Abstract
A numerical finite-difference global ocean tide model with variable grid spacing has been developed. Deep-sea areas are covered by a coarse grid (4-degree meshsize) that is refined in three steps to half-degree mesh-size in most of the shelf areas. The technique of combining coarse and fine grid cells has been generalized. Thus the model is not restricted to a specific arrangement of the numerical grid.
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Krohn, J. (1984). A Global Ocean Tide Model with High Resolution in Shelf Areas. In: Seeber, G., Apel, J.R. (eds) Geodetic Features of the Ocean Surface and their Implications. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-1673-4_18
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DOI: https://doi.org/10.1007/978-94-017-1673-4_18
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