Titlebook: Bottom Gravity Currents and Overflows in Deep Channels of the Atlantic Ocean; Observations, Analys Eugene G. Morozov,Roman Y. Tarakanov,Dmi

Carcinoma

Further Propagation of Antarctic Bottom Water from the Brazil Basin,flows in the region of the main sills of the equatorial channels and outflow of Antarctic Bottom Water to the Guinea Basin. Analysis is based on the CTD casts combined with LADCP profiles, and a mooring deployed in the region. We assume Wüst’s (.) definition of Antarctic Bottom Water propagation. In

Harness

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Passages in the East Azores Ridge,o previous measurements in 1982 (from 2.011 °C to 2.002 °C). The potential temperature at the bottom measured in 2013 in the Western Gap was 1.995 °C. The transport of bottom water through the Western Gap was not less than through the Discovery Gap..The Discovery Gap located at 37° N, 16° W was prev

Contend

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Deep Water Masses of the South and North Atlantic,f the properties of the deep, and bottom waters and conditions of their formation. Despite the fact that almost the whole book is related to the spreading of Antarctic Bottom Water, the dynamics of this water is correlated with the other water masses of the Atlantic. We also describe the properties

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General Overview of Abyssal Pathways, and Channels (for Waters of the Antarctic Origin),ces in the Southern Ocean. The chapter also summarizes the quantitative indicators of bottom flows in the abyssal channels. Comparison of the limits of distribution of Antarctic waters is given depending on the specific characteristics used to identify them.

hypotension

Source Regions,ontinent. The distribution paths of Antarctic waters between the basins of the Atlantic are confined to the depressions of the bottom topography. From the Weddell Sea, Antarctic waters in the abyss spread to the north through four passages in the South Scotia Ridge as well as through the South Sandw

先驱

Exchange Between the Argentine and Brazil Basins; Abyssal Pathways and Bottom Flow Channels (for Wae Santos Plateau. The depths of the Vema Channel exceed 4600 m, while the background depths of the Santos Plateau and Hunter Channel are approximately 4000 m. The Vema Channel is a narrow passage between two terraces with a minimum width slightly greater than 15 km. Investigations in these channels

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Fractures in the Mid-Atlantic Ridge of the North Atlantic,e flows of Antarctic Bottom Water through the fracture zones in the northern part of the Mid-Atlantic Ridge based on the CTD and LADCP observations in 2006, 2014, 2015, and 2016. We measured the thermohaline properties and velocities and analyzed the flows of bottom water in the Strakhov, Bogdanov,