A linear one-dimensional model is fitted to the semidiurnal and diurnal components of the surface tide in the Gulf of California. This simple model accounts for 99% of the total time variance in most components and 90% for the worst cases. Discussion suggests the need for introducing non-uniform parameterizations of linear friction. -English summary
CITATION STYLE
Ripa, P., & Velazquez, G. (1993). Modelo unidimensional de la marea en el Golfo de California. Geofisica Internacional, 32(1), 41–56. https://doi.org/10.22201/igeof.00167169p.1993.32.1.1151
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