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Modeling the deformation regime of Thwaites Glacier, West Antarctica, using a simple flow relation for ice anisotropy (ESTAR) Journal of Geophysical Research: Earth Surface, 2022 (Ref: 16468)
Authors:
McCormack F.S.Warner R.C.Seroussi H.Dow C.F.Roberts J.L.Treverrow A.
Category 1: Peer-reviewed literature

Comparing Present and Paleo Ice Flow in the Amundsen Sea, West Antarctica First Antarctic Climate Evolution Symposium, Granada, Spain, 7-11 September 2009, 2009 (Ref: 13923)
Authors:
Nitsche F.O.Warner R.C.Roberts J.L.
Category 3: Poster

Reconstructing and modeling extent and dynamics of ice sheets is crucial in … understanding and predicting the evolution of ice sheets. Key to ice sheet dynamics are ice … streams, which drain most of the ice from the ice sheet interior to the ice shelves, where most of … the ice is lost.

Growth rate of crystals within the surface-snow/firn layer in Wilkes Land, East Antarctica. Annals of Glaciology, 1988 (Ref: 2360)
Authors:
Qin D.H.Young N.W.Thwaites R.J.
Category 1: Peer-reviewed literature

Measurements of crystal size have been made on seven firn cores drilled at sites covering a range of mean annual temperature from -12.6 °C to -52.5 °C and a range of accumulation rate from 52 to 315 kg/sq.m/a. The sorting coefficient…

Temperature regime and thermal properties at the active layer of Law Dome, Antarctica. A Collection of Antarctic Scientific Explorations: Studies on Glaciology, 1988 (Ref: 2499)
Authors:
Qin D.H..Young N.W.Thwaites R.J.Han J.K.
Category 3: Article

The temperature of upper 20 m was measured at four sites, S1, LJ, LJ24 and BJ, during a period of 21 months at the western Law Dome, Antarctica. the sensors were emplaced at the depths of 1, 2.5, 5, 7.5, 10, 15 and 20 m. S1 is in ablation sphere with a dynamo-metamorphosed ice…

Growth rate of shallow snow/firn crystals in Wilkes Land, Antarctica. A Collection of Antarctic Scientific Explorations: Studies on Glaciology, 1988 (Ref: 2500)
Authors:
Qin D.H.Young N.W.Thwaites R.J.
Category 3: Article

Measured velocities and ice flow in Wilkes Land, Antarctica. Annals of Glaciology, 1989 (Ref: 2414)
Authors:
Young N.W.Goodwin I.D.Hazelton N.W.J.Thwaites R.J.
Category 1: Peer-reviewed literature

Ice velocity, surface elevation, and ice thickness were measured along oversnow traverse routes in the sector of Wilkes Land, East Antarctica, bounded by long. 93°E and 131°E, and the coast and lat. 75°S.

Ice characteristics and structure in the Antarctic seasonal sea ice zone (Abstract). Conference on air-sea interaction and its consequences, Sydney, February 1996. Abstract volume, 1986 (Ref: 2235)
Authors:
Allison I.Jacka T.H.Thwaites R.Wilson J.C.
Category 3: Conference paper

An ice-core drilling site at Law Dome summit, Wilkes Land, Antarctica. ANARE Research Notes, 1986 (Ref: 1824)
Authors:
Hamley T.C.Morgan V.I.Thwaites R.J.Gao X.Q.
Category 3: Article

Characteristics of the seasonal sea ice of East Antarctica and comparisons with satellite observations. Annals of Glaciology, 1987 (Ref: 2081)
Authors:
Jacka T.H.Allison I.Thwaites R.Wilson J.C.
Category 1: Peer-reviewed literature

An Antarctic field study of the rheology and movement of a sea-ice floe aggregate. Annals of Glaciology, 1991 (Ref: 6763)
Authors:
Jacka T.H.Thwaites R.Wilson J.C.
Category 1: Peer-reviewed literature

Does Gribb Bank exist? Polar Record, 1984 (Ref: 1740)
Authors:
Quilty P.G.Thwaites R.J.Burbury R.M.Stagg H.M.Krummel R.W.
Category 3: Article

Relationship between bore-hole closure and crystal fabrics in Antarctic ice core from Cape Folger. Journal of Glaciology, 1984 (Ref: 1700)
Authors:
Thwaites R.J.Wilson C.L.J.McCray A.P.
Category 1: Peer-reviewed literature

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