Satellite altimetry, the marine geoid, and the oceanic general circulation

  • Wunsch C
  • Stammer D
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▪ Abstract For technical reasons, the general circulation of the ocean has historically been treated as a steady, laminar flow field. The recent availability of extremely high-accuracy and high-precision satellite altimetry has provided a graphic demonstration that the ocean is ...

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  • C Wunsch

  • D Stammer

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