A General Ocean Circulation Model Determined in a Simultaneous Solution with the Earth’s Gravity Field
作者： R. Steven Nerem , Byron D. Tapley , C. K. Shum
DOI: 10.1007/978-1-4684-7098-7_18
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摘要: Over the past several years, determination of sea surface topography using satellite altimetry has been greatly improved due to implementation a technique which simultaneously solves for topography, gravity field Earth, and orbit [Tapley et al.,1988; Marsh al., 1989; Nerem,1989; Engelis Knudsen; 1989]. The ζ, is defined as deviation ocean from geoid geostrophic component currents.
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