Abstract
A series of three-dimensional computations are conducted to investigate convective flow generated by an interaction between a vertical solute gradient and a horizontal thermal gradient. The convection develops into what is called a fully developed flow which is composed of the largest number of horizontal convection layers. Within each layer there prevails an array of salt-finger vortices. The multilayered structure changes systematically with boundary values, while the convection layer bears a layer thickness, so that the positive thermal buoyancy can balance with the negative solute buoyancy.
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.