New model and field data on estimates of Antarctic Bottom Water flow through the deep Vema Channel

被引：0
|
作者：
D. I. Frey
V. V. Fomin
N. A. Diansky
E. G. Morozov
V. G. Neiman
机构：
[1] Russian Academy of Sciences,Shirshov Institute of Oceanology
[2] Russian Academy of Sciences,Institute of Numerical Mathematics
[3] Zubov State Oceanographic Institute,undefined
来源：
Doklady Earth Sciences | 2017年 / 474卷
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摘要：
We used a numerical model of the ocean circulation with a high spatial resolution to obtain estimates of the kinematic characteristics of Antarctic Bottom Water flow through the abyssal Vema Channel in the southwestern part of the Atlantic Ocean. The results of simulations correspond to the data of direct velocity measurements made at several locations in the channel. The high horizontal and vertical resolution of the model in the bottom layer allowed us to study in detail the hydrodynamics of this flow over its entire length.
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页码：561 / 564
页数：3
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