Tracing southwest pacific bottom water using potential vorticity and helium-3

This study uses potential vorticity and other tracers to identify the pathways of the densest form of Circumpolar Deep Water in the South Pacific, termed "Southwest Pacific Bottom Water" (SPBW), along the 28.2 kg m sup(-3) surface. This study focuses on the potential vorticity signals asso...

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Bibliographic Details
Published in:Journal of Physical Oceanography
Main Authors: Downes, Stephanie, Key, Robert M, Orsi, Alejandro H, Speer, Kevin G, Swift, James H
Format: Article in Journal/Newspaper
Language:unknown
Published: American Meteorological Society
Subjects:
Keywords: Abyssal circulation
Antarctic Bottom Water
Antarctic circumpolar current
Bottom current
Bottom water
Deep Water
Drake passage
Dynamical process
Helium-3
Hydrothermal vent
Isopycnal surfaces
Pacific ocean
Pacific sector
Potential vorticity
Vo Abyssal circulation
Bottom currents
Currents
South Pacific Ocean
Antarctic
The Antarctic
Drake Passage
Pacific
Antarc*
Online Access:http://hdl.handle.net/1885/71783
https://doi.org/10.1175/JPO-D-12-019.1
https://openresearch-repository.anu.edu.au/bitstream/1885/71783/5/f5625xPUB2878_2012.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/71783/7/01_Downes_Tracing_southwest_pacific_2012.pdf.jpg
Description
Summary:This study uses potential vorticity and other tracers to identify the pathways of the densest form of Circumpolar Deep Water in the South Pacific, termed "Southwest Pacific Bottom Water" (SPBW), along the 28.2 kg m sup(-3) surface. This study focuses on the potential vorticity signals associated with three major dynamical processes occurring in the vicinity of the Pacific-Antarctic Ridge: 1) the strong flow of the Antarctic Circumpolar Current (ACC), 2) lateral eddy stirring, and 3) heat and stratification changes in bottom waters induced by hydrothermal vents. These processes result in southward and downstream advection of low potential vorticity along rising isopycnal surfaces. Using δsup(3)He released from the hydrothermal vents, the influence of volcanic activity on the SPBW may be traced across the South Pacific along the path of the ACC to Drake Passage. SPBW also flowswithin the southern limb of the Ross Gyre, reaching the Antarctic Slope in places and contributes viaentrainment to the formation of Antarctic Bottom Water. Finally, it is shown that the magnitude and location of the potential vorticity signals associated with SPBW have endured over at least the last two decades, and that they are unique to the South Pacific sector.

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