Abstract
There are several bulk flux models for an ocean surface boundary layer, such as surface roughness and TKE fluxes at the ocean surface. However, these bulk flux models have not been calibrated in detail.The validation for the parameterization of bulk flux models is carried out analyzing correlation of temperature and velocity vertical distributions between numerical results and observed data. The numerical experiments were conducted during the Typhoon Melor in 2009 at Tanabe Bay, Wakayama Prefecture, Japan. It was found that the parameterization for the TKE flux has significant influences on temperature and velocity in the nearshore region.
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 callMore From: Journal of Japan Society of Civil Engineers, Ser. B2 (Coastal Engineering)
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.
