scholarly journals Changes in Bottom Water Physical Properties Above the Mid-Atlantic Ridge Flank in the Brazil Basin

2018 ◽  
Vol 123 (1) ◽  
pp. 708-719 ◽  
Author(s):  
Jian Zhao ◽  
Andreas M. Thurnherr
2020 ◽  
Author(s):  
Valentina Volkova ◽  
Alexander Demidov ◽  
Fedor Gippius

<p>Despite the fact that there are numerous estimates of the Antarctic Bottom Water (AABW) formation and transport, its evolution and distribution pathways are still debatable (Morozov E.G. et al., 2010).</p><p>The main task of this work was to identify the structure and transport of deep and bottom water mass of the fracture zones (7 40', Vernadsky and Doldrums). The research is based on new data (multibeam bottom relief, temperature, salinity, velocity) obtained during the research cruise on the RV "Akademik Nikolaj Strakhov" in October-November 2019 and WODB18 historical data.</p><p>The main result of the research is proper estimation of the AABW and LNADW transport, which takes into consideration the influence of fracture zone morphometry. Accordingly, the preliminary circulation scheme of water masses is obtained.</p>


2017 ◽  
Vol 74 (2) ◽  
pp. 147-167 ◽  
Author(s):  
Eugene G. Morozov ◽  
Roman Yu. Tarakanov ◽  
Dmitry I. Frey ◽  
Tatiana A. Demidova ◽  
Nikolay I. Makarenko

2014 ◽  
Vol 456 (1) ◽  
pp. 598-601 ◽  
Author(s):  
E. G. Morozov ◽  
R. Yu. Tarakanov

2021 ◽  
Vol 2 (1) ◽  
Author(s):  
Keir Becker ◽  
Richard E. Thomson ◽  
Earl E. Davis ◽  
Heinrich Villinger ◽  
C. Geoffrey Wheat

AbstractSix-year records of ocean bottom water temperatures at two locations in an isolated, sedimented deep-water (∼4500 m) basin on the western flank of the mid-Atlantic Ridge reveal long periods (months to >1 year) of slow temperature rises punctuated by more rapid (∼1 month) cooling events. The temperature rises are consistent with a combination of gradual heating by the geothermal flux through the basin and by diapycnal mixing, while the sharper cooling events indicate displacement of heated bottom waters by incursions of cold, dense bottom water over the deepest part of the sill bounding the basin. Profiles of bottom water temperature, salinity, and oxygen content collected just before and after a cooling event show a distinct change in the water mass suggestive of an incursion of diluted Antarctic Bottom Water from the west. Our results reveal details of a mechanism for the transfer of geothermal heat and bottom water renewal that may be common on mid-ocean ridge flanks.


2020 ◽  
Vol 47 (18) ◽  
Author(s):  
Gregory C. Johnson ◽  
Chanelle Cadot ◽  
John M. Lyman ◽  
Kristene E. McTaggart ◽  
Elizabeth L. Steffen

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