“…In the natural near‐shore environment, waves often coexist with currents, which can induce excess pore pressure in the porous marine sediments and weaken the stability of the seabed. The dynamic interaction of waves, currents, and the seabed has been considered critical in the studies of sediment transport and local scour (e.g., Anderson et al., 2017; Li, Ong, Fuhrman, & Larsen, 2020; Qi & Gao, 2014), seabed liquefaction (e.g., Klammler et al., 2021; Li, Ong, & Tang, 2020; Zhou, Liu, et al., 2021; Zhou, Qi, et al., 2021), and instability of offshore foundations (e.g., Cuéllar et al., 2012; De Groot et al., 2006; Oumeraci, 1994). Nevertheless, existing laboratory experiments for combined wave‐current induced pore pressure have been limited to small wave periods, and most previous theoretical research did not consider the wave‐current coupling effects adequately.…”