Abstract
The results of integrated monitoring of the water dynamics in the coastal zone of the southern coast of Crimea for 2008–2016 are presented. The mode and features of coastal water circulation are determined. An intensive contribution of low-frequency oscillations of coastal currents on a seasonal and synoptic scale is identified based on the results of the spectral analysis of a nine-year set of vector dynamics series. The longshore structure of reciprocating jet streams caused by water dynamics on the shelf and the continental slope dominates during water fluctuations in the coastal zone.
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.
