Journal of Tropical Oceanography ›› 2019, Vol. 38 ›› Issue (5): 18-31.doi: 10.11978/2018132CSTR: 32234.14.2018132

• Marine Hydrography • Previous Articles     Next Articles

Intraseasonal-to-semiannual variability of barrier layer thickness in the eastern equatorial lndian Ocean and Bay of Bengal

Tian MA1,2,Yiquan QI3(),Xuhua CHENG3   

  1. 1. State Key Laboratory of Tropical Oceanography (South China Sea Institute of Oceanology, Chinese Academy of Sciences), Guangzhou 510301, China
    2. University of Chinese Academy of Sciences, Beijing 100049, China
    3. College of Oceanography, Hohai University, Nanjing, 210098, China
  • Received:2018-11-29 Revised:2019-03-03 Online:2019-09-20 Published:2019-10-09
  • Contact: Yiquan QI E-mail:qiyiquan@hhu.edu.cn
  • Supported by:
    National Key Research Development Program of China(2018YFA0605702);Natural Science Foundation of China(41522601);Natural Science Foundation of China(41876002);Natural Science Foundation of China(41876224);Fundamental Research Funds for the Central Universities(2017B04714);Fundamental Research Funds for the Central Universities(2017B04114)

Abstract:

Based on the gridded temperature and salinity data of ARGO and satellite observations from 2002 to 2015, the intraseasonal-to-semiannual variability of barrier layer (BL) in the eastern equatorial Indian Ocean (EEIO) and Bay of Bengal (BOB) is revealed, and its variation mechanism is discussed. The results show that strong variation of barrier layer thickness (BLT) is located in the EEIO and northern BOB. In the equatorial region, the variability in BLT is affected by both isothermal layer depth (ILD) and mixing layer depth (MLD). From May to July and from November to January, driven by westerly winds, the Wyrtki jet carries high-salinity water from the Arabian Sea to the eastern equatorial region, forming salinity stratification with fresh water on the surface. The downwelling Kelvin wave, which is also driven by westerly winds, deepens the isothermal layer. Then, the isothermal layer separates from the mixed layer. The barrier layer is formed. In the northern BOB, a large amount of fresh water brought by abundant rainfall and runoff produces strong salinity stratification near the surface, which causes the mixed layer to be very shallow all year round. The intraseasonal-to-semiannual variability in BLT is mainly controlled by ILD. A dynamic correlation exists between the two high value regions. The equatorial westerly (easterly) winds force the downwelling (upwelling) Kelvin wave to spread eastward, and it turns into a coastal Kelvin wave when arriving at Sumatra Island; then, the waves propagate northward to the eastern and northern boundaries of the BOB. In addition, at the top of Burma's Irrawaddy Delta, the coastal Kelvin wave radiates Rossby waves that cause positive (negative) anomalies of ILD in the bay. The wave speed determines the change in the bay, which lags the equatorial region by 1~2 months.

Key words: barrier layer thickness, intraseasonal variability, semiannual variability, eastern equatorial Indian Ocean, Bay of Bengal

CLC Number: 

  • P731.1