Flows of bottom water in fractures of the North Mid-Atlantic Ridge

E. G. Morozov; R. Yu. Tarakanov; T. A. Demidova; N. I. Makarenko

doi:10.1134/S1028334X17060058

Flows of bottom water in fractures of the North Mid-Atlantic Ridge

Авторы: Morozov E.G.¹, Tarakanov R.Y.¹, Demidova T.A.¹, Makarenko N.I.²
Учреждения:
1. Shirshov Institute of Oceanology
2. Lavrent’ev Institute of Hydrodynamics, Siberian Branch
Выпуск: Том 474, № 2 (2017)
Страницы: 653-656
Раздел: Oceanology
URL: https://ogarev-online.ru/1028-334X/article/view/190045
DOI: https://doi.org/10.1134/S1028334X17060058
ID: 190045

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It has been shown that the total transport of Antarctic Bottom Water (AABW) in the northern fractures (Kane, Cabo Verde, Marathon) are one order of magnitude smaller than in the southern fractures (Vema, Doldrums, Vernadsky). The estimates of AABW transport through this group of fractures based on measurements in 2014 were approximately 0.28 Sv, which is about 25% of the transport through the Vema Fracture Zone. However, the coldest water flows through the Vema Fracture Zone.