NASA NTRS · 19790013335
The inverse problem: Ocean tides derived from earth tide observations
Abstract
Indirect mapping ocean tides by means of land and island-based tidal gravity measurements is presented. The inverse scheme of linear programming is used for indirect mapping of ocean tides. Open ocean tides were measured by the numerical integration of Laplace's tidal equations.
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Kuo, J. T.. 1978-01-01. The inverse problem: Ocean tides derived from earth tide observations. https://ntrs.nasa.gov/citations/19790013335
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