Figure 10From: Linear stability of plane Poiseuille flow in an infinite elastic medium and volcanic tremorsTime constant of exponential growth in wave amplitude. The e-folding time for the amplitude of linearly unstable antisymmetric solution to grow is plotted as a function of the peak flow speed at the center of the fluid layer. Calculation results are shown for three wavelengths of L∗ = 3.2 km (solid line), 1.6 km (broken line), and 0.8 km (dotted line) and for four fluid viscosities of ζ∗ = 104 Pa ·s (black line), 103 Pa ·s (red line), 102 Pa ·s (blue line), and 10 Pa ·s (orange line). In these examples, we set α 0 ∗ =1 km/s, β s ∗ =2.5 km/s, α s ∗ =4.3 km/s, ρ s ∗ = ρ 0 ∗ =2700 kg/m 3, δ = 0.5, and the fluid layer thickness, 2a∗, is (a) 0.2 m, (b) 0.5 m, and (c) 1 m.Back to article page