Journal of Tropical Oceanography ›› 2016, Vol. 35 ›› Issue (4): 21-30.doi: 10.11978/2015097CSTR: 32234.14.2015097

• Marine Meteorology • Previous Articles     Next Articles

Wind energy input and its secular change of surface waves in the South China Sea

CUI Chaoran1, 5, GUAN Yuping1, 5, 6, ZHU Yaohua2, WANG Hui3, HUANG Ruixin4   

  1. 1. State Key Laboratory of Tropical Oceanography (South China Sea Institute of Oceanology, Chinese Academy of Sciences), Guangzhou 510301, China;
    2. Key Laboratory of Marine Science and Numerical Modeling, First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China;
    3. National Marine Environmental Forecasting Center, Beijing 100081, China;
    4. Woods Hole Oceanographic Institution, Woods Hole, MA02543, USA;
    5. University of Chinese Academy of Sciences, Beijing 100049, China;
    6. Zhuhai Joint Innovative Center for Climate-Environment-Ecosystem, Zhuhai 519078, China;
  • Received:2015-07-20 Online:2016-07-29 Published:2016-08-04
  • Contact: GUAN Yuping. E-mail: guan@scsio.ac.cn
  • Supported by:
    Chinese National Natural Science Foundation (91228202); the National Basic Research Program of China (2013CB956201)

Abstract: The energy of winds into surface waves in the South China Sea during 1871-2008 was estimated by using the ocean reanalysis data of SODA (simple ocean data assimilation) 2.2.4 (1871-2008). The results showed that the annual wind energy input is about 0.2 TW, and that the spatial pattern of this kind of input is mainly located in the northern parts of the South China Sea during winter and in the southern parts in summer; and the intensity of summer input is much weaker than that of winter. Similar results were obtained by using the ERA-40 (European Centre for Medium-Range Weather Forecasts re-analysis-40) (1957-2002) and ERA-20C (1900-2010) data sets. The secular trend of wind energy input into waves was reduced at the rate of 0.43% per year since 1950. We also studied the swells and wind waves, which are two categories of the waves, by using the ERA-interim data. The spatial pattern of wind energy input into the swells and wind waves is mainly located in the northern parts of the South China Sea, but there is also a high wind energy input into the wind waves area in the southern parts of the South China Sea. The secular trend of the wind energy input into swells was increasing, and the same trend of wind energy input into the wind waves was reducing; the total energy input was also reducing by the joint effect of swells and wind waves. All of this was thanks to the weakening East Asian monsoon, which dominated in the South China Sea, in recent decades. These results are significant for understanding the variation of the surface waves in the South China Sea.

Key words: ocean wave, South China Sea, wind power, East Asian monsoon

CLC Number: 

  • P732.6