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

employor

Ferdinand Trendelenburg,Erich Franzidentified as the cumulative effect of fluctuations in the velocity components combined with fluctuations in the concentrations. Recent work enables the vertical eddy diffusivity coefficient to be parameterized in terms of small scale parameters for two portions of the water column; the region just

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Ragnar Holm,Bernhard Kirschsteinany gases, the transfer between the interface and the bulk liquid (transfer coefficient k.) is rate controlling, whereas for other gases, notably reactive ones, a more complex situation has to be dealt with. The available oceanic field data for k. are presented. The value of k. increases considerabl

FER

Die Raumladungsschw?chung des Schroteffektesc processes. The ozone influx is probably the largest and most significant one. Ozone reacts with dissolved iodide and with other unknown components. One consequence is the formation of volatile iodine species, perhaps in sufficient amounts to balance the atmospheric iodine budget. However, most of

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Bernhard Kirschstein,Floris Koppelmannimes, ranged from oligotrophic subtropical gyres to eutrophic eastern boundary and equatorial divergence zones. Modeling of the disequilibria between .Th and .U within the surface waters provides estimates for the residence time of dissolved thorium with respect to particle scavenging, the residence

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Bernhard Kirschstein,Floris Koppelmann, but are so numerous that a 3 or 30 ml sample yields a statistically significant count of the bacteria and flagellates, respectively. The bacterial population contains not only the organotrophs responsible for organic matter decomposition and mineralization, but conspicuous and important population

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heckle

Die Raumladungsschw?chung des Schroteffekteserently 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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