Abstract
A distinct, coastal upwelling cell inshore of the southern limb of the East Madagascar Current is described. The upwelling cell has cold surface water, with high concentrations of chlorophyll- a. It is located where this current moves from a bathymetry characterised by a narrow continental shelf and a steep slope to one characterised by a wider shelf and a less steep slope. There seems to be no correlation between the local winds and the presence of upwelled water, suggesting current-induced upwelling. Advection of upwelling filaments is consistent with the concept of an East Madagascar retroflection.
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.