Evaluation of the geoid based on the SEASAT altimetry data at sea around Antarctica

The SEASAT radar altimetry data, which were obtained during its operational period from June to September 1978,have been processed, and the sea surface topography and/or the geoid in the area between 45°S and the margin of the Antarctic Continent have been contour-mapped. Mainly because of the uncer...

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Bibliographic Details
Main Author: Jiro Segawa
Format: Article in Journal/Newspaper
Language:English
Published: National Institute of Polar Research 1982
Subjects:
geo
envir
Antarctic
East Antarctica
Indian
Ross Sea
The Antarctic
Weddell
Weddell Sea
Antarc*
Antarctica
Online Access:https://doi.org/10.15094/00008320
https://doaj.org/article/fb4b4d8a64b4497eba8afd5ba5adc415
Description
Summary:The SEASAT radar altimetry data, which were obtained during its operational period from June to September 1978,have been processed, and the sea surface topography and/or the geoid in the area between 45°S and the margin of the Antarctic Continent have been contour-mapped. Mainly because of the uncertainty involved in the satellite altitude the sea surface topography includes maximum errors of ±5m. However, some significant features such as geoid depressions at the Ross Sea and the Weddell Sea or the regional geoid upheavals over the Indian Ocean off East Antarctica have been clearly displayed.

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