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

使成波状

https://doi.org/10.1007/978-3-662-62174-5nual changes found whenever an appropriate investigation has sought such variability. The Gulf Stream path meanders with a broad spectrum of variability, particularly downstream of Cape Hatteras. These lateral translations range from interannual and seasonal shifts to the north or south, through sub

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Werner Baumann,Bettina Herberg-Liedtkee times that of the Atlantic. Yet both oceans are forced by roughly similar westerly winds in midlatitude, which separate the easterly trade winds to the south from the polar easterlies to the north. Both oceans respond in their wind-driven circulation by forming a set of basin-wide gyres with inten

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Permanent

,Praxis der behördlichen Genehmigung,al regions. Experimental sites were chosen in the tropics at latitudes higher than 10° (Koshlyakov and Monin 1978) or at mid-latitudes (MODE Group, 1978; Robinson 1980). There exist, however, some XBT (Expendable Bathythermograph) sections through the equatorial belts that were obtained for studying

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Internationale Atomgewichte 1968,nce of the monsoons and has a strongly variable seasonal circulation. As in most parts of the ocean, the only available overall view of eddy properties in this region is the one provided by Wyrtki, Magaard and Hager (1976). They calculated eddy kinetic energy per unit mass for each 5° square of the

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Carbon-Monoxide

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