Steven Phipps1, Jacqueline Halpin1 1Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, Australia Ice sheet models are the only physically-based tools that allow us to simulate the future evolution of the Antarctic Ice Sheet, including its contribution towards...
- March 9, 2018
Brice Van Liefferinge1, Frank Pattyn1, Marie Cavitte2, Nanna Karlsson3,4, Duncan Young2, Johannes Sutter4,5, Olaf Eisen4,6 1Université Libre De Bruxelles, Brussels, Belgium, 2University of Texas at Austin, Austin, USA, 3Geological Survey of Denmark and Greenland (GEUS), Copenhagen, Denmark, 4Alfred Wegener Institute,...
- March 9, 2018
Sandra Mclaren1, Chris Carson2, Roger Powell1 1University Of Melbourne, University Of Melbourne, Australia, 2Geoscience Australia, Canberra, AUSTRALIA Prior to the breakup of Gondwana (beginning around the late Cretaceous) cratonic rocks of southern Australia, including the Gawler and Curnamona cratons, are...
- March 9, 2018
Ben Mather1, Javier Fullea1, Louis Moresi2, Thomas Farrell1, Robert Delhaye1 1Dublin Institute For Advanced Studies, Dublin, Ireland, 2The University of Melbourne, Melbourne, Australia Surface heat flux is highly sensitive to small temperature fluctuations at varying timescales. The magnitude of these...
- March 9, 2018
Yasmina M Martos1,2, Manuel Catalan3, Tom A Jordan4, Alexander Golynsky5, Dmitry Golynsky5, Graeme Eagles6 1NASA Goddard Space Flight Center, Greenbelt, United States, 2University of Maryland, College Park, United States, 3Royal Observatory of the Spanish Navy, San Fernando, Spain, 4British Antarctic...
- March 9, 2018
Alessandro Maritati1, Jacqueline Halpin1, Joanne Whittaker1, 1Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, Australia Heat produced by radioactive decay within East Antarctic crust provides a significant contribution to the total heat flow balance that is supplied at...
- March 9, 2018
Bernd Kulessa1, Kerry Key2, Sarah Thompson1, Martin Siegert3 1Glaciology Group, College of Science, Swansea University, UK, 2Lamont-Doherty Earth Observatory, Columbia University, USA, 3Grantham Institute, and Department of Earth Science and Engineering, Imperial College London, UK Numerical models of contemporary as...
- March 9, 2018
Masaki Kanao1 1National Institute of Polar Research, Tachikawa, Japan Characteristic features of infrasound waves observed in the Antarctic reflect the physical interaction between the surface environment along the continental margin and the surrounding Southern Ocean. The temporal–spatial variability of the...
- March 9, 2018
Genti Toyokuni2, Masaki Kanao1, Hiroshi Takenaka3, Ryota Takagi2, Seiji Tsuboi4, Yoko Tono5, Dean Childs6, Dapeng Zhao2 1National Institute of Polar Research, Tachikawa, Japan, 2Tohoku University, Sendai , Japan, 3Okayama University, Kita-ku, Japan, 4JAMSTEC, Kanazawa-ku, Japan, 5MEXT, Chiyoda-ku, Japan, 6PASSCAL/IRIS, Socorro,...
- March 9, 2018
Audrey Huerta1 1Central Washington University, Ellensburg, United States Results from thermomechanical models of tectonic systems can be used to constrain the magnitude and spatial variability of geothermal heat flux across continents. In the case of the Antarctic Continent, the unique...
- March 9, 2018
