摘要： AbstractThe rightward tendency (in northern hemisphere) of enhanced phytoplankton bloom often observed in the wake of a tropical cyclone has commonly been attributed to the rightward bias of mixing due to stronger wind and wind‐current resonance. We demonstrated using a high‐resolution biophysical model that vertical mixing alone resulted only in weak asymmetry after the passage of the storm. The enhanced bloom was caused instead by decreased turbulence due to restratification by submesoscale recirculation cells preferentially produced on the right side, rightward shift of cool isotherms, and spin‐up of a subsurface jet. We showed using a two‐time scale asymptotic expansion that these slower‐evolving features were forced by resonance Reynolds stresses of the energetic and rapidly oscillating near‐inertial internal waves. 其他題名： J. Geophys. Res. Oceans 出版者： Washington: Blackwell Publishing Ltd 出版日期： 2015-08 出處： Journal of Geophysical Research: Oceans, 2015-08, Vol.120 (8), p.5735-5748 資源來源： Wiley Online Library eJournals 版權： 2015. American Geophysical Union. All Rights Reserved. 識別號： ISSN: 2169-9275 識別號： EISSN: 2169-9291 識別號： DOI: 10.1002/2015JC010896
