Sidedness of Divergence as a Key to Understanding
Southern Ocean Upwelling in the Overturning
Circulation of the Oceans
Volume 2 - Issue 4
L Bruce Railsback*
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- Department of Geology, University of Georgia, USA
*Corresponding author:
L Bruce Railsback, Department of Geology, University of Georgia, USA
Received: February 01, 2019; Published: February 11, 2019
DOI: 10.32474/MAOPS.2019.02.000143
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Abstract
Sidedness of divergence helps resolve a present discordance in our understanding of upwelling in the Southern Ocean, and
thus it contributes to the evolving recognition of the oceans’ overturning circulation. Divergence can be two-sided (one water mass
rises and moves apart in two flows, as is commonly envisioned) or one-sided (one water mass rises and moves away from another
that does not move in the opposite direction). Upwelling in the Southern Ocean can be envisioned as a one-sided divergence north
of a two-sided divergence. In the more northern one-sided divergence, deep to intermediate waters above or from North Atlantic
Deep Water (NADW) upwell into the Antarctica Circumpolar Current (ACC) and move north. In the more southern and two-sided
divergence, North Atlantic Deep Water (NADW) upwells and diverges southward into the Antarctic Coastal Current (ACoC) or Polar
Current (PC) and northward into the ACC, mixing with the waters upwelled in the northern divergence. Understanding the northern
upwelling as one-sided and the southern as two-sided thus eliminates an either/or conundrum that has evolved in the literature.
It also allows the two modes of Southern Ocean upwelling (northern in the ACC and southern in the Antarctic Divergence) to be
seen in the same comparative light as the two modes of upwelling postulated at global scale (upwelling in the Southern Ocean and
upwelling or vertical mixing in the Indo-Pacific): in each comparison, the former involves the greater flux of water, whereas the
latter involves water richer in geochemical tracers indicative of greater time and/or distance traveled at depth.
Keywords:Convergence; Divergence; Upwelling; Southern Ocean; Antarctica Circumpolar Current; Antarctic Coastal Current;
Polar Current; Antarctic Divergence, North Atlantic Deep Water; Circumpolar Deep Water, Overturning circulation; Atlantic
meridional overturning circulation; Sidedness, Great Ocean Conveyor, Plate tectonics, Troposphere
Abbreviations:AABW: Antarctic Bottom Water, ACC: Antarctic Circumpolar Current, ACoC: Antarctic Coastal Current, CDW:
Circumpolar Deep Water, DIC: Dissolved inorganic carbon, NADW: North Atlantic Deep Water, PC: Polar Current
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