[AOS18-P02] 爆弾低気圧下における海洋表面波の発達
キーワード：海洋表面波、爆弾低気圧、北西太平洋
Ocean wave developments under explosive cyclone (EC) conditions are investigated with hindcast simulations of ocean waves in the Northwestern Pacific between 1994 and 2014. Composite analyses of the ocean wave field under EC conditions are conducted in order to obtain an overall depiction of spatio-temporal developments of ocean waves. Because of the rapid development of ECs, ocean waves beneath ECs continue to grow for about half a day after the EC begins to decay. ECs generate two areas with narrow directional spectra: on the cold side of a warm front and on the right-hand-side of the cyclone center, relative to the propagating direction. In comparison, typhoons usually generate just one area with a sharp peak. This research successfully provides a schematic diagram which illustrates the ocean wave development under an EC condition with atmospheric system (Fig. 1). This EC feature is derived from the existence of atmospheric fronts, which produce a complex wind system for the ECs. In one case study, spectral analysis of wave spectra from an EC in January 2013 indicates that the warm front plays a critical role in generating the distinctive ocean wave system in the warm and cold zones along the warm front, both of which have a narrow spectrum in direction and frequency. In contrast, ocean waves on the left-hand-side and in the backward area relative to the propagation direction are composed of swell and wind-wave systems propagating in different directions. Ocean wave disasters under ECs are proved to show dissimilar features from typhoons and should provide substantial information to maritime disaster risk management.