Abstract
Inflow to the South Fiji Basin from the deep boundary current east of New Zealand and the Kermadec Ridge occurs only in the potential-temperature interval 2.0–2.2°C, at a rate of about 0.2 × 10 6 m 3 s −1.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
More From: Deep Sea Research Part I: Oceanographic Research Papers
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.