Azuma, N. and Goto-Azuma, K.
1996. An anisotropic flow law for ice-sheet ice and its implications. Ann. Glaciol., 23, 202–208.
Budd, W.F. and Jacka, T.H.
1989. A review of ice rheology for ice sheet modelling. Cold Reg. Sci. Technol., 16(2), 107–144.
1985. Determination of the flow properties at Dye 3, south Greenland, by bore-hole-tilting measurements and perturbation modelling. J. Glaciol., 31(10 8), 92–98.
Dansgaard, W. and Johnsen, S. J.
1969. A flow model and a time scale for the ice core from Camp Century, Greenland. J. Glaciol., 8(53), 215–223.
D. M., Etheridge
1989. Dynamics of the Law Dome ice cap, Antarctica, as found from bore-hole measurements. Ann. Glaciol., 12, 46–50.
Fujita, S. and Mae, S.
1994. Causes and nature of ice-sheet radio-echo internal reflections estimated from the dielectric properties of ice. Ann. Glaciol., 20, 80–86.
Fujita, S. and 6 others. 1999. Nature of radio-echo layering in the Antarctic ice sheet detected by a two-frequency experiment. J. Geophys. Res., 104(B6), 13, 013–13, 024.
Gagliardini, O. and Meyssonnier, J.
2000. Simulation of anisotropic ice flow and fabric evolution along the GRIP–GISP2 flowline, central Greenland. Ann. Glaciol., 30, 217–223.
1955. The creep of polycrystalline ice. Proc. R. Soc. London, Ser. A, 228(1175), 519–538.
1958. The flow law of ice: a discussion of the assumptions made in glacier theory, their experimental foundation and consequences. International Association of Scientific Hydrology Publication
47 (Symposium at Chamonix 1958—Physics of the Movement of the Ice), 171–183.
Gow, A. J. and Williamson, T.
1976. Rheological implications of the internal structure and crystal fabrics of the West Antarctic ice sheet as revealed by deep core drilling at Byrd Station. Geol. Soc. Am. Bull., 87(12), 1665–1677.
Gundestrup, N. S., Dahl-Jensen, D., Hansen, B. L. and Kelty, J.
1993. Borehole survey at Camp Century. 1989. Cold Reg. Sci. Technol., 21(2), 187–193.
Hamilton, G. S., Whillans, I.M. and Morgan, P. J.
1998. First point measurements of ice-sheet thickness change in Antarctica. Ann. Glaciol., 27, 125–129.
Harrison, C. H.
1973. Radio echo sounding of horizontal layers in ice. J. Glaciol., 12(66), 383–397.
Herron, S.L. and Langway, C. C. Jr., 1982. A comparison of ice fabrics and textures at Camp Century, Greenland and Byrd Station, Antarctica. Ann. Glaciol., 3, 118–124.
Hulbe, C. L., Joughin, I. R., Morse, D. L. and Bindschadler, R. A.
2000. Tributaries to West Antarctic ice streams: characteristics deduced from numerical modelling of ice flow. Ann. Glaciol., 31, 184–190.
Hulbe, C. L., Wang, W., Joughin, I. R. and Siegert, M. J.
2003. The role of lateral and vertical shear in tributary flow toward a West Antarctic ice stream. Ann. Glaciol., 36, 244–250.
Joughin, I. and 7 others. 1999. Tributaries of West Antarctic ice streams revealed by RADARSAT interferometry. Science, 286(5438), 283–286.
Li Jun, T. H. Jacka and Budd, W.F.
1996. Deformation rates in combined compression and shear for ice which is initially isotropic and after the development of strong anisotropy. Ann. Glaciol., 23, 247–252.
1978. The effect of anisotropy on the creep of polycrystalline ice. J. Glaciol., 21(85), 475–483.
Lliboutry, L. and Duval, P.
1985. Various isotropic and anisotropic ices found in glaciers and polar ice caps and their corresponding rheologies. Ann. Geophysicae, 3(2), 207–224.
Nereson, N. A.
1998. The flow history of Siple Dome and Ice Streams C and D, West Antarctica: inferences from geophysical measurements and ice flow models. (Ph.D. thesis, University of Washington.)
Price, S. F., Bindschadler, R. A., Hulbe, C. L. and Blankenship, D. D.
2002. Force balance along an inland tributary and onset to Ice Stream D, West Antarctica. J. Glaciol., 48(160), 20–30.
Robin, G. de Q.1983. Profile data, inland Antarctica. In Robin, G. deQ., ed. The climatic record in polar ice sheets. Cambridge, Cambridge University Press, 112–118.
1978. Radio echo sounding studies of Marie Byrd Land, Antarctica. (Ph.D. thesis, University of Cambridge.)
Rose, K. E.
1979. Characteristics of ice flow in Marie Byrd Land, Antarctica. J. Glaciol., 24(90), 63–75.
Russell-Head, D. S. and Budd, W. F.
1979. Ice-sheet flow properties derived from bore-hole shear measurements combined with ice-core studies. J. Glaciol., 24(90), 117–130.
Siegert, M. J., Payne, A. J. and Joughin, I.
2003. Spatial stability of Ice Stream D and its tributaries, West Antarctica, revealed by radio-echo sounding and interferometry. Ann. Glaciol., 37 (see paper in this volume).
Steig, E. J. and 6 others. 2001. West Antarctic ice sheet elevation changes. In Alley, R. B. and Bindschadler, R. A., eds. The West Antarctic ice sheet: behavior and environment. Washington, DC, American Geophysical Union, 75–90.(Antarctic Research Series 77.)
Ueda, H.T. and Garfield, D. E.
1970. Deep core drilling at Byrd Station, Antarctica. International Association of Scientific Hydrology Publication
86 (Symposium at Hanover 1968—Antarctic Glaciological Exploration (ISAGE)), 56–62.
Wang, W. L.
2000. Incorporation of rheological properties into ice sheet flow models. (Ph.D . thesis, University of Tasmania.)
Wang, W. L. and Warner, R. C.
1999. Modeling of anisotropic ice flow in Law Dome, East Antarctica. Ann. Glaciol., 29, 184–190.
Wang, W., Warner, R. C. and Budd, W. F.
2002a. Ice-flow properties at Dome Summit South, Law Dome, East Antarctica. Ann. Glaciol., 35, 567–573.
Wang, W. L., Zwally, H. J., Abdalati, W. and Luo, S.
2002b. Modeling of ice flow and internal layers along a flowline through Swiss Camp, West Greenland. Ann. Glaciol., 34, 303–308.
1976. Radio-echo layers and the recent stability of the West Antarctic ice sheet. Nature, 264(5582), 152–155.
Whillans, I. M.
1977. The equation of continuity and its application to the ice sheet near “Byrd” Station, Antarctica. J. Glaciol., 18(80), 359–371.
Whillans, I. M.
1979. Ice flow along the Byrd Station strain network, Antarctica. J. Glaciol., 24(90), 15–28.
Zwally, H. J. and 15 others. 2002. IceSat’s laser measurements of polar ice, atmosphere, ocean and land. J. Geodynamics, 34(3–4), 405–445.