Abstract
The paper presents a technique for restoring gaps in the original data, which made it possible to study the variability of fluctuations in the currents speed over significant time intervals. Analysis of the reconstructed continuous series of observations showed that high-frequency fluctuations in current speed predominate in the coastal zone, the possible source of which is the submesoscale eddies present here most of the time. On the continental slope, i.e. in the deep-water part of the sea, larger-scale processes dominate, associated with the dynamics of mesoscale eddies, meandering of the main Black Sea current, as well as global (on the scale of the entire sea) wind variability.
Sign-in/Register to access full text options 
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 callDisclaimer: 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.
