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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Short Term Variations in Primary Productivitye for ocean chemistry and physics. The first concerns implications, for studies of mixing in the surface layer, of the fact that phytoplankton “remember” their past light history. Here time scales of minutes to hours are important. The second concerns primary production as the driving force for the

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Some Perspectives on Ecological Modeling Focused on Upper Ocean Processeserently intricate and are variable in time and space due to environmental dependencies. Modeling provides a mechanism by which complex biological-environmental interactions can be studied. This potential is evident in the progress exhibited in the construction of biological-physical subsystem models

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What Controls the Variability of Carbon Dioxide in the Surface Ocean? A Plea for Complete Informatio, are among the most important problems addressed by ocean chemists today..There is wide agreement as to experimental procedures in this field, through the measurement of alkalinity, total CO., pH and pCO. of ocean waters, together with physical properties and .C. Moreover the uncertainties surround

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Ragnar Holm,Friedrich Güldenpfennigo acids, thiols, low molecular weight carbonyl compounds, carboxylic acids, and metal-organic complexes. Emphasis is placed on how the methods work, their limitations, and examples of field applications.

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Upper Ocean Chemistry: Space and Time Scales to give comparable density of observation in the three dimensions x, z & t, (2) Relations between selected organic compounds which may have large coherence scales as a result of their specific biological functions, and (3) Integration of surface and deep water studies, particularly, but not solely, through the use of sediment trap methods.

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Organic Chemical Dynamics of the Mixed Layer: Measurement of Dissolved Hydrophilic Organics at Seao acids, thiols, low molecular weight carbonyl compounds, carboxylic acids, and metal-organic complexes. Emphasis is placed on how the methods work, their limitations, and examples of field applications.

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Report of Working Group I: Gasesre (e.g., CO, NO, N.O). In some instances (e.g., (CH.).S, CH.I) the fluxes from the ocean to the atmosphere make significant contributions to the global cycling of the elements, and in others (e.g., CO.) the flux into the ocean exerts an important control on atmospheric composition.