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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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樓主: 哪能仁慈
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發(fā)表于 2025-3-23 13:01:12 | 只看該作者
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發(fā)表于 2025-3-23 14:33:32 | 只看該作者
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發(fā)表于 2025-3-23 19:17:41 | 只看該作者
https://doi.org/10.1007/978-3-662-00474-6The oceanic region considered in this chapter is the subtropical South Pacific, bounded by latitudes 23°S and 45°S and by longitudes 150°E and 290°E. It borders the tropical South Pacific and the Southern Ocean, which are considered in Chapters 10 and 14 respectively.
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發(fā)表于 2025-3-24 01:51:27 | 只看該作者
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發(fā)表于 2025-3-24 06:06:52 | 只看該作者
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發(fā)表于 2025-3-24 09:46:46 | 只看該作者
The South Pacific Including the East Australian CurrentThe oceanic region considered in this chapter is the subtropical South Pacific, bounded by latitudes 23°S and 45°S and by longitudes 150°E and 290°E. It borders the tropical South Pacific and the Southern Ocean, which are considered in Chapters 10 and 14 respectively.
17#
發(fā)表于 2025-3-24 10:50:29 | 只看該作者
18#
發(fā)表于 2025-3-24 16:22:45 | 只看該作者
Modelle und Modellvorstellungen,haps the major characteristic, of mesoscale variability in this ocean basin is its very strong qualitative dependence upon proximity to the Gulf Stream system (see Schmitz 1978). The focus of this chapter is upon studies made during the POLYMODE program of the character of mesoscale variability at g
19#
發(fā)表于 2025-3-24 20:11:19 | 只看該作者
Chemiefasern nach dem Viskoseverfahrenar floats. These instruments, like their progenitor the Swallow float, are in essence tagged water parcels which allow us to obtain an explicit description of fluid motion over a wide range of space and time scales. On time scales of months to years the wandering of floats from one region to another
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發(fā)表于 2025-3-25 02:10:05 | 只看該作者
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