By Jorge Guillén, Juan Acosta, Francesco Latino Chiocci, Albert Palanques
This atlas illustrates the features of present-day bedforms, from the coastline to deep-sea environments, and it's also brief experiences of the most mechanisms that generate such bedforms. The atlas is aimed toward the examine group, as well as scholars, the general public at huge and firms with pursuits within the marine surroundings. The e-book is split into seven sections composed of a few brief chapters: 1) bedform research and the most actual methods, 2) bedforms within the coastal quarter, three) bedforms on prodeltas and looked after bedforms, four) bedforms at the continental shelf, five) bedforms and benthos, 6) bedforms in submarine canyons and seven) slope and deep-sea bedforms. This atlas deals a entire, notwithstanding no longer exhaustive, view of the range of bedforms and linked techniques and of the morphological and temporal scales within the enclosed tideless western Mediterranean Sea.
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Extra info for Atlas of Bedforms in the Western Mediterranean
Its limited thickness makes it prone to supercritical flow and causes the downward expansion of the supercritical flow domain in the diagram. Furthermore, the high sediment concentrations near the base of the flow are now thought to suppress the turbulence and thereby preventing the formation of any ripples and dunes. 5 m) dense basal layer, as in case III, its thickness making it less prone to supercritical flow, thereby shifting the supercritical flow domain back up again in the diagram. Panel V shows a very thick (2 m), dense basal layer, which again shifts the supercritical flow ﬁeld further upwards.
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