Mark Pittard1, Ben Galton-Fenzi2,3, Jason Roberts2,3, Christopher Watson4 1Department of Geography, Durham University, Durham, United Kingdom, 2Australian Antarctic Division, Kingston, Australia, 3Antarctic Climate & Ecosystems Cooperative Research Centre, Hobart, Australia, 4School of Land and Food, University of Tasmania, Hobart, Australia...
  • March 9, 2018
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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
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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
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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
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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
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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
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Derrick Hasterok1, Matthew Gard1, Samuel Jennings1 1University Of Adelaide, Adelaide, Australia Fifty years ago isostatic subsidence was proposed as a method to investigate the thermal state of the oceanic lithosphere. But it has always been more difficult to use isostatic...
  • March 9, 2018
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Fausto Ferraccioli1, Jörg Ebbing2 1Nerc/British Antarctic Survey, Cambridge, United Kingdom, 2University of Kiel, Kiel, Germany Geothermal heat flux is a key and yet poorly understood boundary condition that can affect past, present and future ice sheet dynamics via e.g. its...
  • March 9, 2018
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Ricarda Dziadek1, Fausto Ferraccioli2, Karsten Gohl1 1Alfred Wegener Institute – Helmholtz Centre For Polar And Marine Research, Bremerhaven, Germany, 2British Antarctic Survey, Cambridge, UK The West Antarctic Rift System is one of the least understood rift systems on earth, but...
  • March 9, 2018
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Ricarda Dziadek1, Karsten Gohl1, Norbert Kaul2 1Alfred Wegener Institute – Helmholtz Centre For Polar And Marine Research, Bremerhaven, Germany, 2University of Bremen, Department of Geosciences, Bremen, Germany Due to a complex tectonic and magmatic history of West Antarctica, the region...
  • March 9, 2018
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