“…The response produces only a small disturbance from λ over the quasi-steady temporal scale (i) of §3 until a critical value λ = λ c is encountered at which stage (ii) weakly nonlinear amplification can occur ( §4), leading to strongly nonlinear evolution over the faster time scale (iii) of (2.4a-2.4d), (2.6a-2.6b). This is followed by finite-time blowup as in Smith (1988), Peridier, Smith & Walker (1991 which provokes the even faster evolution (iv) described by Davies, Bowles & Smith (2003) (see also Cassel & Conlisk (2014), Gargano, Sammartino, Sciacca & Cassel (2014)) with further restructuring and deep transition towards turbulence taking place. The time scales (i)-(iv) etc for response a are slow, fast, faster, faster, etc.…”