First appearance of the Deep Western Boundary Current in the Bounty Trough region, east of New Zealand

The Bounty Trough lies east of the Tasmanian Gateway, passage of the main deep inflow to the Pacific Ocean manifested as the Deep Western Boundary Current (DWBC). In the Bounty Trough Region tranquil flow conditions allow sediment deposition that records changes in the DWBC flow. It has been the tar...

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Bibliographic Details
Main Authors: Horn, Michael, Uenzelmann-Neben, Gabriele
Format: Conference Object
Language:unknown
Published: 2014
Subjects:
Online Access:https://epic.awi.de/id/eprint/35193/
https://hdl.handle.net/10013/epic.43297