DO WE REALLY KNOW HOW TO SCALE THE TURBULENT KINETIC-ENERGY DISSIPATION-RATE-EPSILON DUE TO BREAKING OF OCEANIC INTERNAL WAVES

被引：69

作者：

GARGETT, AE

机构：

来源：

关键词：

D O I：

10.1029/JC095iC09p15971

中图分类号：

P7 [海洋学];

学科分类号：

0707 ;

摘要：

引用

页码：15971 / 15974

页数：4

共 18 条

[1]

CRAWFORD WR, 1986, J PHYS OCEANOGR, V16, P1847, DOI 10.1175/1520-0485(1986)016<1847:ACOLSA>2.0.CO

[2]

[3]

DASARO EA, 1985, J PHYS OCEANOGR, V15, P943, DOI 10.1175/1520-0485(1985)015<0943:UOTSIC>2.0.CO

[4]

DILLON, TM .

[6] ANISOTROPY OF TURBULENCE AT METEOR LEVEL [J].

DOUGHERTY, J .

JOURNAL OF ATMOSPHERIC AND TERRESTRIAL PHYSICS, 1961, 21 (2-3) :210-&

DUDA, TF ;

COX, CS .

JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1989, 94 (C1) :939-950

[8]

GARGETT AE, 1981, J PHYS OCEANOGR, V11, P1258, DOI 10.1175/1520-0485(1981)011<1258:ACSOVS>2.0.CO

[9]

[10] DISSIPATION AND DIFFUSION BY INTERNAL WAVE BREAKING [J].

GARGETT, AE ;

HOLLOWAY, G .