air towards the Krymsk region (Figure S1). The atmospheric profile early on the 6th, from the down coast station of Tuapse (44.10N/39.07E), shows the lower atmosphere to be saturated at most levels below 500 hPa and primarily conditionally unstable below 750 hPa (Figure S2). Analysis of the lower troposphere reveals the development of a south-westerly low- level jet to the south and east of Krymsk. Maximum wind speeds of over 13 m/s at the 925 hPa level (Figure S3) provided a rich source of shoreward moisture advection, giving rise to the first wave of convection. Later that night, convective cells formed at the head of an equivalent potential temperature (theta- e) ridge before merging into a larger organized mesoscale convective system (MCS).