Journal of Tropical Oceanography ›› 2011, Vol. 30 ›› Issue (5): 48-54.doi: 10.11978/j.issn.1009-5470.2011.05.048cstr: 32234.14.j.issn.1009-5470.2011.05.048

Special Issue: 海洋大数据及应用

• Marine geomorphology • Previous Articles     Next Articles

Effect of surface wave breaking on upper-ocean structure revealed by assimilating sea temperature data

ZHANG Xue-feng1,2, HAN Gui-jun2, WU Xin-rong2, LI Wei2, WANG Dong-xiao1   

  1. 1. State Key Laboratory of Tropical Oceanography South China Sea Institute of Oceanology, CAS , Guangzhou 510301, China ; 2. National Marine Data and Information Service, Tianjin 300171, China
  • Received:2011-11-01 Revised:2011-11-01 Online:2011-11-01 Published:2011-11-01
  • Contact: 张学峰 E-mail:zhangxf@mail.nmdis. gov.cn

Abstract: Sensitivity of sea surface temperature (SST) to wave energy factor a and Charnock parameter b is discussed using Mellor-Yamada 2.5 turbulence closure model in which wave breaking is considered. The upper-ocean temperature data in summer from OWS Station Papa is assimilated to estimate a and b via a variational approach optimally. It shows that the cost function reaches minimum when a =167 and b =4.1×105. Both monthly and daily SSTs at OWS Station Papa can be successfully reconstructed with the optimal a and b , and the simulated temperature and depth of surface mixed layer are also consistent with the observation. The equation of turbulent kinetic energy is diagnosed utilizing the optimal parameters, from which the effect of wave breaking on the turbulent energy budget is revealed.

Key words: sea surface roughness, wave energy factor, assimilation, wave breaking

CLC Number: 

  • P731