This book is dedicated to the study of structure and transport of deep and bottom waters above and through underwater channels of the Atlantic Ocean. The study is based on recent observations, analysis of historical data, and literature reviews. This approach allows us to understand how water transport and water mass prop- ties have changed over the last years and decades. The focus of our study is on the propagation of bottom waters in the Atlantic Ocean based on new field data at key points. At the end of the 1920s, the first integral study of water masses and bottom topography of the Central and South Atlantic was carried out from the German - search vessel Meteor. This German Atlantic Expedition was one of the first cruises equipped with the newly developed echo sounder (fathometer): an obligatory p- requisite for the investigation of bottom morphology in the deep sea on an - erational base. The results of the expedition were published by Wüst, Defant, and colleagues in the multivolume METEOR publication series starting with the cruise report by the ship’s commander (Spiess 1928, 1932). Historically, this series of p- lications, intermittently interrupted by World War II, was the basis for many years of research into the development of modern concepts about Atlantic water masses and their circulation schemes.
This book is dedicated to the analysis of bottom waters flows through underwater channels of the Atlantic Ocean.
Our book reviews the studies carried out in different abyssal channels of the Atlantic Ocean, combined with our recent oceanographic research and analysis of observations in the main underwater channels of the Atlantic Ocean.
Kalb, J. E., C. J. Jolly, A. Mebrate, S. Tebedge, C. Smart, E. B. Oswald, D. Cramer, P. Whitehead, C. B. Wood, G. C. Conroy, T. Adefris, L. Sperling, and B. Kana, 1982, Fossil mammals and artifacts from the Middle Awash Valley, ...
" This series will cover a number of subjects related to sediments and sedimentary rocks in a manner that both the researcher and the industrially oriented earth scientist can use constructively.
On the circulation of bottom water in the region of the Vema Channel. Deep Sea Research, 49, 1119–1139. Morozov, E. G., Demidov, A. N., & Tarakanov, R Yu. (2008). Transport of Antarctic waters in the deep channels of the Atlantic Ocean.
Mar Geol 23:M19–M25. https://doi.org/10.1016/ 0025-3227(77)90092-5 Hlawatsch S, Neumann T, Van Den Berg CMG et al (2002) Fast-growing, shallow-water ferromanganese nodules from the western Baltic Sea: origin and modes of trace element ...
8 Conclusions This Chapter is a review of recent field studies of bottom transport of bottom through the main abyssal channels of the Atlantic Ocean. The expeditions carried out in the last 10 year made measurements with CTD-casts and ...
123 7.1 · Bering Sea The Bering Sea The Pacific Ocean Size of particles (mm) Number of samples Average content ... Coefficient of sorting (So) of the gravel and pebbles from the Black Sea coasts varied from 1.1 to 2.5 and from 1.1 to ...
Abyssal hydrography, nephelometry, currents, and benthic boundary layer structure in the Vema Channel. J. Geophys. ... Influences of Norwegian Sea overflow water on sedimentation in the northern North Atlantic and Labrador Sea.
In this case, choosing a higher value for the flatness parameter ignores the classification of undesired artifacts, but also loses the ability to classify features of interest like the abyssal channels in Figure 12.