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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MENT

rods366

Surface Water 234Th/238U Disequilibria: Spatial and Temporal Variations of Scavenging Rates within td with particulate organic carbon flux throughout a wide range of marine environments ranging from estuaries to the deep sea. Including these environments, which represent end-members for .Th scavenging intensity, the residence time for dissolved .Th is shown to vary from 0.3 days to 2 years dependi

Pastry

Dominant Microorganisms of the Upper Ocean: Form and Function, Spatial Distribution and Photoregulat dominant microorganisms have two major distributions, as plankters free in the water and as epibionts associated with the aggregated seston that makes up marine snow. Their physical state as plankters or as epibionts has a major effect on their spatial distribution and, therefore, their activity an

critique

What Controls the Variability of Carbon Dioxide in the Surface Ocean? A Plea for Complete Informatio those invoking the dominance of physical processes..What appears to be true is that a complete experiment separating these effects has yet to be done, recognizing that the feedback between ocean mixing and biological productivity prevents, of course, a truly separate set of processes. The great var

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Gustav Fr?lich,Walter Sp?ttel,Ernst T?nzero for the marine atmosphere. Such processes include air-sea exchange of stable gases and particles, as well as free radicals and other unstable species. Furthermore, biological and photochemical activity near the ocean surface leads to the production of gases and to speciation changes for ionic form

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nominal

Bernhard Kirschstein,Floris Koppelmannd with particulate organic carbon flux throughout a wide range of marine environments ranging from estuaries to the deep sea. Including these environments, which represent end-members for .Th scavenging intensity, the residence time for dissolved .Th is shown to vary from 0.3 days to 2 years dependi

Ptosis

Bernhard Kirschstein,Floris Koppelmann dominant microorganisms have two major distributions, as plankters free in the water and as epibionts associated with the aggregated seston that makes up marine snow. Their physical state as plankters or as epibionts has a major effect on their spatial distribution and, therefore, their activity an

Anthrp

Werner Nagel,Elisabeth Brandenburger those invoking the dominance of physical processes..What appears to be true is that a complete experiment separating these effects has yet to be done, recognizing that the feedback between ocean mixing and biological productivity prevents, of course, a truly separate set of processes. The great var