Abstract
The nose velocity and thickness of intrusive gravity currents were estimated by force balance between buoyancy and inertia forces or between buoyancy and viscous forces. This laminar model shows both the nose velocity and thickness of intrusion are constant in the buoyancy-inertia regime, and are varied in the buoyancy-viscous regime with time. To clarify the difference between the two regimes, we performed laboratory experiments using a channel filled with linearly stratified fluids. Under the low discharge, or buoyancy-viscous regime, the nose velocity and thickness of intrusion were dependent on the elapsed time and the shapes of intrusion head were very sharp.
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.