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Species Status Assessment Emperor Penguin (Aptenodytes Fosteri)
SPECIES STATUS ASSESSMENT EMPEROR PENGUIN (APTENODYTES FOSTERI) Emperor penguin chicks being socialized by male parents at Auster Rookery, 2008. Photo Credit: Gary Miller, Australian Antarctic Program. Version 1.0 December 2020 U.S. Fish and Wildlife Service, Ecological Services Program Branch of Delisting and Foreign Species Falls Church, Virginia Acknowledgements: EXECUTIVE SUMMARY Penguins are flightless birds that are highly adapted for the marine environment. The emperor penguin (Aptenodytes forsteri) is the tallest and heaviest of all living penguin species. Emperors are near the top of the Southern Ocean’s food chain and primarily consume Antarctic silverfish, Antarctic krill, and squid. They are excellent swimmers and can dive to great depths. The average life span of emperor penguin in the wild is 15 to 20 years. Emperor penguins currently breed at 61 colonies located around Antarctica, with the largest colonies in the Ross Sea and Weddell Sea. The total population size is estimated at approximately 270,000–280,000 breeding pairs or 625,000–650,000 total birds. Emperor penguin depends upon stable fast ice throughout their 8–9 month breeding season to complete the rearing of its single chick. They are the only warm-blooded Antarctic species that breeds during the austral winter and therefore uniquely adapted to its environment. Breeding colonies mainly occur on fast ice, close to the coast or closely offshore, and amongst closely packed grounded icebergs that prevent ice breaking out during the breeding season and provide shelter from the wind. Sea ice extent in the Southern Ocean has undergone considerable inter-annual variability over the last 40 years, although with much greater inter-annual variability in the five sectors than for the Southern Ocean as a whole. -
A Review of Ice-Sheet Dynamics in the Pine Island Glacier Basin, West Antarctica: Hypotheses of Instability Vs
Pine Island Glacier Review 5 July 1999 N:\PIGars-13.wp6 A review of ice-sheet dynamics in the Pine Island Glacier basin, West Antarctica: hypotheses of instability vs. observations of change. David G. Vaughan, Hugh F. J. Corr, Andrew M. Smith, Adrian Jenkins British Antarctic Survey, Natural Environment Research Council Charles R. Bentley, Mark D. Stenoien University of Wisconsin Stanley S. Jacobs Lamont-Doherty Earth Observatory of Columbia University Thomas B. Kellogg University of Maine Eric Rignot Jet Propulsion Laboratories, National Aeronautical and Space Administration Baerbel K. Lucchitta U.S. Geological Survey 1 Pine Island Glacier Review 5 July 1999 N:\PIGars-13.wp6 Abstract The Pine Island Glacier ice-drainage basin has often been cited as the part of the West Antarctic ice sheet most prone to substantial retreat on human time-scales. Here we review the literature and present new analyses showing that this ice-drainage basin is glaciologically unusual, in particular; due to high precipitation rates near the coast Pine Island Glacier basin has the second highest balance flux of any extant ice stream or glacier; tributary ice streams flow at intermediate velocities through the interior of the basin and have no clear onset regions; the tributaries coalesce to form Pine Island Glacier which has characteristics of outlet glaciers (e.g. high driving stress) and of ice streams (e.g. shear margins bordering slow-moving ice); the glacier flows across a complex grounding zone into an ice shelf coming into contact with warm Circumpolar Deep Water which fuels the highest basal melt-rates yet measured beneath an ice shelf; the ice front position may have retreated within the past few millennia but during the last few decades it appears to have shifted around a mean position. -
Article Is Available On- J.: the International Bathymetric Chart of the Southern Ocean Line At
The Cryosphere, 14, 1399–1408, 2020 https://doi.org/10.5194/tc-14-1399-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Getz Ice Shelf melt enhanced by freshwater discharge from beneath the West Antarctic Ice Sheet Wei Wei1, Donald D. Blankenship1, Jamin S. Greenbaum1, Noel Gourmelen2, Christine F. Dow3, Thomas G. Richter1, Chad A. Greene4, Duncan A. Young1, SangHoon Lee5, Tae-Wan Kim5, Won Sang Lee5, and Karen M. Assmann6,a 1Institute for Geophysics and Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, Austin, Texas, USA 2School of GeoSciences, University of Edinburgh, Edinburgh, UK 3Department of Geography and Environmental Management, University of Waterloo, Waterloo, Ontario, Canada 4Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA 5Korea Polar Research Institute, Incheon, South Korea 6Department of Earth Sciences, University of Gothenburg, Gothenburg, Sweden apresent address: Institute of Marine Research, Tromsø, Norway Correspondence: Wei Wei ([email protected]) Received: 18 July 2019 – Discussion started: 26 July 2019 Revised: 8 March 2020 – Accepted: 10 March 2020 – Published: 27 April 2020 Abstract. Antarctica’s Getz Ice Shelf has been rapidly thin- 1 Introduction ning in recent years, producing more meltwater than any other ice shelf in the world. The influx of fresh water is The Getz Ice Shelf (Getz herein) in West Antarctica is over known to substantially influence ocean circulation and bi- 500 km long and 30 to 100 km wide; it produces more fresh ological productivity, but relatively little is known about water than any other source in Antarctica (Rignot et al., 2013; the factors controlling basal melt rate or how basal melt is Jacobs et al., 2013), and in recent years its melt rate has spatially distributed beneath the ice shelf. -
FRISP 2018 PROGRAM (Abstracts Below)
FRISP 2018 PROGRAM (Abstracts below) Monday 3rd 19h00: Arrival in Aussois. 20h00: Dinner. Tuesday 4th 7h30 – 8h30: Breakfast. 8h30 – 8h40: Welcome and Introduction (JB. Sallée & N. Joudain) 8h40 – 10h20: 5 presentations. [Weddell/FRIS, 1st part] • Svenja Ryan. • Markus Janout. • Tore Hattermann. • Camille Akhoudas. • Kaitlin Naughten. 10h20 – 10h40: Tea or coffee Break. 10h40 – 12h00: 4 presentations. [Weddell/FRIS, 2nd part] • Kjersti Daae. • Keith Nicholls. • Ole Zeising. • Lukrecia Stulic. 12h00 – 14h00: Lunch. 14h00 – 16h00: 6 presentations. [Greenland] • Lu An. • Jérémie Mouginot. • Irena Vankova. • Fiama Straneo. • Julia Christmann. • Donald Slater. 16h00 – 18h00: Posters. 19h00: Dinner. Wednesday 5th 7h30 – 8h30: Breakfast. 8h30 – 10h10: 5 presentations. [Processes and parameterizations] • Lionel Favier. • Adrian Jenkins. • Catherine Vreugdenhil. • Lucie Vignes. • Stephen Warren. 10h10 – 10h40: Tea or coffee break. 10h40 – 12h00: 4 presentations. [Ross] • Stevens Craig. • Alena Malyarenko. • Carolyn Branecky Begeman. • Justin Lawrence. 12h00 – 14h00: Lunch. 14h00 – 16h00: 6 presentations. [Amundsen] • Karen Assmann. • Tae-Wan Kim. • Yoshihiro Nakayama. • Paul Holland. • Alessandro Silvano. • Won Sang Lee. 16h00 – 18h00: Posters. 19h00: Dinner. Thursday 6th 7h30 – 8h30: Breakfast. 8h30 – 9h50: 4 presentations. [Antarctic ice sheet/Southern Ocean] • Ole Richter. • Xylar Asay-Davis. • Bertie Miles. • William Lipscomb. 9h50 – 10h20: Tea or coffee Break. 10h20 – 11h20: 3 presentations [East Antarctica] • Minowa Masahiro. • Chad Greene. -
A Case Study of Sea Ice Concentration Retrieval Near Dibble Glacier, East Antarctica
European MSc in Marine Environment MER and Resources UPV/EHU–SOTON–UB-ULg REF: 2013-0237 MASTER THESIS PROJECT A case study of sea ice concentration retrieval near Dibble Glacier, East Antarctica: Contradicting observations between passive microwave remote sensing and optical satellites BY LAM Hoi Ming August 2016 Bremen, Germany PLENTZIA (UPV/EHU), SEPTEMBER 2016 European MSc in Marine Environment MER and Resources UPV/EHU–SOTON–UB-ULg REF: 2013-0237 Dr Manu Soto as teaching staff of the MER Master of the University of the Basque Country CERTIFIES: That the research work entitled “A case study of sea ice concentration retrieval near Dibble Glacier, East Antarctica: Contradiction between passive microwave remote sensing and optical satellite observations” has been carried out by LAM Hoi Ming in the Institute of Environmental Physics, University of Bremen under the supervision of Dr Gunnar Spreen from the of the University of Bremen in order to achieve 30 ECTS as a part of the MER Master program. In September 2016 Signed: Supervisor PLENTZIA (UPV/EHU), SEPTEMBER 2016 Abstract In East Antarctica, around 136°E 66°S, spurious appearance of polynya (open water area within an ice pack) is observed on ice concentration maps derived from the ASI (ARTIST Sea Ice) algorithm during the period of February to April 2014, using satellite data from the Advanced Microwave Scanning Radiometer 2 (AMSR-2). This contradicts with the visual images obtained by the Moderate Resolution Imaging Spectroradiometer (MODIS), which show the area to be ice covered during the period. In this study, data of ice concentration, brightness temperature, air temperature, snowfall, bathymetry, and wind in the area were analysed to identify possible explanations for the occurrence of such phenomenon, hereafter referred to as the artefact. -
Glacier Change Along West Antarctica's Marie Byrd Land Sector
Glacier change along West Antarctica’s Marie Byrd Land Sector and links to inter-decadal atmosphere-ocean variability Frazer D.W. Christie1, Robert G. Bingham1, Noel Gourmelen1, Eric J. Steig2, Rosie R. Bisset1, Hamish D. Pritchard3, Kate Snow1 and Simon F.B. Tett1 5 1School of GeoSciences, University of Edinburgh, Edinburgh, UK 2Department of Earth & Space Sciences, University of Washington, Seattle, USA 3British Antarctic Survey, Cambridge, UK Correspondence to: Frazer D.W. Christie ([email protected]) Abstract. Over the past 20 years satellite remote sensing has captured significant downwasting of glaciers that drain the West 10 Antarctic Ice Sheet into the ocean, particularly across the Amundsen Sea Sector. Along the neighbouring Marie Byrd Land Sector, situated west of Thwaites Glacier to Ross Ice Shelf, glaciological change has been only sparsely monitored. Here, we use optical satellite imagery to track grounding-line migration along the Marie Byrd Land Sector between 2003 and 2015, and compare observed changes with ICESat and CryoSat-2-derived surface elevation and thickness change records. During the observational period, 33% of the grounding line underwent retreat, with no significant advance recorded over the remainder 15 of the ~2200 km long coastline. The greatest retreat rates were observed along the 650-km-long Getz Ice Shelf, further west of which only minor retreat occurred. The relative glaciological stability west of Getz Ice Shelf can be attributed to a divergence of the Antarctic Circumpolar Current from the continental-shelf break at 135° W, coincident with a transition in the morphology of the continental shelf. Along Getz Ice Shelf, grounding-line retreat reduced by 68% during the CryoSat-2 era relative to earlier observations. -
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u... I C) C) co 1 USGS 0.. science for a changing world co :::2: Prepared in cooperation with the Scott Polar Research Institute, University of Cambridge, United Kingdom Coastal-change and glaciological map of the (I) ::E Bakutis Coast area, Antarctica: 1972-2002 ;::+' ::::r ::J c:r OJ ::J By Charles Swithinbank, RichardS. Williams, Jr. , Jane G. Ferrigno, OJ"" ::J 0.. Kevin M. Foley, and Christine E. Rosanova a :;:,..... CD ~ (I) I ("') a Geologic Investigations Series Map I- 2600- F (2d ed.) OJ ~ OJ '!; :;:, OJ ::J <0 co OJ ::J a_ <0 OJ n c; · a <0 n OJ 3 OJ "'C S, ..... :;:, CD a:r OJ ""a. (I) ("') a OJ .....(I) OJ <n OJ n OJ co .....,...... ~ C) .....,0 ~ b 0 C) b C) C) T....., Landsat Multispectral Scanner (MSS) image of Ma rtin and Bea r Peninsulas and Dotson Ice Shelf, Bakutis Coast, CT> C) An tarctica. Path 6, Row 11 3, acquired 30 December 1972. ? "T1 'N 0.. co 0.. 2003 ISBN 0-607-94827-2 U.S. Department of the Interior 0 Printed on rec ycl ed paper U.S. Geological Survey 9 11~ !1~~~,11~1!1! I!IJ 1)11 U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP I-2600-F (2d ed.) U.S. GEOLOGICAL SURVEY COASTAL-CHANGE AND GLACIOLOGICAL MAP OF THE BAKUTIS COAST AREA, ANTARCTICA: 1972-2002 . By Charles Swithinbank, 1 RichardS. Williams, Jr.,2 Jane G. Ferrigno,3 Kevin M. Foley, 3 and Christine E. Rosanova4 INTRODUCTION areas Landsat 7 Enhanced Thematic Mapper Plus (ETM+)), RADARSAT images, and other data where available, to compare Background changes over a 20- to 25- or 30-year time interval (or longer Changes in the area and volume of polar ice sheets are intri where data were available, as in the Antarctic Peninsula). -
S41467-021-23534-W.Pdf
ARTICLE https://doi.org/10.1038/s41467-021-23534-w OPEN Thermohaline structure and circulation beneath the Langhovde Glacier ice shelf in East Antarctica ✉ Masahiro Minowa 1 , Shin Sugiyama 1, Masato Ito1,2, Shiori Yamane1 & Shigeru Aoki1 Basal melting of ice shelves is considered to be the principal driver of recent ice mass loss in Antarctica. Nevertheless, in-situ oceanic data covering the extensive areas of a subshelf cavity are sparse. Here we show comprehensive structures of temperature, salinity and 1234567890():,; current measured in January 2018 through four boreholes drilled at a ~3-km-long ice shelf of Langhovde Glacier in East Antarctica. The measurements were performed in 302–12 m-thick ocean cavity beneath 234–412 m-thick ice shelf. The data indicate that Modified Warm Deep Water is transported into the grounding zone beneath a stratified buoyant plume. Water at the ice-ocean interface was warmer than the in-situ freezing point by 0.65–0.95°C, leading to a mean basal melt rate estimate of 1.42 m a−1. Our measurements indicate the existence of a density-driven water circulation in the cavity beneath the ice shelf of Langhovde Glacier, similar to that proposed for warm-ocean cavities of larger Antarctic ice shelves. 1 Institute of Low Temperature Science, Hokkaido University, Sapporo, Japan. 2Present address: Japan Agency for Marine-Earth Science and Technology, ✉ Yokosuka, Japan. email: [email protected] NATURE COMMUNICATIONS | (2021) 12:4209 | https://doi.org/10.1038/s41467-021-23534-w | www.nature.com/naturecommunications 1 ARTICLE NATURE COMMUNICATIONS | https://doi.org/10.1038/s41467-021-23534-w he Antarctic Ice Sheet feeds ice into the ocean through fast- lines is limited due to the difficulty of obtaining measurements. -
The Contrasting Response of Outlet Glaciers to Interior and Ocean Forcing
https://doi.org/10.5194/tc-2019-301 Preprint. Discussion started: 27 January 2020 c Author(s) 2020. CC BY 4.0 License. The contrasting response of outlet glaciers to interior and ocean forcing John Erich Christian1, Alexander Robel2, Cristian Proistosescu3,4,5, Gerard Roe1, Michelle Koutnik1, and Knut Christianson1 1Department of Earth and Space Sciences, University of Washington, Seattle, Washington, USA 2School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia, USA 3Joint Institute for the Study of the Atmosphere and the Ocean, University of Washington, Seattle, Washington, USA 4Department of Atmospheric Sciences, University of Illinois, Urbana-Champaign, Illinois, USA 5Department of Geology, University of Illinois, Urbana-Champaign, Illinois, USA Correspondence: John Erich Christian ([email protected]) Abstract. The dynamics of marine-terminating outlet glaciers are of fundamental interest in glaciology, and affect mass loss from ice sheets in a warming climate. In this study, we analyze the response of outlet glaciers to different sources of climate forcing. We find that outlet glaciers have a characteristically different transient response to surface-mass-balance forcing ap- plied over the interior than to oceanic forcing applied at the grounding line. A recently developed reduced model represents 5 outlet glacier dynamics via two widely-separated response timescales: a fast response associated with grounding-zone dynam- ics, and a slow response of interior ice. The reduced model is shown to emulate the behavior of a more complex numerical model of ice flow. Together, these models demonstrate that ocean forcing first engages the fast, local response, and then the slow adjustment of interior ice, whereas surface-mass-balance forcing is dominated by the slow interior adjustment. -
ENVIRONMENTAL IMPACT ASSESSMENT – AUSTRALIAN ANTARCTIC PROGRAM AVIATION OPERATIONS 2020-2025 Draft Released for Public Comment
ENVIRONMENTAL IMPACT ASSESSMENT – AUSTRALIAN ANTARCTIC PROGRAM AVIATION OPERATIONS 2020-2025 draft released for public comment This document should be cited as: Commonwealth of Australia (2020). Environmental Impact Assessment – Australian Antarctic Program Aviation Operations 2020-2025 – draft released for public comment. Australian Antarctic Division, Kingston. © Commonwealth of Australia 2020 This work is copyright. You may download, display, print and reproduce this material in unaltered form only (retaining this notice) for your personal, non-commercial use or use within your organisation. Apart from any use as permitted under the Copyright Act 1968, all other rights are reserved. Requests and enquiries concerning reproduction and rights should be addressed to. Disclaimer The contents of this document have been compiled using a range of source materials and were valid as at the time of its preparation. The Australian Government is not liable for any loss or damage that may be occasioned directly or indirectly through the use of or reliance on the contents of the document. Cover photos from L to R: groomed runway surface, Globemaster C17 at Wilkins Aerodrome, fuel drum stockpile at Davis, Airbus landing at Wilkins Aerodrome Prepared by: Dr Sandra Potter on behalf of: Mr Robb Clifton Operations Manager Australian Antarctic Division Kingston 7050 Australia 2 Contents Overview 7 1. Background 9 1.1 Australian Antarctic Program aviation 9 1.2 Previous assessments of aviation activities 10 1.3 Scope of this environmental impact assessment 11 1.4 Consultation and decision outcomes 12 2. Details of the proposed activity and its need 13 2.1 Introduction 13 2.2 Inter-continental flights 13 2.3 Air-drop operations 14 2.4 Air-to-air refuelling operations 14 2.5 Operation of Wilkins Aerodrome 15 2.6 Intra-continental fixed-wing operations 17 2.7 Operation of ski landing areas 18 2.8 Helicopter operations 18 2.9 Fuel storage and use 19 2.10 Aviation activities at other sites 20 2.11 Unmanned aerial systems 20 2.12 Facility decommissioning 21 3. -
Déglaciation De La Vallée Supérieure De L'outaouais, Le Lac Barlow Et Le Sud Du Lac Ojibway, Québec
Document généré le 2 oct. 2021 22:05 Géographie physique et Quaternaire Déglaciation de la vallée supérieure de l’Outaouais, le lac Barlow et le sud du lac Ojibway, Québec Déglaciation of the Upper Ottawa River Valley, Lake Barlow and South of Lake Ojibway, Québec Deglaziation des oberen Tales des Outaouais Flusses, des Barlow Sees, und des sülichen Ojibway Sees, Québec Jean Veillette Volume 37, numéro 1, 1983 Résumé de l'article Cet article propose une séquence de déglaciation pour une région située à l'est URI : https://id.erudit.org/iderudit/032499ar du lac Témiscamingue. La séquence est basée sur la cartographie des DOI : https://doi.org/10.7202/032499ar sédiments superficiels, sur de nombreuses marques d'écoulement glaciaire et sur des âges radiocarbones. Le tracé de la moraine d'Harricana se prolonge sur Aller au sommaire du numéro une longueur additionnelle de 125 km. L'extrémité sud de la moraine, au lac Témiscamingue, se rattache à la moraine du lac McConnell du côté ontarien, et il est probable que les deux fassent partie du même ensemble morainique. Plus Éditeur(s) de 400 mesures d'altitude prises sur des limites de délavage marquant le niveau maximal glaciolacustre et sur des hauts points de la plaine argileuse Les Presses de l'Université de Montréal (varves) indiquent qu'une profondeur d'eau de l'ordre de 50 m est requise pour la sédimentation des varves dans cette région. La zone intermédiaire ISSN comprend les surfaces ennoyées par les eaux proglaciaires, mais d'une profondeur de moins de 50 m. La valeur de Mysis relicta comme indicateur 0705-7199 (imprimé) biologique de l'aire d'extension paléolacustre maximale est mise en doute. -
The Antarctic Sun, December 26, 1999
See you next century! On the Web at http://www.asa.org December 26, 1999 Published during the austral summer at McMurdo Station, Antarctica, for the United States Antarctic Program They dig the Pole By Josh Landis The Antarctic Sun Nearly two miles above the nearest rock, the South Pole is one of the last places you’d expect to find miners. It’s a world of snow, ice and cold, where the “ground” holds no dirt. But it’s also the place three hard-rock miners and one coal miner are living and working this summer. They’re digging the tunnel that will hold the new station’s water and waste systems. More than 40 feet beneath the surface, they will push through 2,000 feet of firn—snow that’s as hard as wood and on its way to becoming ice. When the corridor is finished, two pipes will run through it. One will carry Winging it fresh water up from wells melted deep into Erik Barnes takes a walk atop Pegasus, a U.S. Navy Super Constellation that crashed on the ice cap. The other will carry sewage the McMurdo Ice Shelf in 1970. All passengers and crew survived the wreck. Pegasus back down when the wells are empty. airstrip was named after the downed plane. Photo by Josh Landis. Standing at the entrance to the tunnel, the air is numbingly cold. Insulated by layers of packed snow and chilled by eons of subzero weather, the temperature High-flying science is minus 56 degrees F. By Jeff Inglis Stepping inside, all noise from the The Antarctic Sun See “Miners”—Page 7 In the next few days, a giant floating bubble will appear over Williams Field and climb high into the heavens.