“…Most DF microseisms observed on land are generated in coastal regions by ocean wave activity and propagate into the continent primarily as Rayleigh waves [ Haubrich and McCamy , ; Cessaro , ; Friedrich et al , ; Schimmel et al , ; Bromirski et al , ]. However, it has also been reported that DF microseisms can be generated by distant mid‐ocean storms and propagate as P waves [ Haubrich and McCamy , ; Lacoss et al , ; Vinnik , ; Gerstoft et al , ; Koper et al , ; Sheen , ] and even as P P and P K P phases [ Gerstoft et al , ; Koper and de Foy , ; Koper et al , ; Landes et al , ].…”