Abstract
The time evolution of the thermocline in the Archipelago of La Maddalena in the Summer 1976, when a quick atmospheric front of western origin passed through the archipelago, is discussed. Large-amplitude internal waves are observed. We present and discuss the idea that they are generated through a mechanism of baroclinic compensation of the wind stress, strongly enhanced by the morphology of the archipelago.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
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.