Titlebook: Carbon and Nutrient Fluxes in Continental Margins; A Global Synthesis Kon-Kee Liu,Larry Atkinson,Liana Talaue-McManus Book 2010 Springer-Ve

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Kon-Kee Liu,Larry Atkinson,Liana Talaue-McManusExcellent guide for researchers of all levels and for the study of graduate students.Includes supplementary material:

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Global Change - The IGBP Serieshttp://image.papertrans.cn/c/image/221646.jpg

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Biogeochemistry of Continental Margins in a Global Contextt attention given to continental margins focused on continental shelves, which constitute a major part of continental margins. In recent years, it has been increasingly appreciated that influences of the land–ocean boundary often extend beyond the shelf edge. Such new ideas have led to recognition o

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Eastern Boundary Current Systems2005), Mackas et al. (2006), Fréon et al. (2006), and Taylor and Wolff (2007), compare eastern boundary current systems (EBCS) from physical, productivity, trophic, or biogeochemical standpoints. Therefore, this section focuses mostly on some key research areas that have begun to emerge in the last

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Western Boundary Currents globally significant amounts of heat, nutrients, and carbon to higher latitudes. The movement of material and heat to higher latitudes has significant effects on the global climate but also significantly affects the ocean margin through which they pass.

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Subpolar Marginsns is marked in the west of the ocean basins by the separation point of the major western boundary currents, and in the east by the more diffuse re-attachment of the westwind drift to the continental margin. We also include the landmass of New Zealand, situated within the path of both the South Paci

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