Radar-Derived Internal Structure and Basal Roughness Characterization along a Traverse from Zhongshan Station to Dome A, East Antarctica

[1]  Guangyou Fang,et al.  High-Resolution Ice-Sounding Radar Measurements of Ice Thickness Over East Antarctic Ice Sheet as a Part of Chinese National Antarctic Research Expedition , 2018, IEEE Transactions on Geoscience and Remote Sensing.

[2]  Jason L. Roberts,et al.  High-resolution boundary conditions of an old ice target near Dome C, Antarctica , 2016 .

[3]  T. Neumann,et al.  Extent of low-accumulation 'wind glaze' areas on the East Antarctic plateau: implications for continental ice mass balance , 2012, Journal of Glaciology.

[4]  B. Scheuchl,et al.  Ice Flow of the Antarctic Ice Sheet , 2011, Science.

[5]  D. Sugden,et al.  Assessing the continuity of the blue ice climate record at Patriot Hills, Horseshoe Valley, West Antarctica , 2016 .

[6]  M. Siegert,et al.  Airborne radar evidence for tributary flow switching in Institute Ice Stream, West Antarctica: Implications for ice sheet configuration and dynamics , 2015 .

[7]  D. Vaughan,et al.  The basal roughness of Pine Island Glacier, West Antarctica , 2011, Journal of Glaciology.

[8]  Frank Pattyn,et al.  Antarctic subglacial conditions inferred from a hybrid ice sheet/ice stream model , 2010 .

[9]  A. Payne,et al.  Spectral roughness of subglacial topography and implications for former ice-sheet dynamics in East Antarctica , 2005 .

[10]  I. Joughin,et al.  High Geothermal Heat Flow, Basal Melt, and the Origin of Rapid Ice Flow in Central Greenland , 2001, Science.

[11]  Li Yuansheng,et al.  Ice velocity from static GPS observations along the transect from Zhongshan station to Dome A, East Antarctica , 2008, Annals of Glaciology.

[12]  S. Bo,et al.  Decadal GPS-derived ice surface velocity along the transect from Zhongshan Station to and around Dome Argus, East Antarctica, 2005–16 , 2018, Annals of Glaciology.

[13]  A. Humbert,et al.  Thermal structure and basal sliding parametrisation at Pine Island Glacier – a 3-D full-Stokes model study , 2014 .

[14]  Bo Sun,et al.  Radar isochronic layer dating for a deep ice core at Kunlun Station, Antarctica , 2019, Science China Earth Sciences.

[15]  Donald D. Blankenship,et al.  Initiation and long-term instability of the East Antarctic Ice Sheet , 2018 .

[16]  M. Siegert,et al.  Basal roughness of the Institute and Möller Ice Streams, West Antarctica: Process determination and landscape interpretation , 2014 .

[17]  J. Bamber,et al.  The englacial stratigraphy of Wilkes Land, East Antarctica, as revealed by internal radio-echo sounding layering, and its relationship with balance velocities , 2003, Annals of Glaciology.

[18]  Michael Studinger,et al.  Influence of Persistent Wind Scour on the Surface Mass Balance of Antarctica , 2013 .

[19]  Donald D. Blankenship,et al.  Antarctic Mapping Tools for Matlab , 2017, Comput. Geosci..

[20]  Bo Sun,et al.  A freeze-on ice zone along the Zhongshan–Kunlun ice sheet profile, East Antarctica, by a new ground-based ice-penetrating radar , 2015 .

[21]  D. Qin,et al.  Surface mass balance and its climate significance from the coast to Dome A, East Antarctica , 2015, Science China Earth Sciences.

[22]  Justin Taylor,et al.  Regional-scale bed roughness beneath ice masses: measurement and analysis , 2004, Comput. Geosci..

[23]  D. Vaughan,et al.  The internal layering of Pine Island Glacier, West Antarctica, from airborne radar-sounding data , 2009, Annals of Glaciology.

[24]  Bo Sun,et al.  Summit of the East Antarctic Ice Sheet underlain by thick ice-crystal fabric layers linked to glacial–interglacial environmental change , 2017, Special Publications.

[25]  M. Siegert,et al.  Ice‐flow structure and ice dynamic changes in the Weddell Sea sector of West Antarctica from radar‐imaged internal layering , 2015 .

[26]  F. Pattyn,et al.  Glaciological characteristics in the Dome Fuji region and new assessment for “Oldest Ice” , 2018, The Cryosphere.

[27]  Bo Sun,et al.  Ice thickness, internal layers, and surface and subglacial topography in the vicinity of Chinese Antarctic Taishan station in Princess Elizabeth Land, East Antarctica , 2016, Applied Geophysics.

[28]  D. Vaughan,et al.  A ‘continuity-index’ for assessing ice-sheet dynamics from radar-sounded internal layers , 2012 .

[29]  O. Eisen,et al.  Age stratigraphy in the East Antarctic Ice Sheet inferred from radio-echo sounding horizons , 2018, Earth System Science Data.

[30]  R. Alley,et al.  Basal conditions and ice dynamics inferred from radar-derived internal stratigraphy of the northeast Greenland ice stream , 2013, Annals of Glaciology.

[31]  Kotaro Fukui,et al.  Radar diagnosis of the subglacial conditions in Dronning Maud Land, East Antarctica , 2012 .

[32]  David Braaten,et al.  Widespread Persistent Thickening of the East Antarctic Ice Sheet by Freezing from the Base , 2011, Science.

[33]  M. Siegert,et al.  Radar‐derived bed roughness characterization of Institute and Möller ice streams, West Antarctica, and comparison with Siple Coast ice streams , 2007 .

[34]  Li Yuansheng,et al.  Spatial variability of surface mass balance along a traverse route from Zhongshan station to Dome A, Antarctica , 2011, Journal of Glaciology.

[35]  Christopher Williams,et al.  Self-affine subglacial roughness: consequences for radar scattering and basal water discrimination in northern Greenland , 2017 .

[36]  D. Blankenship,et al.  Organized flow from the South Pole to the Filchner‐Ronne ice shelf: An assessment of balance velocities in interior East Antarctica using radio echo sounding data , 2007 .

[37]  Antony J. Payne,et al.  Hydrological Connections between Antarctic Subglacial Lakes, the Flow of Water beneath the East Antarctic Ice Sheet and Implications for Sedimentary Processes , 2009 .

[38]  Bo Sun,et al.  Bedmap2: improved ice bed, surface and thickness datasets for Antarctica , 2012 .

[39]  Jason L. Roberts,et al.  Evidence of a hydrological connection between the ice divide and ice sheet margin in the Aurora Subglacial Basin, East Antarctica , 2012 .

[40]  Bo Sun,et al.  Characterization of subglacial landscapes by a two-parameter roughness index , 2010, Journal of Glaciology.

[41]  Kenji Kawamura,et al.  Where to find 1.5 million yr old ice for the IPICS "Oldest-Ice" ice core , 2013 .

[42]  D. Blankenship,et al.  Repeated large-scale retreat and advance of Totten Glacier indicated by inland bed erosion , 2016, Nature.

[43]  L. Sime,et al.  Isochronous information in a Greenland ice sheet radio echo sounding data set , 2014 .

[44]  S. Anandakrishnan,et al.  Power loss in dipping internal reflectors, imaged using ice-penetrating radar , 2014, Annals of Glaciology.

[45]  F. Ng,et al.  Fast-flow signature in the stagnated Kamb Ice Stream, West Antarctica , 2004 .

[46]  Bo Sun,et al.  Preliminary results of ice radar investigation along the traverse between Zhongshan and Dome A in East Antarctic ice sheet: Ice thickness and subglacial topography , 2010 .

[47]  Robert Bingham,et al.  Quantifying subglacial bed roughness in Antarctica: implications for ice-sheet dynamics and history , 2009 .

[48]  Uwe Nixdorf,et al.  Subglacial topography and internal structure of central and western Dronning Maud Land, Antarctica, determined from airborne radio echo sounding , 2001 .

[49]  M. E. Peters,et al.  New boundary conditions for the West Antarctic Ice Sheet: Subglacial topography of the Thwaites and Smith glacier catchments , 2006 .