Journal of Tropical Oceanography ›› 2020, Vol. 39 ›› Issue (5): 98-108.doi: 10.11978/2019117CSTR: 32234.14.2019117

• Marine Hydrology • Previous Articles     Next Articles

Preliminary analysis on climatological and seasonal variation of barrier layer thickness in the northern Indian Ocean and it’s mechanism

LIU Ying1,2(), YAN Youfang1, LING Zheng3()   

  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. Guangdong Key Laboratory of Coastal Ocean Variability and Disaster Prediction, College of Ocean and Meteorology, Guangdong Ocean University, Zhanjiang 524088, China
  • Received:2019-11-18 Revised:2020-02-15 Online:2020-09-10 Published:2020-02-25
  • Contact: Zheng LING E-mail:liuying19@mails.ucas.ac.cn;lingz@gdou.edu.cn
  • Supported by:
    Natural Science Foundation of China(41776037);Strategic Priority Research Program of Chinese Academy of Sciences(XDB42000000)

Abstract:

Based on the Array for Real-Time Geostrophic Oceanography (Argo) temperature and salinity observations from 2004 to 2018, we studies the spatial and temporal variations of the barrier layer in the Northern Indian Ocean (40°—105°E, 5°S—25°N) by using EOF (Empirical Orthogonal Function) analysis, wavelet analysis and other methods. The results show that barrier layer exists in the eastern Indian Ocean all year round, but the probability of its occurrence in the western Indian Ocean is low. Thick barriers appear mainly in the south-eastern Arabian Sea (67°—75°E, 3°—12°N), Bay of Bengal (82°—93°E, 11°—20°N) and eastern equatorial Indian Ocean (81°—102°E, 4°S—3°N). The thickness of the barrier layer, which is present in the southeast Arabian Sea and Bay of Bengal, exhibits remarkable annual variation with the largest value in winter and the smallest in summer. In the eastern equatorial Indian Ocean, there is a semi-annual cycle, with peaks in summer and winter. Further analysis shows that the thickness of the barrier layer in the Bay of Bengal and eastern equatorial Indian Ocean is mainly affected by the change of isothermal layer depth, while the change of mixed layer depth has little effect on the change of barrier layer thickness. The thickness of the barrier layer in the Arabian Sea is affected by the changes of both isothermal layer depth and mixed layer depth, of which the isothermal layer depth has a greater influence on it.

Key words: Northern Indian Ocean, barrier layer thickness, isothermal layer, mixed layer

CLC Number: 

  • P731.24