[1] 崔祥斌, 孙波, 田钢, 等. 冰雷达探测研究南极冰盖的进展与展望[J]. 地球科学进展, 2009, 24(4): 392-402.[2] Drewry D J, Jordan S R, Jankowski E. Measured properties of the Antarctic ice sheet: surface configuration, ice thickness, volume and bedrock characteristics[J]. Annals of Glaciology, 1983, 3: 83-91.[3] Scott Polar Research Institute, Drewry D J. Antarctica: Glaciological and Geophysical Folio[M]. University of Cambridge, Scott Polar Research Institute, 1982.[4] Lythe M B, Vaughan D G. BEDMAP: A new ice thickness and subglacial topographic model of Antarctica[J]. Journal of Geophysical Research: Solid Earth (1978–2012), 2001, 106(B6): 11335-11351.[5] Fretwell P, Pritchard H D, Vaughan D G, et al. Bedmap2: improved ice bed, surface and thickness datasets for Antarctica[J]. The Cryosphere Discussions, 2012, 6: 4305-4361.[6] Hansen S E, Nyblade A A, Heeszel D S, et al. Crustal structure of the Gamburtsev Mountains, East Antarctica, from S-wave receiver functions and Rayleigh wave phase velocities[J]. Earth and Planetary Science Letters, 2010, 300(3): 395-401.[7] Blankenship D D, Young D A, Siegert M J, et al. New constraints on the structure and dynamics of the East Antarctic Ice Sheet from the joint IPY/Ice Bridge ICECAP aerogeophysical project[C]//AGU Fall Meeting Abstracts. 2010, 1: 05.[8] Schodlok M P, Menemenlis D, Rignot E, et al. Sensitivity of the ice-shelf/ocean system to the sub-ice-shelf cavity shape measured by NASA IceBridge in Pine Island Glacier, West Antarctica[J]. Annals of Glaciology, 2012, 53(60): 156-162.[9] Welch B C, Jacobel R W. Analysis of deep‐penetrating radar surveys of West Antarctica, US‐ITASE 2001[J]. Geophysical research letters, 2003, 30(8).[10] 孙波, 崔祥斌. 2007/2008 年度中国南极冰穹 A 考察新进展[J]. 极地研究, 2008, 20(4): 371-378.[11] Rippin D M, Bamber J L, Siegert M J, et al. The role of ice thickness and bed properties on the dynamics of the enhanced-flow tributaries of Bailey Ice Stream and Slessor Glacier, East Antarctica[J]. Annals of Glaciology, 2004, 39(1): 366-372.[12] Holt J W, Blankenship D D, Morse D L, et al. New boundary conditions for the West Antarctic Ice Sheet: Subglacial topography of the Thwaites and Smith glacier catchments[J]. Geophysical Research Letters, 2006, 33(9).[13] Vaughan D G, Corr H F J, Ferraccioli F, et al. New boundary conditions for the West Antarctic ice sheet: Subglacial topography beneath Pine Island Glacier[J]. Geophysical Research Letters, 2006, 33(9).[14] Ferraccioli F, Jones P C, Curtis M L, et al. Subglacial imprints of early Gondwana break‐up as identified from high resolution aerogeophysical data over western Dronning Maud Land, East Antarctica[J]. Terra Nova, 2005, 17(6): 573-579.[15] Schutz B E, Zwally H J, Shuman C A, et al. Overview of the ICESat mission[J]. Geophysical Research Letters, 2005, 32(21): L21S01.[16] Drinkwater M R, Haagmans R, Muzi D, et al. The GOCE gravity mission: ESA’s first core Earth explorer[C]//Proceedings of the 3rd international GOCE user workshop. 2006: 6-8.[17] Whittaker J M, Goncharov A, Williams S E, et al. Crustal velocity and sediment thickness asymmetries along and between the conjugate Australian-Antarctic margins[J]. Mares, T.(Ed), 2012.[18] Bamber J L, Gomez-Dans J L, Griggs J A. A new 1 km digital elevation model of the Antarctic derived from combined satellite radar and laser data–Part 1: Data and methods[J]. Cryosphere, 2009, 3(1): 101-111.[19] Liu H, Jezek K C, Li B. Development of an Antarctic digital elevation model by integrating cartographic and remotely sensed data: A geographic information system based approach[J]. Journal of Geophysical Research: Solid Earth (1978–2012), 1999, 104(B10): 23199-23213.[20] Timmermann R, Le Brocq A, Deen T, et al. A consistent data set of Antarctic ice sheet topography, cavity geometry, and global bathymetry[J]. Earth System Science Data, 2010, 2(2): 261-273.[21] Tapley B D, Bettadpur S, Watkins M, et al. The gravity recovery and climate experiment: Mission overview and early results[J]. Geophysical Research Letters, 2004, 31(9).[22] Bentley C R. The structure of Antarctica and its ice cover[C]//Research in Geophysics, Volume 2: Solid Earth and Interface Phenomena. 1964, 2: 335.[23] Griggs J A, Bamber J L. Antarctic ice-shelf thickness from satellite radar altimetry[J]. Journal of Glaciology, 2011, 57(203): 485-498.[24] Clarke G K C, Berthier E, Schoof C G, et al. Neural networks applied to estimating subglacial topography and glacier volume[J]. Journal of Climate, 2009, 22(8): 2146-2160.[25] Hutchinson M F. Calculation of hydrologically sound digital elevation models[C]//Proceedings of the Third International Symposium on Spatial Data Handling. Sydney, 1988, 133.[26] DiMarzio J, Brenner A, Schutz R, et al. GLAS/ICESat 500 m laser altimetry digital elevation model of Antarctica[J]. National Snow and Ice Data Center (NSIDC), 2007.[27] Rippin D M, Bamber J L, Siegert M J, et al. Basal topography and ice flow in the Bailey/Slessor region of East Antarctica[J]. Journal of Geophysical Research: Earth Surface (2003–2012), 2003, 108(F1).[28] 崔祥斌, 孙波, 田钢, 等. 东南极 Dome A 冰雷达探测: 冰厚分布和冰下地形[J]. 科学通报, 2010, 3: 010.[29] Siegert M J. Antarctic subglacial topography and ice‐sheet evolution[J]. Earth Surface Processes and Landforms, 2008, 33(4): 646-660.[30] Bo S, Siegert M J, Mudd S M, et al. The Gamburtsev mountains and the origin and early evolution of the Antarctic Ice Sheet[J]. Nature, 2009, 459(7247): 690-693.[31] Taylor J, Siegert M J, Payne A J, et al. Regional-scale bed roughness beneath ice masses: Measurement and analysis[J]. Computers & geosciences, 2004, 30(8): 899-908.[32] Siegert M J, Taylor J, Payne A J. Spectral roughness of subglacial topography and implications for former ice-sheet dynamics in East Antarctica[J]. Global and Planetary Change, 2005, 45(1): 249-263.[33] 崔祥斌, 孙波, 张向培, 等. 极地冰盖冰雷达探测技术的发展综述[J]. 极地研究, 2009, 21(4):322-335.[34] Hélière F, Lin C C, Corr H, et al. Radio echo sounding of Pine Island Glacier, West Antarctica: Aperture synthesis processing and analysis of feasibility from space[J]. Geoscience and Remote Sensing, IEEE Transactions on, 2007, 45(8): 2573-2582. |