Ice-Covered Regions in International Law
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Ice Flow Impacts the Firn Structure of Greenland's Percolation Zone
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 2019 Ice Flow Impacts the Firn Structure of Greenland's Percolation Zone Rosemary C. Leone University of Montana, Missoula Follow this and additional works at: https://scholarworks.umt.edu/etd Part of the Glaciology Commons Let us know how access to this document benefits ou.y Recommended Citation Leone, Rosemary C., "Ice Flow Impacts the Firn Structure of Greenland's Percolation Zone" (2019). Graduate Student Theses, Dissertations, & Professional Papers. 11474. https://scholarworks.umt.edu/etd/11474 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. ICE FLOW IMPACTS THE FIRN STRUCTURE OF GREENLAND’S PERCOLATION ZONE By ROSEMARY CLAIRE LEONE Bachelor of Science, Colorado School of Mines, Golden, CO, 2015 Thesis presented in partial fulfillMent of the requireMents for the degree of Master of Science in Geosciences The University of Montana Missoula, MT DeceMber 2019 Approved by: Scott Whittenburg, Dean of The Graduate School Graduate School Dr. Joel T. Harper, Chair DepartMent of Geosciences Dr. Toby W. Meierbachtol DepartMent of Geosciences Dr. Jesse V. Johnson DepartMent of Computer Science i Leone, RoseMary, M.S, Fall 2019 Geosciences Ice Flow Impacts the Firn Structure of Greenland’s Percolation Zone Chairperson: Dr. Joel T. Harper One diMensional siMulations of firn evolution neglect horizontal transport as the firn column Moves down slope during burial. -
High Arctic Holocene Temperature Record from the Agassiz Ice Cap and Greenland Ice Sheet Evolution
High Arctic Holocene temperature record from the Agassiz ice cap and Greenland ice sheet evolution Benoit S. Lecavaliera,1, David A. Fisherb, Glenn A. Milneb, Bo M. Vintherc, Lev Tarasova, Philippe Huybrechtsd, Denis Lacellee, Brittany Maine, James Zhengf, Jocelyne Bourgeoisg, and Arthur S. Dykeh,i aDepartment of Physics and Physical Oceanography, Memorial University, St. John’s, Canada, A1B 3X7; bDepartment of Earth and Environmental Sciences, University of Ottawa, Ottawa, Canada, K1N 6N5; cCentre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark, 2100; dEarth System Science and Departement Geografie, Vrije Universiteit Brussel, Brussels, Belgium, 1050; eDepartment of Geography, University of Ottawa, Ottawa, Canada, K1N 6N5; fGeological Survey of Canada, Natural Resources Canada, Ottawa, Canada, K1A 0E8; gConsorminex Inc., Gatineau, Canada, J8R 3Y3; hDepartment of Earth Sciences, Dalhousie University, Halifax, Canada, B3H 4R2; and iDepartment of Anthropology, McGill University, Montreal, Canada, H3A 2T7 Edited by Jeffrey P. Severinghaus, Scripps Institution of Oceanography, La Jolla, CA, and approved April 18, 2017 (received for review October 2, 2016) We present a revised and extended high Arctic air temperature leading the authors to adopt a spatially homogeneous change in reconstruction from a single proxy that spans the past ∼12,000 y air temperature across the region spanned by these two ice caps. 18 (up to 2009 CE). Our reconstruction from the Agassiz ice cap (Elles- By removing the temperature signal from the δ O record of mere Island, Canada) indicates an earlier and warmer Holocene other Greenland ice cores (Fig. 1A), the residual was used to thermal maximum with early Holocene temperatures that are estimate altitude changes of the ice surface through time. -
“Mining” Water Ice on Mars an Assessment of ISRU Options in Support of Future Human Missions
National Aeronautics and Space Administration “Mining” Water Ice on Mars An Assessment of ISRU Options in Support of Future Human Missions Stephen Hoffman, Alida Andrews, Kevin Watts July 2016 Agenda • Introduction • What kind of water ice are we talking about • Options for accessing the water ice • Drilling Options • “Mining” Options • EMC scenario and requirements • Recommendations and future work Acknowledgement • The authors of this report learned much during the process of researching the technologies and operations associated with drilling into icy deposits and extract water from those deposits. We would like to acknowledge the support and advice provided by the following individuals and their organizations: – Brian Glass, PhD, NASA Ames Research Center – Robert Haehnel, PhD, U.S. Army Corps of Engineers/Cold Regions Research and Engineering Laboratory – Patrick Haggerty, National Science Foundation/Geosciences/Polar Programs – Jennifer Mercer, PhD, National Science Foundation/Geosciences/Polar Programs – Frank Rack, PhD, University of Nebraska-Lincoln – Jason Weale, U.S. Army Corps of Engineers/Cold Regions Research and Engineering Laboratory Mining Water Ice on Mars INTRODUCTION Background • Addendum to M-WIP study, addressing one of the areas not fully covered in this report: accessing and mining water ice if it is present in certain glacier-like forms – The M-WIP report is available at http://mepag.nasa.gov/reports.cfm • The First Landing Site/Exploration Zone Workshop for Human Missions to Mars (October 2015) set the target -
Polar Ice in the Solar System
Recommended Reading List for Polar Ice in the Inner Solar System Compiled by: Shane Byrne Lunar and Planetary Laboratory, University of Arizona. April 23rd, 2007 Polar Ice on Airless Bodies................................................................................................. 2 Initial theories and modeling results for these ice deposits: ........................................... 2 Observational evidence (or lack of) for polar ice on airless bodies:............................... 3 Martian Polar Ice................................................................................................................. 4 Good (although dated) introductory material ................................................................. 4 Polar Layered Deposits:...................................................................................................... 5 Ice-flow (or lack thereof) and internal structure in the polar layered deposits............... 5 North polar basal-unit ..................................................................................................... 6 Geologic Mapping and impact cratering......................................................................... 6 Connection of polar layered deposits (PLD) to climate.................................................. 7 Formation of troughs, scarps and chasmata.................................................................... 7 Surface Properties of the PLD ........................................................................................ 8 Eolian Processes -
Greenland's Ice Cap Super Melting Is Currently Losing 200 Cubic Kilometres Our Swiss Army Kit for of Ice Each Year — and Accelerating
MORE GOOD STUFF Speeding up! ADSL DIY We show you how to make Turbocharge your Internet your PC run faster. without having to call in the geeks. Communities: Mon, 21 Aug 2006 You are in: Cooltech > Science & Nature BLOGS CLASSIFIEDS ENVIRONMENT CONVERTERS Greenland's ice cap super DOWNLOADS melting FEATURES Fri, 11 Aug 2006 GAMES MOBILE MAGIC The vast ice cap that covers most of NEW IDEAS Greenland is melting at a spectacular rate, and three times faster than five NEWSLETTER years ago, reports National Geographic SCIENCE & NATURE News. Swiss Army Kit SPACE SWISS ARMY KIT This is according to a new study, Frustrated published online by the journal Science, More Science & Nature TECH NEWS with your PC? which further indicates that Greenland Check out THE GADGET CORNER Greenland's ice cap super melting is currently losing 200 cubic kilometres our Swiss Army Kit for of ice each year — and accelerating. 'Warrior' gene 'linked' to Maori violence the answer! eMail the Ads by Goooooogle Where there's muck, there's Monet Cooltech Editor if you The study also finds that the melting Electric Snow Melt have a problem, and polar ice is raising sea levels around the Elephants show capacity for compassion we'll do our best to Cables globe. This could have a serious impact First koala born in Africa help! Waterproof Electric as global sea levels will rise by 6.5 Heating Cable Thick metres if all the ice on Greenland were China promises smog-free Olympics means durability.Since The Tech Set to melt, which could result in many Adventurer finishes 327km Thames swim 1930 islands being wiped out and even low- www.WarmYourFloor.com lying countries such as the Netherlands. -
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). -
Chapter 7 Seasonal Snow Cover, Ice and Permafrost
I Chapter 7 Seasonal snow cover, ice and permafrost Co-Chairmen: R.B. Street, Canada P.I. Melnikov, USSR Expert contributors: D. Riseborough (Canada); O. Anisimov (USSR); Cheng Guodong (China); V.J. Lunardini (USA); M. Gavrilova (USSR); E.A. Köster (The Netherlands); R.M. Koerner (Canada); M.F. Meier (USA); M. Smith (Canada); H. Baker (Canada); N.A. Grave (USSR); CM. Clapperton (UK); M. Brugman (Canada); S.M. Hodge (USA); L. Menchaca (Mexico); A.S. Judge (Canada); P.G. Quilty (Australia); R.Hansson (Norway); J.A. Heginbottom (Canada); H. Keys (New Zealand); D.A. Etkin (Canada); F.E. Nelson (USA); D.M. Barnett (Canada); B. Fitzharris (New Zealand); I.M. Whillans (USA); A.A. Velichko (USSR); R. Haugen (USA); F. Sayles (USA); Contents 1 Introduction 7-1 2 Environmental impacts 7-2 2.1 Seasonal snow cover 7-2 2.2 Ice sheets and glaciers 7-4 2.3 Permafrost 7-7 2.3.1 Nature, extent and stability of permafrost 7-7 2.3.2 Responses of permafrost to climatic changes 7-10 2.3.2.1 Changes in permafrost distribution 7-12 2.3.2.2 Implications of permafrost degradation 7-14 2.3.3 Gas hydrates and methane 7-15 2.4 Seasonally frozen ground 7-16 3 Socioeconomic consequences 7-16 3.1 Seasonal snow cover 7-16 3.2 Glaciers and ice sheets 7-17 3.3 Permafrost 7-18 3.4 Seasonally frozen ground 7-22 4 Future deliberations 7-22 Tables Table 7.1 Relative extent of terrestrial areas of seasonal snow cover, ice and permafrost (after Washburn, 1980a and Rott, 1983) 7-2 Table 7.2 Characteristics of the Greenland and Antarctic ice sheets (based on Oerlemans and van der Veen, 1984) 7-5 Table 7.3 Effect of terrestrial ice sheets on sea-level, adapted from Workshop on Glaciers, Ice Sheets and Sea Level: Effect of a COylnduced Climatic Change. -
Fast-Ice Properties and Structure in Mcmurdo Sound
Fast-ice properties 00 0, C6 001 MW 00 O 0 A 00 and structure in McMurdo Sound 00000 0 O 0 qM0 = 0 O 0 Dc•= 0 0000 D 0 ooa 50 O 0 41110 m 50 M.O. JEFFRIES and WE WEEKS cc. O 0 00aoo O 0 000 DO Geophysical Institute 0 0O 00 DD University of Alaska 100 o CDCOM 0 DO D 0 D 100 Fairbanks, Alaska 99775-0800 M 00 DO •= 0 oo 00 _ 0 —I I 0 0 41KE 0 O 0 0 C) The fast ice in McMurdo Sound frequently is used as a plat- 3 o acmgo 0 DO DO 000 0 O 0 _ 0 form for oceanographic and biological studies, and the annual 150 0 150 0= 00 O 0 a0 sea ice runway is essential to the movement of personnel, cze 00 0 O 0 DO equipment and supplies in and out of McMurdo Station. Con- O Da 0:2CM 8 sidering the importance of the fast ice to the operation of coo o 0 o McMurdo Station remarkably little is known about its annual 200 000 GOD 0 200 OO SO 0 growth history, properties, and structure. In early January 1991, 00• 0 we obtained 15 first-year cores from the fast ice in McMurdo 0 •0 0 Sound (figure 1). For comparative purposes, an additional core A B 250 .... 250 was obtained from Gerlache Bay, the site of the Italian antarctic 0 2 4 6 8 10-4 -3 -2 -1 0 station, Baie Terra Nova (see Jeffries and Weeks, Antarctic Jour- SALINITY (o/oo) TEMPERATURE (°C) nal, this issue, for location). -
Particle Flux Beneath Fast Ice in the Shallow Southwestern Beaufort Sea, Arctic Ocean
MARINE ECOLOGY - PROGRESS SERIES Published October 28 Mar. Ecol. Prog. Ser. 1 Particle flux beneath fast ice in the shallow southwestern Beaufort Sea, Arctic Ocean Andrew G.Carey, Jr. College of Oceanography, Oregon State University. Corvallis. Oregon 97331, USA ABSTRACT: Flux of organic particulate materials under sea ice to the benthic environment was measured in the nearshore Arctic Ocean during spring 1980. Downward flux of organic carbon started early in the spring and continued at fairly uniform but low levels (approximately 1 % of daily carbon production of ice algae) from April until early June. Particulate organic nitrogen flux tended to be low and erratic. Fecal pellets from 2 crustacean species were among the few recognizable large particles. The amphipod Pseudalibrotus (= Onisimus) litoralis, normally a benthic species, lives in spring on the undersurface of sea ice in the shallow polar environment. Collected pellets from adults decreased through spring, while those from juveniles increased until 5 Jun when their flux declined markedly. Late in spring these pellets contained primarily pennate diatom frustules from the ice algal bloom. Crustacean molts and Mysis relicta fecal pellets were also present, particularly in April and early May. The sinking particles were derived from both the pelagic and ice environments, although most of the material appeared to be from the ice biota. Data suggest that particles falling from the productive ice community during spring are a carbon source for the benthos; one that is small but available -
INTERNATIONAL Greenland's Ice Cap Melting at Accelerating Rate by Finfacts Team Aug 11, 2006, 14:17
Rutherford Roofing Inc. Roofing & Rain Gutters California Roofing Aluminium Composite Panel Roofing Contractor in Los Angeles Serving Long Beach, LA & the 15% Senior Discount! Free Construction, Wall Cladding Re-Roofs, Repairs, New South Bay areas of Southern Estimate. Emergency Repairs. Curtain Wall, Building Materials Construction California Seal Coating. Ads by Goooooogle Advertise on this site INTERNATIONAL Greenland's ice cap melting at accelerating rate By Finfacts Team Aug 11, 2006, 14:17 The Greenland ice sheet experienced record melting in September 2002, as did much of the Arctic. A comparison of images from 2001 through 2003 and 2004 shows the changes in Greenland’s ice sheet over the past few years. In this image, the melt zone appears along the western edge of the ice. In this zone, water has saturated the ice, darkening its color from white to blue-gray. The colored lines indicate the approximate melt zone extents for June 2001 through June 2005. Between June 2001 and June 2003, the melt zone increased substantially, then shrank somewhat in June 2004. The melt zone for June 2005 appears roughly equivalent to that of June 2002, the same year that later set a record in Greenland Ice Sheet melting. These images show the Greenland Ice Sheet midway through the seasonal melt. Summer melting begins in late April and reaches its maximum in late August or early September. As in previous years, blue melt ponds liberally dot the surface. Though they may look pretty, too many ponds spell trouble for the ice sheet. These ponds serve as reservoirs of water that can speed the ice’s journey to the sea. -
Summit Station Skiway Review
6 - 13 - TR L RRE C ERDC/ Engineering for Polar Operations, Logistics and Research (EPOLAR) Summit Station Skiway Review Margaret A. Knuth, Terry D. Melendy, March 2013 and Amy M. Burzynski Laboratory Research Research Engineering Engineering ld Regions Co and Approved for public release; distribution is unlimited. Engineering for Polar Operations, Logistics ERDC/CRREL TR-13-6 and Research (EPOLAR) February 2013 Summit Station Skiway Review Margaret A. Knuth, Terry D. Melendy, and Amy M. Burzynski Cold regions Research and Engineering Laboratory US Army Engineer Research and Development Center 72 Lyme Road Hanover, NH 03755 Final report Approved for public release; distribution is unlimited. Prepared for National Science Foundation, Office of Polar Programs, Arctic Research Support and Logistics Program Under Engineering for Polar Operations, Logistics and Research (EPOLAR) ERDC/CRREL TR-13-6 ii Abstract: Summit Station, located at the peak of the Greenland ice cap, is a scientific research station maintained by the National Science Founda- tion. Transportation to and from the station, for the delivery of personnel and materials, is by skied airplanes or by annual traverse. To support air- craft, the station staff uses heavy equipment to maintain a 5120.6 × 61.0 m (16,800 × 200 ft) skiway. When the station is open for the summer season, from mid-April through August, the skiway sees regular use. This report defines procedures and identifies equipment to strengthen and smooth the skiway surface. Effective skiway maintenance has the potential to help re- duce the overall skiway maintenance time, decrease the number of slides per flight period, increase ACLs, and reduce the need for Jet Assisted Take-Offs (JATO). -
Topography of the North and South Polar Ice Caps on Mars
TOPOGRAPHY OF THE NORTH AND SOUTH POLAR ICE CAPS ON MARS. Anton B. Ivanov, Duane O. Muhleman, California Institute of Technology, Pasadena, CA, 91125, USA, [email protected]. Recent observations by Mars Orbiter Laser Altimeter have of the underlying topography under the ice cap or some other provided high resolution view of the Northern Ice cap [7], large scale process. We know from Viking observations that compiled on the basis of data returned during Science Phasing there is substantially less amounts of water vapor observed Orbit. Starting in March 1999, Mars Global Surveyor was over the south pole than over the north pole. On the other hand transferred into its mapping configuration and began system- the albedo of the southern ice cap is lower, so we can expect atic observations of Mars. Data returned during the mapping higher temperatures on the surface and hence more extensive orbit allowed compilation of high resolution topography grid evaporation. Possibly, an insulating layer of dust prevents for the southern ice cap ( [5]). This paper will concentrate on water ice from escape. Relative age estimates, obtained from description of observations of the southern ice cap topography craters by [4] suggest older ages for the southern polar layered and comparison with the northern ice cap. We will com- deposits, than for the northern polar layered deposits. We do pare topography across the ice caps and apply a sublimation not know well composition of the south polar layered deposits model ( [2]), which was developed to explain the shape of the and it is hard to hypothesize on evaporation rates at this point.