Remote Sensing of the Mass Input, Glacier Dynamics and Surface Characteristics of the Antarctic Icesheet

Related publications

• Surface wind field over the Antarctic ice sheet mapped from satellite thermal infrared images. Abstracts of the SCAR Open Science Conference, Hobart, 12-14 July 2006., 2006 (Ref: 12500)
  Authors:

  Young N.W.Anderson J.G.
  Category 3: Poster

  Thermal infrared images of the cloud-free surface of the Antarctic ice sheet exhibit subtle … stream-like features that can be traced over hundreds of kilometres. The stream features are … superimposed on other features in the temperature field related to the surface topography of … the ice sheet.

• Snow accumulation variability in Wilkes Land, East Antarctica, and the relationship to atmospheric ridging in the 130-170 E region since 1930. Journal of Geophysical Research,, 2003 (Ref: 11565)
  Authors:

  Goodwin I.de Angelis M.Pook M.Young N.W.
  Category 1: Peer-reviewed literature
• Comparison of microwave backscatter measurements with observed roughness of the snow surface in East Queen Maud Land, Antarctica. Proceedings of the 3rd ERS scientific symposium, Florence, 17-21 March., 1997 (Ref: 8549)
  Authors:

  Furukawa T.Young N.W.
  Category 3: Conference paper

  A directional anisotropy is observed in backscatter from the surface of the East Antarctic ice sheet as measured by the C-band wind scatterometer carried by the ERS-1 satellite. The anisotropy is characterised by the amplitude of the variation with azimuth of the backscatter coefficient…

• Applications of time series of microwave backscatter over the Antarctic region. Proceedings of the 3rd ERS scientific symposium, Florence, 17-21 March, 1997., 1997 (Ref: 8553)
  Authors:

  Young N.W.Hyland G.
  Category 3: Conference paper

  The 500 km wide swath of the ERS Wind scatterometer and its orbit geometry allows the measurement of the microwave backscatter of all the Antarctic region between latitudes 55°S and 79°S every three days.

• Directional anisotropy of C-band backscatter and orientation of surface microrelief in East Antarctica. Proceedings of 1st Australian ERS-1 Symposium, University of Tasmania, Hobart, 6 February 1996, 1996 (Ref: 6923)
  Authors:

  Young N.W.Hall D.Hyland G.
  Category 3: Conference paper

  There is a distinct directional anisotropy in microwave backscatter from the surface of the East Antarctic ice sheet as measured by the C-band wind scatterometer carried by the ERS-1 satellite.