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...
Main Authors: | , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2014
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Subjects: | |
Online Access: | https://epic.awi.de/id/eprint/35060/ https://hdl.handle.net/10013/epic.43136 |