[AOS16-P04] Sustainability of wave energy potential in Japan
Keywords:wave enegry, sustainability, decadal change
Marine renewable energies and especially the wave energy, as an alternative to fossil fuels, are sensitive to changing climate. In addition, considering both short-term variations and long-term changes in the available resources is necessary for sustainable development. Wave energy potential has been less investigated in Northeast Asia and Japan in long-term and the previous works are limited to three decades at the most and mainly in limited locations and based on wave records or satellite measurements [e.g., 1-5]. This study focuses on the estimation of wave energy resources in Japan using five decades of modeled wave characteristics. For this purpose, SWAN Cycle III version 41.31 (by the Delft University of Technology) [6] was utilized in order to model the wave characteristics in Northeast Asia. The input wind was JRA-55 re-analysis developed by the Japan Meteorological Agency (JMA) [7]. The spatial and temporal resolutions of the wind field are 60 km and 6 hrs, respectively and it is available for the period of 1958-2012. The boundary condition for the model was also obtained from a global performance. The model was validated against satellite measurements and the bias was calculated on a monthly scale showing the similarity between the monthly mean values in the domain. The validated model was performed to generate the wave climate for five decades. The decadal change of wave climate was assessed in 10-yearly periods, i.e., 1961-1970, 1971-1980, 1981-1990, 1991-2000, 2001-2010. The analysis was performed for wind and wave characteristics as well as wave power parameter and the relationship between their change was discussed. The results indicate the difference between the changing pattern in various decades. However, in general, wave height and wave power have been decreased in the Pacific side of Japan during the two latter decades, while the parameters did not change considerably in the Sea of Japan. In addition, the share of swells in the whole wave energy potential has been discussed and the results indicate that almost fifty percent of the total wave power is provided by swells in the Pacific side of Japan while this value reaches around 40 percent in the Ryukyu Islands. In the Sea of Japan side of Japan, the percentage of wave power obtained from swells varied between 15 and 25 percent of the total wave power. Further analysis will be discussed regarding the sustainability of wave energy resources in different time scales.
References:
[1] Tabata T, Yagyu T, Fukuda I. Wave energy on Japanese coast [in Japanese with English abstract]. 1980.
[2] Sasaki W. Changes in wave energy resources around Japan. Geophys Res Lett 2012;39.
[3] Saruwatari A, Maruyama T. Resource assessment of wave energy around Hokkaido in winter. Proceeding Japan Soc Civ Eng B3 2013;69:I_91-I_96. https://doi.org/https://doi.org/10.2208/jscejoe.69.I_91.
[4] Hirakawa T. Wave energy resource assessment around Kyushu based on numerical hindcast. J Renew Sustain Energy 2018;10:24501. https://doi.org/10.1063/1.5011431.
[5] Sasmal K, Webb A, Waseda T, Miyajima S. Wave energy resource asessment: A comparative study for two coastal areas in Japan. Adv. Renew. Energies Offshore Proc. 3rd Int. Conf. Renew. Energies Offshore (RENEW 2018), CRC Press; 2018, p. 67–71.
[6] Booij N, Ris RC, Holthuijsen LH. A third-generation wave model for coastal regions: 1. Model description and validation. J Geophys Res Ocean 1999;104:7649–66. https://doi.org/10.1029/98JC02622.
[7] KOBAYASHI S, OTA Y, HARADA Y, EBITA A, MORIYA M, ONODA H, et al. The JRA-55 Reanalysis: General Specifications and Basic Characteristics. J Meteorol Soc Japan Ser II 2015;93:5–48. https://doi.org/10.2151/jmsj.2015-001.
References:
[1] Tabata T, Yagyu T, Fukuda I. Wave energy on Japanese coast [in Japanese with English abstract]. 1980.
[2] Sasaki W. Changes in wave energy resources around Japan. Geophys Res Lett 2012;39.
[3] Saruwatari A, Maruyama T. Resource assessment of wave energy around Hokkaido in winter. Proceeding Japan Soc Civ Eng B3 2013;69:I_91-I_96. https://doi.org/https://doi.org/10.2208/jscejoe.69.I_91.
[4] Hirakawa T. Wave energy resource assessment around Kyushu based on numerical hindcast. J Renew Sustain Energy 2018;10:24501. https://doi.org/10.1063/1.5011431.
[5] Sasmal K, Webb A, Waseda T, Miyajima S. Wave energy resource asessment: A comparative study for two coastal areas in Japan. Adv. Renew. Energies Offshore Proc. 3rd Int. Conf. Renew. Energies Offshore (RENEW 2018), CRC Press; 2018, p. 67–71.
[6] Booij N, Ris RC, Holthuijsen LH. A third-generation wave model for coastal regions: 1. Model description and validation. J Geophys Res Ocean 1999;104:7649–66. https://doi.org/10.1029/98JC02622.
[7] KOBAYASHI S, OTA Y, HARADA Y, EBITA A, MORIYA M, ONODA H, et al. The JRA-55 Reanalysis: General Specifications and Basic Characteristics. J Meteorol Soc Japan Ser II 2015;93:5–48. https://doi.org/10.2151/jmsj.2015-001.