We present a geoid solution for the Weddell Sea and adjacent continental Antarctic regions. There, a refined geoid is of interest, especially for oceanographic and glaciological applications. For example, to investigate the Weddell Gyre as a part of the Antarctic Circumpolar Current and, thus, of the global ocean circulation, the mean dynamic topography (MDT) is needed. These days, the marine gravity field can be inferred with high and homogeneous resolution from altimetric height profiles of the mean sea surface.
Schwabe, J., Scheinert, M. Regional geoid of the Weddell Sea, Antarctica, from heterogeneous ground-based gravity data,
Springer Berlin Heidelberg, 2014, с.821-838.
Schwabe, J., Scheinert, M. .
Regional geoid of the Weddell Sea, Antarctica, from heterogeneous ground-based gravity data.
: Springer Berlin Heidelberg, 2014, с.821-838.
Schwabe, J., Scheinert, M. (2014)
Regional geoid of the Weddell Sea, Antarctica, from heterogeneous ground-based gravity data,
: Springer Berlin Heidelberg, с.821-838
Schwabe, J., & Scheinert, M.
(2014).
Regional geoid of the Weddell Sea, Antarctica, from heterogeneous ground-based gravity data. Journal of Geodesy. Springer Berlin Heidelberg 88 (9), с.821-838.
