Ice thickness and subglacial topography are critical factors for ice-sheet models to determine the timescale and location of a deep ice core .

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Therefore the accuracy of the new three-dimensional subglacial topography of Dome A is the best which will play an important role in the regional ice sheet model simulation the understanding of ice flow dynamics and the evolution of the ice sheet .

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The mission of this International Polar Year ( IPY ) project is to uncover secrets of the enigmatic Gamburtsev subglacial mountains that are buried by up to4 km of ice ;

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The formation of subglacial lakes results mainly from geothermal flux and partially from heat produced from basal sliding and internal ice deformation which raise the temperature of the basal ice to melting point and gradually melt the ice .

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Generally the influence of subglacial topography to ice surface is not significant in addition to the location of 900 km where ice surface uplifts evidently caused by rising of subglacial topography .

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Seasonal Evolution of Englacial and Subglacial Drainage System of Temperate Glacier Revealed by Hydrological Analysis

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US Chinese and Japanese teams will study the deeper structure under the Gamburtsev subglacial mountains using seismology .

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The feature extraction of subglacial topography with sub-km resolution scale mainly concentrates in two areas .

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The Gamburtsev subglacial mountains are thought to be the birthplace of the vast East Antarctic Ice Sheet .

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