Fig. 5.From: Dynamic tsunami generation due to sea-bottom deformation: Analytical representation based on linear potential theoryAmplitudes of the source terms in the horizontal component (dashed lines) and the vertical component (solid lines) normalized by the vertical component at the sea bottom for values of k = 0.1 and 0.3 km−1, corresponding to wavelengths λ of 60 and 20 km for a water depth of 4 km (From Eqs. (20) and (21)).Back to article page