New fast delivery 35 days repeat ERS‐1 altimeter data have been used to recover the gravity field in the Norwegian‐Greenland Sea. Furthermore the spectral characteristics of the gravity field have been investigated from 18 arcs of 3 days repeat period data. The recovered gravity field correlates exclusively with the major geological structures, which clearly demonstrates the potential of these new ERS‐1 altimeter data.
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Knudsen et al. (1992) studied this question.
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