Sentence examples for deep water circulation from inspiring English sources
Kwiek, P. & Ravelo, A. C. Pacific Ocean intermediate and deep water circulation during the Pliocene.
Analysis of the Protector and Pirie basins shows that their tectonic evolution influenced regional deep water circulation patterns in an area that makes a significant cold water contribution to the global conveyor belt system.
Tritium provides information on water transit times and the dynamics of deep water circulation, whereas δ18O contributes to understanding the origin and flow paths of water in such mountainous regions.
In contrast with some previous work17, 39, we infer a 'floating' pool of respired carbon between 2 and 3.5 km depth in the central equatorial Pacific Ocean and conclude that existing proxy data reflecting LGM deep water circulation and carbon storage can be reconciled without invoking a significantly different glacial watermass structure in the central equatorial Pacific Ocean.
Koszalka is investigating the deep water circulation patterns of the Irminger Sea, a part of the Atlantic Ocean that lies to the east of Greenland.
Today, the North Pacific is the terminus for global deep water circulation (Broecker et al. 1985), so deep water in the North Pacific contains old carbon from the decomposition of sunken organic matter that accumulated during global circulation.
Rights & permissionsfor article Deep-water circulation changes lead North Atlantic climate during deglaciation.
Stronger contour current activity may have been related to generally enhanced North Atlantic deep-water circulation.
Bell, D. B., Jung, S. J. A. & Kroon, D. The Plio-Pleistocene development of Atlantic deep-water circulation and its influence on climate trends.
Finally, our findings may provide new challenges for investigating the South China Sea Cenozoic palaeoceanography, which are helpful to understand the sedimentary dynamic processes related to the South China Sea deep-water circulation.
The circulation of water masses, especially the deep-water circulation, is greatly influenced by all topographic features along the Brazilian continental margin and the presence of adjacent seamounts.
