Abstract
Warm-core ring 82-B (WCR 82-B) formed from a Gulf Stream meander in the winter of 1982. The T/S properties of the thermostad of the ring in April were different than the surrounding Slope Water and the possible source water, the Gulf Stream or the Sargasso Sea. A convective mixing model was applied to the formation of the thermostad of WCR 82-B. The T/S relationships derived using Gulf Stream source water were more consistent with the field observations in March and April than those obtained using the Sargasso Sea as the source water. Chemical data provided further support for distinguishing Gulf Stream rather than Sargasso Sea as the source. Contrary to earlier notions the source water for WCR 82-B was the Gulf Stream. The thermostad was not modified 18-degree water from the Sargasso Sea.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callMore From: Deep Sea Research Part A. 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.
