Annual Review 2011
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The Commonwealth Trans-Antarctic Expedition 1955-1958
THE COMMONWEALTH TRANS-ANTARCTIC EXPEDITION 1955-1958 HOW THE CROSSING OF ANTARCTICA MOVED NEW ZEALAND TO RECOGNISE ITS ANTARCTIC HERITAGE AND TAKE AN EQUAL PLACE AMONG ANTARCTIC NATIONS A thesis submitted in fulfilment of the requirements for the Degree PhD - Doctor of Philosophy (Antarctic Studies – History) University of Canterbury Gateway Antarctica Stephen Walter Hicks 2015 Statement of Authority & Originality I certify that the work in this thesis has not been previously submitted for a degree nor has it been submitted as part of requirements for a degree except as fully acknowledged within the text. I also certify that the thesis has been written by me. Any help that I have received in my research and the preparation of the thesis itself has been acknowledged. In addition, I certify that all information sources and literature used are indicated in the thesis. Elements of material covered in Chapter 4 and 5 have been published in: Electronic version: Stephen Hicks, Bryan Storey, Philippa Mein-Smith, ‘Against All Odds: the birth of the Commonwealth Trans-Antarctic Expedition, 1955-1958’, Polar Record, Volume00,(0), pp.1-12, (2011), Cambridge University Press, 2011. Print version: Stephen Hicks, Bryan Storey, Philippa Mein-Smith, ‘Against All Odds: the birth of the Commonwealth Trans-Antarctic Expedition, 1955-1958’, Polar Record, Volume 49, Issue 1, pp. 50-61, Cambridge University Press, 2013 Signature of Candidate ________________________________ Table of Contents Foreword .................................................................................................................................. -
Atmospheric Gas Records from Taylor Glacier, Antarctica, Reveal Ancient Ice with Ages Spanning the Entire Last Glacial Cycle Daniel Baggenstos1,*, Thomas K
Clim. Past Discuss., doi:10.5194/cp-2017-25, 2017 Manuscript under review for journal Clim. Past Discussion started: 28 February 2017 c Author(s) 2017. CC-BY 3.0 License. Atmospheric gas records from Taylor Glacier, Antarctica, reveal ancient ice with ages spanning the entire last glacial cycle Daniel Baggenstos1,*, Thomas K. Bauska2, Jeffrey P. Severinghaus1, James E. Lee2, Hinrich Schaefer3, Christo Buizert2, Edward J. Brook2, Sarah Shackleton1, and Vasilii V. Petrenko4 1Scripps Institution of Oceanography (SIO), University of California, San Diego, La Jolla, CA 92093, USA. 2College of Earth, Ocean and Atmospheric Sciences, Oregon State University (OSU), Corvallis, OR, 97331, USA. 3National Institute of Water and Atmospheric Research Ltd (NIWA), PO Box 14901, Kilbirnie, 301 Evans Bay Parade, Wellington, New Zealand. 4Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY 14627, USA. *Current address: Climate and Environmental Physics, University of Bern, Switzerland. Correspondence to: [email protected] Abstract. Old ice for paleo-environmental studies, traditionally accessed through deep core drilling on domes and ridges on the large ice sheets, can also be retrieved at the surface from ice sheet margins and blue ice areas. The practically unlimited amount of ice available at these sites satisfies a need in the community for studies of trace components requiring large sample volumes. For margin sites to be useful as ancient ice archives, the ice stratigraphy needs to be understood and age models 5 need to be established. We present measurements of trapped gases in ice from Taylor Glacier, Antarctica, to date the ice 18 and assess the completeness of the stratigraphic section. -
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. -
A Sedimentological Record of Early Miocene Ice Advance and Retreat, AND-2A Drill Hole, Mcmurdo Sound, Antarctica GEOSPHERE
Research Paper GEOSPHERE A sedimentological record of early Miocene ice advance and retreat, AND-2A drill hole, McMurdo Sound, Antarctica 1 1 2 3 2 4 5 6 7 8 GEOSPHERE; v. 14, no. 4 B.D. Field , G.H. Browne , C.R. Fielding , F. Florindo , D.M. Harwood , S.A. Judge , L.A. Krissek , K.S. Panter , S. Passchier , S.F. Pekar , S. Sandroni9, and F.M. Talarico9,10 1 https://doi.org/10.1130/GES01592.1 GNS Science, PO Box 30368, Lower Hutt, New Zealand 2Department of Earth and Atmospheric Sciences, 126 Bessey Hall, University of Nebraska-Lincoln, Nebraska 68588- 0340, USA 3Istituto Nazionale di Geofisica e Vulcanologia, Via di Vigna Murata 605, 1-00143 Rome, Italy 15 figures 4Department of Geology, College of Wooster, 944 College Mall, Wooster, Ohio 44691, USA 5School of Earth Sciences, Ohio State University, 125 South Oval Mall, Columbus, Ohio 43210, USA 6 CORRESPONDENCE: brad .field@ gns .cri.nz Department of Geology, Bowling Green State University, Bowling Green, Ohio 43402, USA 7Department of Earth & Environmental Sciences, Montclair State University, 252 Mallory Hall, 1 Normal Avenue, Montclair, New Jersey 07043, USA 8School of Earth & Environmental Sciences, Queen’s College, 65-30 Kissena Blvd., Flushing, New York 11367, USA CITATION: Field, B.D., Browne, G.H., Fielding, 9Museo Nazionale dell’Antartide, Università degli Studi di Siena, Via Laterina 8, Siena, Italy C.R., Florindo, F., Harwood, D.M., Judge, S.A., 10Dipartimento di Scienze Fisiche, della Terra e dell’Ambiente, Università degli Studi di Siena, Via Laterina 8, Siena, Italy Krissek, L.A., Panter, K.S., Passchier, S., Pekar, S.F., Sandroni, S., and Talarico, F.M., 2018, A sedimento- logical record of early Miocene ice advance and re- ABSTRACT antarctic Mountains glacial activity under precessional control in CS1 and treat, AND-2A drill hole, McMurdo Sound, Antarctica: Geosphere, v. -
Fault Kinematic Studies in the Transantarctic Mountains, Southern Victoria Land TERRY J
studies. Together these data will be used to develop a model to plate tectonic modeling. In R.A. Hodgson, S.P. Gay, Jr., and J.Y. of the structural architecture and motion history associated Benjamins (Eds.), Proceedings of the First International Conference with the Transantarctic Mountains in southern Victoria Land. on the New Basement Tectonics (Publication number 5). Utah Geo- logical Association. We thank Jane Ferrigno for cooperation and advice on Lucchita, B.K., J. Bowell, K.L. Edwards, E.M. Eliason, and H.M. Fergu- image selection; John Snowden, David Cunningham, and son. 1987. Multispectral Landsat images of Antarctica (U.S. Geo- Tracy Douglass at the Ohio State University Center for Map- logical Survey bulletin 1696). Washington, D.C.: U.S. Government ping for help with computer processing; and Carolyn Merry, Printing Office. Gary Murdock, and Ralph von Frese for helpful discussions Wilson, T.J. 1992. Mesozoic and Cenozoic kinematic evolution of the Transantarctic Mountains. In Y. Yoshida, K. Kaminuma, and K. concerning image analysis. This research was supported by Shiraishi (Eds.), Recent progress in antarctic earth science. Tokyo: National Science Foundation grant OPP 90-18055 and by the Terra Scientific. Byrd Polar Research Center of Ohio State University. Wilson, T.J. 1993. Jurassic faulting and magmatism in the Transantarctic Mountains: Implication for Gondwana breakup. In R.H. Findlay, M.R. Banks, R. Unrug, and J. Veevers (Eds.), Gond- References wana 8—Assembly, evolution, and dispersal. Rotterdam: A.A. Balkema. Wilson, T.J., P. Braddock, R.J. Janosy, and R.J. Elliot. 1993. Fault kine- Isachsen, Y.W. 1974. -
2010-2011 Science Planning Summaries
Find information about current Link to project web sites and USAP projects using the find information about the principal investigator, event research and people involved. number station, and other indexes. Science Program Indexes: 2010-2011 Find information about current USAP projects using the Project Web Sites principal investigator, event number station, and other Principal Investigator Index indexes. USAP Program Indexes Aeronomy and Astrophysics Dr. Vladimir Papitashvili, program manager Organisms and Ecosystems Find more information about USAP projects by viewing Dr. Roberta Marinelli, program manager individual project web sites. Earth Sciences Dr. Alexandra Isern, program manager Glaciology 2010-2011 Field Season Dr. Julie Palais, program manager Other Information: Ocean and Atmospheric Sciences Dr. Peter Milne, program manager Home Page Artists and Writers Peter West, program manager Station Schedules International Polar Year (IPY) Education and Outreach Air Operations Renee D. Crain, program manager Valentine Kass, program manager Staffed Field Camps Sandra Welch, program manager Event Numbering System Integrated System Science Dr. Lisa Clough, program manager Institution Index USAP Station and Ship Indexes Amundsen-Scott South Pole Station McMurdo Station Palmer Station RVIB Nathaniel B. Palmer ARSV Laurence M. Gould Special Projects ODEN Icebreaker Event Number Index Technical Event Index Deploying Team Members Index Project Web Sites: 2010-2011 Find information about current USAP projects using the Principal Investigator Event No. Project Title principal investigator, event number station, and other indexes. Ainley, David B-031-M Adelie Penguin response to climate change at the individual, colony and metapopulation levels Amsler, Charles B-022-P Collaborative Research: The Find more information about chemical ecology of shallow- USAP projects by viewing individual project web sites. -
In This Issue
rvin bse g S O ys th t r e a m E THE EARTH OBSERVER May/June 2003, Vol. 15, No. 3 In this issue ... EDITOR’S CORNER Meeting/Workshop Summaries Michael King Minutes of the March 2003 Aura Science EOS Senior Project Scientist Team Meeting ................................ 3 CERES Science Team Meeting ......... 9 CloudSat/CALIPSO Science Team I’m proud to announce that the International Academy of the Digital Arts Meeting Summary ....................... 14 and Sciences has selected two NASA Web sites for top honors in their ASTER Users Workshop ................. 17 respective categories. The NASA Home Page (at www.nasa.gov), managed SEEDS Update ................................ 23 by Brian Dunbar and his team at NASA Headquarters in Washington, D.C., Other Items of Interest won the Webby in the “Government & Law” category. And NASA’s Earth Observatory (at earthobservatory.nasa.gov), managed by David Herring and CCSDS Lossless Data Compression to be Available in HDF-4 and 5 ....... 19 his team at Goddard Space Flight Center in Greenbelt, MD, won the Webby Aqua Mission Sponsors 2003 Engineer- in the “Education” category. ing Competition ........................ 21 Additionally, both sites won “People’s Voice Awards” for their respective Kudos ................................................ 24 Earth’s Hidden Waters Tracked by categories. In keeping with the spirit of the Web’s capacity for global GRACE .................................... 25 interactivity, the People’s Voice Award is determined by a popular vote in NASA’s ESE Sponsors Creative Problem which anyone in the world can vote for their favorites in each of the Solving competition ................. 30 Webby’s thirty categories. Regular Features The Webby is the most coveted award by the on-line community (visit Earth Science Education Program www.webbyawards.com for details). -
1 Compiled by Mike Wing New Zealand Antarctic Society (Inc
ANTARCTIC 1 Compiled by Mike Wing US bulldozer, 1: 202, 340, 12: 54, New Zealand Antarctic Society (Inc) ACECRC, see Antarctic Climate & Ecosystems Cooperation Research Centre Volume 1-26: June 2009 Acevedo, Capitan. A.O. 4: 36, Ackerman, Piers, 21: 16, Vessel names are shown viz: “Aconcagua” Ackroyd, Lieut. F: 1: 307, All book reviews are shown under ‘Book Reviews’ Ackroyd-Kelly, J. W., 10: 279, All Universities are shown under ‘Universities’ “Aconcagua”, 1: 261 Aircraft types appear under Aircraft. Acta Palaeontolegica Polonica, 25: 64, Obituaries & Tributes are shown under 'Obituaries', ACZP, see Antarctic Convergence Zone Project see also individual names. Adam, Dieter, 13: 6, 287, Adam, Dr James, 1: 227, 241, 280, Vol 20 page numbers 27-36 are shared by both Adams, Chris, 11: 198, 274, 12: 331, 396, double issues 1&2 and 3&4. Those in double issue Adams, Dieter, 12: 294, 3&4 are marked accordingly. Adams, Ian, 1: 71, 99, 167, 229, 263, 330, 2: 23, Adams, J.B., 26: 22, Adams, Lt. R.D., 2: 127, 159, 208, Adams, Sir Jameson Obituary, 3: 76, A Adams Cape, 1: 248, Adams Glacier, 2: 425, Adams Island, 4: 201, 302, “101 In Sung”, f/v, 21: 36, Adamson, R.G. 3: 474-45, 4: 6, 62, 116, 166, 224, ‘A’ Hut restorations, 12: 175, 220, 25: 16, 277, Aaron, Edwin, 11: 55, Adare, Cape - see Hallett Station Abbiss, Jane, 20: 8, Addison, Vicki, 24: 33, Aboa Station, (Finland) 12: 227, 13: 114, Adelaide Island (Base T), see Bases F.I.D.S. Abbott, Dr N.D. -
Ogive Systems on Polar Alpine Glaciers
the present. This period of ablation could con- ceivably be correlated with the climatic optimum NZ of several thousand years ago. During December 1971 the two 10-kilometer-long lines of snow stakes at Byrd Station were remeasured, and further measurements of deformation were made in the drill hole at old Byrd Station. Nearly 10 years of snow stake observations have shown that the large surface depressions around Byrd Station are accumu- lating 30 to 50 percent more snow than the exposed crests. Snow accumulation within a 10-kilometer radius of Byrd over the past 10 years has varied from 8.6 to 15.7 grams per square centimeter per year, with a mean value of 11.7 grams per square centimeter per year. A. I. Gow Only the top 170 meters of the 308-meter-deep hole Figure L South side of Hobbs Glacier, showing abundant lami- at old Byrd is still accessible for measurement with the nated debris composed mainly of dust particles and sand. downhole probe. This part of the hole had been de- forming very slowly, but the latest data, taken nearly 14 years after the hole was drilled, clearly show that accelerating closure has set in at the lower stresses. This work was supported by National Science Foun- dation grant AG-258. Ogive systems on polar alpine glaciers MAURICE J. MCSAVENEY Institute of Polar Studies The Ohio State University The inapplicability of the annual ablation-plastic deformation model of surface wave, or wave ogive, Figure 2. Close-up of contorted debris patterns in Garwood Glacier. -
Landscape Evolution of the Dry Valleys, Transantarctic Mountains: Tectonic Implications David E
The University of Maine DigitalCommons@UMaine Earth Science Faculty Scholarship Earth Sciences 6-10-1995 Landscape Evolution of the Dry Valleys, Transantarctic Mountains: Tectonic Implications David E. Sugden George H. Denton University of Maine - Main, [email protected] David R. Marchant Follow this and additional works at: https://digitalcommons.library.umaine.edu/ers_facpub Part of the Earth Sciences Commons Repository Citation Sugden, David E.; Denton, George H.; and Marchant, David R., "Landscape Evolution of the Dry Valleys, Transantarctic Mountains: Tectonic Implications" (1995). Earth Science Faculty Scholarship. 55. https://digitalcommons.library.umaine.edu/ers_facpub/55 This Article is brought to you for free and open access by DigitalCommons@UMaine. It has been accepted for inclusion in Earth Science Faculty Scholarship by an authorized administrator of DigitalCommons@UMaine. For more information, please contact [email protected]. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 100, NO. B7, PAGES 9949-9967, JUNE 10, 1995 Landscapeevolution of the Dry Valleys,Transantarctic Mountains: Tectonicimplications David E. Sugden Departmentof Geography,University of Edinburgh,Edinburgh, Scotland GeorgeH. Denton Departmentof GeologicalSciences and Institute for QuaternaryStudies, University of Maine,Orono DavidR. Marchant• Departmentof Geography,University of Edinburgh,Edinburgh, Scotland Abstract. Thereare differentviews about the amount and timing of surfaceuplift in the TransantarcticMountains and the geophysicalmechanisms involved. Our new interpretationof the landscapeevolution and tectonichistory of the Dry Valleysarea of the Transantarctic Mountainsis basedon geomorphic mapping of anarea of 10,000km 2. Thelandforms are dated mainlyby their associationwith volcanicashes and glaciomarine deposits and this permitsa reconsmactionof the stagesand timing of landscapeevolution. Followinga loweringof baselevel about55 m.y. ago,there was a phaseof rapid denudationassociated with planationand escarpmentretreat, probably under semiarid conditions. -
SPATIAL PATTERN of ACCUMULATION at TAYLOR DOME DURING the LAST GLACIAL INCEPTION: STRATIGRAPHIC CONSTRAINTS from TAYLOR GLACIER 5 James A
Clim. Past Discuss., https://doi.org/10.5194/cp-2018-53 Manuscript under review for journal Clim. Past Discussion started: 17 May 2018 c Author(s) 2018. CC BY 4.0 License. SPATIAL PATTERN OF ACCUMULATION AT TAYLOR DOME DURING THE LAST GLACIAL INCEPTION: STRATIGRAPHIC CONSTRAINTS FROM TAYLOR GLACIER 5 James A. Menking1, Edward J. Brook1, Sarah A. Shackleton2, Jeffrey P. Severinghaus2, Michael Dyonisius3, Vasilii Petrenko3, Joseph R. McConnell4, Rachael H. Rhodes5, Thomas K. Bauska5, Daniel Baggenstos6, Shaun Marcott7, Stephen Barker8 10 1College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, 97333, United States of America 2Scripps Institution of Oceanography, University of California San Diego, La Jolla, 92037, United States of America 3Department of Earth and Environmental Sciences, University of Rochester, Rochester, 14627, United 15 States of America 4Division of Hydrological Sciences, Desert Research Institute, Reno, 89512, United States of America 5Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, United Kingdom 6Climate and Environmental Physics, University of Bern, Bern, 3012, Switzerland 7Department of Geoscience, University of Wisconsin-Madison, Madison, 53706, United States of America 20 8School of Earth and Ocean Sciences, Cardiff University, Cardiff, CF10 3AT, United Kingdom Correspondence to: James A. Menking ([email protected]) Abstract. A new ice core retrieved from the Taylor Glacier blue ice area contains ice and air spanning the 25 Marine Isotope Stage (MIS) 5/4 transition (74 to 65 ka), a period of global cooling and glacial inception. Dating the ice and air bubbles in the new ice core reveals an ice age-gas age difference (Δage) approaching 10 ka during MIS 4, implying very low accumulation at the Taylor Glacier accumulation zone on the northern flank of Taylor Dome. -
Reconstruction of LGM and Post LGM Glacial Environment of Mcmurdo Sound: Implications for Ice Dynamics, Depositional Systems and Glacial Isostatic Adjustment
Reconstruction of LGM and Post LGM Glacial Environment of McMurdo Sound: Implications for Ice Dynamics, Depositional Systems and Glacial Isostatic Adjustment THESIS Presented in Partial Fulfillment of the Requirements for the Degree Master of Science in the Graduate School of The Ohio State University By James Edward Stutz Graduate Program in Geological Sciences The Ohio State University 2012 Master's Examination Committee: Dr. Terry Wilson, Advisor Dr. Larry Krissek Dr. Peter Webb Copyright by James Edward Stutz 2012 Abstract McMurdo Sound represents a landscape at the crossroads of the West and East Antarctic Ice Sheets and has seen repeated occupation by both cold and warm based ice. Current ice sheet reconstructions place grounded ice across McMurdo Sound at the Last Glacial Maximum (LGM), thus the seafloor is expected to display morphologic features recording the LGM glaciation. Analysis of high-resolution multibeam bathymetry data and seismic surveys documents landforms marking glacial-geological processes beneath and at the margins of the ice sheets and are used to help determine the extent and style of glacial behavior on glacially influenced continental margins. The dominant morphologic features on the seafloor of McMurdo Sound are channel systems emanating eastward from the fjords of the Transantarctic Mountains (TAM) coast and northward from beneath the McMurdo Ice Shelf. A wide range of channel systems is observed. MacKay Sea Valley, at the northern limit of McMurdo Sound, displays a 6-8km wide, u-shaped valley with lineations formed by streaming ice of the expanded MacKay Glacier. A large submarine outwash fan extends 10’s of km eastward from the mouth of the sea valley.