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Volume 2, issue 2
Earth Syst. Sci. Data, 2, 261-273, 2010
https://doi.org/10.5194/essd-2-261-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.
Earth Syst. Sci. Data, 2, 261-273, 2010
https://doi.org/10.5194/essd-2-261-2010
© Author(s) 2010. This work is distributed under
the Creative Commons Attribution 3.0 License.

  22 Dec 2010

22 Dec 2010

A consistent data set of Antarctic ice sheet topography, cavity geometry, and global bathymetry

R. Timmermann1, A. Le Brocq2, T. Deen3, E. Domack4, P. Dutrieux3, B. Galton-Fenzi5, H. Hellmer1, A. Humbert6, D. Jansen7, A. Jenkins3, A. Lambrecht8, K. Makinson3, F. Niederjasper1, F. Nitsche9, O. A. Nøst10, L. H. Smedsrud11, and W. H. F. Smith12 R. Timmermann et al.
  • 1Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany
  • 2University of Exeter, Exter, UK
  • 3British Antarctic Survey, Cambridge, UK
  • 4Hamilton College, Clinton, NY, USA
  • 5University of Tasmania, Hobart, Tasmania
  • 6KlimaCampus, University of Hamburg, Hamburg, Germany
  • 7Swansea University, Swansea, UK
  • 8University Innsbruck, Innsbruck, Austria
  • 9Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY, USA
  • 10Norwegian Polar Institute, Tromsø, Norway
  • 11Bjerknes Centre for Climate Research, Bergen, Norway
  • 12Laboratory for Satellite Altimetry, NOAA NESDIS, Silver Spring, MD, USA

Abstract. Sub-ice shelf circulation and freezing/melting rates in ocean general circulation models depend critically on an accurate and consistent representation of cavity geometry. Existing global or pan-Antarctic topography data sets have turned out to contain various inconsistencies and inaccuracies. The goal of this work is to compile independent regional surveys and maps into a global data set. We use the S-2004 global 1-min bathymetry as the backbone and add an improved version of the BEDMAP topography (ALBMAP bedrock topography) for an area that roughly coincides with the Antarctic continental shelf. The position of the merging line is individually chosen in different sectors in order to capture the best of both data sets. High-resolution gridded data for ice shelf topography and cavity geometry of the Amery, Fimbul, Filchner-Ronne, Larsen C and George VI Ice Shelves, and for Pine Island Glacier are carefully merged into the ambient ice and ocean topographies. Multibeam survey data for bathymetry in the former Larsen B cavity and the southeastern Bellingshausen Sea have been obtained from the data centers of Alfred Wegener Institute (AWI), British Antarctic Survey (BAS) and Lamont-Doherty Earth Observatory (LDEO), gridded, and blended into the existing bathymetry map. The resulting global 1-min Refined Topography data set (RTopo-1) contains self-consistent maps for upper and lower ice surface heights, bedrock topography, and surface type (open ocean, grounded ice, floating ice, bare land surface). The data set is available in NetCDF format from the PANGAEA database at doi:10.1594/pangaea.741917.

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