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Report | First Antarctic Parliamentarian's Assembly Puts
Report | First Antarctic Parliamentarian’s Assembly puts Climate Change at top of Agenda The first ever Antarctic Parliamentarians Assembly hosted by the UK’s All-Party Parliamentary Group for the Polar Regions in London concluded with a warning from parliamentary delegates of “potentially catastrophic” effects of climate change on Antarctica. Plastics, fisheries and tourism were also highlighted with Parliamentarians noting the anticipated continued increase in tourism and its potential impacts on Antarctic ecosystems. The meeting, at the Royal United Services Institute (RUSI) on Whitehall, London on December 2 and 3, was convened to mark the 60th anniversary of the signing of the Antarctic Treaty and discuss the protection and preservation of the white continent, with 19 parliamentarians and delegates representing 13 countries, present. The Assembly provided a valuable learning opportunity for parliamentarians, rather than governments, to enable them to pressure their national legislatures to support the work of the Antarctic Treaty. The first day, attended by IAATO’s Director of Environment and Science Coordination Amanda Lynnes and Communications and Engagement Manager, Hayley Collings aimed to inform parliamentarians about the importance of Antarctica for our planet. It featured scene-setting presentations from Lord Ahmad, UK Minister for the Polar Regions, Dame Jane Francis, Director of British Antarctic Survey and Jane Rumble, head the UK Foreign and Commonwealth Office’s Polar Regions Department before moving on to a series of -
The Triggers of the Disaggregation of Voyeykov Ice Shelf (2007), Wilkes Land, East Antarctica, and Its Subsequent Evolution
Journal of Glaciology The triggers of the disaggregation of Voyeykov Ice Shelf (2007), Wilkes Land, East Antarctica, and its subsequent evolution Article Jennifer F. Arthur1 , Chris R. Stokes1, Stewart S. R. Jamieson1, 1 2 3 Cite this article: Arthur JF, Stokes CR, Bertie W. J. Miles , J. Rachel Carr and Amber A. Leeson Jamieson SSR, Miles BWJ, Carr JR, Leeson AA (2021). The triggers of the disaggregation of 1Department of Geography, Durham University, Durham, DH1 3LE, UK; 2School of Geography, Politics and Voyeykov Ice Shelf (2007), Wilkes Land, East Sociology, Newcastle University, Newcastle-upon-Tyne, NE1 7RU, UK and 3Lancaster Environment Centre/Data Antarctica, and its subsequent evolution. Science Institute, Lancaster University, Bailrigg, Lancaster, LA1 4YW, UK Journal of Glaciology 1–19. https://doi.org/ 10.1017/jog.2021.45 Abstract Received: 15 September 2020 The weakening and/or removal of floating ice shelves in Antarctica can induce inland ice flow Revised: 31 March 2021 Accepted: 1 April 2021 acceleration. Numerical modelling suggests these processes will play an important role in Antarctica’s future sea-level contribution, but our understanding of the mechanisms that lead Keywords: to ice tongue/shelf collapse is incomplete and largely based on observations from the Ice/atmosphere interactions; ice/ocean Antarctic Peninsula and West Antarctica. Here, we use remote sensing of structural glaciology interactions; ice-shelf break-up; melt-surface; sea-ice/ice-shelf interactions and ice velocity from 2001 to 2020 and analyse potential ocean-climate forcings to identify mechanisms that triggered the rapid disintegration of ∼2445 km2 of ice mélange and part of Author for correspondence: the Voyeykov Ice Shelf in Wilkes Land, East Antarctica between 27 March and 28 May 2007. -
Antarctic Drilling Recovers Stratigraphic Records from the Continental Margin David M
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Papers in the Earth and Atmospheric Sciences Earth and Atmospheric Sciences, Department of 3-17-2009 Antarctic Drilling Recovers Stratigraphic Records From the Continental Margin David M. Harwood University of Nebraska-Lincoln, [email protected] Fabio Florindo Istituto Nazionale di Geofisica e Vulcanologia, [email protected] Franco M. Talarico Università di Siena, [email protected] Richard Levy GNS Science Gerhard Kuhn Alfred Wegener Institute for Polar and Marine Research (AWI) See next page for additional authors Follow this and additional works at: https://digitalcommons.unl.edu/geosciencefacpub Part of the Earth Sciences Commons Harwood, David M.; Florindo, Fabio; Talarico, Franco M.; Levy, Richard; Kuhn, Gerhard; Naish, Tim; Niessen, F.; Powell, Ross; Pyne, Alex; and Wilson, Gary, "Antarctic Drilling Recovers Stratigraphic Records From the Continental Margin" (2009). Papers in the Earth and Atmospheric Sciences. 497. https://digitalcommons.unl.edu/geosciencefacpub/497 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Papers in the Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. Authors David M. Harwood, Fabio Florindo, Franco M. Talarico, Richard Levy, Gerhard Kuhn, Tim Naish, F. Niessen, Ross Powell, Alex Pyne, and Gary Wilson This article is available at DigitalCommons@University of Nebraska - Lincoln: https://digitalcommons.unl.edu/geosciencefacpub/ 497 Eos, Vol. 90, No. 11, 17 March 2009 Antarctic Drilling Recovers Stratigraphic Records time interval in the development of mod- ern Antarctic ice sheets [Zachos et al., From the Continental Margin 2001; Shevenell et al., 2004]. -
Tidal Modulation of Antarctic Ice Shelf Melting Ole Richter1,2, David E
Tidal Modulation of Antarctic Ice Shelf Melting Ole Richter1,2, David E. Gwyther1, Matt A. King2, and Benjamin K. Galton-Fenzi3 1Institute for Marine and Antarctic Studies, University of Tasmania, Private Bag 129, Hobart, TAS, 7001, Australia. 2Geography & Spatial Sciences, School of Technology, Environments and Design, University of Tasmania, Hobart, TAS, 7001, Australia. 3Australian Antarctic Division, Kingston, TAS, 7050, Australia. Correspondence: Ole Richter ([email protected]) This is a non-peer reviewed preprint submitted to EarthArXiv. This preprint has also been submitted to The Cryosphere for peer review. 1 Abstract. Tides influence basal melting of individual Antarctic ice shelves, but their net impact on Antarctic-wide ice-ocean interaction has yet to be constrained. Here we quantify the impact of tides on ice shelf melting and the continental shelf seas 5 by means of a 4 km resolution circum-Antarctic ocean model. Activating tides in the model increases the total basal mass loss by 57 Gt/yr (4 %), while decreasing continental shelf temperatures by 0.04 ◦C, indicating a slightly more efficient conversion of ocean heat into ice shelf melting. Regional variations can be larger, with melt rate modulations exceeding 500 % and temperatures changing by more than 0.5 ◦C, highlighting the importance of capturing tides for robust modelling of glacier systems and coastal oceans. Tide-induced changes around the Antarctic Peninsula have a dipolar distribution with decreased 10 ocean temperatures and reduced melting towards the Bellingshausen Sea and warming along the continental shelf break on the Weddell Sea side. This warming extends under the Ronne Ice Shelf, which also features one of the highest increases in area-averaged basal melting (150 %) when tides are included. -
Ice News Bulletin of the International
ISSN 0019–1043 Ice News Bulletin of the International Glaciological Society Number 154 3rd Issue 2010 Contents 2 From the Editor 25 Staff changes 3 Recent work 25 New Chair for the Awards Committee 3 Australia 26 Report from the IGS conference on Snow, 3 Ice cores Ice and Humanity in a Changing Climate, 4 Ice sheets, glaciers and icebergs Sapporo, Japan, 21–25 June 2010 5 Sea ice and glacimarine processes 31 Report from the British Branch Meeting, 6 Large-scale processes Aberystwyth 7 Remote sensing 32 Meetings of other societies 8 Numerical modelling 32 Workshop of Glacial Erosion 9 Ecology within glacial systems Modelling 10 Geosciences and glacial geology 33 Northwest Glaciologists’ Meeting 11 International Glaciological Society 35 UKPN Circumpolar Remote Sensing 11 Journal of Glaciology Workshop 14 Annals of Glaciology 51(56) 35 Notes from the production team 15 Annals of Glaciology 52(57) 36 San Diego symposium, 2nd circular 16 Annals of Glaciology 52(58) 44 News 18 Annals of Glaciology 52(59) 44 Obituary: Keith Echelmeyer 19 Annual General Meeting 2010 46 70th birthday celebration for 23 Books received Sigfús Johnsen 24 Award of the Richardson Medal to 48 Glaciological diary Jo Jacka 54 New members Cover picture: Spiral icicle extruded from the tubular steel frame of a jungle gym in Moscow, November 2010. Photo: Alexander Nevzorov. Scanning electron micrograph of the ice crystal used in headings by kind permission of William P. Wergin, Agricultural Research Service, US Department of Agriculture EXCLUSION CLAUSE. While care is taken to provide accurate accounts and information in this Newsletter, neither the editor nor the International Glaciological Society undertakes any liability for omissions or errors. -
Article Is Available On- Mand of Charles Wilkes, USN
The Cryosphere, 15, 663–676, 2021 https://doi.org/10.5194/tc-15-663-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Recent acceleration of Denman Glacier (1972–2017), East Antarctica, driven by grounding line retreat and changes in ice tongue configuration Bertie W. J. Miles1, Jim R. Jordan2, Chris R. Stokes1, Stewart S. R. Jamieson1, G. Hilmar Gudmundsson2, and Adrian Jenkins2 1Department of Geography, Durham University, Durham, DH1 3LE, UK 2Department of Geography and Environmental Sciences, Northumbria University, Newcastle upon Tyne, NE1 8ST, UK Correspondence: Bertie W. J. Miles ([email protected]) Received: 16 June 2020 – Discussion started: 6 July 2020 Revised: 9 November 2020 – Accepted: 10 December 2020 – Published: 11 February 2021 Abstract. After Totten, Denman Glacier is the largest con- 1 Introduction tributor to sea level rise in East Antarctica. Denman’s catch- ment contains an ice volume equivalent to 1.5 m of global sea Over the past 2 decades, outlet glaciers along the coast- level and sits in the Aurora Subglacial Basin (ASB). Geolog- line of Wilkes Land, East Antarctica, have been thinning ical evidence of this basin’s sensitivity to past warm periods, (Pritchard et al., 2009; Flament and Remy, 2012; Helm et combined with recent observations showing that Denman’s al., 2014; Schröder et al., 2019), losing mass (King et al., ice speed is accelerating and its grounding line is retreating 2012; Gardner et al., 2018; Shen et al., 2018; Rignot et al., along a retrograde slope, has raised the prospect that its con- 2019) and retreating (Miles et al., 2013, 2016). -
Program Here
Paris Agreement: Are we there yet? A Panel Discussion to celebrate the fifth anniversary of the COP21 Wellington 11 December 2 pm Victoria University of Wellington Hunter Council Chamber Level 2, Hunter Building, Kelburn Campus Or join us online https://vuw.zoom.us/j/95363120801 PROGRAMME 2.00-2.15 pm Opening HE Sylvaine Carla Le-Vert, Ambassador of France in New Zealand Welcome Dr Geoffroy Lamarche, President, Fast! 2.15-3.10pm Pre-panel short talks From Kyoto to Paris to … Wellington. Five new things and five big questions for New Zealand Dr Adrian Macey, Institute for Governance and Policy Studies, Victoria University Investigating biological responses to climate change Prof Peter Lockart, School of Fundamental Sciences, Massey University Climate change and migrations in the Pacific: which protection for humans escaping disasters and sea rise level? Prof Geraldine Giraudeau, Public Law, University of Perpignan The science of the climate emergency and implications for mitigation and adaptation Prof Tim Naish, Earth Sciences, Antarctic Research Centre 3:30-4:30 Panel discussion Facilitated by Dr Geoffroy Lamarche, President of Fast! and Julie Merckling Joined by FAST! Christchurch 4.30-5.30 Cheese from The Cheese Wheel and Wine tasting Dr Adrian Macey Adjunct Professor, New Zealand Climate Change Research Institute and Senior Associate, Institute for Governance and Policy Studies, School of Government, Victoria University of Wellington After studies in science and literature, Adrian Macey took up a career in the Ministry of Foreign Affairs in Paris, Apia, Geneva and Bangkok. In Wellington he was director of human resources for four years, and later Chief Trade Negotiator, responsible for the WTO and all bilateral and multilateral trade negotiations for New Zealand. -
Noaa 4860 DS1.Pdf
PROPOSED ACTION: Issuance of an Incidental Harassment Authorization to the National Science Foundation and Antarctic Support Contract to Take Marine Mammals by Harassment Incidental to a Low-Energy Marine Geophysical Survey in the Dumont d’Urville Sea off the Coast of East Antarctica, January to March 2014. TYPE OF STATEMENT: Environmental Assessment LEAD AGENCY: U.S. Department of Commerce, National Oceanic and Atmospheric Administration National Marine Fisheries Service RESPONSIBLE OFFICIAL: Donna S. Wieting, Director, Office of Protected Resources, National Marine Fisheries Service FOR FURTHER INFORMATION: Howard Goldstein National Marine Fisheries Service Office of Protected Resources, Permits and Conservation Division 1315 East West Highway Silver Spring, MD 20910 301-427-8401 LOCATION: Selected regions of the Dumont d’Urville Sea in International Waters of the Southern Ocean off the coast of East Antarctica (Approximately 64º South, between 95 and 135º East, and 65º South, between 140 to 165º East) ABSTRACT: This Environmental Assessment analyzes the environmental impacts of the National Marine Fisheries Service, Office of Protected Resources, Permits and Conservation Division’s proposal to issue an Incidental Harassment Authorization to the National Science Foundation and Antarctic Support Contract for the taking, by Level B harassment, of small numbers of marine mammals, incidental to conducting a low-energy marine geophysical survey in the Dumont d’Urville Sea, January to March 2014. CONTENTS List of Abbreviations or Acronyms -
A Word from the Director an Audience with the Governor-General There Is Something for Everyone in This Newsletter
OTHER ACTIVITIES Climate Change in the Pacific Professor Guilford opened a three-day conference at Victoria community leaders and NGO representatives, from at least 17 University from 15-17 February focusing on the threat of climate Pacific nations. Speakers included Republic of Kiribati President change in the Pacific, stressing his heartfelt concern over the issue. Anote Tong, international experts, James Renwick (SGEES) and the ARC's Tim Naish. Professor Guilford said the science behind climate change is “crystal clear” and can’t be ignored. President Anote Tong described how some of the nation’s islands may disappear within two or three decades due to rising sea Victoria’s own Climate Change Research Institute is working to levels, while James described how changes in rainfall, tropical provide a better link between science and policy, while the cyclones and temperature extremes, are having devastating Antarctic Research Centre is looking at the Antarctic climate and Issue 26: June 2016 IceSkedNewsletter of the Antarctic Research Centre effects on food security and communities, and Tim spoke on the its influence on the global climate system. The conference brought Victoria University of Wellington effects of sea-level rise. together top scientists, environmentalists, policy makers, A Word From the Director An Audience with the Governor-General There is something for everyone in this newsletter. We report on some exciting fieldwork conducted by our staff and students this summer On the 16 February, the ARC was honoured to be involved with a visit from the in New Zealand and Antarctica, as well as profile some outreach and communication activities. -
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Obliquity-Paced Pliocene West Antarctic Ice Sheet Oscillations
Vol 458 | 19 March 2009 | doi:10.1038/nature07867 LETTERS Obliquity-paced Pliocene West Antarctic ice sheet oscillations T. Naish1,2, R. Powell3, R. Levy4{, G. Wilson5, R. Scherer3, F. Talarico6, L. Krissek7, F. Niessen8, M. Pompilio9, T. Wilson7, L. Carter1, R. DeConto10, P. Huybers11, R. McKay1, D. Pollard12, J. Ross13, D. Winter4, P. Barrett1, G. Browne2, R. Cody1,2, E. Cowan14, J. Crampton2, G. Dunbar1, N. Dunbar13, F. Florindo15, C. Gebhardt8, I. Graham2, M. Hannah1, D. Hansaraj1,2, D. Harwood4, D. Helling8, S. Henrys2, L. Hinnov16, G. Kuhn8, P. Kyle13,A.La¨ufer17, P. Maffioli18, D. Magens8, K. Mandernack19, W. McIntosh13, C. Millan7, R. Morin20, C. Ohneiser5, T. Paulsen21, D. Persico22, I. Raine2, J. Reed23,4, C. Riesselman24, L. Sagnotti15, D. Schmitt25, C. Sjunneskog26, P. Strong2, M. Taviani27, S. Vogel3, T. Wilch28 & T. Williams29 Thirty years after oxygen isotope records from microfossils deposited The Earth’s climate system during the Pliocene and early- in ocean sediments confirmed the hypothesis that variations in the Pleistocene epochs was regulated by a ,40-kyr periodicity. The geo- Earth’s orbital geometry control the ice ages1, fundamental questions logical evidence for this is widespread and expressed in polar to remain over the response of the Antarctic ice sheets to orbital cycles2. equatorial depositional environments including (1) ice volume from Furthermore, an understanding of the behaviour of the marine- oxygen isotope (d18O) records, that co-vary with the pattern of ice- based West Antarctic ice sheet (WAIS) -
2010GM000935-SE-Pattyn 27..44
Antarctic Subglacial Lake Discharges Frank Pattyn Laboratoire de Glaciologie, Département des Sciences de la Terre et de l’Environnement Université Libre de Bruxelles, Brussels, Belgium Antarctic subglacial lakes were long time supposed to be relatively closed and stable environments with long residence times and slow circulations. This view has recently been challenged with evidence of active subglacial lake discharge under- neath the Antarctic ice sheet. Satellite altimetry observations witnessed rapid changes in surface elevation across subglacial lakes over periods ranging from several months to more than a year, which were interpreted as subglacial lake discharge and subsequent lake filling, and which seem to be a common and widespread feature. Such discharges are comparable to jökulhlaups and can be modeled that way using the Nye-Röthlisberger theory. Considering the ice at the base of the ice sheet at pressure melting point, subglacial conduits are sustainable over periods of more than a year and over distances of several hundreds of kilo- meters. Coupling of an ice sheet model to a subglacial lake system demonstrated that small changes in surface slope are sufficient to start and sustain episodic subglacial drainage events on decadal time scales. Therefore, lake discharge may well be a common feature of the subglacial hydrological system, influencing the behavior of large ice sheets, especially when subglacial lakes are perched at or near the onset of large outlet glaciers and ice streams. While most of the observed discharge events are relatively small (101–102 m3 sÀ1), evidence for larger subgla- cial discharges is found in ice free areas bordering Antarctica, and witnessing subglacial floods of more than 106 m3 sÀ1 that occurred during the middle Miocene.