We determine inviscid eigensolutions in zero pressure gradient flat plate boundary layers at Mach number five and evaluate the eigensolutions with the method of steepest descent. The resulting wave packets show that with wall cooling the tail of the packets becomes slower. Although the boundary layers investigated are all convectively unstable we interpret the slow tail of the wave packets as a trend towards an absolute instability. From a comparison of the wave packets with turbulent spot transition, we conclude that for wall cooling the general transition properties are close to those of an absolutely unstable flow.
Laminar boundary layers and linear instabilitiesThe linear stability properties of boundary layers are fundamental to the understanding of the laminar-turbulent transition process. Compressible boundary layers have special linear stability properties, such as the presence of inviscid instabilities [1]. In this contribution we focus on inviscid linear stability eigensolutions of zero pressure gradient flat plate boundary layers at Mach number M = 5 without and with wall cooling. The spreading of linear disturbances in these boundary layers is investigated and its relation to the transition process [2, 3] is discussed.The undisturbed stationary, two-dimensional base flow is obtained from the boundary layer equations for a perfect gas with a ratio of specific heats γ = 1.4 and a constant Prandtl number of P r = 0.72. At M = 5 inviscid instabilities are present in the boundary layer [1] which we compute with a local eigenvalue solver based on a shooting method [3]. The resulting complex dispersion relation ω(α), where ω = ω r + i ω i is the frequency and α = α r + i α i is the wavelength, is shown in Fig. 1 for the first and the second modes [1,5]. Eigensolutions propagating in oblique directions can be determined as if they were two-dimensional but with a base flow projected into their propagation direction [1].
Spreading of wave packets and transitionWe use the method of steepest descent [4] to determine the spreading of localised disturbances. The solutions are wave packets described by rays x/t = ∂ω/∂α with ∂ 2 ω/∂α 2 = 0 of constant growth α i x/t − ω i in the limit of time t → ∞. Since the method provides the solution for this limit and inviscid instabilities are eigensolutions far downstream in the boundary layer (also in the limit t → ∞) the method appears to be well suited for the problem.In the case of an adiabatic wall we analyse modes 1 and 2 separately. The results are shown in Fig. 2. For every ray the solution with largest growth represents the resulting wave packet. For the streamwise direction shown in Fig. 2, the solution of mode 2 shows higher growth rates throughout than the solution of mode 1. Thus mode 1 is negligible compared to mode 2, which dominates the wave packet.The amplification of higher modes by wall cooling T w = T ∞ results in wave packets of larger extent (Fig. 2). The packet has the special property of very high wave numbers at the trailing edge which propagates slo...