“…Thus "finite-amplitude" effects are essential to determine the value of U*. Examples of the latter type (say, type II) are the Benard convection (e.g., Chandrasekhar, 1961;Krishnamurti, 1970a, b), the Taylor vortex (Taylor, 1923;Coles, 1965;Burkhalter and Koschmieder, 1973), the baroclinic instability in a rotating annulus (Hide, 1969;King, 1979), and the barotropic instability in a rotating system ( Hide and Titman, 1967;Yamagata and Kimura, 1973;Kimura, 1976). For this type U* generally coincides with Uc.…”