Abstract

In this study, a long-term assessment of the wave energy in the China Sea was performed for a 30-year time interval (1988–2017), using the model WAVEWATCH-III. The reliability of the wave simulation results was increased by means of longer time horizon data compared to other relevant studies in the China Sea. This analysis provided information on the regional distribution as well as on the monthly and seasonal variability. The exploitation and stability of wave energy were taken into consideration, so as to find the advantage of resource exploitation. Results indicated that values of significant wave height and wave power density had obviously differences compared with different months, especially in December with a maximum significant wave height of 2.7 m and 35 kW/m of wave power density. The minimum value of them appeared in May, was 1.0 m and 4.5 kW/m, respectively. The distribution of wave energy was abundant in winter and the poorest in summer. In winter, the significant wave height in most areas was above 1.8 m, while the maximum wave energy density in summer was only 1.2 m. As for the wave power density, in winter values in most areas were above 18 kW/m, while the maximum value in summer was only 12 kW/m. In sight of regional distribution, the highest wave energy potential was located in the Northern South China Sea, the East China Sea, the Ryukyu Islands waters, east of the Taiwan Island and the Luzon Strait, with coefficient of variation was within 2.0 and occurrence of exploitation was above 80%, whereas the Bohai Sea, the northern part of the Yellow sea, the Gulf of Thailand, and the Northern Bay were in poor contribution, with occurrence of exploitation was within 50%.

Highlights

  • China has a vast coastline of 18,000 km, including the Bohai Sea, the Yellow sea, the East China Sea and the South China Sea with many islands and abundant marine resources, including tidal energy, wind energy, wave energy, and so on

  • In order to achieve the spatial distribution of significant wave height (SWH) and wave power density (WPD), they are calculated by taking an average value of simulated records of the same month in each year during 30 years

  • It is quite clear that some important information can be obtained from these contour maps as follows: 1. Generally, it is observed that the value of SWH is between 0.1 m and 2.7 m and the value of WPD is between 2 kW/m and 35 kW/m in the whole areas of the China Sea

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Summary

Introduction

China has a vast coastline of 18,000 km, including the Bohai Sea, the Yellow sea, the East China Sea and the South China Sea with many islands and abundant marine resources, including tidal energy, wind energy, wave energy, and so on. Against a backdrop of dramatic energy consumption increase, serious ecological degradation and environmental pollution (heavy smog in particular) (Li et al, 2015), there is no doubt that the exploitation of wave energy technology has become the focus of energy development and utilization due to its advantages of no pollution, wide distribution, renewable, and large storage (Falnes, 2007; Beyene, 2007; Cornejo-Bueno et al, 2016) compared with the limited fossil energy. The instability and regional differences of wave energy increase difficulties in exploitation and utilization, few of the wave energy is being utilized efficiently. It is necessary to intensify scientific research on long-term distribution characteristics of wave energy and seasonal changes and provide reliable scientific guidance for the utilization of wave energy

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