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The Ross Sea Dipole - Temperature, Snow Accumulation and Sea Ice Variability in the Ross Sea Region, Antarctica, Over the Past 2,700 Years
Clim. Past Discuss., https://doi.org/10.5194/cp-2017-95 Manuscript under review for journal Clim. Past Discussion started: 1 August 2017 c Author(s) 2017. CC BY 4.0 License. The Ross Sea Dipole - Temperature, Snow Accumulation and Sea Ice Variability in the Ross Sea Region, Antarctica, over the Past 2,700 Years 5 RICE Community (Nancy A.N. Bertler1,2, Howard Conway3, Dorthe Dahl-Jensen4, Daniel B. Emanuelsson1,2, Mai Winstrup4, Paul T. Vallelonga4, James E. Lee5, Ed J. Brook5, Jeffrey P. Severinghaus6, Taylor J. Fudge3, Elizabeth D. Keller2, W. Troy Baisden2, Richard C.A. Hindmarsh7, Peter D. Neff8, Thomas Blunier4, Ross Edwards9, Paul A. Mayewski10, Sepp Kipfstuhl11, Christo Buizert5, Silvia Canessa2, Ruzica Dadic1, Helle 10 A. Kjær4, Andrei Kurbatov10, Dongqi Zhang12,13, Ed D. Waddington3, Giovanni Baccolo14, Thomas Beers10, Hannah J. Brightley1,2, Lionel Carter1, David Clemens-Sewall15, Viorela G. Ciobanu4, Barbara Delmonte14, Lukas Eling1,2, Aja A. Ellis16, Shruthi Ganesh17, Nicholas R. Golledge1,2, Skylar Haines10, Michael Handley10, Robert L. Hawley15, Chad M. Hogan18, Katelyn M. Johnson1,2, Elena Korotkikh10, Daniel P. Lowry1, Darcy Mandeno1, Robert M. McKay1, James A. Menking5, Timothy R. Naish1, 15 Caroline Noerling11, Agathe Ollive19, Anaïs Orsi20, Bernadette C. Proemse18, Alexander R. Pyne1, Rebecca L. Pyne2, James Renwick1, Reed P. Scherer21, Stefanie Semper22, M. Simonsen4, Sharon B. Sneed10, Eric J., Steig3, Andrea Tuohy23, Abhijith Ulayottil Venugopal1,2, Fernando Valero-Delgado11, Janani Venkatesh17, Feitang Wang24, Shimeng -
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 -
2. Disc Resources
An early map of the world Resource D1 A map of the world drawn in 1570 shows ‘Terra Australis Nondum Cognita’ (the unknown south land). National Library of Australia Expeditions to Antarctica 1770 –1830 and 1910 –1913 Resource D2 Voyages to Antarctica 1770–1830 1772–75 1819–20 1820–21 Cook (Britain) Bransfield (Britain) Palmer (United States) ▼ ▼ ▼ ▼ ▼ Resolution and Adventure Williams Hero 1819 1819–21 1820–21 Smith (Britain) ▼ Bellingshausen (Russia) Davis (United States) ▼ ▼ ▼ Williams Vostok and Mirnyi Cecilia 1822–24 Weddell (Britain) ▼ Jane and Beaufoy 1830–32 Biscoe (Britain) ★ ▼ Tula and Lively South Pole expeditions 1910–13 1910–12 1910–13 Amundsen (Norway) Scott (Britain) sledge ▼ ▼ ship ▼ Source: Both maps American Geographical Society Source: Major voyages to Antarctica during the 19th century Resource D3 Voyage leader Date Nationality Ships Most southerly Achievements latitude reached Bellingshausen 1819–21 Russian Vostok and Mirnyi 69˚53’S Circumnavigated Antarctica. Discovered Peter Iøy and Alexander Island. Charted the coast round South Georgia, the South Shetland Islands and the South Sandwich Islands. Made the earliest sighting of the Antarctic continent. Dumont d’Urville 1837–40 French Astrolabe and Zeelée 66°S Discovered Terre Adélie in 1840. The expedition made extensive natural history collections. Wilkes 1838–42 United States Vincennes and Followed the edge of the East Antarctic pack ice for 2400 km, 6 other vessels confirming the existence of the Antarctic continent. Ross 1839–43 British Erebus and Terror 78°17’S Discovered the Transantarctic Mountains, Ross Ice Shelf, Ross Island and the volcanoes Erebus and Terror. The expedition made comprehensive magnetic measurements and natural history collections. -
Ice Production in Ross Ice Shelf Polynyas During 2017–2018 from Sentinel–1 SAR Images
remote sensing Article Ice Production in Ross Ice Shelf Polynyas during 2017–2018 from Sentinel–1 SAR Images Liyun Dai 1,2, Hongjie Xie 2,3,* , Stephen F. Ackley 2,3 and Alberto M. Mestas-Nuñez 2,3 1 Key Laboratory of Remote Sensing of Gansu Province, Heihe Remote Sensing Experimental Research Station, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China; [email protected] 2 Laboratory for Remote Sensing and Geoinformatics, Department of Geological Sciences, University of Texas at San Antonio, San Antonio, TX 78249, USA; [email protected] (S.F.A.); [email protected] (A.M.M.-N.) 3 Center for Advanced Measurements in Extreme Environments, University of Texas at San Antonio, San Antonio, TX 78249, USA * Correspondence: [email protected]; Tel.: +1-210-4585445 Received: 21 April 2020; Accepted: 5 May 2020; Published: 7 May 2020 Abstract: High sea ice production (SIP) generates high-salinity water, thus, influencing the global thermohaline circulation. Estimation from passive microwave data and heat flux models have indicated that the Ross Ice Shelf polynya (RISP) may be the highest SIP region in the Southern Oceans. However, the coarse spatial resolution of passive microwave data limited the accuracy of these estimates. The Sentinel-1 Synthetic Aperture Radar dataset with high spatial and temporal resolution provides an unprecedented opportunity to more accurately distinguish both polynya area/extent and occurrence. In this study, the SIPs of RISP and McMurdo Sound polynya (MSP) from 1 March–30 November 2017 and 2018 are calculated based on Sentinel-1 SAR data (for area/extent) and AMSR2 data (for ice thickness). -
Geology of Hut Point Peninsula, Ross Island
significantly below their Curie temperatures (approxi- Wilson, R. L., and N. D. Watkins. 1967. Correlation of mately 550°C.). petrology and natural magnetic polarity in Columbia Plateau basalts. Geophysical Journal of the Royal Astro- Previous work (Pucher, 1969; Stacey and Banerjee, nomical Society, 12(4): 405-424. 1974) indicates that the CRM intensity acquired in a low field is significantly less than the TRM intensity. It thus would appear that if a CRM induced at temperatures considerably below the Curie tempera- Geology of Hut Point Peninsula, ture, contributes a significant proportion to the ob- Ross Island served NRM intensity, too low an intensity value will be assigned to the ancient field. Although it is too early to report a firm value for PHILIP R. KYLE the intensity of the ancient field during the imprint- Department of Geology ing of unit 13 and related flows, we think that the Victoria University strength of the ambient field was more likely to Wellington, New Zealand have been about 0.5 oe (based on samples at about 141 meters) than about 0.1 oe (based on samples SAMUEL B. TREVES 122.18 and 126.06 meters). The virtual dipole Department of Geology moment (Smith, 1967b) calculated for an estimated University of Nebraska field intensity of 0.5 oe at the site is 7 X 10 25 gauss Lincoln, Nebraska 68508 cubic centimeters. This is larger than the value of 5.5 X 1025 gauss cubic centimeters (Smith, 1967b) Hut Point Peninsula is about 20 kilometers long calculated on the basis of paleointensity experiments and 2 to 4 kilometers wide. -
Surface Melt Magnitude Retrieval Over Ross Ice Shelf
The Cryosphere Discuss., 3, 1069–1107, 2009 The Cryosphere www.the-cryosphere-discuss.net/3/1069/2009/ Discussions TCD © Author(s) 2009. This work is distributed under 3, 1069–1107, 2009 the Creative Commons Attribution 3.0 License. This discussion paper is/has been under review for the journal The Cryosphere (TC). Surface melt Please refer to the corresponding final paper in TC if available. magnitude retrieval over Ross Ice Shelf D. J. Lampkin and C. C. Karmosky Surface melt magnitude retrieval over Ross Ice Shelf, Antarctica using coupled Title Page MODIS near-IR and thermal satellite Abstract Introduction measurements Conclusions References Tables Figures D. J. Lampkin1 and C. C. Karmosky2 J I 1Department of Geography, Department of Geosciences, Penn State University, University Park, Pennsylvania, USA J I 2Department of Geography, Penn State University, University Park, Pennsylvania, USA Back Close Received: 4 September 2009 – Accepted: 14 October 2009 – Published: 2 December 2009 Full Screen / Esc Correspondence to: D. J. Lampkin ([email protected]) Published by Copernicus Publications on behalf of the European Geosciences Union. Printer-friendly Version Interactive Discussion 1069 Abstract TCD Surface melt has been increasing over recent years, especially over the Antarctic Peninsula, contributing to disintegration of shelves such as Larsen. Unfortunately, 3, 1069–1107, 2009 we are not realistically able to quantify surface snowmelt from ground-based meth- 5 ods because there is sparse coverage of automatic weather stations. Satellite based Surface melt assessments of melt from passive microwave systems are limited in that they only pro- magnitude retrieval vide an indication of melt occurrence and have coarse spatial resolution. -
Geological Investigations of Volcanic Rocks at Mount Discovery, Mount Morning, and Mason Spur, Mcmurdo Sound Unusual Magnesium
Geological investigations mountain. A sample from one of these parasitic domes has been dated at 1.15 million years (Armstrong 1978). Younger basanite of volcanic rocks cinder cones and lava flows form two north-northeast trending at Mount Discovery, Mount Morning, ridges on the northeast side of Mount Morning, which are interpreted as being aligned along fracture zones parallel to the and Mason Spur, McMurdo Sound range front on the Royal Society Range located 30 kilometers to the northwest. Older trachytic rocks crop out at the lower end of both ridges. Detailed mapping of the trachyte outcrops on the A.C. WRIGHT, P.R. KYLE, J.A. MORE, and K. MEEKER western ridge confirms the similarity of this area to the trachyte outcrops on the eastern ridge, which has been mapped pre- Department of Geoscience, viously by Muncy (1979). Rocks intermediate in age between New Mexico Institute of Mining and Technology the older trachytes and the young basanites, comprise tra- Socorro, New Mexico 87801 chybasalt to trachyandesite flows and domes on the lower end of the western ridge. Description of five geologic sections at Mason Spur has provided a more detailed understanding of the older trachytic Between November 1985 and January 1986, we examined volcanic complex, which is now dated at 11.5 to 12.8 million rocks of the McMurdo Volcanic Group in the southern McMur- years (unpublished argon-40/argon-39 age determinations by do Sound area and at Mount Discovery, Mount Morning, and D. Lux, University of Maine) and is divided into seven mapped Mason Spur. This work is a continuation of field work carried units. -
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. -
Living and Working at USAP Facilities
Chapter 6: Living and Working at USAP Facilities CHAPTER 6: Living and Working at USAP Facilities McMurdo Station is the largest station in Antarctica and the southermost point to which a ship can sail. This photo faces south, with sea ice in front of the station, Observation Hill to the left (with White Island behind it), Minna Bluff and Black Island in the distance to the right, and the McMurdo Ice Shelf in between. Photo by Elaine Hood. USAP participants are required to put safety and environmental protection first while living and working in Antarctica. Extra individual responsibility for personal behavior is also expected. This chapter contains general information that applies to all Antarctic locations, as well as information specific to each station and research vessel. WORK REQUIREMENT At Antarctic stations and field camps, the work week is 54 hours (nine hours per day, Monday through Saturday). Aboard the research vessels, the work week is 84 hours (12 hours per day, Monday through Sunday). At times, everyone may be expected to work more hours, assist others in the performance of their duties, and/or assume community-related job responsibilities, such as washing dishes or cleaning the bathrooms. Due to the challenges of working in Antarctica, no guarantee can be made regarding the duties, location, or duration of work. The objective is to support science, maintain the station, and ensure the well-being of all station personnel. SAFETY The USAP is committed to safe work practices and safe work environments. There is no operation, activity, or research worth the loss of life or limb, no matter how important the future discovery may be, and all proactive safety measures shall be taken to ensure the protection of participants. -
Mcmurdo Preliminary Geotech Report
May 2016 GEOTECHNICAL ASSESSMENT REPORT McMurdo Station, Ross Island, Antarctica Submitted to: National Science Foundation C/- PAE (New Zealand) Ltd Private Bag 4747 Christchurch 8140 Report Number. 1535646_7407-002-R-Rev1 Distribution: REPORT Jeff Fenwick - PAE (New Zealand) Ltd David Winkler - Lockheed Martin GEOTECHNICAL ASSESSMENT REPORT - MCMURDO STATION, ROSS ISLAND, ANTARCTICA RECORD OF ISSUE Company Client Contact Version Date Issued Method of Delivery PAE (New Zealand) Ltd Jeff Fenwick Rev 0 4 April 2016 Email David Winkler Lockheed Martin Rev 0 4 April 2016 Email Brandon Neahusan PAE (New Zealand) Ltd Jeff Fenwick Rev 1 9 May 2016 Email David Winkler Lockheed Martin Rev 1 9 May 2016 Email Brandon Neahusan May 2016 Report No. 1535646_7407-002-R-Rev1 GEOTECHNICAL ASSESSMENT REPORT - MCMURDO STATION, ROSS ISLAND, ANTARCTICA REPORT LIMITATIONS Your attention is drawn to the document, “Report Limitations”, as attached in APPENDIX A. The statements presented in that document are intended to advise you of what your realistic expectations of this report should be, and to present you with recommendations on how to minimise the risks to which this report relates which are associated with this project. The document is not intended to exclude or otherwise limit the obligations necessarily imposed by law on Golder Associates (NZ) Limited, but rather to ensure that all parties who may rely on this report are aware of the responsibilities each assumes in so doing. May 2016 Report No. 1535646_7407-002-R-Rev1 GEOTECHNICAL ASSESSMENT REPORT - -
Movement Determination of the Ross Ice Shelf, Antarctica
Movement determination of the Ross Ice Shelf, Antarctica BY E. DORRER Department of Surveying Engineering, University of New Brunswick, Fredericton, N.B., Canada ABSTRACT Horizontal movements of very large ice sheets and ice shelves can be determined by astronomical positioning, by satellite triangulation, aerial photogrammetric triangulation, or geodetic traversing. A geodetic method is discussed in detail. Because of their dependency upon time, all originally "incoherent" measuring quantities must be reduced to a reference time. Two possible reduction methods involving either time reduction of observations or time reduction of positions, are compared. Some problems which occurred during the movement determination along the Ross Ice Shelf Studies (RISS) traverse, surveyed in 1962-63 and 1965- 66 are discussed together with the results (field of velocity vectors, strain rates) and an error analysis. The purpose of this paper is to show (1) how the surface movement of large ice shelves or ice sheets can be determined, and (2) that a geodetic method can provide most reliable and precise results. The results of the Ross Ice Shelf traverses 1962-63 and 1965-66 are later discussed. All methods have one factor in common, viz. that a certain configuration of well marked points on the ice surface must be surveyed at least twice, the time interval being determined by the size of the ice movement and the accuracy of the method applied. Where points are located close enough to fixed ground to be visible, absolute movements can be determined easily by intersection or resection methods. On very large ice sheets, however, other methods must be applied. -
The Antarctic Sun, December 19, 1999
On the Web at http://www.asa.org December 19, 1999 Published during the austral summer at McMurdo Station, Antarctica, for the United States Antarctic Program Ski-plane crashes at AGO-6 By Aaron Spitzer The Antarctic Sun Two pilots escaped injury Sunday when their Twin Otter aircraft crashed during takeoff from an isolated landing site in East Antarctica. The plane, a deHavilland Twin Otter turboprop owned by Kenn Borek Air Ltd. and chartered to the U.S. Antarc- tic Program, was taking off around 3:15 p.m. Sunday when it caught a ski in the snow and tipped sideways. A wing hit the ground and the plane suffered Congratulations, it’s a helicopter! extensive damage. A New Zealand C-130 delivers a Bell 212 helicopter to the ice runway last week. The new The accident occurred on a tempo- arrival took the place of the Royal New Zealand Air Force helo used in the first part of the rary skiway at Automated Geophysical season. Photo by Ed Bowen. Observatory 6, located in Wilkes Land, about 800 miles northwest of McMurdo. The pilots had flown to the site earlier in the day from McMurdo Station to drop Testing tainted waters off two runway groomers, who were preparing the strip for the arrival of an By Josh Landis LC-130 Hercules ski-plane. The Antarctic Sun On Monday afternoon, another Kenn Borek Twin Otter, chartered to the Most scientists come to Antarctica because it gives them a chance to do their Italian Antarctic Program at Terra Nova work in the most pristine conditions on Earth.