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- W396569860 abstract "Rayleigh-Benard convection (RBC) describes several phenomena of geophysical and industrial interest (Palm and Tveitereid, 1979; Ludvigsen, Palm and McKibbin, 1992; Dietsche and Muller, 1985), and has been studied extensively both theoretically and experimentally. The system has the advantage over many other nonequilibrium systems that theoretical and experimental results can be compared quantitatively, because the boundary conditions and stress parameters of the system can be accurately controlled in laboratory experiments. RBC has also played an important role in studies of pattern forming systems, because the system describes a richness of bifurcations and pattern stability problems (Palm, 1975; Swinney and Gollub, 1985; Manneville, 1990). For example, at the first bifurcation RBC often shows a transition from the basic structureless state to a pattern of two-dimensional rolls. At the next bifurcation it is commonly observed that rolls become unstable with respect to the Eckhaus instability (E) (Eckhaus, 1965) or the zigzag instability (ZZ) (Busse and Whitehead, 1971" @default.
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- W396569860 date "1996-01-01" @default.
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- W396569860 title "Rayleigh-Bénard Convection with Weak Shear Flow: Absolute and Convective Instabilities" @default.
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- W396569860 doi "https://doi.org/10.1007/978-94-009-0253-4_24" @default.
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