ROUGH SEA FOAM

被引:52
作者
NEWELL, AC
ZAKHAROV, VE
机构
[1] Arizona Center for Mathematical Sciences, University of Arizona, Tucson
关键词
D O I
10.1103/PhysRevLett.69.1149
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
A simple theory is developed for rough seas in which the energy cascade towards small scales is too much for a surface tension dominated wrinkling of the surface to handle. We suggest that a new phase, consisting of an air-water foam, is created and becomes the principal medium for energy dissipation. The foam depth and droplet size are calculated and we suggest how the predicted dependence on energy flux and surface tension could be verified experimentally.
引用
收藏
页码:1149 / 1151
页数:3
相关论文
共 9 条
[1]   ON THE NON-LINEAR ENERGY TRANSFER IN A GRAVITY-WAVE SPECTRUM .1. GENERAL THEORY [J].
HASSELMANN, K .
JOURNAL OF FLUID MECHANICS, 1962, 12 (04) :481-500
[2]  
KITAIGORODSKII SA, 1983, J PHYS OCEANOGR, V13, P816, DOI 10.1175/1520-0485(1983)013<0816:OTTOTE>2.0.CO
[3]  
2
[4]   THE EQUILIBRIUM RANGE IN THE SPECTRUM OF WIND-GENERATED WAVES [J].
PHILLIPS, OM .
JOURNAL OF FLUID MECHANICS, 1958, 4 (04) :426-433
[6]  
Toba Y., 1973, J OCEANOGRAPHICAL SO, V29, P209, DOI DOI 10.1007/BF02108528
[7]  
Zakharov V.E., 1967, J APPL MECH TECH PHY, V5, P310
[8]  
ZAKHAROV VE, 1966, SOV PHYS DOKL, V11, P881
[9]  
ZAKHAROV VE, 1991, IN PRESS P IUTAM C W