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

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Eastern Basin Pathways and Further Propagation of Antarctic Bottom Water in the East Atlantic, the basin. In 1983, Mantyla and Reid wrote that bottom waters propagating through the Romanche Fracture Zone influence only the equatorial and southeastern part of the Atlantic Ocean and do not spread to the north through the Kane Gap, whereas the Vema Fracture Zone is the main pathway for bottom w

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Passages in the East Azores Ridge,adeira Basin to the Iberian Basin is studied on the basis of hydrographic measurements in October 2011 and in September 2013, historical data from the WOD18 database, and recent data on bottom topography. The overflow of the coldest water occurs through two passages with close depths at 16° W (Disco

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Flows Through the Northern Channels in the North Atlantic,the Strait of Denmark,?Faroe Bank Channel, and in the Bear Island Trough. The flows are investigated on the basis of CTD/LADCP casts and moorings and review of previous publications. The Charlie Gibbs Fracture Zone is the main pathway for deep water exchange across the Reykjanes Ridge, while the Big

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Deep Water Masses of the South and North Atlantic,of several water masses in the deep and bottom layers of the Atlantic. We analyze the mechanisms of the formation of these waters and their circulation. We compare different definitions of Antarctic Bottom Water (as well as some other water masses) and criteria to identify their boundaries.

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Fractures in the Mid-Atlantic Ridge of the North Atlantic,nnect the deep basins of the East and West Atlantic. In addition to the known fact that the main portion of water (approximately 1?Sv) propagates through the Vema Fracture Zone (11° N) we revealed that approximately half of this volume propagates through the other fractures.

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Book 2021ions of the authors, analysis of historical data, numerical modeling, and literature review. For example, studying both the measurements from the World Ocean Circulation experiment in the 1990s and recent measurements reveals the decadal variations of water properties in the ocean..Seawater is coole

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London’s Women Artists, 1900-1914hrough the Vema Chanel, Hunter Channel, and over the Santos Plateau. Another part of this flow is entrained into the Antarctic Circumpolar Current and propagates to the east around Antarctica. A small upper part of Antarctic waters spreads through the Agulhas and Cape basins to the Angola Basin.

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