Warming Temperatures Are Impacting the Hydrometeorological Regime of Russian Rivers in the Zone of Continuous Permafrost
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The Fluvial Geochemistry of the Rivers of Eastern Siberia: I. Tributaries Of
Geochimica et Cosmochimica Acta, Vol. 62, No. 10, pp. 1657–1676, 1998 Copyright © 1998 Elsevier Science Ltd Pergamon Printed in the USA. All rights reserved 0016-7037/98 $19.00 1 .00 PII S0016-7037(98)00107-0 The fluvial geochemistry of the rivers of Eastern Siberia: I. Tributaries of the Lena River draining the sedimentary platform of the Siberian Craton 1, 1 2 1 YOUNGSOOK HUH, *MAI-YIN TSOI, ALEXANDR ZAITSEV, and JOHN M. EDMONd 1Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA 2Laboratory of Erosion and Fluvial Processes, Department of Geography, Moscow State University, Moscow, Russia (Received June 11, 1997; accepted in revised form February 12, 1998) ABSTRACT—The response of continental weathering rates to changing climate and atmospheric PCO2 is of considerable importance both to the interpretation of the geological sedimentary record and to predictions of the effects of future anthropogenic influences. While comprehensive work on the controlling mechanisms of contemporary chemical and mechanical weathering has been carried out in the tropics and, to a lesser extent, in the strongly perturbed northern temperate latitudes, very little is known about the peri-glacial environments in the subarctic and arctic. Thus, the effects of climate, essentially temperature and runoff, on the rates of atmospheric CO2 consumption by weathering are not well quantified at this climatic extreme. To remedy this lack a comprehensive survey has been carried out of the geochemistry of the large rivers of Eastern Siberia, the Lena, Yana, Indigirka, Kolyma, Anadyr, and numerous lesser streams which drain a pristine, high-latitude region that has not experienced the pervasive effects of glaciation and subsequent anthropogenic impacts common to western Eurasia and North America. -
FSC National Risk Assessment
FSC National Risk Assessment for the Russian Federation DEVELOPED ACCORDING TO PROCEDURE FSC-PRO-60-002 V3-0 Version V1-0 Code FSC-NRA-RU National approval National decision body: Coordination Council, Association NRG Date: 04 June 2018 International approval FSC International Center, Performance and Standards Unit Date: 11 December 2018 International contact Name: Tatiana Diukova E-mail address: [email protected] Period of validity Date of approval: 11 December 2018 Valid until: (date of approval + 5 years) Body responsible for NRA FSC Russia, [email protected], [email protected] maintenance FSC-NRA-RU V1-0 NATIONAL RISK ASSESSMENT FOR THE RUSSIAN FEDERATION 2018 – 1 of 78 – Contents Risk designations in finalized risk assessments for the Russian Federation ................................................. 3 1 Background information ........................................................................................................... 4 2 List of experts involved in risk assessment and their contact details ........................................ 6 3 National risk assessment maintenance .................................................................................... 7 4 Complaints and disputes regarding the approved National Risk Assessment ........................... 7 5 List of key stakeholders for consultation ................................................................................... 8 6 List of abbreviations and Russian transliterated terms* used ................................................... 8 7 Risk assessments -
Quantifying the Northward Spread of Ticks (Ixodida) As Climate Warms in Northern Russia
atmosphere Article Quantifying the Northward Spread of Ticks (Ixodida) as Climate Warms in Northern Russia Leonid N. Vladimirov 1, Grigory N. Machakhtyrov 1, Varvara A. Machakhtyrova 1 , Albertus S. Louw 2 , Netrananda Sahu 3 , Ali P. Yunus 4 and Ram Avtar 2,5,* 1 Yakut Scientific Research Institute of Agriculture, Yakutsk 677001, Russia; [email protected] (L.N.V.); [email protected] (G.N.M.); [email protected] (V.A.M.) 2 Graduate School of Environmental Science, Hokkaido University, Sapporo 060-0810, Japan; [email protected] 3 Department of Geography, Delhi School of Economics, University of Delhi, Delhi 110007, India; [email protected] 4 Center for Climate Change Adaptation, National Institute for Environmental Studies, Tsukuba 305-8506, Japan; [email protected] 5 Faculty of Environmental Earth Science, Hokkaido University, Sapporo 060-0810, Japan * Correspondence: [email protected]; Tel.: +81-011-706-2261 Abstract: Climate change is affecting human health worldwide. In particular, changes to local and global climate parameters influence vector and water-borne diseases like malaria, dengue fever, and tick-borne encephalitis. The Republic of Sakha in northern Russia is no exception. Long-term trends of increasing annual temperatures and thawing permafrost have corresponded with the northward range expansion of tick-species in the Republic. Indigenous communities living in these remote areas may be severely affected by human and livestock diseases introduced by disease vectors like ticks. To better understand the risk of vector-borne diseases in Sakha, we aimed to describe the Citation: Vladimirov, L.N.; increase and spatial spread of tick-bite cases in the Republic. -
Winter Atmospheric Conditions
Th or collective redistirbution of any portion article of any by of this or collective redistirbution SPECIAL ISSUE ON THE JAPAN/EAST SEA articleis has been in published Oceanography Winter 19, Number journal of Th 3, a quarterly , Volume Atmospheric Conditions only permitted is means reposting, or other machine, photocopy over the Japan/East Sea Th e Structure and Impact of 2006 by Th e Oceanography Society. Copyright Severe Cold-Air Outbreaks with the approval of Th approval the with BY CLIVE E. DORMAN, CARL A. FRIEHE, DJAMAL KHELIF, ALBERTO SCOTTI, JAMES EDSON, ROBERT C. BEARDSLEY, gran e Oceanography is Society. All rights reserved. Permission or Th e Oceanography [email protected] Society. Send to: all correspondence RICHARD LIMEBURNER, AND SHUYI S. CHEN The Japan/East Sea is a marginal sea strategically placed phy of the Japan/East Sea and its surface forcing. During between the world’s largest land mass and the world’s this program, we made atmospheric observations with largest ocean. The Eurasian land mass extending to a research aircraft and ships to understand the lower high latitudes generates several unique winter synoptic atmosphere and surface air-sea fl uxes. We report here weather features, the most notable being the vast Siberian several highlights of these investigations with a focus on Anticyclone that covers much of the northeast Asian land the dramatic severe cold-air outbreaks that occur three ted to copy this article for use in teaching and research. Repu article for use and research. this copy in teaching to ted mass. The Japan/East Sea’s very distinctive winter condi- to fi ve times a winter month. -
Vast Atmospheric Cold Traps Within the Large Ringed Topographic Features in Ne Siberia: Implication for Mars
Third Mars Polar Science Conference (2003) 8117.pdf VAST ATMOSPHERIC COLD TRAPS WITHIN THE LARGE RINGED TOPOGRAPHIC FEATURES IN NE SIBERIA: IMPLICATION FOR MARS. G. A. Burba, Vernadsky Institute of Geochemistry and Analytical Chemistry, 19 Kosygin St., Moscow 119991, Russia e-mail: [email protected] Introduction: The ridges within the vast mountain plained that each of these “cold poles” is located country of the NE Siberia have been revealed recently within the lower areas at the central parts of the large to comprise two giant ring structures (RS), 500 and ring structures (intermountain basins), which works as 400 km in diameter [1] . Such evidence is a new look a giant cold traps being enclosed within a ring wall of on the general topographic structure of the area and mountain ridges. Such situation could lead to the cir- could be of importance for climatic consequences.The cumstances of the temperature inversion in the near- central lower areas of these structures, which are en- surface layer of the atmosphere. closed within a ring wall of mountain ridges, work as Implication for Mars: Couldn’t the similar situa- giant “cold traps” for the atmospheric air. During the tion with the air temperature take place during the win- winter seasons the temperature inversion in the near- ter season within the craters and large basins in the surface layer of the atmosphere take place there. polar regions of Mars? Topographic description: The highest area of the References: [1] Burba G. A. (1995) LPSC XXVI, North-East Siberia, Russia, consists of the mountain 189-190. [2] Atlas SSSR (1984) Map “Air tempera- ridges arranged as the two adjacent RS. -
Sediment Transport to the Laptev Sea-Hydrology and Geochemistry of the Lena River
Sediment transport to the Laptev Sea-hydrology and geochemistry of the Lena River V. RACHOLD, A. ALABYAN, H.-W. HUBBERTEN, V. N. KOROTAEV and A. A, ZAITSEV Rachold, V., Alabyan, A., Hubberten, H.-W., Korotaev, V. N. & Zaitsev, A. A. 1996: Sediment transport to the Laptev Sea-hydrology and geochemistry of the Lena River. Polar Research 15(2), 183-196. This study focuses on the fluvial sediment input to the Laptev Sea and concentrates on the hydrology of the Lena basin and the geochemistry of the suspended particulate material. The paper presents data on annual water discharge, sediment transport and seasonal variations of sediment transport. The data are based on daily measurements of hydrometeorological stations and additional analyses of the SPM concentrations carried out during expeditions from 1975 to 1981. Samples of the SPM collected during an expedition in 1994 were analysed for major, trace, and rare earth elements by ICP-OES and ICP-MS. Approximately 700 h3freshwater and 27 x lo6 tons of sediment per year are supplied to the Laptev Sea by Siberian rivers, mainly by the Lena River. Due to the climatic situation of the drainage area, almost the entire material is transported between June and September. However, only a minor part of the sediments transported by the Lena River enters the Laptev Sea shelf through the main channels of the delta, while the rest is dispersed within the network of the Lena Delta. Because the Lena River drains a large basin of 2.5 x lo6 km2,the chemical composition of the SPM shows a very uniform composition. -
Terminal Evaluation of the UNEP/GEF Project
United Nations Environment Programme Terminal Evaluation of the UNEP/GEF Project “Russian Federation – Support to the National Programme of Action for the Protection of the Arctic Marine Environment” Prof. Dr. Ivan Holoubek & Oleg Sutkaitis UNEP Evaluation Office September 2012 Table of Contents Project Identification Table _________________________________________________ i Executive summary ________________________________________________________ ii 1. Evaluation background ________________________________________________ 1 A. Context _____________________________________________________________________________ 1 B. The Project __________________________________________________________________________ 2 C. Evaluation objectives, scope and methodology ____________________________________________ 4 C. 1 Objective and Scope of the Evaluation ________________________________________________ 4 C. 2 Overall Approach and Methods ______________________________________________________ 4 C. 3. Limitations and Constraints ________________________________________________________ 5 2. Project performance and impact ___________________________________________ 6 A. Attainment of objectives and planned results ___________________________________ 6 A.1 Achievement of outputs and activities __________________________________________________ 6 A.2 Relevance __________________________________________________________________________ 7 A. 3 Effectiveness _______________________________________________________________________ 9 A.4 Efficiency _________________________________________________________________________ -
Goldman Et Al. (2016) Monitoring of the Ecological Security in the North-Western Region of the Republic …
ISSN 2056-9386 Volume 3 (2016) issue 3, article 2 Monitoring of the ecological security in the north- western region of the Republic of Sakha, Russian Federation 俄罗斯联邦萨哈共和国西北地区的生态安全监测 Albina A. Goldman, Elena V. Sleptsova, Raissa P. Ivanova Mirny Polytechnic Institute (branch) of Ammosov North-Eastern Federal University (NEFU), Mirny, Tikhonova street 5, build.1, Russian Federation [email protected], [email protected], [email protected] Accepted for publication on 3rd September 2016 Abstract – The paper is devoted to the environmental diamonds and hydrocarbon crude are located in western and impact of industrial sector in Western Yakutia and the south-western parts of the republic. The largest diamond, oil role of the Mirny Polytechnic Institute (branch) of the and gas fields are situated in Western Yakutia. Ammosov North-Eastern Federal University in training specialists for oil and gas and diamond mining industries II. INDUSTRIAL SECTORS OF THE REGION and the research carried out at the educational and scientific laboratory of complex analysis of The area of disturbed lands in Mirny district ranks second anthropogenic disturbances of the Institute on in the Republic after the Neryungrinsky district (about 9 compliance with the requirements. thousand hectares). Key words – environment, industry, oil and gas, diamond The history of diamond mining in Yakutia dates back to mining, ecological monitoring, East Siberia. 1954, when prospectors discovered the first diamond pipe, Zarnitsa (‘Summer Lightning’). In 1957 the Soviet I. INTRODUCTION government established Yakutalmaz Group of enterprises, and diamond mining operations commenced. Two years later The Mirny Polytechnic Institute (branch) of the the USSR sold the first parcel of Yakutian diamonds on the Ammosov North-Eastern Federal University is located in the world market. -
Spiders (Aranei) from Oymyakon, the Cold Pole of the Northern Hemisphere (Yakutia, Siberia)
Arthropoda Selecta 13 (12): 6975 © ARTHROPODA SELECTA, 2004 Spiders (Aranei) from Oymyakon, the cold pole of the northern hemisphere (Yakutia, Siberia) Ïàóêè (Aranei) Îéìÿêîíà, ïîëþñà õîëîäà ñåâåðíîãî ïîëóøàðèÿ (ßêóòèÿ) Yuri M. Marusik1, Seppo Koponen2 & Nadezhda K. Potapova3 Þ.Ì. Ìàðóñèê, Ñ. Êîïîíåí, Í.Ê. Ïîòàïîâà 1Institute for Biological Problems of the North, Russian Academy of Sciences, Portovaya Str. 18, Magadan 685000 Russia; E-mail: [email protected] 1 Èíñòèòóò áèîëîãè÷åñêèõ ïðîáëåì Ñåâåðà ÄÂÎ ÐÀÍ, Ïîðòîâàÿ 18, Ìàãàäàí 685000 Ðîññèÿ. 2Zoological Museum, Centre for Biodiversity, University of Turku, FI-20014 Turku, Finland; E-mail: [email protected] 3Institute for Biological Problems of Cryolithozone, Siberian Division of the Russian Academy of Sciences, Prospect Lenina 41, Yakutsk 677891, Russia; E-mail: [email protected] 3 Èíñòèòó áèîëîãè÷åñêèõ ïðîáëåì êðèîëèòîçîíû ÑÎ ÐÀÍ, ïð. Ëåíèíà 41, ßêóòñê 677891 Ðîññèÿ. KEY WORDS: Araneae, spiders, faunistic records, distribution patterns, Yakutia. ÊËÞ×ÅÂÛÅ ÑËÎÂÀ: Araneae, ïàóêè, ôàóíèñòè÷åñêèå íàõîäêè, ðàñïðîñòðàíåíèå, ßêóòèÿ. ABSTRACT: Fifty-five species of spiders were col- Introduction lected in the Oymyakon area (ca 64.565°N, 142 145°E), eastern Yakutia, 2003. The vast majority of Yakutia (or Republic of Sakha) is the largest admin- species found are boreal and hypoarctic spiders. The istrative unit of Russia, about 3 100 000 km2, consisting material include some steppe species, e.g. Zelotes bal- of taiga, steppe, forest tundra, tundra and mountain tistanus Caporiacco, 1935, Pellenes gobiensis Schen- ecosystems. This wide area is reaching from the Amur kel, 1936 and P. limbatus Kulczyñski, 1895, at the region to the Arctic Ocean. northern limits of their range. -
Climate Change and Human Mobility in Indigenous Communities of the Russian North
Climate Change and Human Mobility in Indigenous Communities of the Russian North January 30, 2013 Susan A. Crate George Mason University Cover image: Winifried K. Dallmann, Norwegian Polar Institute. http://www.arctic-council.org/index.php/en/about/maps. TABLE OF CONTENTS Acknowledgements .......................................................................................................................... i Executive Summary ........................................................................................................................ ii 1. Introduction and Purpose ............................................................................................................ 1 1.1 Focus of paper and author’s approach................................................................................... 2 1.2 Human mobility in the Russian North: Physical and Cultural Forces .................................. 3 1.2.1 Mobility as the Historical Rule in the Circumpolar North ............................................. 3 1.2.2. Changing the Rules: Mobility and Migration in the Russian and Soviet North ............ 4 1.2.3 Peoples of the Russian North .......................................................................................... 7 1.2.4 The contemporary state: changes affecting livelihoods ................................................. 8 2. Overview of the physical science: actual and potential effects of climate change in the Russian North .............................................................................................................................................. -
Trace Elements and Stable Isotope Diagrams of Late Pleistocene Ice Wedges of Batagaika Yedoma, Central Yakutia
Trace elements and stable isotope diagrams of Late Pleistocene ice wedges of Batagaika yedoma, Central Yakutia Yu.K.Vasil'chuk1 J.Yu.Vasil'chuk1 N. A. Budantseva1 A.C. Vasil'chuk1 1Department of Geography, Lomonosov Moscow State University, Moscow, Russia, e-mail: [email protected] Abstract The subject of the study is the yedoma ice complex, which locates in the Batagaika depression, Sakha Republic, Russia. The oxygen and hydrogen stable isotope composition, and the content of the dissolved forms of minor and major elements were studied for the first time in ice-wedges of Batagaika depression, which makes the novelty of the study. The isotope composition of the two most saline ice-wedges located in the upper and lower parts of the Batagay depression indicates that they were formed in a close temperature range, the average winter temperature was close to –34/–35 °C, and the average January air temperature was –51/ –53 °C. The ice-wedge with the lowest content of all the trace elements was formed in more severe conditions, the average winter air temperature was close to -36 °C, and the average January air temperature was –54/–55 °C. Keywords: permafrost; ice wedge; oxygen isotope; hydrogen isotope; trace elements; East Siberia, Late Pleistocene The subject of the study is the yedoma, which is found lacustrine or taberal deposits, which are form horizontal in the Batagaika depression (67°34'49" N, 134°46'19" E), wedge 150-200 meters long and intruding into the located 10 km southeast of Batagai settlement (about 17 yedoma deposits and overlaying it. -
Supplementary Information
Supplementary Information Table S1. List of samples that yielded DNA in this study (EE2-EE26), followed by successfully amplified samples of cave lion from the study by Barnett et al. 2009. ALA=Alaska, EUR=Europe, SIB=Siberia, NC=not calibrated as out of range. The asterisk (*) denotes the approximate age as reported in Barnett et al. 2009. Sample CR haplotype/ Uncalibrated Calendar years Site and geographic region ID Genbank nr. 14C date before present EE2 D/ DQ899903 Schusterlucke cave (EUR) 15400 ± 130 18521 ± 1844 EE4 - Tyung, C Siberia (SIB) 46700±1300 48181 ± 6747 EE3 Y3 Tain cave, Urals (EUR) >49600 NC EE6 Y1 Elovka, Baikal (SIB) 18350 ± 75 21634 ± 1504 EE7 Y1 Volchika, C Siberia (SIB) 20085 ± 80 23266 ± 576 EE13 J/ DQ899909 New Siberian Islands (SIB) 47700 ± 800 48970 ± 6009 EE14 Y4 Yakutia, NE Siberia (SIB) >55400 NC EE15 B/ DQ899901 Yakutia, NE Siberia (SIB) 27720 ± 140 30880 ± 1543 EE16 Y2 Irkutsk, Baikal (SIB) 17910 ± 75 21024 ± 1041 EE17 B/ DQ899901 Khroma river, Yakutia (SIB) 19755 ± 80 20006 ± 404 EE19 - New Siberian Islands (SIB) 52000±1500 54373 ± 6396 EE20 J/ DQ899909 Yakutia, NE Siberia (SIB) >62400 NC EE21 G/ DQ899906 Nizhnyaya, C Siberia (SIB) 50500 ± 290 52785 ± 10541 EE26 Y5 (partial) Kyttyk Peninsula (SIB) 36550 ± 290 41025 ± 970 IB133 A/ DQ899900 Gold Run Creek, Yukon (ALA) 12640 ± 75 15016 ± 1463 RB112 A Caribou Creek, Yukon (ALA) n/a - RB74 A Fairbanks Creek, Alaska (ALA) n/a - RB75 A Ester Creek, Alaska (ALA) 12090 ± 80 13822 ± 341 IB134 B/ DQ899901 Gold Hill, Alaska (ALA) 18240 ± 90 21533 ± 1335 IB136 B Hunker