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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 Significant Acceleration of Ice Volume Discharge Preceded a Major Retreat of a West Antarctic Paleo–Ice Stream
https://doi.org/10.1130/G46916.1 Manuscript received 26 August 2019 Revised manuscript received 23 November 2019 Manuscript accepted 26 November 2019 © 2019 Geological Society of America. For permission to copy, contact [email protected]. A signifcant acceleration of ice volume discharge preceded a major retreat of a West Antarctic paleo–ice stream Philip J. Bart1 and Slawek Tulaczyk2 1 Department of Geology and Geophysics, Louisiana State University, Baton Rouge, Louisiana 70803, USA 2 Department of Earth and Planetary Sciences, University of California Santa Cruz, Santa Cruz, California 95064, USA ABSTRACT SEDIMENT AND ICE DISCHARGE For the period between 14.7 and 11.5 cal. (calibrated) kyr B.P, the sediment fux of Bind- FROM THE PALEO–BINDSCHADLER schadler Ice Stream (BIS; West Antarctica) averaged 1.7 × 108 m3 a−1. This implies that BIS ICE STREAM velocity averaged 500 ± 120 m a−1. At a fner resolution, the data suggest two stages of ice Radiocarbon ages from benthic foramin- stream fow. During the frst 2400 ± 400 years of a grounding-zone stillstand, ice stream fow ifera (Bart et al., 2018) (Table 1) indicate that averaged 200 ± 90 m a−1. Following ice-shelf breakup at 12.3 ± 0.2 cal. kyr B.P., fow acceler- the paleo-BIS grounding line had retreated ated to 1350 ± 580 m a−1. The estimated ice volume discharge after breakup exceeds the bal- 70 km from its maximum (LGM) position by ance velocity by a factor of two and implies ice mass imbalance of −40 Gt a−1 just before the 14.7 ± 0.4 cal. -
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. -
Education Personal Research Interests Employment
Douglas Reed MacAyeal Department of the Geophysical Sciences The University of Chicago 5734 S. Ellis Ave. HGS 424 Chicago, IL Phone: (773) 702-8027 (o) (773) 752-6078 (h) (773) 702-9505 (f) (224) 500-7775 (c) [email protected] [email protected] last updated: March, 2020 Education 1983 Ph.D. Princeton University, Princeton, NJ Geophysical Fluid Dynamics advisor: Kirk Bryan 1979 M.S. University of Maine, Orono, ME Physics/Glaciology advisor: Robert Thomas 1976 Sc.B. Brown University, Providence, RI Physics Magna cum laude, honors in physics Personal Birth Date: 8 December, 1954; Age: 65 Birth Place: Boston, MA, USA Marital Status: Married, Linda A. MacAyeal (Sparks) Children: Leigh C. (MacAyeal) Kasten (Brown U., Sc.B.; Cornell U., DVM), Hannah R. MacAyeal (U. Penn, B.S., U. Penn Veterinary Medicine, DVM), Evan C. MacAyeal (Carleton College, B.A., Columbia University, Financial Engineering, M.S.) Research Interests The physical processes that determine the evolution of ice and climate on Earth over the past, present and future. Employment Department of the Geophysical Sciences, University of Chicago 1983-Present Professor (Asst. until 1987, Assoc. until 1992 and Full until present) Prior to 1983: I was a graduate student at Princeton University and University of Maine. Awards and Honors • 2019 Seligman Crystal, International Glaciological Society (IGS) • 2013 Nye Lecture, American Geophysical Union (AGU), Fall Meeting • 2010 Goldthwait Award (Polar Medal) of the Byrd Polar Research Center, Ohio State University • 2005 Provost’s Teaching Award of the University of Chicago • 2002 Quantrell Teaching Award of the University of Chicago • 1997 Richardson Medal of the IGS • 1988 James Macelwane Medal of the AGU • 1988 Fellow of the AGU • Antarctic geographic names: MacAyeal Ice Stream, MacAyeal Peak Teaching Experience • GeoSci 242: Geophysical Fluid Dynamics, I. -
Studies of Antarctic Ice Shelf Stability: Surface Melting, Basal Melting, and Ice Flow Dynamics
Studies of Antarctic ice shelf stability: surface melting, basal melting, and ice flow dynamics by Karen E. Alley B.A., Colgate University, 2012 A thesis submitted to the Faculty of the Graduate School of the University of Colorado in partial fulfillment of the requirement for the degree of Doctor of Philosophy Department of Geological Sciences 2017 This thesis entitled: Studies of Antarctic ice shelf stability: Surface melting, basal melting, and ice flow dynamics written by Karen E. Alley has been approved for the Department of Geological Sciences James White Ted Scambos Date The final copy of this thesis has been examined by the signatories, and we find that both the content and the form meet acceptable presentation standards of scholarly work in the above-mentioned discipline. ii Alley, Karen Elizabeth (Ph.D., Department of Geological Sciences) Studies of Antarctic ice shelf stability: Surface melting, basal melting, and ice flow dynamics Thesis directed by Senior Research Scientist T.A. Scambos and Professor J.W.C. White Abstract: Floating extensions of ice sheets, known as ice shelves, play a vital role in regulating the rate of ice flow into the Southern Ocean from the Antarctic Ice Sheet. Shear stresses imparted by contact with islands, embayment walls, and other obstructions transmit “backstress” to grounded ice. Ice shelf collapse reduces or eliminates this backstress, increasing mass flux to the ocean and therefore rates of sea level rise. This dissertation presents studies that address three main factors that regulate ice shelf stability: surface melt, basal melt, and ice flow dynamics. The first factor, surface melt, is assessed using active microwave backscatter. -
Did Holocene Climate Changes Drive West Antarctic Grounding Line Retreat and Re-Advance?
https://doi.org/10.5194/tc-2020-308 Preprint. Discussion started: 19 November 2020 c Author(s) 2020. CC BY 4.0 License. Did Holocene climate changes drive West Antarctic grounding line retreat and re-advance? Sarah U. Neuhaus1, Slawek M. Tulaczyk1, Nathan D. Stansell2, Jason J. Coenen2, Reed P. Scherer2, Jill 5 A. Mikucki3, Ross D. Powell2 1Earth and Planetary Sciences, University oF CaliFornia Santa Cruz, Santa Cruz, CA, 95064, USA 2Department oF Geology and Environmental Geosciences, Northern Illinois University, DeKalb, IL, 60115, USA 3Department oF Microbiology, University oF Tennessee Knoxville, Knoxville, TN, 37996, USA 10 Correspondence to: Sarah U. Neuhaus ([email protected]) Abstract. Knowledge oF past ice sheet conFigurations is useFul For informing projections of Future ice sheet dynamics and For calibrating ice sheet models. The topology oF grounding line retreat in the Ross Sea Sector oF Antarctica has been much debated, but it has generally been assumed that the modern ice sheet is as small as it has been for more than 100,000 years 15 (Conway et al., 1999; Lee et al., 2017; Lowry et al., 2019; McKay et al., 2016; Scherer et al., 1998). Recent findings suggest that the West Antarctic Ice Sheet (WAIS) grounding line retreated beyond its current location earlier in the Holocene and subsequently re-advanced to reach its modern position (Bradley et al., 2015; Kingslake et al., 2018). Here, we further constrain the post-LGM grounding line retreat and re-advance in the Ross Sea Sector using a two-phase model of radiocarbon input and decay in subglacial sediments From six sub-ice sampling locations. -
Variability in the Mass Flux of the Ross Sea Ice Streams, Antarctica, Over the Last Millennium
Portland State University PDXScholar Geology Faculty Publications and Presentations Geology 1-1-2012 Variability in the Mass Flux of the Ross Sea Ice Streams, Antarctica, over the last Millennium Ginny Catania University of Texas at Austin Christina L. Hulbe Portland State University Howard Conway University of Washington - Seattle Campus Ted A. Scambos University of Colorado at Boulder C. F. Raymond University of Washington - Seattle Campus Follow this and additional works at: https://pdxscholar.library.pdx.edu/geology_fac Part of the Geology Commons Let us know how access to this document benefits ou.y Citation Details Catania. G. A., C.L. Hulbe, H.B. Conway, T.A. Scambos, C.F. Raymond, 2012, Variability in the mass flux of the Ross Sea ice streams, Antarctica, over the last millennium. Journal of Glaciology, 58 (210), 741-752. This Article is brought to you for free and open access. It has been accepted for inclusion in Geology Faculty Publications and Presentations by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. Journal of Glaciology, Vol. 58, No. 210, 2012 doi: 10.3189/2012JoG11J219 741 Variability in the mass flux of the Ross ice streams, West Antarctica, over the last millennium Ginny CATANIA,1,2 Christina HULBE,3 Howard CONWAY,4 T.A. SCAMBOS,5 C.F. RAYMOND4 1Institute for Geophysics, University of Texas, Austin, TX, USA E-mail: [email protected] 2Department of Geology, University of Texas, Austin, TX, USA 3Department of Geology, Portland State University, Portland, OR, USA 4Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA 5National Snow and Ice Data Center, University of Colorado, Boulder, CO, USA ABSTRACT. -
Information to Users
Variations In Ice Flow And Glaciers Over Time And Space Item Type Thesis Authors Elsberg, Daniel Harry Download date 24/09/2021 03:40:40 Link to Item http://hdl.handle.net/11122/8657 INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter face, while others may be from any type of computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand comer and continuing from left to right in equal sections with small overlaps. ProQuest Information and Learning 300 North Zeeb Road, Ann Arbor, Ml 48106-1346 USA 800-521-0600 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. VARIATIONS IN ICE FLOW AND GLACIERS OVER TIME AND SPACE A THESIS Presented to the Faculty of the University of Alaska Fairbanks in Partial Fulfillment of the Requirements for the Degree of DOCTOR OF PHILOSOPHY By Daniel Harry Elsberg, B.S. -
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. -
Spatiotemporal Variations in the Surface Velocities of Antarctic Peninsula Glaciers
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | The Cryosphere Discuss., 8, 5875–5910, 2014 www.the-cryosphere-discuss.net/8/5875/2014/ doi:10.5194/tcd-8-5875-2014 TCD © Author(s) 2014. CC Attribution 3.0 License. 8, 5875–5910, 2014 This discussion paper is/has been under review for the journal The Cryosphere (TC). Spatiotemporal Please refer to the corresponding final paper in TC if available. variations in the surface velocities of Spatiotemporal variations in the surface Antarctic Peninsula glaciers velocities of Antarctic Peninsula glaciers J. Chen et al. J. Chen1,2, C. Q. Ke1,2, and Z. D. Shao1,2 1Jiangsu Provincial Key Laboratory of Geographic Information Science and Technology, Title Page Nanjing University, Nanjing, 210023, China Abstract Introduction 2Key Laboratory for Satellite Mapping Technology and Applications of State Administration of Surveying, Mapping and Geoinformation of China, Nanjing University, Nanjing, 210023, China Conclusions References Received: 25 October 2014 – Accepted: 2 November 2014 – Published: 25 November 2014 Tables Figures Correspondence to: C. Q. Ke ([email protected]) J I Published by Copernicus Publications on behalf of the European Geosciences Union. J I Back Close Full Screen / Esc Printer-friendly Version Interactive Discussion 5875 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract TCD Velocity is an important parameter for the estimation of glacier mass balance, which directly signals the response of glaciers to climate change. Antarctic ice sheet move- 8, 5875–5910, 2014 ment and the associated spatiotemporal velocity variations are of great significance to 5 global sea level rise. In this study, we estimate Antarctic Peninsula glacier velocities Spatiotemporal using the co-registration of optically sensed images and correlation (hereafter referred variations in the to as COSI-Corr) based on moderate-resolution imaging spectroradiometer Level 1B surface velocities of data (hereafter referred to as MODIS L1B). -
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. -
Fast-Flow Signature in the Stagnated Kamb Ice Stream, West Antarctica
This is a repository copy of Fast-flow signature in the stagnated Kamb Ice Stream, West Antarctica. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/92154/ Version: Accepted Version Article: Ng, F. and Conway, H. (2004) Fast-flow signature in the stagnated Kamb Ice Stream, West Antarctica. Geology, 32 (6). 481 - 484. ISSN 0091-7613 https://doi.org/10.1130/G20317.1 Reuse Unless indicated otherwise, fulltext items are protected by copyright with all rights reserved. The copyright exception in section 29 of the Copyright, Designs and Patents Act 1988 allows the making of a single copy solely for the purpose of non-commercial research or private study within the limits of fair dealing. The publisher or other rights-holder may allow further reproduction and re-use of this version - refer to the White Rose Research Online record for this item. Where records identify the publisher as the copyright holder, users can verify any specific terms of use on the publisher’s website. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ Ng & Conway (G20317), p. 1 1 2 3 Fast-flow signature in the stagnated Kamb Ice 4 Stream, West Antarctica 5 Felix Ng 6 Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of 7 Technology, Cambridge, Massachusetts 02139, USA 8 Howard Conway 9 Department of Earth and Space Sciences, University of Washington, Seattle, Washington 98195, 10 USA 11 12 ABSTRACT 13 Among the major ice streams that drain West Antarctica, Kamb Ice Stream 14 (formerly called Ice Stream C) is unique in that it stagnated ~150 yr ago, but its former 15 fast-flow conditions are virtually unknown.