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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. -
Mcmurdo Dry Valleys, Southern Victoria Land
Measure 1 (2004) Annex Management Plan for Antarctic Specially Managed Area No. 2 MCMURDO DRY VALLEYS, SOUTHERN VICTORIA LAND 1. Description of values to be protected and activities to be managed The McMurdo Dry Valleys are characterized as the largest relatively ice-free region in Antarctica with approximately thirty percent of the ground surface largely free of snow and ice. The region encompasses a cold desert ecosystem, whose climate is not only cold and extremely arid (in the Wright Valley the mean annual temperature is –19.8°C and annual precipitation is less than 100 mm water equivalent), but also windy. The landscape of the Area contains glaciers, mountain ranges, ice-covered lakes, meltwater streams, arid patterned soils and permafrost, sand dunes, and interconnected watershed systems. These watersheds have a regional influence on the McMurdo Sound marine ecosystem. The Area’s location, where large-scale seasonal shifts in the water phase occur, is of great importance to the study of climate change. Through shifts in the ice-water balance over time, resulting in contraction and expansion of hydrological features and the accumulations of trace gases in ancient snow, the McMurdo Dry Valley terrain also contains records of past climate change. The extreme climate of the region serves as an important analogue for the conditions of ancient Earth and contemporary Mars, where such climate may have dominated the evolution of landscape and biota. The Area is characterized by unique ecosystems of low biodiversity and reduced food web complexity. However, as the largest ice-free region in Antarctica, the McMurdo Dry Valleys also contain relatively diverse habitats compared with other ice-free areas. -
Draft ASMA Plan for Dry Valleys
Measure 18 (2015) Management Plan for Antarctic Specially Managed Area No. 2 MCMURDO DRY VALLEYS, SOUTHERN VICTORIA LAND Introduction The McMurdo Dry Valleys are the largest relatively ice-free region in Antarctica with approximately thirty percent of the ground surface largely free of snow and ice. The region encompasses a cold desert ecosystem, whose climate is not only cold and extremely arid (in the Wright Valley the mean annual temperature is –19.8°C and annual precipitation is less than 100 mm water equivalent), but also windy. The landscape of the Area contains mountain ranges, nunataks, glaciers, ice-free valleys, coastline, ice-covered lakes, ponds, meltwater streams, arid patterned soils and permafrost, sand dunes, and interconnected watershed systems. These watersheds have a regional influence on the McMurdo Sound marine ecosystem. The Area’s location, where large-scale seasonal shifts in the water phase occur, is of great importance to the study of climate change. Through shifts in the ice-water balance over time, resulting in contraction and expansion of hydrological features and the accumulations of trace gases in ancient snow, the McMurdo Dry Valley terrain also contains records of past climate change. The extreme climate of the region serves as an important analogue for the conditions of ancient Earth and contemporary Mars, where such climate may have dominated the evolution of landscape and biota. The Area was jointly proposed by the United States and New Zealand and adopted through Measure 1 (2004). This Management Plan aims to ensure the long-term protection of this unique environment, and to safeguard its values for the conduct of scientific research, education, and more general forms of appreciation. -
Terrestrial Biology
Terrestrial biology Impacts of ultraviolet-B radiation and regional warming on antarctic vascular plants THOMAS A. DAY, CHRISTOPHER T. R UHLAND, and FUSHENG XIONG, Department of Plant Biology, Arizona State University, Tempe, Arizona 85287-1601 he Antarctic Peninsula provides a unique opportunity to tion. Additionally, key enzymes in the photosynthetic Calvin T examine the influence of climate change on plants. Cycle of these species appear sensitive to higher temperatures Stratospheric ozone depletion events over the continent dur- and further depress photosynthetic rates. ing spring and early summer lead to well-documented Because of the sensitivity of the photosynthetic apparatus enhanced levels of ultraviolet-B (UV-B) radiation [280-320 to higher temperatures in these species, continued regional nanometers (nm); UV-B] levels (Booth et al. 1994; Madronich warming might prove detrimental to their performance on the et al. 1995). In addition, mean summer air temperatures along peninsula, but an assessment of their performance under ris- the peninsula have risen more than 1°C in the last 45 years ing temperatures also depends on (Smith 1994; Smith, Stammerjohn, and Baker 1996). • their ability to acclimate photosynthetically to warmer The 1996–1997 field season (November to March) was the growing temperatures as well as second year of our main field experiment on Stepping Stones • how well photosynthetic rates predict plant growth rates Island, near Palmer Station, Antarctic Peninsula. We are using and overall performance. filters to manipulate UV levels and temperatures around natu- With respect to acclimation, when we grew both species rally growing plants of Deschampsia antarctica (antarctic hair under contrasting temperature regimes (ranging from 7 to 20°) grass) and Colobanthus quitensis (antarctic pearlwort), the in growth chambers at Arizona State University, their photo- only vascular plant species native to Antarctica. -
Approaches to Antarctic Solid Waste Management Logistics: Past, Present, Potential
Approaches to Antarctic solid waste management logistics: past, present, potential Sandra Potter, Bachelor of Fine Arts Submitted in partial fulfilment for Master of Environmental Management Centre for Environmental Studies University of Tasmania Hobart, Tasmania, Australia May 2003 Statement of Authenticity This thesis contains no material which has been accepted for the award of any other degree or diploma in any university and to the best of the author's knowledge and belief the thesis contains no copy or paraphrase of material previously published or written by other persons except where due reference is made in the text of the thesis. Sandra Potter Abstract Past and present solid waste management practices in Antarctica, and the local impacts of waste, are described. The provisions of Annex III of the Protocol on Environmental Protection to the Antarctic Treaty (the Madrid Protocol) are reviewed, in particular the requirement to remove waste from Antarctica and clean up past waste disposal sites and abandoned infrastructure. It is noted that the language used in the Protocol, and the absence of clearly defined environmental standards for the region, make examination of the compliance of signatories problematic. Australian, French, Russian, Chinese and Japanese program policy and operations in East Antarctica are discussed. Issues related to the on-site processing, containment and shipment of waste are considered in an Integrated Solid Waste Management System framework. Particular reference is made to the differing demands presented by the erection and demolition of facilities, the handling of annually generated and principally non-hazardous domestic waste, and the clean up of abandoned, and often contaminated, sites. -
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 -
Mmymtmmx* a N E W S B U L L E T I N
mmymtmmx* A N E W S B U L L E T I N published b y t h e NEW ZEALAND ANTARCTIC SOCIETY 7i^ ■ I l , U.S.N.S. MAUMEE DOCKED AT McMURDO. Official U.S. Navy photo. Vol. 5, No. 9 MARCH, 1970 AUSTRALIA y»L/ E 'T w / ) WELLINGTONI -SCHRISTCHURCH I NEW ZEALAND TASMANIA VOSS DEPENDED ^ <k \^«**V t\ / Byrd(US)* ANTARCTICA, \ / l\ Ah Pliteiu <US)0<' Alferej Sobnl (Arj) < J,Gtncnl Belfrano \ / W N G M A L ) 0 \ j H . l l t y B a y ( U K ) / ^ < / (USSR)X%*r)\»»A-^ %^D "VVAY) I * aXA Tsplent."xsfi&** ^J#/&**?&- (USSM ^V^X^^ ^'^ 0r< DRAWN BY DEPARTMENT OF LANDS * SURVEY WELLINGTON. NEW ZEALAND. AUG IM9 3rd EDITION MLiHTOA IB ©INKD" (Successor to "Antarctic News Bulletin") Vol. 5. No. 9 57th ISSUE MARCH, 1970 Contributions, enquiries, etc., to the Acting Editor, C/- P.O. Box 2110, Wellington. Business Communications, Subscriptions, etc., to: Secretary, New Zealand Antarctic Society, P.O. Box 2110, Wellington, N.Z. CONTENTS ■ EXPEDITIONS New Zealand The First Year at Vanda Station: S. K. Cutfield U.S.A. France Belgium Australia U.S.S.R. South Africa Japan 389, 406 United Kingdom Argentina Sub-Antarctic Islands Flights to the Pole Antarctic Bookshelf Co-operation in Antarctic Research Antarctic Tourism 403 March, 1970 BAD WEATHER HAMPERS ACTIVITIES AT NEW ZEALAND STATIONS At Scott Base. Vanda Station and in the field, a very extensive summer programme was carried through despite much stormy weather and in the face of unexpected transport and other difficulties. Leader Bruce Willis reported late in AT TERRA NOVA BAY December: Unfortunately not as much ground as "With such a splendid start to the expected was covered by the four-man month as the celebration of the tenth DS1R geological party at Terro Nova anniversary of the signing of the Ant Bay owing to a combination of deep arctic Treaty, it seemed that we were soft snow and warm weather, but never set for a period of concerted activity. -
Nan Ummsmmm a N E W S B U L L E T I N
nan UmmSmmm A N E W S B U L L E T I N p u b l i s h e d q u a r t e r l y b y t h e NEW ZEALAND ANTARCTIC SOCIETY (INC) BORGA BASE. A WINTERING STATION OF THE SOUTH AFRICAN NATIONAL ANTARCTIC EXPEDITION IN WESTERN QUEEN MAUD LAND. ESTABLISHED IN MAY. 1969' THE BASE IS 350 KILOMETRES SOUTH OF THE MAIN BASE. SANAE. IT WAS BUILT AT A HEIGHT OF 7920FT IN THE BORGE MASSIF. NEAR THE HULDRESLOITTET NUNATAK, AND IS LOCATED AT 72 DEG 50 MIN S - 3DEG 48 MIN W. South African Geological Survey Photo | '.▶'Hev*^ ■ w. ■_■_ /+:-£*&■ ' •Tf*^*' Registered at Post Office Headquarters. Vol. 7. No. 1 Wellington, New Zealand, as a magazine. March, 1974 e-.i.-. M' AUSTRALIA CHRISTCHURCH NEW ZEALAND TASMANIA /^WsDEPENDENcy^. v£ft\ \**° \ 'Sis \ / - V\ . H i lt l e t te f U ! . ) /y . \\(nz) w |X XrS8* •V, / Byrd (US)* ANTARCTICA, Alferei Sobral (Arg)* />*> -toa \ - ^ING mauo\ « Molodyozhnaya^'^. VO/?way * xA ass** (USSR) (USSR)/^ * I B o r g M a s s i f \ <^*/SI{ny I (UK) DRAWN BY DEPARTMENT OF LANDS 4 SURVEY WELLINGTON. NEW ZEALAND. AUG 1969 3rd EDITION vrii::.T■ e<ui^*[PiiLB(S1Fa(B*d (Successor to "Antarctic News Bulletin") Vol. 7. No. 1 73rd Issue Editor: J. M. CAFFIN, 35 Chepstow Avenue, Christchurch 5. Address all contributions, enquiries, etc., to-the Editor. All Business Communications, Subscriptions, etc., to: Secretary, New Zealand Antarctic Society (Inc.), P.O. Box 1223, Christchurch, N.Z. CONTENTS ARTICLES POLAR CRIMINAL LAW 27, 28, 29 QUAIL ISLAND 31, 32 POLAR ACTIVITIES NEW ZEALAND 2, 3, 4, 5, 6, 7, 8 UNITED KINGDOM 9, 10, 11 AUSTRALIA 19, 20, 21, 22 UNITED STATES 12, 13, 14, 15, 16, 17, 18 SOVIET UNION 30 FRANCE 23, 24 SOUTH AFRICA 25, 26 ARGENTINE ITALY GENERAL TOURISM OBITUARY THE READER WRITES ANTARCTIC BOOKSHELF 34, 35, 36 Winter is always cold in Antarctica; this year it will be colder for the men living there. -
The First 50 Years of Victoria University of Wellington Antarctic
The First 50 Years of Victoria University of Wellington Antarctic Research Centre Antarctic Expeditions Victoria University of Wellington, PO Box 600, Wellington, New Zealand Phone +64-4-463 6587, Fax +64-4-463 5186 E-mail [email protected] www.vuw.ac.nz/antarctic Recollections and reunion programme Victoria University of Wellington 30 June – 1 July 2007 Table of Contents inside front cover Welcome . .2 Recent Benefactors . .3 Reunion programme . .4 Reunion participants . .6 The Birth of VUWAE . .10 Members of VUWAE: 1957-2007 . .12 Recollections of the first 50 years . .18 Victoria University of Wellington Antarctic Expeditions: The First 50 Years Welcome Recent Benefactors Prior to my first departure for the Ice on a VUWAE expedition, I heard the Throughout the history of VUWAE, Harry Keys, Barry Kohn, Phil Kyle, pre-season talk that ARC Director, Professor Peter Barrett claims to have inherited from Bob Clark. organizations and individuals have sponsored Judy Lawrence, Barrie McKelvey, John and supported the programme with equipment Nankervis, Anthony Parker, Russell Plume, “There are basically only two things to remember”, he instructed. “Firstly, help out and money. Most recently the Antarctic Bryan Sissons, David Skinner, Tim Stern, with the boring jobs at Scott Base. This will put you in a good position with base Research Centre has received a $1 million David Sugden, Tony Taylor, John Thurston, staff, which will make their job easier, and will help make the rest of your field donation from former student Alan Eggers, who Colin Vucetich, Trish Walbridge, Robin season go smoothly. Secondly, come back safely. -
Visual Recovery of Desert Pavement Surfaces Following Impacts from Vehicle and Foot Traffic in the Ross Sea Region of Antarctica TANYA A
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Research Commons@Waikato Antarctic Science 25(4), 514–530 (2013) & Antarctic Science Ltd 2013 doi:10.1017/S0954102012001125 Visual recovery of desert pavement surfaces following impacts from vehicle and foot traffic in the Ross Sea region of Antarctica TANYA A. O’NEILL1, MEGAN R. BALKS1 and JERO´ NIMO LO´ PEZ-MARTI´NEZ2 1Earth and Ocean Sciences, University of Waikato, Hamilton, New Zealand 2Faculty of Sciences, Universidad Auto´noma de Madrid, Spain [email protected] Abstract: Sites of past human activity were investigated to assess the visual recovery of the desert pavement following impacts from human trampling and vehicle traffic. Visually disturbed and nearby control sites were assessed using comparative photographic records, a field-based Visual Site Assessment, and Desert Pavement Recovery Assessment. Sites included: vehicle and walking tracks at Marble Point and Taylor Valley; a campsite, experimental treading trial site, and vehicle tracks in Wright Valley; and vehicle and walking tracks at Cape Roberts. The time since last disturbance ranged from three months to over 50 years. This investigation also attempted to determine what has the greatest lasting visual impact on soil surfaces in the Ross Sea region: dispersed trafficking or track formation? Walking tracks remained visible in the landscape (due to larger clasts concentrating along track margins) long after the desert pavement surface had recovered. However, randomly dispersed footprints were undetectable within five years. For many sites, allowing widespread trampling will give lower medium-term visible impact than concentrating traffic flow by track formation. -
Weather Extremes
Answers archive: Weather extremes Link: http://www.usatoday.com/weather/resources/askjack/archives-weather-extremes.htm Q: What's the hottest city in the country? A: When measured by average year-round temperature, the hottest city is Key West, where the temperature averages 78°F. A better measurement is a city’s average high temperature in July, taken during the hottest of the hot weather. Using this method, the hottest U.S. city is Lake Havasu City, Ariz., which has an average July daily high temperature of about 111°F. As for large cities, the hottest is Phoenix, where the typical July day has a high of 106°F. This information is from Christopher Burt's book Extreme Weather. (Answered by Doyle Rice, USA TODAY’s weather editor, July 23, 2007) Q: How much do Hawaii's temperatures vary throughout the year? A: Thanks to the moderating influence of the Pacific Ocean, Hawaii has a mild, tropical climate, where the temperatures don't change all that much on a day-to-day basis, in comparison to much of the USA. To illustrate this, compare Hawaii and the continental climate of Fargo, N.D. The average high temperature in Honolulu in January is about 80°F. In August, it’s about 89°F. Compare that to Fargo's high of 16°F in January and 81°F in August. Where Hawaii's high temperature only varied 9°F from summer to winter, Fargo's varied 65°F. This USA TODAY state snapshot has more about the weather and climate of Hawaii, as does this report from the National Weather Service in Honolulu. -
Mcmurdo Dry Valleys: Exploring Antarctica As a Mars Analogue
49th Lunar and Planetary Science Conference 2018 (LPI Contrib. No. 2083) 2627.pdf MCMURDO DRY VALLEYS: EXPLORING ANTARCTICA AS A MARS ANALOGUE. Hunter Quintal1, James Head1, Ashley Palumbo1, James Dickson2, 1Department of Earth, Environmental and Planetary Sciences, Brown University, Providence, RI 02912 USA ([email protected]), 2Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125 USA. Introduction: The current martian climate is hyper- a meandering channel until it ponds in Lake Vanda arid and hypothermal, similar in many ways to the cli- (~160 m above sea level) (Fig. 1) [11]. mate of the Antarctic McMurdo Dry Valleys (MDV) [1]. This climate has persisted throughout the Amazonian (past ~3 Gyr) on Mars. Geologic evidence, including the widespread fluvial valley networks (VNs) [2] and lakes [3], suggest that the earlier Late Noachian and Early Hesperian (~3.7 Ga) climate may have been much dif- ferent than today, with abundant stable liquid water at the surface and persistent rainfall to form these fluvial and lacustrine features [4]. In contrast with this geologic evidence, recent climate models have suggested that the early climate may have been “cold and icy”, character- ized by mean annual temperatures far below the melting point of water (~225 K), an adiabatic cooling effect [5], and ice distributed across the southern highlands [6]. In Fig. 1. Schematic map view of Southfork Valley Antarctica, highlight- this climate scenario, transient or punctuated heating ing the path of the Onyx River. From [11]. McMurdo Dry Valleys Climate: We utilized events would be responsible for ice melting, liquid water Long-Term Ecological Research (LTER) data [12] to runoff, ponding at the surface, and formation of the VNs determine which climatic factors appear best correlated and lakes [7].