Journal of Tropical Oceanography ›› 2018, Vol. 37 ›› Issue (5): 86-97.doi: 10.11978/2017113CSTR: 32234.14.2017113

• Orginal Article • Previous Articles     Next Articles

Bottom water temperature measurements in the South China Sea, eastern Indian Ocean and western Pacific Ocean*

Xiaoqiu YANG1(), Xiaobin SHI1, Junfeng ZHAO1, Chuanhai YU1,2, Hongfang GAO3, Aihua CHEN3, Yuanzheng LU4, Xianrong CEN4, Weiren LIN5, Xin ZENG1, Hehua XU1, Ziqiang REN1,2, Shengqi ZHOU4, Ziying XU3, Jinlong SUN1, Nana KAMIYA5, Jian LIN1   

  1. 1. CAS Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Guangzhou 510301, China 2. University of Chinese Academy of Sciences, Beijing 100049, China
    3. Key Laboratory of Marine Mineral Resources, Ministry of Land and Resources, Guangzhou Marine Geological Survey, Guangzhou 510075, China
    4. State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
    5. Graduate School of Engineering, Kyoto University, Kyoto 615-8540, Japan
  • Received:2017-10-20 Revised:2018-02-27 Online:2018-09-20 Published:2018-10-13
  • Supported by:
    Instrument Developing Project of the Chinese Academy of Sciences (YZ201136);National Natural Science Foundation of China (41106086, 41474065, 41376059, 41376061, 91428205, 41576036, 41076028, 41476167, and 41606080);Chinese Academy of Sciences Scholarship, the Strategic Priority Research Program of the Chinese Academy of Sciences (XDA11040303, XDA13010104 and XDA11030301);National High Technology Research and Development Program of China (“863” Program) (2006AA07A203 and 2009AA09A201-05);China Geological Survey Program (1212011220117);Open Project of Key Laboratory of Submarine Geosciences, State Oceanic Administration (KLSG1502);and Mariana Trench Project of the Chinese Academy of Sciences (Y4SL021001).

Abstract:

In this paper, we reported the latest bottom water temperature (BWT) data, from 158 stations in the South China Sea (SCS), 30 stations in the eastern Indian Ocean (EIO) and 37 stations in the western Pacific Ocean (WPO). Based on the new data in the SCS and WPO, we obtained good empirical relationships between BWT and water depth. They can provide accurate and reliable boundary conditions for geophysics and physical oceanography in the SCS and WPO. Furthermore, it will be very helpful for the investigation and assessment of oil and gas resources in the oceans. The measured BWT in the SCS (~2.47°C) is higher than that in the EIO (~1.34°C) and WPO (~1.60°C) where the water depth is deeper than 3500 m. This is consistent with the model of the great ocean conveyor belt since the cold and saline deep water, which is from Greenland, Iceland in the North Atlantic and the sea area around the Antarctica, enters the Indian and Pacific oceans from the south. In the Southwest Taiwan Basin, the BWTs at several stations are around 3.00°C, which is clearly higher than the average value (~2.33°C) at other stations with the same water depth range (2700~3000 m) in this basin. The local high anomaly of BWT is probably caused by the hydrothermal activity in the Southwest Taiwan Basin. In the EIO and WPO, the BWT increases slightly at the rates of 10.6 mK·MPa-1 and 12.0 mK·MPa-1, respectively, when the water depth is deeper than 4800 m. The rising rates are consistent with the estimated adiabatic pressure derivative of the temperature of the deep bottom water. It indicates that the BWT rising is mainly caused by the adiabatic compression in the deep water.

Key words: bottom water temperature, South China Sea, eastern Indian Ocean, western Pacific Ocean, model of the great ocean conveyor belt

CLC Number: 

  • P733.41