Abstract
Numerical experiments are described in which overturning motions mix temperature and salt across stabilizing vertical gradients. In all instances, mixing of temperature exceeds that of salt. Temperature and salinity fluxes can differ significantly, even when large compared to the thermal conductive flux.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
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 call
