Titlebook: Dynamic Processes in the Chemistry of the Upper Ocean; J. D. Burton,P. G. Brewer,R. Chesselet Book 1986 Springer Science+Business Media Ne

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Upper Ocean Chemistry: Space and Time Scalesep ocean. The complexity and variability of the upper layers of the ocean at a wide range of space and time scales has been demonstrated by the dense sampling techniques available for temperature, salinity and chlorophyll. It is highly probable that for many chemical constituents there will be simil

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The Chemistry of Near-Surface Seawaters almost impossible to define in a meaningful way, and microlayer thicknesses are by default specified in terms of what the various sampling devices appear to collect. The organic composition of the microlayer is poorly characterized and its study suffers from similar problems to analogous work in b

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Processes Affecting Upper Ocean Chemical Structure in an Eastern Boundary Currentthe Californian coast have been examined from the process-oriented perspective of space and time scale analysis. In this region of the ocean, upwelling, offshore mesoscale eddies and large-scale “El Niño”-type processes dominate. Each of these physical processes has a velocity field which transports

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Convection in the Upper Oceanan occur just below the sea surface whenever there is a transfer of heat from the ocean to the atmosphere. The horizontal scale of this convection will typically be a few centimetres. Usually this convection will be intermittent with a characteristic period of the order of a minute. The small scale

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