Surface instability of icicles

Physical Review E - Statistical Physics, Plasmas, Fluids, and Related Interdisciplinary Topics

Volumn 66, Issue 4, 2002, Pages 11-

  Ogawa, Naohisa ^a   Furukawa, Yoshinori ^a  

^a HOKKAIDO UNIVERSITY   (Japan)

Author keywords

[No Author keywords available]

Indexed keywords

FLOW OF WATER; HEAT TRANSFER; HYDRODYNAMICS; LAMINAR FLOW; MELTING; SURFACE PHENOMENA; THERMAL DIFFUSION; THERMAL EFFECTS;

GAUSSIAN DISTRIBUTION; ICICLES; MELTING POINTS; SURFACE INSTABILITY;

ICE;

ARTICLE;

EID: 41349118486     PISSN: 1063651X     EISSN: None     Source Type: Journal    
DOI: 10.1103/PhysRevE.66.041202     Document Type: Article

References (24)

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24. The amplification rate of a wave (fluctuation) depends on its wavelength. Only the wave with the largest amplification rate can survive during the development of the fluctuations, and other modes will be observed as lower-amplitude noise. The constant rate of (Formula presented) means that the growth is exponential in time; hence, small differences in this constant result in large differences in the fluctuation amplitude at long times. In this sense, a mode distribution like that in Fig. 44 will be hidden in the external noise and thus not observed in experiments. This situation is the same as that in the original MS theory.