Titlebook: Oceanography of the Ross Sea Antarctica; Antarctica Giancarlo Spezie,Giuseppe M. R. Manzella Conference proceedings 1999 Springer-Verlag It

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Particle Fluxes at the Edge of the Ross Ice Shelf: the Role of Physical Forcingatter, biogenic silica and carbonate) in a site located at the edge of the Ross Ice Shelf. The focus of this study is on data from mooring site named F, located at 77°59’.998 S, 177°01’.623 W in the framework of the C.L.I.M.A. Project (Climatic Long-term Interaction for the Mass Balance in Antarctic

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Mundane

General Characteristics of Density-Turbidity Currents in the Ross Sea (Antarctica) stability, considering also bottom erosion phenomena: in other words, the current is assumed to exchange sediments with the bottom. To simplify this complex problem a model of sediment evolution is assumed. As in recent work the excess mass due to the bottom erosion and deposition is assumed to dep

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V. Gouretskidescription of the fundamentals of sampling for wildlife and other ecological studies. We discuss a majority of sampling issues from the perspective of design-based . where empirical data are collected according to a specific study design. We end the chapter with a discussion of several common model

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description of the fundamentals of sampling for wildlife and other ecological studies. We discuss a majority of sampling issues from the perspective of design-based . where empirical data are collected according to a specific study design. We end the chapter with a discussion of several common model

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P. Picco,L. Amici,R. Meloni,L. Langone,M. Ravaiolihe best laid plans…” certainly applies to study design. The initial plan that any researcher, no matter how experienced, develops will undergo numerous changes throughout the duration of a study. As one’s experience with designing and implementing studies grows, he or she anticipates and resolves mo