Corroborate 发表于 2025-3-23 10:07:53

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信任 发表于 2025-3-23 14:49:50

Book 1987gly never changing. Each wave that progresses through the. imme­ diate surf zone on every coast is strikingly different, yet the waves come again and again, as if never to end. The seasons come with essential reg­ ularity, and· yet each is individual-whatever did happen to that year of the normal ra

amygdala 发表于 2025-3-23 20:00:44

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BRIDE 发表于 2025-3-24 01:53:52

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sultry 发表于 2025-3-24 04:07:28

1431-9314 and seemingly never changing. Each wave that progresses through the. imme­ diate surf zone on every coast is strikingly different, yet the waves come again and again, as if never to end. The seasons come with essential reg­ ularity, and· yet each is individual-whatever did happen to that year of the

FER 发表于 2025-3-24 06:35:54

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Constitution 发表于 2025-3-24 10:59:38

Inverse Methods for Ocean Circulation,e mean velocity directly is therefore not feasible, oceanographers have had to turn to indirect methods based on property distributions that are apparently steady or that change only slowly with time.

deforestation 发表于 2025-3-24 17:45:10

Coastal Sedimentary Environments major simplification: vortex tilting and twisting cannot effectively produce vertical vorticity. Hence the privileged position of vertical vorticity in the theory of rapidly rotating fluids. Section 2 develops the two layer model and potential vorticity dynamics. Tractable models are obtained by si

首创精神 发表于 2025-3-24 22:56:09

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murmur 发表于 2025-3-25 01:25:31

1431-9314 with long time scales; namely, those varying on annual or at least seasonal cycles. Planning for all the named enterprises depended, as they still do, of course978-1-4612-9093-3978-1-4612-4636-7Series ISSN 1431-9314
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查看完整版本: Titlebook: General Circulation of the Ocean; Henry D. I. Abarbanel,W. R. Young Book 1987 Springer-Verlag New York Inc. 1987 Atlantic Ocean.Coast.Diss