2002-2003 AWS Field Report
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Office of Polar Programs
DEVELOPMENT AND IMPLEMENTATION OF SURFACE TRAVERSE CAPABILITIES IN ANTARCTICA COMPREHENSIVE ENVIRONMENTAL EVALUATION DRAFT (15 January 2004) FINAL (30 August 2004) National Science Foundation 4201 Wilson Boulevard Arlington, Virginia 22230 DEVELOPMENT AND IMPLEMENTATION OF SURFACE TRAVERSE CAPABILITIES IN ANTARCTICA FINAL COMPREHENSIVE ENVIRONMENTAL EVALUATION TABLE OF CONTENTS 1.0 INTRODUCTION....................................................................................................................1-1 1.1 Purpose.......................................................................................................................................1-1 1.2 Comprehensive Environmental Evaluation (CEE) Process .......................................................1-1 1.3 Document Organization .............................................................................................................1-2 2.0 BACKGROUND OF SURFACE TRAVERSES IN ANTARCTICA..................................2-1 2.1 Introduction ................................................................................................................................2-1 2.2 Re-supply Traverses...................................................................................................................2-1 2.3 Scientific Traverses and Surface-Based Surveys .......................................................................2-5 3.0 ALTERNATIVES ....................................................................................................................3-1 -
Rapid Transport of Ash and Sulfate from the 2011 Puyehue-Cordón
PUBLICATIONS Journal of Geophysical Research: Atmospheres RESEARCH ARTICLE Rapid transport of ash and sulfate from the 2011 10.1002/2017JD026893 Puyehue-Cordón Caulle (Chile) eruption Key Points: to West Antarctica • Ash and sulfate from the June 2011 Puyehue-Cordón Caulle eruption were Bess G. Koffman1,2 , Eleanor G. Dowd1 , Erich C. Osterberg1 , David G. Ferris1, deposited in West Antarctica 3 3 3,4 1 • Depositional phasing and duration Laura H. Hartman , Sarah D. Wheatley , Andrei V. Kurbatov , Gifford J. Wong , 5 6 3,4 4 suggest rapid transport through the Bradley R. Markle , Nelia W. Dunbar , Karl J. Kreutz , and Martin Yates troposphere • Ash/sulfate phasing, ash size 1Department of Earth Sciences, Dartmouth College, Hanover, New Hampshire, USA, 2Now at Department of Geology, Colby distributions, and geochemistry College, Waterville, Maine, USA, 3Climate Change Institute, University of Maine, Orono, Maine, USA, 4School of Earth and distinguish this midlatitude eruption Climate Sciences, University of Maine, Orono, Maine, USA, 5Department of Earth and Space Sciences, University of from low- and high-latitude eruptions Washington, Seattle, Washington, USA, 6New Mexico Bureau of Geology and Mineral Resources, Socorro, New Mexico, USA Supporting Information: • Supporting Information S1 Abstract The Volcanic Explosivity Index 5 eruption of the Puyehue-Cordón Caulle volcanic complex (PCC) in central Chile, which began 4 June 2011, provides a rare opportunity to assess the rapid transport and Correspondence to: deposition of sulfate and ash from a midlatitude volcano to the Antarctic ice sheet. We present sulfate, B. G. Koffman, [email protected] microparticle concentrations of fine-grained (~5 μm diameter) tephra, and major oxide geochemistry, which document the depositional sequence of volcanic products from the PCC eruption in West Antarctic snow and shallow firn. -
A NEWS BULLETIN Published Quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC)
A NEWS BULLETIN published quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC) An English-born Post Office technician, Robin Hodgson, wearing a borrowed kilt, plays his pipes to huskies on the sea ice below Scott Base. So far he has had a cool response to his music from his New Zealand colleagues, and a noisy reception f r o m a l l 2 0 h u s k i e s . , „ _ . Antarctic Division photo Registered at Post Ollice Headquarters. Wellington. New Zealand, as a magazine. II '1.7 ^ I -!^I*"JTr -.*><\\>! »7^7 mm SOUTH GEORGIA, SOUTH SANDWICH Is- . C I R C L E / SOUTH ORKNEY Is x \ /o Orcadas arg Sanae s a Noydiazarevskaya ussr FALKLAND Is /6Signyl.uK , .60"W / SOUTH AMERICA tf Borga / S A A - S O U T H « A WEDDELL SHETLAND^fU / I s / Halley Bav3 MINING MAU0 LAN0 ENOERBY J /SEA uk'/COATS Ld / LAND T> ANTARCTIC ••?l\W Dr^hnaya^^General Belgrano arg / V ^ M a w s o n \ MAC ROBERTSON LAND\ '■ aust \ /PENINSULA' *\4- (see map betowi jrV^ Sobldl ARG 90-w {■ — Siple USA j. Amundsen-Scott / queen MARY LAND {Mirny ELLSWORTH" LAND 1, 1 1 °Vostok ussr MARIE BYRD L LAND WILKES LAND ouiiiv_. , ROSS|NZJ Y/lnda^Z / SEA I#V/VICTORIA .TERRE , **•»./ LAND \ /"AOELIE-V Leningradskaya .V USSR,-'' \ --- — -"'BALLENYIj ANTARCTIC PENINSULA 1 Tenitnte Matianzo arg 2 Esptrarua arg 3 Almirarrta Brown arc 4PttrtlAHG 5 Otcipcion arg 6 Vtcecomodoro Marambio arg * ANTARCTICA 7 Arturo Prat chile 8 Bernardo O'Higgins chile 1000 Miles 9 Prasid«fTtB Frei chile s 1000 Kilometres 10 Stonington I. -
U.S. Advance Exchange of Operational Information, 2005-2006
Advance Exchange of Operational Information on Antarctic Activities for the 2005–2006 season United States Antarctic Program Office of Polar Programs National Science Foundation Advance Exchange of Operational Information on Antarctic Activities for 2005/2006 Season Country: UNITED STATES Date Submitted: October 2005 SECTION 1 SHIP OPERATIONS Commercial charter KRASIN Nov. 21, 2005 Depart Vladivostok, Russia Dec. 12-14, 2005 Port Call Lyttleton N.Z. Dec. 17 Arrive 60S Break channel and escort TERN and Tanker Feb. 5, 2006 Depart 60S in route to Vladivostok U.S. Coast Guard Breaker POLAR STAR The POLAR STAR will be in back-up support for icebreaking services if needed. M/V AMERICAN TERN Jan. 15-17, 2006 Port Call Lyttleton, NZ Jan. 24, 2006 Arrive Ice edge, McMurdo Sound Jan 25-Feb 1, 2006 At ice pier, McMurdo Sound Feb 2, 2006 Depart McMurdo Feb 13-15, 2006 Port Call Lyttleton, NZ T-5 Tanker, (One of five possible vessels. Specific name of vessel to be determined) Jan. 14, 2006 Arrive Ice Edge, McMurdo Sound Jan. 15-19, 2006 At Ice Pier, McMurdo. Re-fuel Station Jan. 19, 2006 Depart McMurdo R/V LAURENCE M. GOULD For detailed and updated schedule, log on to: http://www.polar.org/science/marine/sched_history/lmg/lmgsched.pdf R/V NATHANIEL B. PALMER For detailed and updated schedule, log on to: http://www.polar.org/science/marine/sched_history/nbp/nbpsched.pdf SECTION 2 AIR OPERATIONS Information on planned air operations (see attached sheets) SECTION 3 STATIONS a) New stations or refuges not previously notified: NONE b) Stations closed or refuges abandoned and not previously notified: NONE SECTION 4 LOGISTICS ACTIVITIES AFFECTING OTHER NATIONS a) McMurdo airstrip will be used by Italian and New Zealand C-130s and Italian Twin Otters b) McMurdo Heliport will be used by New Zealand and Italian helicopters c) Extensive air, sea and land logistic cooperative support with New Zealand d) Twin Otters to pass through Rothera (UK) upon arrival and departure from Antarctica e) Italian Twin Otter will likely pass through South Pole and McMurdo. -
The Antarctic Sun, December 25, 2005
December 25, 2005 Scientists seek to label whale species By Steven Profaizer Sun staff Patches of pure white splashed on an inky black body. Two-meter-tall dorsal fin slicing through the water’s surface. An attraction at SeaWorld. A pack hunter with cunning intelligence and stunning power. The killer whale, or orca, is one of the most universally known animals in the world. They are also one of the most wide- spread mammals, second only to humans, and inhabit all of the world’s oceans. Yet scientists are still working to deter- mine how many species of killer whales exist. Only one species is currently rec- ognized, but many people, including researcher Robert Pitman, believe there may be two additional species among the estimated 20,000 to 80,000 killer whales that inhabit Antarctic waters. Pitman is far from the first to believe this: Soviet 5 Union whalers in the early 1980s first Deep Freeze turns 0 observed the killer whales’ differences in diet, preferred habitat and coloring. He By Emily Stone does, however, hope to be part of the team Sun staff that finally solves the mystery. Al Hisey spent one of his first nights at McMurdo Station by accident. Pitman, of the National Oceanic and It was 1955, and he was ferrying supplies by tractor from Navy ships across the Atmospheric Administration, led a team sea ice of McMurdo Sound to the spot on Ross Island where the station was being to Antarctica last year on a two-week mis- built. During one of the first trips, there was a major break in the ice between the sion that used sophisticated technology to fledgling station and the ships. -
2006 NSIDC Annual Report
National Snow and Ice Data Center World Data Center for Glaciology, Boulder Annual Report 2006 Supporting Cryospheric Research Since 1976 National Snow and Ice Data Center World Data Center for Glaciology, Boulder Annual Report 2006 Cover image captions (clockwise from upper left) During the IceTrek expedition, team members tow a sled with equipment to install on an Antarctic iceberg. (Courtesy Ted Scambos, NSIDC) This image shows the Beaufort Sea Polynya. A polynya, or area of persistent open water surrounded by ice, appeared during the summer 2006 Arctic sea ice melt season. The polynya is the dark area of open water; to the left is the coastline of Alaska, showing fall foliage color, and to the bottom right is the North Pole. This image is from the Moderate Resolution Imaging Spectroradiometer (MODIS) sensor, which flies on the NASA Terra and Aqua satellites. (Courtesy NSIDC) Toboggan Glacier, Alaska, in 1909. This image one of a pair of photographs available through the “Repeat Photography of Glaciers” portion of NSIDC’s online Glacier Photograph Collection. These photograph pairs illustrate the dramatic changes that researchers have observed in glaciers worldwide over the past century. (Photograph courtesy of Sidney Paige/USGS Photo Library, available through NSIDC’s online Glacier Photograph Collection). Members of the IceTrek expedition practiced installing their meteorological equipment on this small Antarctic iceberg, nicknamed “Chip,” before installing the equipment permanently on larger icebergs. (Courtesy Ted Scambos, NSIDC) Supporting Cryospheric Research Since 1976 Supporting Cryospheric Research Since 1976 ii Supporting Cryospheric Research Since 1976 Contents Table of Contents Introduction 1 Highlights 3 Data Management at NSIDC 5 Programs 10 The Distributed Active Archive Center (DAAC) 10 The Arctic System Science (ARCSS) Data Coordination Center (ADCC) 14 U.S. -
Siple Dome Ice Reveals Two Modes of Millennial CO2 Change During the Last Ice Age
ARTICLE Received 4 Dec 2013 | Accepted 26 Mar 2014 | Published 29 Apr 2014 DOI: 10.1038/ncomms4723 OPEN Siple Dome ice reveals two modes of millennial CO2 change during the last ice age Jinho Ahn1 & Edward J. Brook2 Reconstruction of atmospheric CO2 during times of past abrupt climate change may help us better understand climate-carbon cycle feedbacks. Previous ice core studies reveal simultaneous increases in atmospheric CO2 and Antarctic temperature during times when Greenland and the northern hemisphere experienced very long, cold stadial conditions during the last ice age. Whether this relationship extends to all of the numerous stadial events in the Greenland ice core record has not been clear. Here we present a high-resolution record of atmospheric CO2 from the Siple Dome ice core, Antarctica for part of the last ice age. We find that CO2 does not significantly change during the short Greenlandic stadial events, implying that the climate system perturbation that produced the short stadials was not strong enough to substantially alter the carbon cycle. 1 School of Earth and Environmental Sciences, Seoul National University, Seoul 151742, Korea. 2 College of Earth, Ocean and Atmospheric Sciences, Oregon State University, Corvallis, Oregon 97331, USA. Correspondence and requests for materials should be addressed to J.A. (email: [email protected]). NATURE COMMUNICATIONS | 5:3723 | DOI: 10.1038/ncomms4723 | www.nature.com/naturecommunications 1 & 2014 Macmillan Publishers Limited. All rights reserved. ARTICLE NATURE COMMUNICATIONS | DOI: 10.1038/ncomms4723 ce core records from Greenland reveal a detailed history of the last ice age, marine sediment records indicate shoaled abrupt climate change during the last glacial period. -
Blue Sky Airlines
GPS Support to the National Science Foundation Office of Polar Programs 2001-2002 Season Report GPS Support to the National Science Foundation Office of Polar Programs 2001-2002 Season Report April 15, 2002 Bjorn Johns Chuck Kurnik Shad O’Neel UCAR/UNAVCO Facility University Corporation for Atmospheric Research 3340 Mitchell Lane Boulder, CO 80301 (303) 497-8034 www.unavco.ucar.edu Support funded by the National Science Foundation Office of Polar Programs Scientific Program Order No. 2 (EAR-9903413) to Cooperative Agreement No. 9732665 Cover photo: Erebus Ice Tongue Mapping – B-017 1 UNAVCO 2001-2002 Report Table of Contents: Summary........................................................................................................................................................ 3 Table 1 – 2001-2001 Antarctic Support Provided................................................................................. 4 Table 2 – 2001 Arctic Support Provided................................................................................................ 4 Science Support............................................................................................................................................. 5 Training.................................................................................................................................................... 5 Field Support........................................................................................................................................... 5 Data Processing .................................................................................................................................... -
Gazette Quarterly
EEXXPPLLOORREERR’’SS GGAAZZEETTTTEE Published Quarterly in Pensacola, Florida USA for the Old Antarctic Explorers Association Uniting All OAEs in Perpetuating the Memory of United States Involvement in Antarctica Volume 18, Issue 3 Old Antarctic Explorers Association, Inc Jul-Sep 2018 Photo courtesy of Sydney Cullis The HMS Terra Nova departing Simon’s Bay for Antarctica in 1910. Painting commissioned by Sydney Cullis The Antarctic-African Connection By Ed Hamblin off our tour with four nights there. I thought we might be hen one thinks of Africa, probably jungles, rugged able to get together for a drink or something and socialize a W landscapes, and wild animals are what come to mind. bit. After a series of back and forth e-mails, we had a date But Antarctica? during some of our tour “dead time” to meet up. Also Last fall, my wife and I decided to take a trip to South through those e-mails, Dr. Cullis started apprising me of the Africa, as part of an organized tour in order to get an Cape Town area Antarctic points of interest, and forwarded opportunity to see routine African “stuff”. We booked a me a few pictures. Thanks to the pictures, I found out Cape two-week trip for April of 2018 with some “travel buddies” Town has been a stopping off point for Antarctic we had met previously in the Galapagos Islands. Shortly expeditions dating to the 18th century. Many of the early after that, I decided to see if I could connect with one of our explorers we are all familiar with spent time in Cape Town international OAEA members, Dr. -
Waba Directory 2003
DIAMOND DX CLUB www.ddxc.net WABA DIRECTORY 2003 1 January 2003 DIAMOND DX CLUB WABA DIRECTORY 2003 ARGENTINA LU-01 Alférez de Navió José María Sobral Base (Army)1 Filchner Ice Shelf 81°04 S 40°31 W AN-016 LU-02 Almirante Brown Station (IAA)2 Coughtrey Peninsula, Paradise Harbour, 64°53 S 62°53 W AN-016 Danco Coast, Graham Land (West), Antarctic Peninsula LU-19 Byers Camp (IAA) Byers Peninsula, Livingston Island, South 62°39 S 61°00 W AN-010 Shetland Islands LU-04 Decepción Detachment (Navy)3 Primero de Mayo Bay, Port Foster, 62°59 S 60°43 W AN-010 Deception Island, South Shetland Islands LU-07 Ellsworth Station4 Filchner Ice Shelf 77°38 S 41°08 W AN-016 LU-06 Esperanza Base (Army)5 Seal Point, Hope Bay, Trinity Peninsula 63°24 S 56°59 W AN-016 (Antarctic Peninsula) LU- Francisco de Gurruchaga Refuge (Navy)6 Harmony Cove, Nelson Island, South 62°18 S 59°13 W AN-010 Shetland Islands LU-10 General Manuel Belgrano Base (Army)7 Filchner Ice Shelf 77°46 S 38°11 W AN-016 LU-08 General Manuel Belgrano II Base (Army)8 Bertrab Nunatak, Vahsel Bay, Luitpold 77°52 S 34°37 W AN-016 Coast, Coats Land LU-09 General Manuel Belgrano III Base (Army)9 Berkner Island, Filchner-Ronne Ice 77°34 S 45°59 W AN-014 Shelves LU-11 General San Martín Base (Army)10 Barry Island in Marguerite Bay, along 68°07 S 67°06 W AN-016 Fallières Coast of Graham Land (West), Antarctic Peninsula LU-21 Groussac Refuge (Navy)11 Petermann Island, off Graham Coast of 65°11 S 64°10 W AN-006 Graham Land (West); Antarctic Peninsula LU-05 Melchior Detachment (Navy)12 Isla Observatorio -
II. Expedition Dates
Information Exchange Under United States Antarctic Activities Articles III and VII(5) of the Modifications of Activities Planned for 2003-2004 ANTARCTIC TREATY II. Expedition Dates II. Expedition Dates Section II of the Modifications of Activities Planned for 2003-2004 lists the actual dates of significant events occurring during this time period. Significant Dates of Expeditions Date Activity 05 Apr 03 LMG03-04 10 May 03 LMG03-04A 16 June 03 LMG03-05 16 Aug 03 LMG03-05A 21 Aug 03 First flight to McMurdo Station for Winfly operations 22 Aug 03 NBP03-04C 07 Sep 03 LMG Maintenance open period for maintenance 14 Sep 03 NBP03-04C 22 Sep 03 LMG03-06 28 Sep 03 Palmer Station annual relief 30 Sep 03 First C-141 mission to McMurdo Station during Ice Runway period McMurdo Station commenced summer operations (1 of 19) 05 Oct 03 Marble Point opens 01 Oct 03 First C-17 mission of the season to McMurdo Station (1 of 12) 09 Oct 03 NBP03-04D 10 Oct 03 LMG03-07 (Palmer Station Shuttle) 14 Oct 03 Pieter J. Lenie Field Station (Copacabana) opens 14 Oct 03 Odell Glacier Camp Opens 14 Oct 03 Lake Hoare Camp opens 16 Oct 03 Lake Bonney Camp opens 17 Oct 03 F6 Camp opens 18 Oct 03 Lake Fryxell Camp opens National Science Foundation 2 Arlington, Virginia 22230 October 1, 2004 Information Exchange Under United States Antarctic Activities Articles III and VII(5) of the Modifications of Activities Planned for 2003-2004 ANTARCTIC TREATY II. Expedition Dates Date Activity 22 Oct 03 Three (3) 109th AW LC-130’s arrive McMurdo Station to start on-continent missions -
Wilderness and Aesthetic Values of Antarctica
Wilderness and Aesthetic Values of Antarctica Abstract Antarctica is the least inhabited region in the world and has therefore had the least influence from human activities and, unlike the majority of the Earth’s continents and oceans, can still be considered as mostly wilderness. As every visitor to Antarctica knows, its landscapes are exceptionally beautiful. It was the recognition of the importance of these characteristics that resulted in their protection being included in the Madrid Protocol. Both wilderness and aesthetic values can be impaired by human activities in a variety of ways with the severity varying from negligible to severe, according to the type Protocol on Environmental Protec tion to the Antarctic Trea ty - of activity and its duration, spatial extent and intensity. A map of infrastructure and major travel routes the "M adrid Protocol" in Antarctica will be the first step in visually representing where wilderness and aesthetic values Article 3[1] may be impacted. It is hoped that this will stimulate further discussion on how to describe, acknowledge, The protection of the Antarctic environment and dependent an d associated ecosystems and the intrinsic value of Antarctica, understand and further protect the wilderness and aesthetic values of Antarctica. including its wilderness and aesthetic values and its value as an area for the conduct of scientific research, in particular research essential to understanding the global environment, shall be fundamental considerations in the planning and condu ct of all activities