Baron Eduard Von Toll's Last Expedition
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Protostar II Mission Overview
THE VEHICLE THE SATELLITE PROTON HISTORY PROTON DESCRIPTION Lead designer was Vladimir Chelomei, who designed it TOTAL HEIGHT with the intention of creating both a powerful rocket for 58.2 m (191 ft) military payloads and a high-performance ICBM. The program was changed, and the rocket was developed GRoss LIFT-OFF exclusively for launching spacecraft. WEIGHT 705,000 kg First named UR-500, but adopted the name (1,554,000 lb) “Proton,” which also was the name of the first PROPELLANT three payloads launched. UDMH and NTO Proton launched Russian interplanetary mis- INITIAL LAUNCH sions to the Moon, Venus, Mars, and Hal- 16 July 1965 ley’s Comet. Proton-1 Spacecraft Proton launched the Salyut space sta- PAYLOAD FAIRINGS tions, the Mir core segment and both There are multiple payload fairing designs presently the Zarya (Dawn) and Zvezda (Star) mod- qualified for flight, including ules for today’s International Space Station. standard commercial payload fairings developed specifically to First commercial Proton launch — 9 April 1996. meet the needs of our customers. First commercial Proton M Breeze M launch BREEZE M UPPER STAGE — 30 December 2002 The Breeze M is powered by one pump-fed Mission Overview gimbaled main engine that develops thrust of 20 kN (4,500 lbf). It is composed of a central core and an auxilliary propellant tank which is jettisoned in flight SATELLITE OPERATOR following depletion. The Breeze M control system includes an SES on-board computer, a three-axis gyro stabilized platform, and a www.ses.com navigation system. The quantity of propellant carried is dependent SATELLITE MANUFACTURER on specific mission requirements and is varied to maximize mission Experience ILS: Achieve Your Mission performance. -
Scott's Discovery Expedition
New Light on the British National Antarctic Expedition (Scott’s Discovery Expedition) 1901-1904. Andrew Atkin Graduate Certificate in Antarctic Studies (GCAS X), 2007/2008 CONTENTS 1 Preamble 1.1 The Canterbury connection……………...………………….…………4 1.2 Primary sources of note………………………………………..………4 1.3 Intent of this paper…………………………………………………...…5 2 Bernacchi’s road to Discovery 2.1 Maria Island to Melbourne………………………………….…….……6 2.2 “.…that unmitigated fraud ‘Borky’ ……………………….……..….….7 2.3 Legacies of the Southern Cross…………………………….…….…..8 2.4 Fellowship and Authorship………………………………...…..………9 2.5 Appointment to NAE………………………………………….……….10 2.6 From Potsdam to Christchurch…………………………….………...11 2.7 Return to Cape Adare……………………………………….….…….12 2.8 Arrival in Winter Quarters-establishing magnetic observatory…...13 2.9 The importance of status………………………….……………….…14 3 Deeds of “Derring Doe” 3.1 Objectives-conflicting agendas…………………….……………..….15 3.2 Chivalrous deeds…………………………………….……………..…16 3.3 Scientists as Heroes……………………………….…….……………19 3.4 Confused roles……………………………….……..………….…...…21 3.5 Fame or obscurity? ……………………………………..…...….……22 2 4 “Scarcely and Exhibition of Control” 4.1 Experiments……………………………………………………………27 4.2 “The Only Intelligent Transport” …………………………………….28 4.3 “… a blasphemous frame of mind”……………………………….…32 4.4 “… far from a picnic” …………………………………………………34 4.5 “Usual retine Work diggin out Boats”………...………………..……37 4.6 Equipment…………………………………………………….……….38 4.8 Reflections on management…………………………………….…..39 5 “Walking to Christchurch” 5.1 Naval routines………………………………………………………….43 -
Arctic Marine Transport Workshop 28-30 September 2004
Arctic Marine Transport Workshop 28-30 September 2004 Institute of the North • U.S. Arctic Research Commission • International Arctic Science Committee Arctic Ocean Marine Routes This map is a general portrayal of the major Arctic marine routes shown from the perspective of Bering Strait looking northward. The official Northern Sea Route encompasses all routes across the Russian Arctic coastal seas from Kara Gate (at the southern tip of Novaya Zemlya) to Bering Strait. The Northwest Passage is the name given to the marine routes between the Atlantic and Pacific oceans along the northern coast of North America that span the straits and sounds of the Canadian Arctic Archipelago. Three historic polar voyages in the Central Arctic Ocean are indicated: the first surface shop voyage to the North Pole by the Soviet nuclear icebreaker Arktika in August 1977; the tourist voyage of the Soviet nuclear icebreaker Sovetsky Soyuz across the Arctic Ocean in August 1991; and, the historic scientific (Arctic) transect by the polar icebreakers Polar Sea (U.S.) and Louis S. St-Laurent (Canada) during July and August 1994. Shown is the ice edge for 16 September 2004 (near the minimum extent of Arctic sea ice for 2004) as determined by satellite passive microwave sensors. Noted are ice-free coastal seas along the entire Russian Arctic and a large, ice-free area that extends 300 nautical miles north of the Alaskan coast. The ice edge is also shown to have retreated to a position north of Svalbard. The front cover shows the summer minimum extent of Arctic sea ice on 16 September 2002. -
The International Space Station and the Space Shuttle
Order Code RL33568 The International Space Station and the Space Shuttle Updated November 9, 2007 Carl E. Behrens Specialist in Energy Policy Resources, Science, and Industry Division The International Space Station and the Space Shuttle Summary The International Space Station (ISS) program began in 1993, with Russia joining the United States, Europe, Japan, and Canada. Crews have occupied ISS on a 4-6 month rotating basis since November 2000. The U.S. Space Shuttle, which first flew in April 1981, has been the major vehicle taking crews and cargo back and forth to ISS, but the shuttle system has encountered difficulties since the Columbia disaster in 2003. Russian Soyuz spacecraft are also used to take crews to and from ISS, and Russian Progress spacecraft deliver cargo, but cannot return anything to Earth, since they are not designed to survive reentry into the Earth’s atmosphere. A Soyuz is always attached to the station as a lifeboat in case of an emergency. President Bush, prompted in part by the Columbia tragedy, made a major space policy address on January 14, 2004, directing NASA to focus its activities on returning humans to the Moon and someday sending them to Mars. Included in this “Vision for Space Exploration” is a plan to retire the space shuttle in 2010. The President said the United States would fulfill its commitments to its space station partners, but the details of how to accomplish that without the shuttle were not announced. The shuttle Discovery was launched on July 4, 2006, and returned safely to Earth on July 17. -
Late Quaternary Environment of Central Yakutia (NE' Siberia
Late Quaternary environment of Central Yakutia (NE’ Siberia): Signals in frozen ground and terrestrial sediments Spätquartäre Umweltentwicklung in Zentral-Jakutien (NO-Sibirien): Hinweise aus Permafrost und terrestrischen Sedimentarchiven Steffen Popp Steffen Popp Alfred-Wegener-Institut für Polar- und Meeresforschung Forschungsstelle Potsdam Telegrafenberg A43 D-14473 Potsdam Diese Arbeit ist die leicht veränderte Fassung einer Dissertation, die im März 2006 dem Fachbereich Geowissenschaften der Universität Potsdam vorgelegt wurde. 1. Introduction Contents Contents..............................................................................................................................i Abstract............................................................................................................................ iii Zusammenfassung ............................................................................................................iv List of Figures...................................................................................................................vi List of Tables.................................................................................................................. vii Acknowledgements ........................................................................................................ vii 1. Introduction ...............................................................................................................1 2. Regional Setting and Climate...................................................................................4 -
The China Relief Expedition Joint Coalition Warfare in China Summer 1900
07-02574 China Relief Cover.indd 1 11/19/08 12:53:03 PM 07-02574 China Relief Cover.indd 2 11/19/08 12:53:04 PM The China Relief Expedition Joint Coalition Warfare in China Summer 1900 prepared by LTC(R) Robert R. Leonhard, Ph.D. The Johns Hopkins University Applied Physics Laboratory This essay reflects the views of the author alone and does not necessarily imply concurrence by The Johns Hopkins University Applied Physics Laboratory (JHU/APL) or any other organization or agency, public or private. About the Author LTC(R) Robert R. Leonhard, Ph.D., is on the Principal Professional Staff of The Johns Hopkins University Applied Physics Laboratory and a member of the Strategic Assessments Office of the National Security Analysis Department. He retired from a 24-year career in the Army after serving as an infantry officer and war planner and is a veteran of Operation Desert Storm. Dr. Leonhard is the author of The Art of Maneuver: Maneuver-Warfare Theory and AirLand Battle (1991), Fighting by Minutes: Time and the Art of War (1994), The Principles of War for the Informa- tion Age (1998), and The Evolution of Strategy in the Global War on Terrorism (2005), as well as numerous articles and essays on national security issues. Foreign Concessions and Spheres of Influence China, 1900 Introduction The summer of 1900 saw the formation of a perfect storm of conflict over the northern provinces of China. Atop an anachronistic and arrogant national government sat an aged and devious woman—the Empress Dowager Tsu Hsi. -
Microfilm Publication M617, Returns from U.S
Publication Number: M-617 Publication Title: Returns from U.S. Military Posts, 1800-1916 Date Published: 1968 RETURNS FROM U.S. MILITARY POSTS, 1800-1916 On the 1550 rolls of this microfilm publication, M617, are reproduced returns from U.S. military posts from the early 1800's to 1916, with a few returns extending through 1917. Most of the returns are part of Record Group 94, Records of the Adjutant General's Office; the remainder is part of Record Group 393, Records of United States Army Continental Commands, 1821-1920, and Record Group 395, Records of United States Army Overseas Operations and Commands, 1898-1942. The commanding officer of every post, as well ad commanders of all other bodies of troops such as department, division, brigade, regiment, or detachment, was required by Army Regulations to submit a return (a type of personnel report) to The Adjutant General at specified intervals, usually monthly, on forms provided by that office. Several additions and modifications were made in the form over the years, but basically it was designed to show the units that were stationed at a particular post and their strength, the names and duties of the officers, the number of officers present and absent, a listing of official communications received, and a record of events. In the early 19th century the form used for the post return usually was the same as the one used for regimental or organizational returns. Printed forms were issued by the Adjutant General’s Office, but more commonly used were manuscript forms patterned after the printed forms. -
AQUILA BOOKS Specializing in Books and Ephemera Related to All Aspects of the Polar Regions
AQUILA BOOKS Specializing in Books and Ephemera Related to all Aspects of the Polar Regions Winter 2012 Presentation copy to Lord Northcliffe of The Limited Edition CATALOGUE 112 88 ‘The Heart of the Antarctic’ 12 26 44 49 42 43 Items on Front Cover 3 4 13 9 17 9 54 6 12 74 84 XX 72 70 21 24 8 7 7 25 29 48 48 48 37 63 59 76 49 50 81 7945 64 74 58 82 41 54 77 43 80 96 84 90 100 2 6 98 81 82 59 103 85 89 104 58 AQUILA BOOKS Box 75035, Cambrian Postal Outlet Calgary, AB T2K 6J8 Canada Cameron Treleaven, Proprietor A.B.A.C. / I.L.A.B., P.B.F.A., N.A.A.B., F.R.G.S. Hours: 10:30 – 5:30 MDT Monday-Saturday Dear Customers; Welcome to our first catalogue of 2012, the first catalogue in the last two years! We are hopefully on schedule to produce three catalogues this year with the next one mid May before the London Fairs and the last just before Christmas. We are building our e-mail list and hopefully we will be e-mailing the catalogues as well as by regular mail starting in 2013. If you wish to receive the catalogues by e-mail please make sure we have your correct e-mail address. Best regards, Cameron Phone: (403) 282-5832 Fax: (403) 289-0814 Email: [email protected] All Prices net in US Dollars. Accepted payment methods: by Credit Card (Visa or Master Card) and also by Cheque or Money Order, payable on a North American bank. -
Geochemistry of Surficial and Ice-Rafted Sediments from The
Estuarine, Coastal and Shelf Science (1999) 49, 45–59 Article No. ecss.1999.0485, available online at http://www.idealibrary.com on Geochemistry of Surficial and Ice-rafted Sediments from the Laptev Sea (Siberia) J. A. Ho¨lemanna, M. Schirmacherb, H. Kassensa and A. Prangeb aGEOMAR, Forschungszentrum fu¨r marine Geowissenschaften, Wischhofstr. 1–3, 24148 Kiel, Germany bGKSS, Forschungszentrum Geesthacht GmbH, Max-Planck-Str., 21502 Geesthacht, Germany Received 20 June 1997 and accepted in revised form 19 February 1999 The Laptev Sea, as a part of the world’s widest continental shelves surrounding the Arctic Ocean, is a key area for understanding the land–ocean interaction in high latitude regions. With a yearly freshwater input of 511 km3, the Lena River—one of the eight major world rivers—has an influencing control over the environment of this Arctic marginal sea, which is ice-covered during most of the year. In this paper, the first measurements are presented of the major and trace element distribution within the <20 ìm grain size fraction of surficial sediments and of particulate matter in new and young ice from the Laptev Sea (Siberian Arctic). The concentration and distribution of major and trace elements have been determined in 51 surficial sediment samples covering the whole Laptev Sea shelf south of the 50 m isobath. Thirty-one samples of particulate matter in newly formed ice were taken during the freeze-up period in 1995. Median concentration levels of heavy metals in surficial sediments (Ni (46 ìgg"1), Cu (26 ìgg"1), Zn (111 ìgg"1) and Pb (21 ìgg"1) are within the concentration range of marine unpolluted sediments. -
A NTARCTIC Southpole-Sium
N ORWAY A N D THE A N TARCTIC SouthPole-sium v.3 Oslo, Norway • 12-14 May 2017 Compiled and produced by Robert B. Stephenson. E & TP-32 2 Norway and the Antarctic 3 This edition of 100 copies was issued by The Erebus & Terror Press, Jaffrey, New Hampshire, for those attending the SouthPole-sium v.3 Oslo, Norway 12-14 May 2017. Printed at Savron Graphics Jaffrey, New Hampshire May 2017 ❦ 4 Norway and the Antarctic A Timeline to 2006 • Late 18th Vessels from several nations explore around the unknown century continent in the south, and seal hunting began on the islands around the Antarctic. • 1820 Probably the first sighting of land in Antarctica. The British Williams exploration party led by Captain William Smith discovered the northwest coast of the Antarctic Peninsula. The Russian Vostok and Mirnyy expedition led by Thaddeus Thadevich Bellingshausen sighted parts of the continental coast (Dronning Maud Land) without recognizing what they had seen. They discovered Peter I Island in January of 1821. • 1841 James Clark Ross sailed with the Erebus and the Terror through the ice in the Ross Sea, and mapped 900 kilometres of the coast. He discovered Ross Island and Mount Erebus. • 1892-93 Financed by Chr. Christensen from Sandefjord, C. A. Larsen sailed the Jason in search of new whaling grounds. The first fossils in Antarctica were discovered on Seymour Island, and the eastern part of the Antarctic Peninsula was explored to 68° 10’ S. Large stocks of whale were reported in the Antarctic and near South Georgia, and this discovery paved the way for the large-scale whaling industry and activity in the south. -
Inventory Acc.12696 William Laird Mckinlay
Acc.12696 December 2006 Inventory Acc.12696 William Laird McKinlay National Library of Scotland Manuscripts Division George IV Bridge Edinburgh EH1 1EW Tel: 0131-466 2812 Fax: 0131-466 2811 E-mail: [email protected] © Trustees of the National Library of Scotland Correspondence and papers of William Laird McKinlay, Glasgow. Background William McKinlay (1888-1983) was for most of his working life a teacher and headmaster in the west of Scotland; however the bulk of the papers in this collection relate to the Canadian National Arctic Expedition, 1913-18, and the part played in it by him and the expedition leader, Vilhjalmur Stefansson. McKinlay’s account of his experiences, especially those of being shipwrecked and marooned on Wrangel Island, off the coast of Siberia, were published by him in Karluk (London, 1976). For a rather more detailed list of nos.1-27, and nos.43-67 (listed as nos.28-52), see NRA(S) survey no.2546. Further items relating to McKinlay were presented in 2006: see Acc.12713. Other items, including a manuscript account of the expedition and the later activities of Stefansson – much broader in scope than Karluk – have been deposited in the National Archives of Canada, in Ottawa. A small quantity of additional documents relating to these matters can be found in NRA(S) survey no.2222, papers in the possession of Dr P D Anderson. Extent: 1.56 metres Deposited in 1983 by Mrs A.A. Baillie-Scott, the daughter of William McKinlay, and placed as Dep.357; presented by the executor of Mrs Baillie-Scott’s estate, November 2006. -
The Contribution of Shore Thermoabrasion to the Laptev Sea Sediment Balance
THE CONTRIBUTION OF SHORE THERMOABRASION TO THE LAPTEV SEA SEDIMENT BALANCE F.E. Are Petersburg State University of Means of Communications, Moskovsky av. 9, St.-Petersburg, 190031, Russia e-mail: [email protected] Abstract A schematic map of Laptev Sea shore dynamics is compiled for the first time, using available published data. It shows the distribution of thermoabrasion shores, mean long-term shore retreat rates, and areas of seabed ero- sion and accretion. The amount of sediment released to the sea from the 85 km Anabar-Olenyok section of the coast is calculated, as an example, at 3.4 Mt/year. These results are compared with published data on sediment transport of rivers running into the Laptev Sea. Estimates of the Lena River discharge range from 12 to 21 Mt/year, of which only 2.1 to 3.5 Mt may reach the sea. The analysis shows that the input of thermoabrasion at mean shoreline retreat rates of 0.7 to 0.9 m/year is at least of the same order as the river input and may great- ly exceed it. Introduction ble to determine the input from shore thermoabrasion offshore more accurately. Thousands of kilometres of Arctic sea coast retreat at rates 2-6 m/year under the action of thermoabrasion1 Maps of shore dynamics are needed to solve this (Are, 1985; Barnes et al., 1991). Tens of square kilome- problem and others related to climate change impacts. tres of Arctic land therefore are consumed by the sea Such maps have been compiled for about 650 km of every year.