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Titlebook: Eddies in Marine Science; Allan R. Robinson (Gordon McKay Professor of Geoph Conference proceedings 1983 Springer-Verlag, Berlin Heidelber

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https://doi.org/10.1007/978-3-642-49796-4in terms of the areas where they are found. While the presentation is not intended to be exhaustive, it will be seen that enough is known to show that quasi-geostrophic motions play a variety of major roles in the dynamics of the northern oceans.
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https://doi.org/10.1007/978-3-662-06237-1to the “mid-ocean” area (south of 20°S and between 50° and 100°E) so that the atlas compiled of the IIOE data (Wyrtki 1971) reveals a much lower station density in the central part of the Indian Ocean than elsewhere.
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Vierstellige Mantissen der Logarithmen,s. The acute non-uniformity in the coverage of data, with adequate resolution, will often be mentioned and will be frequently invoked in qualifying any of the conclusions drawn. Most discussions will be concerned with the Northern and Equatorial Atlantic and Pacific Oceans.
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