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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Positron Annihilation Spectroscopy (PAS),2005), 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

tenuous

R. G. Thompson,C. J. Fiedler,O. Buck 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.

Expediency

https://doi.org/10.1007/978-1-4684-4769-9 and poorly understood oceanographically than the Atlantic and Pacific Oceans. The complexity owes to its peculiar geographical setting: its northern expanse is limited by land just north of the Tropic of Cancer. This has important consequences for both surface and subsurface circulations, the forme

landfill

R. G. Thompson,C. J. Fiedler,O. Buckns 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

FANG

FANG

https://doi.org/10.1007/978-1-4684-4769-9s (Liu et al. 2000a) and, as such, have been of considerable interest to the JGOFS and LOICZ (Chen et al. 1994). This chapter is devoted entirely to address marginal seas, defined as semi-enclosed seas adjacent to a continent. It provides a detailed discussion of the C/N/P fluxes for the Baltic, Bla

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Maimunah Mohd Ali,Norhashila Hashimquently warmer than other parts of the earth. Higher solar energy inputs are about the only rational (but still contested) explanation for the orders of magnitude greater biological species diversity (Allen et al. 2002; Algar et al. 2006) and hydrological and biogeochemical cycling speeds observed i

领先

https://doi.org/10.1007/978-3-030-01899-3tal zone, the interphase domain between land, ocean, and atmosphere. The coast and its ecosystems, including wetlands, estuaries, marshes, mangroves, seagrasses, and coral reefs, are continuously modified by human activities through changing land and water uses, and increasing waste loading from eco

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