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Titlebook: Global Climate and Ecosystem Change; Gordon J. MacDonald,Luigi Sertorio Book 1990 Springer Science+Business Media New York 1990 Potential.

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發(fā)表于 2025-3-25 06:36:24 | 只看該作者
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發(fā)表于 2025-3-25 10:03:01 | 只看該作者
The Impact of Global Climate Change on Marine Ecosystemsal climate will therefore affect not only the circulation patterns of the oceans, but also, by extension, the role of the oceans as a reservoir for heat and atmospheric gases. Elements such as carbon take approximately 100 years to be exchanged between the surface waters and deeper layers of the oce
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發(fā)表于 2025-3-25 14:56:55 | 只看該作者
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發(fā)表于 2025-3-25 17:30:10 | 只看該作者
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發(fā)表于 2025-3-25 22:43:57 | 只看該作者
Predictability and Dimensionality of a Simplified Atmospheric Modelcertain range is lost. Chaotic behavior can be found in systems with only a few total or relevant dynamical variables. It has recently been suggested, however, that a few variables may be sufficient to model the dynamics of the atmosphere. This hypothesis is supported only by studies aimed at estima
26#
發(fā)表于 2025-3-26 00:24:02 | 只看該作者
Xiaoguang Cheng,Yongbin Su,Mingqian Huangoceans produced oxygen in the atmosphere, which led to the development of the protective ozone layer in the stratosphere and the eventual dominance by aerobic organisms near the earth’s surface. The development and evolution of life were accompanied by profound changes in atmospheric composition and corresponding changes in surface climate.
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發(fā)表于 2025-3-26 05:21:32 | 只看該作者
28#
發(fā)表于 2025-3-26 08:28:57 | 只看該作者
Book 1990es to the atmosphere, oceans, and land produce changes in the living parts of the planet, while, at the same time, alterations in the biosphere modify the atmosphere, oceans, and land. Understanding this complex web of interactions poses unprecedented intellectual challenges. The atmospheric concent
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發(fā)表于 2025-3-26 16:06:09 | 只看該作者
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發(fā)表于 2025-3-26 20:12:22 | 只看該作者
Predictability and Dimensionality of a Simplified Atmospheric Model however, that a few variables may be sufficient to model the dynamics of the atmosphere. This hypothesis is supported only by studies aimed at estimating the dimensionality of the climate system through analysis of observational data (Fraedrich, 1986; Keppenne and Nicolis, 1989).
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